{"pageNumber":"2148","pageRowStart":"53675","pageSize":"25","recordCount":68909,"records":[{"id":70047835,"text":"70047835 - 1981 - Integrated uranium system in the Marysvale volcanic field, west-central Utah","interactions":[{"subject":{"id":16128,"text":"ofr80524 - 1980 - Integrated uranium system in the Marysvale volcanic field, west-central Utah","indexId":"ofr80524","publicationYear":"1980","noYear":false,"title":"Integrated uranium system in the Marysvale volcanic field, west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70047835,"text":"70047835 - 1981 - Integrated uranium system in the Marysvale volcanic field, west-central Utah","indexId":"70047835","publicationYear":"1981","noYear":false,"title":"Integrated uranium system in the Marysvale volcanic field, west-central Utah"},"id":1}],"lastModifiedDate":"2025-09-15T15:29:16.808416","indexId":"70047835","displayToPublicDate":"2013-01-01T14:47:00","publicationYear":"1981","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Integrated uranium system in the Marysvale volcanic field, west-central Utah","docAbstract":"

Uranium in the Marysvale volcanic field is known to occur in several geologic environments and is thought to occur in others. These known and hypothetical occurrences are of various kinds, ranging in derivation from rhyolite magma, through porphyry-type deposits, hydrothermal vein deposits, dispersed hydrothermal deposits, and, after secondary transport in ground and surface water, roll–front or sedimentary–trap deposits in basin-fill sediments. To date, only the hydrothermal vein environment has been productive, but billions of pounds of uranium were available in all other environments, and if proper conditions existed, significant concentrations probably formed by other processes. The intracaldera fill of the Mount Belknap caldera and sediment-filled basins adjoining the Tushar Mountains are especially favorable exploration targets for the undiscovered uranium believed to exist.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Uranium in volcanic and volcaniclastic rocks","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/St13421C11","usgsCitation":"Steven, T.A., Cunningham, C.G., and Machette, M.N., 1981, Integrated uranium system in the Marysvale volcanic field, west-central Utah, chap. of Uranium in volcanic and volcaniclastic rocks, v. 13, p. 111-122, https://doi.org/10.1306/St13421C11.","productDescription":"12 p.","startPage":"111","endPage":"122","costCenters":[],"links":[{"id":277012,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.05,37.0 ], [ -114.05,42.0 ], [ -109.04,42.0 ], [ -109.04,37.0 ], [ -114.05,37.0 ] ] ] } } ] }","volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78e9e4b01458f784295e","contributors":{"authors":[{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":483100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":483101,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Machette, M. N.","contributorId":19561,"corporation":false,"usgs":true,"family":"Machette","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":483099,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70047643,"text":"70047643 - 1981 - Water resources of the Kisatchie well-field area near Alexandria, Louisiana","interactions":[],"lastModifiedDate":"2025-04-02T16:52:44.264495","indexId":"70047643","displayToPublicDate":"2013-01-01T09:47:29","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":147,"text":"Water Resources Technical Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"26","title":"Water resources of the Kisatchie well-field area near Alexandria, Louisiana","docAbstract":"

Sands of Miocene, Pliocene(?), and Pleistocene age contain fresh-water in central Rapides Parish, La. In this area the base of fresh ground water ranges from 900 feet to more than 2,500 feet below National Geodetic Vertical Datum of 1929. The principal sources of water are the Carnahan Bayou, Williamson Creek, and Blounts Creek Members of the Fleming Formation of Miocene and Pliocene(?) age and terrace deposits of Pleistocene age.

