{"pageNumber":"2938","pageRowStart":"73425","pageSize":"25","recordCount":184563,"records":[{"id":50536,"text":"ofr02396 - 2002 - Cruise report RV Moana Wave Cruise M-1-02-GM bathymetry and acoustic backscatter of the mid and outer continental shelf, head of De Soto Canyon, northeastern Gulf of Mexico June 17, through July 9, 2002 Pensacola, FL to Pensacola, FL","interactions":[],"lastModifiedDate":"2021-09-21T18:25:42.01172","indexId":"ofr02396","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-396","title":"Cruise report RV Moana Wave Cruise M-1-02-GM bathymetry and acoustic backscatter of the mid and outer continental shelf, head of De Soto Canyon, northeastern Gulf of Mexico June 17, through July 9, 2002 Pensacola, FL to Pensacola, FL","docAbstract":"The mid to outer continental shelf off Mississippi-Alabama and off northwest Florida were the focus of US Geological Survey (USGS) multibeam echosounder (MBES) mapping cruises in 2000 and 2001, respectively. These areas were mapped to investigate the extent of \"deep-water reefs\" first suggested by Ludwick and Walton (1957). The reefs off Mississippi and Alabama were initially described in water depths of 60 to 120 m (Ludwick and Walton, 1957) but the 2000 mapping found reef and hardgrounds to be much more extensive than previously thought (Gardner et al., 2001). The persistent trend of reef-like features along the outer shelf of Mississippi-Alabama suggested the trend might continue along the northwest Florida mid and outer shelf so a MBES-mapping effort was mounted in 2001 to test this suggestion. It is critical to determine the accurate location, geomorphology, and types of the ridges and reefs that occur in this region to understand the Quaternary history of the area and to assess their importance as benthic habitats for fisheries. The 2001 survey found a series of shelf-depth platforms with ridges (possibly reefs) constructed on their surfaces (Gardner et al., 2002).\n\nThe area known as the \"head of De Soto Canyon\" is the large unmapped region between the 2000 and 2001 mapped areas. The head of De Soto Canyon is an outer shelf zone with a relatively steep western wall and a much gentler eastern wall. It was unknown prior to this cruise whether the reefs of the Mississippi-Alabama shelf continue eastward into the head of De Soto Canyon and connect with the ridges and reefs mapped on the northwest Florida outer shelf. The existence of carbonate-cemented latest Quaternary to Holocene sandstones along the western wall of the head of De Soto Canyon (Shipp and Hopkins, 1978; Benson et al., 1997; W.W. Schroeder, personnel comm., 2002) is of interest because of the potential benthic habitats they may represent. \n\nPrecisely georeferenced high-resolution mapping of bathymetry is a fundamental first step in the study of an area suspected to be critical benthic habitats. Morphology is thought to be critical to define the distribution of dominant demersal plankton/planktivores communities. Community structure and trophodynamics of demersal fishes of the outer continental shelf of the northeastern Gulf of Mexico presently are focuses of a major USGS research project. A goal of the project is to answer questions concerning the relative roles played by morphology and surficial geology in controlling biological differentiation. Deep-water ridges, reefs, and outcrops are important because they are fish havens and key spawning sites, and are critical habitats for larval, juvenile, and economically important sport/food fishes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02396","usgsCitation":"Gardner, J.V., Hughes Clarke, J.E., and Meyer, L.A., 2002, Cruise report RV Moana Wave Cruise M-1-02-GM bathymetry and acoustic backscatter of the mid and outer continental shelf, head of De Soto Canyon, northeastern Gulf of Mexico June 17, through July 9, 2002 Pensacola, FL to Pensacola, FL: U.S. Geological Survey Open-File Report 2002-396, HTML Document, https://doi.org/10.3133/ofr02396.","productDescription":"HTML Document","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":389557,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52492.htm"},{"id":283871,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0396/intro.html"},{"id":178428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02396.jpg"},{"id":4348,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0396/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Gulf of Mexico, head Of De Soto Canyon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.333333,23.716667 ], [ -92.333333,31.25 ], [ -79.683333,31.25 ], [ -79.683333,23.716667 ], [ -92.333333,23.716667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ee4b07f02db63ff7c","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":241732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes Clarke, John E.","contributorId":58676,"corporation":false,"usgs":false,"family":"Hughes Clarke","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":241731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, Larry A.","contributorId":12555,"corporation":false,"usgs":true,"family":"Meyer","given":"Larry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241730,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50480,"text":"ofr0281 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, October 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0281","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-81","title":"Streamflow gain/loss in the Republican River basin, Nebraska, October 1975","docAbstract":"This arc and point data set contains streamflow-measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along Republican River tributaries in Dundy and Chase Counties, Nebraska during October 6 to 8, 1975 (U.S. Geological Survey, 1977). The streamflow measurements were made to obtain data on ground-water/surface-water interaction. Flow was observed visually to be zero, was measured, or was estimated at 64 sites. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site also were checked. \r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites.\r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate stream-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000 hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses of tributary streams to the Republican River in Dundy and Chase Counties, Nebraska, in October 1975, and make the data available for use with geographic information systems (GIS).\r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0281","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, October 1975: U.S. Geological Survey Open-File Report 2002-81, 2 refs, https://doi.org/10.3133/ofr0281.","productDescription":"2 refs","costCenters":[],"links":[{"id":179100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4289,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-081/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb6","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":241557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241556,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241558,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241555,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50485,"text":"ofr0287 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, March 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0287","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-87","title":"Streamflow gain/loss in the Republican River basin, Nebraska, March 1989","docAbstract":"This arc and point data set contains streamflow measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along the Republican River and tributaries in Nebraska during March 21 to 22, 1989 (Boohar and others, 1990). These measurements were made to obtain data on ground-water/surface-water interaction. Flow was visually observed to be zero, was measured, or was estimated at 136 sites. The measurements were made on the main stem of the Republican River and all flowing tributaries that enter the Republican River above Swanson Reservoir and parts of the Frenchman, Red Willow, and Medicine Creek drainages in the Nebraska part of the Republican River Basin. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site were also checked. \r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites. \r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate stream-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000 hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses of selected streams in part of the Republican River Basin, Nebraska in March 1989, and make the data available for use with geographic information systems (GIS). \r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0287","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, March 1989: U.S. Geological Survey Open-File Report 2002-87, 2 refs, https://doi.org/10.3133/ofr0287.","productDescription":"2 refs","costCenters":[],"links":[{"id":179674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4294,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-087/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4cf8","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241575,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50479,"text":"ofr0280 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, July 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0280","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-80","title":"Streamflow gain/loss in the Republican River basin, Nebraska, July 1975","docAbstract":"This arc and point data set contains streamflow-measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along Republican River tributaries in Dundy and Chase Counties, Nebraska during July 14 to 18, 1975 (U.S. Geological Survey, 1976). The streamflow measurements were made to obtain data on ground-water/surface-water interaction. Flow was observed visually to be zero, was measured, or was estimated at 55 sites. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site also were checked. \r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites. \r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate stream-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000 hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses of tributary streams to the Republican River in Dundy and Chase Counties, Nebraska, in July 1975, and make the data available for use with geographic information systems (GIS). \r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0280","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, July 1975: U.S. Geological Survey Open-File Report 2002-80, 2 refs, https://doi.org/10.3133/ofr0280.","productDescription":"2 refs","costCenters":[],"links":[{"id":179099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4288,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-080/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae213","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241554,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241551,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50746,"text":"wri024185 - 2002 - Flow-system analysis of the Madison and Minnelusa aquifers in the Rapid City area, South Dakota — Conceptual model","interactions":[],"lastModifiedDate":"2022-01-18T22:47:50.271307","indexId":"wri024185","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2002-4185","title":"Flow-system analysis of the Madison and Minnelusa aquifers in the Rapid City area, South Dakota — Conceptual model","docAbstract":"<p>The conceptual model of the Madison and Minnelusa aquifers in the Rapid City area synthesizes the physical geography, hydraulic properties, and ground-water flow components of these important aquifers. The Madison hydrogeologic unit includes the karstic Madison aquifer, which is defined as the upper, more permeable 100 to 200 ft of the Madison Limestone, and the Madison confining unit, which consists of the lower, less permeable part of the Madison Limestone and the Englewood Formation. Overlying the Madison hydrogeologic unit is the Minnelusa hydrogeologic unit, which includes the Minnelusa aquifer in the upper, more permeable 200 to 300 ft and the Minnelusa confining unit in the lower, less permeable part. The Madison and Minnelusa hydrogeologic units outcrop in the study area on the eastern flank of the Black Hills where recharge occurs from streamflow losses and areal recharge. The conceptual model describes streamflow recharge, areal recharge, ground-water flow, storage in aquifers and confining units, unsaturated areas, leakage between aquifers, discharge from artesian springs, and regional outflow.