{"pageNumber":"182","pageRowStart":"4525","pageSize":"25","recordCount":37001,"records":[{"id":79564,"text":"ofr20061358 - 2006 - Knowledge and Understanding of the Hydrogeology of the Salt Basin in South-Central New Mexico and Future Study Needs","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061358","displayToPublicDate":"2007-01-13T00:00:00","publicationYear":"2006","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":"2006-1358","title":"Knowledge and Understanding of the Hydrogeology of the Salt Basin in South-Central New Mexico and Future Study Needs","docAbstract":"The Salt Basin covers about 2,400 square miles of south-central New Mexico and extends across the State line into Texas. As much as 57 million acre-feet of ground water may be stored within the New Mexico part of the Salt Basin of which 15 million acre-feet are potentially potable and recoverable. Recent work suggests that the volume of ground water in storage within the New Mexico portion of the Salt Basin may be substantially greater than 57 million acre-feet. \r\n\r\nIn this report, aquifers contained in the San Andres, Bone Spring, and Victorio Peak Limestones and in the Yeso, Hueco, and Abo Formations are collectively referred to as the carbonate aquifer. Porosity and permeability of the major aquifer are primarily determined by the density and interconnectedness of fractures and karstic solution channels. The spatial variability of these fractures and karstic features leads to a large spatial variability in hydraulic properties in the carbonate aquifer. \r\n\r\nGround water generally moves southward away from recharge areas along the northern border of the Salt Basin and generally moves eastward to southeastward away from areas of distributed recharge on the Otero Mesa and the Diablo Plateau. Ground water originating from these recharge areas generally moves toward the central valley. Present day discharge is mostly through ground-water withdrawal for agricultural irrigation. A zone of relatively low hydraulic gradient, corresponding to the location of the Otero Break, extends from near the Sacramento River watershed southward toward Dell City, Texas. Ground water in the carbonate aquifer generally is very hard and has dissolved-solids concentrations ranging from 500 to 6,500 milligrams per liter. \r\n\r\nSubstantial variability exists in current estimates of (1) ground-water recharge, (2) natural ground-water discharge, (3) the volume of ground water in storage, (4) the volume of recoverable ground water, (5) the conceptual model of ground-water flow, (6) the distribution of ground-water quality, and (7) the distribution of hydraulic characteristics. Future study could reduce uncertainty in these estimates and allow for better management of ground-water resources in the Salt Basin.\r\n","language":"ENGLISH","doi":"10.3133/ofr20061358","usgsCitation":"Huff, G.F., and Chace, D., 2006, Knowledge and Understanding of the Hydrogeology of the Salt Basin in South-Central New Mexico and Future Study Needs (Version 1.0): U.S. Geological Survey Open-File Report 2006-1358, iv, 17 p., https://doi.org/10.3133/ofr20061358.","productDescription":"iv, 17 p.","numberOfPages":"21","onlineOnly":"Y","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":194507,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9181,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1358/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48c0","contributors":{"authors":[{"text":"Huff, G. F.","contributorId":11229,"corporation":false,"usgs":true,"family":"Huff","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":290244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chace, D.A.","contributorId":60338,"corporation":false,"usgs":true,"family":"Chace","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":290245,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79550,"text":"ofr20061313 - 2006 - Flood Study of Warren Brook in Alstead and Cold River in Alstead, Langdon, and Walpole, New Hampshire, 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061313","displayToPublicDate":"2007-01-12T00:00:00","publicationYear":"2006","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":"2006-1313","title":"Flood Study of Warren Brook in Alstead and Cold River in Alstead, Langdon, and Walpole, New Hampshire, 2005","docAbstract":"This report presents water-surface elevations and profiles as determined using the U.S. Army Corps of Engineers (USACE) one-dimensional Hydrologic Engineering Center River Analysis System, also known as HEC-RAS. Steady flow water-surface profiles were developed for two stream reaches: the Cold River from its confluence with the Connecticut River in Walpole, through Alstead to the McDermott Bridge in Langdon, NH, and Warren Brook from its confluence with the Cold River to Warren Lake in Alstead, NH. Flood events of a magnitude, which are expected to be equaled or exceeded once on the average during any 10-, 50-, 100-, or 500-year period (recurrence interval), were modeled using HEC-RAS as these flood events are recognized as being significant for flood-plain management, determination of flood insurance rates, and design of structures such as bridges and culverts. These flood events are referred to as the 10-, 50-, 100-, and 500-year floods and have a 10-, 2-, 1-, and 0.2-percent chance, respectively, of being equaled or exceeded during any year. The recurrence intervals represent the long-term average between floods of a specific magnitude. The risk of experiencing rare floods at short intervals or within the same year increases when periods greater than one year are considered. The analyses in this study reflect the flooding potentials based on conditions existing in the communities of Walpole, Alstead and Langdon at the time of completion of this study.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061313","collaboration":"Prepared in cooperation with the New Hampshire Department of Transportation","usgsCitation":"Flynn, R.H., 2006, Flood Study of Warren Brook in Alstead and Cold River in Alstead, Langdon, and Walpole, New Hampshire, 2005: U.S. Geological Survey Open-File Report 2006-1313, iv, 48 p., https://doi.org/10.3133/ofr20061313.","productDescription":"iv, 48 p.","numberOfPages":"52","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":194465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9166,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1313/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eee8a","contributors":{"authors":[{"text":"Flynn, Robert H. rflynn@usgs.gov","contributorId":2137,"corporation":false,"usgs":true,"family":"Flynn","given":"Robert","email":"rflynn@usgs.gov","middleInitial":"H.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79548,"text":"ofr20061372 - 2006 - Geologic Map of the Edwards Aquifer In Northern Medina and Northeastern Uvalde Counties, South-central Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"ofr20061372","displayToPublicDate":"2007-01-11T00:00:00","publicationYear":"2006","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":"2006-1372","title":"Geologic Map of the Edwards Aquifer In Northern Medina and Northeastern Uvalde Counties, South-central Texas","docAbstract":"The southern segment of the Edwards aquifer in south-central Texas is one of the most productive subsurface reservoirs of potable water in the world, providing water of excellent quality to more than a million people in the San Antonio region, where the Environmental Protection Agency (EPA) has declared it to be a sole-source aquifer (van der Leeden and others, 1990). Depending on the depositional province within which the associated carbonate rocks originated (Maclay and Small, 1984), the Edwards aquifer is composed of several geologic formations (primarily limestone and dolostone) of Early Cretaceous age.\r\n\r\nMost water pumped from the Edwards aquifer comes form the Person and Kainer Formations, which were deposited over the San Marcos Platform. The principal source of ground water in study area is the Devils River Formation, which was deposited in the Devils River trend. The Devils River Formation provides large quantities of irrigation water to fertile bottomland areas of Medina and Uvalde Counties, where the success of farming and ranching activities has long depended upon water from the Edwards aquifer.\r\n\r\nThe study area includes all of the Edwards aquifer recharge zone between the Sabinal River (on the west) and the Medina River (on the east) plus an updip fringe of the confined zone in east-central Uvalde and central Medina Counties. Over about ninety percent of the study area--within the Devils River trend--the Edwards aquifer is composed of the Georgetown Formation plus the underlying Devils River Formation. Over the remaining area--over the southwestern margin of the San Marcos platform--the Edwards aquifer consists of the Georgetown Formation plus the underlying Edwards Group (Rose, 1972), which comprises the Kainer and Person Formations.\r\n","language":"ENGLISH","doi":"10.3133/ofr20061372","usgsCitation":"Clark, A.K., Faith, J.R., Blome, C.D., and Pedraza, D.E., 2006, Geologic Map of the Edwards Aquifer In Northern Medina and Northeastern Uvalde Counties, South-central Texas (Version 1.0): U.S. Geological Survey Open-File Report 2006-1372, 22 p.; plate, 36 by 43 inches; data files, https://doi.org/10.3133/ofr20061372.","productDescription":"22 p.; plate, 36 by 43 inches; data files","numberOfPages":"22","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":110699,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_80464.htm","linkFileType":{"id":5,"text":"html"},"description":"80464"},{"id":194823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9163,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1372/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8528","contributors":{"authors":[{"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":290200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faith, Jason R.","contributorId":92758,"corporation":false,"usgs":true,"family":"Faith","given":"Jason","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290202,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blome, Charles D. 0000-0002-3449-9378 cblome@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-9378","contributorId":1246,"corporation":false,"usgs":true,"family":"Blome","given":"Charles","email":"cblome@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":290199,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pedraza, Diana E. 0000-0003-4483-8094 dpedraza@usgs.gov","orcid":"https://orcid.org/0000-0003-4483-8094","contributorId":1281,"corporation":false,"usgs":false,"family":"Pedraza","given":"Diana","email":"dpedraza@usgs.gov","middleInitial":"E.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290201,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79546,"text":"ofr20061359 - 2006 - Calculation of area and volume for the north part of Great Salt Lake, Utah","interactions":[],"lastModifiedDate":"2017-04-10T15:58:54","indexId":"ofr20061359","displayToPublicDate":"2007-01-11T00:00:00","publicationYear":"2006","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":"2006-1359","title":"Calculation of area and volume for the north part of Great Salt Lake, Utah","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Utah Department of Natural Resources, Division of Forestry, Fire, and State Lands, collected bathymetric data for the north part of Great Salt Lake during the spring and early summer of 2006 using a single-beam, high-definition fathometer and real-time differential global positioning system. About 5.2 million depth measurements were collected along more than 765 miles (1,230 kilometers) of survey transects. Sound-velocity profiles were obtained in conjunction with the bathymetric data to provide time-of-travel corrections to the depth calculations. Data were processed with commercial hydrographic software and exported into geographic information system (GIS) software for mapping and calculation of area and volume. Area and volume calculations show a maximum area of about 385,000 acres (1,560 square kilometers) and a maximum volume of about 5,693,000 acre-feet (about 7 cubic kilometers) at a water-surface altitude of 4,200 feet (1,280 meters). Minimum natural water-surface altitude of the north part of Great Salt Lake is just below 4,167 feet (1,270 meters) in the area just north of the Union Pacific railroad causeway halfway between Saline and the western edge of the lake. The north part of Great Salt Lake generally grades gradually to the west and north and is bounded by steep scarps along its eastern border. Calculations for area and volume are based on a low altitude of 4,167 feet (1,270 meters) to a high altitude of 4,200 feet (1,280 meters).