{"pageNumber":"5346","pageRowStart":"133625","pageSize":"25","recordCount":165227,"records":[{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","interactions":[{"subject":{"id":15062,"text":"ofr75615 - 1975 - Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho","indexId":"ofr75615","publicationYear":"1975","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","indexId":"70042717","publicationYear":"1976","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho"},"id":1}],"lastModifiedDate":"2013-01-18T14:10:29","indexId":"70042717","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"42","title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","docAbstract":"Springs discharging from the Snake Plain aquifer contribute approximately 6,000 cubic feet per second (170 cubic metres per second) to flow in the Snake River between Milner and King Hill. Before irrigation began on the Snake River Plain north and east of the springs, total spring discharge was about 4,200 cubic feet per second (120 cubic meters per second). Increasing amounts of irrigated acreage from the early 1900's to the mid-1940's contributed more irrigation-return water to the aquifer resulting in increased discharge at the springs. Maximum discharge of about 6,800 cubic feet per second (190 cubic metres per second) occurred during the late 1940's and early 1950's. Increased use of pumped ground water for irrigation and changing irrigation practices have since resulted in a decline in spring discharge.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise, ID","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Idaho Department of Water Resources, Statehouse, Boise, Idaho","usgsCitation":"Moreland, J.A., 1976, Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho: Water Information Bulletin 42, vi, 46 p.; ill.; maps.","productDescription":"vi, 46 p.; ill.; maps","startPage":"i","endPage":"46","numberOfPages":"53","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":265963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265962,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib42-water-use_alternatives.pdf"}],"country":"United States","state":"Idaho","county":"Gooding County;Jerome County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0875,42.4981 ], [ -115.0875,43.2001 ], [ -113.9308,43.2001 ], [ -113.9308,42.4981 ], [ -115.0875,42.4981 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d53e4b061045bf9ac32","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":472107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","interactions":[{"subject":{"id":16567,"text":"ofr75322 - 1975 - Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A.","indexId":"ofr75322","publicationYear":"1975","noYear":false,"title":"Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A."},"predicate":"SUPERSEDED_BY","object":{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","indexId":"70042576","publicationYear":"1976","noYear":false,"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA"},"id":1}],"lastModifiedDate":"2017-11-03T11:01:24","indexId":"70042576","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","docAbstract":"The Raft River valley, near the boundary of the Snake River plain with the Basin and Range province, is a north-trending late Cenozoic downwarp bounded by faults on the west, south, and east. Pleistocene alluvium and Miocene-Pliocene tuffaceous sediments, conglomerate, and felsic volcanic rocks aggregate 2 km in thickness. Large gravity, magnetic, and total field resistivity highs probably indicate a buried igneous mass that is too old to serve as a heat source. Differing seismic velocities relate to known or inferred structures and to a suspected shallow zone of warm water. Resistivity anomalies reflect differences of both composition and degree of alteration of Cenozoic rocks. Resistivity soundings show a 2 to 5 ohm·m unit with a thickness of 1 km beneath a large part of the valley, and the unit may indicate partly hot water and partly clayey sediments. Observed self-potential anomalies are believed to indicate zones where warm water rises toward the surface. Boiling wells at Bridge, Idaho are near the intersection of north-northeast normal faults which have moved as recently as the late (?) Pleistocene, and an east-northeast structure, probably a right-lateral fault. Deep circulation of ground water in this region of relatively high heat flow and upwelling along faults is the probable cause of the thermal anomaly.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Williams, P., Mabey, D.R., Zohdy, A.A., Ackermann, H.D., Hoover, D.B., Pierce, K.L., and Oriel, S.S., 1976, Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1273-1282.","productDescription":"10 p.","startPage":"1273","endPage":"1282","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":265587,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Raft River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,42.0 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,42.0 ], [ -117.24,42.0 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f293f4e4b0c9e41dd3ab73","contributors":{"authors":[{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":471858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":471856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ackermann, Hans D.","contributorId":44539,"corporation":false,"usgs":false,"family":"Ackermann","given":"Hans","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":471854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":471857,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":471853,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":471859,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70042824,"text":"70042824 - 1976 - Regional geologic framework off northeastern United States","interactions":[{"subject":{"id":15831,"text":"ofr7560 - 1975 - Structure of continental margin off Mid-Atlantic states (Baltimore Canyon Trough)","indexId":"ofr7560","publicationYear":"1975","noYear":false,"title":"Structure of continental margin off Mid-Atlantic states (Baltimore Canyon Trough)"},"predicate":"SUPERSEDED_BY","object":{"id":70042824,"text":"70042824 - 1976 - Regional geologic framework off northeastern United States","indexId":"70042824","publicationYear":"1976","noYear":false,"title":"Regional geologic framework off northeastern United States"},"id":1}],"lastModifiedDate":"2023-01-25T16:42:25.487197","indexId":"70042824","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Regional geologic framework off northeastern United States","docAbstract":"<p>Six multichannel seismic-reflection profiles taken across the Atlantic continental margin off the northeastern United States show an excess of 14 km of presumed Mesozoic and younger sedimentary rocks in the Baltimore Canyon trough and 8 km in the Georges Bank basin.</p><p>Beneath the continental rise, the sedimentary prism thickness exceeds 7 km south of New Jersey and Maryland, and it is 4.5 km thick south of Georges Bank. Stratigraphically, the continental slope–outer edge of the continental shelf is a transition zone of high-velocity sedimentary rock, probably carbonate, that covers deeply subsided basement.</p><p>Acoustically, the sedimentary sequence beneath the shelf is divided into three units which are correlated speculatively with the Cenozoic, the Cretaceous, and the Jurassic-Triassic sections. These units thicken offshore, and some have increased seismic velocities farther offshore. The uppermost unit thickens from a fraction of a kilometer to slightly more than a kilometer in a seaward direction, and velocity values range from 1.7 to 2.2 km/sec. The middle unit thickens from a fraction of a kilometer to as much as 5 km (northern Baltimore Canyon trough), and seismic velocity ranges from 2.2 to 5.4 km/sec. The lowest unit thickens to a maximum of 9 km (northern Baltimore Canyon), and velocities span the 3.9 to 5.9-km/sec interval.</p><p>The spatial separation of magnetic and gravity anomalies on line 2 (New Jersey) suggests that in the Baltimore Canyon region the magnetic-slope anomaly is due to edge effects and that the previously reported free-air and isostatic gravity anomalies over the outer shelf may be due in part to a lateral increase in sediment density (velocity) near the shelf edge. The East Coast magnetic anomaly and the free-air gravity high both coincide over the outer shelf edge on line 1 (Georges Bank) but are offset by 20 km from the ridge on the reflection profile. Because the magnetic-slope-anomaly wavelength is nearly 50 km across, a deep source is likely. In part, the positive free-air gravity anomaly likewise may represent the significant lateral density increase within the sedimentary section toward the outer edge of the shelf.</p>","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/C1EA35E1-16C9-11D7-8645000102C1865D","usgsCitation":"Schlee, J., Behrendt, J.C., Grow, J., Robb, J.M., Mattick, R.E., Taylor, P.T., and Lawson, B.J., 1976, Regional geologic framework off northeastern United States: American Association of Petroleum Geologists Bulletin, v. 60, no. 6, p. 926-951, https://doi.org/10.1306/C1EA35E1-16C9-11D7-8645000102C1865D.","productDescription":"26 p.","startPage":"926","endPage":"951","numberOfPages":"26","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266431,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Atlantic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.57445495565841,\n              34.54201079036788\n            ],\n            [\n              -67.00870217573663,\n              32.68969202501184\n            ],\n            [\n              -64.4151885851629,\n              33.653394442107356\n            ],\n            [\n              -58.9581858826422,\n              40.6927360683957\n            ],\n            [\n              -68.50221203592804,\n              42.200234266771474\n            ],\n            [\n              -70.993156429557,\n              40.57584686002005\n            ],\n            [\n              -73.8834116106613,\n              39.16159111213017\n            ],\n            [\n              -75.18467319036125,\n              36.48592421852297\n            ],\n            [\n              -74.48849487074959,\n              34.39791504686983\n            ],\n            [\n              -74.57445495565841,\n              34.54201079036788\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"60","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026629e4b0d4f5ea817c51","contributors":{"authors":[{"text":"Schlee, John","contributorId":16078,"corporation":false,"usgs":true,"family":"Schlee","given":"John","affiliations":[],"preferred":false,"id":472336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"preferred":false,"id":472334,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grow, John A.","contributorId":51739,"corporation":false,"usgs":true,"family":"Grow","given":"John A.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":472335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":472338,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mattick, Robert E.","contributorId":44130,"corporation":false,"usgs":true,"family":"Mattick","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":472333,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Taylor, P. T.","contributorId":69858,"corporation":false,"usgs":true,"family":"Taylor","given":"P.