{"pageNumber":"811","pageRowStart":"20250","pageSize":"25","recordCount":46883,"records":[{"id":97166,"text":"sim3055 - 2008 - Hydrogeologic Framework of Onslow County, North Carolina, 2008","interactions":[],"lastModifiedDate":"2012-03-08T17:16:32","indexId":"sim3055","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3055","title":"Hydrogeologic Framework of Onslow County, North Carolina, 2008","docAbstract":"The unconsolidated sediments that underlie the Onslow County area are composed of interlayered permeable and impermeable beds, which overlie the crystalline basement rocks. The aquifers, composed mostly of sand and limestone, are separated by confining units composed mostly of clay and silt. The aquifers from top to bottom are the surficial, Castle Hayne, Beaufort, Peedee, Black Creek, and Upper and Lower Cape Fear aquifers. For this study, the Castle Hayne aquifer is informally divided into the upper and lower Castle Hayne aquifers.\r\n\r\nThe eight aquifers and seven confining units of the Tertiary and Cretaceous strata beneath Onslow County are presented in seven hydrogeologic sections. The hydrogeologic framework was refined from existing interpretations by using geophysical logs, driller's logs, and other available data from 123 wells and boreholes.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sim3055","collaboration":"Prepared in cooperation with the City of Jacksonville, Onslow Water and Sewer Authority, and U.S. Marine Corps, Camp Lejeune","usgsCitation":"Fine, J.M., 2008, Hydrogeologic Framework of Onslow County, North Carolina, 2008: U.S. Geological Survey Scientific Investigations Map 3055, Map Sheet: 32 x 32 inches, https://doi.org/10.3133/sim3055.","productDescription":"Map Sheet: 32 x 32 inches","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2008-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"links":[{"id":196181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12152,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3055/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.91666666666667,34.333333333333336 ], [ -77.91666666666667,35.166666666666664 ], [ -77,35.166666666666664 ], [ -77,34.333333333333336 ], [ -77.91666666666667,34.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628dc2","contributors":{"authors":[{"text":"Fine, Jason M. 0000-0002-6386-256X jmfine@usgs.gov","orcid":"https://orcid.org/0000-0002-6386-256X","contributorId":2238,"corporation":false,"usgs":true,"family":"Fine","given":"Jason","email":"jmfine@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97170,"text":"sim3035 - 2008 - Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona","interactions":[],"lastModifiedDate":"2017-03-29T12:11:43","indexId":"sim3035","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3035","title":"Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona","docAbstract":"This geologic map is the result of a cooperative effort of the U.S. Geological Survey, the National Park Service, the U.S. Forest Service, and the Bureau of Land Management (BLM) and the Kaibab-Paiute Tribe to provide a regional geologic database for resource management officials of all government and agencies, city municipalities, private enterprises, and individuals of this part of the Arizona Strip. The Arizona Strip is part of northwestern Arizona north of the Colorado River and bounded by the States of Nevada and Utah. Field work on the Kaibab-Paiute Indian Reservation was conducted from 2002 to 2005 with permission from the Kaibab-Paiute Tribal Government of that administration and permission was granted to publish a geologic map of 4 quadrangles online (Billingsley and others, 2004). The Kaibab-Paiute Tribal government of 2006 to 2008 requested that all geologic information within the Kaibab-Paiute Indian Reservation not be published as part of the Fredonia 30' x 60' quadrangle (this publication). For further information, contact the Kaibab-Paiute Tribal government at HC 65 Box 2, Fredonia, Arizona, 86022, telephone # (928) 643-7245. Visitors to the Kaibab-Paiute Indian Reservation are required to obtain a permit and permission for access from the Tribal Offices at the junction of State Highway 389 and the paved road leading to Pipe Spring National Monument. \r\n\r\nThe Fredonia 30' x 60' quadrangle encompasses approximately 5,018 km2 (1,960 mi2) within Mohave and Coconino Counties, northern Arizona and is bounded by longitude 112 deg to 113 deg W., and latitude 36 deg 30' to 37 deg N. The map area lies within the southern Colorado Plateaus geologic province (herein Colorado Plateau). The map area is locally subdivided into seven physiographic parts: the Grand Canyon (Kanab Canyon and its tributaries), Kanab Plateau, Uinkaret Plateau, Kaibab Plateau, Paria Plateau, House Rock Valley, and Moccasin Mountains as defined by Billingsley and others, 1997, (fig. 1). Elevations range from 2,737 m (8,980 ft) just west of State Highway 67 on the Kaibab Plateau, southeast corner of the map area to about 927 m (3,040 ft) in Kanab Canyon, south-central edge of the map area. \r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim3035","collaboration":"Prepared in cooperation with the National Park Service, U.S. Forest Service, and Bureau of Land Management","usgsCitation":"Billingsley, G.H., Priest, S.S., and Felger, T.J., 2008, Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona (Version 1.0): U.S. Geological Survey Scientific Investigations Map 3035, Report: ii, 23 p.; Map Sheet: 49.5 x 36 inches; GIS files, https://doi.org/10.3133/sim3035.","productDescription":"Report: ii, 23 p.; Map Sheet: 49.5 x 36 inches; GIS files","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110801,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86238.htm","linkFileType":{"id":5,"text":"html"},"description":"86238"},{"id":12155,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3035/","linkFileType":{"id":5,"text":"html"}},{"id":196268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","projection":"Universal Transverse Mercator","country":"United States","state":"Arizona","county":"Coconino County, Mohave County","city":"Fredonia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113,36.5 ], [ -113,37 ], [ -112,37 ], [ -112,36.5 ], [ -113,36.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8506","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":301241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":30204,"corporation":false,"usgs":true,"family":"Priest","given":"Susan","email":"spriest@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":301242,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Felger, Tracey J. 0000-0003-0841-4235 tfelger@usgs.gov","orcid":"https://orcid.org/0000-0003-0841-4235","contributorId":1117,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","email":"tfelger@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":301240,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97163,"text":"ds387 - 2008 - Ground-water quality data in the coastal Los Angeles Basin study unit, 2006: Results from the California GAMA Program","interactions":[],"lastModifiedDate":"2022-07-05T18:17:33.675636","indexId":"ds387","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"387","title":"Ground-water quality data in the coastal Los Angeles Basin study unit, 2006: Results from the California GAMA Program","docAbstract":"Ground-water quality in the approximately 860 square-mile Coastal Los Angeles Basin study unit (CLAB) was investigated from June to November of 2006 as part of the Statewide Basin Assessment Project of the Ground-Water Ambient Monitoring and Assessment (GAMA) Program. The GAMA Statewide Basin Assessment was developed in response to the Ground-Water Quality Monitoring Act of 2001, and is being conducted by the U.S. Geological Survey (USGS) in cooperation with the California State Water Resources Control Board (SWRCB).\r\n\r\nThe Coastal Los Angeles Basin study was designed to provide a spatially unbiased assessment of raw ground-water quality within CLAB, as well as a statistically consistent basis for comparing water quality throughout California. Samples were collected from 69 wells in Los Angeles and Orange Counties. Fifty-five of the wells were selected using a spatially distributed, randomized grid-based method to provide statistical representation of the study area (?grid wells?). Fourteen additional wells were selected to evaluate changes in ground-water chemistry or to gain a greater understanding of the ground-water quality within a specific portion of the Coastal Los Angeles Basin study unit ('understanding wells').\r\n\r\nGround-water samples were analyzed for: a large number of synthetic organic constituents [volatile organic compounds (VOCs), gasoline oxygenates and their degradates, pesticides, polar pesticides, and pesticide degradates, pharmaceutical compounds, and potential wastewater-indicators]; constituents of special interest [perchlorate, N-nitrosodimethylamine (NDMA), 1,4-dioxane, and 1,2,3-trichloropropane (1,2,3-TCP)]; inorganic constituents that can occur naturally [nutrients, major and minor ions, and trace elements]; radioactive constituents [gross-alpha and gross-beta radiation, radium isotopes, and radon-222]; and microbial indicators. Naturally occurring isotopes [stable isotopic ratios of hydrogen and oxygen, and activities of tritium and carbon-14] and dissolved noble gases also were measured to help identify the sources and ages of the sampled ground water.\r\n\r\nQuality-control samples (blanks, replicates, and samples for matrix spikes) were collected at approximately one-fourth of the wells, and the results for these samples were used to evaluate the quality of the data for the ground-water samples. Field blanks rarely contained detectable concentrations of any constituent, suggesting that contamination was not a significant source of bias. Differences between replicate samples were within acceptable ranges, indicating acceptably low variability. Matrix spike recoveries were within acceptable ranges for most compounds. Assessment of the quality-control information resulted in applying ?V? codes to approximately 0.1 percent of the data collected for ground-water samples (meaning a constituent was detected in blanks as well as the corresponding environmental data).\r\n\r\nThis study did not attempt to evaluate the quality of drinking water delivered to consumers; after withdrawal from the ground, water typically is treated, disinfected, and (or) blended with other waters to maintain acceptable drinking-water quality. Regulatory thresholds are applied to the treated drinking water that is served to the consumer, not to raw ground water. However, to provide some context for the results, concentrations of constituents measured in the raw ground water were compared with regulatory and non-regulatory health-based thresholds established by the U.S. Environmental Protection Agency (USEPA), California Department of Public Health (CDPH, formerly California Department of Health Services [CADHS]) and thresholds established for aesthetic concerns (secondary maximum contaminant levels, SMCL-CA) by CDPH. Comparisons between data collected for this study and drinking-water thresholds are for illustrative purposes only, and are not indicative of compliance or non-compliance with those thresholds.\r\n\r\nVOCs were detected in alm","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds387","collaboration":"Prepared in cooperation with the California State Water Resources Control Board","usgsCitation":"Mathany, T., Land, M., and Belitz, K., 2008, Ground-water quality data in the coastal Los Angeles Basin study unit, 2006: Results from the California GAMA Program (Version 1.1, Revised Mar 2009): U.S. Geological Survey Data Series 387, x, 98 p., https://doi.org/10.3133/ds387.","productDescription":"x, 98 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":195553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402999,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86219.htm","linkFileType":{"id":5,"text":"html"}},{"id":12149,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/387/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Los Angeles Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.75146484375,\n              33.62376800118811\n            ],\n            [\n              -117.520751953125,\n              34.134541681937364\n            ],\n            [\n              -117.861328125,\n              34.252676117101515\n            ],\n            [\n              -118.43261718749999,\n              34.37064492478658\n            ],\n            [\n              -118.69628906249999,\n              34.27083595165\n            ],\n            [\n              -118.99291992187499,\n              34.17090836352573\n            ],\n            [\n              -118.91601562499999,\n              34.016241889667015\n            ],\n            [\n              -118.50952148437499,\n              33.99802726234877\n            ],\n            [\n              -118.377685546875,\n              33.715201644740844\n            ],\n            [\n              -118.0810546875,\n              33.706062655101206\n            ],\n            [\n              -117.88330078125,\n              33.55055114384406\n            ],\n            [\n              -117.75146484375,\n              33.62376800118811\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.1, Revised Mar 2009","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d53e","contributors":{"authors":[{"text":"Mathany, Timothy M. 0000-0002-4747-5113","orcid":"https://orcid.org/0000-0002-4747-5113","contributorId":99949,"corporation":false,"usgs":true,"family":"Mathany","given":"Timothy M.","affiliations":[],"preferred":false,"id":301228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":301227,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":301226,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97143,"text":"sir20075101 - 2008 - The coral reef of South Moloka'i, Hawai'i— Portrait of a sediment-threatened fringing reef","interactions":[],"lastModifiedDate":"2021-11-05T20:40:57.850638","indexId":"sir20075101","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2007-5101","title":"The coral reef of South Moloka'i, Hawai'i— Portrait of a sediment-threatened fringing reef","docAbstract":"<p>Moloka‘i, with the most extensive coral reef in the main Hawaiian Islands, is especially sacred to Hina, the Goddess of the Moon. As Hinaalo, she is the Mother of the Hawaiian people; as Hinapuku‘a, she is the Goddess of Fishermen; and in the form Hina‘opuhalako‘a, she is the Goddess who gave birth to coral, coral reefs, and all spiny marine organisms. Interdependence between the reef’s living resources, the people, and their cosmology was the basis for management of Moloka‘i’s coastal waters for over a thousand years.</p><p><span>The ancient residents of Moloka‘i built the greatest concentration of fishponds known anywhere, but their mastery of mariculture, something needed now more than ever, was lost after near genocide from exotic Western diseases. Subsequent destruction of the native vegetation for exotic cattle, goats, pigs, sugar cane, and pineapple caused soil erosion and sedimentation on the reef flat. This masterful volume clearly documents that soil washing into the sea is the major threat to the reef today. Abandoned fishponds, choked with sediment, now act as barriers and mud traps, making damage to corals less than it would otherwise would have been.</span></p><p><span>The role of mud and freshwater from land in preventing coral reef growth, clearly articulated in Charles Darwin’s first book, The Structure and Distribution of Coral Reefs, is the major theme of this book. All around the tropics, coral reefs have died from huge increases in terrestrial sedimentation that resulted from destruction of hillside forests for cash-crop agriculture and pastures in the colonial era, especially in Latin America, Asia, and the islands of the Caribbean and Indo-Pacific. It is obvious that one cannot manage the coastal zone as a unit separate from the watersheds that drain into it. Yet there has been surprisingly little comprehensive scientific study of these impacts.</span></p><p><span>In this landmark volume, U.S. Geological Survey researchers and their colleagues have developed and applied a remarkably integrated approach to the reefs of Moloka‘i, combining geology, oceanography, and biology to provide an in-depth understanding of the processes that have made these reefs grow and that now limit them. They have joined old fashioned natural history of marine animals and plants with study of the geological evolution of the island, hydrology, meteorology, and land-use history, to an arsenal of new methods of remote sensing, including aerial photography, laser ranging, infrared thermal mapping, seismic reflection, in-situ instrumentation to measure chemical parameters of water quality, and direct measurements of the physical driving forces affecting them—such as wave energy, currents, sedimentation, and sediment transport. They provide a level of documentation and insight that has never been available for any reef before.</span></p><p><span>A remarkable feature of this book is that it is aimed at the people of Moloka‘i to inform them of what is happening to their reef and what they might do to preserve their vital resources. The scientific data and interpretations are expressed in unusually clear and comprehensible language, free of the professional jargon that makes most technical publications impenetrable to the public that most needs to know about them, yet without loss of scientific rigor.