","language":"English","publisher":"Louisiana Office of Public Works","publisherLocation":"Baton Rouge, LA","collaboration":"Prepared by United States Department of the Interior, Geological Survey in cooperation with Louisiana Department of Transportation and Development, Office of Public Works","usgsCitation":"Rogers, J.E., 1981, Water resources of the Kisatchie well-field area near Alexandria, Louisiana: Water Resources Technical Report 26, vi, 57 p., 6 plates.","productDescription":"vi, 57 p., 6 plates","costCenters":[],"links":[{"id":484138,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047643/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":276672,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047643/report-thumb.jpg"}],"country":"United States","state":"Louisiana","city":"Alexandria","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.981735,30.892014 ], [ -92.981735,31.517929 ], [ -92.07235,31.517929 ], [ -92.07235,30.892014 ], [ -92.981735,30.892014 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49eae4b0fc50304bc533","contributors":{"authors":[{"text":"Rogers, James E.","contributorId":14380,"corporation":false,"usgs":true,"family":"Rogers","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047642,"text":"70047642 - 1981 - Water resources of the terrace aquifers, central Louisiana","interactions":[],"lastModifiedDate":"2013-08-16T09:45:05","indexId":"70047642","displayToPublicDate":"2013-01-01T09:40:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":147,"text":"Water Resources Technical Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"25","title":"Water resources of the terrace aquifers, central Louisiana","language":"English","publisher":"Louisiana Office of Public Works","publisherLocation":"Baton Rouge, LA","collaboration":"Prepared by State of Louisiana Department of Transportation and Development, Office of Public Works, in cooperation with the United States Geological Survey","usgsCitation":"Snider, J., and Sanford, T., 1981, Water resources of the terrace aquifers, central Louisiana: Water Resources Technical Report 25, viii, 48 p.; Maps: 18 Sheets.","productDescription":"viii, 48 p.; Maps: 18 Sheets","costCenters":[],"links":[{"id":276671,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0434,28.9254 ], [ -94.0434,33.0195 ], [ -88.8162,33.0195 ], [ -88.8162,28.9254 ], [ -94.0434,28.9254 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49eae4b0fc50304bc537","contributors":{"authors":[{"text":"Snider, J.L.","contributorId":97808,"corporation":false,"usgs":true,"family":"Snider","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":482617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Thomas H.","contributorId":62612,"corporation":false,"usgs":true,"family":"Sanford","given":"Thomas H.","affiliations":[],"preferred":false,"id":482616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046131,"text":"70046131 - 1981 - Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","interactions":[{"subject":{"id":8527,"text":"ofr781038 - 1978 - Hydrologic data for the Antlers aquifer, southeastern Oklahoma","indexId":"ofr781038","publicationYear":"1978","noYear":false,"title":"Hydrologic data for the Antlers aquifer, southeastern Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046131,"text":"70046131 - 1981 - Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","indexId":"70046131","publicationYear":"1981","noYear":false,"title":"Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma"},"id":1},{"subject":{"id":9377,"text":"ofr78766 - 1978 - Geohydrology of the Antlers aquifer, southeastern Oklahoma","indexId":"ofr78766","publicationYear":"1978","noYear":false,"title":"Geohydrology of the Antlers aquifer, southeastern Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046131,"text":"70046131 - 1981 - Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","indexId":"70046131","publicationYear":"1981","noYear":false,"title":"Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma"},"id":2}],"lastModifiedDate":"2013-05-28T14:13:37","indexId":"70046131","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":244,"text":"Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"81","title":"Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","docAbstract":"The Antlers aquifer, which consists of as much as 900 feet of friable sandstone, silt, clay, and shale, crops out in an area of 1,860 square miles and underlies about 4,400 square miles in southeastern Oklahoma. Precipitation ranges from 35 to 50 inches per year across the outcrop area, which is well suited to allow high rates of infiltration. The aquifer contains an estimated 31,600,000 acre-feet of water having less than 1,000 milligrams per liter dissolved solids. The average saturated sand thickness is 250 feet. Aquifer tests in the confined part of the aquifer give an average storage coefficient of 0.0005 and an average transmissivity of 1,480 feet squared per day. The estimated specific yield of the unconfined part of the aquifer is 0.15; the transmissivity has not been determined. Large-capacity wells tapping the aquifer commonly yield 100 to 500 gallons per minute; the maximum measured yield is 1,700 gallons per minute. Water usage from the aquifer is very small owing to the availability of an abundance of surface water. Water quality throughout the central and northern part of the aquifer is generally acceptable for municipal use. A few wells, however, yield water containing concentrations of iron and manganese exceeding the limit recommended for municipal use by the National Academy of Sciences and National Academy of Engineering (1972).","language":"English","publisher":"Oklahoma Geological Survey","publisherLocation":"Reston, VA","collaboration":"Prepared by the United States Geological Survey in cooperation with the Oklahoma Geological Survey","usgsCitation":"Hart, D.L., and Davis, R.E., 1981, Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma: Circular 81, iv, 33 p.: Map: 1 Sheet: 47 x 22 inches.","productDescription":"iv, 33 p.: Map: 1 Sheet: 47 x 22 inches","numberOfPages":"38","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":272907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046131.jpg"},{"id":272906,"type":{"id":17,"text":"Plate"},"url":"https://www.ogs.ou.edu/pubsscanned/CircularsPlates/C81PI.pdf"},{"id":272904,"type":{"id":11,"text":"Document"},"url":"https://www.ogs.ou.edu/pubsscanned/Circulars/circular81mm.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,33.6158 ], [ -103.0,37.0 ], [ -94.4307,37.0 ], [ -94.4307,33.6158 ], [ -103.0,33.6158 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a5d1e8e4b0605bc571efb5","contributors":{"authors":[{"text":"Hart, Donald L. Jr.","contributorId":89946,"corporation":false,"usgs":true,"family":"Hart","given":"Donald","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":478988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":478987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70042517,"text":"70042517 - 1981 - Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico","interactions":[{"subject":{"id":17900,"text":"ofr81487 - 1981 - Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico","indexId":"ofr81487","publicationYear":"1981","noYear":false,"title":"Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":70042517,"text":"70042517 - 1981 - Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico","indexId":"70042517","publicationYear":"1981","noYear":false,"title":"Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico"},"id":1}],"lastModifiedDate":"2017-09-20T10:29:12","indexId":"70042517","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":295,"text":"Technical Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"43","title":"Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico","docAbstract":"

The Rincon and Mesilla Valleys of New Mexico extend from Caballo Reservoir to El Paso del Norte, west of El Paso, Texas. Water supplies for this area are obtained from the Rio Grande and from the saturated sediments filling the intermontane basins of south-central New Mexico.

The two major aquifers are the Santa Fe Group of Miocene to middle Pleistocene age and the flood-plain alluvium of late Pleistocene and Holocene age. The Santa Fe Group is composed of thick deposits of interbedded clay, silt, sand, and gravel. The flood-plain alluvium, generally less than 80 feet thick, is composed of a basal gravel layer overlain by interbedded sand, silt, and clay.

In the Rincon Valley, the flood-plain alluvium is the principal source of ground water because the underlying Santa Fe is composed predominantly of lacustrine clay deposits. In the Mesilla Valley, thick deposits of fluvial sands and gravels in the Santa Fe Group are hydraulically connected with the flood-plain alluvium. Water-table conditions occur in the flood-plain alluvium, which is recharged primarily by infiltration of surface water from the Rio Grande, irrigation canals, and irrigated fields. Recharge to the Santa Fe Group occurs primarily from downward infiltration of water from the flood-plain alluvium and secondarily from runoff infiltrating upland sediments and mountain-front fan deposits. In the short term, the Santa Fe Group responds as a leaky confined aquifer due to the presence of interbedded clays that reduce vertical permeability.

Aquifer tests were conducted on 58 wells and test holes, most of which were completed in the Santa Fe Group. Transmissivities range from 1.3 to 21,100 feet squared per day. Average well yields range from about 1,050 gallons per minute in the Rincon Valley to about 1,500 gallons per minute in the Mesilla Valley. Yields in the Jornada del Muerto generally are much smaller.

Movement of ground water is generally southward in the Rincon and Mesilla Valleys and toward the valleys in the adjacent upland areas. Ground water moves southeastward beneath the West Mesa area, converging with ground-water flow in the southern end of the Mesilla Valley. Good hydraulic connection exists between sediments of the West Mesa and Mesilla Valley areas. Ground water in the southern end of the Jornada del Muerto moves generally to the northwest, converges with south-flowing ground water near Point of Rocks, and moves westward into Rincon Valley sediments near Rincon. A small amount of ground water flows westward from the southern end of the Jornada del Muerto across a subsurface igneous body into the Mesilla Valley. Ground-water discharge occurs throughout the Rincon and Mesilla Valleys as drain flow to the river and evapotranspiration.

Dissolved-solids concentrations in the water in the flood-plain alluvium of the Rincon and Mesilla Valleys are generally greater than 1,000 milligrams per liter. A freshwater zone, with dissolved-solids concentrations less than 1,000 milligrams per liter, underlies this thin, slightly saline zone beneath much of the Mesilla Valley. This freshwater zone, occurring in the Santa Fe Group, is surrounded by saline water. Within the study area, major dissolved ions in ground water include sodium, calcium, bicarbonate, and sulfate.