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":472337,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lawson, B. J.","contributorId":11905,"corporation":false,"usgs":true,"family":"Lawson","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":472332,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","interactions":[{"subject":{"id":14188,"text":"ofr76323 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"ofr76323","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"70042934","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"id":1}],"lastModifiedDate":"2016-12-12T13:40:24","indexId":"70042934","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"53","title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","docAbstract":"<p>This report presents a part of the results of an investigation of the hydrology of the northern Uinta Basin area by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources. The purpose of the report is to summarize the hydraulic and geohydrologic characteristics of the aquifers in the area.</p>","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., 1976, Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado: Technical Publication 53, vi, 71 p.","productDescription":"vi, 71 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331878,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-330"},{"id":331879,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009f.pdf"}],"country":"United States","state":"Colorado, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -102.0,42.0 ], [ -102.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd7fe4b0d965cd9f2319","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":472616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","interactions":[{"subject":{"id":13216,"text":"ofr74214 - 1974 - Estimating mean streamflow in the Duchesne River basin, Utah","indexId":"ofr74214","publicationYear":"1974","noYear":false,"title":"Estimating mean streamflow in the Duchesne River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":1},{"subject":{"id":16124,"text":"ofr75392 - 1975 - Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah","indexId":"ofr75392","publicationYear":"1975","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":2}],"lastModifiedDate":"2016-12-12T13:38:13","indexId":"70042823","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","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":"51","title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","docAbstract":"The Pine Valley drainage basin is an area of about 730 square miles (1,890 square kilometres) in Millard, Beaver, and Iron Counties in southwestern Utah. Total annual precipitation in the basin averages about 410,000 acre-ft (acre-feet) or 506 hm<sup>3</sup> (cubic hectometres). Less than 500 acre-ft (0.6 hm<sup>3</sup>) of runoff reaches the playa on the lowest part of the valley floor. There is no surface outflow from the basin. All streams are ephemeral except in short headwater reaches of a few streams where perennial or intermittent ground-water discharge sustains flow. Surface-water development and use in the basin are insignificant.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights.","usgsCitation":"Stephens, J.C., 1976, Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah: Technical Publication 51, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267163,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009d.pdf"},{"id":331876,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-300"}],"country":"United States","state":"Utah","county":"Beaver County, Iron County, Millard County","otherGeospatial":"Pine Valley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026618e4b0d4f5ea817c00","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":472331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042949,"text":"70042949 - 1976 - A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","interactions":[{"subject":{"id":13783,"text":"ofr72129 - 1972 - Genesis of oil in metalliferous veins, San Juan Mountains, Colorado","indexId":"ofr72129","publicationYear":"1972","noYear":false,"title":"Genesis of oil in metalliferous veins, San Juan Mountains, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042949,"text":"70042949 - 1976 - A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","indexId":"70042949","publicationYear":"1976","noYear":false,"title":"A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado"},"id":1}],"lastModifiedDate":"2015-08-25T14:23:55","indexId":"70042949","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","docAbstract":"<p>A tarry, benzene-soluble material is present in metal-rich veins in the Idarado mine, Ouray County, Colo., in an area not known to have petroleum resources. The material was compared chemically, spectometrically, and chromatographically with oils from four fields in the nearby Paradox basin. Each of these oil fields contains reservoir rocks equivalent to rock units known to extend beneath volcanic rocks near the mine. Carbon and sulfur isotope data and gas chromatographic data indicate a similarity between the oil from the nearby Sierra field and the oil from the mine. Thus, it seems both geologically and chemically possible that oil in the mine originated in Cretaceous sediments. Variations in the composition of oil from the mine and differences between the mine oil and Sierra oil, notably in the distributions of hydrocarbons, are attributed