{"pageNumber":"2384","pageRowStart":"59575","pageSize":"25","recordCount":68846,"records":[{"id":70047677,"text":"70047677 - 1974 - Digital-model study of ground-water hydrology, Columbia Basin Irrigation Project Area, Washington","interactions":[],"lastModifiedDate":"2013-08-19T10:53:50","indexId":"70047677","displayToPublicDate":"2013-01-01T10:24:04","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":148,"text":"Water Supply Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"40","title":"Digital-model study of ground-water hydrology, Columbia Basin Irrigation Project Area, Washington","docAbstract":"Since 1952 water diverted from the Columbia River at Grand Coulee Dam has been used to irrigate parts of the Columbia Basin Irrigation Project area in eastern Washington, and as a result ground-water levels generally have risen in the area. The rapid increases in ground-water inflow, outflow, and storage from irrigation have created a need for a better understanding of the ground-water system before and after the start of irrigation to establish guidelines necessary for management of the area's ground-water resource. Data and information from previous geologic and hydrologic studies were used as a basis for quantitative analyses of ground-water inflow and outflow by means of digital computer models representing three major areas--Quincy Basin, Pasco Basin, and Royal Slope.","language":"English","publisher":"Washington State Department of Ecology","publisherLocation":"Olympia, WA","collaboration":"Prepared in cooperation with U.S. Geological Survey","usgsCitation":"Tanaka, H., Hansen, A.J., and Skrivan, J., 1974, Digital-model study of ground-water hydrology, Columbia Basin Irrigation Project Area, Washington: Water Supply Bulletin 40, iv, 60 p.","productDescription":"iv, 60 p.","numberOfPages":"75","costCenters":[],"links":[{"id":276743,"type":{"id":11,"text":"Document"},"url":"https://www.ecy.wa.gov/programs/eap/wsb/pdfs/WSB_40_Book.pdf"},{"id":276744,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047677.JPG"}],"country":"United States","state":"Washington","otherGeospatial":"Columbia Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125.0,45.0 ], [ -125.0,49.0 ], [ -117.0,49.0 ], [ -117.0,45.0 ], [ -125.0,45.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e32e4b0b08f446198c9","contributors":{"authors":[{"text":"Tanaka, H.H.","contributorId":30610,"corporation":false,"usgs":true,"family":"Tanaka","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":482700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, A. J. Jr.","contributorId":29840,"corporation":false,"usgs":true,"family":"Hansen","given":"A.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":482699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Skrivan, J.A.","contributorId":107743,"corporation":false,"usgs":true,"family":"Skrivan","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":482701,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047713,"text":"70047713 - 1974 - The availability of water in the Little Lost River Basin, Idaho","interactions":[{"subject":{"id":52641,"text":"ofr67268 - 1967 - A reexamination of water yield in the Little Lost River basin, Idaho","indexId":"ofr67268","publicationYear":"1967","noYear":false,"title":"A reexamination of water yield in the Little Lost River basin, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70047713,"text":"70047713 - 1974 - The availability of water in the Little Lost River Basin, Idaho","indexId":"70047713","publicationYear":"1974","noYear":false,"title":"The availability of water in the Little Lost River Basin, Idaho"},"id":1}],"lastModifiedDate":"2022-02-28T17:25:02.955253","indexId":"70047713","displayToPublicDate":"2013-01-01T10:17:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":141,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"37","title":"The availability of water in the Little Lost River Basin, Idaho","docAbstract":"The Little Lost River basin, an elongated, northwest trending structurally formed intermontane valley, drains an area of about 900 square miles into a closed depression near the northwestern edge of the Snake River Plain. Runoff from snowmelt and rainfall on the Lost River Range on the west and the Lemhi Range on the east maintains the flow of the Little Lost River, and recharges the ground-water reservoir, Both mountain ranges are complexly faulted and are underlain by a variety of rocks, dominantly limestone, of Paleozoic age The principal aquifers are highly transmissive alluvial fill in the middle and upper valley and alluvial fill interfingered with basalt in the southernmost part of the valley.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with ldaho Department of Water Resources","usgsCitation":"Clebsch, A., Waite, H., and Decker, S., 1974, The availability of water in the Little Lost River Basin, Idaho: Water Information Bulletin 37, vii, 60 p.; Maps: 2 Sheets.","productDescription":"vii, 60 p.; Maps: 2 Sheets","numberOfPages":"70","costCenters":[],"links":[{"id":276797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047713.JPG"},{"id":396567,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://idwr.idaho.gov/wp-content/uploads/sites/2/publications/wib37-little-lost-river-basin.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52148fe6e4b06d85e08fb528","contributors":{"authors":[{"text":"Clebsch, Alfred Jr.","contributorId":27886,"corporation":false,"usgs":true,"family":"Clebsch","given":"Alfred","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":482788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waite, H.A.","contributorId":58336,"corporation":false,"usgs":true,"family":"Waite","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":482789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Decker, S.O.","contributorId":101692,"corporation":false,"usgs":true,"family":"Decker","given":"S.O.","email":"","affiliations":[],"preferred":false,"id":482790,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047243,"text":"70047243 - 1974 - A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area","interactions":[],"lastModifiedDate":"2013-07-26T10:18:59","indexId":"70047243","displayToPublicDate":"2013-01-01T10:07:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":301,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"38","title":"A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area","docAbstract":"Direct-current resistivity soundings and exploratory drilling suggest that the basalt of the Snake River Group is relatively thin in the area along the Snake River that is topographically suitable for pumping large quantities of ground water in exchange for surface water. The formations underlying the Snake River Group appear to have low permeability and probably would not yield large amounts of water. Previous studies have indicated that the southern edge of the Snake Plain aquifer extended to the Snake River. Data presented in this report implies that, in general, the southern boundary should, in fact, be several miles north of the river.