</p><p>Effective transmissivities estimated for the Madison aquifer range from 500 to 20,000 ft<span class=\"sup\">2</span>/d and for the Minnelusa aquifer from 500 to 10,000 ft<span class=\"sup\">2</span>/d. Localized anisotropic transmissivity in the Madison aquifer has tensor ratios as high as 45:1. Vertical hydraulic conductivities for the Minnelusa confining unit determined from aquifer tests range from 1.3x10<span class=\"sup\">-3</span><span>&nbsp;</span>to 3.0x10<span class=\"sup\">-1</span><span>&nbsp;</span>ft/d. The confined storage coefficient of the Madison and Minnelusa hydrogeologic units was estimated as 3x10<span class=\"sup\">-4</span><span>&nbsp;</span>ft/d. Specific yield was estimated as 0.09 for the Madison and Minnelusa aquifers and 0.03 for the Madison and Minnelusa confining units. Potentiometric surfaces for the Madison and Minnelusa aquifers have a general easterly gradient of about 70 ft/mi with local variations. Temporal change in hydraulic head in the Madison and Minnelusa aquifers ranged from about 5 to 95 ft in water years 1988-97. The unconfined areas were estimated at about 53 and 36 mi<span class=\"sup\">2</span><span>&nbsp;</span>for the Madison and Minnelusa hydrogeologic units, respectively, in contrast to an aquifer analysis area of 629 mi<span class=\"sup\">2</span>.</p><p>Dye-tracer tests, stable isotopes, and hydrogeologic features were analyzed conjunctively to estimate generalized ground-water flowpaths in the Madison aquifer and their influences on the Minnelusa aquifer. The western Rapid City area between Boxelder Creek and Spring Creek was characterized as having undergone extensive tectonic activity, greater brecciation in the Minnelusa Formation, large transmissivities, generally upward hydraulic gradients from the Madison aquifer to the Minnelusa aquifer, many karst springs, and converging flowpaths.</p><p>Water-budget analysis included: (1) a dry-period budget for declining water levels; October 1, 1987, to March 31, 1993; (2) a wet-period budget for rising water levels, April 1, 1993, to September 30, 1997; and (3) a full 10-year period budget for water years 1988-97. By simultaneously balancing these water budgets, initial estimates of recharge, discharge, change in storage, and hydraulic properties were refined. Inflow rates for the 10-year budget included streamflow recharge of about 45 ft<span class=\"sup\">3</span>/s or 61 percent of the total budget and areal recharge of 22 ft<span class=\"sup\">3</span>/s or 30 percent. Streamflow recharge to the Madison hydrogeologic unit was about 86 percent of the total streamflow recharge. Outflow for the 10-year budget included springflow of 31 ft<span class=\"sup\">3</span>/s or 42 percent of the total budget, water use of about 10 ft<span class=\"sup\">3</span>/s or 14 percent, and regional outflow of 22 ft<span class=\"sup\">3</span>/s or 30 percent. Ground-water storage increased 9 ft<span class=\"sup\">3</span>/s during the 10-year period, and net ground-water movement from the Madison to Minnelusa hydrogeologic unit was about 8 ft<span class=\"sup\">3</span>/s.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024185","usgsCitation":"Long, A.J., and Putnam, L.D., 2002, Flow-system analysis of the Madison and Minnelusa aquifers in the Rapid City area, South Dakota — Conceptual model: U.S. Geological Survey Water-Resources Investigations Report 2002-4185, vii, 100 p., https://doi.org/10.3133/wri024185.","productDescription":"vii, 100 p.","costCenters":[],"links":[{"id":175295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4237,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024185/","linkFileType":{"id":5,"text":"html"}},{"id":394486,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52784.htm"}],"country":"United States","state":"South Dakota","city":"Rapid City","otherGeospatial":"Madison and Minnelusa aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.5296630859375,\n              43.810747313446996\n            ],\n            [\n              -102.9144287109375,\n              43.810747313446996\n            ],\n            [\n              -102.9144287109375,\n              44.422011314236634\n            ],\n            [\n              -103.5296630859375,\n              44.422011314236634\n            ],\n            [\n              -103.5296630859375,\n              43.810747313446996\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489a6a","contributors":{"authors":[{"text":"Long, Andrew J. 0000-0001-7385-8081 ajlong@usgs.gov","orcid":"https://orcid.org/0000-0001-7385-8081","contributorId":989,"corporation":false,"usgs":true,"family":"Long","given":"Andrew","email":"ajlong@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Putnam, Larry D. ldputnam@usgs.gov","contributorId":990,"corporation":false,"usgs":true,"family":"Putnam","given":"Larry","email":"ldputnam@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":242219,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51125,"text":"ofr02204 - 2002 - Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity","interactions":[],"lastModifiedDate":"2025-04-18T15:33:42.888476","indexId":"ofr02204","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-0204","title":"Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02204","isbn":"0607990627","usgsCitation":"Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity; 2002; OFR; 2002-204; Smith, Thomas J., III; Foster, Ann M.; Briere, Peter R.; Jones, John W.; Van Arsdall, Carson","productDescription":"HTML Document: 1 CD-ROM","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4512,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0204/","linkFileType":{"id":5,"text":"html"}},{"id":179137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0204/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.09479583359331,\n              26.643885296477606\n            ],\n            [\n              -82.09479583359331,\n              24.327972112803963\n            ],\n            [\n              -80.11513304200784,\n              24.327972112803963\n            ],\n            [\n              -80.11513304200784,\n              26.643885296477606\n            ],\n            [\n              -82.09479583359331,\n              26.643885296477606\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"2002-11-01","noUsgsAuthors":false,"publicationDate":"2002-11-01","publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6865d5","contributors":{"authors":[{"text":"Smith, Thomas J. III tom_j_smith@usgs.gov","contributorId":1615,"corporation":false,"usgs":true,"family":"Smith","given":"Thomas","suffix":"III","email":"tom_j_smith@usgs.gov","middleInitial":"J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":242987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, Ann M. amfoster@usgs.gov","contributorId":3545,"corporation":false,"usgs":true,"family":"Foster","given":"Ann","email":"amfoster@usgs.gov","middleInitial":"M.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":242989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briere, Peter R.","contributorId":14789,"corporation":false,"usgs":true,"family":"Briere","given":"Peter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242990,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, John 0000-0001-6117-3691 jwjones@usgs.gov","orcid":"https://orcid.org/0000-0001-6117-3691","contributorId":2220,"corporation":false,"usgs":true,"family":"Jones","given":"John","email":"jwjones@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true}],"preferred":true,"id":242988,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Arsdall, Carson","contributorId":73271,"corporation":false,"usgs":true,"family":"Van Arsdall","given":"Carson","email":"","affiliations":[],"preferred":false,"id":242991,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50535,"text":"ofr02391 - 2002 - Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska","interactions":[],"lastModifiedDate":"2014-03-12T13:16:02","indexId":"ofr02391","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-391","title":"Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska","docAbstract":"Glacier Bay is a diverse fjord ecosystem with multiple tidewater glaciers and complex biological, geological, and oceanographic patterns that vary greatly along its length. The bay was completely glaciated prior to the 1700's, and subsequently experienced the fastest glacial retreat recorded in historical times. As a result, some of the highest rates of glacial sedimentation and uplift are observed here.\n\nGlacier Bay is the deepest silled fjord in Alaska, with depths of over 450 meters. The variety of physical processes and depths creates many diverse habitats within a relatively small area. Mapping benthic (seafloor) habitats is thus crucial to understanding and managing Glacier Bay's complex marine ecosystem and the marine species therein. High-resolution multibeam mapping of the bay, funded jointly by USGS and the National Park System, provides an unprecedented new baseline for resource and habitat assessment. Full integration of the new data set will require additional ground-truthing data (sampling) and analysis. The USGS goal is to develop integrated geological and oceanographic habitat models for the marine benthos in Glacier Bay, as a step toward determining the habitat relationships of critical species and resources within the Park.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02391","usgsCitation":"Carlson, P.R., Hooge, P., Cochrane, G., Stevenson, A., Dartnell, P., and Lee, K., 2002, Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska: U.S. Geological Survey Open-File Report 2002-391, HTML page, https://doi.org/10.3133/ofr02391.","productDescription":"HTML page","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":4347,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0391/","linkFileType":{"id":5,"text":"html"}},{"id":178427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02391.jpg"},{"id":283892,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0391/intro.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Glacier Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -137.0187,58.3049 ], [ -137.0187,59.0615 ], [ -135.3983,59.0615 ], [ -135.3983,58.3049 ], [ -137.0187,58.3049 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b485c","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hooge, Philip","contributorId":51644,"corporation":false,"usgs":true,"family":"Hooge","given":"Philip","affiliations":[],"preferred":false,"id":241725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cochrane, Guy","contributorId":104164,"corporation":false,"usgs":true,"family":"Cochrane","given":"Guy","affiliations":[],"preferred":false,"id":241729,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stevenson, Andrew","contributorId":102787,"corporation":false,"usgs":true,"family":"Stevenson","given":"Andrew","affiliations":[],"preferred":false,"id":241728,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dartnell, Pete","contributorId":33412,"corporation":false,"usgs":true,"family":"Dartnell","given":"Pete","email":"","affiliations":[],"preferred":false,"id":241724,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, Kristen","contributorId":78809,"corporation":false,"usgs":true,"family":"Lee","given":"Kristen","affiliations":[],"preferred":false,"id":241726,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":44708,"text":"wri994174 - 2002 - Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2020-02-16T11:36:52","indexId":"wri994174","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"99-4174","title":"Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts","docAbstract":"A numerical model was used to simulate pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts. Simulation results show that pond-bottom hydraulic conductivity, which represents the degree of hydraulic connection between the pond and the aquifer, is an important control on these interactions. As this parameter was incrementally increased from 10 to 350 feet per day, the rate of ground-water inflow into the pond under natural conditions increased by about 250 percent, the associated residence times of water in the pond decreased by about 50 percent, and ground-water inflow to the pond shifted closer to the pond shore. Most ground-water inflow (90 to 98 percent) was in the upper model layer, which corresponded to shallow, near-shore areas of the pond, over the entire range of pond-bottom hydraulic conductivity. Ground-water flow paths into the pond became more vertical, the contributing area to the pond became larger, and the pond captured water from greater depths in the aquifer as the hydraulic conductivity of the pond bottom was increased. The pond level, however, remained nearly constant, and regional ground-water levels and gradients differed little over the range of pond-bottom hydraulic conductivity, indicating that calibrated models with similar head solutions can have different pond-aquifer interaction characteristics.