</span></p><p><span>Here readers will see clearly explained the whole path of soil loss, from the impacts of wild pigs and goats at higher elevations, deforestation of the hills for cattle pasture at lower levels, and denudation of low lands for cash crops. The resulting biological impoverishment has bared the soils, which wash away in flash storms, smothering the inshore reefs, whose growth was already limited because they had grown right up to sea level. The data in this book show that the mud doesn’t get far if it is washed into the sea during a big storm with heavy waves. Afterwards this mud keeps getting stirred up by every succeeding storm, spreading and affecting corals over wider areas until it is finally washed out of the system—and that only happens if there is no more new mud washing onto the reef.</span></p><p><span>I saw this myself a few years ago in Pila‘a Bay on Kaua‘i, where a bulldozed hillside of abandoned sugar cane fields had slumped right on top of a coral reef following exceptional rains. Years later, the algae species were zoned in a way that clearly mapped the distribution of nutrients washed into the bay, most likely from fertilizers bound to the eroded soils. That pattern closely mimics, on a small scale, that shown in Moloka‘i in this volume, where the inner reef is covered with algae, zoned by species in a way that points to land-based sources of nutrients, while the outermost reef slope is still coral dominated, and the deep algae seem to indicate deep-water nutrient upwelling.</span></p><p><span>What of the future? The Hawaiian Islands have been exceptionally fortunate to be spared the worst coral heatstroke death from high temperatures, at least to date. So far, the worst global warming impacts have luckily been small in this region, and the small number of people on Moloka‘i has kept population densities, and sewage pollution, low compared to the more developed islands. Nutrients from years of sugar and pineapple fertilization, and the washing of this soil onto the reefs, show clear influences on the pattern of algae on the reef. Even at very low levels of nutrients, well below that which drives algae to smother and kill coral reefs, more algae is present. Soil erosion control is therefore the key to better management of both nutrients and turbidity on Moloka‘i reefs. To that end land management actions mentioned in this book, such as suppressing wild fires and eliminating wild goats and pigs, could be made even more effective if supplemented by active erosion control using plants whose roots bind the soil effectively in place. Through all of these efforts, Hina and the people of Moloka‘i could be happy again!</span><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20075101","isbn":"1411322886","usgsCitation":"2008, The coral reef of South Moloka'i, Hawai'i— Portrait of a sediment-threatened fringing reef (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2007-5101, vi, 190 p., https://doi.org/10.3133/sir20075101.","productDescription":"vi, 190 p.","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":196394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20075101.JPG"},{"id":391450,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85395.htm"},{"id":12128,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5101/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawaii","otherGeospatial":"South Molokai Reef","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.7762756347656,\n              21.21514025408941\n            ],\n            [\n              -156.89712524414062,\n              21.20105715553566\n            ],\n            [\n              -157.02621459960935,\n              21.24074244508678\n            ],\n            [\n              -157.30224609375,\n              21.249702161806933\n            ],\n            [\n              -157.30224609375,\n              21.185692243796037\n            ],\n            [\n              -157.34344482421875,\n              21.09346926561652\n            ],\n            [\n              -157.18139648437497,\n              21.04861794324536\n            ],\n            [\n              -157.10037231445312,\n              21.074248926792812\n            ],\n            [\n              -157.03445434570312,\n              21.04477291496186\n            ],\n            [\n              -156.94793701171872,\n              21.025546284581797\n            ],\n            [\n              -156.84219360351562,\n              21.021700660816588\n            ],\n            [\n              -156.73095703125,\n              21.06399706324597\n            ],\n            [\n              -156.66366577148438,\n              21.140868798573788\n            ],\n            [\n              -156.68975830078125,\n              21.197216077387107\n            ],\n            [\n              -156.7762756347656,\n              21.21514025408941\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb66","contributors":{"editors":[{"text":"Field, Michael E. mfield@usgs.gov","contributorId":2101,"corporation":false,"usgs":true,"family":"Field","given":"Michael","email":"mfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":579481,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Cochran, Susan A. 0000-0002-2442-8787 scochran@usgs.gov","orcid":"https://orcid.org/0000-0002-2442-8787","contributorId":2062,"corporation":false,"usgs":true,"family":"Cochran","given":"Susan A.","email":"scochran@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":579482,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Logan, Joshua B. 0000-0002-6191-4119 jlogan@usgs.gov","orcid":"https://orcid.org/0000-0002-6191-4119","contributorId":2335,"corporation":false,"usgs":true,"family":"Logan","given":"Joshua","email":"jlogan@usgs.gov","middleInitial":"B.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":579483,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Storlazzi, Curt D. 0000-0001-8057-4490 cstorlazzi@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-4490","contributorId":2333,"corporation":false,"usgs":true,"family":"Storlazzi","given":"Curt D.","email":"cstorlazzi@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":579484,"contributorType":{"id":2,"text":"Editors"},"rank":4}]}}
,{"id":97156,"text":"sim3058 - 2008 - Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008","interactions":[],"lastModifiedDate":"2017-01-11T12:22:21","indexId":"sim3058","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3058","title":"Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008","docAbstract":"The U.S. Geological Survey (USGS) - in cooperation with the Troup County Board of Commissioners - conducted a well inventory to provide information to help evaluate ground-water resources for Troup County, Georgia. In addition, borehole geophysical logs were collected in selected wells to provide a better understanding of the subsurface geologic and water-bearing characteristics in specific areas of interest. This investigation provides information to help guide future ground-water development and water-management decisions for Troup County while enhancing understanding of the hydrogeology of fractured rocks in the Piedmont physiographic province. This report presents well data compiled from USGS files and from site visits to wells during November and December 2007. Data were entered into the USGS National Water Information System (NWIS) and made available on the Web at http://waterdata.usgs.gov/ga/nwis/inventory.\r\n\r\nPrevious studies of ground-water resources have been conducted in the vicinity, but did not include Troup County. The ground-water resources of Heard and Coweta Counties, located north and northeast, respectively, of Troup County were part of a larger study by Cressler and others (1983) that encompassed the Greater Atlanta Region. That study evaluated the quantity and quality of ground water in the Atlanta region and described the methods that could be used for locating high-yielding wells in the Piedmont Province. The geology underlying the Atlanta area is similar to that underlying Troup County. Clarke and Peck (1990) conducted a similar investigation that included Meriwether and Coweta Counties, located to the east and northeast of Troup County.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sim3058","collaboration":"Prepared in cooperation with the Troup County Board of Commissioners","usgsCitation":"Peck, M., Leeth, D.C., and Hamrick, M.D., 2008, Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008: U.S. Geological Survey Scientific Investigations Map 3058, Map Sheet: 42 x 32 inches, https://doi.org/10.3133/sim3058.","productDescription":"Map Sheet: 42 x 32 inches","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2007-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":195700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12141,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3058/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","county":"Troup County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.33333333333333,32.833333333333336 ], [ -85.33333333333333,33.25 ], [ -84.83333333333333,33.25 ], [ -84.83333333333333,32.833333333333336 ], [ -85.33333333333333,32.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0c51","contributors":{"authors":[{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":301208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leeth, David C. cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":301207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamrick, Michael D. hamrick@usgs.gov","contributorId":3237,"corporation":false,"usgs":true,"family":"Hamrick","given":"Michael","email":"hamrick@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301209,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97157,"text":"sir20065171 - 2008 - Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority","interactions":[],"lastModifiedDate":"2012-03-08T17:16:26","indexId":"sir20065171","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5171","title":"Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority","docAbstract":"Chemical modeling was used by the U.S. Geological Survey, in cooperation with the Albuquerque Bernalillo County Water Utility Authority (henceforth, Authority), to gain insight into the potential chemical effects that could occur in the Authority's water distribution system as a result of changing the source of water used for municipal and industrial supply from ground water to surface water, or to some mixture of the two sources. From historical data, representative samples of ground-water and surface-water chemistry were selected for modeling under a range of environmental conditions anticipated to be present in the distribution system. Mineral phases calculated to have the potential to precipitate from ground water were compared with the compositions of precipitate samples collected from the current water distribution system and with mineral phases calculated to have the potential to precipitate from surface water and ground-water/surface-water mixtures.\r\n\r\nSeveral minerals that were calculated to have the potential to precipitate from ground water in the current distribution system were identified in precipitate samples from pipes, reservoirs, and water heaters. These minerals were the calcium carbonates aragonite and calcite, and the iron oxides/hydroxides goethite, hematite, and lepidocrocite. Several other minerals that were indicated by modeling to have the potential to precipitate were not found in precipitate samples. For most of these minerals, either the kinetics of formation were known to be unfavorable under conditions present in the distribution system or the minerals typically are not formed through direct precipitation from aqueous solutions.\r\n\r\nThe minerals with potential to precipitate as simulated for surface-water samples and ground-water/surface-water mixtures were quite similar to the minerals with potential to precipitate from ground-water samples. Based on the modeling results along with kinetic considerations, minerals that appear most likely to either dissolve or newly precipitate when surface water or ground-water/surface-water mixtures are delivered through the Authority's current distribution system are carbonates (particularly aragonite and calcite). Other types of minerals having the potential to dissolve or newly precipitate under conditions present throughout most of the distribution system include a form of silica, an aluminum hyroxide (gibbsite or diaspore), or the Fe-containing mineral Fe3(OH)8. Dissolution of most of these minerals (except perhaps the Fe-containing minerals) is not likely to substantially affect trace-element concentrations or aesthetic characteristics of delivered water, except perhaps hardness. Precipitation of these minerals would probably be of concern only if the quantities of material involved were large enough to clog pipes or fixtures. The mineral Fe3(OH)8 was not found in the current distribution system. Some Fe-containing minerals that were identified in the distribution system were associated with relatively high contents of selected elements, including As, Cr, Cu, Mn, Pb, and Zn. However, these Fe-containing minerals were not identified as minerals likely to dissolve when the source of water was changed from ground water to surface water or a ground-water/surface-water mixture.\r\n\r\nBased on the modeled potential for calcite precipitation and additional calculations of corrosion indices ground water, surface water, and ground-water/surface-water mixtures are not likely to differ greatly in corrosion potential. In particular, surface water and ground-water/surface-water mixtures do not appear likely to dissolve large quantities of existing calcite and expose metal surfaces in the distribution system to substantially increased corrosion. Instead, modeling calculations indicate that somewhat larger masses of material would tend to precipitate from surface water or ground-water/surface-water mixtures compared to ground water alone.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065171","isbn":"9781411311367","collaboration":"Prepared in cooperation with the Albuquerque Bernalillo County Water Utility Authority","usgsCitation":"Bexfield, L.M., and Anderholm, S.K., 2008, Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5171, iv, 49 p., https://doi.org/10.3133/sir20065171.","productDescription":"iv, 49 p.","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":195578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12142,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5171/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.83333333333333,35 ], [ -106.83333333333333,35.25 ], [ -106.41666666666667,35.25 ], [ -106.41666666666667,35 ], [ -106.83333333333333,35 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c163","contributors":{"authors":[{"text":"Bexfield, Laura M. 0000-0002-1789-654X bexfield@usgs.gov","orcid":"https://orcid.org/0000-0002-1789-654X","contributorId":1273,"corporation":false,"usgs":true,"family":"Bexfield","given":"Laura","email":"bexfield@usgs.gov","middleInitial":"M.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderholm, Scott K.","contributorId":94270,"corporation":false,"usgs":true,"family":"Anderholm","given":"Scott","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":301211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97154,"text":"sir20085220 - 2008 - Methods to Evaluate Influence of Onsite Septic Wastewater-Treatment Systems on Base Flow in Selected Watersheds in Gwinnett County, Georgia, October 2007","interactions":[],"lastModifiedDate":"2017-01-17T10:09:37","indexId":"sir20085220","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5220","title":"Methods to Evaluate Influence of Onsite Septic Wastewater-Treatment Systems on Base Flow in Selected Watersheds in Gwinnett County, Georgia, October 2007","docAbstract":"The influence of onsite septic wastewater-treatment systems (OWTS) on base-flow quantity needs to be understood to evaluate consumptive use of surface-water resources by OWTS. If the influence of OWTS on stream base flow can be measured and if the inflow to OWTS is known from water-use data, then water-budget approaches can be used to evaluate consumptive use. This report presents a method to evaluate the influence of OWTS on ground-water recharge and base-flow quantity. Base flow was measured in Gwinnett County, Georgia, during an extreme drought in October 2007 in 12 watersheds that have low densities of OWTS (22 to 96 per square mile) and 12 watersheds that have high densities (229 to 965 per square mile) of OWTS. Mean base-flow yield in the high-density OWTS watersheds is 90 percent greater than in the low-density OWTS watersheds. The density of OWTS is statistically significant (p-value less than 0.01) in relation to base-flow yield as well as specific conductance. Specific conductance of base flow increases with OWTS density, which may indicate influence from treated wastewater. The study results indicate considerable unexplained variation in measured base-flow yield for reasons that may include: unmeasured processes, a limited dataset, and measurement errors. Ground-water recharge from a high density of OWTS is assumed to be steady state from year to year so that the annual amount of increase in base flow from OWTS is expected to be constant. In dry years, however, OWTS contributions represent a larger percentage of natural base flow than in wet years. The approach of this study could be combined with water-use data and analyses to estimate consumptive use of OWTS.