The Rio Grande is a gainlng stream in the northern parts of the Rincon and Mesilla Valleys and a losing stream in the southern part of the Mesilla Valley. Gains and losses result from a close interconnection with ground-water flow systems. Large surface-water irrigation allotments increase ground-water recharge. Increased recharge raises ground-water levels and improves shallow ground-water quality adjacent to these recharge areas. Shallow ground-water discharges to drains, which flow into the Rio Grande. Dissolved-solids concentrations in the Rio Grande increase by as much as 60 percent between Caballo Reservoir and the southern end of the study area.

","language":"English","publisher":"New Mexico State Engineer","publisherLocation":"Santa Fe, NM","collaboration":"Prepared by the U.S. Geological Survey in cooperation with: New Mexico State Engineer Office; U.S. Bureau of Reclamation; Elephant Butte Irrigation District; City of Las Cruces; New Mexico Water Resources Research Institute","usgsCitation":"Wilson, C.A., White, R., Orr, B.R., and Roybal, R.G., 1981, Water resources of the Rincon and Mesilla Valleys and adjacent areas, New Mexico: Technical Report 43, ix, 514 p.; Plates: 1-16: 24 x 38 inches.","productDescription":"ix, 514 p.; Plates: 1-16: 24 x 38 inches","numberOfPages":"540","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":265519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70042517.JPG"},{"id":265518,"type":{"id":11,"text":"Document"},"url":"https://www.ose.state.nm.us/Pub/TechnicalReports/TechReport-043.pdf","text":"Report","size":"24.36 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New Mexico","otherGeospatial":"Mesilla Valley, Rincon Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7ccee4b0b2908510eff0","contributors":{"authors":[{"text":"Wilson, Clyde A.","contributorId":65464,"corporation":false,"usgs":true,"family":"Wilson","given":"Clyde","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":471680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Robert R.","contributorId":16420,"corporation":false,"usgs":true,"family":"White","given":"Robert R.","affiliations":[],"preferred":false,"id":471678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roybal, R. Gary","contributorId":88948,"corporation":false,"usgs":true,"family":"Roybal","given":"R.","email":"","middleInitial":"Gary","affiliations":[],"preferred":false,"id":471681,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70042990,"text":"70042990 - 1981 - Water resources of the southern Powder River area, southeastern Montana","interactions":[{"subject":{"id":10361,"text":"ofr79343 - 1979 - Water resources of the southern Powder River area of southeastern Montana","indexId":"ofr79343","publicationYear":"1979","noYear":false,"title":"Water resources of the southern Powder River area of southeastern Montana"},"predicate":"SUPERSEDED_BY","object":{"id":70042990,"text":"70042990 - 1981 - Water resources of the southern Powder River area, southeastern Montana","indexId":"70042990","publicationYear":"1981","noYear":false,"title":"Water resources of the southern Powder River area, southeastern Montana"},"id":1}],"lastModifiedDate":"2013-01-29T19:47:26","indexId":"70042990","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":187,"text":"Memoir","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"47","title":"Water resources of the southern Powder River area, southeastern Montana","language":"English","publisher":"Montana Bureau of Mines and Geology","publisherLocation":"Butte, MT","usgsCitation":"Miller, W.R., 1981, Water resources of the southern Powder River area, southeastern Montana: Memoir 47, vi, 53 p.","productDescription":"vi, 53 p.","costCenters":[{"id":400,"text":"Montana Water Science Center","active":false,"usgs":true}],"links":[{"id":266745,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.0,44.36 ], [ -116.0,49.0 ], [ -104.0,49.0 ], [ -104.0,44.36 ], [ -116.0,44.36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd97e4b0d965cd9f23a0","contributors":{"authors":[{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":472764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043705,"text":"70043705 - 1981 - Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah","interactions":[{"subject":{"id":23103,"text":"ofr80445 - 1980 - Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah","indexId":"ofr80445","publicationYear":"1980","noYear":false,"title":"Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043705,"text":"70043705 - 1981 - Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah","indexId":"70043705","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah"},"id":1}],"lastModifiedDate":"2017-05-24T10:55:23","indexId":"70043705","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1981","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":"71","title":"Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah","docAbstract":"This report is the last of 19 hydrologic reconnaissances of the basins in western Utah. The purposes of this series of studies are (1) to analyze available hydrologic data and describe the hydrologic system, (2) to evaluate existing and potential water-resources development, and (3) to identify additional studies that might be needed. Part 1 of this report gives an estimate of recharge and discharge, an estimate of the potential for water-resources development, and a statement on the quality of water in the southern Great Salt Lake Desert part of west-central Utah. Part 2 deals with the same aspects of west-central Utah as a whole. Part 2 also summarizes the evidence of interbasin ground-water flow in west-central Utah and presents a theory for the origin of the water discharged from Fish Springs.","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":"Gates, J., and Kruer, S.A., 1981, Hydrologic reconnaissance of the southern Great Salt Lake Desert and summary of the hydrology of west-central Utah: Technical Publication 71, Report: vi, 55 p.; 4 Plates: 15.71 x 30.64 inches or smaller.","productDescription":"Report: vi, 55 p.; 4 Plates: 15.71 x 30.64 inches or smaller","numberOfPages":"61","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331991,"rank":1,"type":{"id":15,"text":"Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad46e4b0b6328103b455","contributors":{"authors":[{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":474127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kruer, Stacie A.","contributorId":51786,"corporation":false,"usgs":true,"family":"Kruer","given":"Stacie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":474128,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70043754,"text":"70043754 - 1981 - Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone","interactions":[{"subject":{"id":9557,"text":"ofr791163 - 1979 - Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo 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Precipitation, the main source of water in the area, ranges from slightly less than 6 inches (152 millimeters) per year in the lowlands to more than 30 inches per year (762 millimeters) in the Henry Mountains and along the western boundary.","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":"Hood, J.W., and Danielson, T.W., 1981, Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone: Technical Publication 68, vi, 143 p.","productDescription":"vi, 143 p.","numberOfPages":"152","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267773,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267772,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009u.pdf"},{"id":331979,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-630"}],"country":"United States","state":"Utah","otherGeospatial":"Dirty Devil River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.5,\n 37.9\n ],\n [\n -111.5,\n 38.9\n ],\n [\n -110,\n 38.9\n ],\n [\n -110,\n 37.9\n ],\n [\n -111.5,\n 37.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad05e4b0b6328103b359","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danielson, T. 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It includes about 1,300 square miles (3,370 square kilometers) in the upper Virgin River basin and about 650 square miles (1,680 square kilometers) in the upper Kanab Creek basin. The area is sparsely populated with Kanab (population about 1,400 in 1975) being the largest community. Although the area is largely agricultural, it is known to contain large coal reserves with potential for development.","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":"Cordova, R., 1981, Ground-water conditions in the upper Virgin River and Kanab Creek basins area, Utah, with emphasis on the Navajo sandstone: Technical Publication 70, vi, 87 p.","productDescription":"vi, 87 p.","numberOfPages":"98","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267713,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331987,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-670"},{"id":267712,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009w.pdf"}],"country":"United States","state":"Utah","county":"Iron County, Kane County, Washington County","otherGeospatial":"Kanab Creek Basin, Virgin River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.291015625,\n 37.046408899699564\n ],\n [\n -113.291015625,\n 37.82280243352756\n ],\n [\n -111.87377929687499,\n 37.82280243352756\n ],\n [\n -111.87377929687499,\n 37.046408899699564\n ],\n [\n -113.291015625,\n 37.046408899699564\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad3be4b0b6328103b420","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":474174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70042792,"text":"70042792 - 1981 - Ground-water conditions in Tooele Valley, Utah, 1976-78","interactions":[{"subject":{"id":15581,"text":"ofr80439 - 1980 - Ground water conditions in Tooele Valley, Utah, 1976-78","indexId":"ofr80439","publicationYear":"1980","noYear":false,"title":"Ground water conditions in Tooele Valley, Utah, 1976-78"},"predicate":"SUPERSEDED_BY","object":{"id":70042792,"text":"70042792 - 1981 - Ground-water conditions in Tooele Valley, Utah, 1976-78","indexId":"70042792","publicationYear":"1981","noYear":false,"title":"Ground-water conditions in Tooele Valley, Utah, 1976-78"},"id":1}],"lastModifiedDate":"2017-09-02T14:09:40","indexId":"70042792","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1981","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":"69","title":"Ground-water conditions in Tooele Valley, Utah, 1976-78","docAbstract":"