\r\n\r\n\r\nHydrologic stresses caused by a simulated plume-containment system that specifies the extraction and injection of large volumes of ground water near the pond increased the pond level by about 0.4 foot and ground-water inflow rates into the pond by about 25 percent. Several factors related to the operation of the simulated containment system are affected by the hydraulic conductivity of the pond bottom. With increasing pond-bottom hydraulic conductivity, the amount of injected water that flows into Snake Pond increased and the amount of water recirculated between extraction and injection wells decreased. Comparison of simulations in which pond-bottom hydraulic conductivity was varied throughout the pond and simulations in which hydraulic conductivity was varied only in areas corresponding to shallow, near-shore areas of the pond indicate that the simulated hydraulic conductivity of the pond bottom in deeper parts of the pond had little effect on pond-aquifer interactions under both natural and stressed conditions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri994174","usgsCitation":"Walter, D.A., Masterson, J., and LeBlanc, D.R., 2002, Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 99-4174, v, 35 p. , https://doi.org/10.3133/wri994174.","productDescription":"v, 35 p. ","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":172716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3750,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri994174/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.7080078125,\n              41.57436130598913\n            ],\n            [\n              -69.89501953125,\n              41.57436130598913\n            ],\n            [\n              -69.89501953125,\n              42.049292638686836\n            ],\n            [\n              -70.7080078125,\n              42.049292638686836\n            ],\n            [\n              -70.7080078125,\n              41.57436130598913\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f9af","contributors":{"authors":[{"text":"Walter, Donald A. 0000-0003-0879-4477 dawalter@usgs.gov","orcid":"https://orcid.org/0000-0003-0879-4477","contributorId":1101,"corporation":false,"usgs":true,"family":"Walter","given":"Donald","email":"dawalter@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":1865,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":230296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230295,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70161957,"text":"70161957 - 2002 - Modeling fish community dynamics in Florida Everglades: Role of temperature variation","interactions":[],"lastModifiedDate":"2016-01-11T11:22:23","indexId":"70161957","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3724,"text":"Water Science and Technology","active":true,"publicationSubtype":{"id":10}},"title":"Modeling fish community dynamics in Florida Everglades: Role of temperature variation","docAbstract":"<p id=\"p-1\">Temperature variation is an important factor in Everglade wetlands ecology. A temperature fluctuation from 17&deg;C to 32&deg;C recorded in the Everglades may have significant impact on fish dynamics. The short life cycles of some of Everglade fishes has rendered this temperature variation to have even more impacts on the ecosystem. Fish population dynamic models, which do not explicitly consider seasonal oscillations in temperature, may fail to describe the details of such a population. Hence, a model for fish in freshwater marshes of the Florida Everglades that explicitly incorporates seasonal temperature variations is developed. The model's main objective is to assess the temporal pattern of fish population and densities through time subject to temperature variations. Fish population is divided into 2 functional groups (FGs) consisting of small fishes; each group is subdivided into 5-day age classes during their life cycles. Many governing sub-modules are set directly or indirectly to be temperature dependent. Growth, fecundity, prey availability, consumption rates and mortality are examples. Several mortality sub-modules are introduced in the model, of which starvation mortality is set to be proportional to the ratio of prey needed to prey available at that particular time step. As part of the calibration process, the model is run for 50 years to ensure that fish densities do not go to extinction, while the simulation period is about 8 years.</p>\n<p id=\"p-2\">The model shows that the temperature dependent starvation mortality is an important factor that influences fish population densities. It also shows high fish population densities at some temperature ranges when this consumption need is minimum. Several sensitivity analyses involving variations in temperature terms, food resources and water levels are conducted to ascertain the relative importance of temperature dependence terms.</p>","language":"English","publisher":"IWA Publishing","usgsCitation":"Al-Rabai’ah, H.A., Koh, H.L., DeAngelis, D., and Lee, H., 2002, Modeling fish community dynamics in Florida Everglades: Role of temperature variation: Water Science and Technology, v. 46, no. 9, p. 71-78.","productDescription":"8 p.","startPage":"71","endPage":"78","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":314112,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314111,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wst.iwaponline.com/content/46/9/71"}],"volume":"46","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e049e4b039675d005e3b","contributors":{"authors":[{"text":"Al-Rabai’ah, H. A.","contributorId":152147,"corporation":false,"usgs":false,"family":"Al-Rabai’ah","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":588194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koh, H. L.","contributorId":44362,"corporation":false,"usgs":true,"family":"Koh","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":588195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeAngelis, Donald L. 0000-0002-1570-4057 don_deangelis@usgs.gov","orcid":"https://orcid.org/0000-0002-1570-4057","contributorId":147289,"corporation":false,"usgs":true,"family":"DeAngelis","given":"Donald L.","email":"don_deangelis@usgs.gov","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":588196,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, Hooi-Ling","contributorId":16618,"corporation":false,"usgs":true,"family":"Lee","given":"Hooi-Ling","email":"","affiliations":[],"preferred":false,"id":588197,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70180946,"text":"70180946 - 2002 - Depositional sequences and facies in the Torok Formation, National Petroleum Reserve, Alaska (NPRA)","interactions":[],"lastModifiedDate":"2017-02-09T11:24:38","indexId":"70180946","displayToPublicDate":"2002-10-31T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Depositional sequences and facies in the Torok Formation, National Petroleum Reserve, Alaska (NPRA)","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">Brookian turbidites (Cretaceous through Tertiary) have become oil exploration objectives on the <span class=\"searchword\">North</span><span class=\"searchword\">Slope</span> of <span class=\"searchword\">Alaska</span> during the past decade, and it is likely this focus will extend into the <span class=\"searchword\">National</span> <span class=\"searchword\">Petroleum</span> <span class=\"searchword\">Reserve</span>-<span class=\"searchword\">Alaska</span> (<span class=\"searchword\">NPRA</span>). A regional grid of 2-<span class=\"searchword\">D</span> seismic data, sparse well control, and field work in the Brooks Range foothills provide constraints for an ongoing effort to establish a sequence stratigraphic framework for Brookian turbidites in the <span class=\"searchword\">Torok</span> <span class=\"searchword\">Formation</span> across <span class=\"searchword\">NPRA</span>. The <span class=\"searchword\">Torok</span> <span class=\"searchword\">Formation</span> and overlying Nanushuk <span class=\"searchword\">Formation</span> (both mostly Albian) display the overall seismic geometry of bottomset-clinoform-topset strata indicating northeastward migration of a shelf margin. Within bottomset and clinoform strata of the <span class=\"searchword\">Torok</span>, <span class=\"searchword\">depositional</span> <span class=\"searchword\">sequences</span> have been identified that represent four distinct phases of shelf-margin sedimentation. (1) Regression, representing low relative sea level, is characterized by the development of an erosional surface on the shelf and upper <span class=\"searchword\">slope</span>, and the deposition of turbidite channel deposits on the middle to lower slope and submarine fan deposits at the base of slope. These deposits constitute a lowstand systems tract (LST). (2) Transgression, representing rising relative sea level, is characterized by the deposition of a mudstone drape on the basin floor, slope, and outer shelf. This drape comprises relatively condensed facies that constitute a transgressive systems tract (TST). (3) Aggradation, representing high relative sea level, is characterized by the deposition of relatively thick strata on the outer shelf and moderately thick mudstones on the slope. (4) Progradation, also representing high relative sea level, is characterized by the deposition of relatively thin strata on the outer shelf and very thick mudstones on the slope. Together, deposits of the aggradation and progradation phases constitute a highstand systems tract (HST). Large scale geometries of Torok strata vary across the Colville basin. In southern NPRA, high rates of subsidence accommodated the deposition of a \"foredeep clinoform wedge\" that contains a high proportion of sand-rich LST deposits. In northern NPRA, lower rates of subsidence favored the accumulation of mud-rich HST deposits. The most favorable stratigraphic trapping geometries in the Torok Formation occur where amalgamated sandstones deposited in turbidite channels incised on the mid- to lower-slope and on the proximal parts of submarine fans during regression (LSTs) are capped by relatively condensed mudstone facies deposited during transgression (TSTs). Common successions observed in Torok cores include a spectrum of slope and turbidite facies. Upper slope facies comprise laminated mudstones and siltstones that locally display evidence of slumping, sliding, and chaotic failure. Lower slope facies comprise heterolithic turbidites at some locations and interlaminated mudstones and thin, very fine-grained sandstones at others. Torok turbidites include amalgamated sandstones deposited in channel systems as well as thin-bedded, widespread sandstones deposited by unconfined flows on lobes or in channel overbank settings. These turbidite facies likely occur in both channel-lobe systems and slope apron systems within the Torok.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"SEPM core workshop","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"language":"English","publisher":"American Geosciences Institute ","issn":"0278-0720 ","usgsCitation":"Houseknecht, D.W., and Schenk, C.J., 2002, Depositional sequences and facies in the Torok Formation, National Petroleum Reserve, Alaska (NPRA), <i>in</i> SEPM core workshop, v. 21, p. 5-26.","productDescription":"12 p.","startPage":"5","endPage":"26","costCenters":[],"links":[{"id":335084,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"589d8dd7e4b0efcedb7ae5db","contributors":{"authors":[{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":662932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":662933,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206325,"text":"70206325 - 2002 - Overview of catastrophic landslides of South America in the twentieth century","interactions":[],"lastModifiedDate":"2019-10-31T06:56:10","indexId":"70206325","displayToPublicDate":"2002-10-30T13:31:08","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3853,"text":"Reviews in Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"Overview of catastrophic landslides of South America in the twentieth century","docAbstract":"<p><span>This chapter summarizes the processes and effects of the most notable catastrophic mass movement events in South America in the twentieth century. We present 23 case histories of individual and regional landslide events, beginning at the northeast terminus of the Andes Mountains in Venezuela, proceeding counterclockwise down the Pacific Coast to the southern Andes of Chile and Argentina, and ending with discussion of catastrophic regional mass movements in the Brazilian Highlands. The types of landslides involved in these disasters ranged from high-velocity rockslides and rock or debris avalanches to high-to medium-velocity debris flows and mudflows. Most casualties were caused by high-velocity debris avalanches and high-to medium-velocity, highly mobile, long-runout debris flows. A common, and particularly devastating, regional occurrence consisted of earthquake-triggered slides on steep slopes covered with saturated residual soils; these slides were rapidly transformed into very fluid, high-velocity debris avalanches, which in turn changed into devastating debris flows that ran out into populated areas on valley bottoms.