to bacterial degradation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Research of the U.S. Geological Survey","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Gerrild, P.M., 1976, A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado: Journal of Research of the U.S. Geological Survey, v. 4, no. 5, p. 593-599.","productDescription":"7 p.","startPage":"593","endPage":"599","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue5/report.pdf"}],"country":"United States","state":"Colorado","county":"Ouray County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.1,\n              36.8\n            ],\n            [\n              -109.1,\n              39\n            ],\n            [\n              -106,\n              39\n            ],\n            [\n              -106,\n              36.8\n            ],\n            [\n              -109.1,\n              36.8\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd70e4b0d965cd9f22e0","contributors":{"authors":[{"text":"Gerrild, Peter M.","contributorId":37340,"corporation":false,"usgs":true,"family":"Gerrild","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472654,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","interactions":[{"subject":{"id":10744,"text":"ofr7787 - 1977 - Electronic thermal sensor and Landsat data collection platform technology","indexId":"ofr7787","publicationYear":"1977","noYear":false,"title":"Electronic thermal sensor and Landsat data collection platform technology"},"predicate":"SUPERSEDED_BY","object":{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","indexId":"70043109","publicationYear":"1976","noYear":false,"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>"},"id":1}],"lastModifiedDate":"2013-02-05T12:00:58","indexId":"70043109","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":360,"text":"Final Report","active":false,"publicationSubtype":{"id":6}},"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","docAbstract":"Five Data Collection Platforms (DCP) were integrated electronically with thermall sensing systems, emplaced and operated in an analog mode at selected thermally significant volcanic and geothermal sites. The DCP's transmitted 3260 messages comprising 26,080 ambient, surface, and near-surface temperature records at an accuracy of ±1.15 &deg;C for 1121 instrument days between November 14, 1972 and April 17, 1974. In harsh, windy, high-altitude volcanic environments the DCP functioned best with a small dipole antenna. Sixteen kg of alkaline batteries provided a viable power supply for the DCP systems, operated at a low-duty cycle, for 5 to 8 months. A proposed solar power supply system would lengthen the period of unattended operation of the system considerably. Special methods of data handling such as data storage via a proposed memory system would increase the significance of the twice-daily data reception enabling the DCP's to record full diurnal-temperature cycles at volcanic or geothermal sites. Refinements in the temperature-monitoring system designed and operated in experiment SR 251 included a backup system consisting of a multipoint temperature scanner, a servo mechanism and an analog-to-digital recorder. Improvements were made in temperature-probe design and in construction of corrosion-resistant seals by use of a hydrofluoric-acid-etching technique.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043109","usgsCitation":"Preble, D.M., Friedman, J.D., and Frank, D., 1976, Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>: Final Report, 64 p., https://doi.org/10.3133/70043109.","productDescription":"64 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":266996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5112382ce4b0ebe69d7eb6ce","contributors":{"authors":[{"text":"Preble, Duane M.","contributorId":36560,"corporation":false,"usgs":true,"family":"Preble","given":"Duane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Jules D.","contributorId":79464,"corporation":false,"usgs":true,"family":"Friedman","given":"Jules","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":472978,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frank, David","contributorId":13969,"corporation":false,"usgs":true,"family":"Frank","given":"David","affiliations":[],"preferred":false,"id":472976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043033,"text":"70043033 - 1976 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","interactions":[{"subject":{"id":14197,"text":"ofr75362 - 1975 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","indexId":"ofr75362","publicationYear":"1975","noYear":false,"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration"},"predicate":"SUPERSEDED_BY","object":{"id":70043033,"text":"70043033 - 1976 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","indexId":"70043033","publicationYear":"1976","noYear":false,"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration"},"id":1}],"lastModifiedDate":"2013-01-31T11:28:37","indexId":"70043033","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration","docAbstract":"An audio-magnetotelluric (AMT) system has been developed by the U.S. Geological Survey for low-cost reconnaissance exploration of geothermal regions. This is an electromagnetic sounding technique in which the scalar or Cagniard resistivity is computed at 12 frequencies logarithmically spaced from 7.5 to 18 600 Hz. Our system uses natural source fields except at the two upper frequencies of 10 200\nand 18 600 Hz where artificial VLF sources are available. As a reconnaissance technique we use AMT surveys in conjunction with regional gravity, magnetic, and