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise City, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with the Idaho Department of Water Resources","usgsCitation":"Crosthwaite, E., 1974, A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area: Water Information Bulletin 38, iv, 25 p.","productDescription":"iv, 25 p.","numberOfPages":"30","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047243.png"},{"id":275426,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib38-lake_walcott-bonanza_lake.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake Plain Aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a62e4b0a32220222f56","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":481486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047240,"text":"70047240 - 1974 - Application of digital modeling to the prediction of radioisotope migration in ground water","interactions":[],"lastModifiedDate":"2013-07-26T10:00:20","indexId":"70047240","displayToPublicDate":"2013-01-01T09:24:00","publicationYear":"1974","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Application of digital modeling to the prediction of radioisotope migration in ground water","docAbstract":"Recently developed numerical techniques have been adapted to the solution of transient radioactive solute migration problems in groundwater.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Isotope Techniques in Groundwater Hydrology","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"IAEA","usgsCitation":"Robertson, J., 1974, Application of digital modeling to the prediction of radioisotope migration in ground water, <i>in</i> Isotope Techniques in Groundwater Hydrology, v. 2, p. 451-478.","productDescription":"28 p.","startPage":"451","endPage":"478","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275423,"type":{"id":11,"text":"Document"},"url":"https://www-naweb.iaea.org/napc/ih/documents/IAEA%20Symposia/W-04%20Proc%20Symposium%201974%20Vol%20II%20Isotope%20Techniques%20in%20gw%20hydrology%201974.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a64e4b0a32220222f69","contributors":{"authors":[{"text":"Robertson, J.B.","contributorId":85173,"corporation":false,"usgs":true,"family":"Robertson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":481484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045954,"text":"70045954 - 1974 - Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana","interactions":[],"lastModifiedDate":"2013-07-08T10:48:55","indexId":"70045954","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana","docAbstract":"Chemical analyses of water samples from 296 wells in the Red River alluvial aquifer indicate that the ground water in the valley is generally hard (more than 120 milligrams per liter) and has a high iron concentration (greater than 6,000 micrograms per liter). The predominant ions found in the water were calcium and bicarbonate. However, in places in the vicinity of Natchitoches, saline water, probably from underlying formations, has infiltrated the aquifer and sodium and chloride are the principal constituents.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70045954","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the  U.S. Army Corps of Engineers","usgsCitation":"Ludwig, A.H., 1974, Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana: Open-File Report, ii, 7, A3, B3, C3, D2, E2, F2, G4, H4, I4, J2 p., https://doi.org/10.3133/70045954.","productDescription":"ii, 7, A3, B3, C3, D2, E2, F2, G4, H4, I4, J2 p.","startPage":"1","endPage":"J2","numberOfPages":"67","costCenters":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"links":[{"id":272263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045954/report-thumb.jpg"},{"id":274512,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-1.pdf"},{"id":274511,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045954/report.pdf"},{"id":274513,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-2.pdf"},{"id":274514,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-3.pdf"},{"id":274515,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-4.pdf"},{"id":274516,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-5.pdf"},{"id":274517,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-6.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0,28.93 ], [ -94.0,33.0 ], [ -88.82,33.0 ], [ -88.82,28.93 ], [ -94.0,28.93 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dbdf73e4b0f81004b77da2","contributors":{"authors":[{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":478598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043778,"text":"70043778 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","interactions":[{"subject":{"id":16125,"text":"ofr74137 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver counties, Utah","indexId":"ofr74137","publicationYear":"1974","noYear":false,"title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043778,"text":"70043778 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","indexId":"70043778","publicationYear":"1974","noYear":false,"title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-10T15:21:08","indexId":"70043778","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"47","title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","docAbstract":"The Wah Wah Valley drainage basin is an area of about 600 square miles (1,550 km<sup>2</sup>) in Millard and Beaver Counties in southwestern Utah. Surface-water supplies of the area are negligible--total runoff averages about 7,800 acre-feet (9.62 hm<sup>3</sup>) annually, all streams are ephemeral or intermittent, and surface storage is negligible. Evaporation and transpiration within the basin consume more than 97 percent of total annual precipitation. There is no surface outflow.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Stephens, J.C., 1974, Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah: Technical Publication 47, v, 53 p.","productDescription":"v, 53 p.","numberOfPages":"60","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267803,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331871,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-220"},{"id":267802,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200099.pdf"}],"country":"United States","state":"Utah","county":"Beaver County, Millard County","otherGeospatial":"Wah Wah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.97766113281249,\n              38.14751758025121\n            ],\n            [\n              -113.97766113281249,\n              38.886757140695906\n            ],\n            [\n              -113.2470703125,\n              38.886757140695906\n            ],\n            [\n              -113.2470703125,\n              38.14751758025121\n            ],\n            [\n              -113.97766113281249,\n              38.14751758025121\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad45e4b0b6328103b44e","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":474227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046284,"text":"70046284 - 1974 - Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, Georgia","interactions":[{"subject":{"id":46059,"text":"ofr7179 - 1971 - Maps of Gordon, Whitfield, and Murray counties, Georgia, showing geology and location of wells and springs","indexId":"ofr7179","publicationYear":"1971","noYear":false,"title":"Maps of Gordon, Whitfield, and Murray counties, Georgia, showing geology and location of wells and springs"},"predicate":"SUPERSEDED_BY","object":{"id":70046284,"text":"70046284 - 1974 - Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, Georgia","indexId":"70046284","publicationYear":"1974","noYear":false,"title":"Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, 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,{"id":70038681,"text":"wdrCA7312 - 1974 - Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA7312","displayToPublicDate":"2012-06-04T10:44:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-73-1-2","title":"Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"Surface-water records for the 1973 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report, Records for a few pertinent gaging stations in bordering States also are included, The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Lee R. Peterson, district chief. These data represent that portion of the National Water Data System collected by the Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA7312","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-73-1-2, xiv, 523 p., https://doi.org/10.3133/wdrCA7312.","productDescription":"xiv, 523 p.","startPage":"511","endPage":"1033","costCenters":[],"links":[{"id":257515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_73_1_2.jpg"},{"id":257492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/ca-73/WDR-1973-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc957e4b08c986b32cce3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535194,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038245,"text":"70038245 - 1974 - Water resources inventory of Connecticut Part 5: lower Housatonic River basin","interactions":[],"lastModifiedDate":"2014-06-26T15:00:35","indexId":"70038245","displayToPublicDate":"2012-04-22T14:28:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"19","title":"Water resources inventory of Connecticut Part 5: lower Housatonic River basin","docAbstract":"<p>The 557 square miles of the lower Housatonic River basin in western Connecticut include the basins of two major tributaries, the Pomperaug and Naugatuck Rivers. Nearly all water is derived from precipitation, which averaged 47 inches per year during 1931-60, In this period an additional 570 billion gallons of water per year entered the basin in the main stem of the Housatonic River at Lake Lillinonah, and some water was imported by water-supply systems from outside the basin. Almost half the precipitation--21.6 inches--was lost from the basin by evapotranspiration. Except for small amounts exported, the remainder discharged as runoff and underflow into Long Island Sound.  </p>\n<br/>\n<p>Variations in streamflow at 6 long-term continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean flow and two low-flow characteristics, the 7-day annual minimum flow for 2-year and 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.</p>\n<br/>\n<p>Of the 37 principal lakes, ponds, and reservoirs in the basin, 6 have usable storage of more than 1 billion gallons. The “maximum safe draft rate” (described in: “Storage of Water in Lakes and Reservoirs”) of the largest of these, Thomaston Reservoir near Thomaston, is 75.6 million gallons per day for the 10-year and 20-year recurrence intervals of annual lowest mean flow.</p>\n<br/>\n<p>Floods have occurred during every month, at one time or another. The two greatest floods on the Naugatuck River in historical time occurred 2 months apart in 1955. The larger, in August, had a peak of 106,000 cfs (cubic feet per second) at Beacon Falls. Since then, the likelihood of major floods has been considerably reduced by a program of flood control in the basin.</p>\n<br/>\n<p>Water can be obtained from three aquifers under-lying the basin-stratified drift, till, and bedrock. Stratified drift covers about 16 percent of the basin, mostly in valleys and lowlands, and its saturated part generally ranges in thickness from 10 feet in small valleys to 200 feet in the Housatonic River valley. Its transmissivity ranges from 0 to 47,000 ft<sup>2</sup>/day (feet shared per day). Till, deposited directly by glacial ice, forms a widespread but discontinuous mantle over bedrock in most upland areas and extends beneath stratified drift in lowlands; it ranges in thickness from 0 to 200 feet. The median value of 31 published determinations of hydraulic conductivity of till in southern New England is 0.67 ft/day and ranges from 0.013 to 29 ft/day. Crystalline bedrock underlies most of the basin and is composed principally of granite, gneiss, and schist. Sedimentary volcanic bedrock underlies only the Pomperaug River basin. Regardless of rock type, water is obtained mostly from fractures. </p>\n<br/>\n<p>Streambed deposits are significant features of the hydrogeologic system because they affect the amount of water from streams and lakes that can be induced to infiltrate aquifers. Based on field tests, characteristic values of vertical hydraulic conductivity of streambed deposits are 0.40 ft/day for fine-grained deposits and 14 ft/day for gravelly deposits.</p>\n<br/>\n<p>Ground-water supplies generally range in yield from several millions of gallons per day from large well fields to 1 gpm (gallons per minute) from single wells. Large supplies, with yields of 100 gpm or more from individual wells, are most commonly obtained from stratified drift. Yields to be expected from screened wells tapping this aquifer can be calculated by use of a series of graphs in conjunction with estimates of transmissivity and aquifer thickness.</p>\n<br/>\n<p>The yields of 14 principal ground-water reservoirs are estimated from aquifer characteristics and also from the amount of water that can be obtained from aquifer storage, from interception or runoff, and from infiltration of streamflow at low-flow conditions, using a hypothetical well-field arrangement for each reservoir. It is assumed that induced infiltration is restricted to an amount equal to the 7-day annual minimum stream-flow for a 2-year recurrence interval. Yields range from 1.4 to 15 mgd (million gallons per day) during periods of no recharge, and from 2.0 to 17 mgd during recharge periods.</p>\n<br/>\n<p>Small to moderate water supplies can be obtained from any of the aquifers under suitable conditions. For example, data from 294 wells in the basin indicate that yields of a few gallons per minute can be obtained from bedrock at most sites. The likelihood of obtaining an adequate domestic supply is slightly greater in granite than in schist and also is greater where the overburden is stratified drift rather than till.