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Catastrophic landslides: Effects, occurrence, and mechanisms","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/REG15-p1","isbn":"9780813758152","usgsCitation":"Schuster, R., Salcedo, D.A., and Valenzuela, L., 2002, Overview of catastrophic landslides of South America in the twentieth century: Reviews in Engineering Geology, v. 15, p. 1-34, https://doi.org/10.1130/REG15-p1.","productDescription":"35 p.","startPage":"1","endPage":"34","costCenters":[],"links":[{"id":368744,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"South America","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.3984375,\n              7.013667927566642\n            ],\n            [\n              -85.78125,\n              -3.688855143147035\n            ],\n            [\n              -79.453125,\n              -13.581920900545844\n            ],\n            [\n              -71.3671875,\n              -20.13847031245114\n            ],\n            [\n              -77.16796875,\n              -51.72702815704774\n            ],\n            [\n              -69.43359375,\n              -56.26776108757582\n            ],\n            [\n              -63.6328125,\n              -55.07836723201513\n            ],\n            [\n              -67.8515625,\n              -52.26815737376816\n            ],\n            [\n              -59.94140624999999,\n              -41.90227704096369\n            ],\n            [\n              -37.08984375,\n              -19.642587534013032\n            ],\n            [\n              -33.75,\n              -3.864254615721396\n            ],\n            [\n              -40.42968749999999,\n              -1.5818302639606454\n            ],\n            [\n              -48.33984375,\n              3.8642546157214084\n            ],\n            [\n              -58.88671875,\n              10.487811882056695\n            ],\n            [\n              -73.828125,\n              12.554563528593656\n            ],\n            [\n              -78.3984375,\n              7.013667927566642\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","noUsgsAuthors":false,"publicationDate":"2002-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Schuster, Robert","contributorId":44300,"corporation":false,"usgs":true,"family":"Schuster","given":"Robert","affiliations":[],"preferred":false,"id":774152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Salcedo, Daniel A.","contributorId":220114,"corporation":false,"usgs":false,"family":"Salcedo","given":"Daniel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":774153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Valenzuela, Luis","contributorId":220115,"corporation":false,"usgs":false,"family":"Valenzuela","given":"Luis","email":"","affiliations":[],"preferred":false,"id":774154,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70206322,"text":"70206322 - 2002 - Engineering history and impacts of the Bonneville landslide, Columbia River Gorge, Washington-Oregon, U.S.A","interactions":[],"lastModifiedDate":"2019-10-31T06:59:28","indexId":"70206322","displayToPublicDate":"2002-10-30T12:33:09","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Engineering history and impacts of the Bonneville landslide, Columbia River Gorge, Washington-Oregon, U.S.A","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Landslides: Proceedings of the first European conference on andslides","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"First European Conference on Landslides","conferenceDate":"June 24-26, 2002","conferenceLocation":"Prague, Czech Republic","language":"English","publisher":"A.A. Balkema","usgsCitation":"Schuster, R.L., and Pringle, P.T., 2002, Engineering history and impacts of the Bonneville landslide, Columbia River Gorge, Washington-Oregon, U.S.A, <i>in</i> Landslides: Proceedings of the first European conference on andslides, v. 1, Prague, Czech Republic, June 24-26, 2002, p. 689-699.","productDescription":"11 p.","startPage":"689","endPage":"699","costCenters":[],"links":[{"id":368739,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington, Oregon","otherGeospatial":"Columbia River Gorge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.31353759765624,\n              45.625563438215984\n            ],\n            [\n              -122.310791015625,\n              45.6178796835697\n            ],\n            [\n              -122.26959228515624,\n              45.4524242413431\n            ],\n            [\n              -121.68182373046875,\n              45.48324350868221\n            ],\n            [\n              -121.17919921875001,\n              45.506346901083425\n            ],\n            [\n              -120.728759765625,\n              45.56406391514301\n            ],\n            [\n              -120.7012939453125,\n              45.70234306798271\n            ],\n            [\n              -120.87432861328125,\n              45.74069339553309\n            ],\n            [\n              -121.29180908203125,\n              45.775186183521036\n            ],\n            [\n              -121.52252197265626,\n              45.78284835197676\n            ],\n            [\n              -122.31353759765624,\n              45.625563438215984\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schuster, R. L.","contributorId":19135,"corporation":false,"usgs":true,"family":"Schuster","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":774142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pringle, P. T.","contributorId":116886,"corporation":false,"usgs":true,"family":"Pringle","given":"P.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":774143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179972,"text":"70179972 - 2002 - Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon.  Annual report 2001","interactions":[],"lastModifiedDate":"2017-01-20T15:04:16","indexId":"70179972","displayToPublicDate":"2002-10-30T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon.  Annual report 2001","docAbstract":"<p>The Bureau of Reclamation (BOR) constructed Agency Valley Dam on the North Fork of the Malheur River in 1934-35, creating Beulah Reservoir. The project is operated and maintained by the Vale Irrigation District for irrigation and downstream flood control, with no minimum pool or outflow operational criteria. Although the project is not operated for fish and wildlife values, the reservoir supports a rainbow trout Oncorhynchus mykiss fishery and also seasonally harbors an adfluvial population of bull trout Salvelinus confluentus (Oregon Department of Fish and Wildlife [ODFW]; Burns Paiute Tribe). Bull trout were listed by the USFWS as a threatened species throughout the Columbia and Klamath river basins in 1998, and Oregon has listed the North Fork Malheur River population “Of Special Concern”. </p>","language":"English","publisher":"U.S. Bureau of Reclamation ","usgsCitation":"Petersen, J.H., and Kofoot, E.E., 2002, Conditions for growth and survival of bull trout in Beulah Reservoir, Oregon.  Annual report 2001, 43 p.","productDescription":"43 p.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333625,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Beulah Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.16104888916014,\n              43.94870940420277\n            ],\n            [\n              -118.17306518554688,\n              43.94141717295212\n            ],\n            [\n              -118.16946029663085,\n              43.92893178545033\n            ],\n            [\n              -118.16551208496092,\n              43.91384693067827\n            ],\n            [\n              -118.1624221801758,\n              43.90927125982932\n            ],\n            [\n              -118.15143585205078,\n              43.911002636116976\n            ],\n            [\n              -118.13959121704102,\n              43.92707729641145\n            ],\n            [\n              -118.13289642333984,\n              43.94104635763355\n            ],\n            [\n              -118.13581466674805,\n              43.94450721066432\n            ],\n            [\n              -118.14886093139648,\n              43.945001601793486\n            ],\n            [\n              -118.157958984375,\n              43.94772067950785\n            ],\n            [\n              -118.16104888916014,\n              43.94870940420277\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58833026e4b0d002316377c2","contributors":{"authors":[{"text":"Petersen, James H. petersen@usgs.gov","contributorId":23231,"corporation":false,"usgs":true,"family":"Petersen","given":"James","email":"petersen@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":false,"id":659367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kofoot, Eric E. pkofoot@usgs.gov","contributorId":4673,"corporation":false,"usgs":true,"family":"Kofoot","given":"Eric","email":"pkofoot@usgs.gov","middleInitial":"E.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":659368,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206326,"text":"70206326 - 2002 - Late Cenozoic deformation by evaporite tectonism in the Grand Hogback monocline, southwest of the White River uplift, Colorado","interactions":[],"lastModifiedDate":"2019-10-31T07:16:19","indexId":"70206326","displayToPublicDate":"2002-10-29T14:11:19","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Late Cenozoic deformation by evaporite tectonism in the Grand Hogback monocline, southwest of the White River uplift, Colorado","docAbstract":"<p><span>Along 50 km of the complex, southwest-dipping, Laramide Grand Hogback monocline, which wraps around the southwest flank of the White River uplift in westcentral Colorado, detailed mapping provides evidence of late Cenozoic collapse that resulted from subsurface flow, diapirism, and dissolution of Pennsylvanian Eagle Valley Evaporite. Numerous discontinuous, small-amplitude, strike-parallel folds and steeply dipping faults that overlie the evaporite are interpreted as the result of both flow-induced and dissolution-induced collapse and diapirism concentrated along cross-strike, radial valleys draining the uplift. Folding of an immature Pliocene conglomerate into a tight syncline by collapse into an underlying diapir emphasizes the young age of evaporite tectonism. Major evaporite diapirs in valleys penetrate overlying Pennsylvanian Eagle Valley and Pennsylvanian-Permian Maroon Formations. In the absence of a Miocene basaltic datum used to quantify collapse elsewhere in west-central Colorado, we quantify removal of evaporite by contrasting estimated original evaporite thicknesses with thicknesses of remaining evaporite based on surface structural control and cross section construction. We estimate that ∼40 km3 of evaporite were removed along the southwest flank, the majority of which came from cross-strike valleys and a minority from intervening drainage divides. The mechanism for initiation of flow of evaporite is interpreted to be late Cenozoic regional uplift and accompanying deep incision of valleys draining the White River uplift. Unloading of evaporite beneath these valleys channeled evaporite to flow northward up dip to diapirically extrude from overlying Maroon and Eagle Valley Formations. Laramide monoclinal structures change gradually along strike from a single monocline, which produced a complexly folded back thrust, to double monoclines stacked on one another, which are located close to bends in the flank of the uplift.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Late cenozoic evaporite tectonism and volcanism in west-Central Colorado","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2366-3.121","usgsCitation":"Scott, R.B., Bryant, B., and Perry, W.J., 2002, Late Cenozoic deformation by evaporite tectonism in the Grand Hogback monocline, southwest of the White River uplift, Colorado: Special Paper of the Geological Society of America, v. 366, p. 121-148, https://doi.org/10.1130/0-8137-2366-3.121.","productDescription":"28 p.","startPage":"121","endPage":"148","costCenters":[],"links":[{"id":368746,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.0283203125,\n              36.94989178681327\n            ],\n            [\n              -103.73291015625,\n              36.94989178681327\n            ],\n            [\n              -103.73291015625,\n              39.57182223734374\n            ],\n            [\n              -109.0283203125,\n              39.57182223734374\n            ],\n            [\n              -109.0283203125,\n              36.94989178681327\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"366","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Scott, Robert B. rbscott@usgs.gov","contributorId":766,"corporation":false,"usgs":true,"family":"Scott","given":"Robert","email":"rbscott@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":774167,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":774168,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perry, William J. Jr.","contributorId":220116,"corporation":false,"usgs":false,"family":"Perry","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":774169,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70206229,"text":"70206229 - 2002 - Usoi landslide dam, southeastern Tajikistan","interactions":[],"lastModifiedDate":"2019-10-28T06:28:01","indexId":"70206229","displayToPublicDate":"2002-10-25T10:05:36","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Usoi landslide dam, southeastern Tajikistan","docAbstract":"<p>No abstract available.&nbsp;</p>","conferenceTitle":"International Symposium on Landslide Risk Mitigation and Protection of Cultural and Natural Heritage","conferenceDate":"January 21-25, 2002","conferenceLocation":"Kyoto, Japan","language":"English","usgsCitation":"2002, Usoi landslide dam, southeastern Tajikistan, International Symposium on Landslide Risk Mitigation and Protection of Cultural and Natural Heritage, Kyoto, Japan, January 21-25, 2002, p. 489-505.","productDescription":"17 p.","startPage":"489","endPage":"505","costCenters":[],"links":[{"id":368601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Tajikistan ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[71.0142,40.24437],[70.64802,39.93575],[69.55961,40.10321],[69.46489,39.52668],[70.54916,39.6042],[71.78469,39.27946],[73.67538,39.43124],[73.92885,38.50582],[74.25751,38.60651],[74.86482,38.37885],[74.82999,37.99001],[74.98,37.41999],[73.9487,37.42157],[73.26006,37.49526],[72.63689,37.04756],[72.19304,36.94829],[71.84464,36.73817],[71.44869,37.06564],[71.54192,37.90577],[71.2394,37.95327],[71.34813,38.25891],[70.80682,38.48628],[70.3763,38.1384],[70.27057,37.73516],[70.11658,37.58822],[69.51879,37.609],[69.19627,37.15114],[68.85945,37.34434],[68.13556,37.02312],[67.83,37.14499],[68.39203,38.15703],[68.17603,38.90155],[67.44222,39.14014],[67.70143,39.58048],[68.53642,39.53345],[69.01163,40.08616],[69.32949,40.72782],[70.66662,40.96021],[70.45816,40.49649],[70.60141,40.21853],[71.0142,40.24437]]]},\"properties\":{\"name\":\"Tajikistan\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW"}