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20085220","collaboration":"Prepared in cooperation with the Georgia Environmental Protection Division","usgsCitation":"Landers, M.N., and Ankcorn, P.D., 2008, Methods to Evaluate Influence of Onsite Septic Wastewater-Treatment Systems on Base Flow in Selected Watersheds in Gwinnett County, Georgia, October 2007: U.S. Geological Survey Scientific Investigations Report 2008-5220, iv, 12 p., https://doi.org/10.3133/sir20085220.","productDescription":"iv, 12 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2007-10-16","temporalEnd":"2007-10-17","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":197897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12139,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5220/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","county":"Gwinnett County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.26666666666667,33.733333333333334 ], [ -84.26666666666667,34.166666666666664 ], [ -83.75,34.166666666666664 ], [ -83.75,33.733333333333334 ], [ -84.26666666666667,33.733333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62cca1","contributors":{"authors":[{"text":"Landers, Mark N. 0000-0002-3014-0480 landers@usgs.gov","orcid":"https://orcid.org/0000-0002-3014-0480","contributorId":1103,"corporation":false,"usgs":true,"family":"Landers","given":"Mark","email":"landers@usgs.gov","middleInitial":"N.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":301203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ankcorn, Paul D. pankcorn@usgs.gov","contributorId":1447,"corporation":false,"usgs":true,"family":"Ankcorn","given":"Paul","email":"pankcorn@usgs.gov","middleInitial":"D.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97160,"text":"fs20083095 - 2008 - Management and research applications of long-range surveillance radar data for birds, bats, and flying insects","interactions":[],"lastModifiedDate":"2019-09-20T10:07:27","indexId":"fs20083095","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3095","displayTitle":"Management and Research Applications of Long-range Surveillance Radar Data for Birds, Bats, and Flying Insects","title":"Management and research applications of long-range surveillance radar data for birds, bats, and flying insects","docAbstract":"There is renewed interest in using long-range surveillance radar as a biological research tool due to substantial improvements in the network of radars within the United States. Technical improvements, the digital nature of the radar data, and the availability of computing power and geographic information systems, enable a broad range of biological applications. This publication provides a summary of long-range surveillance radar technology and applications of these data to questions about movement patterns of birds and other flying wildlife. The intended audience is potential radar-data end users, including natural-resource management and regulatory agencies, conservation organizations, and industry. This summary includes a definition of long-range surveillance radar, descriptions of its strengths and weaknesses, information on applications of the data, cost, methods of calibration, and what end users need to do, and some key references and resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20083095","usgsCitation":"Ruth, J.M., Buler, J., Diehl, R.H., and Sojda, R.S., 2008, Management and research applications of long-range surveillance radar data for birds, bats, and flying insects (Version 1.0): U.S. Geological Survey Fact Sheet 2008-3095, 4 p., https://doi.org/10.3133/fs20083095.","productDescription":"4 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":121084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3095.jpg"},{"id":367582,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2008/3095/pdf/FS08-3095_508.pdf"},{"id":12145,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3095/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.8277587890625,\n              27.22044113007616\n            ],\n            [\n              -96.74011230468749,\n              27.22044113007616\n            ],\n            [\n              -96.74011230468749,\n              28.001676807403094\n            ],\n            [\n              -97.8277587890625,\n              28.001676807403094\n            ],\n            [\n              -97.8277587890625,\n              27.22044113007616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1e4","contributors":{"authors":[{"text":"Ruth, Janet M. 0000-0003-1576-5957 janet_ruth@usgs.gov","orcid":"https://orcid.org/0000-0003-1576-5957","contributorId":1408,"corporation":false,"usgs":true,"family":"Ruth","given":"Janet","email":"janet_ruth@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":301219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buler, Jeffrey J.","contributorId":78431,"corporation":false,"usgs":true,"family":"Buler","given":"Jeffrey J.","affiliations":[],"preferred":false,"id":301222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diehl, Robert H. 0000-0001-9141-1734 rhdiehl@usgs.gov","orcid":"https://orcid.org/0000-0001-9141-1734","contributorId":3396,"corporation":false,"usgs":true,"family":"Diehl","given":"Robert","email":"rhdiehl@usgs.gov","middleInitial":"H.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":301221,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sojda, Richard S. sojda@usgs.gov","contributorId":1663,"corporation":false,"usgs":true,"family":"Sojda","given":"Richard","email":"sojda@usgs.gov","middleInitial":"S.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":301220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97144,"text":"ofr20081312 - 2008 - Sediment deposition, erosion, and bathymetric change in central San Francisco Bay:  1855-1979","interactions":[],"lastModifiedDate":"2022-07-07T21:02:11.523395","indexId":"ofr20081312","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1312","title":"Sediment deposition, erosion, and bathymetric change in central San Francisco Bay:  1855-1979","docAbstract":"<p>Central San Francisco Bay is the hub of a dynamic estuarine system connecting the San Joaquin and Sacramento River Deltas, Suisun Bay, and San Pablo Bay to the Pacific Ocean and South San Francisco Bay. To understand the role that Central San Francisco Bay plays in sediment transport throughout the system, it is necessary to first determine historical changes in patterns of sediment deposition and erosion from both natural and anthropogenic forces.</p><p>The first extensive hydrographic survey of Central San Francisco Bay was conducted in 1853 by the National Ocean Service (NOS) (formerly the United States Coast and Geodetic Survey (USCGS)). From 1894 to 1979, four additional surveys, composed of a total of approximately 700,000 bathymetric soundings, were collected within Central San Francisco Bay. Converting these soundings into accurate bathymetric models involved many steps. The soundings were either hand digitized directly from the original USCGS and NOS hydrographic sheets (H-sheets) or obtained digitally from the National Geophysical Data Center's (NGDC) Geophysical Data System (GEODAS) (National Geophysical Data Center, 1996). Soundings were supplemented with contours that were either taken directly from the H-sheets or added in by hand. Shorelines and marsh areas were obtained from topographic sheets. The digitized soundings, depth contours, shorelines, and marsh areas were entered into a geographic information system (GIS) and georeferenced to a common horizontal datum. Using surface modeling software, bathymetric grids with a horizontal resolution of 25 m were developed for each of the five hydrographic surveys. Before analyses of sediment deposition and erosion were conducted, interpolation bias was removed and all of the grids were converted to a common vertical datum. These bathymetric grids were then used to develop bathymetric change maps for subsequent survey periods and to determine long-term changes in deposition and erosion by calculating volumes and rates of net sediment change.</p><p>Central San Francisco Bay experienced periods of both deposition and erosion, but overall experienced a net gain in sediment from 1855 to 1979 of approximately 42x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>(0.33x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>/ yr). Over this same time period, 92 percent of the tidal marsh and 69 percent of the intertidal mudflats were lost as human activity increased and the shorefront was developed. During the first time period, from 1855 to 1895, Central San Francisco Bay was erosional, losing roughly 2x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>/ yr of sediment. The next time period was depositional, with a net gain of approximately 3x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>/ yr of sediment from 1895 to 1947. The last time period, from 1947 to 1979, was erosional again, losing roughly 2x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>/ yr of sediment. Sedimentation patterns also varied spatially. The northern part of Central San Francisco Bay was depositional during all change periods while the eastern region alternated between erosional and depositional.</p><p>Central San Francisco Bay sedimentation patterns have also been strongly impacted by anthropogenic activities, such as dredging and dredge disposal, borrow pits, and sand mining. For example, bathymetric change at a borrow pit created near Bay Farm Island sometime between the 1947 and 1979 surveys indicates roughly 25x10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup><span>&nbsp;</span>of sediment was removed from the system</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081312","usgsCitation":"Fregoso, T.A., Foxgrover, A., and Jaffe, B.E., 2008, Sediment deposition, erosion, and bathymetric change in central San Francisco Bay:  1855-1979 (Version 1.0): U.S. Geological Survey Open-File Report 2008-1312, v, 41 p., https://doi.org/10.3133/ofr20081312.","productDescription":"v, 41 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true}],"links":[{"id":195699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20081312.PNG"},{"id":316660,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2008/1312/of2008-1312.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":12129,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1312/","linkFileType":{"id":5,"text":"html"}},{"id":403237,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85394.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.59368896484374,\n              37.69903420794415\n            ],\n            [\n              -122.18719482421874,\n              37.69903420794415\n            ],\n            [\n              -122.18719482421874,\n              37.99183365313853\n            ],\n            [\n              -122.59368896484374,\n              37.99183365313853\n            ],\n            [\n              -122.59368896484374,\n              37.69903420794415\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc167","contributors":{"authors":[{"text":"Fregoso, Theresa A.","contributorId":67181,"corporation":false,"usgs":true,"family":"Fregoso","given":"Theresa","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":301151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foxgrover, Amy C.","contributorId":45775,"corporation":false,"usgs":true,"family":"Foxgrover","given":"Amy C.","affiliations":[],"preferred":false,"id":301150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jaffe, Bruce E. 0000-0002-8816-5920 bjaffe@usgs.gov","orcid":"https://orcid.org/0000-0002-8816-5920","contributorId":2049,"corporation":false,"usgs":true,"family":"Jaffe","given":"Bruce","email":"bjaffe@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":301149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97153,"text":"fs20083099 - 2008 - Hydrologic Streamflow Conditions for Georgia, 2007","interactions":[],"lastModifiedDate":"2016-12-07T09:56:59","indexId":"fs20083099","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3099","title":"Hydrologic Streamflow Conditions for Georgia, 2007","docAbstract":"The U.S. Geologic Survey (USGS) Georgia Water Science Center (GaWSC) maintains a long-term hydrologic monitoring network of more than 260 real-time streamflow stations and more than 100 noncontinuous streamflow stations throughout Georgia. This network is operated by the USGS GaWSC in cooperation with more than 50 different partners at Federal, State, and local government levels. One of the many benefits of data collected from this monitoring network is that it allows for the analysis of the overall hydrologic condition of streams and lakes of Georgia.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20083099","usgsCitation":"Knaak, A.E., and Joiner, J.K., 2008, Hydrologic Streamflow Conditions for Georgia, 2007: U.S. Geological Survey Fact Sheet 2008-3099, 4 p. (available as 11 x 17 or 8.5 x 11), https://doi.org/10.3133/fs20083099.","productDescription":"4 p. (available as 11 x 17 or 8.5 x 11)","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2006-10-01","temporalEnd":"2007-09-30","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":121156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3099.jpg"},{"id":12138,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3099/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.810477,34.987607],[-83.619985,34.986592],[-83.620185,34.992091],[-83.108714,35.000768],[-83.1046,34.992783],[-83.106991,34.98272],[-83.120387,34.968406],[-83.12114,34.958966],[-83.127035,34.953778],[-83.120502,34.941262],[-83.122585,34.938062],[-83.12807,34.938113],[-83.140621,34.924915],[-83.153253,34.926342],[-83.160937,34.918269],[-83.168524,34.91788],[-83.186541,34.899534],[-83.203351,34.893717],[-83.201183,34.884653],[-83.205627,34.880142],[-83.213323,34.882796],[-83.220099,34.878124],[-83.23751,34.877057],[-83.238419,34.869771],[-83.245602,34.865522],[-83.255718,34.845592],[-83.267656,34.845289],[-83.268159,34.821393],[-83.275656,34.816862],[-83.289914,34.824477],[-83.294292,34.814725],[-83.301368,34.814154],[-83.301182,34.804008],[-83.313782,34.799911],[-83.323866,34.789712],[-83.320062,34.759616],[-83.348829,34.737194],[-83.353238,34.728648],[-83.349411,34.697575],[-83.339029,34.683807],[-83.321463,34.677543],[-83.316401,34.669316],[-83.304641,34.669561],[-83.292883,34.654196],[-83.27796,34.644853],[-83.255281,34.637696],[-83.240669,34.624507],[-83.243381,34.617997],[-83.23178,34.611297],[-83.169994,34.605444],[-83.170278,34.592398],[-83.154577,34.588198],[-83.152577,34.578299],[-83.122901,34.560129],[-83.103987,34.540166],[-83.103176,34.533406],[-83.084855,34.530967],[-83.078113,34.524837],[-83.086861,34.517798],[-83.069451,34.502131],[-83.054463,34.50289],[-83.034712,34.483495],[-83.002924,34.472132],[-82.99509,34.472483],[-82.992671,34.479072],[-82.979568,34.482702],[-82.960668,34.482002],[-82.954667,34.477302],[-82.940867,34.486102],[-82.922866,34.481402],[-82.902665,34.485902],[-82.876864,34.475303],[-82.873831,34.471508],[-82.876464,34.465803],[-82.862156,34.458748],[-82.855762,34.443977],[-82.835004,34.366069],[-82.795223,34.34096],[-82.780308,34.296701],[-82.746656,34.266407],[-82.74192,34.210063],[-82.732761,34.195338],[-82.730824,34.175906],[-82.717507,34.150504],[-82.70414,34.141007],[-82.67732,34.131657],[-82.659077,34.103544],[-82.641553,34.092212],[-82.64398,34.072237],[-82.635991,34.064941],[-82.626963,34.063457],[-82.609655,34.039917],[-82.596155,34.030517],[-82.589245,34.000118],[-82.57554,33.992049],[-82.579576,33.979761],[-82.569864,33.970684],[-82.556835,33.945353],[-82.543128,33.940949],[-82.526741,33.943765],[-82.51295,33.936969],[-82.492929,33.909754],[-82.455105,33.88165],[-82.422803,33.863754],[-82.403881,33.865477],[-82.371775,33.843813],[-82.32448,33.820033],[-82.300213,33.800627],[-82.298286,33.783518],[-82.285804,33.780058],[-82.247472,33.752591],[-82.239098,33.730872],[-82.234576,33.700216],[-82.200718,33.66464],[-82.196583,33.630582],[-82.186154,33.62088],[-82.174351,33.613117],[-82.158331,33.60971],[-82.142872,33.594278],[-82.12908,33.589925],[-82.116545,33.596485],[-82.10624,33.595637],[-82.096352,33.58407],[-82.046335,33.56383],[-82.033023,33.546454],[-82.001338,33.520135],[-81.985938,33.486536],[-81.926336,33.462937],[-81.913356,33.437418],[-81.926789,33.426576],[-81.919217,33.413126],[-81.9373,33.401259],[-81.925737,33.37114],[-81.930634,33.368165],[-81.939637,33.37254],[-81.946337,33.37064],[-81.944737,33.364041],[-81.934837,33.356041],[-81.939737,33.344941],[-81.917973,33.34159],[-81.919137,33.334442],[-81.909285,33.324181],[-81.898187,33.329664],[-81.884137,33.310443],[-81.875836,33.307443],[-81.870436,33.312943],[-81.847296,33.306783],[-81.849636,33.299544],[-81.861536,33.297944],[-81.863236,33.288844],[-81.838257,33.272975],[-81.838337,33.269098],[-81.847336,33.266345],[-81.852136,33.247544],[-81.827936,33.228746],[-81.811736,33.223847],[-81.805236,33.211447],[-81.784535,33.208147],[-81.778935,33.209847],[-81.778435,33.221847],[-81.768935,33.217447],[-81.758235,33.200248],[-81.760635,33.189248],[-81.772435,33.181249],[-81.763135,33.159449],[-81.743835,33.14145],[-81.704634,33.116451],[-81.683533,33.112651],[-81.646433,33.094552],[-81.614298,33.094661],[-81.609476,33.089862],[-81.610078,33.082883],[-81.600211,33.083966],[-81.600091,33.073497],[-81.583804,33.067021],[-81.57288,33.05418],[-81.562066,33.055568],[-81.558336,33.046183],[-81.54251,33.045254],[-81.540081,33.040613],[-81.513231,33.028546],[-81.492253,33.009342],[-81.494736,32.978998],[-81.499471,32.96478],[-81.506449,32.962423],[-81.508436,32.955765],[-81.499446,32.944988],[-81.502427,32.935353],[-81.483198,32.921802],[-81.479184,32.905638],[-81.464069,32.897814],[-81.479445,32.881082],[-81.45392,32.874074],[-81.453949,32.849761],[-81.444866,32.850967],[-81.426475,32.840773],[-81.417984,32.818196],[-81.423772,32.810514],[-81.428313,32.78311],[-81.421128,32.778039],[-81.426481,32.770291],[-81.417606,32.762684],[-81.410845,32.741694],[-81.418542,32.732586],[-81.421194,32.711978],[-81.427517,32.701896],[-81.4131,32.692648],[-81.41075,32.694772],[-81.401256,32.680156],[-81.405273,32.656517],[-81.393818,32.653491],[-81.403582,32.643398],[-81.407271,32.631737],[-81.413411,32.637368],[-81.41866,32.629392],[-81.389338,32.595436],[-81.380999,32.589652],[-81.369757,32.591231],[-81.366964,32.577059],[-81.328753,32.561228],[-81.29676,32.562648],[-81.281324,32.556464],[-81.275213,32.545202],[-81.277131,32.535417],[-81.252882,32.51833],[-81.237095,32.517314],[-81.234023,32.513778],[-81.238281,32.505988],[-81.233585,32.498488],[-81.200029,32.467985],[-81.186829,32.464086],[-81