</p>\n<br/>\n<p>Chemical analyses of precipitation samples collected monthly from five stations in the basin during a 9-month period in 1966 show that rainfall is acidic and that sulfate is the dominant anion, probably because of industrial fumes and smoke within and near the basin.</p>\n<br/>\n<p>Where unaffected by man’s activities, water in the basin is generally low in dissolved-solids concentration, is of the calcium magnesium bicarbonate type, and is soft to moderately hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streamflow becomes more highly mineralized during low-flow conditions, when most of it consists of more highly mineralized water discharged from aquifers. The median value of dissolved-solids concentration of water at 22 stream sites was 51 mg/1 (milligrams per liter) during high flow, and 68 mg/1 during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in parts of the basin, particularly in streams draining swamps and in water from bedrock containing iron and manganese-bearing minerals.</p>\n<br/>\n<p>Man’s activities have degraded the quality of water in streams in much of the basin, except in the Pomperaug subbasin. In the Naugatuck River basin, the degradation in quality is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of certain trace elements, a low dissolved oxygen content, and abnormally high temperatures. Ground water is degraded principally by induced infiltration of stream water containing chemical wastes, by wastes stored on the ground and by effluents from septic tanks.</p>\n<br/>\n<p>Below its confluence with the Naugatuck River, much of the Housatonic River and adjoining marshes, wetlands, and aquifers contain salt water. Measurements of specific conductance during low-flow conditions in 1969 indicate that the dissolved-solids concentration of water in the estuary ranged from 210 mg/1 near Twomile Island to 20,000 mg/1 near Long Island Sound.</p>\n<br/>\n<p>The quantity and quality of water in the basin are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. In 1967, the total amount of water used in the basin was about 194 billion gallons. About 90 percent of this was used for industrial purposes, and 95 percent of the industrial water was obtained from surface-water sources. In the same year, 17 municipal and private water-supply systems supplied water of satisfactory quality to about three-fourths of the population.</p>","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Wilson, W.E., Burke, E.L., and Thomas, C.E., 1974, Water resources inventory of Connecticut Part 5: lower Housatonic River basin: Connecticut Water Resources Bulletin 19, Report: viii, 79 p.; 6 Plates: 28.66 x 40.55 inches and smaller.","productDescription":"Report: viii, 79 p.; 6 Plates: 28.66 x 40.55 inches and smaller","numberOfPages":"85","costCenters":[],"links":[{"id":258805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0019/report.pdf","size":"29327","linkFileType":{"id":1,"text":"pdf"}},{"id":258806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0019/report-thumb.jpg"},{"id":285980,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-a.pdf"},{"id":285981,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-b.pdf"},{"id":285982,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-1.pdf"},{"id":285983,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-2.pdf"},{"id":285984,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-3.pdf"},{"id":285985,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-d.pdf"}],"scale":"125000","country":"United States","state":"Connecticut","otherGeospatial":"Housatonic River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.333333,41.125 ], [ -73.333333,42.0 ], [ -72.9,42.0 ], [ -72.9,41.125 ], [ -73.333333,41.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7be4b08c986b32d693","contributors":{"authors":[{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, Edward L.","contributorId":38398,"corporation":false,"usgs":true,"family":"Burke","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039072,"text":"70039072 - 1974 - Tour guide: John Wesley Powell Federal Building","interactions":[],"lastModifiedDate":"2012-08-10T01:01:49","indexId":"70039072","displayToPublicDate":"2012-01-01T14:38:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Tour guide: John Wesley Powell Federal Building","docAbstract":"Data from 5,594 samples collected from 1931 through 2006 were used to describe naturally occurring fluoride concentrations in freshwater aquifers in Louisiana. Statistical analyses were used to summarize fluoride concentrations in the aquifers.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039072","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Tour guide: John Wesley Powell Federal Building: General Information Product, 15 p., https://doi.org/10.3133/70039072.","productDescription":"15 p.","numberOfPages":"16","costCenters":[{"id":410,"text":"National Center","active":false,"usgs":true}],"links":[{"id":261291,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039072/report.pdf"},{"id":261292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039072/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.61666666666666,38.75 ], [ -77.61666666666666,39.11666666666667 ], [ -77.11666666666666,39.11666666666667 ], [ -77.11666666666666,38.75 ], [ -77.61666666666666,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb5a5e4b08c986b3267e6","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039202,"text":"70039202 - 1974 - New activities at the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2017-05-19T18:47:24","indexId":"70039202","displayToPublicDate":"2012-01-01T11:41:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"New activities at the U.S. Geological Survey","docAbstract":"As the Nation's principal source of information about the configuration of the land surface, the composition and structure of the rocks at and beneath the surface, the distribution and character of its energy, mineral, and water resources, and the nature of natural geologic processes, the U. S. Geological Survey focuses its work on some of the Nation's most critical problems. As the Survey tackles new problems with new techniques, it is fully aware of the resource needs and environmental pressures of an expanding economy and growing population.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039202","usgsCitation":"McKelvey, V., 1974, New activities at the U.S. Geological Survey: General Information Product, 6 p. (11 columns), https://doi.org/10.3133/70039202.","productDescription":"6 p. (11 columns)","costCenters":[],"links":[{"id":261370,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039202/report.pdf"},{"id":261371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039202/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a654ee4b0c8380cd72b63","contributors":{"authors":[{"text":"McKelvey, Vincent E.","contributorId":106637,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent E.","affiliations":[],"preferred":false,"id":465771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039200,"text":"70039200 - 1974 - Studying the Earth from space","interactions":[],"lastModifiedDate":"2017-05-19T18:48:11","indexId":"70039200","displayToPublicDate":"2012-01-01T11:17:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Studying the Earth from space","docAbstract":"Pictures of the Earth's surface obtained from satellites are providing scientists with new tools to investigate tne Earth and its environment. A growing population and an everexpanding technology place demands on our natural resources. However, man can no longer treat his resources strictly according to immediate economic dictates; a balance must be struck between the short-term demands of technological and industrial development and the long-term effects on the environment. Intelligent development, management, and conservation of resources are goals that represent an unprecedented challenge in the acquisition and use of information.