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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Person, W.J., 1975, Earthquakes: July-August 1974: Earthquake Information Bulletin (USGS), v. 6, no. 5, p. 29-31.","productDescription":"3 p.","startPage":"29","endPage":"31","numberOfPages":"3","costCenters":[],"links":[{"id":331975,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584fc569e4b00645734c5405","contributors":{"editors":[{"text":"Mallis, Robert","contributorId":77935,"corporation":false,"usgs":true,"family":"Mallis","given":"Robert","email":"","affiliations":[],"preferred":false,"id":655658,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Person, Waverly J.","contributorId":75143,"corporation":false,"usgs":true,"family":"Person","given":"Waverly","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":655657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178958,"text":"70178958 - 1975 - Earthquake strikes northern Pakistan","interactions":[],"lastModifiedDate":"2016-12-13T10:01:19","indexId":"70178958","displayToPublicDate":"2016-04-06T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1437,"text":"Earthquakes & Volcanoes (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake strikes northern Pakistan","docAbstract":"No abstract available.
Good-quality water is available from the sand-and-gravel, Niagara, and sandstone aquifers in Waukesha County, Wis. As much as 15 gallons per minute (0.95 litres per second) can be obtained from wells almost everywhere in the county. Several hundred gallons per minute are available from aquifers in the glacial drift that fill bedrock valleys to thicknesses of 300 feet (91 metres) or more. Estimated well yields from much of the surficial outwash in western Waukesha County exceed 500 gallons per minute (31 litres per second). Estimated well yields from most of the Niagara aquifer, a dolomite as much as 325 feet (99 metres) thick in the eastern two-thirds of the county, exceed 50 gallons per minute (3.2 litres per second). The sandstone aquifer underlies the entire county and ranges in thickness from about 400 feet (120 metres) in the northwest corner to about 2,400 feet (730 metres) in the southeast corner. This aquifer yields more than 1,000 gallons per minute (63 litres per second) to wells over most of the county and is the principal source for municipal and subdivision water. Ground water in Waukesha County is of good quality and is suitable for most uses. Most of the water is a calcium magnesium bicarbonate type, is very hard [more than 180 mg/l (milligrams per litre) hardness], and requires softening for some uses. The ground water locally contains iron and manganese concentrations that exceed the limits (0.3 and 0.05 mg/l, respectively) recommended by the U.S. Public Health Service (1962, p. 7). Water high in sulfate and dissolved solids (saline water) is present locally in the Niagara and sandstone aquifers. Water from one well contained excessive nitrate (more than 45 mg/l). With one exception, wells sampled at irregular intervals indicated no significant changes in their chemical characteristics with time. About 24.3 million gallons per day (1.06 cubic metres per second) of ground water was pumped in the county in 1970. Sixty-two percent was withdrawn from the sandstone aquifer. More than one-half of the latter amount was for domestic use, and more than one-third was for industrial and commercial uses.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Gonthier, J.B., 1975, Ground-water resources and geology of Waukesha County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 29, vii, 47 p.","productDescription":"vii, 47 p.","numberOfPages":"55","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308483,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350393,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic29/"}],"country":"United States","state":"Wisconsin","county":"Waukesha County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5401,43.1978],[-88.4183,43.1964],[-88.3027,43.1954],[-88.1827,43.1948],[-88.0639,43.194],[-88.0664,43.1076],[-88.0682,43.0202],[-88.0692,42.9725],[-88.0675,42.9334],[-88.0699,42.8447],[-88.1868,42.8451],[-88.3044,42.8444],[-88.5413,42.8445],[-88.5413,42.9341],[-88.5407,43.0232],[-88.5407,43.111],[-88.5401,43.1978]]]},\"properties\":{\"name\":\"Waukesha\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ecae4b058f706e512db","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70157468,"text":"70157468 - 1975 - Ground-water resources and geology of Jefferson