telluric surveys. The exploration depth is a function of the resistivities of the lithologic section, but typically ranges from the surface to 0.2 km in low-resistivity areas and to greater than 2 km in high-resistivity regions. Results of the initial reconnaissance AMT surveys provide a rational basis for deciding on the extent of costlier follow-up surveys. As part of the U.S. Geological Survey geothermal program, surveys were conducted in Long Valley and Surprise Valley, California; the Vale, Ore-Weiser, Idaho region; and Bruneau-Grand View, Raft River, and Island Park regions of Idaho. AMT surveys in five additional known geothermal resource areas (KGRA's) have been scheduled for completion by May 1975. In the Raft River and Bruneau-Grand View regions and Long Valley, follow-up electrical surveys substantiated the effectiveness of the AMT technique for reconnaissance surveying.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Hoover, D., and Long, C.L., 1976, Audio-magnetotelluric methods in reconnaissance geothermal exploration, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1059-1064.","productDescription":"6 p.","startPage":"1059","endPage":"1064","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510ba07ae4b0947afa3c856c","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":472809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":472810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043506,"text":"70043506 - 1976 - Beacon Hill end moraine, Boston: new explanation of an important urban feature","interactions":[{"subject":{"id":14425,"text":"ofr7557 - 1975 - Beacon Hill End Moraine, Boston; a new explanation of an important urban feature","indexId":"ofr7557","publicationYear":"1975","noYear":false,"title":"Beacon Hill End Moraine, Boston; a new explanation of an important urban feature"},"predicate":"SUPERSEDED_BY","object":{"id":70043506,"text":"70043506 - 1976 - Beacon Hill end moraine, Boston: new explanation of an important urban feature","indexId":"70043506","publicationYear":"1976","noYear":false,"title":"Beacon Hill end moraine, Boston: new explanation of an important urban feature"},"id":1}],"lastModifiedDate":"2013-02-20T13:04:04","indexId":"70043506","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Beacon Hill end moraine, Boston: new explanation of an important urban feature","docAbstract":"The usefulness of geology to engineers is in direct proportion to how well it helps us predict the subsurface; these predictions, in turn, depend on our knowledge of the geomorphic processes that molded the terrain. The uncertainties of interpretation are particularly great in glaciated terrain because our understanding of both glacial processes and history is so incomplete, a fact well illustrated in Beacon Hill. Recent construction activities in the eastern part of the hill, until now classified as a drumlin, have shown that it is better interpreted as an end moraine formed by a Wisconsonian glacial readvance. Instead of the firm till that was anticipated as foundation material, excavations exposed a complex of sand, gravel, and clay, with only minor zones of till. The structure of these deposits strongly suggests that originally they were plates of the glacial bed that froze to the glacier and were transported englacially. Thrust faulting and other deformations are glacial structures formed within the ice in the glacier's terminal zone. In spite of the complex englacial history, these deposits lost little of their original appearance and intergranular relationships. Upon deglaciation, the frozen moraine thawed, and slumping formed complex secondary structures on the ridge's lower flanks.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Urban Gomorphology (Geological Society of America, Special Paper 174)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","usgsCitation":"Kaye, C., 1976, Beacon Hill end moraine, Boston: new explanation of an important urban feature, chap. <i>of</i> Urban Gomorphology (Geological Society of America, Special Paper 174), v. 174, p. 7-20.","productDescription":"14 p.","startPage":"7","endPage":"20","costCenters":[],"links":[{"id":267360,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Boston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.1911,42.2279 ], [ -71.1911,42.3989 ], [ -70.9232,42.3989 ], [ -70.9232,42.2279 ], [ -71.1911,42.2279 ] ] ] } } ] }","volume":"174","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511cc3f7e4b0f79c4d2cebc8","contributors":{"editors":[{"text":"Coates, Donald R.","contributorId":111569,"corporation":false,"usgs":true,"family":"Coates","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509212,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Kaye, Clifford A.","contributorId":17624,"corporation":false,"usgs":true,"family":"Kaye","given":"Clifford A.","affiliations":[],"preferred":false,"id":473735,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043504,"text":"70043504 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","interactions":[{"subject":{"id":15451,"text":"ofr7684 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","indexId":"ofr7684","publicationYear":"1976","noYear":false,"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70043504,"text":"70043504 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","indexId":"70043504","publicationYear":"1976","noYear":false,"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska"},"id":1}],"lastModifiedDate":"2013-02-13T14:55:50","indexId":"70043504","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","docAbstract":"Perhaps the world's longest and most