No abstract available.

","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the Unied States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Razem, A.C., and Steiger, J.I., 1981, Ground-water conditions in Tooele Valley, Utah, 1976-78: Technical Publication 69, vi, 95 p.","productDescription":"vi, 95 p.","numberOfPages":"102","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331981,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009v.pdf"},{"id":266326,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331980,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-650"}],"country":"United States","state":"Utah","otherGeospatial":"Tooele Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.587890625,\n 40.46157664398329\n ],\n [\n -112.587890625,\n 40.81588791441588\n ],\n [\n -112.16217041015624,\n 40.81588791441588\n ],\n [\n -112.16217041015624,\n 40.46157664398329\n ],\n [\n -112.587890625,\n 40.46157664398329\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51011478e4b033b1feeb2bf6","contributors":{"authors":[{"text":"Razem, Allan C.","contributorId":72390,"corporation":false,"usgs":true,"family":"Razem","given":"Allan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":472283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steiger, Judy I. jsteiger@usgs.gov","contributorId":3689,"corporation":false,"usgs":true,"family":"Steiger","given":"Judy","email":"jsteiger@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":472282,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70038303,"text":"70038303 - 1981 - Water resources inventory of Connecticut Part 7: upper Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T14:07:44","indexId":"70038303","displayToPublicDate":"2012-04-29T10:03:00","publicationYear":"1981","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":"24","title":"Water resources inventory of Connecticut Part 7: upper Connecticut River basin","docAbstract":"

The 508 square miles of the upper Connecticut River basin in north-central Connecticut include the basins of four major tributaries: the Scantic, Park, and Hockanum Rivers, and the Farmington River downstream from Tariffville. Precipitation over this area averaged 44 inches per year during 1931-60. In this period, an additional 3,800 billion gallons of water per year entered the basin in the main stem of the Connecticut River at the Massachusetts state line, about 230 billion gallons per year in the Farmington River at Tariffville, and about 10 billion gallons per year in the Seantic River at the Massachusetts state line. Some water was also imported from outside the basin by water-supply systems. About half the precipitation, 22.2 inches, was lost from the basin by evapotranspiration; the remainder flowed out of the study area in the Connecticut River at Portland.

\n
\n

Variations in streamflow at 41 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: (1) the 7-day annual minimum flow for 2-year and (2) 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.

\n
\n

Of the 30 principal lakes, ponds, and reservoirs, two have usable storage capacities of more than 1 billion gallons. The maximum safe draft rate (regulated flow) of the largest of these, Shenipsit Lake at Rockville, is 6.5 million gallons per day for the 2-year and 30-year recurrence intervals (median and lowest annual flow).

\n
\n

Floods have occurred within each month of the year but in different years. The greatest known flood on the Connecticut River was in March 1936; it had a peak flow of 130,000 cubic feet per second at Hartford. Since then, major floods have been reduced by flood-control measures.

\n
\n

The major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock. Stratified drift overlies till and bedrock in valleys and lowlands in the eastern and western parts and in most of the broad central valley. The stratified drift generally ranges in thickness from 10 feet in small valleys to more than 200 feet in the Connecticut River Valley. Bedrock underlies the entire basin and is composed of (1) interbedded sedimentary and igneous rocks and (2) crystalline rocks.

\n
\n

Ground-water sources yield from several million gallons per day from large well fields to 1 gallon per minute from single wells. Yields of 100 gal/min or more are most commonly obtained from screened wells tapping stratified-drift aquifers; amounts can be calculated by use of a series of graphs in conjunction with estimates of aquifer transmissivity and thickness. Eighteen areas underlain by good aquifers are selected as the most favorable locations for large-scale development of ground water. Selection of these areas is based on estimates of aquifer characteristics and the amount of water potentially available from induced infiltration of streamflow at low-flow conditions.

\n
\n

Small to moderate water supplies can generally be obtained from any of the aquifers. Wells in bedrock yield at least a few gallons per minute at most sites. The probability of obtaining an adequate yield for domestic supply is greater in sedimentary than in crystalline bedrock and is also greater in stratified-drift overburden than in till.

\n
\n

Where unaffected by man's activities, the water is of the calcium magnesium bicarbonate type, is generally low to moderate in dissolved-solids concentration, and ranges from soft to hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streams become more highly mineralized during low-flow conditions, when most flow consists of more highly mineralized water discharged from aquifers. The median dissolved-solids concentration in water from 25 stream sites was 113 mg/L (milligrams per liter) during high flow, and 148 mg/L during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in some streams draining swamps and in some waters draining from sedimentary bedrock which contains iron- and manganese-bearing minerals.