County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:37:35","indexId":"70157468","displayToPublicDate":"2015-04-13T08:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Ground-water resources and geology of Jefferson County, Wisconsin","docAbstract":"A steadily increasing population in Jefferson County, Wisconsin, is expanding the need for good-quality ground water. This need can be met by good-quality water available from the sand-and-gravel, Galena-Platteville, and sandstone aquifers. As much as 15 gallons per minute (0.95 liters per second) can be obtained from wells almost everywhere in the county. Yields of more than 1,000 gallons per minute (63 liters per second) are available from glacial drift where it contains a sufficient thickness of saturated sand and gravel. The Galena-Platteville aquifer is a dolomite that occurs mainly in the eastern one-half of the county and is locally more than 300 feet (90 meters) thick. Estimated well yields from this aquifer exceed 500 gallons per minute (32 liters per second). The sandstone aquifer underlies nearly the entire county except for small areas in the northwest corner. It is more than 1,100 feet (330 meters) thick in the southwest along the Dane-Jefferson County line. This aquifer is capable of yielding more than 1,000 gallons per minute (63 liters per second) to wells in much of the county and is the principal source of municipal water. The chemical quality of water from the three aquifers is similar. The water is very hard, having a median hardness between 315 and 325 milligrams per liter. Median values for dissolved solids range between 325 and 349 milligrams per liter. Iron and manganese commonly are present in bothersome amounts (combined total exceeding 0.3 milligrams per liter. About 13.0 million gallons per day (0.570 cubic meters per second) of ground water was pumped in the county in 1972, 87 percent from the sandstone aquifer. About 62 percent of the total water pumped was for industrial and commercial purposes, 26 percent for residential use, and 12 percent for municipal, irrigation, and institutional use.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Borman, R.G., and Trotta, L.C., 1975, Ground-water resources and geology of Jefferson County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 33, vi, 31 p.","productDescription":"vi, 31 p.","numberOfPages":"39","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308479,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350394,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic33/"}],"country":"United States","state":"Wisconsin","county":"Jefferson County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5401,43.1978],[-88.5407,43.111],[-88.5407,43.0232],[-88.5413,42.9341],[-88.5413,42.8445],[-88.66,42.8453],[-88.7757,42.8455],[-88.8951,42.8457],[-89.0119,42.8471],[-89.013,42.8762],[-89.0132,42.9353],[-89.0107,43.0271],[-89.0109,43.0849],[-89.01,43.1131],[-89.0094,43.2],[-88.8919,43.1995],[-88.7732,43.1998],[-88.6563,43.1986],[-88.5401,43.1978]]]},\"properties\":{\"name\":\"Jefferson\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d5","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trotta, L. C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70157470,"text":"70157470 - 1975 - The availability of ground water for irrigation in the Rice Lake-Eau Claire Area, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:38:23","indexId":"70157470","displayToPublicDate":"2015-03-30T04:15:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"The availability of ground water for irrigation in the Rice Lake-Eau Claire Area, Wisconsin","docAbstract":"An abundance of ground water of excellent chemical quality for irrigating crops is available from glacial outwash sand and gravel and from the underlying sandstones in the Rice Lake-Eau Claire area.
\nThick deposits of glacial outwash sand and gravel in the valleys of the Red Cedar and lower Chippewa Rivers yield more than 1,000 gallons per minute (63 lit res per second) to many wells. Large tracts of irrigable soils, delineated in two subareas (Rice Lake and Cameron) in Barron County and one subarea (Menomonie) in Dunn County, lie within the outwash plains where ground water is available in large quantities. Yields are especially large in the Rice Lake and Cameron subareas where the sand and gravel is highly permeable and the thickness of saturated aquifer exceeds 250 feet (75 metres). Yields generally are less than 1,000 gallons per minute (63 litres per second) in the Menomonie subarea where large amounts of clay locally reduce the permeability of the aquifer and the thickness of saturated aquifer is less than 200 feet (60 metres).