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061359","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Forestry, Fire, and State Lands","usgsCitation":"Baskin, R.L., 2006, Calculation of area and volume for the north part of Great Salt Lake, Utah: U.S. Geological Survey Open-File Report 2006-1359, 6 p., https://doi.org/10.3133/ofr20061359.","productDescription":"6 p.","numberOfPages":"6","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":191386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334872,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sim2954","text":"Scientific Investigations Map 2954: Bathymetric map of the north part of Great Salt Lake, Utah, 2006","linkHelpText":"Scientific Investigations Map 2954: Bathymetric map of the north part of Great Salt Lake, Utah, 2006"},{"id":9161,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1359/","linkFileType":{"id":5,"text":"html"}},{"id":334871,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1359/PDF/ofr2006-1359.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.1139,\n              41.19889\n            ],\n            [\n              -113.1139,\n              41.76667\n            ],\n            [\n              -112.4717,\n              41.76667\n            ],\n            [\n              -112.4717,\n              41.19889\n            ],\n            [\n              -113.1139,\n              41.19889\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96a6","contributors":{"authors":[{"text":"Baskin, Robert L. 0000-0002-2175-8502 rbaskin@usgs.gov","orcid":"https://orcid.org/0000-0002-2175-8502","contributorId":360,"corporation":false,"usgs":true,"family":"Baskin","given":"Robert","email":"rbaskin@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79545,"text":"ofr20061397 - 2006 - Map showing features and displacements of the Scenic Drive landslide, La Honda, California, during the period March 31, 2005–November 5, 2006","interactions":[],"lastModifiedDate":"2021-09-02T20:10:52.433431","indexId":"ofr20061397","displayToPublicDate":"2007-01-10T00:00:00","publicationYear":"2006","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":"2006-1397","title":"Map showing features and displacements of the Scenic Drive landslide, La Honda, California, during the period March 31, 2005–November 5, 2006","docAbstract":"<p>The Scenic Drive landslide in La Honda, San Mateo County, California began movement during the El Ni<span>ñ</span>o winter of 1997-98. Recurrent motion occurred during the mild El Ni<span>ñ</span>o winter of 2004-2005 and again during the winter of 2005-06. This report documents the changing geometry and motion of the Scenic Drive landslide in 2005-2006, and it documents changes and persistent features that we interpret to reflect underlying structural control of the landslide. We have also compared the displacement history to near-real time rainfall history at a continuously recording gauge for the period October 2004-November 2006.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061397","usgsCitation":"Wells, R., Rymer, M.J., Prentice, C.S., and Wheeler, K.L., 2006, Map showing features and displacements of the Scenic Drive landslide, La Honda, California, during the period March 31, 2005–November 5, 2006 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1397, HTML Document, https://doi.org/10.3133/ofr20061397.","productDescription":"HTML Document","temporalStart":"2005-03-31","temporalEnd":"2006-11-05","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":192546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9103,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1397/","linkFileType":{"id":5,"text":"html"}},{"id":110694,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78841.htm","linkFileType":{"id":5,"text":"html"},"description":"78841"}],"country":"United States","state":"California","city":"LaHonda","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.27,37.31 ], [ -122.27,37.32 ], [ -122.26,37.32 ], [ -122.26,37.31 ], [ -122.27,37.31 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6587c6","contributors":{"authors":[{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":290194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":290192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prentice, Carol S. 0000-0003-3732-3551 cprentice@usgs.gov","orcid":"https://orcid.org/0000-0003-3732-3551","contributorId":2676,"corporation":false,"usgs":true,"family":"Prentice","given":"Carol","email":"cprentice@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":290193,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wheeler, Karen L. kwheeler@usgs.gov","contributorId":3404,"corporation":false,"usgs":true,"family":"Wheeler","given":"Karen","email":"kwheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":290195,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79540,"text":"ofr20061343 - 2006 - Preliminary Assessment of Landslides Along the Florida River Downstream from Lemon Reservoir, La Plata County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20061343","displayToPublicDate":"2007-01-06T00:00:00","publicationYear":"2006","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":"2006-1343","title":"Preliminary Assessment of Landslides Along the Florida River Downstream from Lemon Reservoir, La Plata County, Colorado","docAbstract":"Nearly two-dozen shallow landslides were active during spring 2005 on a hillside located along the east side of the Florida River about one kilometer downstream from Lemon Reservoir in La Plata County, southwestern Colorado. Landslides on the hillside directly threaten human safety, residential structures, a county roadway, utilities, and the Florida River, and indirectly threaten downstream areas and Lemon Dam. Most of the area where the landslides occurred was burned during the 2002 Missionary Ridge wildfire. We performed geologic mapping, subsurface exploration and sampling, radiocarbon dating, and shallow ground-water and ground-displacement monitoring to assess landslide activity. Active landslides during spring 2005 were as large as 35,000 m3 and confined to colluvium. Debris flows were mobilized from most of the landslides, were as large as 1,500 m3, and traveled as far as 250 m. Landslide activity was triggered by elevated ground-water pressures within the colluvium caused by infiltration of snowmelt. Landslide activity ceased as ground-water pressures dropped during the summer. Shallow landslides on the hillside appear to be much more likely following the Missionary Ridge fire because of the loss of tree root strength and evapotranspiration. We used monitoring data and observations to develop preliminary, approximate rainfall/snowmelt thresholds above which shallow landslide activity can be expected. Landslides triggered during spring 2005 occurred within a 1.97 x 107 m3 older landslide that extends, on average, about 40 m into bedrock. The south end of this older landslide appears to have experienced deep secondary landsliding. Radiocarbon dating of sediments at the head of the older landslide suggests that the landslide was active about 1,424-1,696 years ago. A relatively widespread wildfire may have preceded the older landslide, and the landslide may have occurred during a wetter time. The wetter climate and effects of the wildfire would likely have resulted in increased ground-water pressures, which may have triggered the older landslide. This landslide appears to have crossed the valley floor and been subsequently eroded from this area. We found no evidence that landslide debris across the valley floor formed an impoundment of the Florida River, although it is very likely. Erosion of buttressing landslide debris from the valley floor and the lower strength of the landslide basal shear zone relative to pre-slide strength created less stable conditions than were present prior to occurrence of the landslide. However, deep ground-water conditions largely control the stability of the slope and are unknown here; hence, the potential for future deep landsliding is unknown. Additional investigation could be undertaken to further characterize landslide hazards in the area. This investigation could include episodic surveying of monuments we installed across the older landslide, obtaining detailed topographic data and aerial photography, mapping landslide debris and lacustrine deposits related to the potential former landslide dam, mapping secondary landslides, obtaining additional ages of landslide activity, constructing deep boreholes and ground-water monitoring wells, laboratory testing of soil and rock strength and hydraulic properties, and ground-water and slope-stability modeling.\r\n","language":"ENGLISH","doi":"10.3133/ofr20061343","usgsCitation":"Schulz, W.H., Coe, J.A., Ellis, W., and Kibler, J.D., 2006, Preliminary Assessment of Landslides Along the Florida River Downstream from Lemon Reservoir, La Plata County, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2006-1343, v, 29 p.; 1 plate, map with cross sections; GIS data, https://doi.org/10.3133/ofr20061343.","productDescription":"v, 29 p.; 1 plate, map with cross sections; GIS data","numberOfPages":"34","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":193313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9095,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1343/","linkFileType":{"id":5,"text":"html"}}],"scale":"2770","projection":"Lambert Conformal Conic projection","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e791","contributors":{"authors":[{"text":"Schulz, William H.","contributorId":91927,"corporation":false,"usgs":true,"family":"Schulz","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":290182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coe, Jeffrey A. 0000-0002-0842-9608 jcoe@usgs.gov","orcid":"https://orcid.org/0000-0002-0842-9608","contributorId":1333,"corporation":false,"usgs":true,"family":"Coe","given":"Jeffrey","email":"jcoe@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":290179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellis, William L.","contributorId":89128,"corporation":false,"usgs":true,"family":"Ellis","given":"William L.","affiliations":[],"preferred":false,"id":290181,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kibler, John D.","contributorId":14523,"corporation":false,"usgs":true,"family":"Kibler","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":290180,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79537,"text":"ofr20061319 - 2006 - Flood of April 2-3, 2005, Neversink River Basin, New York","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061319","displayToPublicDate":"2007-01-05T00:00:00","publicationYear":"2006","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":"2006-1319","title":"Flood of April 2-3, 2005, Neversink River Basin, New York","docAbstract":"Heavy rain on April 2-3, 2005 produced rainfall amounts of 3 inches to almost 6 inches within a 36-hour period throughout the Delaware River basin. Major flooding occurred in the East and West Branches of the Delaware River and their tributaries, the main stem of the Delaware River and the Neversink River, a major tributary to the Delaware River. The resultant flooding damaged hundreds of homes, caused millions of dollars in damage to infrastructure in Orange and Sullivan Counties, and forced more than 1,000 residents to evacuate their homes. A total of 20 New York counties were declared Federal disaster areas. Some of the most extensive flooding occurred along the Neversink and Delaware Rivers in Orange and Sullivan Counties, New York. Disaster recovery assistance from the April 2005 flooding in New York stood at almost $35 million in 2005, at which time more than 3,400 New Yorkers had registered for Federal aid. All U.S. Geological Survey stream-gaging stations on the Neversink River below the Neversink Reservoir recorded peak water-surface elevations higher than those recorded during the September 2004 flooding. Peak water-surface elevations at some study sites on the Neversink River exceeded the 500-year flood elevation as documented in flood-insurance studies by the Federal Emergency Management Agency. Flood peaks at some long-term U.S. Geological Survey stream-gaging stations were the highest ever recorded. Several U.S. Geological Survey stream-gaging stations on the Delaware River also recorded peak water-surface elevations that exceeded those recorded during the September 2004 flooding.","language":"ENGLISH","doi":"10.3133/ofr20061319","collaboration":"Prepared in cooperation with the Federal Emergency Management Agency","usgsCitation":"Suro, T.P., and Firda, G.D., 2006, Flood of April 2-3, 2005, Neversink River Basin, New York: U.S. Geological Survey Open-File Report 2006-1319, v, 98 p., https://doi.org/10.3133/ofr20061319.","productDescription":"v, 98 p.","numberOfPages":"103","temporalStart":"2005-04-02","temporalEnd":"2005-04-03","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":194464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9088,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1319/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b6e4b07f02db534025","contributors":{"authors":[{"text":"Suro, Thomas P. 0000-0002-9476-6829 tsuro@usgs.gov","orcid":"https://orcid.org/0000-0002-9476-6829","contributorId":2841,"corporation":false,"usgs":true,"family":"Suro","given":"Thomas","email":"tsuro@usgs.gov","middleInitial":"P.