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039200","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Studying the Earth from space: General Interest Publication, 19 p., https://doi.org/10.3133/70039200.","productDescription":"19 p.","numberOfPages":"20","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261366,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039200/report.pdf"},{"id":261367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039200/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ce9e4b08c986b31d515","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040602,"text":"70040602 - 1974 - Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York","interactions":[],"lastModifiedDate":"2012-11-02T13:43:22","indexId":"70040602","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ARB-2","title":"Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Frimpter, M., 1974, Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York: Basin Planning Report ARB-2, 98 p.","productDescription":"98 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5094ebc6e4b0e5cfc2acdcd1","contributors":{"authors":[{"text":"Frimpter, M. H.","contributorId":34127,"corporation":false,"usgs":true,"family":"Frimpter","given":"M. H.","affiliations":[],"preferred":false,"id":468660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040712,"text":"70040712 - 1974 - Ground-water resources of the western Oswego River basin, New York","interactions":[],"lastModifiedDate":"2012-11-13T12:49:40","indexId":"70040712","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ORB-5","title":"Ground-water resources of the western Oswego River basin, New York","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Crain, L., 1974, Ground-water resources of the western Oswego River basin, New York: Basin Planning Report ORB-5, 137 p.; 3 Plates in 4 Sheets.","productDescription":"137 p.; 3 Plates in 4 Sheets","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263108,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a3ba6ee4b0855e233c074e","contributors":{"authors":[{"text":"Crain, L.J.","contributorId":70829,"corporation":false,"usgs":true,"family":"Crain","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":468858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046328,"text":"wdrNM731 - 1974 - Water resources data for New Mexico, water year 1973; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:54:41","indexId":"wdrNM731","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-73-1","title":"Water resources data for New Mexico, water year 1973; Part 1. Surface water records","docAbstract":"Surface-water records for the 1973 calendar year for New Mexico, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a 'few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the US. Geological Survey under the direction of W. E. Hale, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico. Through September 30, 1960, the records of discharge and stage of streams and canals and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water supply papers entitled \"Surface Water Supply of the United States\" Beginning with the 1961 water year, surface-water records have been released by the Geological Survey in annual reports on a State boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. The discharge and reservoir storage records for 1961-65 also are published in a Geological Survey water supply paper series entitled \"Surface Water Supply of the United States 1961-65.\" There will be a similar series of water-supply papers for the water years 1966-70.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM731","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for New Mexico, water year 1973; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-73-1, 250 p., https://doi.org/10.3133/wdrNM731.","productDescription":"250 p.","costCenters":[],"links":[{"id":273457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274526,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/nm-73/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300ebe4b01368e589e42f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039048,"text":"70039048 - 1974 - Abstracting and indexing guide","interactions":[],"lastModifiedDate":"2012-07-18T01:01:44","indexId":"70039048","displayToPublicDate":"2011-07-17T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":47,"text":"Monograph","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"501","subseriesTitle":"Water Resources Scientific Information Center","title":"Abstracting and indexing guide","docAbstract":"These instructions have been prepared for those who abstract and index scientific and technical documents for the Water Resources Scientific Information Center (WRSIC). With the recent publication growth in all fields, information centers have undertaken the task of keeping the various scientific communities aware of current and past developments. An abstract with carefully selected index terms offers the user of WRSIC services a more rapid means for deciding whether a document is pertinent to his needs and professional interests, thus saving him the time necessary to scan the complete work. These means also provide WRSIC with a document representation or surrogate which is more easily stored and manipulated to produce various services. Authors are asked to accept the responsibility for preparing abstracts of their own papers to facilitate quick evaluation, announcement, and dissemination to the scientific community.