\n
\n

Man's activities have affected the water quality of streams in much of the area, particularly in the Hockanum and Park River basins. The degradation in quality in these streams is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of trace elements, a low dissolved-oxygen content, and abnormally high temperatures. Ground water within this area is degraded principally by induced infiltration of surface water that contains chemical wastes, by leachate from wastes stored or disposed of on the ground, and by effluents discharged from septic tanks.

\n
\n

The quantity and quality of water are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. The total amount of water used in 1968 was more than 100 billion gallons. About 80 percent of this was used for industrial purposes, and 90 percent of the industrial water was obtained from surface-water sources. About 85 percent of the population was supplied with water for domestic use by 15 major public and municipal systems and 25 private associations. Analyses of water from the 13 largest systems show generally good quality.

","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":"Ryder, R.B., Thomas, M.P., and Weiss, L.A., 1981, Water resources inventory of Connecticut Part 7: upper Connecticut River basin: Connecticut Water Resources Bulletin 24, Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller.","productDescription":"Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller","numberOfPages":"83","costCenters":[],"links":[{"id":258813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0024/report.pdf","size":"17112","linkFileType":{"id":1,"text":"pdf"}},{"id":258814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0024/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.533333 ], [ -72.833333,42.058333 ], [ -72.366667,42.058333 ], [ -72.366667,41.533333 ], [ -72.833333,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc907e4b08c986b32cc15","contributors":{"authors":[{"text":"Ryder, Robert B. rryder@usgs.gov","contributorId":68294,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":463828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463829,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70039444,"text":"70039444 - 1981 - Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division","interactions":[],"lastModifiedDate":"2012-08-04T01:01:57","indexId":"70039444","displayToPublicDate":"2012-01-01T15:55:28","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":379,"text":"Report","active":false,"publicationSubtype":{"id":6}},"title":"Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division","docAbstract":"Research in the WRD had its beginnings in the late 1950's when the \"core research\" line item was added to the Congressional budget. Since this time the Federal program has grown from a \"basic sciences\" program to one that includes a broad spectrum of basic and applied scientific investigations. Water resources research in WRD includes the study of water in all its phases and uses the basic sciences of mathematics, chemistry, physics, biology, geology and engineering to gain a fundamental understanding of the processes that affect the movement of water and its chemical constituents through hydrologic systems. The basic knowledge and methodologies derived from water resources research are applicable not only to the solution of current problems associated with the Nation's water resources, but also to anticipated hydrologic issues.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70039444","collaboration":"Compiled by the Office of the Assistant Chief Hydrologist for Research and Technical Coordination, Water Resources Division","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water Resources Research October 1, 1979 - September 30, 1980: Summary statements of research activities by the Water Resources Division: Report, x, 233 p., https://doi.org/10.3133/70039444.","productDescription":"x, 233 p.","numberOfPages":"247","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261584,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039444/report.pdf"},{"id":261585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039444/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc780e4b08c986b32c496","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":535304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039196,"text":"70039196 - 1981 - The EROS Data Center","interactions":[],"lastModifiedDate":"2017-05-19T18:37:59","indexId":"70039196","displayToPublicDate":"2012-01-01T15:50:15","publicationYear":"1981","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":"The EROS Data Center","docAbstract":"The Earth Resources Observation Systems (EROS) Program of the U.S. Department of the Interior, administered by the Geological Survey, was established in 1966 to apply remote-sensing techniques to the inventory, monitoring, and management of natural resources. To meet its primary objective, the EROS Program includes research and training in the interpretation and application of remotely sensed data and provides remotely sensed data at nominal cost to scientists, resource planners, managers, and the public.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039196","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, The EROS Data Center: General Information Product, 37 p., https://doi.org/10.3133/70039196.","productDescription":"37 p.","numberOfPages":"40","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261364,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039196/report.pdf"},{"id":261365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039196/report-thumb.jpg"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97,43.36666666666667 ], [ -97,43.75 ], [ -96.36666666666666,43.75 ], [ -96.36666666666666,43.36666666666667 ], [ -97,43.36666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba70de4b08c986b32133c","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":535238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039034,"text":"70039034 - 1981 - United States Geological Survey Yearbook, fiscal year 1980","interactions":[],"lastModifiedDate":"2017-03-08T16:36:34","indexId":"70039034","displayToPublicDate":"2012-01-01T11:52:39","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1980","docAbstract":"It is not very often that a single event is so overwhelming that it changes public perceptions of natural hazards for generations. Perhaps for the U.S. Geological Survey, the explosive volcanic activity of Mount St. Helens began such a change. After 101 years of careful science of the Earth's past and meticulous observations and assessments of the present, predictive earth science was in full public view. However vague and faint the glimpse of the future made possible by earth science, it was enough. Warnings were issued, thousands of lives were saved, and the age of real-time geology began. The Survey's basic mission has not changed, but the power of our analytical tools has increased by several orders of magnitude. The Survey's efforts to understand Earth processes and hydrologic principles continued with the collection, during fiscal year 1980, of valuable new data on the geologic origin and framework, seismicity, and mineral and energy resources of the United States. The Survey is also responsible for classification of the leasable minerals on Federal lands and the regulation of mineral exploration and development activities on Federal and Indian lands. As the principal earth science fact-gathering agency, the Survey provides information for sound decisionmaking by government and private industry. Industry uses the Survey's information in exploring for energy and minerals and improving their efforts to make development of energy and minerals compatible with environmental protection standards. Government uses the Survey's information in conducting leasing operations on public lands, in regulating the safe design and siting of nuclear plants, and in establishing guidelines for determining and locating areas that are subject to geologic hazards such as landslides, earthquakes, and volcanic eruptions. The Yearbook reports a broad range of the Survey's accomplishments during the past fiscal year and provides an overview of future directions. Many of the topics covered will continue to be important natural resource and earth science issues of the 1980's.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039034","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, United States Geological Survey Yearbook, fiscal year 1980: Yearbook, vi, 137 p., https://doi.org/10.3133/70039034.","productDescription":"vi, 137 p.","costCenters":[],"links":[{"id":261273,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039034/report.pdf","text":"Report","size":"49.