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Firda, Gary D. gfirda@usgs.gov","contributorId":1552,"corporation":false,"usgs":true,"family":"Firda","given":"Gary","email":"gfirda@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":290172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79538,"text":"ofr20061375 - 2006 - Mineral Facilities of Latin America and Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:22","indexId":"ofr20061375","displayToPublicDate":"2007-01-05T00:00:00","publicationYear":"2006","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":"2006-1375","title":"Mineral Facilities of Latin America and Canada","docAbstract":"This data set consists of records for over 900 mineral facilities in Latin America and Canada. The mineral facilities include mines, plants, smelters, or refineries of aluminum, cement, coal, copper, diamond, gold, iron and steel, nickel, platinum-group metals, salt, and silver, among others. Records include attributes such as commodity, country, location, company name, facility type and capacity if applicable, and generalized coordinates. The data were compiled from multiple sources, including the 2003 and 2004 USGS Minerals Yearbooks (Latin America and Candada volume), data to be published in the 2005 Minerals Yearbook Latin America and Canada Volume, minerals statistics and information from the USGS minerals information Web site (minerals.usgs.gov/minerals), and data collected by USGS minerals information country specialists. Data reflect the most recent published table of industry structure for each country. Other sources include statistical publications of individual countries, annual reports and press releases of operating companies,and trade journals. Due to the sensitivity of some energy commodity data, the quality of these data should be evaluated on a country-by-country basis. Additional information and explanation is available from the country specialists.","language":"ENGLISH","doi":"10.3133/ofr20061375","usgsCitation":"Bernstein, R., Eros, M., and Quintana-Velazquez, M., 2006, Mineral Facilities of Latin America and Canada: U.S. Geological Survey Open-File Report 2006-1375, map, 42 by 60 inches; data set, https://doi.org/10.3133/ofr20061375.","productDescription":"map, 42 by 60 inches; data set","onlineOnly":"Y","temporalStart":"2003-01-01","temporalEnd":"2005-12-31","costCenters":[],"links":[{"id":194618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9244,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1375/","linkFileType":{"id":5,"text":"html"}}],"scale":"6000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63578c","contributors":{"authors":[{"text":"Bernstein, Rachel","contributorId":45580,"corporation":false,"usgs":true,"family":"Bernstein","given":"Rachel","email":"","affiliations":[],"preferred":false,"id":290176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eros, Mike","contributorId":39243,"corporation":false,"usgs":true,"family":"Eros","given":"Mike","email":"","affiliations":[],"preferred":false,"id":290175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Quintana-Velazquez, Meliany","contributorId":9526,"corporation":false,"usgs":true,"family":"Quintana-Velazquez","given":"Meliany","email":"","affiliations":[],"preferred":false,"id":290174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79530,"text":"ofr20061393 - 2006 - A Reconnaissance for Emerging Contaminants in the South Branch Potomac River, Cacapon River, and Williams River Basins, West Virginia, April-October 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"ofr20061393","displayToPublicDate":"2007-01-04T00:00:00","publicationYear":"2006","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":"2006-1393","title":"A Reconnaissance for Emerging Contaminants in the South Branch Potomac River, Cacapon River, and Williams River Basins, West Virginia, April-October 2004","docAbstract":"In 2003 a team of scientists from West Virginia Division of Natural Resources and the U. S. Geological Survey found a high incidence of an intersex condition, oocytes in the testes, among smallmouth bass (Micropterus dolomieu) in the South Branch Potomac River and the Cacapon River of West Virginia, indicating the possible presence of endocrine-disrupting compounds (EDCs). Possible sources of EDCs include municipal and domestic wastewater, and agricultural and industrial activities. Several sampling strategies were used to identify emerging contaminants, including potential EDCs, and their possible sources in these river basins and at an out-of-basin reference site. Passive water-sampling devices, which accumulate in-stream organic chemical compounds, were deployed for 40-41 days at 8 sampling sites. Sampler extracts were analyzed for a broad range of polar and non-polar organic compounds including pesticides, flame retardants, pharmaceuticals, and personal-care products. Analysis of passive-sampler extracts found 4 compounds; hexachloro-benzene; pentachloroanisole; 2,2',4,4',5-penta-bromo-diphenyl ether (BDE 47); and 2,2',4,4',6-penta-bromo-diphenyl ether (BDE 99) to be present at every sampled site, including the reference site, and several sites had detectable quantities of other compounds. No detectable quantity of any antibiotics was found in any passive-sampler extract. Effluent samples were analyzed for 39 antibiotics as tracers of human and agricultural waste. Additionally, poultry-processing plant effluent was sampled for roxarsone, an organoarsenic compound used as a poultry-feed additive, and other arsenic species as tracers of poultry waste. Antibiotics were detected in municipal wastewater, aquaculture, and poultry-processing effluent, with the highest number of antibiotics and the greatest concentrations found in municipal effluent. Arsenate was the only arsenic species detected in the poultry-processing plant effluent, at a concentration of 1.0 ?g/L. Water samples were collected from 7 stream sites and analyzed for arsenic species, including roxarsone. Arsenate was detected in samples from 6 of the 7 stream samples, in concentrations ranging from 0.3 to 0.5 ?g/L. Additionally, the analysis of smallmouth bass blood plasma for potential EDCs indicated the presence of several compounds including some found in the passive sampler extracts, specifically BDE 47 and BDE 99. Data from this reconnaissance will help to focus efforts for further studies of the occurrence of emerging contaminants, EDCs, and intersex in smallmouth bass in these Potomac River tributaries.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061393","collaboration":"In cooperation with the West Virginia Department of Environmental Protection, Division of Water and Waste Management and the West Virginia Division of Natural Resources","usgsCitation":"Chambers, D., and Leiker, T.J., 2006, A Reconnaissance for Emerging Contaminants in the South Branch Potomac River, Cacapon River, and Williams River Basins, West Virginia, April-October 2004: U.S. Geological Survey Open-File Report 2006-1393, v, 23 p., https://doi.org/10.3133/ofr20061393.","productDescription":"v, 23 p.","numberOfPages":"28","onlineOnly":"Y","temporalStart":"2004-04-01","temporalEnd":"2004-10-31","costCenters":[{"id":642,"text":"West Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":194686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9084,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1393/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,37 ], [ -83,40 ], [ -80,40 ], [ -80,37 ], [ -83,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4965e4b0b290850ef1ff","contributors":{"authors":[{"text":"Chambers, Douglas B. 0000-0002-5275-5427 dbchambe@usgs.gov","orcid":"https://orcid.org/0000-0002-5275-5427","contributorId":2520,"corporation":false,"usgs":true,"family":"Chambers","given":"Douglas B.","email":"dbchambe@usgs.gov","affiliations":[{"id":642,"text":"West Virginia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leiker, Thomas J.","contributorId":47805,"corporation":false,"usgs":true,"family":"Leiker","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79523,"text":"ofr20051082 - 2006 - Ground-Water Levels in Huron County, Michigan, 2004-05","interactions":[{"subject":{"id":79523,"text":"ofr20051082 - 2006 - Ground-Water Levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082","publicationYear":"2006","noYear":false,"title":"Ground-Water Levels in Huron County, Michigan, 2004-05"},"predicate":"SUPERSEDED_BY","object":{"id":81295,"text":"ofr20051082B - 2006 - Ground-water levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082B","publicationYear":"2006","noYear":false,"chapter":"B","title":"Ground-water levels in Huron County, Michigan, 2004-05"},"id":1}],"supersededBy":{"id":81295,"text":"ofr20051082B - 2006 - Ground-water levels in Huron County, Michigan, 2004-05","indexId":"ofr20051082B","publicationYear":"2006","noYear":false,"title":"Ground-water levels in Huron County, Michigan, 2004-05"},"lastModifiedDate":"2017-02-06T13:28:27","indexId":"ofr20051082","displayToPublicDate":"2006-12-30T00:00:00","publicationYear":"2006","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":"2005-1082","title":"Ground-Water Levels in Huron County, Michigan, 2004-05","docAbstract":"<p class=\"body\">In 1990, the U.S. Geological Survey (USGS) completed a study of the hydrogeology of Huron County, Michigan (Sweat, 1991). In 1993, Huron County and the USGS entered into a continuing agreement to measure water levels at selected wells throughout Huron County. As part of the agreement, USGS has operated four continuous water-level recorders, installed from 1988 to 1991 on wells in Bingham, Fairhaven, Grant, and Lake Townships (fig. 1) and summarized the data collected in an annual or bi-annual report. The agreement was altered in 2003, and beginning January 1, 2004, only the wells in Fairhaven and Lake Townships retained continuous waterlevel recorders, while the wells in Grant and Bingham Townships reverted primarily to periodic or quarterly measurement status. USGS also has provided training for County or Huron Conservation District personnel to measure the water level, on a quarterly basis, in 25 wells. USGS personnel regularly accompany County or Huron Conservation District personnel to provide a quality assurance/quality control check of all measurements being made. Water-level data collected from the 25 periodically or quarterly-measured wells is summarized in an annual or bi-annual report. In 1998, the USGS also completed a temporal and spatial analysis of the monitoring well network in Huron County (Holtschlag and Sweat, 1998).</p><p class=\"body\">The altitude of Lake Huron and precipitation are good indicators of general climatic conditions and, therefore, provide an environmental context for ground-water levels in Huron County. Figure 2 shows the mean-monthly water-level altitude of Lake Huron, averaged from measurements made by the U.S. Army Corps of Engineers at sites near Essexville or Harbor Beach, or both (National Oceanic and Atmospheric Administration, 2003-05), and monthly precipitation measured in Bad Axe (National Oceanic and Atmospheric Administration, 2003-05). In March 2003, a new low-water level for the period from 1991 through 2005 was measured in Lake Huron. There was almost no net change in the water level of Lake Huron from January 2004 through December 2005. In 2004, annual precipitation measured in Port Hope was about 3.7 inches above normal, but precipitation measured in Bad Axe was about 1.4 inches below normal. About 14.5 inches of precipitation was measured in Bad Axe during the 2004 summer growing season (May through August), which is about the same as was measured in Port Hope during the same period. Provisional precipitation totals for 2005 were 30.7 inches for January through November in Port Hope, and about 31.7 inches for the year in Bad Axe. About 10.6 inches of precipitation was measured in Bad Axe during the 2005 summer growing season, which is about 0.2 inches more than was recorded at Port Hope during the same period.</p><p class=\"body\">Two wells equipped with continuous-data recorders are completed in the Saginaw and Marshall aquifers in Fairhaven and Lake Townships, respectively. From January 2004 through December 2005, the net rise in the water level in the Fairhaven Township well was 0.71 ft, and the net rise in the Lake Township well was 0.98 ft. The Fairhaven Township well is drilled adjacent to Saginaw Bay (Lake Huron), and, as previously noted, there was almost no net change in the water level in Saginaw Bay over the same period. Hydrographs showing water levels are presented for the two wells equipped with continuous-data recorders. Continuous-data recorders were discontinued in the Grant and Bingham Township wells at the end of 2003 due to budget constraints. The decision of which two wells to discontinue was based on an analysis of the intrinsic value to Huron County of data from each well. The Grant Township well was selected for periodic or quarterly measurement at that time because it is completed in the glacial aquifer, which is little used for drinking water purposes or absent in much of Huron County. The Bingham Township well, which is completed in the Marshall aquifer, was selected for periodic or quarterly measurement because water levels in the well are often perturbed as a result of pumpage from nearby production wells and do not reflect baseline conditions within the aquifer.