.203046,32.448844],[-81.201595,32.44136],[-81.207246,32.437542],[-81.20513,32.423788],[-81.177231,32.39169],[-81.181072,32.380398],[-81.169332,32.369436],[-81.170858,32.362722],[-81.155136,32.34717],[-81.144032,32.351093],[-81.133632,32.341293],[-81.135733,32.324594],[-81.122933,32.307295],[-81.121433,32.284496],[-81.145834,32.263397],[-81.155995,32.241478],[-81.136727,32.213669],[-81.128283,32.208634],[-81.118234,32.189201],[-81.119361,32.177142],[-81.129634,32.165602],[-81.123134,32.162902],[-81.120034,32.153303],[-81.117234,32.117605],[-81.113334,32.113205],[-81.093386,32.11123],[-81.066906,32.090351],[-81.050234,32.085308],[-81.032674,32.08545],[-81.011961,32.100176],[-81.002297,32.100048],[-80.983133,32.079609],[-80.954482,32.068622],[-80.922794,32.039151],[-80.885517,32.0346],[-80.859111,32.023693],[-80.852276,32.026676],[-80.84313,32.024226],[-80.840549,32.011306],[-80.848441,31.988279],[-80.862814,31.969346],[-80.897687,31.949065],[-80.911207,31.943769],[-80.929101,31.944964],[-80.930279,31.956705],[-80.948491,31.95723],[-80.972392,31.94127],[-80.975714,31.923602],[-80.968494,31.915822],[-80.934508,31.90918],[-80.99269,31.857641],[-81.000317,31.856744],[-81.014478,31.867474],[-81.041548,31.876198],[-81.065255,31.877095],[-81.05907,31.850106],[-81.076178,31.836132],[-81.075812,31.829031],[-81.057181,31.822687],[-81.039808,31.823],[-81.036873,31.812721],[-81.077057,31.761256],[-81.097402,31.753126],[-81.130634,31.722692],[-81.138448,31.720934],[-81.192784,31.733245],[-81.203572,31.719448],[-81.186303,31.701509],[-81.161084,31.691401],[-81.151888,31.698411],[-81.139394,31.699917],[-81.131137,31.695774],[-81.136408,31.674832],[-81.131728,31.654484],[-81.133493,31.623348],[-81.160364,31.570436],[-81.173079,31.555908],[-81.178822,31.55553],[-81.186114,31.568032],[-81.204315,31.568183],[-81.214536,31.557601],[-81.240699,31.552313],[-81.254218,31.55594],[-81.260076,31.54828],[-81.263905,31.532579],[-81.258809,31.52906],[-81.217948,31.527284],[-81.199518,31.537596],[-81.181592,31.527697],[-81.177254,31.517074],[-81.189643,31.503588],[-81.204883,31.473124],[-81.246911,31.422784],[-81.278798,31.367214],[-81.282923,31.326491],[-81.268027,31.324218],[-81.25482,31.315452],[-81.274688,31.289454],[-81.276862,31.254734],[-81.289136,31.225487],[-81.288403,31.211065],[-81.293359,31.206332],[-81.314183,31.207938],[-81.339028,31.186918],[-81.35488,31.167204],[-81.360791,31.155903],[-81.359349,31.149166],[-81.368241,31.136534],[-81.399677,31.134113],[-81.403732,31.107115],[-81.401267,31.072781],[-81.420474,31.016703],[-81.432475,31.012991],[-81.434923,31.017804],[-81.451444,31.015515],[-81.469298,30.996028],[-81.490586,30.984952],[-81.493651,30.977528],[-81.486966,30.969602],[-81.475789,30.965976],[-81.466814,30.97091],[-81.453568,30.965573],[-81.447388,30.956732],[-81.426929,30.956615],[-81.420108,30.974076],[-81.408484,30.977718],[-81.403409,30.957914],[-81.405153,30.908203],[-81.428577,30.836336],[-81.446927,30.81039],[-81.460061,30.769912],[-81.45947,30.741979],[-81.444124,30.709714],[-81.472597,30.713312],[-81.487332,30.726081],[-81.528278,30.723359],[-81.540923,30.713343],[-81.561706,30.715597],[-81.571419,30.721636],[-81.601206,30.728141],[-81.607667,30.721924],[-81.617663,30.722046],[-81.625098,30.733017],[-81.646137,30.727591],[-81.65177,30.732284],[-81.651723,30.740235],[-81.662173,30.746521],[-81.672824,30.738935],[-81.688925,30.741434],[-81.692815,30.7471],[-81.719927,30.744634],[-81.732227,30.749634],[-81.747572,30.766455],[-81.763372,30.77382],[-81.779171,30.768062],[-81.792769,30.784432],[-81.806652,30.789683],[-81.840375,30.786384],[-81.852626,30.794439],[-81.868608,30.792754],[-81.89572,30.821098],[-81.910926,30.815889],[-81.949787,30.827493],[-81.962175,30.818001],[-81.962534,30.796526],[-81.973856,30.778487],[-81.988605,30.780056],[-82.007865,30.792937],[-82.022866,30.787991],[-82.024035,30.783156],[-82.011597,30.763122],[-82.017917,30.755263],[-82.038967,30.749262],[-82.043795,30.729641],[-82.036426,30.706585],[-82.050432,30.676266],[-82.049507,30.655548],[-82.042271,30.649452],[-82.039941,30.637144],[-82.028499,30.621829],[-82.027338,30.606726],[-82.016503,30.602484],[-82.012109,30.593773],[-82.005477,30.563495],[-82.018361,30.531184],[-82.01477,30.513009],[-82.017779,30.475081],[-82.037209,30.434518],[-82.034005,30.422357],[-82.04199,30.403266],[-82.036825,30.377884],[-82.047917,30.363265],[-82.060034,30.360328],[-82.094687,30.360781],[-82.104834,30.368319],[-82.161757,30.357851],[-82.170054,30.358929],[-82.19294,30.378779],[-82.210291,30.42459],[-82.203975,30.444507],[-82.207708,30.460503],[-82.200938,30.474438],[-82.201416,30.485164],[-82.226933,30.510281],[-82.23582,30.537187],[-82.231916,30.55627],[-82.214385,30.566958],[-83.499876,30.645671],[-84.86346,30.711506],[-84.896122,30.750591],[-84.914322,30.753591],[-84.920123,30.76599],[-84.917423,30.77589],[-84.928323,30.79309],[-84.927923,30.80279],[-84.936042,30.820671],[-84.928335,30.844263],[-84.935256,30.854328],[-84.935413,30.882481],[-84.966726,30.917287],[-84.971026,30.928187],[-84.983127,30.934786],[-84.979627,30.954686],[-84.982527,30.965586],[-85.005931,30.97704],[-84.999428,31.013843],[-85.009409,31.032378],[-85.011392,31.053546],[-85.028573,31.074583],[-85.026068,31.08418],[-85.029736,31.096163],[-85.035615,31.108192],[-85.054677,31.120818],[-85.064028,31.142495],[-85.076628,31.156927],[-85.100207,31.16549],[-85.098426,31.17777],[-85.106503,31.185305],[-85.106963,31.202693],[-85.09977,31.209751],[-85.096763,31.225651],[-85.111711,31.258022],[-85.114548,31.276302],[-85.110309,31.281733],[-85.099107,31.284165],[-85.089774,31.295026],[-85.084152,31.328313],[-85.088983,31.334292],[-85.085918,31.353146],[-85.09099,31.354428],[-85.092487,31.362881],[-85.078641,31.39636],[-85.079978,31.410472],[-85.074762,31.424879],[-85.06697,31.428594],[-85.071621,31.468384],[-85.045642,31.516813],[-85.047196,31.528671],[-85.041305,31.540987],[-85.05796,31.57084],[-85.055976,31.605178],[-85.060418,31.611271],[-85.057473,31.618624],[-85.082829,31.637967],[-85.083545,31.656071],[-85.092429,31.659966],[-85.12553,31.694965],[-85.12653,31.716764],[-85.11913,31.730964],[-85.129231,31.758663],[-85.12523,31.767063],[-85.140431,31.779663],[-85.132231,31.795162],[-85.131331,31.817562],[-85.141831,31.839261],[-85.138331,31.844161],[-85.140131,31.858761],[-85.128831,31.87636],[-85.132931,31.89306],[-85.114031,31.89336],[-85.10803,31.90516],[-85.112731,31.909859],[-85.07893,31.940159],[-85.08683,31.957758],[-85.067829,31.967358],[-85.07093,31.981658],[-85.068098,31.991857],[-85.064544,32.002489],[-85.053815,32.013502],[-85.05883,32.046656],[-85.055491,32.072657],[-85.047063,32.090433],[-85.06206,32.132486],[-85.045593,32.143758],[-85.011267,32.180493],[-84.966828,32.193952],[-84.966346,32.208034],[-84.957057,32.21671],[-84.925427,32.221551],[-84.912488,32.247463],[-84.890894,32.261504],[-84.9338,32.29826],[-85.001874,32.322015],[-85.007103,32.328362],[-85.004582,32.345196],[-84.983466,32.363186],[-84.976767,32.392648],[-84.981098,32.402833],[-84.979431,32.412244],[-84.96343,32.422544],[-84.967031,32.435343],[-84.971831,32.442843],[-84.995331,32.453243],[-84.998231,32.469842],[-84.994831,32.486042],[-85.0071,32.523868],[-85.015805,32.528428],[-85.022509,32.542923],[-85.067535,32.579546],[-85.076399,32.594665],[-85.08224,32.616264],[-85.088319,32.623032],[-85.087294,32.634407],[-85.098259,32.642708],[-85.089736,32.655635],[-85.093536,32.669734],[-85.114737,32.685634],[-85.122738,32.715727],[-85.1202,32.737647],[-85.138101,32.753836],[-85.133275,32.780609],[-85.167939,32.811612],[-85.168342,32.828516],[-85.159309,32.841382],[-85.160792,32.848466],[-85.177127,32.853895],[-85.1844,32.861317],[-85.42947,34.125096],[-85.561416,34.750079],[-85.605165,34.984678],[-84.810477,34.987607]]]},\"properties\":{\"name\":\"Georgia\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611966","contributors":{"authors":[{"text":"Knaak, Andrew E. 0000-0003-1813-8959 aknaak@usgs.gov","orcid":"https://orcid.org/0000-0003-1813-8959","contributorId":3123,"corporation":false,"usgs":true,"family":"Knaak","given":"Andrew","email":"aknaak@usgs.gov","middleInitial":"E.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Joiner, John K. 0000-0001-9702-4911 jkjoiner@usgs.gov","orcid":"https://orcid.org/0000-0001-9702-4911","contributorId":3056,"corporation":false,"usgs":true,"family":"Joiner","given":"John","email":"jkjoiner@usgs.gov","middleInitial":"K.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97152,"text":"ofr20081265 - 2008 - Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:27","indexId":"ofr20081265","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1265","title":"Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2005","docAbstract":"The U.S. Geological Survey, in cooperation with the U.S. Department of Energy, Office of Civilian Radioactive Waste Management, collected, compiled, and summarized hydrologic data in the Yucca Mountain region of southern Nevada and eastern California. These data were collected to allow assessments of ground-water resources during activities to determine the potential suitability or development of Yucca Mountain for storing high-level nuclear waste.\r\n\r\nData collected from January through December 2005 are provided for ground-water levels at 35 boreholes and 1 fissure (Devils Hole), ground-water discharge at 5 springs, ground-water levels and discharge at 1 flowing borehole, and total reported ground-water withdrawals within Crater Flat, Jackass Flats, Mercury Valley, and the Amargosa Desert. Ground-water level, discharge, and withdrawal data collected by other agencies, or as part of other programs, are provided.\r\n\r\nA statistical summary of ground-water levels at seven boreholes in Jackass Flats is presented for 1992-2005 to indicate potential effects of ground-water withdrawals associated with U.S. Department of Energy activities near Yucca Mountain. The statistical summary includes the annual number of measurements; maximum, minimum, and median water-level altitudes; and average deviation of measured water-level altitudes compared to the 1992-93 baseline period. At seven boreholes in Jackass Flats, median water levels for 2005 were slightly higher (0.4-2.7 feet) than the median water levels for 1992-93.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081265","collaboration":"Prepared in cooperation with the Office of Civilian Radioactive Waste Management of the U.S. Department of Energy, under Interagency Agreement DE-AI28-02RW12167","usgsCitation":"Locke, G.L., 2008, Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2005: U.S. Geological Survey Open-File Report 2008-1265, vi, 63 p., https://doi.org/10.3133/ofr20081265.","productDescription":"vi, 63 p.","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":195143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12137,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1265/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,36 ], [ -117.25,37.5 ], [ -115.5,37.5 ], [ -115.5,36 ], [ -117.25,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7ef","contributors":{"authors":[{"text":"Locke, Glenn L. gllocke@usgs.gov","contributorId":2479,"corporation":false,"usgs":true,"family":"Locke","given":"Glenn","email":"gllocke@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":301200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97162,"text":"tm2A7 - 2008 - Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks","interactions":[],"lastModifiedDate":"2012-02-10T00:11:46","indexId":"tm2A7","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2-A7","title":"Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks","docAbstract":"Rivers and streams that drain from Olympic, Mount Rainier, and North Cascades National Parks are among the most protected corridors in the lower 48 States, and represent some of the largest tracts of contiguous, undisturbed habitat throughout the range of several key fish species of the Pacific Northwest. These watersheds are of high regional importance as freshwater habitat sanctuaries for native fish, where habitat conditions are characterized as having little to no disturbance from development, channelization, impervious surfaces, roads, diversions, or hydroelectric projects. Fishery resources are of high ecological and cultural importance in Pacific Northwest National Parks, and significantly contribute to economically important recreational, commercial, and tribal fisheries.\r\n\r\nThis protocol describes procedures to monitor trends in fish assemblages, fish abundance, and water temperature in eight rivers and five wadeable streams in Olympic National Park during summer months, and is based on 4 years of field testing. Fish assemblages link freshwater, marine, and terrestrial ecosystems. They also serve as focal resources of national parks and are excellent indicators of ecological conditions of rivers and streams. Despite the vital importance of native anadromous and resident fish populations, there is no existing monitoring program for fish assemblages in the North Coast and Cascades Network.\r\n\r\nSpecific monitoring objectives of this protocol are to determine seasonal and annual trends in: (1) fish species composition, (2) timing of migration of adult fish, (3) relative abundance, (4) age and size structure, (5) extent of non-native and hatchery fish, and (6) water temperature. To detect seasonal and annual trends in fish assemblages in reference sites, we rely on repeated and consistent annual sampling at each monitoring site. The general rationale for the repeated sampling of reference sites is to ensure that we account for the high interannual variability in fish movements and abundances in rivers. One underlying assumption is that the monitoring program is designed in perpetuity, and consequently our capability to detect trends substantially increases with time.\r\n\r\nThe protocol describes sampling designs, methods, training procedures, safety considerations, data management, data analysis, and reporting. The allocation of sampling effort represents a balance between ecological considerations, a sound monitoring approach, and practical limitations caused by logistical constraints and a limited annual budget of $55,000. The widespread declines of native fish species in western North America highlights the importance and urgency of understanding trends in fish assemblages from undisturbed habitats. Seasonal and annual trends in fish assemblages will provide insights at the individual, population, and assemblage level.\r\n\r\nThis protocol will allow managers to detect increases and decreases in abundance of priority management species, and occurrence of non-native, hatchery, and federally listed fish. The detection of trends in fish assemblages will allow for specific management actions that may include: implementation of more appropriate fishing regulations, evaluation of existing hatchery releases, control of non-native fish species, and prioritization of habitat restoration projects. Dissemination and communication of scientific findings on North Coast and Cascades Network fish assemblages will be a core product of this protocol, which will have much relevance to decision makers, park visitors, researchers, and educators.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Chapter 7 of Section A, Biological Science, Book 2, Collection of Environmental Data","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/tm2A7","collaboration":"Prepared in cooperation with the North Coast and Cascades Network, National Park Service","usgsCitation":"Brenkman, S.J., and Connolly, P., 2008, Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks: U.S. Geological Survey Techniques and Methods 2-A7, vi, 131 p., https://doi.org/10.3133/tm2A7.","productDescription":"vi, 131 p.","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":124593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_2_a7.png"},{"id":12147,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/tm2a7/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,47.25 ], [ -125,48.5 ], [ -122,48.5 ], [ -122,47.25 ], [ -125,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ec3","contributors":{"authors":[{"text":"Brenkman, Samuel J.","contributorId":50864,"corporation":false,"usgs":true,"family":"Brenkman","given":"Samuel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connolly, Patrick J. 0000-0001-7365-7618 pconnolly@usgs.gov","orcid":"https://orcid.org/0000-0001-7365-7618","contributorId":2920,"corporation":false,"usgs":true,"family":"Connolly","given":"Patrick J.","email":"pconnolly@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":301224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97145,"text":"ofr20081344 - 2008 - Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California","interactions":[],"lastModifiedDate":"2022-06-15T20:57:29.361448","indexId":"ofr20081344","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1344","displayTitle":"Comments on Potential Geologic and Seismic Hazards Affecting Proposed Liquefied Natural Gas Site in Santa Monica Bay, California","title":"Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California","docAbstract":"In a letter to the U.S. Geological Survey (USGS) dated March 25, 2008, Representative Jane Harman (California 36th district) requested advice on geologic hazards that should be considered in the review of a proposed liquefied natural gas (LNG) facility off the California coast in Santa Monica Bay. In 2004, the USGS responded to a similar request from Representative Lois Capps, regarding two proposed LNG facilities offshore Ventura County, Calif., with a report summarizing potential geologic and seismic hazards (Ross and others, 2004).\r\n\r\nThe proposed LNG Deepwater Port (DWP) facility includes single point moorings (SPMs) and 35 miles of underwater pipelines. The DWP submersible buoys, manifolds, and risers would be situated on the floor of the southern Santa Monica Basin, in 3,000 feet of water, about 23 miles offshore of the Palos Verdes Peninsula. Twin 24-inch diameter pipelines would extend northeastward from the buoys across the basin floor, up the basin slope and across the continental shelf, skirting north around the Santa Monica submarine canyon. Figure 1 provides locations of the project and geologic features. Acronyms are defined in table 1.