,{"id":70206183,"text":"70206183 - 2002 - Geothermal California: California claims the world's highest geothermal power output, with potential for even more production with advanced techniques","interactions":[],"lastModifiedDate":"2019-10-25T06:39:14","indexId":"70206183","displayToPublicDate":"2002-10-24T13:09:53","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5879,"text":"Geothermal Resources Council Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geothermal California: California claims the world's highest geothermal power output, with potential for even more production with advanced techniques","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geothermal Resources Council","issn":"0160-7782","usgsCitation":"Sass, J., and Priest, S., 2002, Geothermal California: California claims the world's highest geothermal power output, with potential for even more production with advanced techniques: Geothermal Resources Council Bulletin, v. 31, no. 5, p. 183-187.","productDescription":"5 p.","startPage":"183","endPage":"187","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":368558,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Glass Mountain, Casa Diablo, Coso, Honey Lake, Imperial Valley, Long Valley, Salton Sea, Surprise Valley, The Geysers","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-122.421439,37.869969],[-122.41847,37.852721],[-122.434403,37.852434],[-122.446316,37.861046],[-122.430958,37.872242],[-122.421439,37.869969]]],[[[-122.3785,37.826505],[-122.377879,37.830648],[-122.369941,37.832137],[-122.358779,37.814278],[-122.362661,37.807577],[-122.372422,37.811301],[-122.3785,37.826505]]],[[[-120.248484,33.999329],[-120.230001,34.010136],[-120.19578,34.004284],[-120.167306,34.008219],[-120.147647,34.024831],[-120.140362,34.025974],[-120.115058,34.019866],[-120.090182,34.019806],[-120.073609,34.024477],[-120.057637,34.03734],[-120.043259,34.035806],[-120.050382,34.013331],[-120.046575,34.000002],[-120.011123,33.979894],[-119.978876,33.983081],[-119.979913,33.969623],[-119.97026,33.944359],[-120.017715,33.936366],[-120.048611,33.915775],[-120.098601,33.907853],[-120.121817,33.895712],[-120.168974,33.91909],[-120.224461,33.989059],[-120.248484,33.999329]]],[[[-119.789798,34.05726],[-119.755521,34.056716],[-119.712576,34.043265],[-119.686507,34.019805],[-119.637742,34.013178],[-119.612226,34.021256],[-119.604287,34.031561],[-119.608798,34.035245],[-119.59324,34.049625],[-119.5667,34.053452],[-119.52064,34.034262],[-119.542449,34.021082],[-119.547072,34.005469],[-119.560464,33.99553],[-119.575636,33.996009],[-119.596877,33.988611],[-119.662825,33.985889],[-119.721206,33.959583],[-119.742966,33.963877],[-119.758141,33.959212],[-119.842748,33.97034],[-119.873358,33.980375],[-119.884896,34.008814],[-119.876329,34.032087],[-119.916216,34.058351],[-119.923337,34.069361],[-119.919155,34.07728],[-119.912857,34.077508],[-119.857304,34.071298],[-119.825865,34.059794],[-119.818742,34.052997],[-119.789798,34.05726]]],[[[-120.46258,34.042627],[-120.440248,34.036918],[-120.415287,34.05496],[-120.403613,34.050442],[-120.390906,34.051994],[-120.368813,34.06778],[-120.370176,34.074907],[-120.362251,34.073056],[-120.354982,34.059256],[-120.36029,34.05582],[-120.358608,34.050235],[-120.346946,34.046576],[-120.331161,34.049097],[-120.302122,34.023574],[-120.317052,34.018837],[-120.347706,34.020114],[-120.35793,34.015029],[-120.409368,34.032198],[-120.427408,34.025425],[-120.454134,34.028081],[-120.465329,34.038448],[-120.46258,34.042627]]],[[[-118.524531,32.895488],[-118.535823,32.90628],[-118.551134,32.945155],[-118.573522,32.969183],[-118.586928,33.008281],[-118.596037,33.015357],[-118.606559,33.01469],[-118.605534,33.030999],[-118.594033,33.035951],[-118.57516,33.033961],[-118.569013,33.029151],[-118.559171,33.006291],[-118.540069,32.980933],[-118.496811,32.933847],[-118.369984,32.839273],[-118.353504,32.821962],[-118.356541,32.817311],[-118.379968,32.824545],[-118.394565,32.823978],[-118.425634,32.800595],[-118.44492,32.820593],[-118.496298,32.851572],[-118.507193,32.876264],[-118.524531,32.895488]]],[[[-118.500212,33.449592],[-118.477646,33.448392],[-118.445812,33.428907],[-118.423576,33.427258],[-118.382037,33.409883],[-118.370323,33.409285],[-118.365094,33.388374],[-118.310213,33.335795],[-118.303174,33.320264],[-118.305084,33.310323],[-118.325244,33.299075],[-118.374768,33.320065],[-118.440047,33.318638],[-118.465368,33.326056],[-118.48877,33.356649],[-118.478465,33.38632],[-118.48875,33.419826],[-118.515914,33.422417],[-118.52323,33.430733],[-118.53738,33.434608],[-118.563442,33.434381],[-118.60403,33.47654],[-118.54453,33.474119],[-118.500212,33.449592]]],[[[-119.543842,33.280329],[-119.528141,33.284929],[-119.465717,33.259239],[-119.429559,33.228167],[-119.444269,33.21919],[-119.476029,33.21552],[-119.545872,33.233406],[-119.564971,33.24744],[-119.578942,33.278628],[-119.562042,33.271129],[-119.543842,33.280329]]],[[[-122.289533,42.007764],[-121.035195,41.993323],[-120.001058,41.995139],[-119.995926,40.499901],[-120.005743,39.228664],[-120.001014,38.999574],[-119.333423,38.538328],[-118.714312,38.102185],[-117.875927,37.497267],[-117.244917,37.030244],[-116.488233,36.459097],[-115.852908,35.96966],[-115.102881,35.379371],[-114.633013,35.002085],[-114.629015,34.986148],[-114.634953,34.958918],[-114.629753,34.938684],[-114.635176,34.875003],[-114.623939,34.859738],[-114.586842,34.835672],[-114.57101,34.794294],[-114.552682,34.766871],[-114.516619,34.736745],[-114.470477,34.711368],[-114.452628,34.668546],[-114.451753,34.654321],[-114.441465,34.64253],[-114.438739,34.621455],[-114.424202,34.610453],[-114.429747,34.591734],[-114.422382,34.580711],[-114.405228,34.569637],[-114.380838,34.529724],[-114.378124,34.507288],[-114.386699,34.457911],[-114.375789,34.447798],[-114.335372,34.450038],[-114.32613,34.437251],[-114.294836,34.421389],[-114.286802,34.40534],[-114.264317,34.401329],[-114.226107,34.365916],[-114.199482,34.361373],[-114.176909,34.349306],[-114.157206,34.317862],[-114.138282,34.30323],[-114.134768,34.268965],[-114.139055,34.259538],[-114.159697,34.258242],[-114.223384,34.205136],[-114.229715,34.186928],[-114.254141,34.173831],[-114.287294,34.170529],[-114.320777,34.138635],[-114.353031,34.133121],[-114.366521,34.118575],[-114.390565,34.110084],[-114.411681,34.110031],[-114.43338,34.088413],[-114.43934,34.057893],[-114.434949,34.037784],[-114.438266,34.022609],[-114.46283,34.008421],[-114.46117,33.994687],[-114.499883,33.961789],[-114.522002,33.955623],[-114.535478,33.934651],[-114.533679,33.926072],[-114.508558,33.906098],[-114.518555,33.889847],[-114.50434,33.876882],[-114.503017,33.867998],[-114.514673,33.858638],[-114.52453,33.858477],[-114.529597,33.848063],[-114.520465,33.827778],[-114.527161,33.816191],[-114.504863,33.760465],[-114.504483,33.750998],[-114.512348,33.734214],[-114.496565,33.719155],[-114.494197,33.707922],[-114.495719,33.698454],[-114.523959,33.685879],[-114.531523,33.675108],[-114.525201,33.661583],[-114.530244,33.65014],[-114.526947,33.637534],[-114.529662,33.622794],[-114.524813,33.611351],[-114.540617,33.591412],[-114.5403,33.580615],[-114.524391,33.553683],[-114.558898,33.531819],[-114.560552,33.518272],[-114.569533,33.509219],[-114.591554,33.499443],[-114.622918,33.456561],[-114.627125,33.433554],[-114.635183,33.422726],[-114.652828,33.412922],[-114.687953,33.417944],[-114.701732,33.408388],[-114.725535,33.404056],[-114.708408,33.384147],[-114.698035,33.352442],[-114.707962,33.323421],[-114.731223,33.302434],[-114.723259,33.288079],[-114.684363,33.276025],[-114.672401,33.26047],[-114.689421,33.24525],[-114.674479,33.225504],[-114.678749,33.203448],[-114.675831,33.18152],[-114.679359,33.159519],[-114.703682,33.113769],[-114.706488,33.08816],[-114.68902,33.084036],[-114.686991,33.070969],[-114.674296,33.057171],[-114.673659,33.041897],[-114.662317,33.032671],[-114.64598,33.048903],[-114.618788,33.027202],[-114.589778,33.026228],[-114.575161,33.036542],[-114.52013,33.029984],[-114.502871,33.011153],[-114.492938,32.971781],[-114.476156,32.975168],[-114.467664,32.966861],[-114.469113,32.952673],[-114.48074,32.937027],[-114.47664,32.923628],[-114.462929,32.907944],[-114.468971,32.845155],[-114.494116,32.823288],[-114.510217,32.816417],[-114.530755,32.793485],[-114.532432,32.776923],[-114.526856,32.757094],[-114.539093,32.756949],[-114.539224,32.749812],[-114.564447,32.749554],[-114.564508,32.742298],[-114.581736,32.742321],[-114.581784,32.734946],[-114.612697,32.734516],[-114.618373,32.728245],[-114.688779,32.737675],[-114.701918,32.745548],[-114.719633,32.718763],[-116.04662,32.623353],[-117.124862,32.534156],[-117.136664,32.618754],[-117.168866,32.671952],[-117.196767,32.688851],[-117.213068,32.687751],[-117.236239,32.671353],[-117.246069,32.669352],[-117.25757,32.72605],[-117.25257,32.752949],[-117.25497,32.786948],[-117.26107,32.803148],[-117.280971,32.822247],[-117.28217,32.839547],[-117.27387,32.851447],[-117.26497,32.848947],[-117.25617,32.859447],[-117.25167,32.874346],[-117.25447,32.900146],[-117.28077,33.012343],[-117.315278,33.093504],[-117.328359,33.121842],[-117.362572,33.168437],[-117.469794,33.296417],[-117.50565,33.334063],[-117.547693,33.365491],[-117.59588,33.386629],[-117.607905,33.406317],[-117.645582,33.440728],[-117.684584,33.461927],[-117.691984,33.456627],[-117.715349,33.460556],[-117.726486,33.483427],[-117.784888,33.541525],[-117.814188,33.552224],[-117.840289,33.573523],[-117.87679,33.592322],[-117.927091,33.605521],[-117.940591,33.620021],[-118.000593,33.654319],[-118.029694,33.676418],[-118.088896,33.729817],[-118.132698,33.753217],[-118.180831,33.763072],[-118.187701,33.749218],[-118.181367,33.717367],[-118.207476,33.716905],[-118.258687,33.703741],[-118.317205,33.712818],[-118.360505,33.736817],[-118.385006,33.741417],[-118.396606,33.735917],[-118.411211,33.741985],[-118.428407,33.774715],[-118.405007,33.800215],[-118.394376,33.804289],[-118.392107,33.840915],[-118.460611,33.969111],[-118.482729,33.995912],[-118.519514,34.027509],[-118.543115,34.038508],[-118.569235,34.04164],[-118.609652,34.036424],[-118.668358,34.038887],[-118.706215,34.029383],[-118.744952,34.032103],[-118.783433,34.021543],[-118.805114,34.001239],[-118.854653,34.034215],[-118.928048,34.045847],[-118.938081,34.043383],[-119.004644,34.066231],[-119.037494,34.083111],[-119.088536,34.09831],[-119.109784,34.094566],[-119.130169,34.100102],[-119.18864,34.139005],[-119.216441,34.146105],[-119.257043,34.213304],[-119.278644,34.266902],[-119.290945,34.274902],[-119.313034,34.275689],[-119.337475,34.290576],[-119.370356,34.319486],[-119.388249,34.317398],[-119.42777,34.353016],[-119.461036,34.374064],[-119.536957,34.395495],[-119.559459,34.413395],[-119.616862,34.420995],[-119.638864,34.415696],[-119.671866,34.416096],[-119.688167,34.412497],[-119.684666,34.408297],[-119.709067,34.395397],[-119.729369,34.395897],[-119.794771,34.417597],[-119.835771,34.415796],[-119.853771,34.407996],[-119.873971,34.408795],[-119.925227,34.433931],[-119.956433,34.435288],[-120.008077,34.460447],[-120.038828,34.463434],[-120.088591,34.460208],[-120.141165,34.473405],[-120.25777,34.467451],[-120.295051,34.470623],[-120.341369,34.458789],[-120.471376,34.447846],[-120.47661,34.475131],[-120.511421,34.522953],[-120.581293,34.556959],[-120.622575,34.554017],[-120.637805,34.56622],[-120.645739,34.581035],[-120.640244,34.604406],[-120.60197,34.692095],[-120.60045,34.70464],[-120.614852,34.730709],[-120.62632,34.738072],[-120.637415,34.755895],[-120.616296,34.816308],[-120.610266,34.85818],[-120.616325,34.866739],[-120.639283,34.880413],[-120.647328,34.901133],[-120.670835,34.904115],[-120.63999,35.002963],[-120.629931,35.061515],[-120.630957,35.101941],[-120.644311,35.139616],[-120.651134,35.147768],[-120.662475,35.153357],[-120.675074,35.153061],[-120.698906,35.171192],[-120.714185,35.175998],[-120.74887,35.177795],[-120.754823,35.174701],[-120.756086,35.160459],[-120.760492,35.15971],[-120.778998,35.168897],[-120.786076,35.177666],[-120.856047,35.206487],[-120.89679,35.247877],[-120.862684,35.346776],[-120.866099,35.393045],[-120.884757,35.430196],[-120.907937,35.449069],[-120.946546,35.446715],