</p><p class=\"body\">Twenty five wells were measured on a periodic or quarterly basis in 2004-05. These wells are completed in the glacial, Saginaw, and Marshall aquifers, and the Coldwater confining unit. Although each quarterly measurement only provides a “snapshot” water level (measured in feet below land surface), the data adequately define the generalized water-level trend in the aquifer near the well. Water levels in 15 quarterlymeasured wells had a net rise ranging from 0.20 to 1.31 ft for the period from January 2004 to December 2005, while water levels in 10 of the wells had a net decline ranging from 0.07 to 0.99 ft over the same period (fig. 3; table 1). Period-of-record (the time period when water levels have been measured by U.S. Geological Survey or their cooperators) minimum depths to water (high-water levels) were measured in March 2004 in two quarterly-measured wells completed in the Marshall aquifer in Lake and Hume Townships. Period-of-record maximum depths to water were measured in September 2005 in three wells completed in the Marshall aquifer near Bad Axe. Water levels in those three wells recovered about 3 to 5 ft between September and December 2005. No period-of-record minimum or maximum depths to water were measured for the period from January 2004 through December 2005 in wells completed in either the glacial and Saginaw aquifers, or the Coldwater confining unit. Hydrographs showing water levels measured in each well are presented for the 25 wells measured on a quarterly basis.</p><p class=\"body\">Water-level trends measured for the period from January 2004 through December 2005 in other wells in Lower Michigan have similarities to those measured in Huron County wells. Several external factors influence water-level trends including proximity to nearby production wells, amount and timing of precipitation events, evapotranspiration and type of prevalent ground cover, proximity of aquifer to the surface, and hydraulic characteristics of overlying geologic materials.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051082","collaboration":"Prepared in cooperation with Huron County, Michigan","usgsCitation":"Weaver, T.L., Crowley, S.L., and Blumer, S.P., 2006, Ground-Water Levels in Huron County, Michigan, 2004-05: U.S. Geological Survey Open-File Report 2005-1082, iv, 16 p., https://doi.org/10.3133/ofr20051082.","productDescription":"iv, 16 p.","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":382,"text":"Michigan Water Science 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County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"1259\",\"properties\":{\"name\":\"Huron\",\"state\":\"MI\"},\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-82.9219,44.0668],[-82.9138,44.0639],[-82.9081,44.0628],[-82.8963,44.0584],[-82.8914,44.0537],[-82.8877,44.0522],[-82.8753,44.0464],[-82.8626,44.0452],[-82.8482,44.0402],[-82.8419,44.0405],[-82.8262,44.0359],[-82.8179,44.0353],[-82.8161,44.0347],[-82.8136,44.0324],[-82.8118,44.0314],[-82.8068,44.0295],[-82.7967,44.0274],[-82.7919,44.0231],[-82.7888,44.0212],[-82.7877,44.018],[-82.7824,44.0101],[-82.7805,44.0091],[-82.7735,44.0103],[-82.7678,44.0097],[-82.7659,44.0087],[-82.7622,44.0068],[-82.7543,44.0011],[-82.7483,43.9945],[-82.7408,43.9916],[-82.7384,43.9893],[-82.7314,43.9776],[-82.726,43.9716],[-82.7233,43.9633],[-82.7222,43.9592],[-82.7192,43.9559],[-82.7089,43.9474],[-82.7073,43.9423],[-82.7005,43.9376],[-82.6979,43.9288],[-82.6936,43.926],[-82.6925,43.9218],[-82.6897,43.9154],[-82.6855,43.9112],[-82.686,43.9021],[-82.6843,43.8984],[-82.6755,43.8858],[-82.6659,43.8755],[-82.6561,43.8688],[-82.6549,43.8674],[-82.6546,43.8619],[-82.6482,43.8522],[-82.6458,43.8485],[-82.6453,43.8471],[-82.6453,43.8462],[-82.648,43.844],[-82.6481,43.8431],[-82.6469,43.8417],[-82.6438,43.8393],[-82.6358,43.8345],[-82.6356,43.8277],[-82.6338,43.8258],[-82.6302,43.8102],[-82.6248,43.8046],[-82.6259,43.7973],[-82.6247,43.7959],[-82.6232,43.7886],[-82.6166,43.7824],[-82.6143,43.7774],[-82.6171,43.7733],[-82.6176,43.7533],[-82.6108,43.7385],[-82.6099,43.7225],[-82.6072,43.7138],[-82.6099,43.6998],[-82.6072,43.6906],[-82.6403,43.6893],[-82.7601,43.6854],[-82.8794,43.6815],[-83.0005,43.6788],[-83.1184,43.675],[-83.2357,43.6725],[-83.3536,43.6686],[-83.4664,43.6657],[-83.4668,43.7409],[-83.4624,43.7417],[-83.4543,43.7529],[-83.4509,43.7569],[-83.4438,43.7609],[-83.4428,43.7672],[-83.4341,43.7793],[-83.432,43.7838],[-83.4222,43.7886],[-83.4188,43.7935],[-83.4161,43.798],[-83.4146,43.8039],[-83.41,43.8075],[-83.4118,43.8102],[-83.4117,43.8112],[-83.4104,43.812],[-83.4034,43.8119],[-83.4028,43.8123],[-83.3981,43.8177],[-83.3891,43.8339],[-83.3864,43.837],[-83.3901,43.8403],[-83.3897,43.8485],[-83.3903,43.8498],[-83.3883,43.8516],[-83.3825,43.8542],[-83.3652,43.8561],[-83.3594,43.8587],[-83.3494,43.8685],[-83.3421,43.8765],[-83.3284,43.8848],[-83.3301,43.8881],[-83.3273,43.8944],[-83.3264,43.8989],[-83.3314,43.9027],[-83.3445,43.9062],[-83.3686,43.9086],[-83.3824,43.9112],[-83.3907,43.9091],[-83.4027,43.9112],[-83.4018,43.9166],[-83.3747,43.9137],[-83.3326,43.9177],[-83.314,43.9209],[-83.301,43.9265],[-83.2938,43.9314],[-83.2853,43.9366],[-83.2832,43.9407],[-83.2754,43.9451],[-83.2783,43.9492],[-83.2783,43.9501],[-83.2756,43.9533],[-83.2714,43.9605],[-83.2642,43.979],[-83.2636,43.979],[-83.2443,43.9831],[-83.2366,43.9847],[-83.1939,43.9873],[-83.1793,43.986],[-83.1787,43.986],[-83.1722,43.9886],[-83.1478,43.9925],[-83.1264,44.002],[-83.1211,44.005],[-83.1172,44.0063],[-83.1039,44.006],[-83.0906,44.0052],[-83.0823,44.005],[-83.0709,44.0042],[-83.0671,44.0037],[-83.0554,44.0084],[-83.0548,44.0079],[-83.0427,44.0217],[-83.0418,44.0253],[-83.0396,44.0312],[-83.0341,44.0402],[-83.0307,44.0433],[-83.0305,44.0474],[-83.0299,44.0474],[-83.0159,44.0479],[-83.0101,44.0487],[-82.996,44.0506],[-82.9843,44.0548],[-82.9684,44.0681],[-82.9607,44.0692],[-82.9594,44.0687],[-82.9602,44.066],[-82.9596,44.0656],[-82.9507,44.0639],[-82.9411,44.0664],[-82.9275,44.0706],[-82.9256,44.0706],[-82.9237,44.0701],[-82.9231,44.0682],[-82.9219,44.0668]]],[[[-83.4078,43.8275],[-83.4099,43.8225],[-83.4159,43.8167],[-83.4303,43.8202],[-83.4361,43.8199],[-83.4425,43.8173],[-83.444,43.8119],[-83.4511,43.8102],[-83.4617,43.8132],[-83.4602,43.8187],[-83.4579,43.8282],[-83.4531,43.8349],[-83.4512,43.8367],[-83.4442,43.8361],[-83.4445,43.8306],[-83.4415,43.8255],[-83.4365,43.824],[-83.4388,43.8286],[-83.436,43.8345],[-83.4389,43.84],[-83.4402,43.841],[-83.4444,43.8452],[-83.4449,43.8488],[-83.448,43.8512],[-83.4496,43.8567],[-83.4476,43.8603],[-83.4444,43.8611],[-83.4335,43.8618],[-83.4295,43.8535],[-83.4327,43.8513],[-83.4386,43.8487],[-83.4268,43.8411],[-83.41,43.8344],[-83.4096,43.8302],[-83.4078,43.8275]]],[[[-83.4138,43.8773],[-83.4164,43.8764],[-83.4214,43.8779],[-83.4277,43.8785],[-83.4295,43.8808],[-83.4319,43.8827],[-83.4319,43.8841],[-83.4299,43.8858],[-83.4311,43.8877],[-83.4291,43.8886],[-83.4255,43.8848],[-83.4205,43.8824],[-83.4194,43.8801],[-83.4156,43.8782],[-83.4138,43.8773]]],[[[-83.4892,43.7656],[-83.4911,43.7647],[-83.4924,43.7656],[-83.4942,43.767],[-83.4954,43.768],[-83.496,43.7694],[-83.4959,43.7721],[-83.4913,43.7752],[-83.4895,43.7733],[-83.4883,43.7724],[-83.4871,43.771],[-83.4872,43.7687],[-83.4879,43.7669],[-83.4892,43.7656]]],[[[-83.4212,43.8123],[-83.418,43.8113],[-83.4174,43.8117],[-83.4175,43.8095],[-83.4189,43.8068],[-83.4215,43.805],[-83.4228,43.805],[-83.4246,43.806],[-83.4252,43.8065],[-83.4239,43.8087],[-83.4238,43.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T. L.","contributorId":24339,"corporation":false,"usgs":true,"family":"Weaver","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":290140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crowley, S. L.","contributorId":77614,"corporation":false,"usgs":true,"family":"Crowley","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":290141,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":290139,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79519,"text":"ofr20051306 - 2006 - Continuous resistivity profiling data from the upper Neuse River Estuary, North Carolina, 2004-2005","interactions":[],"lastModifiedDate":"2022-10-04T19:16:44.746441","indexId":"ofr20051306","displayToPublicDate":"2006-12-29T00:00:00","publicationYear":"2006","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":"2005-1306","title":"Continuous resistivity profiling data from the upper Neuse River Estuary, North Carolina, 2004-2005","docAbstract":"<p>The Neuse River Estuary in North Carolina has suffered impacts of eutrophication in recent years. As part of a larger project to better constrain nutrient budgets in the estuary, field investigations were performed to study occurrence and discharge of fresh and brackish ground water and nutrients beneath the estuary itself (fig. 1). A Continuous Resistivity Profiling (CRP) system (Manheim and others, 2004) was used to map the depth of the freshwater-saltwater interface (FSI) in sub-estuarine groundwater. This study area serves as a typological representation of a submarine groundwater environment characteristic of a shallow estuary in a wide coastal plain that has not experienced glaciation. Similar settings extend from New Jersey to Georgia, and along the Gulf of Mexico in the U.S. This report archives 29 lines of data collected during 2004 and 2005 surveys representing almost 210 km of survey lines. These data are further explained in the Data Processing section of the report and previews available of the processed data are available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051306","usgsCitation":"Cross, V.A., Bratton, J.F., Bergeron, E., Meunier, J.K., Crusius, J., and Koopmans, D., 2006, Continuous resistivity profiling data from the upper Neuse River Estuary, North Carolina, 2004-2005: U.S. Geological Survey Open-File Report 2005-1306, HTML Document, https://doi.org/10.3133/ofr20051306.","productDescription":"HTML Document","temporalStart":"2004-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":194681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20051306.png"},{"id":9074,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1306/","linkFileType":{"id":5,"text":"html"}},{"id":407874,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78801.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Neuse River","geographicExtents":"{\"crs\": {\"type\": \"name\", \"properties\": {\"name\": \"urn:ogc:def:crs:OGC:1.3:CRS84\"}}, \"geometry\": {\"type\": \"MultiPolygon\", \"coordinates\": [[[[-76.71133973195622, 34.97024152121188], [-76.72913164154619, 34.96317708652167], [-76.73173819350723, 34.968024358589496], [-76.71216270936696, 34.97394491956021], [-76.71133973195622, 34.97024152121188]]], [[[-76.97428101469212, 35.05871159286782], [-76.95740997777172, 35.05665414934099], [-76.93848149732429, 35.078051562020555], [-76.93477809897585, 35.063649457332374], [-76.94547680531564, 35.04842437523347], [-76.93354363285975, 35.03525673666142], [-76.90473942348343, 35.02908440608075], [-76.87552372540159, 35.00604103857967], [-76.86235608682955, 35.001514662820455], [-76.81009702124669, 34.967772588979514], [-76.80968553254127, 34.962834724515], [-76.76874955978852, 34.95338796157209], [-76.76958719585565, 34.94853848960479], [-76.81091999865747, 34.95789686005046], [-76.81174297606822, 34.94226028924629], [-76.85001142566826, 34.93485349254944], [-76.8631790642403, 34.944317732773136], [-76.8928062510275, 34.9480211311215], [-76.90103602513501, 34.959954303577305], [-76.93477809897585, 34.97229896473873], [-76.97757292433515, 35.0019261515258], [-76.98786014196946, 35.03690269148291], [-77.02736305768576, 35.08710431353892], [-77.0294205012126, 35.10438683916482], [-77.0360043204987, 35.11179363586147], [-77.03312389956103, 35.123315319612054], [-77.02900901250727, 35.12578425184437], [-76.98786014196946, 35.06899881050236], [-76.97428101469212, 35.05871159286782]]]]}, \"properties\": {\"extentType\": \"Custom\", \"code\": \"\", \"name\": \"\", \"notes\": \"\", \"promotedForReuse\": false, \"abbreviation\": \"\", \"shortName\": \"\", \"description\": \"\"}, \"bbox\": [-77.0360043204987, 34.93485349254944, -76.71133973195622, 35.12578425184437], \"type\": \"Feature\", \"id\": \"3091875\"}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691994","contributors":{"authors":[{"text":"Cross, VeeAnn A.","contributorId":103311,"corporation":false,"usgs":true,"family":"Cross","given":"VeeAnn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":290128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bratton, John F. 0000-0003-0376-4981 jbratton@usgs.gov","orcid":"https://orcid.org/0000-0003-0376-4981","contributorId":92757,"corporation":false,"usgs":true,"family":"Bratton","given":"John","email":"jbratton@usgs.gov","middleInitial":"F.