\r\n\r\nThis facility is being proposed in a region of known geologic hazards that arise from both the potential for strong earthquakes and geologic processes related to sediment transport and accumulation in the offshore environment. The probability of a damaging earthquake (considered here as magnitude 6.5 or greater) in the next 30 years within about 30 miles (50 km) of the proposed pipeline ranges from 16% at the pipeline's offshore end to 48% where it nears land (Petersen, 2008). Earthquakes of this magnitude are capable of producing strong shaking, surface fault offsets, liquefaction phenomena, landslides, underwater turbidity currents and debris flow avalanches, and tsunamis.\r\n\r\nAs part of the DWP license application for the Woodside Natural Gas proposal in Santa Monica Bay (known as the OceanWay Secure Energy Project), Fugro West, Inc., had already prepared a document discussing geologic hazards in the area, titled 'Exhibit B Topic Report 6 - Geological Resources' (Fugro West, Inc., 2007); hereafter, this will be called the 'Geological Resources document'. The USGS agreed to evaluate the information in the Geological Resources document regarding (1) proximity of active faults to the proposed project, (2) potential magnitude of seismic events from nearby faults, (3) thoroughness of the assessment of earthquake hazards in general, (4) potential hazards from ground rupture and strong shaking, (5) potential hazards from tsunamis, and (6) other geologic hazards including landslides and debris flows. Because two new earthquake probability reports were scheduled to be released in mid-April, 2008, by the USGS and the California Geological Survey (CGS), the USGS suggested a 6-month review period to enable a thorough incorporation of this new information.\r\n\r\nTwenty-seven scientists from the USGS and the CGS reviewed various sections of the Geological Resources document. This report outlines our major conclusions. The appendix is a longer list of comments by these reviewers, grouped by section of the Geological Resources document. Before discussing our reviews, we first provide a brief overview of geologic hazards in the proposed site area.\r\n\r\nThis report is a snapshot in time and any future work in the area will need to take into account ongoing research efforts. For example, USGS scientists collected seismic reflection data in the spring of 2008 to study the structure and seismic potential of several faults in the area. Their interpretations (Conrad and others, 2008a and 2008b) are too preliminary to be included in this report, but their final results, along with other researchers' studies in the project area, should be considered in any future work on the Deepwater Port project.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081344","usgsCitation":"Ross, S.L., Lee, H., Parsons, T.E., Beyer, L.A., Boore, D.M., Conrad, J.E., Edwards, B.D., Fisher, M.A., Frankel, A.D., Geist, E.L., Hudnut, K.W., Hough, S.E., Kayen, R., Lorenson, T., Luco, N., McCrory, P.A., McGann, M., Nathenson, M., Nolan, M., Petersen, M.D., Ponti, D.J., Powell, C.L., Ryan, H., Tinsley, J., Wills, C.J., Wong, F.L., and Xu, J., 2008, Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California (Version 1.0): U.S. Geological Survey Open-File Report 2008-1344, vi, 60 p., https://doi.org/10.3133/ofr20081344.","productDescription":"vi, 60 p.","onlineOnly":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":196141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402242,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85392.htm","linkFileType":{"id":5,"text":"html"}},{"id":12130,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1344/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Santa Monica Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.3333,\n              33\n            ],\n            [\n              -117.8333,\n              33\n            ],\n            [\n              -117.8333,\n              34.3833\n            ],\n            [\n              -119.3333,\n              34.3833\n            ],\n            [\n              -119.3333,\n              33\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6b3","contributors":{"authors":[{"text":"Ross, Stephanie L. 0000-0003-1389-4405 sross@usgs.gov","orcid":"https://orcid.org/0000-0003-1389-4405","contributorId":1024,"corporation":false,"usgs":true,"family":"Ross","given":"Stephanie","email":"sross@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Homa J. hjlee@usgs.gov","contributorId":1021,"corporation":false,"usgs":true,"family":"Lee","given":"Homa J.","email":"hjlee@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":301154,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parsons, Tom E. 0000-0002-0582-4338","orcid":"https://orcid.org/0000-0002-0582-4338","contributorId":36647,"corporation":false,"usgs":true,"family":"Parsons","given":"Tom","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":301175,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beyer, Larry A. lbeyer@usgs.gov","contributorId":2819,"corporation":false,"usgs":true,"family":"Beyer","given":"Larry","email":"lbeyer@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":301170,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":301164,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Conrad, James E. 0000-0001-6655-694X jconrad@usgs.gov","orcid":"https://orcid.org/0000-0001-6655-694X","contributorId":2316,"corporation":false,"usgs":true,"family":"Conrad","given":"James","email":"jconrad@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301163,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Edwards, Brian D. bedwards@usgs.gov","contributorId":3161,"corporation":false,"usgs":true,"family":"Edwards","given":"Brian","email":"bedwards@usgs.gov","middleInitial":"D.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301172,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fisher, Michael A. mfisher@usgs.gov","contributorId":1991,"corporation":false,"usgs":true,"family":"Fisher","given":"Michael","email":"mfisher@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":301162,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Frankel, Arthur D. 0000-0001-9119-6106 afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":1363,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":301159,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Geist, Eric L. 0000-0003-0611-1150 egeist@usgs.gov","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":1956,"corporation":false,"usgs":true,"family":"Geist","given":"Eric","email":"egeist@usgs.gov","middleInitial":"L.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301160,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Hudnut, Kenneth W. 0000-0002-3168-4797 hudnut@usgs.gov","orcid":"https://orcid.org/0000-0002-3168-4797","contributorId":2550,"corporation":false,"usgs":true,"family":"Hudnut","given":"Kenneth","email":"hudnut@usgs.gov","middleInitial":"W.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true}],"preferred":true,"id":301165,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Hough, Susan E. 0000-0002-5980-2986 hough@usgs.gov","orcid":"https://orcid.org/0000-0002-5980-2986","contributorId":587,"corporation":false,"usgs":true,"family":"Hough","given":"Susan","email":"hough@usgs.gov","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":301152,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Kayen, Robert E. rkayen@usgs.gov","contributorId":2787,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert E.","email":"rkayen@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":301169,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Lorenson, T.D. tlorenson@usgs.gov","contributorId":2622,"corporation":false,"usgs":true,"family":"Lorenson","given":"T.D.","email":"tlorenson@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":301167,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Luco, Nicolas 0000-0002-5763-9847 nluco@usgs.gov","orcid":"https://orcid.org/0000-0002-5763-9847","contributorId":1188,"corporation":false,"usgs":true,"family":"Luco","given":"Nicolas","email":"nluco@usgs.gov","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":false,"id":301157,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"McCrory, Patricia A. 0000-0003-2471-0018 pmccrory@usgs.gov","orcid":"https://orcid.org/0000-0003-2471-0018","contributorId":2728,"corporation":false,"usgs":true,"family":"McCrory","given":"Patricia","email":"pmccrory@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":301168,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"McGann, Mary 0000-0002-3057-2945 mmcgann@usgs.gov","orcid":"https://orcid.org/0000-0002-3057-2945","contributorId":2849,"corporation":false,"usgs":true,"family":"McGann","given":"Mary","email":"mmcgann@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":301171,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":301158,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Nolan, Michael","contributorId":78838,"corporation":false,"usgs":true,"family":"Nolan","given":"Michael","email":"","affiliations":[],"preferred":false,"id":301177,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Petersen, Mark D. 0000-0001-8542-3990 mpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-8542-3990","contributorId":1163,"corporation":false,"usgs":true,"family":"Petersen","given":"Mark","email":"mpetersen@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":301156,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Ponti, Daniel J. 0000-0002-2437-5144 dponti@usgs.gov","orcid":"https://orcid.org/0000-0002-2437-5144","contributorId":1020,"corporation":false,"usgs":true,"family":"Ponti","given":"Daniel","email":"dponti@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":301153,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":301173,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Ryan, Holly F.","contributorId":67616,"corporation":false,"usgs":true,"family":"Ryan","given":"Holly F.","affiliations":[],"preferred":false,"id":301176,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Tinsley, John C. III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":301174,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Wills, Chris J.","contributorId":97576,"corporation":false,"usgs":true,"family":"Wills","given":"Chris","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301178,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Wong, Florence L. 0000-0002-3918-5896 fwong@usgs.gov","orcid":"https://orcid.org/0000-0002-3918-5896","contributorId":1990,"corporation":false,"usgs":true,"family":"Wong","given":"Florence","email":"fwong@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301161,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Xu, Jingping jpx@usgs.gov","contributorId":2574,"corporation":false,"usgs":true,"family":"Xu","given":"Jingping","email":"jpx@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301166,"contributorType":{"id":1,"text":"Authors"},"rank":27}]}}
,{"id":97147,"text":"ofr20081343 - 2008 - Report on the Aseismic Slip, Tremor, and Earthquakes Workshop","interactions":[],"lastModifiedDate":"2019-07-18T09:43:53","indexId":"ofr20081343","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1343","title":"Report on the Aseismic Slip, Tremor, and Earthquakes Workshop","docAbstract":"This report summarizes the discussions and information presented during the workshop on Aseismic Slip, Tremor, and Earthquakes. Workshop goals included improving coordination among those involved in conducting research related to these phenomena, assessing the implications for earthquake hazard assessment, and identifying ways to capitalize on the education and outreach opportunities presented by these phenomena. Research activities of focus included making, disseminating, and analyzing relevant measurements; the relationships among tremor, aseismic or 'slow-slip', and earthquakes; and discovering the underlying causative physical processes. More than 52 participants contributed to the workshop, held February 25-28, 2008 in Sidney, British Columbia. The workshop was sponsored by the U.S. Geological Survey, the National Science Foundation?s Earthscope Program and UNAVCO Consortium, and the Geological Survey of Canada. \r\n\r\nThis report has five parts. In the first part, we integrate the information exchanged at the workshop as it relates to advancing our understanding of earthquake generation and hazard. In the second part, we summarize the ideas and concerns discussed in workshop working groups on Opportunities for Education and Outreach, Data and Instrumentation, User and Public Needs, and Research Coordination. The third part presents summaries of the oral presentations. The oral presentations are grouped as they were at the workshop in the categories of phenomenology, underlying physical processes, and implications for earthquake hazards. The fourth part contains the meeting program and the fifth part lists the workshop participants. References noted in parentheses refer to the authors of presentations made at the workshop, and published references are noted in square brackets and listed in the Reference section. Appendix A contains abstracts of all participant presentations and posters, which also have been posted online, along with presentations and author contact information at http://www.earthscope.org/science/cascadia.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081343","collaboration":"Prepared in cooperation with Earthscope, UNAVCO, the National Science Foundation and the Geological Survey of Canada","usgsCitation":"Gomberg, J., Roeloffs, E., Trehu, A., Dragert, H., and Meertens, C., 2008, Report on the Aseismic Slip, Tremor, and Earthquakes Workshop (Version 1.0): U.S. Geological Survey Open-File Report 2008-1343, 77 p. , https://doi.org/10.3133/ofr20081343.","productDescription":"77 p. ","onlineOnly":"Y","temporalStart":"2008-02-25","temporalEnd":"2008-02-28","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":196179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12132,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1343/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c6b7","contributors":{"authors":[{"text":"Gomberg, Joan","contributorId":77919,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","affiliations":[],"preferred":false,"id":301184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roeloffs, Evelyn","contributorId":35417,"corporation":false,"usgs":true,"family":"Roeloffs","given":"Evelyn","affiliations":[],"preferred":false,"id":301183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trehu, Anne","contributorId":82016,"corporation":false,"usgs":true,"family":"Trehu","given":"Anne","affiliations":[],"preferred":false,"id":301185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dragert, Herb","contributorId":100497,"corporation":false,"usgs":true,"family":"Dragert","given":"Herb","email":"","affiliations":[],"preferred":false,"id":301186,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meertens, Charles","contributorId":28333,"corporation":false,"usgs":true,"family":"Meertens","given":"Charles","affiliations":[],"preferred":false,"id":301182,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":97155,"text":"sir20085171 - 2008 - Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008","interactions":[],"lastModifiedDate":"2012-02-10T00:11:49","indexId":"sir20085171","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5171","title":"Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008","docAbstract":"A one-dimensional step-backwater model was used to simulate flooding conditions for Catoma Creek near Montgomery, Alabama. A peak flow of 50,000 cubic feet per second was computed by the U.S. Geological Survey for the March 1990 flood at the Norman Bridge Road gaging station. Using this estimated peak flow, flood-plain surveys with associated roughness coefficients, and surveyed high-water marks for the March 1990 flood, a flow model was calibrated to closely match the known event. The calibrated model then was used to simulate flooding for the 10-, 50-, 100-, and 500-year recurrence-interval floods. The 100-year flood stage for the Alabama River also was computed in the vicinity of the Catoma Creek confluence using observed high-water profiles from the 1979 and 1990 floods and gaging-station data. \r\n\r\nThe results indicate that the 100-year flood profile for Catoma Creek within the 15-mile study reach is about 2.5 feet higher, on average, than the profile published by the Federal Emergency Management Agency. The maximum and minimum differences are 6.0 feet and 0.8 foot, respectively. All water-surface elevations computed for the 100-year flood are higher than those published by the Federal Emergency Management Agency. The 100-year flood stage computed for the Alabama River in the vicinity of the Catoma Creek confluence was about 4.5 feet lower than the elevation published by the Federal Emergency Management Agency. The results of this study provide the community with flood-profile information that can be used for flood-plain mitigation, future development, and safety plans for the city.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20085171","collaboration":"Prepared in cooperation with the City of Montgomery, Alabama","usgsCitation":"Lee, K., and Hedgecock, T., 2008, Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008: U.S. Geological Survey Scientific Investigations Report 2008-5171, iv, 33 p., https://doi.org/10.3133/sir20085171.","productDescription":"iv, 33 p.","temporalStart":"2008-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":105,"text":"Alabama Water Science Center","active":true,"usgs":true}],"links":[{"id":124404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5171.jpg"},{"id":12140,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5171/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.75,31.75 ], [ -86.75,32.75 ], [ -85.75,32.75 ], [ -85.75,31.75 ], [ -86.75,31.