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039034/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc91e4b08c986b328cf5","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":535203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006721,"text":"70006721 - 1981 - Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds","interactions":[],"lastModifiedDate":"2012-07-07T01:01:38","indexId":"70006721","displayToPublicDate":"2012-01-01T10:27:53","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2149,"text":"Journal of Agricultural and Food Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds","docAbstract":"Isobornyl thiocyanoacetate (Thanite) is an insecticide that induces a surfacing response in fish and therefore has been considered to have potential as a fish collection agent. Analyses for residues of Thanite in carp (Cyprinus carpio) and largemouth bass (Micropterus salmoides) exposed to chemical yielded only a trace of the parent compound. A metabolite, isobornyl a-(methylthio)acetate, was isolated and indentified by GC-MS,and a reference standard for the metabolite was synthesized. Residues of the metabolite were present in largemouth bass muscle tissue within 1 h after exposure to Thanite. The metabolite was also observed in the muscle, blood plasma, and bile of carp. Residues of the metaboliteare rapidly elimanated after the fish are transferred to Thanite-free water. Residues of Thanite in water, algae, and from soil from ponds treated with Thanite declined to undetectable levels within 28 days after treatment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Agricultural and Food Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"ACS Publications","publisherLocation":"Washington, D.C.","doi":"10.1021/jf00105a049","collaboration":"None","usgsCitation":"Allen, J.L., Sills, J., Dawson, V.K., and Amel, R., 1981, Residues of isobornyl thiocyanoacetate (Thanite) and a metabolite in fish and treated ponds: Journal of Agricultural and Food Chemistry, v. 29, no. 3, p. 634-636, https://doi.org/10.1021/jf00105a049.","productDescription":"3 p.","startPage":"634","endPage":"636","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258224,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/jf00105a049","linkFileType":{"id":5,"text":"html"}}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505aa9a9e4b0c8380cd85eea","contributors":{"authors":[{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":355091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sills, J.B.","contributorId":55380,"corporation":false,"usgs":true,"family":"Sills","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":355092,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, V. K.","contributorId":48900,"corporation":false,"usgs":true,"family":"Dawson","given":"V.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":355090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amel, R.T.","contributorId":46818,"corporation":false,"usgs":true,"family":"Amel","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":355089,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70039567,"text":"70039567 - 1981 - Studying the Earth from space","interactions":[],"lastModifiedDate":"2012-08-13T17:03:59","indexId":"70039567","displayToPublicDate":"2012-01-01T00:12:25","publicationYear":"1981","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":"Studying the Earth from space","docAbstract":"Space age technology contains a key to increased knowledge about the Earth's resources; this key is remote sensing detecting the nature or condition of something without actually touching it. An early and still most useful form of remote sensing is photography which records the\nscene, as man sees it, on film sensitive to that part of the electromagnetic spectrum called visible energy. Electromagnetic energy travels in waves of various lengths; most are invisible to the human eye. Wavelengths progressively longer than those that the eye can see are infrared and microwave. Wavelengths progressively shorter than the eye can see are ultraviolet, X-rays, and gamma rays.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039567","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Studying the Earth from space: General Information Product, 24 p., https://doi.org/10.3133/70039567.","productDescription":"24 p.","numberOfPages":"28","costCenters":[],"links":[{"id":259582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"otherGeospatial":"Earth","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ceae4b08c986b31d518","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":535367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046351,"text":"70046351 - 1981 - Improved methods for national water assessment, water resources contract: WR15249270","interactions":[],"lastModifiedDate":"2013-07-08T12:50:12","indexId":"70046351","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Improved methods for national water assessment, water resources contract: WR15249270","docAbstract":"The purpose of our research is to develop methods to make National Water Assessment more useful in estimating water availability for economic growth and more helpful in determining the effect of water resource development upon the environmental quality of related land resources. There are serious questions pertaining to the 1975 Water Assessment and these amplify the significance of decisions made as to the planning and scheduling of the next assessment.","language":"English","publisher":"Harvard Water Resources Group","doi":"10.3133/70046351","usgsCitation":"Thomas, H., 1981, Improved methods for national water assessment, water resources contract: WR15249270, 59 p., https://doi.org/10.3133/70046351.","productDescription":"59 p.","costCenters":[],"links":[{"id":273507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046351/report-thumb.jpg"},{"id":274618,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046351/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f568e4b0097a7158e5c6","contributors":{"authors":[{"text":"Thomas, Harold A. Jr.","contributorId":82206,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold A.","suffix":"Jr.","affiliations":[],"preferred":false,"id":479538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006392,"text":"70006392 - 1981 - \"Duck stamp\" dollars reserve native prairie tracts","interactions":[],"lastModifiedDate":"2017-11-16T10:19:25","indexId":"70006392","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3230,"text":"Rangelands","active":true,"publicationSubtype":{"id":10}},"title":"\"Duck stamp\" dollars reserve native prairie tracts","docAbstract":"Ducks and wetlands are inseparable in the prairies. Hunters know this, bird watchers know this, wildlife managers know this, and most importantly people who manage the croplands and rangelands know this. The 1,746 tracts of native prairie within these upland-wetland complexes known as Waterfowl Production Areas are not the only lands purchased with \"duck stamp\" dollars. Considerable acreages have also been purchased in central and southern parts of the United States to provide staging, resting, and wintering areas for waterfowl. Since 1934, when \"duck stamps\" were first sold, nearly 2.5 million acres of waterfowl habitats have been acquired or taken under easement within the United States with revenue from these sales. By purchasing \"duck stamps\", more than 2.2 million people provide over $16.5 million in annual revenue. It is certainly gratifying to know that some of the remaining native prairie remnants in the Northern Great Plains are being reserved for the future with \"duck stamp\" dollars.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Rangelands","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"University of Arizona","publisherLocation":"Tucson, AZ","usgsCitation":"Higgins, K., 1981, \"Duck stamp\" dollars reserve native prairie tracts: Rangelands, v. 3, no. 5, p. 190-191.","productDescription":"2 p.","startPage":"190","endPage":"191","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":263631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":263630,"type":{"id":11,"text":"Document"},"url":"https://journals.uair.arizona.edu/index.php/rangelands/article/view/11685/10958"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,18.9 ], [ 172.5,71.4 ], [ -66.9,71.4 ], [ -66.9,18.9 ], [ 172.5,18.9 ] ] ] } } ] }","volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50bd1353e4b069d93eefc4bb","contributors":{"authors":[{"text":"Higgins, K.F.","contributorId":55767,"corporation":false,"usgs":true,"family":"Higgins","given":"K.F.","email":"","affiliations":[],"preferred":false,"id":354434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70012020,"text":"70012020 - 1981 - Earth fissures and localized differential subsidence","interactions":[{"subject":{"id":70012020,"text":"70012020 - 1981 - Earth fissures and localized differential subsidence","indexId":"70012020","publicationYear":"1981","noYear":false,"title":"Earth fissures and localized differential subsidence"},"predicate":"SUPERSEDED_BY","object":{"id":9554,"text":"ofr79951 - 1979 - Earth fissures and localized differential subsidence","indexId":"ofr79951","publicationYear":"1979","noYear":false,"title":"Earth fissures and localized differential subsidence"},"id":1}],"supersededBy":{"id":9554,"text":"ofr79951 - 1979 - Earth fissures and localized differential subsidence","indexId":"ofr79951","publicationYear":"1979","noYear":false,"title":"Earth fissures and localized differential subsidence"},"lastModifiedDate":"2019-07-17T16:10:35","indexId":"70012020","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Earth fissures and localized differential subsidence","docAbstract":"