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Department of the Interior, and Office of Water Resources Research, 1974, Abstracting and indexing guide (Revised): Monograph 501, iii, 13 p.; Appendices.","productDescription":"iii, 13 p.; Appendices","numberOfPages":"47","costCenters":[{"id":635,"text":"Water Resources Scientific Information Center","active":false,"usgs":true}],"links":[{"id":261285,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fedgov/70039048/report.pdf"},{"id":261286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fedgov/70039048/report-thumb.jpg"}],"edition":"Revised","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e64ee4b0c8380cd47332","contributors":{"authors":[{"text":"U.S. Department of the Interior","contributorId":127996,"corporation":true,"usgs":false,"organization":"U.S. Department of the Interior","id":535209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Office of Water Resources Research","contributorId":128060,"corporation":true,"usgs":false,"organization":"Office of Water Resources Research","id":535210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70001287,"text":"70001287 - 1974 - Obsidian hydration profile measurements using a nuclear reaction technique","interactions":[],"lastModifiedDate":"2021-01-04T14:12:17.595409","indexId":"70001287","displayToPublicDate":"2010-09-28T23:09:33","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Obsidian hydration profile measurements using a nuclear reaction technique","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>AMBIENT water diffuses into the exposed surfaces of obsidian, forming a hydration layer which increases in thickness with time to a maximum depth of 20–40 µm (ref. 1), this layer being the basic foundation of obsidian dating<sup>2,3</sup>.</p></div></div>","language":"English","publisher":"Nature","doi":"10.1038/250044a0","issn":"00280836","usgsCitation":"Lee, R., Leich, D., Tombrello, T., Ericson, J., and Friedman, I., 1974, Obsidian hydration profile measurements using a nuclear reaction technique: Nature, v. 250, no. 5461, p. 44-47, https://doi.org/10.1038/250044a0.","productDescription":"4 p.","startPage":"44","endPage":"47","costCenters":[],"links":[{"id":203399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"250","issue":"5461","noUsgsAuthors":false,"publicationDate":"1974-07-01","publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6963ed","contributors":{"authors":[{"text":"Lee, R.R.","contributorId":18090,"corporation":false,"usgs":true,"family":"Lee","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":346712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leich, D.A.","contributorId":84054,"corporation":false,"usgs":true,"family":"Leich","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":346714,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tombrello, T.A.","contributorId":13232,"corporation":false,"usgs":true,"family":"Tombrello","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":346711,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ericson, J.E.","contributorId":77643,"corporation":false,"usgs":true,"family":"Ericson","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":346713,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":346715,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70000782,"text":"70000782 - 1974 - Measurement in a marine environment using low cost sensors of temperature and dissolved oxygen","interactions":[],"lastModifiedDate":"2021-01-15T13:49:55.212436","indexId":"70000782","displayToPublicDate":"2010-09-28T23:09:29","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1228,"text":"Chesapeake Science","active":true,"publicationSubtype":{"id":10}},"title":"Measurement in a marine environment using low cost sensors of temperature and dissolved oxygen","docAbstract":"<p>Continuous records of physical parameters of the marine environment are difficult as well as expensive to obtain. This paper describes preliminary results of an investigative program with the purpose of developing low cost time integrating measurement and averaging devices for water temperature and dissolved oxygen.</p><p>Measurements were made in an estuarine area of the Chesapeake Bay over two week periods. With chemical thermometers average water temperature for the two week period was found to be equal to average water temperature measured with thermocouples plus or minus 1.0 C. The slow diffusion of oxygen through the semipermiable sides of plastic bottles permitted the use of water filled bottles to obtain averaged oxygen measurements.</p><p>Oxygen measurements for two week averaging times using 500 ml polyethylene bottles were found to vary from conventionally measured and averaged dissolved oxygen by about 1.8 mg/l.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02688849","issn":"15592723","usgsCitation":"Godshall, F., Cory, R.L., and Phinney, D., 1974, Measurement in a marine environment using low cost sensors of temperature and dissolved oxygen: Chesapeake Science, v. 15, no. 3, p. 178-181, https://doi.org/10.1007/BF02688849.","productDescription":"4 p.","startPage":"178","endPage":"181","costCenters":[],"links":[{"id":203473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Chesapeake Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.47558593749999,\n              37.020098201368114\n            ],\n            [\n              -75.234375,\n              37.020098201368114\n            ],\n            [\n              -75.234375,\n              40.34654412118006\n            ],\n            [\n              -77.47558593749999,\n              40.34654412118006\n            ],\n            [\n              -77.47558593749999,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610fd0","contributors":{"authors":[{"text":"Godshall, F.A.","contributorId":48290,"corporation":false,"usgs":true,"family":"Godshall","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":346529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cory, R. L.","contributorId":49456,"corporation":false,"usgs":true,"family":"Cory","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":346530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phinney, D.E.","contributorId":84484,"corporation":false,"usgs":true,"family":"Phinney","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":346531,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221029,"text":"5221029 - 1974 - The status of the light-footed clapper rail","interactions":[],"lastModifiedDate":"2012-02-02T00:14:40","indexId":"5221029","displayToPublicDate":"2010-06-16T12:17:58","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":708,"text":"American Birds","active":true,"publicationSubtype":{"id":10}},"title":"The status of the light-footed clapper rail","docAbstract":"Only 12 California marsh areas are presently believed to be inhabited by the Light-footed Clapper Rail, and eight of these appear to support only 5-15 birds apiece.  Tentative estimates for the other four are: Anaheim Bay 200, Upper Newport 30-35, Los Penasquitos 30, and Tijuana Estuary 150.  These estimates, admittedly very rough, indicate a total Light-footed Rail population on only about 500 birds.  Recognizing that rails are secretive and hard to inventory, the actual count could be somewhat higher, but I feel it is most unlikely that the number could be more than 750 birds altogether.  Reductions in Light-footed Clapper Rail populations can be attributed almost entirely to loss of habitat.  An estimated 26,000 acres of saltmarsh once existed between Santa Barbara and the Mexican border.  At present there are approximately 8500 acres, much of which has been degraded by pollution, water diversion, and restriction of tidal flow.  Of those areas currently occupied by Clapper Rails, few can be considered to have a very secure future.  