\nAdequate water for irrigation is available also from sandstone underlying the glacial outwash plains. Because the two aquifers generally are connected hydraulically, wells penetrating the sandstone also withdraw water indirectly from the glacial drift. Most irrigation wells in Barron County withdraw water from glacial outwash; more than half the irrigation wells in Dunn County withdraw water from sandstone.
\nIn most years, recharge to the ground-water reservoir is 6 to 8 inches (150 to 200 millimetres), which is more than ample to sustain pumping for irrigation without lowering the water table significantly.
\nGround water in the area is a calcium bicarbonate water that ranges in dissolved-solids concentration from 35 to 330 milligrams per litre. Concentrations of sodium and' boron are very low.
","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Bell, E., and Hindall, S.M., 1975, The availability of ground water for irrigation in the Rice Lake-Eau Claire Area, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 31, viii, 65 p.","productDescription":"viii, 65 p.","numberOfPages":"76","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350395,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic31/"}],"country":"United States","state":"Wisconsin","county":"Barron County, Chippewa County, Dunn County, Eau Claire County, Pepin County, Washburn County","city":"Cameron, Eau Claire, Menomonie, Rice Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.0050048828125,\n 44.77111175531266\n ],\n [\n -92.0050048828125,\n 45.57175504130605\n ],\n [\n -91.1865234375,\n 45.57175504130605\n ],\n [\n -91.1865234375,\n 44.77111175531266\n ],\n [\n -92.0050048828125,\n 44.77111175531266\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ee9e4b058f706e51322","contributors":{"authors":[{"text":"Bell, E.A.","contributorId":27931,"corporation":false,"usgs":true,"family":"Bell","given":"E.A.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":573257,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047581,"text":"70047581 - 1975 - Stratigraphy of Atlantic coastal margin of United States north of Cape Hatteras: Brief survey","interactions":[{"subject":{"id":15377,"text":"ofr741084 - 1974 - Stratigraphy of the Atlantic continental margin of the United States north of Cape Hatteras; a brief survey","indexId":"ofr741084","publicationYear":"1974","noYear":false,"title":"Stratigraphy of the Atlantic continental margin of the United States north of Cape Hatteras; a brief survey"},"predicate":"SUPERSEDED_BY","object":{"id":70047581,"text":"70047581 - 1975 - Stratigraphy of Atlantic coastal margin of United States north of Cape Hatteras: Brief survey","indexId":"70047581","publicationYear":"1975","noYear":false,"title":"Stratigraphy of Atlantic coastal margin of United States north of Cape Hatteras: Brief survey"},"id":1}],"lastModifiedDate":"2023-01-25T16:52:02.792993","indexId":"70047581","displayToPublicDate":"2013-01-01T15:20:00","publicationYear":"1975","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":"Stratigraphy of Atlantic coastal margin of United States north of Cape Hatteras: Brief survey","docAbstract":"A synthesis of studies of sea-floor outcrops of the sedimentary wedge beneath the northeastern United States continental shelf and slope and a reassessment of coastal plain Mesozoic stratigraphy, particularly of the coastal margin, provide insight for estimating the oil and gas potential and provide geologic control for marine seismic investigations of the Atlantic continental margin.
The oldest strata known to crop out on the continental slope are late Campanian in age. The Cretaceous-Tertiary contact along the slope ranges from a water depth of 0.6 to 1.5 km south of Georges Bank to 1.8 km in Hudson Canyon. Few samples are available from Tertiary and Late Cretaceous outcrops along the slope.
Sediments of the Potomac Group, chiefly of Early Cretaceous age, constitute a major deltaic sequence in the emerged coastal plain. This thick sequence lies under coastal Virginia, Maryland, Delaware, southeastern New Jersey, and the adjacent continental shelf. Marine sands associated with this deltaic sequence may be present seaward under the outer continental shelf. South of the Norfolk arch, under coastal North Carolina, carbonate rocks interfinger with Lower Cretaceous clastic strata.