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290127,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergeron, Emile M. ebergeron@usgs.gov","contributorId":3449,"corporation":false,"usgs":true,"family":"Bergeron","given":"Emile M.","email":"ebergeron@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":290124,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meunier, Jeff K.","contributorId":29753,"corporation":false,"usgs":true,"family":"Meunier","given":"Jeff","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":290125,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crusius, John 0000-0003-2554-0831 jcrusius@usgs.gov","orcid":"https://orcid.org/0000-0003-2554-0831","contributorId":2155,"corporation":false,"usgs":true,"family":"Crusius","given":"John","email":"jcrusius@usgs.gov","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":290123,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Koopmans, Dirk","contributorId":33647,"corporation":false,"usgs":true,"family":"Koopmans","given":"Dirk","email":"","affiliations":[],"preferred":false,"id":290126,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79518,"text":"ofr20061266 - 2006 - Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana","interactions":[],"lastModifiedDate":"2020-01-27T06:39:38","indexId":"ofr20061266","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1266","title":"Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana","docAbstract":"Water, bed sediment, and biota were sampled in streams from Butte to below Missoula as part of a long-term monitoring program, conducted in cooperation with the U.S. Environmental Protection Agency, to characterize aquatic resources in the upper Clark Fork basin of western Montana. Sampling sites were located on the Clark Fork, six major tributaries, and three smaller tributaries. Water-quality samples were collected periodically at 18 sites during October 2004 through September 2005 (water year 2005). Bed-sediment and biological samples were collected once in August 2005. The primary constituents analyzed were trace elements associated with tailings from historical mining and smelting activities. This report summarizes the results of water-quality, bed-sediment, and biota samples col-lected in water year 2005 and provides statistical summaries of data collected since 1985.\r\n\r\nWater-quality data for samples collected periodically from streams include concentrations of selected major ions, trace ele-ments, and suspended sediment. Daily values of suspended-sed-iment concentration and suspended-sediment discharge were determined for three sites. Bed-sediment data include trace-ele-ment concentrations in the fine-grained fraction. Bio-logical data include trace-element concentrations in whole-body tissue of aquatic benthic insects. Quality-assurance data are reported for analytical results of water, \r\nbed sediment, and biota. Statistical summaries of water-quality, bed-sediment, and biological data are provided for the period of record since 1985 for each site.\r\n\r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061266","usgsCitation":"Dodge, K.A., Hornberger, M.I., and Dyke, J., 2006, Water-quality, bed-sediment, and biological data (October 2004 through September 2005) and statistical summaries of data for streams in the Upper Clark Fork Basin, Montana: U.S. Geological Survey Open-File Report 2006-1266, v, 109 p., https://doi.org/10.3133/ofr20061266.","productDescription":"v, 109 p.","numberOfPages":"114","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":400,"text":"Montana Water Science Center","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":195393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9073,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1266/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","otherGeospatial":"Upper Clark Fork 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jldyke@usgs.gov","contributorId":1035,"corporation":false,"usgs":true,"family":"Dyke","given":"Jessica","email":"jldyke@usgs.gov","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":290120,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79515,"text":"ofr20061367 - 2006 - The Unified Lunar Control Network 2005","interactions":[],"lastModifiedDate":"2018-12-07T16:32:47","indexId":"ofr20061367","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1367","title":"The Unified Lunar Control Network 2005","docAbstract":"<p><span>This report documents a new general unified lunar control network and lunar topographic model based on a combination of Clementine images and a previous network derived from Earth-based &amp; Apollo photographs, and Mariner 10, &amp; Galileo images. This photogrammetric network solution is the largest planetary control network ever completed. It includes the determination of the 3-D positions of 272,931 points on the lunar surface and the correction of the camera angles for 43,866 Clementine images, using 546,126 tie point measurements. The solution RMS is 20 μm (= 0.9 pixels) in the image plane, with the largest residual of 6.4 pixels. The explanation given here, along with the accompanying files, comprises the release of the network information and of global lunar digital elevation models (DEMs) derived from the network. A paper that will describe the solution and network in further detail will be submitted to a refereed journal, and will include additional background information, solution details, discussion of accuracy and precision, and explanatory figures.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061367","usgsCitation":"Archinal, B.A., Rosiek, M.R., Kirk, R.L., and Redding, B.L., 2006, The Unified Lunar Control Network 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1367, iii, 18 p.; data files, https://doi.org/10.3133/ofr20061367.","productDescription":"iii, 18 p.; data files","additionalOnlineFiles":"Y","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":192581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6725af","contributors":{"authors":[{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":290115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosiek, Mark R. mrosiek@usgs.gov","contributorId":824,"corporation":false,"usgs":true,"family":"Rosiek","given":"Mark","email":"mrosiek@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":290113,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":290114,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Redding, Bonnie L. 0000-0001-8178-1467 bredding@usgs.gov","orcid":"https://orcid.org/0000-0001-8178-1467","contributorId":4798,"corporation":false,"usgs":true,"family":"Redding","given":"Bonnie","email":"bredding@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":290116,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79512,"text":"ofr20061312 - 2006 - Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061312","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1312","title":"Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05","docAbstract":"Micrometeorological and soil-moisture data were collected at two instrumented sites on Rainier Mesa at the Nevada Test Site, January 1, 2002 - August 23, 2005. Data collected at each site include net radiation, air temperature, and relative humidity at two heights; wind speed and direction; subsurface soil heat flux; subsurface soil temperature; volumetric soil water; and matric water potential. These data were used to estimate 20-minute average and daily average evapotranspiration values. The data presented in this report are collected and calculated evapotranspiration rates.","language":"ENGLISH","doi":"10.3133/ofr20061312","collaboration":"Prepared in cooperation with the Nevada Operation Office of the U.S. Department of Energy, under Interagency Agreement DE-AI52-01NV13944","usgsCitation":"DeMeo, G.A., Flint, A.L., Laczniak, R.J., and Nylund, W.E., 2006, Micrometeorological and Soil Data for Calculating Evapotranspiration for Rainier Mesa, Nevada Test Site, Nevada, 2002-05: U.S. Geological Survey Open-File Report 2006-1312, iv, 12 p., https://doi.org/10.3133/ofr20061312.","productDescription":"iv, 12 p.","numberOfPages":"16","temporalStart":"2002-01-01","temporalEnd":"2005-08-23","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":194429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9066,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1312/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a034","contributors":{"authors":[{"text":"DeMeo, Guy A. gademeo@usgs.gov","contributorId":2124,"corporation":false,"usgs":true,"family":"DeMeo","given":"Guy","email":"gademeo@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":290101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":290100,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laczniak, Randell J.","contributorId":90687,"corporation":false,"usgs":true,"family":"Laczniak","given":"Randell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290103,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nylund, Walter E.","contributorId":12913,"corporation":false,"usgs":true,"family":"Nylund","given":"Walter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290102,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79513,"text":"ofr20061377 - 2006 - Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California","interactions":[],"lastModifiedDate":"2014-10-09T14:15:40","indexId":"ofr20061377","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1377","title":"Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California","docAbstract":"<p>In February 1993, the U.S. Geological Survey (USGS) acquired high-resolution seismic-reflection data to map the distribution and thickness of fine-grained sediments associated with acid-mine drainage in Keswick Reservoir on the Sacramento River, near Redding, California. In the Spring Creek Arm of Keswick Reservoir, the sediments occurred in three distinct accumulations; thicknesses are greater than 2 meters (m) in the western accumulation, greater than 5 m in the central accumulation, and up to 8 m in the eastern accumulation. In Keswick Reservoir, fine-grained sediments related to acid-mine drainage were present from slightly north of the Spring Creek Arm downstream to the Keswick Dam. Sediment thickness varies from about 3 m opposite the mouth of the Spring Creek Arm to less than 1 m near Keswick Dam.</p>\n<br>\n<p>Our estimate for the total volume of fine-grained sediments in the Spring Creek Arm at the time of the geophysical survey in February 1993 is about 152,000 cubic meters in three sediment accumulations, with about 14,000, 32,000, and 105,000 cubic meters respectively in the western, central, and eastern accumulations. We interpreted that an additional 110, 000 cubic meters of material was present in the main part of Keswick Reservoir. At the time of data collection, we therefore estimate that the total volume of fine-grained sediment was 260,000 cubic meters. In the main part of Keswick Reservoir, 42% to 50% of the reservoir area contiguous to Spring Creek Arm had mappable fine-grained sediments. Decreasing sediment supply down-reservoir meant that mappable sediment covered only about 35% of the reservoir in the area to the south, decreasing to about 12% near Keswick Dam. Much of the reservoir bottom below the Spring Creek Arm could have had a thin (less than 20-30 cm) cover of fine-grained sediment that was not mappable using the seismic-reflection data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20061377","usgsCitation":"Bruns, T.R., Alpers, C.N., and Carlson, P., 2006, Distribution, thickness, and volume of fine-grained sediment from precipitation of metals from acid-mine waters in Keswick Reservoir, Shasta County, California: U.S. Geological Survey Open-File Report 2006-1377, HTML Document, https://doi.org/10.3133/ofr20061377.","productDescription":"HTML Document","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":192524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20061377.PNG"},{"id":9067,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1377/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Shasta County","otherGeospatial":"Keswick Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634a01","contributors":{"authors":[{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlson, Paul","contributorId":52234,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","affiliations":[],"preferred":false,"id":290106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79506,"text":"ofr20061350 - 2006 - Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004","interactions":[],"lastModifiedDate":"2022-06-17T13:30:02.369889","indexId":"ofr20061350","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1350","title":"Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004","docAbstract":"<p class=\"indent\">Twenty-eight composite and replicate sediment samples from 8 Lake Roosevelt sites were collected and analyzed for 10 alkali and alkaline earth elements, 2 non-metals, 20 metals, and 4 lanthanide and actinide elements. All elements were detected in all sediment samples except for silver (95&nbsp;percent of the elements detected for 1,008 analyses), which was detected only in 4 samples. Sequential selective extraction procedures were performed on single composite samples from the eight sites. The percentage of detections for the 31 elements analyzed ranged from 76 percent for the first extraction fraction using a weak extractant to 93 percent for the four-acid dissolution of the sediments remaining after the third sequential selective extraction.