Of the four major areas only Anaheim Bay appears to be relatively safe from future habitat destruction.  Tijuana Estuary, Los Penasquitos Lagoon, and Upper Newport Bay are all threatened by commercial developments that could reduce or destroy local rail populations.  I have not visited Baja California, but I believe there is still a substantial population of Clapper Rails in the marshes around San Quintin Bay.  Taxonomists do not agree on the subspecific identity of these birds, but some feel they are representatives of the Light-footed race.  If so, it is fortunate to have a relatively secure (for now) reservoir of these birds, but whether the Light-footed Clapper Rail survives within the United States may well be decided within the next few years.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Birds","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Wilbur, S., 1974, The status of the light-footed clapper rail: American Birds, v. 28, no. 5, p. 868-870.","productDescription":"868-870","startPage":"868","endPage":"870","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5349","contributors":{"authors":[{"text":"Wilbur, S.R.","contributorId":53908,"corporation":false,"usgs":true,"family":"Wilbur","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":332897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220965,"text":"5220965 - 1974 - Range expansion and population increase of the gadwall in eastern North America","interactions":[],"lastModifiedDate":"2012-02-02T00:14:40","indexId":"5220965","displayToPublicDate":"2010-06-16T12:17:57","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"Range expansion and population increase of the gadwall in eastern North America","docAbstract":"A disjunct breeding population of Gadwall in eastern North America was first recorded in 1939 This population has extended its range during recent years to the point where it is now found breeding in more than thirty locations (primarily National Wildlife Refuges and Wildlife Management Areas). These are 1,600-2,000 km (1,000-1,200 miles) from the main breeding range in the west and midwest. The number of breeding birds and the harvest have both increased during the last decade. Approximately 40,000 Gadwall were harvested in the northern portion of the Atlantic Flyway between 1961 and 1970. The impoundment of water seems to be responsible for the increase, providing focal points for nesting activities,","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildfowl","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Henny, C.J., and Holgersen, N., 1974, Range expansion and population increase of the gadwall in eastern North America: Wildfowl, v. 25, p. 95-101.","productDescription":"95-101","startPage":"95","endPage":"101","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649500","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holgersen, N.E.","contributorId":10889,"corporation":false,"usgs":true,"family":"Holgersen","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":332773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5224970,"text":"5224970 - 1974 - Percutaneous absorption of several chemicals, some pesticides included, in the red-winged blackbird","interactions":[],"lastModifiedDate":"2013-03-13T16:06:51","indexId":"5224970","displayToPublicDate":"2010-06-16T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1554,"text":"Environmental Physiology and Biochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Percutaneous absorption of several chemicals, some pesticides included, in the red-winged blackbird","docAbstract":"Percutaneous absorption in vivo through the skin of the feet of the red-winged blackbird (Agelaius phoeniceus) has been investigated.  Absorption after 18-24 hours exposure to 0.01 M solutions of salicylic acid, caffeine, urea, 2,4-D, dieldrin, diethylstilbesterol, and DDT was measured.  Of these, only DDT and diethylstilbesterol were not absorbed to a measurable degree.  The solvents ethanol, dimethylsulfoxide (DMSO), and vegetable oil were compared with water in their effects on the absorption ofcaffeine, urea, and salicylic acid. Ethanol, DMSO,and oil each decreased percutaneous absorption of salicylic acid.  DMSO increased absorption of caffeine, and ethanol had no effect on it. Neither DMSO nor ethanol affected penetration of urea.  Partition coefficients (K) (epidermis/water) were determined for all seven penetrants.  Compounds with higher values of K showed lower percutaneous absorption.  These findings suggest that K may be useful to predict percutaneous absorption in vivo.  It appears unlikely that percutaneous absorption contributes greatly to the body burden of 2,4-D and dieldrin in A. phoeniceus.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Physiology and Biochemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"7119_Rogers.pdf","usgsCitation":"Rogers, J., Cagan, R., and Kare, M., 1974, Percutaneous absorption of several chemicals, some pesticides included, in the red-winged blackbird: Environmental Physiology and Biochemistry, v. 4, no. 3, p. 104-111.","productDescription":"104-111","startPage":"104","endPage":"111","numberOfPages":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b41d4","contributors":{"authors":[{"text":"Rogers, J.G. Jr.","contributorId":46651,"corporation":false,"usgs":true,"family":"Rogers","given":"J.G.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":343333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cagan, R.H.","contributorId":65587,"corporation":false,"usgs":true,"family":"Cagan","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":343334,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kare, M.R.","contributorId":31088,"corporation":false,"usgs":true,"family":"Kare","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":343332,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039550,"text":"70039550 - 1974 - The National Center of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-08-11T01:01:52","indexId":"70039550","displayToPublicDate":"2008-01-08T12:52:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The National Center of the U.S. Geological Survey","docAbstract":"In August of 1973, the U. S. Geological Survey moved its first group of employees into the John Wesley Powell Federal Building of its newly constructed National Center at Reston, Virginia. The move signaled the fruition of more than a decade of planning and work to consolidate the agency's widespread activities into one location which could truly serve as a National Center. The Survey's leadership in the natural resources field has been materially strengthened through the availability of the Center's outstanding research and engineering facilities. Also the Center affords important professional and administrative advantages by bringing together the 2,200 Survey employees in the Washington, D.C, metropolitan area.