From all available data, Mesozoic correlations in coastal wells between coastal Virginia and Long Island have been revised. The Upper-Lower Cretaceous boundary is placed at the transition between Albian and Cenomanian floras. Potential hydrocarbon source beds are present along the coast in the subsurface sediments of Cretaceous age. Potential reservoir sandstones are abundant in this sequence.
","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/83D91FFB-16C7-11D7-8645000102C1865D","usgsCitation":"Perry, W.J., Minard, J.P., Weed, E.G., Robbins, E.I., and Rhodehamel, E., 1975, Stratigraphy of Atlantic coastal margin of United States north of Cape Hatteras: Brief survey: American Association of Petroleum Geologists Bulletin, v. 59, no. 9, p. 1529-1548, https://doi.org/10.1306/83D91FFB-16C7-11D7-8645000102C1865D.","productDescription":"20 p.","startPage":"1529","endPage":"1548","costCenters":[],"links":[{"id":276550,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Atlantic coastal plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.64468881612208,\n 25.1795362704098\n ],\n [\n -73.8280244352542,\n 24.803932460591597\n ],\n [\n -63.57731702802809,\n 42.60769632479955\n ],\n [\n -68.07033954617219,\n 45.456909094649006\n ],\n [\n -72.25318054701177,\n 43.965208680871456\n ],\n [\n -81.04912758160249,\n 35.70883333730893\n ],\n [\n -83.65269742198177,\n 31.073657668062182\n ],\n [\n -83.90174386776873,\n 27.691092309247523\n ],\n [\n -80.80104545039107,\n 25.02119048598709\n ],\n [\n -80.56390745366714,\n 25.184090956371847\n ],\n [\n -80.64468881612208,\n 25.1795362704098\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"59","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03fee4b0026c2bc11cd0","contributors":{"authors":[{"text":"Perry, W. J.","contributorId":24752,"corporation":false,"usgs":true,"family":"Perry","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":482448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minard, J. P.","contributorId":8065,"corporation":false,"usgs":true,"family":"Minard","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":482447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weed, Elaine G. A.","contributorId":91496,"corporation":false,"usgs":true,"family":"Weed","given":"Elaine","email":"","middleInitial":"G. A.","affiliations":[],"preferred":false,"id":482449,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robbins, E. I.","contributorId":101269,"corporation":false,"usgs":true,"family":"Robbins","given":"E.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":482451,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rhodehamel, E. C.","contributorId":91517,"corporation":false,"usgs":true,"family":"Rhodehamel","given":"E. C.","affiliations":[],"preferred":false,"id":482450,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70047533,"text":"70047533 - 1975 - Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort Seas","interactions":[{"subject":{"id":19122,"text":"ofr75124 - 1975 - Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort seas","indexId":"ofr75124","publicationYear":"1975","noYear":false,"title":"Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort seas"},"predicate":"SUPERSEDED_BY","object":{"id":70047533,"text":"70047533 - 1975 - Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort Seas","indexId":"70047533","publicationYear":"1975","noYear":false,"title":"Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort Seas"},"id":1}],"lastModifiedDate":"2017-05-04T11:19:35","indexId":"70047533","displayToPublicDate":"2013-01-01T14:26:00","publicationYear":"1975","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort Seas","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Canada's continental margins and offshore petroleum exploration (CSPG Memoir 4)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Canadian Society of Petroleum Geologists","publisherLocation":"Calgary, AB","usgsCitation":"Grantz, A., Holmes, M., and Kososki, B.A., 1975, Geologic framework of the Alaskan Continental Terrace in the Chukchi and Beaufort Seas, in Canada's continental margins and offshore petroleum exploration (CSPG Memoir 4), p. 669-700.","productDescription":"32 p.","startPage":"669","endPage":"700","costCenters":[],"links":[{"id":276236,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276235,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/cspg_sp/data/004/004001/v_cspgsp004v.htm"}],"country":"Canada, United States","otherGeospatial":"Alaskan Continental Terrace,Beaufort Sea, Chukchi