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977fb","contributors":{"authors":[{"text":"Lee, K.G.","contributorId":28319,"corporation":false,"usgs":true,"family":"Lee","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":301206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedgecock, T.S.","contributorId":16107,"corporation":false,"usgs":true,"family":"Hedgecock","given":"T.S.","email":"","affiliations":[],"preferred":false,"id":301205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97150,"text":"ofr20081290 - 2008 - Floods of May and June 2004 in central and eastern Ohio: FEMA disaster declaration 1519","interactions":[],"lastModifiedDate":"2022-07-14T13:11:03.325774","indexId":"ofr20081290","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1290","title":"Floods of May and June 2004 in central and eastern Ohio: FEMA disaster declaration 1519","docAbstract":"Several severe thunderstorms that passed through Ohio between May 17 and June 17, 2004, produced large amounts of rain in an already wet central and eastern Ohio, resulting in flooding in this region from May 18 to June 21, 2004. Record peak streamflow occurred at three U.S. Geological Survey (USGS) streamgages. Damages caused by the flooding resulting from these storms were severe enough that 25 counties in central and eastern Ohio were declared Federal disaster areas. In all, there were two storm- or flood-related deaths, 3,529 private structures damaged or destroyed, and an estimated $43 million in damages.\r\n\r\nThis report describes the meteorological factors that resulted in severe flooding in central and eastern Ohio between May 18 and June 21, 2004, and addresses the damages caused by the storms and flooding. Peak-stage, peak-streamflow, and recurrence-interval data are reported for selected USGS streamgages. Flood profiles determined by the USGS are presented for selected streams.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081290","collaboration":"Prepared in cooperation with the Ohio Emergency Management Agency","usgsCitation":"Ebner, A.D., Straub, D.E., and Lageman, J.D., 2008, Floods of May and June 2004 in central and eastern Ohio: FEMA disaster declaration 1519: U.S. Geological Survey Open-File Report 2008-1290, vi, 85 p., https://doi.org/10.3133/ofr20081290.","productDescription":"vi, 85 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2004-05-17","temporalEnd":"2004-06-21","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":195335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403716,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85398.htm","linkFileType":{"id":5,"text":"html"}},{"id":12135,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1290/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.726806640625,\n              39.5633531658293\n            ],\n            [\n              -80.584716796875,\n              39.5633531658293\n            ],\n            [\n              -80.584716796875,\n              41.74672584176937\n            ],\n            [\n              -83.726806640625,\n              41.74672584176937\n            ],\n            [\n              -83.726806640625,\n              39.5633531658293\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5df97f","contributors":{"authors":[{"text":"Ebner, Andrew D. aebner@usgs.gov","contributorId":1849,"corporation":false,"usgs":true,"family":"Ebner","given":"Andrew","email":"aebner@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, David E. destraub@usgs.gov","contributorId":1908,"corporation":false,"usgs":true,"family":"Straub","given":"David","email":"destraub@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":301195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lageman, Jonathan D. jlageman@usgs.gov","contributorId":1910,"corporation":false,"usgs":true,"family":"Lageman","given":"Jonathan","email":"jlageman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97151,"text":"ofr20081291 - 2008 - Floods of August and September 2004 in eastern Ohio: FEMA disaster declaration 1556","interactions":[],"lastModifiedDate":"2022-07-20T21:47:04.918824","indexId":"ofr20081291","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1291","title":"Floods of August and September 2004 in eastern Ohio: FEMA disaster declaration 1556","docAbstract":"A band of severe thunderstorms at the end of August 2004 and the passage of the remnants of Hurricanes Frances and Ivan during September 2004 caused severe flooding in eastern Ohio during August and September 2004. Record peak streamflow occurred at 12 U.S. Geological Survey (USGS) streamgages. Damages caused by the flooding produced by these storms were severe enough for 21 counties in eastern Ohio to be declared Federal disaster areas. In all, there were 4 storm- or flood-related deaths, 2,563 private structures damaged or destroyed, and an estimated $81 million in damages.\r\n\r\nThis report describes the meteorological factors that resulted in severe flooding in eastern Ohio during August 27-September 27, 2004, and examines the damages caused by the storms and flooding. Peak-stage, peak-streamflow, and recurrence-interval data are reported for selected USGS streamgages. Flood profiles determined by the USGS are presented for selected streams.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081291","collaboration":"Prepared in cooperation with the Ohio Emergency Management Agency","usgsCitation":"Ebner, A.D., Straub, D.E., and Lageman, J.D., 2008, Floods of August and September 2004 in eastern Ohio: FEMA disaster declaration 1556: U.S. Geological Survey Open-File Report 2008-1291, viii, 104 p., https://doi.org/10.3133/ofr20081291.","productDescription":"viii, 104 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2004-08-27","temporalEnd":"2004-09-27","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":195002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12136,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1291/","linkFileType":{"id":5,"text":"html"}},{"id":404174,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85399.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.6667,\n              38.4106\n            ],\n            [\n              -80.5192,\n              38.4106\n            ],\n            [\n              -80.5192,\n              41.5\n            ],\n            [\n              -82.6667,\n              41.5\n            ],\n            [\n              -82.6667,\n              38.4106\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe3d","contributors":{"authors":[{"text":"Ebner, Andrew D. aebner@usgs.gov","contributorId":1849,"corporation":false,"usgs":true,"family":"Ebner","given":"Andrew","email":"aebner@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, David E. destraub@usgs.gov","contributorId":1908,"corporation":false,"usgs":true,"family":"Straub","given":"David","email":"destraub@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":301198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lageman, Jonathan D. jlageman@usgs.gov","contributorId":1910,"corporation":false,"usgs":true,"family":"Lageman","given":"Jonathan","email":"jlageman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301199,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97149,"text":"ofr20081289 - 2008 - Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580","interactions":[],"lastModifiedDate":"2022-08-04T21:15:16.232185","indexId":"ofr20081289","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1289","title":"Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580","docAbstract":"A large snowstorm at the end of December 2004 that left more than 20 inches of snow in some areas of Ohio, followed by unseasonably warm temperatures in early January 2005, caused snowmelt to begin filling river channels. Widespread rain showers during January 2005 combined with this snowmelt to cause flooding throughout Ohio and mudslides in some areas. Record peak streamflows occurred at nine U.S. Geological Survey (USGS) streamgages. Damages caused by the snowstorms, flooding, and mudslides were severe enough for 62 counties in Ohio to be declared Federal disaster areas. In all, approximately 3,664 private structures were damaged or destroyed, and an estimated $238 million in damages occurred.\r\n\r\nThis report describes the meteorological factors that resulted in severe flooding throughout Ohio between December 22, 2004, and February 1, 2005, and examines the damages caused by the storms and flooding. Peak-stage, peak-streamflow, and recurrence-interval data are reported for selected USGS streamgages. Flood profiles determined by the USGS are presented for selected streams.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081289","collaboration":"Prepared in cooperation with the Ohio Emergency Management Agency","usgsCitation":"Ebner, A.D., Straub, D.E., and Lageman, J.D., 2008, Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580: U.S. Geological Survey Open-File Report 2008-1289, viii, 98 p., https://doi.org/10.3133/ofr20081289.","productDescription":"viii, 98 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2004-12-22","temporalEnd":"2005-02-01","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":195739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404853,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85397.htm","linkFileType":{"id":5,"text":"html"}},{"id":12134,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1289/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-82.835118,41.708971],[-82.82572,41.72281],[-82.820409,41.724549],[-82.810487,41.720524],[-82.782719,41.694003],[-82.793069,41.664692],[-82.827011,41.633701],[-82.842099,41.628323],[-82.843602,41.647009],[-82.835118,41.708971]]],[[[-82.700208,41.61219],[-82.691123,41.611331],[-82.68015,41.61897],[-82.677772,41.617986],[-82.680669,41.594611],[-82.686033,41.587246],[-82.702027,41.585437],[-82.735766,41.600982],[-82.735707,41.603361],[-82.718802,41.619629],[-82.70731,41.619609],[-82.703438,41.617734],[-82.700208,41.61219]]],[[[-81.725583,39.215835],[-81.733357,39.205868],[-81.737085,39.193836],[-81.741533,39.189596],[-81.752754,39.184676],[-81.755754,39.180976],[-81.756254,39.177276],[-81.743565,39.141933],[-81.744838,39.130898],[-81.742153,39.116777],[-81.745453,39.098078],[-81.752353,39.089878],[-81.760753,39.084078],[-81.775554,39.078378],[-81.785554,39.078578],[-81.803055,39.083878],[-81.810655,39.083278],[-81.813855,39.079278],[-81.811655,39.059578],[-81.803355,39.047678],[-81.772854,39.026179],[-81.764253,39.015279],[-81.765153,39.002579],[-81.774062,38.993682],[-81.776723,38.985142],[-81.775734,38.980737],[-81.78182,38.964935],[-81.778845,38.955892],[-81.756975,38.937152],[-81.756131,38.933545],[-81.759995,38.925828],[-81.76976,38.92273],[-81.781248,38.924804],[-81.793372,38.930204],[-81.806137,38.942112],[-81.814235,38.946168],[-81.827354,38.945898],[-81.831516,38.943697],[-81.844486,38.928746],[-81.845312,38.910088],[-81.848653,38.901407],[-81.855971,38.892734],[-81.889233,38.874279],[-81.898541,38.874582],[-81.910312,38.879294],[-81.928,38.893492],[-81.926671,38.901311],[-81.90091,38.924338],[-81.89847,38.929603],[-81.900595,38.937671],[-81.933186,38.987659],[-81.941829,38.993295],[-81.951447,38.996032],[-81.967769,38.992955],[-81.979371,38.993193],[-81.982032,38.995697],[-81.987061,39.011978],[-81.994961,39.022478],[-82.002261,39.027878],[-82.017562,39.030078],[-82.035963,39.025478],[-82.041563,39.017878],[-82.045663,39.003778],[-82.051563,38.994378],[-82.091565,38.973778],[-82.094865,38.964578],[-82.109065,38.945579],[-82.111666,38.932579],[-82.128866,38.909979],[-82.143167,38.898079],[-82.145267,38.883479],[-82.139224,38.86502],[-82.144867,38.84048],[-82.16157,38.824632],[-82.179478,38.817376],[-82.191172,38.815137],[-82.20929,38.802672],[-82.217269,38.79568],[-82.221566,38.787187],[-82.220449,38.773739],[-82.216614,38.76835],[-82.198882,38.757725],[-82.195606,38.752441],[-82.193268,38.741182],[-82.188268,38.734082],[-82.182467,38.708782],[-82.190167,38.687382],[-82.190867,38.680383],[-82.186067,38.666783],[-82.185567,38.659583],[-82.179067,38.648883],[-82.172667,38.629684],[-82.172066,38.619284],[-82.177267,38.603784],[-82.188767,38.594984],[-82.205171,38.591719],[-82.222168,38.591384],[-82.245969,38.598483],[-82.26207,38.598183],[-82.27427,38.593683],[-82.291271,38.578983],[-82.293871,38.572683],[-82.293271,38.560283],[-82.295671,38.538483],[-82.303971,38.517683],[-82.304223,38.496308],[-82.310639,38.483172],[-82.318111,38.457876],[-82.323999,38.449268],[-82.330335,38.4445],[-82.34064,38.440948],[-82.381773,38.434783],[-82.389746,38.434355],[-82.404882,38.439347],[-82.529579,38.405182],[-82.549799,38.403202],[-82.569368,38.406258],[-82.588249,38.415489],[-82.596921,38.426705],[-82.600761,38.437425],[-82.604089,38.459841],[-82.610458,38.471457],[-82.618474,38.477089],[-82.637707,38.484449],[-82.657051,38.496816],[-82.675724,38.515504],[-82.689965,38.53592],[-82.700045,38.544336],[-82.730958,38.559264],[-82.763695,38.560399],[-82.779472,38.559023],[-82.800112,38.563183],[-82.820161,38.572703],[-82.844306,38.590862],[-82.854291,38.613454],[-82.856791,38.632878],[-82.856291,38.646078],[-82.859391,38.660378],[-82.863291,38.669277],[-82.874892,38.682827],[-82.877592,38.690177],[-82.870392,38.722077],[-82.871292,38.739376],[-82.879492,38.751476],[-82.889193,38.756076],[-82.894193,38.756576],[-82.923694,38.750076],[-82.943147,38.74328],[-82.968695,38.728776],[-82.979395,38.725976],[-83.011816,38.730057],[-83.030702,38.72572],[-83.053104,38.695831],[-83.064319,38.688976],[-83.084226,38.68109],[-83.102746,38.677316],[-83.112372,38.671685],[-83.122547,38.6592],[-83.128973,38.640231],[-83.135046,38.631719],[-83.142836,38.625076],[-83.156926,38.620547],[-83.202453,38.616956],[-83.211027,38.618578],[-83.232404,38.627569],[-83.245572,38.627936],[-83.254558,38.623403],[-83.264011,38.621535],[-83.26851,38.615104],[-83.286514,38.599241],[-83.294193,38.596588],[-83.307832,38.600824],[-83.317542,38.609242],[-83.322383,38.630615],[-83.327636,38.637489],[-83.356445,38.654009],[-83.384755,38.663171],[-83.420194,38.668428],[-83.446989,38.670143],[-83.468059,38.67547],[-83.493342,38.694187],[-83.504365,38.699256],[-83.520953,38.703045],[-83.533339,38.702105],[-83.569098,38.692842],[-83.615736,38.684145],[-83.626922,38.679387],[-83.636208,38.670584],[-83.642994,38.643273],[-83.649737,38.632753],[-83.663911,38.62793],[-83.679484,38.630036],[-83.704006,38.639724],[-83.713405,38.641591],[-83.720779,38.646704],[-83.74992,38.649613],[-83.769347,38.65522],[-83.775761,38.666748],[-83.78362,38.695641],[-83.787113,38.699489],[-83.798549,38.704668],[-83.821854,38.709575],[-83.836696,38.717857],[-83.841689,38.724264],[-83.846207,38.74229],[-83.852085,38.751433],[-83.859028,38.756793],[-83.873168,38.762418],[-83.926986,38.771562],[-83.928454,38.774583],[-83.943978,38.783616],[-83.962123,38.787384],[-83.978814,38.787104],[-84.044486,38.770572],[-84.071491,38.770475],[-84.108836,38.779247],[-84.135088,38.789485],[-84.155912,38.794909],[-84.198358,38.80092],[-84.212904,38.805707],[-84.2253,38.817665],[-84.231306,38.830552],[-84.233727,38.853576],[-84.232132,38.880483],[-84.234453,38.893226],[-84.25701,38.923208],[-84.279916,38.945168],[-84.288164,38.955789],[-84.295076,38.968295],[-84.297255,38.989694],[-84.304698,39.006455],[-84.31368,39.016981],[-84.326539,39.027463],[-84.346039,39.036963],[-84.360439,39.041362],[-84.38684,39.045162],[-84.406941,39.045662],[-84.42573,39.053059],[-84.429841,39.058262],[-84.432341,39.067561],[-84.432941,39.083961],[-84.434641,39.086861],[-84.432841,39.094261],[-84.435541,39.102261],[-84.445242,39.114461],[-84.455342,39.12036],[-84.470542,39.12146],[-84.476243,39.11916],[-84.487743,39.11076],[-84.496543,39.10026],[-84.509743,39.09366],[-84.524644,39.09216],[-84.541344,39.09916],[-84.550844,39.09936],[-84.572144,39.08206],[-84.607928,39.073238],[-84.620112,39.073457],[-84.632446,39.07676],[-84.657246,39.09546],[-84.684847,39.100459],[-84.718548,39.137059],[-84.732048,39.144458],[-84.744149,39.147458],[-84.754449,39.146658],[-84.766749,39.138558],[-84.78768,39.115297],[-84.820157,39.10548],[-84.819451,39.305152],[-84.814955,39.566251],[-84.814179,39.814212],[-84.803918,40.310094],[-84.804504,40.411555],[-84.802547,40.50181],[-84.803919,41.435531],[-84.806082,41.696089],[-84.360546,41.706621],[-83.453832,41.732647],[-83.455626,41.727445],[-83.446032,41.706847],[-83.409531,41.691247],[-83.39263,41.691947],[-83.37573,41.686647],[-83.357073,41.687763],[-83.341817,41.693518],[-83.337985,41.698682],[-83.337977,41.70341],[-83.326825,41.701562],[-83.293928,41.680846],[-83.29068,41.676794],[-83.238191,41.651167],[-83.23166,41.644218],[-83.194524,41.631008],[-83.145887,41.617904],[-83.103928,41.613558],[-83.086036,41.60668],[-83.066593,41.59534],[-83.043287,41.568205],[-83.028072,41.555656],[-82.999916,41.538534],[-82.96985,41.524327],[-82.934369,41.514353],[-82.897728,41.519241],[-82.875229,41.529684],[-82.85677,41.548262],[-82.855197,41.564114],[-82.859531,41.576371],[-82.852957,41.583327],[-82.834101,41.587587],[-82.820207,41.570664],[-82.794324,41.546486],[-82.785496,41.540675],[-82.77201,41.54058],[-82.749907,41.54647],[-82.717878,41.54193],[-82.711332,41.53695],[-82.711632,41.527201],[-82.721914,41.516677],[-82.713904,41.501697],[-82.710013,41.49759],[-82.687921,41.492324],[-82.658302,41.461878],[-82.617745,41.431833],[-82.616952,41.428425],[-82.55808,41.400005],[-82.513827,41.384257],[-82.499099,41.381541],[-82.481214,41.381342],[-82.460599,41.386316],[-82.431315,41.396866],[-82.398086,41.413945],[-82.361784,41.426644],[-82.334182,41.430243],[-82.29158,41.428442],[-82.268479,41.430842],[-82.254678,41.434441],[-82.193375,41.46454],[-82.184774,41.47404],[-82.181598,41.471634],