Long linear tension cracks associated with declining groundwater levels at four sites in subsiding areas in south-central Arizona, Fremont Valley, California, and Las Vegas Valley, Nevada, occur near points of maximum convex-upward curvature in subsidence profiles oriented perpendicular to the cracks. Profiles are based on repeated precise vertical control surveys of lines of closely spaced bench marks. Association of these fissures with zones of localized differential subsidence indicates that linear earth fissures are caused by horizontal tensile strains probably resulting from localized differential compaction. Horizontal tensile strains across the fissures at the point of maximum convex-upward curvature, ranging from approximately 100 to 700 microstrains (0.01 to 0.07% per year), were indicated based on measurements with a tape or electronic distance meter.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR017i001p00223","usgsCitation":"Holzer, T.L., and Pampeyan, E.H., 1981, Earth fissures and localized differential subsidence: Water Resources Research, v. 17, no. 1, p. 223-227, https://doi.org/10.1029/WR017i001p00223.","productDescription":"5 p.","startPage":"223","endPage":"227","additionalOnlineFiles":"N","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":222334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, Utah","otherGeospatial":"Fremont Valley, Las Vegas Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,31.3 ], [ -124.8,43.5 ], [ -109.0,43.5 ], [ -109.0,31.3 ], [ -124.8,31.3 ] ] ] } } ] }","volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505a0499e4b0c8380cd50a9a","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":362535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pampeyan, Earl H.","contributorId":54698,"corporation":false,"usgs":true,"family":"Pampeyan","given":"Earl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362536,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221652,"text":"5221652 - 1981 - Winter waterfowl research needs and efforts in the Mississippi delta","interactions":[],"lastModifiedDate":"2012-02-02T00:14:51","indexId":"5221652","displayToPublicDate":"2010-06-16T12:19:33","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2092,"text":"International Waterfowl Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Winter waterfowl research needs and efforts in the Mississippi delta","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Waterfowl Symposium","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Reinecke, K.J., 1981, Winter waterfowl research needs and efforts in the Mississippi delta: International Waterfowl Symposium, v. 4, p. 231-236.","productDescription":"231-236","startPage":"231","endPage":"236","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5dff9a","contributors":{"authors":[{"text":"Reinecke, K. J.","contributorId":54537,"corporation":false,"usgs":true,"family":"Reinecke","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":334360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221646,"text":"5221646 - 1981 - Common tern colonies along the mid-Atlantic coast. I. Nestling chronology","interactions":[],"lastModifiedDate":"2023-11-20T12:59:34.316282","indexId":"5221646","displayToPublicDate":"2010-06-16T12:19:18","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1272,"text":"Colonial Waterbirds","printIssn":"07386028","active":false,"publicationSubtype":{"id":10}},"title":"Common tern colonies along the mid-Atlantic coast. I. Nestling chronology","docAbstract":"1. Sixteen Common Tern colonies in Rhode Island, New Jersey, Virginia, and North Carolina were studied from May through July 1980 by four investigators. Nests were marked during egg laying and were monitored every 5-7 days until fledging of young. 2. Results from 1980 indicate that ambient temperature differences in the four study areas account for differences in the onset of egg laying with North Carolina and Virginia colonies beginning 12-16 days before New Jersey and Rhode Island birds. Temperature alone, however, does not seem to have a significant effect on either median egg-laying dates or total duration of the season. 3. The low frequency of late-season nesting was not correlated with colony size or success of peak nests in 1980, but renesting (or late nesting) in all study areas was rare because of the benign weather conditions during the spring. Similarly, no significant correlation was found between success of nests and colony size.","language":"English","publisher":"Waterbird Society","doi":"10.2307/1521131","usgsCitation":"Smith, D.C., Erwin, R., Custer, T., and Fussell, J., 1981, Common tern colonies along the mid-Atlantic coast. I. Nestling chronology: Colonial Waterbirds, v. 4, no. 1, p. 160-165, https://doi.org/10.2307/1521131.","productDescription":"6 p.","startPage":"160","endPage":"165","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196644,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5ee","contributors":{"authors":[{"text":"Smith, D. C. davidsmith@usgs.gov","contributorId":31057,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":false,"id":334349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erwin, R.M.","contributorId":57396,"corporation":false,"usgs":true,"family":"Erwin","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":334350,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":334352,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fussell, J.O. III","contributorId":69265,"corporation":false,"usgs":true,"family":"Fussell","given":"J.O.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":334351,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5221657,"text":"5221657 - 1981 - Asiatic clam (Corbicula manilensis) and other foods used by waterfowl in the James River, Virginia","interactions":[],"lastModifiedDate":"2023-10-16T16:32:30.805639","indexId":"5221657","displayToPublicDate":"2010-06-16T12:19:15","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1583,"text":"Estuaries","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Asiatic clam (Corbicula manilensis) and other foods used by waterfowl in the James River, Virginia","title":"Asiatic clam (Corbicula manilensis) and other foods used by waterfowl in the James River, Virginia","docAbstract":"

Corbicula manilensis was found in the gizzards of 24 ducks of 5 species taken from the James River, Virginia, between 1973 and 1976. Percent average volume in these species ranged from trace to 6%. This is the first known occurrence of this exotic clam in the food of duck in Chesapeake Bay. A total of 135 other food items was identified from the 116 gizzards of 9 species that were examined. Food that predominated included Cyperus spp.,Leersia oryzoides, Polygonum spp., and Zea mays. The great diversity of food consumed in this fresh tidal section of the James River indicates the high value of these wetlands to waterfowl.