sea","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5204bde6e4b0403aa62629fd","contributors":{"editors":[{"text":"Yorath, C.J.","contributorId":43620,"corporation":false,"usgs":true,"family":"Yorath","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":509554,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Parker, E.R.","contributorId":112150,"corporation":false,"usgs":true,"family":"Parker","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":509555,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Glass, D.J.","contributorId":112816,"corporation":false,"usgs":true,"family":"Glass","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":509556,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Grantz, A.","contributorId":60378,"corporation":false,"usgs":true,"family":"Grantz","given":"A.","email":"","affiliations":[],"preferred":false,"id":482288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holmes, M.L.","contributorId":89528,"corporation":false,"usgs":true,"family":"Holmes","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":482290,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kososki, B. A.","contributorId":85182,"corporation":false,"usgs":true,"family":"Kososki","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":482289,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70047834,"text":"70047834 - 1975 - San Simeon-Hosgri fault system, coastal California: economic and environmental implications","interactions":[{"subject":{"id":9300,"text":"ofr75533 - 1975 - San Simeon-Hosgri fault system, coastal California: economic and environmental implications","indexId":"ofr75533","publicationYear":"1975","noYear":false,"title":"San Simeon-Hosgri fault system, coastal California: economic and environmental implications"},"predicate":"SUPERSEDED_BY","object":{"id":70047834,"text":"70047834 - 1975 - San Simeon-Hosgri fault system, coastal California: economic and environmental implications","indexId":"70047834","publicationYear":"1975","noYear":false,"title":"San Simeon-Hosgri fault system, coastal California: economic and environmental implications"},"id":1}],"lastModifiedDate":"2013-08-26T14:25:12","indexId":"70047834","displayToPublicDate":"2013-01-01T14:18:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"San Simeon-Hosgri fault system, coastal California: economic and environmental implications","docAbstract":"Comparison of stratigraphic sections exposed on opposite sides of the late Quaternary San Simeon-Hosgri fault system at Point Sal and near San Simeon (Fig. 1) strongly suggests large-scale lateral displacement.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AAAS","doi":"10.1126/science.190.4221.1291","usgsCitation":"Hall, C., 1975, San Simeon-Hosgri fault system, coastal California: economic and environmental implications: Science, v. 190, no. 4221, p. 1291-1294, https://doi.org/10.1126/science.190.4221.1291.","productDescription":"4 p.","startPage":"1291","endPage":"1294","costCenters":[],"links":[{"id":277011,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":277010,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1126/science.190.4221.1291"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42.0 ], [ -114.1,42.0 ], [ -114.1,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","volume":"190","issue":"4221","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78ece4b01458f7842984","contributors":{"authors":[{"text":"Hall, C.A. 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A leachate was detected in ground water within and beneath two sites where the water table is very near land surface and refuse is deposited either at or below the water table in some parts of the filled areas. 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[Talk delivered to Wyoming Geological Association, Caspar, WY, Jan. 3, 1975]","indexId":"ofr7586","publicationYear":"1975","noYear":false,"title":"Lithium in sediments and brines--how, why, and where to search? 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The Clayton Valley, Nev., subsurface lithium brine has been the major source of lithium carbonate since about 1967, but the life of this brine field is probably limited to several more decades at the present rate of production. Lithium is so highly soluble during weathering and in sedimentary environments that no lithium-rich sedimentary minerals other than clays have been identified to date. The known deposits of lithium, such as the clay mineral hectorite and the lithium-rich brines, occur in closed desert basins of the Southwest in association with nonmarine evaporites. However, the ultimate source for the lithium in these deposits may be from hydrothermal solutions. The search for previously unreported deposits of nonpegmatitic lithium should consider its probable association, not only with nonmarine evaporite minerals, but also with recent volcanic and tectonic activity, as well as with deposits of boron, beryllium, fluorine, manganese, and possibly phosphate.