complete onshore sedimentary record of late Cenozoic glaciation is preserved in the Gulf of Alaska Tertiary province that extends 800 km along the coast of southern Alaska. The Yakataga Formation, with an aggregate outcrop thickness of about 5,000 m, is characterized by variable amounts of distinctive neritic marine tillite-like diamictite and laminated siltstone containing dropstones interpreted as ice-rafted glacial debris. The lithology, sedimentary structures and molluscan fauna of the formation suggest that active tidal glaciers or an ice shelf were present along the landward margin of the basin possibly beginning in early or early middle Miocene time. Dropstone distribution in outcrop sections indicates that glaciers reached tidewater intermittently during the Miocene and were almost continually present throughout the Pliocene and much of the Pleistocene. Paleomagnetic and nannoplankton dating of the upper 1,181 m of the Yakataga Formation at Middleton Island indicate that this part of the sequence probably was entirely deposited during the Matuyama reversed polarity epoch of the Pleistocene during which the sedimentation rate was of the order of 1 m/1,000 years. Lithologically similar deposits of poorly consolidated sandy mud and pebbly mud continue to accumulate locally near tidal glaciers in the same area, and older late Quaternary deposits are undoubtedly present offshore. The anomalous late Cenozoic glaciation recorded in the sediments along the Gulf of Alaska margin reflects a fortuitous combination of a subsiding shelf basin adjacent to an area of extremely high elevations and exceptionally heavy precipitation, an environment that persists to the present.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Recent and ancient sedimentary environments in Alaska: Proceedings of the Alaska Geological Society Symposium held April 2-4, 1975, at Anchorage, Alaska","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Alaska Geological Society","publisherLocation":"Anchorage, AK","usgsCitation":"Plafker, G., and Addicott, W., 1976, Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska, <i>in</i> Recent and ancient sedimentary environments in Alaska: Proceedings of the Alaska Geological Society Symposium held April 2-4, 1975, at Anchorage, Alaska, p. 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,{"id":70039591,"text":"70039591 - 1976 - National Cartographic Information Center Newsletter No. 4","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039591","displayToPublicDate":"2012-01-01T13:05:24","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":373,"text":"Newsletter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"4","title":"National Cartographic Information Center Newsletter No. 4","docAbstract":"Last week, the editor of this publication was told to start signing the introduction. Something to do with credit given for work done. We look at it in the unfortunate light of accountability; our days under the bushel of anonymity are over. Speaking of accountability, it's about time we gave some recognition to the Newsletter's unknowing progenitor, John Wright, of the British Directorate of Overseas Surveys. Editorially and stylistically, the NCIC Newsletter owes him a large debt. Last month we received a suggestion from a reader that the Newsletter begin consistently listing prices for new products. In the publishing business, however, there is an infallible law of inflation prices increase as soon as they appear in print. We do try to quote exact prices where possible, and as our reader suggested, ballpark figures when we have to. In nearly all cases, additional information is available either by contacting the addresses listed in the article or indexed in the back or by calling NCIC's User Services Section. Numerous bits and pieces of information make up the bulk of this issue. Among them are the possibility of the Geological Survey issuing readable indexes to available topographic maps, the development of an NCIC classification system for U.S. cartographic data, and information on the publication of prototype topographic-bathymetric maps. Lastly, here is our quarterly solicitation for suggestions, comments, criticism, notes, and information for publication. Call it your bicentennial contribution to participatory democracy.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039591","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Cartographic Information Center Newsletter No. 4: Newsletter 4, 12 p., https://doi.org/10.3133/70039591.","productDescription":"12 p.","numberOfPages":"14","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261115,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report.pdf"},{"id":261116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a619ce4b0c8380cd71a77","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":535383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70039027,"text":"70039027 - 1976 - United States Geological Survey Annual Report, Fiscal Year 1975","interactions":[],"lastModifiedDate":"2017-05-19T18:43:48","indexId":"70039027","displayToPublicDate":"2012-01-01T11:12:54","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Annual Report, Fiscal Year 1975","docAbstract":"The Survey resumes the practice of annually summarizing the progress it has made in identifying the Nation's land, water, energy, and mineral resources, classifying federally owned mineral lands and waterpower sites, and in supervising the exploration and development of energy and mineral resources on Federal and Indian lands. The Annual Report for 1975 consists of five parts: * The Year in Review - a