[-82.165373,41.47444],[-82.094169,41.495039],[-82.011966,41.515639],[-81.994565,41.51444],[-81.964912,41.505446],[-81.958463,41.498642],[-81.937862,41.491443],[-81.87736,41.483445],[-81.860262,41.483841],[-81.810992,41.495592],[-81.794449,41.49663],[-81.782258,41.49605],[-81.744755,41.48715],[-81.738755,41.48855],[-81.710986,41.501734],[-81.664884,41.53143],[-81.633652,41.540458],[-81.599747,41.560649],[-81.529955,41.614374],[-81.50044,41.623448],[-81.48864,41.631348],[-81.466038,41.649148],[-81.441339,41.674074],[-81.353229,41.727743],[-81.301626,41.750543],[-81.286925,41.760243],[-81.264224,41.758143],[-81.248672,41.761291],[-81.112885,41.817571],[-81.092716,41.822988],[-81.05192,41.839557],[-81.024525,41.846469],[-81.01049,41.853962],[-80.936244,41.862352],[-80.900342,41.868912],[-80.814943,41.897694],[-80.799822,41.909749],[-80.784682,41.911525],[-80.782052,41.906635],[-80.757945,41.913352],[-80.720816,41.919744],[-80.581882,41.95761],[-80.519461,41.977513],[-80.518991,40.638801],[-80.551126,40.628847],[-80.56784,40.617552],[-80.576736,40.614224],[-80.583633,40.61552],[-80.592049,40.622496],[-80.598764,40.625263],[-80.627171,40.619936],[-80.634355,40.616095],[-80.651716,40.597744],[-80.662564,40.5916],[-80.667957,40.582496],[-80.666917,40.573664],[-80.652436,40.562544],[-80.633107,40.538705],[-80.627507,40.535793],[-80.618003,40.502049],[-80.609058,40.489506],[-80.599194,40.482566],[-80.595494,40.475266],[-80.596094,40.463366],[-80.612295,40.434867],[-80.612195,40.402667],[-80.615195,40.399867],[-80.632196,40.393667],[-80.633596,40.390467],[-80.631596,40.385468],[-80.619196,40.381768],[-80.609695,40.374968],[-80.607595,40.369568],[-80.612796,40.347668],[-80.610796,40.340868],[-80.602895,40.327869],[-80.599895,40.317669],[-80.602895,40.307069],[-80.614896,40.291969],[-80.616796,40.285269],[-80.616196,40.27227],[-80.619297,40.26517],[-80.622497,40.26177],[-80.644598,40.25127],[-80.652098,40.24497],[-80.661543,40.229798],[-80.6681,40.199671],[-80.6726,40.192371],[-80.686137,40.181607],[-80.704602,40.154823],[-80.710042,40.138311],[-80.710554,40.125271],[-80.706702,40.110872],[-80.709102,40.101472],[-80.713003,40.096872],[-80.730704,40.086472],[-80.738604,40.075672],[-80.737104,40.064972],[-80.733104,40.058772],[-80.730904,40.046672],[-80.731504,40.037472],[-80.737389,40.027593],[-80.741901,40.007929],[-80.738717,39.985113],[-80.740126,39.970793],[-80.758527,39.959241],[-80.764479,39.95025],[-80.761312,39.929098],[-80.756784,39.920586],[-80.756432,39.91393],[-80.759296,39.909466],[-80.762592,39.908906],[-80.772641,39.911306],[-80.782849,39.917162],[-80.795714,39.91969],[-80.806018,39.91713],[-80.809283,39.910314],[-80.809011,39.903226],[-80.802339,39.89161],[-80.793989,39.882787],[-80.790156,39.872252],[-80.790761,39.86728],[-80.799898,39.858912],[-80.821279,39.849982],[-80.826124,39.844238],[-80.826228,39.835802],[-80.82248,39.824971],[-80.822181,39.811708],[-80.826079,39.798584],[-80.835311,39.79069],[-80.863048,39.775197],[-80.869092,39.766364],[-80.869933,39.763555],[-80.865339,39.753251],[-80.854717,39.742592],[-80.846091,39.737812],[-80.831551,39.719475],[-80.829764,39.711839],[-80.831871,39.705655],[-80.839112,39.701033],[-80.854599,39.697473],[-80.863698,39.691724],[-80.86633,39.683167],[-80.866647,39.652616],[-80.876002,39.627084],[-80.88036,39.620706],[-80.892208,39.616756],[-80.91762,39.618703],[-80.925841,39.617396],[-80.936906,39.612616],[-80.970436,39.590127],[-80.993695,39.571253],[-81.020055,39.55541],[-81.030169,39.545211],[-81.044902,39.5363],[-81.070594,39.515991],[-81.100833,39.487175],[-81.114433,39.466275],[-81.132534,39.446275],[-81.138134,39.443775],[-81.152534,39.443175],[-81.170634,39.439175],[-81.185946,39.430731],[-81.190714,39.423562],[-81.208231,39.407147],[-81.211433,39.402031],[-81.211654,39.392977],[-81.217315,39.38759],[-81.223581,39.386062],[-81.24184,39.390276],[-81.270716,39.385914],[-81.281405,39.379258],[-81.297517,39.374378],[-81.347567,39.34577],[-81.375961,39.341697],[-81.384556,39.343449],[-81.393794,39.351706],[-81.406689,39.38809],[-81.412706,39.394618],[-81.435642,39.408474],[-81.446543,39.410374],[-81.456143,39.409274],[-81.473188,39.40017],[-81.489044,39.384074],[-81.503189,39.373242],[-81.542346,39.352874],[-81.557547,39.338774],[-81.565047,39.293874],[-81.565247,39.276175],[-81.570247,39.267675],[-81.585559,39.268747],[-81.59516,39.273387],[-81.608408,39.276043],[-81.621305,39.273643],[-81.656138,39.277355],[-81.678331,39.273755],[-81.689483,39.266043],[-81.69638,39.257035],[-81.696636,39.246123],[-81.691067,39.230139],[-81.692395,39.226443],[-81.700908,39.220844],[-81.725583,39.215835]]]]},\"properties\":{\"name\":\"Ohio\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe1c","contributors":{"authors":[{"text":"Ebner, Andrew D. aebner@usgs.gov","contributorId":1849,"corporation":false,"usgs":true,"family":"Ebner","given":"Andrew","email":"aebner@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, David E. destraub@usgs.gov","contributorId":1908,"corporation":false,"usgs":true,"family":"Straub","given":"David","email":"destraub@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":301192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lageman, Jonathan D. jlageman@usgs.gov","contributorId":1910,"corporation":false,"usgs":true,"family":"Lageman","given":"Jonathan","email":"jlageman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301193,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97141,"text":"ds386 - 2008 - Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07","interactions":[],"lastModifiedDate":"2017-05-24T15:22:41","indexId":"ds386","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"386","title":"Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07","docAbstract":"<p><span>This report is a repository of reach-scale maps of hydraulic and substrate characteristics generated for the habitat-use portion of an interdisciplinary sturgeon research project on the Lower Missouri River (from Gavins Point Dam to the junction with the Mississippi River). The maps were derived from hydroacoustic data sets that were collected for the purpose of assessing physical aquatic habitat in the vicinity of locations of adult shovelnose sturgeon (</span><i>Scaphirhynchus platorynchus</i><span>) and pallid sturgeon (</span><i>S. albus</i><span>). Hydroacoustic data sets were collected at the reach scale (mean reach length, 2.4 kilometers) in order to include the immediate vicinity of a targeted sturgeon location as well as the full range of habitat available at the bend and crossover scale. Reaches typically were surveyed on the day following the relocation of a telemetered sturgeon and at a discharge within 10 percent of the discharge on the sturgeon relocation date in order to characterize as closely as possible the channel morphology and flow-field conditions at the time that the sturgeon was present. One hundred fifty-three reaches were mapped during April–September in the years 2005 through 2007, with the majority of data collection occurring in the months of May and June (coinciding with the period of sturgeon migration and spawning in the Lower Missouri River). Interpolated maps (grid cell size, 5 meters) depict depth, generalized substrate, and depth-averaged velocity. Side-scan sonar imagery is also available for a subset of reaches. Collectively, the maps represent more than 20 percent of the length of the Lower Missouri River.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds386","collaboration":"Prepared for the Missouri River Recovery-Integrated Science Program, U.S. Army Corps of Engineers, Yankton, South Dakota","usgsCitation":"Reuter, J.M., Jacobson, R.B., Elliott, C.M., Johnson, H.E., and DeLonay, A.J., 2008, Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07 (Version 1.0): U.S. Geological Survey Data Series 386, vi, 442 p., https://doi.org/10.3133/ds386.","productDescription":"vi, 442 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2005-04-01","temporalEnd":"2007-09-30","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":195439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":341688,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/386/pdf/DS386_508.pdf","text":"Report","size":"166.7 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":12125,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/386/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,38 ], [ -100,44 ], [ -88,44 ], [ -88,38 ], [ -100,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a353","contributors":{"authors":[{"text":"Reuter, Joanna M.","contributorId":50179,"corporation":false,"usgs":true,"family":"Reuter","given":"Joanna","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":301141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, Robert B. 0000-0002-8368-2064 rjacobson@usgs.gov","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":1289,"corporation":false,"usgs":true,"family":"Jacobson","given":"Robert","email":"rjacobson@usgs.gov","middleInitial":"B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":301138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, Caroline M. 0000-0002-9190-7462 celliott@usgs.gov","orcid":"https://orcid.org/0000-0002-9190-7462","contributorId":2380,"corporation":false,"usgs":true,"family":"Elliott","given":"Caroline","email":"celliott@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":301139,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Harold E. III","contributorId":47470,"corporation":false,"usgs":true,"family":"Johnson","given":"Harold","suffix":"III","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":301140,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeLonay, Aaron J.","contributorId":53360,"corporation":false,"usgs":true,"family":"DeLonay","given":"Aaron","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301142,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70198276,"text":"70198276 - 2008 - Seismicity and deformation induced by magma accumulation at three basaltic volcanoes","interactions":[],"lastModifiedDate":"2019-03-20T12:19:05","indexId":"70198276","displayToPublicDate":"2008-12-18T08:46:44","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"subseriesTitle":"Seismology","title":"Seismicity and deformation induced by magma accumulation at three basaltic volcanoes","docAbstract":"<p><span>We analyzed the evolution of volcano‐tectonic (VT) seismicity and deformation at three basaltic volcanoes (Kilauea, Mauna Loa, Piton de la Fournaise) during phases of magma accumulation. We observed that the VT earthquake activity displays an accelerating evolution at the three studied volcanoes during the time of magma accumulation. At the same times, deformation rates recorded at the summit of Kilauea and Mauna Loa volcanoes were not accelerating but rather tend to decay. To interpret these observations, we propose a physical model describing the evolution of pressure produced by the accumulation of magma into a reservoir. This variation of pressure is then used to force a simple model of damage, where damage episodes are equivalent to earthquakes. This model leads to an exponential increase of the VT activity and to an exponential decay of the deformation rate during accumulation phases. Seismicity and deformation data are well fitted by such an exponential model. The time constant, deduced from the exponential increase of the seismicity, is in agreement with the time constant predicted by the model of magma accumulation. This VT activity can thus be a direct indication of the accumulation of magma at depth, and therefore can be seen as a long‐term precursory phenomenon, at least for the three studied basaltic volcanoes. Unfortunately, it does not allow the prediction of the onset of future eruptions, as no diverging point (i.e., critical time) is present in the model.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/2008JB005937","usgsCitation":"Lengline, O., Marsan, D., Got, J., Pinel, V., Ferrazzini, V., and Okubo, P.G., 2008, Seismicity and deformation induced by magma accumulation at three basaltic volcanoes: Journal of Geophysical Research B: Solid Earth, v. 113, no. B12, B12305; 12 p., https://doi.org/10.1029/2008JB005937.","productDescription":"B12305; 12 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":476576,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2008jb005937","text":"Publisher Index Page"},{"id":356029,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"113","issue":"B12","noUsgsAuthors":false,"publicationDate":"2008-12-18","publicationStatus":"PW","scienceBaseUri":"5b98bc7ee4b0702d0e845427","contributors":{"authors":[{"text":"Lengline, O.","contributorId":206506,"corporation":false,"usgs":false,"family":"Lengline","given":"O.","email":"","affiliations":[],"preferred":false,"id":740861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marsan, David","contributorId":198073,"corporation":false,"usgs":false,"family":"Marsan","given":"David","email":"","affiliations":[],"preferred":false,"id":740862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Got, J.-L.","contributorId":80867,"corporation":false,"usgs":true,"family":"Got","given":"J.-L.","email":"","affiliations":[],"preferred":false,"id":740863,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pinel, Virginie","contributorId":139984,"corporation":false,"usgs":false,"family":"Pinel","given":"Virginie","email":"","affiliations":[{"id":13343,"text":"Université de Savoie · ISTerre Sciences Institute EARTH","active":true,"usgs":false}],"preferred":false,"id":740864,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ferrazzini, Valerie","contributorId":100035,"corporation":false,"usgs":true,"family":"Ferrazzini","given":"Valerie","email":"","affiliations":[],"preferred":false,"id":740865,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Okubo, Paul G. 0000-0002-0381-6051 pokubo@usgs.gov","orcid":"https://orcid.org/0000-0002-0381-6051","contributorId":2730,"corporation":false,"usgs":true,"family":"Okubo","given":"Paul","email":"pokubo@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":740866,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":97137,"text":"ofr20081359 - 2008 - Bathymetric and hydraulic survey of the Matanuska River near Circle View Estates, Alaska","interactions":[],"lastModifiedDate":"2018-04-23T10:35:45","indexId":"ofr20081359","displayToPublicDate":"2008-12-18T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1359","title":"Bathymetric and hydraulic survey of the Matanuska River near Circle View Estates, Alaska","docAbstract":"<p>An acoustic Doppler current profiler interfaced with a differentially corrected global positioning system was used to map bathymetry and multi-dimensional velocities on the Matanuska River near Circle View Estates, Alaska. Data were collected along four spur dikes and a bend in the river during a period of active bank erosion. These data were collected as part of a larger investigation into channel processes being conducted to aid land managers with development of a long-term management plan for land near the river. The banks and streambed are composed of readily erodible material and the braided channels frequently scour and migrate. Lateral channel migration has resulted in the periodic loss of properties and structures along the river for decades.</p><p>For most of the survey, discharge of the Matanuska River was less than the 25th percentile of long-term streamflow. Despite this relatively low flow, measured water velocities were as high as 15 feet per second. The survey required a unique deployment of the acoustic Doppler current profiler in a tethered boat that was towed by a small inflatable raft. Data were collected along cross sections and longitudinal profiles. The bathymetric and velocity data document river conditions before the installation of an additional spur dike in 2006 and during a period of bank erosion. Data were collected along 1,700 feet of river in front of the spur dikes and along 1,500&nbsp;feet of an eroding bank.</p><p>Data collected at the nose of spur dikes 2, 3, and 4 were selected to quantify the flow hydraulics at the locations subject to the highest velocities. The measured velocities and flow depths were greatest at the nose of the downstream-most spur dike. The maximum point velocity at the spur dike nose was 13.3 feet per second and the maximum depth-averaged velocity was 11.6 feet per second. The maximum measured depth was 12.0 feet at the nose of spur dike 4 and velocities greater than 10 feet per second were measured to a depth of 10&nbsp;feet.</p><p>Data collected along an eroding bank provided details of the spatial distribution and variability in magnitude of velocities and flow depths while erosion was taking place. Erosion was concentrated in an area just downstream of the apex of a river bend. Measured velocities and flow depths were greater in the apex of the bend than in the area of maximum bank erosion. The maximum measured velocity was 12.9 feet per second at the apex and 11.2 feet per second in front of the eroding bank. The maximum measured depth was 10.2 feet at the apex and 5.2 feet in front of the eroding bank.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081359","collaboration":"Prepared in cooperation with the Matanuska-Susitna Borough","usgsCitation":"Conaway, J.S., 2008, Bathymetric and hydraulic survey of the Matanuska River near Circle View Estates, Alaska: U.S. Geological Survey Open-File Report 2008-1359, Report: iv, 21 p.; 2 Appendixes, https://doi.org/10.3133/ofr20081359.","productDescription":"Report: iv, 21 p.; 2 Appendixes","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":195283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12121,"rank":99,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1359/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,60.75 ], [ -150,62.5 ], [ -147,62.5 ], [ -147,60.75 ], [ -150,60.