[-120.969436,35.460197],[-121.003359,35.46071],[-121.101595,35.548814],[-121.126027,35.593058],[-121.143561,35.606046],[-121.166712,35.635399],[-121.251034,35.656641],[-121.284973,35.674109],[-121.289794,35.689428],[-121.314632,35.71331],[-121.315786,35.75252],[-121.332449,35.783106],[-121.388053,35.823483],[-121.413146,35.855316],[-121.439584,35.86695],[-121.462264,35.885618],[-121.461227,35.896906],[-121.472435,35.91989],[-121.4862,35.970348],[-121.503112,36.000299],[-121.531876,36.014368],[-121.574602,36.025156],[-121.590395,36.050363],[-121.592853,36.065062],[-121.606845,36.072065],[-121.618672,36.087767],[-121.629634,36.114452],[-121.680145,36.165818],[-121.717176,36.195146],[-121.779851,36.227407],[-121.797059,36.234211],[-121.813734,36.234235],[-121.826425,36.24186],[-121.851967,36.277831],[-121.874797,36.289064],[-121.888491,36.30281],[-121.894714,36.317806],[-121.892917,36.340428],[-121.905446,36.358269],[-121.903195,36.393603],[-121.914378,36.404344],[-121.91474,36.42589],[-121.9416,36.485602],[-121.938763,36.506423],[-121.944666,36.521861],[-121.925937,36.525173],[-121.932508,36.559935],[-121.942533,36.566435],[-121.957335,36.564482],[-121.978592,36.580488],[-121.970427,36.582754],[-121.941666,36.618059],[-121.93643,36.636746],[-121.923866,36.634559],[-121.890164,36.609259],[-121.889064,36.601759],[-121.860604,36.611136],[-121.831995,36.644856],[-121.814462,36.682858],[-121.807062,36.714157],[-121.805643,36.750239],[-121.788278,36.803994],[-121.809363,36.848654],[-121.862266,36.931552],[-121.894667,36.961851],[-121.930069,36.97815],[-121.95167,36.97145],[-121.972771,36.954151],[-122.012373,36.96455],[-122.023373,36.96215],[-122.027174,36.95115],[-122.050122,36.948523],[-122.105976,36.955951],[-122.155078,36.98085],[-122.20618,37.013949],[-122.252181,37.059448],[-122.284882,37.101747],[-122.306139,37.116383],[-122.337071,37.117382],[-122.337833,37.135936],[-122.359791,37.155574],[-122.367085,37.172817],[-122.390599,37.182988],[-122.405073,37.195791],[-122.407181,37.219465],[-122.419113,37.24147],[-122.411686,37.265844],[-122.40085,37.359225],[-122.423286,37.392542],[-122.443687,37.435941],[-122.452087,37.48054],[-122.472388,37.50054],[-122.493789,37.492341],[-122.499289,37.495341],[-122.516689,37.52134],[-122.519533,37.537302],[-122.513688,37.552239],[-122.517187,37.590637],[-122.501386,37.599637],[-122.494085,37.644035],[-122.496784,37.686433],[-122.514483,37.780829],[-122.50531,37.788312],[-122.485783,37.790629],[-122.478083,37.810828],[-122.463793,37.804653],[-122.407452,37.811441],[-122.398139,37.80563],[-122.385323,37.790724],[-122.375854,37.734979],[-122.356784,37.729505],[-122.361749,37.71501],[-122.370411,37.717572],[-122.391374,37.708331],[-122.387626,37.67906],[-122.374291,37.662206],[-122.3756,37.652389],[-122.387381,37.648462],[-122.386072,37.637662],[-122.35531,37.615736],[-122.358583,37.611155],[-122.373309,37.613773],[-122.378545,37.605592],[-122.360219,37.592501],[-122.317676,37.590865],[-122.305895,37.575484],[-122.262698,37.572866],[-122.214264,37.538505],[-122.196593,37.537196],[-122.194957,37.522469],[-122.168449,37.504143],[-122.155686,37.501198],[-122.140142,37.507907],[-122.127706,37.500053],[-122.111344,37.50758],[-122.111998,37.528851],[-122.147014,37.588411],[-122.145378,37.600846],[-122.152905,37.640771],[-122.163049,37.667933],[-122.246826,37.72193],[-122.257953,37.739601],[-122.257134,37.745001],[-122.242638,37.753744],[-122.253753,37.761218],[-122.293996,37.770416],[-122.330963,37.786035],[-122.33555,37.799538],[-122.333711,37.809797],[-122.323567,37.823214],[-122.303931,37.830087],[-122.301313,37.847758],[-122.310477,37.873938],[-122.309986,37.892755],[-122.32373,37.905845],[-122.33453,37.908791],[-122.35711,37.908791],[-122.367582,37.903882],[-122.385908,37.908136],[-122.39049,37.922535],[-122.413725,37.937262],[-122.430087,37.963115],[-122.415361,37.963115],[-122.399832,37.956009],[-122.367582,37.978168],[-122.361905,37.989991],[-122.367909,38.01253],[-122.340093,38.003694],[-122.321112,38.012857],[-122.300823,38.010893],[-122.283478,38.022674],[-122.262861,38.0446],[-122.273006,38.07438],[-122.314567,38.115287],[-122.366273,38.141467],[-122.39638,38.149976],[-122.403514,38.150624],[-122.409798,38.136231],[-122.439577,38.116923],[-122.454958,38.118887],[-122.489974,38.112014],[-122.483757,38.071762],[-122.499465,38.032165],[-122.497828,38.019402],[-122.481466,38.007621],[-122.462812,38.003367],[-122.452995,37.996167],[-122.448413,37.984713],[-122.456595,37.978823],[-122.471975,37.981768],[-122.488665,37.966714],[-122.487684,37.948716],[-122.479175,37.941516],[-122.48572,37.937589],[-122.499465,37.939225],[-122.503064,37.928753],[-122.478193,37.918608],[-122.471975,37.910427],[-122.472303,37.902573],[-122.458558,37.894064],[-122.448413,37.89341],[-122.438268,37.880974],[-122.45005,37.871157],[-122.462158,37.868866],[-122.480811,37.873448],[-122.479151,37.825428],[-122.505383,37.822128],[-122.548986,37.836227],[-122.561487,37.851827],[-122.584289,37.859227],[-122.60129,37.875126],[-122.656519,37.904519],[-122.682171,37.90645],[-122.70264,37.89382],[-122.727297,37.904626],[-122.736898,37.925825],[-122.766138,37.938004],[-122.783244,37.951334],[-122.797405,37.976657],[-122.821383,37.996735],[-122.856573,38.016717],[-122.882114,38.025273],[-122.939711,38.031908],[-122.956811,38.02872],[-122.981776,38.009119],[-122.97439,37.992429],[-123.024066,37.994878],[-123.011533,38.003438],[-122.99242,38.041758],[-122.960889,38.112962],[-122.949074,38.15406],[-122.953629,38.17567],[-122.965408,38.187113],[-122.968112,38.202428],[-122.993959,38.237602],[-122.968569,38.242879],[-122.967203,38.250691],[-122.977082,38.267902],[-122.986319,38.273164],[-123.002911,38.295708],[-123.024333,38.310573],[-123.038742,38.313576],[-123.051061,38.310693],[-123.053504,38.299385],[-123.063671,38.302178],[-123.074684,38.322574],[-123.068437,38.33521],[-123.068265,38.359865],[-123.128825,38.450418],[-123.202277,38.494314],[-123.249797,38.511045],[-123.287156,38.540223],[-123.331899,38.565542],[-123.343338,38.590008],[-123.371876,38.607235],[-123.398166,38.647044],[-123.441774,38.699744],[-123.461291,38.717001],[-123.514784,38.741966],[-123.541837,38.776764],[-123.579856,38.802835],[-123.58638,38.802857],[-123.605317,38.822765],[-123.647387,38.845472],[-123.659846,38.872529],[-123.71054,38.91323],[-123.725367,38.917438],[-123.726315,38.936367],[-123.738886,38.95412],[-123.729053,38.956667],[-123.711149,38.977316],[-123.6969,39.004401],[-123.690095,39.031157],[-123.693969,39.057363],[-123.713392,39.108422],[-123.721505,39.125327],[-123.737913,39.143442],[-123.742221,39.164885],[-123.765891,39.193657],[-123.774998,39.212083],[-123.777368,39.237214],[-123.787893,39.264327],[-123.803848,39.278771],[-123.803081,39.291747],[-123.811387,39.312825],[-123.808772,39.324368],[-123.822085,39.343857],[-123.826306,39.36871],[-123.81469,39.446538],[-123.766475,39.552803],[-123.787417,39.604552],[-123.782322,39.621486],[-123.792659,39.684122],[-123.808208,39.710715],[-123.829545,39.723071],[-123.838089,39.752409],[-123.839797,39.795637],[-123.851714,39.832041],[-123.907664,39.863028],[-123.930047,39.909697],[-123.954952,39.922373],[-123.980031,39.962458],[-124.035904,40.013319],[-124.056408,40.024305],[-124.068908,40.021307],[-124.079983,40.029773],[-124.080709,40.06611],[-124.110549,40.103765],[-124.187874,40.130542],[-124.214895,40.160902],[-124.296497,40.208816],[-124.320912,40.226617],[-124.327691,40.23737],[-124.34307,40.243979],[-124.363414,40.260974],[-124.363634,40.276212],[-124.347853,40.314634],[-124.362796,40.350046],[-124.365357,40.374855],[-124.373599,40.392923],[-124.391496,40.407047],[-124.409591,40.438076],[-124.38494,40.48982],[-124.383224,40.499852],[-124.387023,40.504954],[-124.382816,40.519],[-124.329404,40.61643],[-124.158322,40.876069],[-124.137066,40.925732],[-124.118147,40.989263],[-124.112165,41.028173],[-124.125448,41.048504],[-124.138217,41.054342],[-124.153622,41.05355],[-124.154513,41.087159],[-124.160556,41.099011],[-124.159065,41.121957],[-124.165414,41.129822],[-124.158539,41.143021],[-124.149674,41.140845],[-124.1438,41.144686],[-124.106986,41.229678],[-124.072294,41.374844],[-124.063076,41.439579],[-124.066057,41.470258],[-124.081427,41.511228],[-124.081987,41.547761],[-124.092404,41.553615],[-124.101123,41.569192],[-124.097385,41.585251],[-124.100961,41.602499],[-124.114413,41.616768],[-124.120225,41.640354],[-124.135552,41.657307],[-124.147412,41.717955],[-124.164716,41.740126],[-124.17739,41.745756],[-124.194953,41.736778],[-124.23972,41.7708],[-124.248704,41.771459],[-124.255994,41.783014],[-124.245027,41.7923],[-124.230678,41.818681],[-124.208439,41.888192],[-124.203402,41.940964],[-124.204948,41.983441],[-124.211605,41.99846],[-123.656998,41.995137],[-123.624554,41.999837],[-123.347562,41.999108],[-123.145959,42.009247],[-123.045254,42.003049],[-122.893961,42.002605],[-122.289533,42.007764]]]]},\"properties\":{\"name\":\"California\",\"nation\":\"USA  \"}}]}","volume":"31","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":773789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":1116,"corporation":false,"usgs":true,"family":"Priest","given":"Susan S.","email":"spriest@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":773790,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180956,"text":"70180956 - 2002 - Water-level measurements and chloride concentrations for selected wells in Louisiana, January 1988-October 1997","interactions":[],"lastModifiedDate":"2017-02-09T15:57:27","indexId":"70180956","displayToPublicDate":"2002-10-16T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":303,"text":"Water-Resources Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"23","title":"Water-level measurements and chloride concentrations for selected wells in Louisiana, January 1988-October 1997","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">This <span class=\"searchword\">report</span> presents <span class=\"searchword\">water</span>-<span class=\"searchword\">level</span> <span class=\"searchword\">measurements</span> and <span class=\"searchword\">chloride</span><span class=\"searchword\">concentrations</span> in <span class=\"searchword\">water</span> from <span class=\"searchword\">selected</span> <span class=\"searchword\">wells</span> completed in aquifers in <span class=\"searchword\">Louisiana</span>. The data were collected during the period <span class=\"searchword\">January</span><span class=\"searchword\">1988</span>-<span class=\"searchword\">October</span> <span class=\"searchword\">1997</span>. <span class=\"searchword\">Water</span>-<span class=\"searchword\">level</span> data are presented for 109 <span class=\"searchword\">wells</span>, and <span class=\"searchword\">chloride</span> data are presented for 45 <span class=\"searchword\">wells</span>. Hydrographs and summaries of <span class=\"searchword\">water</span>-<span class=\"searchword\">level</span> trends are presented for <span class=\"searchword\">wells</span>completed in aquifers throughout the State. Chlorographs and summaries of <span class=\"searchword\">chloride</span> trends are presented for <span class=\"searchword\">wells</span> completed in the Mississippi River alluvial and Sparta aquifers; Chicot aquifer system; and Gramercy, Norco, and Gonzales-New Orleans aquifers. Data are presented in graphical and tabular formats.