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Vine, J.D., 1975, Lithium in sediments and brines--how, why and where to search: Journal of Research of the U.S. Geological Survey, v. 3, no. 4, p. 479-485.","productDescription":"7 p.","startPage":"479","endPage":"485","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":265747,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265781,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue4/report.pdf","text":"Report","size":"24.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f7da1be4b0faa3ef21ebf6","contributors":{"authors":[{"text":"Vine, James D.","contributorId":105287,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":472005,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046166,"text":"70046166 - 1975 - Geology of Porcupine Mountains in Carp River and White Pine Quadrangles, Michigan","interactions":[{"subject":{"id":42270,"text":"ofr741052 - 1974 - Bedrock geology of the Porcupine Mountains, Michigan","indexId":"ofr741052","publicationYear":"1974","noYear":false,"title":"Bedrock geology of the Porcupine Mountains, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":70046166,"text":"70046166 - 1975 - Geology of Porcupine Mountains in Carp River and White Pine Quadrangles, Michigan","indexId":"70046166","publicationYear":"1975","noYear":false,"title":"Geology of Porcupine Mountains in Carp River and White Pine Quadrangles, Michigan"},"id":1}],"lastModifiedDate":"2013-05-29T13:11:51","indexId":"70046166","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","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":"Geology of Porcupine Mountains in Carp River and White Pine Quadrangles, Michigan","docAbstract":"The Porcupine Mountains are the eroded remnants of the upper limb of an anticline that is faulted along most of its southern, overturned, limb. The exposed rocks include about 5,000 ft (1,525 m) of middle Keweenawan intermediate to mafic lava flows interbedded with subordinate lithic sedimentary rocks and also include about 3,000 ft (915 m) of overlying middle and upper Keweenawan sedimentary rocks. The sediments are derived from lower Keweenawan and older rocks. The structural relief is at least 8,000 ft (2,440 m) between the crest of the Porcupine Mountains anticline and the trough of the Iron River syncline about 5 mi (8 km) to the south. The reverse fault along the southern, overturned, limb of the anticline has a displacement of about 5,000 ft (1,525 m).","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":"Hubbard, H., 1975, Geology of Porcupine Mountains in Carp River and White Pine Quadrangles, Michigan: Journal of Research of the U.S. Geological Survey, v. 3, no. 5, p. 519-528.","productDescription":"10 p.","startPage":"519","endPage":"528","costCenters":[],"links":[{"id":272960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":272959,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue5/report.pdf"}],"country":"United States","state":"Michigan","otherGeospatial":"Porcupine Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.42,41.7 ], [ -90.42,48.29 ], [ -82.41,48.29 ], [ -82.41,41.7 ], [ -90.42,41.7 ] ] ] } } ] }","volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a72369e4b09db86f875cf5","contributors":{"authors":[{"text":"Hubbard, Harold A.","contributorId":99203,"corporation":false,"usgs":true,"family":"Hubbard","given":"Harold A.","affiliations":[],"preferred":false,"id":479080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70042935,"text":"70042935 - 1975 - Possible extension of mineral belts, northern part of Coeur d'Alene district, Idaho","interactions":[{"subject":{"id":13860,"text":"ofr7467 - 1974 - Posssible extension of mineral belts, northern part of Coeur d'Alene district, Idaho","indexId":"ofr7467","publicationYear":"1974","noYear":false,"title":"Posssible extension of mineral belts, northern part of Coeur d'Alene district, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70042935,"text":"70042935 - 1975 - Possible extension of mineral belts, northern part of Coeur d'Alene district, Idaho","indexId":"70042935","publicationYear":"1975","noYear":false,"title":"Possible extension of mineral belts, northern part of Coeur d'Alene district, Idaho"},"id":1}],"lastModifiedDate":"2013-01-29T10:33:59","indexId":"70042935","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","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":"Possible extension of mineral belts, northern part of Coeur d'Alene district, Idaho","docAbstract":"The ore deposits in the northern part of the Coeur d'Alene district are located within rocks of the Belt Supergroup that have been intruded by Cretaceous quartz monzonites. Lead-zinc-silver replacement veins constitute most of the deposits. The geometry of the district has been modified by post-ore faulting along the Osburn, Dobson Pass, and other faults. The original position of the Gem stocks, before their separation from the Diego Peak stocks by the Dobson Pass fault, can be approximately