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039550","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, The National Center of the U.S. Geological Survey, 34 p., https://doi.org/10.3133/70039550.","productDescription":"34 p.","numberOfPages":"35","costCenters":[],"links":[{"id":261674,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039550/report.pdf"},{"id":261675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039550/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.36666666666666,38.95 ], [ -77.36666666666666,38.93333333333333 ], [ -77.35,38.93333333333333 ], [ -77.35,38.95 ], [ -77.36666666666666,38.95 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba819e4b08c986b3219eb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010047,"text":"70010047 - 1974 - An Anvilian (early pleistocene) marine fauna from western Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2025-07-11T16:25:08.944253","indexId":"70010047","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"An Anvilian (early pleistocene) marine fauna from western Seward Peninsula, Alaska","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>Cover sediments of the York Terrace exposed near the California River, western Seward Peninsula, Alaska, yield mollusks, ostracodes, and foraminifera that lived during the Anvilian transgression of early Pleistocene age. The fossiliferous sediments lie at the inner edge of the York Terrace, a deformed wave-cut platform that extends eastward from Bering Strait along much of the southern coast of Seward Peninsula. The seaward margin is truncated by the little-deformed Lost River Terrace, carved during the Pelukian (Sangamonian) transgression. The early Pleistocene sediments seem to have been deposited between the first and second of four glaciations for which evidence can be found in the California River area.</p><p>The California River fauna includes several extinct species and several species now confined to areas as remote as the northwestern Pacific and north Atlantic. The fauna probably lived in water temperatures much like those of the present time but deeper water on the Bering Shelf is suggested.</p><p>The presence of an early Pleistocene fauna at the inner edge of the York Terrace at California River shows that the terrace was largely carved before and during early Pleistocene time. However, a marine fauna apparently of middle Pleistocene age is found on the York Terrace near Cassiterite Peak, and this seems to indicate that the terrace remained low until middle Pleistocene time. Uplift of the York Terrace probably was accompanied by uplift of Bering Strait. The strait may have been deeper, and there may have been no land bridge between the Seward Peninsula of Alaksa and the Chukotka Peninsula of Siberia during most of early and middle Pleistocene time.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(74)90039-8","issn":"00335894","usgsCitation":"Hopkins, D., Rowland, R., Echols, R., and Valentine, P.C., 1974, An Anvilian (early pleistocene) marine fauna from western Seward Peninsula, Alaska: Quaternary Research, v. 4, no. 4, p. 441-470, https://doi.org/10.1016/0033-5894(74)90039-8.","productDescription":"30 p.","startPage":"441","endPage":"470","costCenters":[],"links":[{"id":218698,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.00292968749997,\n              64.89558934777301\n            ],\n            [\n              -164.90478515625,\n              64.89558934777301\n            ],\n            [\n              -164.90478515625,\n              65.73965627227945\n            ],\n            [\n              -168.00292968749997,\n              65.73965627227945\n            ],\n            [\n              -168.00292968749997,\n              64.89558934777301\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e9d1e4b0c8380cd48498","contributors":{"authors":[{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":357771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowland, R.W.","contributorId":36153,"corporation":false,"usgs":true,"family":"Rowland","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":357769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Echols, R.E.","contributorId":12186,"corporation":false,"usgs":true,"family":"Echols","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":357768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valentine, P. C.","contributorId":46505,"corporation":false,"usgs":true,"family":"Valentine","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010256,"text":"70010256 - 1974 - Bimodal tholeiitic-dacitic magmatism and the Early Precambrian crust","interactions":[],"lastModifiedDate":"2025-06-25T15:54:00.353372","indexId":"70010256","displayToPublicDate":"2003-04-03T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3112,"text":"Precambrian Research","active":true,"publicationSubtype":{"id":10}},"title":"Bimodal tholeiitic-dacitic magmatism and the Early Precambrian crust","docAbstract":"<p><span>Interlayered plagioclase-quartz gneisses and amphibolites from 2.7 to more than 3.6 b.y. old form much of the basement underlying Precambrian greenstone belts of the world; they are especially well-developed and preserved in the Transvaal and Rhodesian cratons. We postulate that these basement rocks are largely a metamorphosed, volcanic, bimodal suite of tholeiite and high-silica low-potash dacite—compositionally similar to the 1.8-b.y.-old Twilight Gneiss — and partly intrusive equivalents injected into the lower parts of such volcanic piles.</span></p><p>We speculate that magmatism in the Early Precambrian involved higher heat flow and more hydrous conditions than in the Phanerozoic. Specifically, we suggest that the early degassing of the Earth produced a basaltic crust and pyrolitic upper mantle that contained much amphibole, serpentine, and other hydrous minerals. Dehydration of the lower parts of a downgoing slab of such hydrous crust and upper mantle would release sufficient water to prohibit formation of andesitic liquid in the upper part of the slab. Instead, a dacitic liquid and a residuum of amphibole and other silica-poor phases would form, according to Green and Ringwood's experimental results. Higher temperatures farther down the slab would cause total melting of basalt and generation of the tholeiitic member of the suite. This type of magma generation and volcanism persisted until the early hydrous lithosphere was consumed.</p><p>An implication of this hypothesis is that about half the present volume of the oceans formed before about 2.6 b.y. ago.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0301-9268(74)90014-X","issn":"03019268","usgsCitation":"Barker, F., and Peterman, Z.E., 1974, Bimodal tholeiitic-dacitic magmatism and the Early Precambrian crust: Precambrian Research, v. 1, no. 1, p. 1-12, https://doi.org/10.1016/0301-9268(74)90014-X.","productDescription":"12 p.","startPage":"1","endPage":"12","costCenters":[],"links":[{"id":219748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f134e4b0c8380cd4aabe","contributors":{"authors":[{"text":"Barker, F.","contributorId":101368,"corporation":false,"usgs":true,"family":"Barker","given":"F.","affiliations":[],"preferred":false,"id":358465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}