</span> </p>","language":"English","publisher":"United States: Louisiana Department of Transportation and Development, Office of Public Works ","publisherLocation":"Baton Rouge, LA","issn":"0731-7638 ","usgsCitation":"Lovelace, W.M., 2002, Water-level measurements and chloride concentrations for selected wells in Louisiana, January 1988-October 1997: Water-Resources Bulletin 23.","costCenters":[],"links":[{"id":335097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"589d8dd7e4b0efcedb7ae5dd","contributors":{"authors":[{"text":"Lovelace, Wendell M.","contributorId":56750,"corporation":false,"usgs":true,"family":"Lovelace","given":"Wendell","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":662964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70223167,"text":"70223167 - 2002 - The flood pulse concept in wetland restoration","interactions":[],"lastModifiedDate":"2021-08-13T18:18:29.742847","indexId":"70223167","displayToPublicDate":"2002-10-15T12:01:43","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"title":"The flood pulse concept in wetland restoration","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Flood pulsing in wetlands: Restoring the natural hydrological balance","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"John Wiley & Sons, Inc.","publisherLocation":"Hoboken, NJ","usgsCitation":"Middleton, B.A., 2002, The flood pulse concept in wetland restoration, chap. <i>of</i> Flood pulsing in wetlands: Restoring the natural hydrological balance, p. 1-10.","startPage":"1","endPage":"10","numberOfPages":"10","costCenters":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":387926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":387925,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wiley.com/en-us/Flood+Pulsing+in+Wetlands%3A+Restoring+the+Natural+Hydrological+Balance-p-9780471418078","description":"Index Page"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Middleton, Beth A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":2029,"corporation":false,"usgs":true,"family":"Middleton","given":"Beth","email":"middletonb@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":821203,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Middleton, Beth A. 0000-0002-1220-2326 middletonb@usgs.gov","orcid":"https://orcid.org/0000-0002-1220-2326","contributorId":2029,"corporation":false,"usgs":true,"family":"Middleton","given":"Beth","email":"middletonb@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":821202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205922,"text":"70205922 - 2002 - Ancestral submarine growth of Kïlauea Volcano and instability of its south flank","interactions":[],"lastModifiedDate":"2023-04-28T14:51:12.376586","indexId":"70205922","displayToPublicDate":"2002-10-11T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Ancestral submarine growth of Kïlauea Volcano and instability of its south flank","docAbstract":"<p>Joint Japan-USA cruises in 1998-99 explored and sampled the previously unstudied deep offshore region south of Kilauea. Bathymetric features, dive observations, and recovered samples indicate that the 3-km-deep mid-slope bench, bounded seaward by a 2-km-high lower scarp, is underlain by massive turbidite sandstone and interbedded debris-flow breccia. Debris-flow clasts are submarineerupted (high-S) alkalic basalt, distinctive fine- to coarse-grained alkalic gabbro and nephelinite (some containing phlogopite), and subordinate transitional basalt. N o recovered clasts are similar to recent Kilauea tholeiite. Primary volcanic deposits (pillow basalt, hyaloclastite breccia) are absent. The sandstone and breccia matrix, a large fraction of the volcaniclastic apron, are mainly subaerially erupted (low-S) tholeiitic glass sand generated by shoreline processes on pre-Kilauea volcanoes. Fractures, shears, slickensided clasts, and open folds indicate widespread deformation low in the lower scarp; upward-decreasing proportions of alkalic materials define a gross stratigraphy. Alkalic high-S compositions of many basalt clasts and some sandstone glass indicate derivation from the submarine \"Lo'ihi\" stage of ancestral Kilauea, prior to growth of its tholeiitic shield. Slopes (3300-2800 m depth) above the mid-slope bench contain submarine-erupted (S &gt;750 ppm) pillow lava of transitional basalt, defining the initial flank of subalkaline Kilauea. The geometry and diverse constituents of the bench and lower scarp require initial landsliding during alkalic volcanism at 200-300 ka, prior to shield growth at Kilauea and inception of Hilina faults. The active Hilina slump structures on Kilauea's south flank are in an early growth stage, thus possibly posing greater potential for future large-scale landsliding and tsunamis</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian volcanoes: Deep underwater perspectives","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/GM128p0161","usgsCitation":"Lipman, P.W., Sisson, T.W., Ui, T., Naka, J., and Smith, J., 2002, Ancestral submarine growth of Kïlauea Volcano and instability of its south flank, chap. <i>of</i> Hawaiian volcanoes: Deep underwater perspectives, v. 128, p. 161-191, https://doi.org/10.1029/GM128p0161.","productDescription":"31p.","startPage":"161","endPage":"191","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368226,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.45654296875,\n              18.8335153964335\n            ],\n            [\n              -154.70947265625,\n              18.8335153964335\n            ],\n            [\n              -154.70947265625,\n              19.48730751856426\n            ],\n            [\n              -155.45654296875,\n              19.48730751856426\n            ],\n            [\n              -155.45654296875,\n              18.8335153964335\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ui, Tadahide","contributorId":219701,"corporation":false,"usgs":false,"family":"Ui","given":"Tadahide","email":"","affiliations":[],"preferred":false,"id":772916,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Naka, Jiro","contributorId":64347,"corporation":false,"usgs":true,"family":"Naka","given":"Jiro","email":"","affiliations":[],"preferred":false,"id":772917,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, John R.","contributorId":13321,"corporation":false,"usgs":true,"family":"Smith","given":"John R.","affiliations":[],"preferred":false,"id":772918,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70205931,"text":"70205931 - 2002 - Deep-sea volcaniclastic sedimentation around the southern flank of Hawaii","interactions":[],"lastModifiedDate":"2019-10-10T12:06:41","indexId":"70205931","displayToPublicDate":"2002-10-10T11:58:21","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Deep-sea volcaniclastic sedimentation around the southern flank of Hawaii","docAbstract":"<p>Most slopes of the Hilina slump are steep, but local small benches, mantled by volcaniclastic sand and fine sediments, were sampled in 1998-1999 with ROV KAIKO and DSRV SHINKAI 6500. Most surficial glass sands on the Hilina slump have compositions of subaerially erupted Kilauea lava, which fragmented and quenched as they entered the sea. Samples from the base of the Puna Ridge contain both subaerially and submarine-erupted fragments of Kilauea composition. Some glass sands from the base of Loihi contain both subaerial Kilauea and submarine Loihi compositions in the same bed. Two piston cores, collected 120 km (P6) and 250 km (P5) southeast of Hawaii, are composed of fine sediments interbedded with volcaniclastic turbidite layers. Although some volcaniclastic fragments in the fine sediments intervals are disturbed by bioturbation, nearly continuous volcanostratigraphic sequences are preserved. P6 and the upper 2.3 m of P5 are normally magnetized: the lower part of P5 is reversed and is therefore older than 0.78 Ma. At depths of 4 m below sea floor (mbsf) in P6 and 1 mbsf in P5, the dominant glass compositions change down core from Kilauea to Mauna Loa type. In the P6, an interval of abundant submarine-erupted alkalic glasses lies between 3.3 and 1.75 mbsf and may record the ancestral alkalic phase of Kilauea volcano. Magnetic susceptibility trends and glass compositions suggest that the entire P6 core correlates with only the uppermost 1.2 m of the P5, and that the average sedimentation rate at the P6 is about 5 times greater than that at P5. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian Volcanoes: Deep Underwater Perspectives ","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":" American Geophysical Union","doi":"10.1029/GM128p0029","usgsCitation":"Naka, J., Kanamatsu, T., Lipman, P.W., Sisson, T.W., Tsuboyama, N., Morgan, J.K., Smith, J., and Ui, T., 2002, Deep-sea volcaniclastic sedimentation around the southern flank of Hawaii, chap. <i>of</i> Hawaiian Volcanoes: Deep Underwater Perspectives , v. 128, p. 29-50, https://doi.org/10.1029/GM128p0029.","productDescription":"22 p.","startPage":"29","endPage":"50","numberOfPages":"22","costCenters":[],"links":[{"id":368232,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":" Puna Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.3741455078125,\n              18.911483222018383\n            ],\n            [\n              -154.324951171875,\n              18.911483222018383\n            ],\n            [\n              -154.324951171875,\n              19.590844152960923\n            ],\n            [\n              -155.3741455078125,\n              19.590844152960923\n            ],\n            [\n              -155.3741455078125,\n              18.911483222018383\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Naka, Jiro","contributorId":64347,"corporation":false,"usgs":true,"family":"Naka","given":"Jiro","email":"","affiliations":[],"preferred":false,"id":772941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kanamatsu, Toshiya","contributorId":108203,"corporation":false,"usgs":true,"family":"Kanamatsu","given":"Toshiya","email":"","affiliations":[],"preferred":false,"id":772942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":772943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772944,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tsuboyama, Nohiro","contributorId":219712,"corporation":false,"usgs":false,"family":"Tsuboyama","given":"Nohiro","email":"","affiliations":[],"preferred":false,"id":772945,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Morgan, Julia K.","contributorId":127859,"corporation":false,"usgs":false,"family":"Morgan","given":"Julia","email":"","middleInitial":"K.","affiliations":[{"id":7173,"text":"Rice University","active":true,"usgs":false}],"preferred":false,"id":772946,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Smith, John R.","contributorId":13321,"corporation":false,"usgs":true,"family":"Smith","given":"John R.","affiliations":[],"preferred":false,"id":772947,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ui, Tadahide","contributorId":219701,"corporation":false,"usgs":false,"family":"Ui","given":"Tadahide","email":"","affiliations":[],"preferred":false,"id":772948,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70205925,"text":"70205925 - 2002 - Emplacement and inflation structures of submarine and subaerial pahoehoe lavas from Hawaii","interactions":[],"lastModifiedDate":"2019-10-10T11:54:52","indexId":"70205925","displayToPublicDate":"2002-10-10T11:40:35","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Emplacement and inflation structures of submarine and subaerial pahoehoe lavas from Hawaii","docAbstract":"<p>Features of subaerial pahoehoe tumuli from Kilauea and Mauna Loa Volcanoes in Hawaii and subaqueous flow lobes from Loihi Seamount off Hawaii and north of Oahu Island document the controlling factors of flow-lobe formation. Studied subaerial flow-lobe tumuli consist of uplifted pahoehoe crust, formed from coalesced flow lobes. The south rift zone of Loihi has abundant conical lava mounds and terraces with flat tops. Steep flanks (&gt;4°) of these mounds are covered with elongate pillows, but the flat tops are overlain by lobate sheets and inflated pahoehoe flows. The pahoehoe lobes have an elongate dome-like shape 2 x 0.5 m to 20 x 20 m and up to 5 m in height. Hollow pahoehoe lobes, which are rare among subaerial pahoehoe flows on coastal plains in Hawaii Island, are common on Loihi. Similar hollow lobes and a subaqueous tumulus were found on a 2200-m deep terrace offshore of Oahu Island. In contrast to corrugated pillow lobes, these subaqueous flows have smooth surfaces covered with fine streaks of thin glass flakes. We suggest that subaqueous flow lobes grow like a slowly advancing subaerial pahoehoe flow. The plastic crust stretches, thins, and ruptures at the flow front, where new lava is exposed, and subsequently is quenched by water to form thin flaky glass. The Graetz number, giving a dimensionless temperature distribution within lava, varies flow by flow but remains almost constant for subaqueous flow lobes. This means that the lateral extension of a flow lobe is cooling limited, which results in a linear correlation between the rate of lava supply and the volume of lobes. Flow lobes stop advancing due to heat loss to the environment, as brittle crust thickens and hinders the lobes from deforming freely. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian Volcanoes: Deep Underwater Perspectives","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/GM128p0085","usgsCitation":"Umino, S., Obata, S., Lipman, P.W., Smith, J., Shibata, T., Naka, J., and Trusdell, F., 2002, Emplacement and inflation structures of submarine and subaerial pahoehoe lavas from Hawaii, chap. <i>of</i> Hawaiian Volcanoes: Deep Underwater Perspectives, v. 128, p. 85-101, https://doi.org/10.1029/GM128p0085.","productDescription":"17 p.","startPage":"85","endPage":"101","costCenters":[],"links":[{"id":368231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -158.28826904296872,\n              21.555284406923192\n            ],\n            [\n              -157.7801513671875,\n              21.555284406923192\n            ],\n            [\n              -157.7801513671875,\n              21.922663209325922\n            ],\n            [\n              -158.28826904296872,\n              21.922663209325922\n            ],\n            [\n              -158.28826904296872,\n              21.555284406923192\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.37939453125,\n              18.687878686034182\n            ],\n            [\n              -154.423828125,\n              18.687878686034182\n            ],\n            [\n              -154.423828125,\n              20.437307950568957\n            ],\n            [\n              -156.37939453125,\n              20.437307950568957\n            ],\n            [\n              -156.37939453125,\n              18.687878686034182\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Umino, Susumu","contributorId":42773,"corporation":false,"usgs":true,"family":"Umino","given":"Susumu","email":"","affiliations":[],"preferred":false,"id":772928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Obata, Sumie","contributorId":219708,"corporation":false,"usgs":false,"family":"Obata","given":"Sumie","email":"","affiliations":[],"preferred":false,"id":772929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772930,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, John R.","contributorId":13321,"corporation":false,"usgs":true,"family":"Smith","given":"John R.","affiliations":[],"preferred":false,"id":772931,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Shibata, Tsugio","contributorId":219709,"corporation":false,"usgs":false,"family":"Shibata","given":"Tsugio","email":"","affiliations":[],"preferred":false,"id":772932,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Naka, Jiro","contributorId":64347,"corporation":false,"usgs":true,"family":"Naka","given":"Jiro","email":"","affiliations":[],"preferred":false,"id":772933,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Trusdell, Frank A. 0000-0002-0681-0528 trusdell@usgs.gov","orcid":"https://orcid.org/0000-0002-0681-0528","contributorId":754,"corporation":false,"usgs":true,"family":"Trusdell","given":"Frank A.","email":"trusdell@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772934,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70205921,"text":"70205921 - 2002 - Submarine landslides and volcanic features on Kohala and Mauna Kea volcanoes and the Hana Ridge, Hawaii","interactions":[],"lastModifiedDate":"2020-09-27T22:06:01.644507","indexId":"70205921","displayToPublicDate":"2002-10-10T10:34:16","publicationYear":"2002","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Submarine landslides and volcanic features on Kohala and Mauna Kea volcanoes and the Hana Ridge, Hawaii","docAbstract":"<p><span>The deep submarine eastern flanks of Mauna Kea, Kohala, and Haleakala volcanoes were mapped for the first time with a multibeam bathymetric and sidescan sonar system during joint Japan-US cruises aboard the JAMSTEC vessel R/V Yokosuka in 1999. The Pololu slump off northeast Kohala is overlain by a carbonate platform in the shallow region and the deeper areas are incised by downslope oriented channels. It is cut by several faults and slump scars and appears to override an older slide located farther east, here named the Laupahoehoe slump. The structures characteristic of the Laupahoehoe slump are NW-SE oriented scarp-and-bench topographic features analogous to the Hilina slump on the mobile SE flank of Kilauea. Enclosed basins lie at 3000-5000 m, fronted by ridges on their seaward sides. The basins may result from local rotational slumps or from uplift above discontinuous thrust faults. The Laupahoehoe slump appears to be overlapped by shield margins of both Kohala and Mauna Kea and thus may have been derived from an elongate Kohala edifice. A large debris apron continues from the base of the two-slide complex, abutting the distal Hana Ridge (Haleakala east rift zone). The tip of the Hana Ridge displays a curious steepsided arcuate rift tip that resembles the classic amphitheater scarp of a landslide. Numerous flat-topped volcanic domes are distributed along the broad crest of the lower rift zone. Similar cones, though fewer in number, are also present on the Hilo Ridge, which may be the continuation of a Kohala rift zone.&nbsp;</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian Volcanoes: Deep Underwater Perspectives","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/GM128p0011","issn":"00658448","usgsCitation":"Smith, J., Kenji, S., Morgan, J., and Lipman, P.W., 2002, Submarine landslides and volcanic features on Kohala and Mauna Kea volcanoes and the Hana Ridge, Hawaii, chap. <i>of</i> Hawaiian Volcanoes: Deep Underwater Perspectives, v. 128, p. 11-28, https://doi.org/10.1029/GM128p0011.","productDescription":"18 p.","startPage":"11","endPage":"28","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Southeast flank of the island of Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.148681640625,\n              19.78738018198621\n            ],\n            [\n              -154.654541015625,\n              19.78738018198621\n            ],\n            [\n              -154.654541015625,\n              20.930658643632885\n            ],\n            [\n              -156.148681640625,\n              20.930658643632885\n            ],\n            [\n              -156.148681640625,\n              19.78738018198621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, J.R.","contributorId":43942,"corporation":false,"usgs":true,"family":"Smith","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":772905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kenji, Satake","contributorId":88829,"corporation":false,"usgs":true,"family":"Kenji","given":"Satake","email":"","affiliations":[],"preferred":false,"id":772906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, J.K.","contributorId":83333,"corporation":false,"usgs":true,"family":"Morgan","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":772907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772908,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70205909,"text":"70205909 - 2002 - Submarine alkalic through tholeiitic shield-stage development of Kïlauea volcano, Hawai’i","interactions":[],"lastModifiedDate":"2019-10-10T07:08:06","indexId":"70205909","displayToPublicDate":"2002-10-09T14:30:22","publicationYear":"2002","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Submarine alkalic through tholeiitic shield-stage development of Kïlauea volcano, Hawai’i","docAbstract":"<p><span>The submarine Hilina region exposes a succession of magma compositions spanning the juvenile \"Lō‘ihi\" through tholeiitic shield stages of Kïlauea volcano. Early products, preserved as glass grains and clasts in volcaniclastic rocks of the 3000 m deep Hilina bench, include nephelinite, basanite, phonotephrite, hawaiite, alkali basalt, transitional basalt, and rare alkali-poor Mauna Loa-like tholeiite. Transitional basalt pillow lavas overlie the volcaniclastic section and record an early phase of subsequent subalkaline magmatism. Rare degassed tholeiitic pillow lava and talus above the volcaniclastic section are products of subaerial shield volcanism. Major and trace element variations of clasts and pillow lavas point to a factor of 2 - 2.5 increase in degree of melting from juvenile alkalic to modern tholeiitic Kïlauea. Progressive changes in element ratios that distinguish Hawaiian shield volcanoes, without commensurate changes in elements fractionated by partial melting, also signal increased contributions from Mauna Loa-type source regions as Kïlauea matured from its juvenile alkalic to its tholeiitic shield stage. Ancestral Kïlauea basanites and nephelinites were not primitive magmas but might have evolved from plume-derived alkali picritic parents by lithospheric- level crystallization differentiation, or solidification and remelting, involving pyroxene and garnet, similar to the subcrustal differentiation origin of hawaiites [Frey et al, 1990]. Low magmatic productivity early in Kïlauea’s history sustained a poorly integrated trans-lithospheric conduit system in which magmas stalled and differentiated, producing evolved hawaiites, nephelinites, and basanites. This contrasts with shield-stage Kïlauea where high magmatic productivity flushes the conduit system and delivers primitive magmas to shallow levels.&nbsp;</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian volcanoes: Deep underwater perspectives","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/GM128p0193","issn":"9781118668436 ","isbn":"9780875909875","usgsCitation":"Sisson, T.W., Lipman, P.W., and Naka, J., 2002, Submarine alkalic through tholeiitic shield-stage development of Kïlauea volcano, Hawai’i, v. 128, 27 p., https://doi.org/10.1029/GM128p0193.","productDescription":"27 p.","startPage":"193","endPage":"219","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368180,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kïlauea volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.16666666666666,19.25 ], [ -155.16666666666666,19.5 ], [ -154.91666666666666,19.5 ], [ -154.91666666666666,19.25 ], [ -155.16666666666666,19.25 ] ] ] } } ] }","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sisson, Thomas W. 0000-0003-3380-6425 tsisson@usgs.gov","orcid":"https://orcid.org/0000-0003-3380-6425","contributorId":2341,"corporation":false,"usgs":true,"family":"Sisson","given":"Thomas","email":"tsisson@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":772833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naka, J.","contributorId":47540,"corporation":false,"usgs":true,"family":"Naka","given":"J.","email":"","affiliations":[],"preferred":false,"id":772834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205908,"text":"70205908 - 2002 -  Introduction to section 2 climax-stage magmatism: Growth history of Kïlauea volcano and its instability","interactions":[],"lastModifiedDate":"2019-10-10T07:10:09","indexId":"70205908","displayToPublicDate":"2002-10-09T14:20:10","publicationYear":"2002","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":" Introduction to section 2 climax-stage magmatism: Growth history of Kïlauea volcano and its instability","docAbstract":"<p>No abstract available.&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hawaiian volcanoes: Deep underwater perspectives, volume 128","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Geophysical Union","doi":"10.1029/GM128","issn":"9781118668436 ","isbn":"9780875909875","usgsCitation":"Lipman, P.W., 2002,  Introduction to section 2 climax-stage magmatism: Growth history of Kïlauea volcano and its instability, v. 128, 2 p., https://doi.org/10.1029/GM128.","productDescription":"2 p.","startPage":"103","endPage":"104","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":368179,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kïlauea volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.16666666666666,19.25 ], [ -155.16666666666666,19.5 ], [ -154.91666666666666,19.5 ], [ -154.91666666666666,19.25 ], [ -155.16666666666666,19.25 ] ] ] } } ] }","volume":"128","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":772831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70128349,"text":"70128349 - 2002 - Effects of water use diversion regulation and conservation on sediemtn transport with comparisons from the United States","interactions":[],"lastModifiedDate":"2017-12-15T15:02:51","indexId":"70128349","displayToPublicDate":"2002-10-07T14:47:00","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Effects of water use diversion regulation and conservation on sediemtn transport with comparisons from the United States","docAbstract":"Too much sediment and too little water are related problems in China’s Yellow River Basin. Sediment yield in the basin averages about 2,100 t/(km<sup>2</sup>·a), greatest is of the world’s large rivers although the Yellow River ranks 31st in mean flow. A quarter of the sediment deposited in the 780-km lower reach, causing bed levels to rise an average of a meter per decade wang and other. Sediment aggradation along this reach is concentrated between dikes, resulting in average river-bed elevations 5 m higher, and at Xinxiang as much as 10 m higher, than surrounding bottomlands. The dikes, which have breached nearly 1,600 times in the last 24 centuries, reduce the threat of flooding for 85-million people on 120,000 km<sup>2</sup> in five provinces of northeastern China (Decun, undated). This paper addresses some environmental and social factors related to this problem, and provides descriptions of two United States rivers that exhibit some analogous responses, albeit not to the extent of those associated with the Yellow River, “China’s Sorrow”.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the International Soil Conservation Organization, May 27-31, Beijing","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","usgsCitation":"Gray, J.R., Osterkamp, W., and Jianhua, X., 2002, Effects of water use diversion regulation and conservation on sediemtn transport with comparisons from the United States, <i>in</i> Proceedings of the International Soil Conservation Organization, May 27-31, Beijing, v. II, p. 555-569.","productDescription":"15 p.","startPage":"555","endPage":"569","costCenters":[],"links":[{"id":295062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295061,"type":{"id":15,"text":"Index Page"},"url":"https://tucson.ars.ag.gov/isco/isco12/volume_2.html"}],"country":"China","otherGeospatial":"Yellow River","volume":"II","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"543500a4e4b0a4f4b46a2389","contributors":{"authors":[{"text":"Gray, J. R.","contributorId":46025,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":502912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osterkamp, W. R.","contributorId":67432,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W. R.","affiliations":[],"preferred":false,"id":502913,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jianhua, Xu","contributorId":95407,"corporation":false,"usgs":true,"family":"Jianhua","given":"Xu","email":"","affiliations":[],"preferred":false,"id":502914,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}