reconstructed by moving the truncated stocks and associated geochemical dispersion patterns back into matching positions. The known mineral belts are defined by dispersion patterns of both lead and the Pb:Zn ratio. Similar dispersion patterns of lead and the Pb:Zn ration northwest of the original position of the Gem stocks suggest that the mineral belts extend into that area.","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":"Gott, G.B., and Botbol, J.M., 1975, Possible extension of mineral belts, northern part of Coeur d'Alene district, Idaho: Journal of Research of the U.S. Geological Survey, v. 3, no. 1, p. 1-7.","productDescription":"7 p.","startPage":"1","endPage":"7","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266673,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266672,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue1/report.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,42.0 ], [ -117.24,49.0 ], [ -111.0,49.0 ], [ -111.0,42.0 ], [ -117.24,42.0 ] ] ] } } ] }","volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd8ce4b0d965cd9f2366","contributors":{"authors":[{"text":"Gott, Garland B.","contributorId":8837,"corporation":false,"usgs":true,"family":"Gott","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":472617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Botbol, Joseph M.","contributorId":19857,"corporation":false,"usgs":true,"family":"Botbol","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472618,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70042719,"text":"70042719 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","interactions":[{"subject":{"id":14933,"text":"ofr75304 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","indexId":"ofr75304","publicationYear":"1975","noYear":false,"title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70042719,"text":"70042719 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","indexId":"70042719","publicationYear":"1975","noYear":false,"title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin"},"id":1}],"lastModifiedDate":"2013-01-18T15:34:06","indexId":"70042719","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":259,"text":"Information Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"30","title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","docAbstract":"The extensive use of ground water for water supply within Dane County has resulted in the need for an appraisal of the area's ground-water resources. Water-resources planners and other water-oriented groups have expressed concern over ground-water level declines and reductions in streamflow that are occurring as a result of heavy pumping. Digital-computer modeling techniques were used to estimate hydrologic changes in the aquifer system that would be caused by continued development. The system was modeled as a two-aquifer system consisting of a confined sandstone aquifer overlain by a leaky unconfined aquifer and underlain by impermeable bedrock. The physical properties of the aquifer system needed for the model were approximated using aquifer-test data and well-log data and by matching observed hydrologic changes in the system with corresponding changes computed by the model. Computed hydrologic changes do not represent a serious depletion of the available ground-water supply for the foreseeable future. Maximum added regional declines in ground-water levels (drawdowns) from 1970 to 1990 were computed to be approximately 10 feet (3 metres) in the unconfined aquifer and approximately 40 feet (12 metres) in the confined aquifer. It is computed that for the same period the average annual streamflow from the upper Yahara River basin would be reduced by approximately 29 cubic feet per second (0.82 cubic metre per second). These changes are computed based on estimated development trends for the confined sandstone aquifer.","language":"English","publisher":"Wisconsin Geological and Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by the United States Department of the Interior Geological Survey in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"McLeod, R., 1975, A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin: Information Circular 30, vii, 40 p.; ill.; maps.","productDescription":"vii, 40 p.; ill.; maps","startPage":"i","endPage":"40","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":265977,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265976,"type":{"id":11,"text":"Document"},"url":"https://wisconsingeologicalsurvey.org/pdfs/IC30.pdf"}],"country":"United States","state":"Wisconsin","county":"Dane County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.8394,42.8448 ], [ -89.8394,43.2943 ], [ -89.0084,43.2943 ], [ -89.0084,42.8448 ], [ -89.8394,42.8448 