</p><p class=\"indent\">Water samples in various degrees of contact with the sediment were analyzed for 10 alkali and alkaline earth elements, 5 non-metals, 25 metals, and 16 lanthanide and actinide elements. The filtered water samples included 10 samples from the reservoir water column at 8 sites, 32 samples of porewater, 55 samples from reservoir water overlying sediments in 8 cores from the site incubated in a field laboratory, and 24 water samples that were filtered after being tumbled with sediments from 8 sites. Overall, the concentrations of only 37 percent of the 6,776 analyses of the 121 water samples were greater than the reporting limit. Selenium, bismuth, chromium, niobium, silver, and zirconium were not detected in any water samples. The percentage of concentrations for the water samples that were above the reporting limit ranged from 14 percent for the lanthanide and actinide elements to 77 percent for the alkali and alkaline earth elements. Concentrations were greater than reporting limits in only 23 percent of the analyses of reservoir water and 29 percent of the analyses of reservoir water overlying incubation cores. In contrast, 47 and 48 percent of the concentrations of porewater and water samples tumbled with sediments, respectively, were greater than the reporting limit.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061350","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Paulson, A.J., Wagner, R.J., Sanzolone, R.F., and Cox, S.E., 2006, Concentrations of elements in sediments and selective fractions of sediments, and in natural waters in contact with sediments from Lake Roosevelt, Washington, September 2004: U.S. Geological Survey Open-File Report 2006-1350, vi, 84 p., https://doi.org/10.3133/ofr20061350.","productDescription":"vi, 84 p.","numberOfPages":"90","temporalStart":"2004-09-01","temporalEnd":"2004-09-30","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":195519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1350/","linkFileType":{"id":5,"text":"html"}},{"id":402307,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78794.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Lake Roosevelt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.4271240234375,\n              47.84634433782511\n            ],\n            [\n              -117.960205078125,\n              47.84634433782511\n            ],\n            [\n              -117.960205078125,\n              48.777912755501845\n            ],\n            [\n              -118.4271240234375,\n              48.777912755501845\n            ],\n            [\n              -118.4271240234375,\n              47.84634433782511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8563","contributors":{"authors":[{"text":"Paulson, Anthony J. 0000-0002-2358-8834 apaulson@usgs.gov","orcid":"https://orcid.org/0000-0002-2358-8834","contributorId":5236,"corporation":false,"usgs":true,"family":"Paulson","given":"Anthony","email":"apaulson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":290086,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Richard J. rjwagner@usgs.gov","contributorId":3122,"corporation":false,"usgs":true,"family":"Wagner","given":"Richard","email":"rjwagner@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sanzolone, Richard F.","contributorId":88007,"corporation":false,"usgs":true,"family":"Sanzolone","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":290088,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cox, Steven E.","contributorId":24875,"corporation":false,"usgs":true,"family":"Cox","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290087,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79504,"text":"ofr20061374 - 2006 - Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:22","indexId":"ofr20061374","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1374","title":"Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005","docAbstract":"Previous investigations have shown that natural attenuation and biodegradation of chlorinated volatile organic compounds (VOCs) are substantial in shallow ground water beneath the 9-acre former landfill at Operable Unit 1 (OU-1), Naval Undersea Warfare Center, Division Keyport, Washington. The U.S. Geological Survey (USGS) has continued to monitor ground-water geochemistry to assure that conditions remain favorable for contaminant biodegradation. This report presents the ground-water geochemical and selected VOC data collected at OU-1 by the USGS during June 21-24, 2005, in support of long-term monitoring for natural attenuation.\r\n\r\nFor June 2005, the strongly reducing conditions (sulfate reduction and methanogenesis) most favorable for reductive dechlorination of chlorinated VOCs were detected in fewer upper-aquifer wells than were detected during 2004. Redox conditions in ground water from the intermediate aquifer just downgradient of the landfill remained somewhat favorable for reductive dechlorination. Overall, the changes in redox conditions observed at individual wells have not been consistent or substantial throughout either the upper or the intermediate aquifers.\r\n\r\nIn apparent contrast to changes in redox conditions, the chlorinated VOC concentrations were lower than previously measured in many of the piezometers in the northern phytoremediation plantation. The decrease in contaminant concentrations beneath the northern plantation and the end-product (ethane and ethene) evidence for reductive dechlorination are consistent with 2000-04 results.\r\n\r\nIn the southern phytoremediation plantation, changes in chlorinated VOC concentrations were variable. Most notable was a substantial decrease in the sum of trichloroethene, cis-1,2-dichloroethene, and vinyl chloride concentrations at piezometer P1-9 from 75,000 to 1,000 micrograms per liter between 2004 and 2005. The high concentrations of the reductive dechlorination end-products ethane and ethene measured at the most contaminated sites (P1-6 and P1-7), as well as measurable concentrations at sites P1-9 and P1-10, are reliable evidence that reductive dechlorination of chlorinated VOCs is ongoing in the southern plantation.\r\n\r\nIn the 10 passive-diffusion samplers deployed beneath the marsh stream, the highest chlorinated VOC concentrations measured were at a site (S-4) about midway along the sampled stream reach. In 2005, the sum of trichloroethene, cis-1,2-dichloroethene, and vinyl chloride concentrations increased nearly twofold in comparison to 2004. It is not certain that the apparent increase in concentrations is representative of site conditions. However, the chlorinated VOC concentrations have increased each time at the two most contaminated passive-diffusion sampler sites that have been sampled for multiple years. In the marsh stream, chlorinated VOC concentrations in surface water were low at the site (SW-S6) near the upgradient margin of the former landfill. Concentrations in the stream increased substantially after flowing past the southern phytoremediation plantation to the downstream site (MA-12).\r\n\r\nOverall, the 2005 data were consistent with previous findings of continued biodegradation of chlorinated VOCs in ground water, along with continued discharge of some chlorinated VOCs to surface water in the marsh stream.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061374","collaboration":"Prepared in cooperation with Department of the Navy, Naval Facilities Engineering Command, Northwest","usgsCitation":"Dinicola, R., and Huffman, R., 2006, Selected Natural Attenuation Monitoring Data, Operable Unit 1, Naval Undersea Warfare Center, Division Keyport, Washington, June 2005: U.S. Geological Survey Open-File Report 2006-1374, iv, 28 p.; 2 figs.; 3 tables, https://doi.org/10.3133/ofr20061374.","productDescription":"iv, 28 p.; 2 figs.; 3 tables","numberOfPages":"32","temporalStart":"2005-06-21","temporalEnd":"2005-06-24","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":190718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9061,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1374/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7dd","contributors":{"authors":[{"text":"Dinicola, Richard S. 0000-0003-4222-294X dinicola@usgs.gov","orcid":"https://orcid.org/0000-0003-4222-294X","contributorId":352,"corporation":false,"usgs":true,"family":"Dinicola","given":"Richard S.","email":"dinicola@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, R.L.","contributorId":44956,"corporation":false,"usgs":true,"family":"Huffman","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":290081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79514,"text":"ofr20061373 - 2006 - High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego","interactions":[],"lastModifiedDate":"2023-03-24T20:01:10.221922","indexId":"ofr20061373","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1373","title":"High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego","docAbstract":"High-resolution boomer data were collected in the California Continental Borderland as part of the southern California Earthquake Hazards Task of the Southern California Coastal and Marine Geology Regional Investigations Project. During the period from 1997 to 2002, five data-acquisition cruises collected seismic-reflection data using several different systems from offshore Santa Barbara, California, south to the Exclusive Economic Zone boundary with Mexico. A key mission of this project was to map late Quaternary deformation in addition to improving our understanding of which offshore fault zones might have potential to damage highly populated areas of southern California. State regulations concerning the use of seismic-reflection equipment within three miles of the coastline precluded the routine gathering of high-resolution multichannel data in that swath adjacent to the coast. Boomer seismic-reflection data, however, can be obtained within the state 3-mile limit provided the operation receives authorization from the California State Lands Commission. \r\n\r\nThe Geopulse boomer data accessible through this report were collected on the cruise A-1-00-SC, which was the only survey where we requested permission to work inside the 3-mile limit of the State of California. These data are critical to discovering connections between onshore and offshore faults, the overall lengths of which are related to the potential size of an earthquake that might be generated along them. The 2000 survey was designed to fill the gap between onshore data and reflection data obtained in deeper water on previous cruises as well as data anticipated from future surveys. This report includes trackline maps showing the location of the data, as well as both digital data files (SEG-Y) and images of all of the profiles.