review of the issues and events which affected Survey programs and highlights of program accomplishments. * Perspectives - several short papers which address major resource issues and summarize recent advances in the earth sciences. * A description of the Survey's budget, programs, and accomplishments. * A set of statistical tables and related information which documents program trends, workloads, and accomplishments. * A compendium of Survey publications and information services available to the public. One purpose of this report is to increase public awareness and understanding of the Geological Survey's programs and, more generally, of the role of earth sciences information in helping to resolve many of the natural resource conflicts that face our society now and in the years ahead. To be useful, however, information must be available and readily accessible to those responsible for natural resource policy at the time that the decisions are made. This report emphasizes the types of information products and services provided by the Survey and tells how to obtain additional information.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039027","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, United States Geological Survey Annual Report, Fiscal Year 1975: Annual Report, vi, 194 p., https://doi.org/10.3133/70039027.","productDescription":"vi, 194 p.","numberOfPages":"203","costCenters":[],"links":[{"id":261263,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039027/report.pdf"},{"id":261264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039027/report-thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,16.916666666666668 ], [ 173,71.83333333333333 ], [ -66.95,71.83333333333333 ], [ -66.95,16.916666666666668 ], [ 173,16.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc8ee4b08c986b328cdd","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":535198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039401,"text":"70039401 - 1976 - Chart of conversion factors: From English to metric system and metric to English system","interactions":[],"lastModifiedDate":"2017-05-19T18:44:10","indexId":"70039401","displayToPublicDate":"2012-01-01T11:04:52","publicationYear":"1976","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":"Chart of conversion factors: From English to metric system and metric to English system","docAbstract":"The conversion factors in the following tables are for conversion of our customary (English) units of measurement to SI*units, and for convenience, reciprocals are shown for converting SI units back to the English system. The first table contains rule-of-thumb figures, useful for \"getting the feel\" of SI units or mental estimation. The succeeding tables contain factors accurate to 3 or more significant figures. Please refer to known reference volumes for additional accuracy, as well as for factors dealing with other scientific notation involving SI units.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039401","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Chart of conversion factors: From English to metric system and metric to English system: General Information Product, 5 p., https://doi.org/10.3133/70039401.","productDescription":"5 p.","costCenters":[],"links":[{"id":261548,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039401/report.pdf"},{"id":261549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039401/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f505e4b0c8380cd4c054","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":535290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039211,"text":"70039211 - 1976 - Man against volcano: The eruption on Heimaey, Vestmann Islands, Iceland","interactions":[],"lastModifiedDate":"2012-07-27T01:01:50","indexId":"70039211","displayToPublicDate":"2012-01-01T09:12:46","publicationYear":"1976","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":"Man against volcano: The eruption on Heimaey, Vestmann Islands, Iceland","docAbstract":"The U.S. Geological Survey carries out scientific studies in the geological, hydrological, and cartographic sciences generally within the 50 states, but also in cooperation with scientific organizations in many foreign countries for the investigation of unusual earth science phenomena throughout the world. The following material discusses the impact of the 1973 volcanic eruption of Eldfell on the fishing port of Vestmannaeyjar on the island of Heimaey, Iceland. Before the eruption was over, approximately one-third of the town of Vestmannaeyjar had been obliterated but, more importantly, the potential damage had been reduced markedly by the spraying of seawater onto the advancing lava flows, causing them to be slowed, stopped, or diverted from the undamaged portion of the town. The Survey's interest and involvement in the Heimaey eruption in Iceland was occasioned by the possibility that the procedures used to control the course of the flowing lava and to reduce the damage in a modern town may some day be needed in Hawaii and possibly even in the continental United States. This publication is based on the observations of two USGS geologists, Richard S. Williams, Jr. and James G. Moore, as well as on information from the Icelandic Ministry for Foreign Affairs, Icelandic scientists' reports through the Center for Short-Lived Phenomena, and other published scientific reports. A number of Icelandic scientists studied the scientific aspects of the eruption and the engineering aspects of the control of lava flows, in particular, Professors Thorbjb'rn Sigurgeirsson and Sigurdur Thorarinsson of the University of Iceland Science Institute. Also, Icelandic governmental officials provided logistical and other support, in particular, Mr. Steingnmur Hermannsson, Director, Icelandic National Research Council and Professor Magnus Magnusson, Director, University of Iceland Science Institute.