","language":"English","publisher":"Springer","doi":"10.2307/1351481","usgsCitation":"Perry, M., and Uhler, F., 1981, Asiatic clam (Corbicula manilensis) and other foods used by waterfowl in the James River, Virginia: Estuaries, v. 4, no. 3, p. 229-233, https://doi.org/10.2307/1351481.","productDescription":"5 p.","startPage":"229","endPage":"233","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199229,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"James River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.96703251441268,\n 37.93871880617202\n ],\n [\n -79.9937374752602,\n 37.89102274261042\n ],\n [\n -79.99596288866374,\n 37.86233169782183\n ],\n [\n -80.01116988025761,\n 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F.M.","contributorId":81965,"corporation":false,"usgs":true,"family":"Uhler","given":"F.M.","email":"","affiliations":[],"preferred":false,"id":334375,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221674,"text":"5221674 - 1981 - Management of waterfowl during severe weather","interactions":[],"lastModifiedDate":"2012-02-02T00:14:44","indexId":"5221674","displayToPublicDate":"2010-06-16T12:19:15","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2859,"text":"New Jersey Outdoors","active":true,"publicationSubtype":{"id":10}},"title":"Management of waterfowl during severe weather","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"New Jersey Outdoors","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Kirby, R., and Ferrigno, F., 1981, Management of waterfowl during severe weather: New Jersey Outdoors, v. 8, no. 1, p. 14-16.","productDescription":"14-16","startPage":"14","endPage":"16","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a30e","contributors":{"authors":[{"text":"Kirby, R.E.","contributorId":75871,"corporation":false,"usgs":true,"family":"Kirby","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":334415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferrigno, Fred","contributorId":55107,"corporation":false,"usgs":false,"family":"Ferrigno","given":"Fred","email":"","affiliations":[],"preferred":false,"id":334414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5223593,"text":"5223593 - 1981 - Breeding habit of the toad Bufo coccifer in Costa Rica, with a description of the tadpole","interactions":[],"lastModifiedDate":"2012-02-02T00:15:36","indexId":"5223593","displayToPublicDate":"2010-06-16T12:19:15","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3451,"text":"Southwestern Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Breeding habit of the toad Bufo coccifer in Costa Rica, with a description of the tadpole","docAbstract":"The breeding habits of Bufo coccifer were studied in northwestern Costa Rica between 1971 and 1974. This species breeds during the rainy season, at least from May through August. Males chorus from areas of shallow water. Their calls resemble those of Mexican representatives of the species in pulse rate and duration, but are closer to those of other Costa Rican and Panamanian populations in dominant frequency. Thus, our data do not clearly support recognition of Bufo cycladen as a distinct species for the Mexican populations. Amplexus is axillary, and two strings of eggs are extruded simultaneously during oviposition. Tadpoles, described for the first time in this paper, are secretive and do not aggregate. Development to metamorphosis requires about 5 weeks.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Southwestern Naturalist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"McDiarmid, R., and Foster, M., 1981, Breeding habit of the toad Bufo coccifer in Costa Rica, with a description of the tadpole: Southwestern Naturalist, v. 26, no. 4, p. 353-363.","productDescription":"353-363","startPage":"353","endPage":"363","numberOfPages":"11","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18138,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3671077","linkFileType":{"id":5,"text":"html"}}],"volume":"26","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f94ab","contributors":{"authors":[{"text":"McDiarmid, R.W.","contributorId":15130,"corporation":false,"usgs":true,"family":"McDiarmid","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":339039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, M.S. 0000-0001-8272-4608","orcid":"https://orcid.org/0000-0001-8272-4608","contributorId":10116,"corporation":false,"usgs":true,"family":"Foster","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":339038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221693,"text":"5221693 - 1981 - The effects of ingested petroleum on the maphthalene-metabolizing properties of the liver tissue in seawater-adapted mallard ducks (Anas platyrhynchos)","interactions":[],"lastModifiedDate":"2012-02-02T00:14:36","indexId":"5221693","displayToPublicDate":"2010-06-16T12:19:12","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1561,"text":"Environmental Research","active":true,"publicationSubtype":{"id":10}},"title":"The effects of ingested petroleum on the maphthalene-metabolizing properties of the liver tissue in seawater-adapted mallard ducks (Anas platyrhynchos)","docAbstract":"Hepatic mixed function oxidase activities were estimated in seawater-adapted mallard ducks (Anas platyrhynchos) that had been consuming food contaminated with one of five different types of crude oil. After 50 days of exposure to contaminated food, enzyme activities of liver microsomal preparations were assessed in terms of their naphthalenemetabolizing properties in vitro. Although dose-dependent increases in the total hepatic enzyme activities (nmole naphthalene metabolized per minute per unit mass body weight) were observed in birds consuming food contaminated with each type of crude oil, three patterns of response were apparent. Crude oils from South Louisiana and Kuwait stimulated large and significant increases in the specific activity of the enzyme system (nmole naphthalene metabolized per minute per unit mass microsomal protein), whereas little or no increase in either microsomal protein content or relative liver weight were observed. In contrast, two crude oils from Santa Barbara, Calif., induced only small increases in specific activity but significant increases occurred in hepatic microsomal protein concentration and relative liver weight. The crude oil from Prudhoe Bay, Ala., evoked intermediate patterns of response. The possible significance of these data is discussed in relation to the survival of seabirds consuming petroleum-contaminated food and drinking water.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0013-9351(81)90167-5","collaboration":"2527_Gorsline.pdf","usgsCitation":"Gorsline, J., Holmes, W.N., and Cronshaw, J., 1981, The effects of ingested petroleum on the maphthalene-metabolizing properties of the liver tissue in seawater-adapted mallard ducks (Anas platyrhynchos): Environmental Research, v. 24, no. 2, p. 377-390, https://doi.org/10.1016/0013-9351(81)90167-5.","productDescription":"377-390","startPage":"377","endPage":"390","numberOfPages":"14","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18078,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://dx.doi.org/10.1016/0013-9351(81)90167-5","linkFileType":{"id":5,"text":"html"}},{"id":194109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6358cc","contributors":{"authors":[{"text":"Gorsline, J.","contributorId":30307,"corporation":false,"usgs":true,"family":"Gorsline","given":"J.","email":"","affiliations":[],"preferred":false,"id":334465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holmes, W. N.","contributorId":70497,"corporation":false,"usgs":false,"family":"Holmes","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":334467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cronshaw, J.","contributorId":44247,"corporation":false,"usgs":true,"family":"Cronshaw","given":"J.","email":"","affiliations":[],"preferred":false,"id":334466,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}