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061373","usgsCitation":"Gutmacher, C.E., Ross, S.L., Triezenberg, P., Sliter, R.W., Normark, W.R., and Edwards, B.D., 2006, High-resolution boomer seismic-reflection profiles of the shelf off southern California from cruise A-1-00-SC: Santa Monica Bay to San Diego (Version 1.0): U.S. Geological Survey Open-File Report 2006-1373, HTML Document, https://doi.org/10.3133/ofr20061373.","productDescription":"HTML Document","additionalOnlineFiles":"Y","temporalStart":"2000-06-05","temporalEnd":"2000-06-29","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":192424,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414730,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78843.htm","linkFileType":{"id":5,"text":"html"}},{"id":9068,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1373/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"San Diego","otherGeospatial":"Santa Monica Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.1208,\n              32.5828\n            ],\n            [\n              -117.1208,\n              34.0328\n            ],\n            [\n              -118.8056,\n              34.0328\n            ],\n            [\n              -118.8056,\n              32.5828\n            ],\n            [\n              -117.1208,\n              32.5828\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fa08","contributors":{"authors":[{"text":"Gutmacher, Christina E.","contributorId":28272,"corporation":false,"usgs":true,"family":"Gutmacher","given":"Christina","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":290107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Triezenberg, Peter J.","contributorId":32625,"corporation":false,"usgs":true,"family":"Triezenberg","given":"Peter J.","affiliations":[],"preferred":false,"id":290111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sliter, Ray W. 0000-0003-0337-3454 rsliter@usgs.gov","orcid":"https://orcid.org/0000-0003-0337-3454","contributorId":1992,"corporation":false,"usgs":true,"family":"Sliter","given":"Ray","email":"rsliter@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":290108,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Normark, William R.","contributorId":69570,"corporation":false,"usgs":true,"family":"Normark","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290112,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"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":290109,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79505,"text":"ofr20061305 - 2006 - Genetic Considerations for the Restoration of Smooth Cordgrass (Spartina alterniflora) Within Its Native Range","interactions":[],"lastModifiedDate":"2012-02-02T00:14:08","indexId":"ofr20061305","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1305","title":"Genetic Considerations for the Restoration of Smooth Cordgrass (Spartina alterniflora) Within Its Native Range","docAbstract":"In order to remain viable over many generations, plant populations require the ability to respond adaptively to a changing environment. Such adaptive potential is directly controlled by underlying genetic variation, which can be measured in terms of both heterozygosity at the individual level and clonal, or genotypic diversity at the population level. This report summarizes research relating to the importance of genetic diversity in the restoration of salt marsh smooth cordgrass, Spartina alterniflora, a dominant member of low elevation intertidal marshes throughout the northern Gulf of Mexico and Atlantic Coasts of North America. Recent research has indicated that S. alterniflora is a partially clonal species characterized by the recruitment of seedlings exclusively during the initial colonization phase of population establishment. A major consequence of this finding is that clonal diversity generally peaks rather early in the development of a restored marsh, depending on the rate of natural immigration and/or the clonal diversity of planting units, and then undergoes a steady decline over geological time spans because of stochastic mortality and intraspecific competition. Low levels of clonal diversity resulting from restricted immigration or clonally depauperate planting materials in turn places strict limits on opportunities for outcrossing in a species known to suffer from severe inbreeding depression. Low clonal diversity may further lead to declining levels of heterozyosity of individual clones, which directly affects competitive ability. In addition, the planting of genetically diverse plant materials should take into account the genetic and adaptive differentiation that takes place when plant populations are widely separated in space and/or dwell under varying sets of environmental conditions. Thus, steps should be taken to ensure that S. alterniflora clones developed for restorative plantings are both genetically diverse and sufficiently pre-adapted to environmental conditions at the proposed restoration site. This can be achieved by growing plant materials collected from local sources and by either taking care to maintain relatively high levels of clonal diversity or by planting clones at sufficiently low densities that they will not quickly grow to monopolize a restoration site without first producing several generations of sexual recruits through crosses with nearby native populations.","language":"ENGLISH","doi":"10.3133/ofr20061305","usgsCitation":"Travis, S.E., Proffitt, C.E., and Edwards, K.R., 2006, Genetic Considerations for the Restoration of Smooth Cordgrass (Spartina alterniflora) Within Its Native Range (Version 1.0): U.S. Geological Survey Open-File Report 2006-1305, iv, 11 p., https://doi.org/10.3133/ofr20061305.","productDescription":"iv, 11 p.","numberOfPages":"15","costCenters":[],"links":[{"id":192506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9062,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1305/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebb8","contributors":{"authors":[{"text":"Travis, Steven E.","contributorId":64724,"corporation":false,"usgs":true,"family":"Travis","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":290083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Proffitt, C. Edward 0000-0002-0845-8441","orcid":"https://orcid.org/0000-0002-0845-8441","contributorId":93568,"corporation":false,"usgs":true,"family":"Proffitt","given":"C.","email":"","middleInitial":"Edward","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":290084,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Keith R.","contributorId":29906,"corporation":false,"usgs":true,"family":"Edwards","given":"Keith","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":290082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":79516,"text":"ofr20061157 - 2006 - Alaska resource data file, Noatak quadrangle","interactions":[],"lastModifiedDate":"2025-05-21T18:04:08.026616","indexId":"ofr20061157","displayToPublicDate":"2006-12-28T00:00:00","publicationYear":"2006","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":"2006-1157","title":"Alaska resource data file, Noatak quadrangle","docAbstract":"<p>This report gives descriptions of the mineral occurrences in the Noatak 1:250,000-scale quadrangle, Alaska. The data presented here are maintained as part of a statewide database on mines, prospects and mineral occurrences throughout Alaska.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061157","usgsCitation":"Grybeck, D.J., and Dumoulin, J.A., 2006, Alaska resource data file, Noatak quadrangle (Version 1.0): U.S. Geological Survey Open-File Report 2006-1157, 19 p., https://doi.org/10.3133/ofr20061157.","productDescription":"19 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":484076,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78840.htm","linkFileType":{"id":5,"text":"html"}},{"id":484077,"rank":4,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}},{"id":9070,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1157/","linkFileType":{"id":5,"text":"html"}},{"id":194616,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":486308,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2006/1157/of2006-1157.pdf","text":"Report","size":"156 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2006-1157 PDF"}],"country":"United States","state":"Alaska","otherGeospatial":"Noatak quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -165.25,\n              68\n            ],\n            [\n              -165.25,\n              67\n            ],\n            [\n              -162,\n              67\n            ],\n            [\n              -162,\n              68\n            ],\n            [\n              -165.25,\n              68\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f3b","contributors":{"authors":[{"text":"Grybeck, Donald J.","contributorId":20013,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":290117,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":79502,"text":"ofr20061347 - 2006 - Preliminary geologic map of the Black Mountain area northeast of Victorville, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:43","indexId":"ofr20061347","displayToPublicDate":"2006-12-23T00:00:00","publicationYear":"2006","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":"2006-1347","title":"Preliminary geologic map of the Black Mountain area northeast of Victorville, San Bernardino County, California","docAbstract":"The Black Mountain area is in the Mojave Desert about 20 km northeast of Victorville, California.  The geology of this area is of interest primarily for its excellent exposures of the early Mesozoic Fairview Valley Formation, a sequence of weakly metamorphosed sedimentary rocks including a thick, commercially important unit of limestone conglomerate that has been mined for cement at Black Mountain Quarry for several decades.  Recent geochronologic work has shown that the Fairview Valley Formation is probably of Early Jurassic age.  This preliminary geologic map of the Black Mountain area depicts the stratigraphic and structural relations of the Fairview Valley Formation and the associated rocks, most notably the overlying Sidewinder Volcanics of Early(?), Middle, and Late(?) Jurassic age.  The map is based on new field studies by the author designed to clarify details of the stratigraphy and structure unresolved by previous investigations.  The map is considered preliminary because the ages of some geologic units critical for a satisfactory understanding of the stratigraphic and structural framework remain unknown.\r\n\r\nThe map area also includes a segment of the Helendale Fault, one of several faults of known or inferred late Cenozoic right-lateral displacement that make up the Eastern California Shear Zone.  The fault is marked by aligned northeast-facing scarps in Pleistocene or older alluvial deposits and the underlying bedrock units.  Relations in the map area suggest that right-lateral displacement on the Helendale Fault probably does not exceed 2 km, a conclusion compatible with previous estimates of displacement on this fault based on relations both within and outside the Black Mountain area.\r\n","language":"ENGLISH","doi":"10.3133/ofr20061347","usgsCitation":"Stone, P., 2006, Preliminary geologic map of the Black Mountain area northeast of Victorville, San Bernardino County, California (Version 1.0 ): U.S. Geological Survey Open-File Report 2006-1347, map, 34 by 34 inches; data files, https://doi.org/10.3133/ofr20061347.","productDescription":"map, 34 by 34 inches; data files","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110692,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78792.htm","linkFileType":{"id":5,"text":"html"},"description":"78792"},{"id":9059,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1347/","linkFileType":{"id":5,"text":"html"}},{"id":194642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0 ","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bcda","contributors":{"authors":[{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":290075,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":79503,"text":"ofr20061285 - 2006 - Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"ofr20061285","displayToPublicDate":"2006-12-23T00:00:00","publicationYear":"2006","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":"2006-1285","title":"Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004","docAbstract":"The U.S. Geological Survey, in support of the U.S. Department of Energy, Office of Repository Development, collects, compiles, and summarizes hydrologic data in the Yucca Mountain region of southern Nevada and eastern California. These data are 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 on ground-water levels at 35 boreholes and 1 fissure (Devils Hole), ground-water discharge at 5 springs, both 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 are tabulated from January through December 2004. Also tabulated are ground-water levels, discharges, and withdrawals collected by other agencies (or collected as part of other programs) and data revised from those previously published at monitoring sites. Historical data on water levels, discharges, and withdrawals are presented graphically to indicate variations through time.\r\n\r\nA statistical summary of ground-water levels at seven boreholes in Jackass Flats is presented for the period 1992-2004 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 six boreholes in Jackass Flats, median water levels for 2004 were slightly higher (0.3-2.7 feet) than their median water levels for 1992-93. At one borehole in Jackass Flats, median water level for 2004 equaled the median water level for 1992-93.