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039211","collaboration":"Prepared in cooperation with the Icelandic Ministry for Foreign Affairs, The Center for Short-Lived Phenomena, the University of Iceland Science Institute, and the Icelandic National Research Council","usgsCitation":"Williams, R., and Moore, J., 1976, Man against volcano: The eruption on Heimaey, Vestmann Islands, Iceland: General Information Product, 19 p., https://doi.org/10.3133/70039211.","productDescription":"19 p.","numberOfPages":"20","costCenters":[],"links":[{"id":261386,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039211/report.pdf"},{"id":261387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039211/report-thumb.jpg"}],"country":"Iceland","city":"Vestmannaeyjar","otherGeospatial":"Heimaey Island;Vestmann Islands;Eldfell","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -20.333333333333332,63.38333333333333 ], [ -20.333333333333332,63.5 ], [ -20.166666666666668,63.5 ], [ -20.166666666666668,63.38333333333333 ], [ -20.333333333333332,63.38333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c5ae4b0c8380cd69bc6","contributors":{"authors":[{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":465789,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":465790,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039584,"text":"itr7221 - 1976 - Nature . . . an environmental yardstick","interactions":[],"lastModifiedDate":"2013-02-22T20:17:11","indexId":"itr7221","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":366,"text":"Information and Technology Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"72-21","title":"Nature . . . an environmental yardstick","docAbstract":"To one who has spent his professional career in geologic science, conservation always has had special meaning. In the measurements so necessary to his work the geologist develops an integrity in the use of numbers and in the qualifications attending the validity of numbers. Scientific analysis of geologic events and sequence develops a keen sense of what is coincidental, correlative, and consequential. The geologist applies his science in evaluating hazards to man as natural catastrophes and/or benefits to man such as earth materials that form the resource base of his society. But more than these the geologist has acquired a deep appreciation for the planet as a whole, its inner structure, its landscape, and the living things that abound.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/itr7221","usgsCitation":"Pecora, W.T., 1976, Nature . . . an environmental yardstick: Information and Technology Report 72-21, 16 p., https://doi.org/10.3133/itr7221.","productDescription":"16 p.","numberOfPages":"19","costCenters":[],"links":[{"id":261103,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/itr/1972/0021/report.pdf"},{"id":261104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/itr/1972/0021/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a638ee4b0c8380cd72568","contributors":{"authors":[{"text":"Pecora, William T.","contributorId":45167,"corporation":false,"usgs":true,"family":"Pecora","given":"William","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":466515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040758,"text":"70040758 - 1976 - Floods in New York, 1973 and 1974","interactions":[],"lastModifiedDate":"2017-09-13T18:22:37","indexId":"70040758","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-15","title":"Floods in New York, 1973 and 1974","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Robison, F., Embree, W., and Dunn, B., 1976, Floods in New York, 1973 and 1974: New York State Department of Environmental Conservation Report of Investigations RI-15, 81 p.","productDescription":"81 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263192,"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":"50a61d0ce4b0d446a665c9ce","contributors":{"authors":[{"text":"Robison, F.L.","contributorId":41889,"corporation":false,"usgs":true,"family":"Robison","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":468965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Embree, W.N.","contributorId":85143,"corporation":false,"usgs":true,"family":"Embree","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":468967,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":468966,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70005424,"text":"70005424 - 1976 - Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76","interactions":[],"lastModifiedDate":"2012-02-02T00:15:57","indexId":"70005424","displayToPublicDate":"2011-09-14T18:00:00","publicationYear":"1976","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":"Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Cheyenne, Wyoming","doi":"10.3133/70005424","usgsCitation":"U.S. Geological Survey, Water Resources Division, 1976, Water-resources investigations of the U.S. Geological Survey in the major coal and oil shale areas of Wyoming, 1975-76: Open-File Report, iv, 43 p. : maps ; 27 cm., https://doi.org/10.3133/70005424.","productDescription":"iv, 43 p. : maps ; 27 cm.","costCenters":[],"links":[{"id":204358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94451,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015018204738?urlappend=%3Bseq=3"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c28"}
]}