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640aaa","contributors":{"authors":[{"text":"Conaway, Jeffrey S. 0000-0002-3036-592X jconaway@usgs.gov","orcid":"https://orcid.org/0000-0002-3036-592X","contributorId":2026,"corporation":false,"usgs":true,"family":"Conaway","given":"Jeffrey","email":"jconaway@usgs.gov","middleInitial":"S.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":301127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97124,"text":"sir20085181 - 2008 - An Integrated Hydrogeologic and Geophysical Investigation to Characterize the Hydrostratigraphy of the Edwards Aquifer in an Area of Northeastern Bexar County, Texas","interactions":[],"lastModifiedDate":"2016-08-23T12:45:41","indexId":"sir20085181","displayToPublicDate":"2008-12-18T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5181","title":"An Integrated Hydrogeologic and Geophysical Investigation to Characterize the Hydrostratigraphy of the Edwards Aquifer in an Area of Northeastern Bexar County, Texas","docAbstract":"<p>In August 2007, the U.S. Geological Survey, in cooperation with the San Antonio Water System, did a hydrogeologic and geophysical investigation to characterize the hydrostratigraphy (hydrostratigraphic zones) and also the hydrogeologic features (karst features such as sinkholes and caves) of the Edwards aquifer in a 16-square-kilometer area of northeastern Bexar County, Texas, undergoing urban development. Existing hydrostratigraphic information, enhanced by local-scale geologic mapping in the area, and surface geophysics were used to associate ranges of electrical resistivities obtained from capacitively coupled (CC) resistivity surveys, frequency-domain electromagnetic (FDEM) surveys, time-domain electromagnetic (TDEM) soundings, and two-dimensional direct-current (2D-DC) resistivity surveys with each of seven hydrostratigraphic zones (equivalent to members of the Kainer and Person Formations) of the Edwards aquifer. The principal finding of this investigation is the relation between electrical resistivity and the contacts between the hydrostratigraphic zones of the Edwards aquifer and the underlying Trinity aquifer in the area. In general, the TDEM data indicate a two-layer model in which an electrical conductor underlies an electrical resistor, which is consistent with the Trinity aquifer (conductor) underlying the Edwards aquifer (resistor). TDEM data also show the plane of Bat Cave fault, a well-known fault in the area, to be associated with a local, nearly vertical zone of low resistivity that provides evidence, although not definitive, for Bat Cave fault functioning as a flow barrier, at least locally. In general, the CC resistivity, FDEM survey, and 2D-DC resistivity survey data show a sharp electrical contrast from north to south, changing from high resistivity to low resistivity across Bat Cave fault as well as possible karst features in the study area. Interpreted karst features that show relatively low resistivity within a relatively high-resistivity area likely are attributable to clay or soil filling a sinkhole. In general, faults are inferred where lithologic incongruity indicates possible displacement. Along most inferred faults, displacement was not sufficient to place different members of the Kainer or Person Formations (hydrostratigraphic zones) adjacent across the inferred fault plane. In general, the Kainer Formation (hydrostratigraphic zones V through VIII) has a higher resistivity than the Person Formation (hydrostratigraphic zones II through IV). Although resistivity variations from the CC resistivity, FDEM, and 2D-DC resistivity surveys, with mapping information, were sufficient to allow surface mapping of the lateral extent of hydrostratigraphic zones in places, resistivity variations from TDEM data were not sufficient to allow vertical delineation of hydrostratigraphic zones; however, the Edwards aquifer-Trinity aquifer contact could be identified from the TDEM data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20085181","collaboration":"Prepared in cooperation with the San Antonio Water System","usgsCitation":"Shah, S., Smith, B.D., Clark, A.K., and Payne, J., 2008, An Integrated Hydrogeologic and Geophysical Investigation to Characterize the Hydrostratigraphy of the Edwards Aquifer in an Area of Northeastern Bexar County, Texas (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2008-5181, Report: vi, 26 p.; Plate: 24 x 18 inches; Data Files, https://doi.org/10.3133/sir20085181.","productDescription":"Report: vi, 26 p.; Plate: 24 x 18 inches; Data Files","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2007-08-01","temporalEnd":"2007-08-31","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5181.jpg"},{"id":12108,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5181/","linkFileType":{"id":5,"text":"html"}},{"id":327655,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2008/5181/pdf/sir2008-5181.pdf","size":"8.59 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":327656,"rank":102,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sir/2008/5181/pdf/sir2008-5181-pl1.pdf","size":"26.7 MB","linkFileType":{"id":1,"text":"pdf"}}],"projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.43416666666667,29.634166666666665 ], [ -98.43416666666667,29.683333333333334 ], [ -98.36666666666666,29.683333333333334 ], [ -98.36666666666666,29.634166666666665 ], [ -98.43416666666667,29.634166666666665 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864d4","contributors":{"authors":[{"text":"Shah, Sachin D.","contributorId":60174,"corporation":false,"usgs":true,"family":"Shah","given":"Sachin D.","affiliations":[],"preferred":false,"id":301100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Bruce D. 0000-0002-1643-2997 bsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-1643-2997","contributorId":845,"corporation":false,"usgs":true,"family":"Smith","given":"Bruce","email":"bsmith@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":301097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, Allan K. 0000-0003-0099-1521 akclark@usgs.gov","orcid":"https://orcid.org/0000-0003-0099-1521","contributorId":1279,"corporation":false,"usgs":true,"family":"Clark","given":"Allan","email":"akclark@usgs.gov","middleInitial":"K.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Payne, Jason  0000-0003-4294-7924 jdpayne@usgs.gov","orcid":"https://orcid.org/0000-0003-4294-7924","contributorId":1062,"corporation":false,"usgs":true,"family":"Payne","given":"Jason ","email":"jdpayne@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":false,"id":301098,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97129,"text":"fs20083090 - 2008 - Water quality of streams in Johnson County, Kansas, 2002-07","interactions":[],"lastModifiedDate":"2017-08-08T13:47:32","indexId":"fs20083090","displayToPublicDate":"2008-12-18T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3090","title":"Water quality of streams in Johnson County, Kansas, 2002-07","docAbstract":"Water quality of streams in Johnson County, Kansas was evaluated from October 2002 through December 2007 in a cooperative study between the U.S. Geological Survey and the Johnson County Stormwater Management Program. Water quality at 42 stream sites, representing urban and rural basins, was characterized by evaluating benthic macroinvertebrates, water (discrete and continuous data), and/or streambed sediment. Point and nonpoint sources and transport were described for water-quality constituents including suspended sediment, dissolved solids and major ions, nutrients (nitrogen and phosphorus), indicator bacteria, pesticides, and organic wastewater and pharmaceutical compounds. The information obtained from this study is being used by city and county officials to develop effective management plans for protecting and improving stream quality. This fact sheet summarizes important results from three comprehensive reports published as part of the study and available on the World Wide Web at http://ks.water.usgs.gov/Kansas/studies/qw/joco/ .\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20083090","collaboration":"Prepared in cooperation with the Johnson County Stormwater Management Program","usgsCitation":"Rasmussen, T.J., 2008, Water quality of streams in Johnson County, Kansas, 2002-07 (Version 1.0): U.S. Geological Survey Fact Sheet 2008-3090, 4 p., https://doi.org/10.3133/fs20083090.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2002-10-01","temporalEnd":"2007-12-31","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":124770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3090.jpg"},{"id":12113,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3090/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.08333333333333,38.666666666666664 ], [ -95.08333333333333,39.166666666666664 ], [ -94.41666666666667,39.166666666666664 ], [ -94.41666666666667,38.666666666666664 ], [ -95.08333333333333,38.666666666666664 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655143","contributors":{"authors":[{"text":"Rasmussen, Teresa J. 0000-0002-7023-3868 rasmuss@usgs.gov","orcid":"https://orcid.org/0000-0002-7023-3868","contributorId":3336,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Teresa","email":"rasmuss@usgs.gov","middleInitial":"J.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":301109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97134,"text":"ds380 - 2008 - River Channel Topographic Surveys Collected Prior to and Following Elevated Flows in the Central Platte River, Spring 2008","interactions":[],"lastModifiedDate":"2012-02-10T00:11:55","indexId":"ds380","displayToPublicDate":"2008-12-18T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"380","title":"River Channel Topographic Surveys Collected Prior to and Following Elevated Flows in the Central Platte River, Spring 2008","docAbstract":"Rainfall in central Nebraska in late May and early June 2008 elevated streamflows in the central Platte River. Topographic surveys collected along geomorphic monitoring transects prior to these flows (May 2007, July 2007, and March 2008) were repeated in mid-June 2008. These surveys provide characterization of river topography that could be used (1) to infer changes in channel morphology that occurred as a result of this flow event, and (2) to aid in the determination of the effect of managed and natural flow events on habitats for endangered and threatened species in the Platte River basin. The primary purposes of this report are to summarize the methods of data collection, processing, and editing and to make the data described in the report publicly available.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ds380","collaboration":"Prepared in cooperation with the Platte River Recovery Implementation Program","usgsCitation":"Kinzel, P.J., 2008, River Channel Topographic Surveys Collected Prior to and Following Elevated Flows in the Central Platte River, Spring 2008 (Version 1.0): U.S. Geological Survey Data Series 380, Report: iv, 10 p.; Downloads Directory, https://doi.org/10.3133/ds380.","productDescription":"Report: iv, 10 p.; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2007-05-01","temporalEnd":"2008-06-30","costCenters":[{"id":434,"text":"National Research Program","active":false,"usgs":true}],"links":[{"id":196430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12117,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/380/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,40.5 ], [ -100,41 ], [ -98,41 ], [ -98,40.5 ], [ -100,40.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce9e","contributors":{"authors":[{"text":"Kinzel, Paul J. 0000-0002-6076-9730 pjkinzel@usgs.gov","orcid":"https://orcid.org/0000-0002-6076-9730","contributorId":743,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","email":"pjkinzel@usgs.gov","middleInitial":"J.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97135,"text":"ofr20081358 - 2008 - Analytical Results for Municipal Biosolids Samples from a Monitoring Program near Deer Trail, Colorado (U.S.A.), 2007","interactions":[],"lastModifiedDate":"2012-02-10T00:11:48","indexId":"ofr20081358","displayToPublicDate":"2008-12-18T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-1358","title":"Analytical Results for Municipal Biosolids Samples from a Monitoring Program near Deer Trail, Colorado (U.S.A.), 2007","docAbstract":"Since late 1993, the Metro Wastewater Reclamation District of Denver (Metro District), a large wastewater treatment plant in Denver, Colorado, has applied Grade I, Class B biosolids to about 52,000 acres of nonirrigated farmland and rangeland near Deer Trail, Colorado (U.S.A.). In cooperation with the Metro District in 1993, the U.S. Geological Survey (USGS) began monitoring ground water at part of this site. In 1999, the USGS began a more comprehensive monitoring study of the entire site to address stakeholder concerns about the potential chemical effects of biosolids applications to water, soil, and vegetation. This more comprehensive monitoring program recently has been extended through 2010. Monitoring components of the more comprehensive study include biosolids collected at the wastewater treatment plant, soil, crops, dust, alluvial and bedrock ground water, and streambed sediment. Streams at the site are dry most of the year, so samples of streambed sediment deposited after rain were used to indicate surface-water effects. This report will present only analytical results for the biosolids samples collected at the Metro District wastewater treatment plant in Denver and analyzed during 2007. We have presented earlier a compilation of analytical results for the biosolids samples collected and analyzed for 1999 through 2006. More information about the other monitoring components is presented elsewhere in the literature. Priority parameters for biosolids identified by the stakeholders and also regulated by Colorado when used as an agricultural soil amendment include the total concentrations of nine trace elements (arsenic, cadmium, copper, lead, mercury, molybdenum, nickel, selenium, and zinc), plutonium isotopes, and gross alpha and beta activity. Nitrogen and chromium also were priority parameters for ground water and sediment components.\r\n\r\nIn general, the objective of each component of the study was to determine whether concentrations of priority parameters (1) were higher than regulatory limits, (2) were increasing with time, or (3) were significantly higher in biosolids-applied areas than in a similar farmed area where biosolids were not applied.\r\n\r\nPrevious analytical results indicate that the elemental composition of the biosolids from the Denver plant was consistent during 1999-2006 and this consistency continues with the samples for 2007; total concentrations of regulated trace elements remained consistently lower than the regulatory limits for the entire monitoring period.\r\n\r\nOur previously reported data (1999-2006) and data presented in this report were used to compile an inorganic-chemical biosolids signature that can be contrasted with the geochemical signature for this site. The biosolids signature and an understanding of the geology and hydrology of the site can be used to separate biosolids effects from natural geochemical effects. Elements of particular interest for a biosolids signature include bismuth, copper, silver, mercury, phosphorus, and silver.\r\n\r\nAn alternative method of digestion of biosolids was also recently investigated, and the results are presented in this report. A microwave digestion using only nitric acid at controlled elevated temperature and pressure was tested to replace the much more time-consuming and labor-intensive, traditional four-acid, hotplate method for the preparation of solutions to be analyzed by inductively coupled plasma-mass spectrometry (ICP-MS). Elements of concern determined by ICP-MS following digestion include cadmium, copper, lead, molybdenum, nickel, and zinc. The microwave 'digestion' proved to be a strong acid leach, and it was less efficient at digesting the biosolids samples with consistently lower recoveries (compared to the four-acid digestion value) for most elements, but especially for the elements of concern - copper, nickel, and zinc. Other elements traditionally associated with the silicate or oxide minerals demonstrated low recoveries, especially titaniu","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081358","usgsCitation":"Crock, J., Smith, D.B., Yager, T.J., Berry, C., and Adams, M.G., 2008, Analytical Results for Municipal Biosolids Samples from a Monitoring Program near Deer Trail, Colorado (U.S.A.), 2007 (Version 1.0): U.S. Geological Survey Open-File Report 2008-1358, iv, 35 p., https://doi.org/10.3133/ofr20081358.","productDescription":"iv, 35 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2007-01-01","temporalEnd":"2007-12-31","costCenters":[{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"links":[{"id":195097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12118,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1358/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,39.3675 ], [ -104,39.73444444444444 ], [ -103.7,39.73444444444444 ], [ -103.7,39.3675 ], [ -104,39.3675 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb63","contributors":{"authors":[{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":301120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":301118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yager, T. J. B.","contributorId":77256,"corporation":false,"usgs":true,"family":"Yager","given":"T.","email":"","middleInitial":"J. B.","affiliations":[],"preferred":false,"id":301121,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Berry, C. J.","contributorId":52680,"corporation":false,"usgs":true,"family":"Berry","given":"C. J.","affiliations":[],"preferred":false,"id":301119,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Adams, M. G.","contributorId":84812,"corporation":false,"usgs":true,"family":"Adams","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":301122,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}