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061285","usgsCitation":"La Camera, R.J., Locke, G.L., Habte, A.M., and Darnell, J.G., 2006, Selected Ground-Water Data for Yucca Mountain Region, Southern Nevada and Eastern California, January-December 2004: U.S. Geological Survey Open-File Report 2006-1285, vi, 71 p., https://doi.org/10.3133/ofr20061285.","productDescription":"vi, 71 p.","numberOfPages":"77","temporalStart":"2004-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":194867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9060,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1285/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa7e9","contributors":{"authors":[{"text":"La Camera, Richard J.","contributorId":52212,"corporation":false,"usgs":true,"family":"La Camera","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":290076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Habte, Aron M.","contributorId":108206,"corporation":false,"usgs":true,"family":"Habte","given":"Aron","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":290079,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Darnell, Jon G.","contributorId":47042,"corporation":false,"usgs":true,"family":"Darnell","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":290077,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":79501,"text":"ofr20061311 - 2006 - Water-Surface Elevations, Discharge, and Water-Quality Data for Selected Sites in the Warm Springs Area near Moapa, Nevada","interactions":[],"lastModifiedDate":"2012-03-08T17:16:22","indexId":"ofr20061311","displayToPublicDate":"2006-12-22T00:00:00","publicationYear":"2006","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":"2006-1311","title":"Water-Surface Elevations, Discharge, and Water-Quality Data for Selected Sites in the Warm Springs Area near Moapa, Nevada","docAbstract":"The U.S. Geological Survey, in cooperation with Southern Nevada Water Authority and the Nevada Division of Water Resources, operates and maintains a surface-water monitoring network of 6 continuous-record stream-flow gaging stations and 11 partial-record stations in the Warm Springs area near Moapa, Nevada. Permanent land-surface bench marks were installed within the Warm Springs area by the Las Vegas Valley Water District, the Southern Nevada Water Authority, and the U.S. Geological Survey to determine water-surface elevations at all network monitoring sites. Vertical datum elevation and horizontal coordinates were established for all bench marks through a series of Differential Global Positioning System surveys. Optical theodolite surveys were made to transfer Differential Global Positioning System vertical datums to reference marks installed at each monitoring site. The surveys were completed in June 2004 and water-surface elevations were measured on August 17, 2004. Water-surface elevations ranged from 1,810.33 feet above North American Vertical Datum of 1988 at a stream-gaging station in the Pederson Springs area to 1,706.31 feet at a station on the Muddy River near Moapa.\r\n\r\nDischarge and water-quality data were compiled for the Warm Springs area and include data provided by the U.S. Geological Survey, Nevada Division of Water Resources, U.S. Fish and Wildlife Service, Moapa Valley Water District, Desert Research Institute, and Converse Consultants. Historical and current hydrologic data-collection networks primarily are related to changes in land- and water-use activities in the Warm Springs area. These changes include declines in ranching and agricultural use, the exportation of water to other areas of Moapa Valley, and the creation of a national wildlife refuge. Water-surface elevations, discharge, and water-quality data compiled for the Warm Springs area will help identify (1) effects of changing vegetation within the former agricultural lands, (2) effects of restoration activities in the wildlife refuge, and (3) potential impacts of ground-water withdrawals.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr20061311","collaboration":"Prepared in cooperation with the Southern Nevada Water Authority","usgsCitation":"Beck, D.A., Ryan, R., Veley, R.J., Harper, D.P., and Tanko, D.J., 2006, Water-Surface Elevations, Discharge, and Water-Quality Data for Selected Sites in the Warm Springs Area near Moapa, Nevada: U.S. Geological Survey Open-File Report 2006-1311, vi, 230 p. plus appendices, https://doi.org/10.3133/ofr20061311.","productDescription":"vi, 230 p. plus appendices","numberOfPages":"235","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":190688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9058,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1311/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5456e0","contributors":{"authors":[{"text":"Beck, David A.","contributorId":102874,"corporation":false,"usgs":true,"family":"Beck","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":290074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, Roslyn","contributorId":51366,"corporation":false,"usgs":true,"family":"Ryan","given":"Roslyn","email":"","affiliations":[],"preferred":false,"id":290071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Veley, Ronald J. rjveley@usgs.gov","contributorId":4013,"corporation":false,"usgs":true,"family":"Veley","given":"Ronald","email":"rjveley@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":290070,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harper, Donald P.","contributorId":90394,"corporation":false,"usgs":true,"family":"Harper","given":"Donald","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":290073,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tanko, Daron J.","contributorId":88343,"corporation":false,"usgs":true,"family":"Tanko","given":"Daron","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290072,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":79496,"text":"ofr20061362 - 2006 - Mineralogy and Morphology of Amphiboles Observed in Soils and Rocks in El Dorado Hills, California","interactions":[],"lastModifiedDate":"2012-02-02T00:14:10","indexId":"ofr20061362","displayToPublicDate":"2006-12-20T00:00:00","publicationYear":"2006","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":"2006-1362","title":"Mineralogy and Morphology of Amphiboles Observed in Soils and Rocks in El Dorado Hills, California","docAbstract":"From the Executive Summary: At the request of the U.S. Environmental Protection Agency (USEPA), the U.S. Geological Survey (USGS) has conducted an independent study of amphiboles in rocks and soils in the El Dorado Hills, California, area. The purpose of this study is to investigate specific issues regarding the presence of 'naturally occurring asbestos' raised by an USEPA activity-based sampling study and subsequent criticisms of that study outlined in a review prepared by The R.J. Lee Group (RJLG).","language":"ENGLISH","doi":"10.3133/ofr20061362","collaboration":"Prepared for U.S. Environmental Protection Agency Region 9 IAG DW1492190501-2","usgsCitation":"Meeker, G., Lowers, H., Swayze, G., Van Gosen, B.S., Sutley, S.J., and Brownfield, I.K., 2006, Mineralogy and Morphology of Amphiboles Observed in Soils and Rocks in El Dorado Hills, California: U.S. Geological Survey Open-File Report 2006-1362, vii, 47 p.; 4 appendices, https://doi.org/10.3133/ofr20061362.","productDescription":"vii, 47 p.; 4 appendices","numberOfPages":"54","costCenters":[],"links":[{"id":192015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9054,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1362/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e79","contributors":{"authors":[{"text":"Meeker, G.P.","contributorId":34539,"corporation":false,"usgs":true,"family":"Meeker","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":290059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lowers, H.A. 0000-0001-5360-9264","orcid":"https://orcid.org/0000-0001-5360-9264","contributorId":31843,"corporation":false,"usgs":true,"family":"Lowers","given":"H.A.","affiliations":[],"preferred":false,"id":290058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swayze, G.A. 0000-0002-1814-7823","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":21570,"corporation":false,"usgs":true,"family":"Swayze","given":"G.A.","affiliations":[],"preferred":false,"id":290057,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Van Gosen, B. S. 0000-0003-4214-3811","orcid":"https://orcid.org/0000-0003-4214-3811","contributorId":97907,"corporation":false,"usgs":true,"family":"Van Gosen","given":"B.","middleInitial":"S.","affiliations":[],"preferred":false,"id":290062,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":290061,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brownfield, I. K.","contributorId":77915,"corporation":false,"usgs":true,"family":"Brownfield","given":"I.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":290060,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":79497,"text":"ofr20061382 - 2006 - Use of DNA markers for investigating sources of bacteria in contaminated ground water: Wooster Township, Wayne County, Ohio","interactions":[],"lastModifiedDate":"2022-06-30T21:40:57.195412","indexId":"ofr20061382","displayToPublicDate":"2006-12-20T00:00:00","publicationYear":"2006","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":"2006-1382","title":"Use of DNA markers for investigating sources of bacteria in contaminated ground water: Wooster Township, Wayne County, Ohio","docAbstract":"In 2004, a public-health nuisance was declared by the Wayne County Board of Health in the Scenic Heights Drive-Batdorf Road area of Wooster Township, Wayne County, Ohio, because of concerns about the safety of water from local wells. Repeated sampling had detected the presence of fecal-indicator bacteria and elevated nitrate concentrations. In June 2006, the U.S. Geological Survey (USGS), in cooperation with the Ohio Environmental Protection Agency (Ohio EPA), collected and analyzed samples from some of the affected wells to help investigate the possibility of human-origin bacterial contamination. Water samples from 12 wells and 5 home sewage-treatment systems (HSTS) were collected. Bromide concentrations were determined in samples from the 12 wells. Samples from 5 of the 12 wells were analyzed for wastewater compounds. Total coliform, enterococci and Escherichia coli (E. coli) bacteria concentrations were determined for samples from 8 of the 12 wells. In addition, two microbial source-tracking tools that employ DNA markers were used on samples from several wells and a composite sample of water from five septic tanks. The DNA markers from the Enterococcus faecium species and the order Bacteroidales are associated with specific sources, either human or ruminant sources.\r\n\r\nBromide concentrations ranged from 0.04 to 0.18 milligrams per liter (mg/L). No wastewater compounds were detected at concentrations above the reporting limits. Samples from the 12 wells also were collected by Ohio EPA and analyzed for chloride and nitrate. Chloride concentrations ranged from 12.6 to 61.6 mg/L and nitrate concentrations ranged from 2.34 to 11.9 mg/L (as N).\r\n\r\nTotal coliforms and enterococci were detected in samples from 8 wells, at concentrations from 2 to 200 colony-forming units per 100 milliliters (CFU/100 mL) and 0.5 to 17 CFU/100 mL, respectively. E. coli were detected in samples from three of the eight wells, at concentrations of 1 or 2 CFU/100 mL. Tests for the human-specific marker of enterococci, the esp gene, were negative in the seven samples tested, including the composite sample of HSTS water. DNA with the general Bacteroidales marker was detected in samples from four wells, but the tests for both the human- and ruminant-associated markers were negative. The presence of the PCR (polymerase chain reaction) -detectable DNA for the general fecal Bacteroidales marker is indicative of fecal contamination and recently recharged water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061382","collaboration":"Prepared in cooperation with the Ohio Environmental Protection Agency","usgsCitation":"Dumouchelle, D.H., 2006, Use of DNA markers for investigating sources of bacteria in contaminated ground water: Wooster Township, Wayne County, Ohio: U.S. Geological Survey Open-File Report 2006-1382, iv, 13 p., https://doi.org/10.3133/ofr20061382.","productDescription":"iv, 13 p.","numberOfPages":"17","onlineOnly":"Y","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":402798,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78786.htm","linkFileType":{"id":5,"text":"html"}},{"id":192042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9051,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1382/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","county":"Wayne County","otherGeospatial":"Wooster Township","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.9697,\n              40.7478\n            ],\n            [\n              -81.9633,\n              40.7478\n            ],\n            [\n              -81.9633,\n              40.7561\n            ],\n            [\n              -81.9697,\n              40.7561\n            ],\n            [\n              -81.9697,\n              40.7478\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6051e4","contributors":{"authors":[{"text":"Dumouchelle, Denise H. ddumouch@usgs.gov","contributorId":1847,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"Denise","email":"ddumouch@usgs.gov","middleInitial":"H.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":290063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}