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d34e4b061045bf9aba5","contributors":{"authors":[{"text":"McLeod, R.S.","contributorId":7283,"corporation":false,"usgs":true,"family":"McLeod","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":472112,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70042682,"text":"70042682 - 1975 - Apollo 12 voice transcript pertaining to the geology of the landing site","interactions":[{"subject":{"id":56052,"text":"ofr70288 - 1970 - Paraphrased geologic excerpts from Apollo 12 mission","indexId":"ofr70288","publicationYear":"1970","noYear":false,"title":"Paraphrased geologic excerpts from Apollo 12 mission"},"predicate":"SUPERSEDED_BY","object":{"id":70042682,"text":"70042682 - 1975 - Apollo 12 voice transcript pertaining to the geology of the landing site","indexId":"70042682","publicationYear":"1975","noYear":false,"title":"Apollo 12 voice transcript pertaining to the geology of the landing site"},"id":1}],"lastModifiedDate":"2013-01-17T13:53:45","indexId":"70042682","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","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":"Apollo 12 voice transcript pertaining to the geology of the landing site","docAbstract":"This document is an edited record of the conversations between the Apollo 12 astronauts and mission control pertaining to the geology of the landing site. It contains all discussions and observations documenting the lunar landscape, its geologic characteristics, the rocks and soils collected, and the lunar surface photographic record along with supplementary remarks essential to the continuity of events during the mission. This transcript is derived from audio tapes and the NASA Technical Air-to-Ground Voice Transcription and includes time of transcription, and photograph and sample numbers. The report also includes a glossary, landing site amp, and sample table.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70042682","usgsCitation":"Bailey, N.G., and Ulrich, G., 1975, Apollo 12 voice transcript pertaining to the geology of the landing site: Final Report, 175 p., https://doi.org/10.3133/70042682.","productDescription":"175 p.","numberOfPages":"179","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265809,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":265808,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a12/Apollo12VoiceTranscript-Geology.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f92b7ae4b0727905955f3f","contributors":{"authors":[{"text":"Bailey, N. G.","contributorId":14408,"corporation":false,"usgs":true,"family":"Bailey","given":"N.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":472046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":472047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046307,"text":"70046307 - 1975 - Geology of Griggs and Steele Counties","interactions":[],"lastModifiedDate":"2018-05-23T12:18:49","indexId":"70046307","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64-1","title":"Geology of Griggs and Steele Counties","docAbstract":"Griggs and Steele Counties, located at the eastern edge of the Williston basin, are underlain by 400 to 2,600 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The Cretaceous Greenhorn, Carlile, Niobrara, and Pierre Formations lie directly beneath the glacial drift, and shale of the Pierre Formation is exposed in several places along the Sheyenne River. The Pleistocene Coleharbor Formation, which covers most of the area, consists mainly of glacial, fluvial, and lake sediment. The Coleharbor Formation averages 200 to 300 feet thick, but it is as much as 550 feet thick in some of the buried valleys. The Holocene Walsh Formation occurs in parts of the area, chiefly sloughs and river bottomland. It consists mainly of alluvial and eolian sediment. Griggs County and the western two-thirds of Steele County are part of the Drift Prairie, which is characterized by flat to gently rolling topography that is rugged in areas of end moraines and intense ice thrusting, subdued on the ground moraine and outwash plains. Associated with these major landforms are numerous washboard moraines, drumlins, eskers, kames, meltwater trenches, and water-washed areas. The eastern third of Steele County is a nearly flat area covered by lake deposits of the glacial Lake Agassiz. As the Late Wisconsinan glacier in eastern North Dakota thinned and receded eastward, it was increasingly affected by the topography over which it was flowing. This resulted in lobation of the glacier. Locally intense areas of thrusting developed within the lobate glacier, and large blocks of subglacial material were moved short distances. Large areas of Griggs County were washed by water flowing from the glacier, and in some areas gravel and sand were deposited. Continued withdrawal of the glacier resulted in ponding of melt water in parts of the two counties. These and other ponds tended to coalesce at lower and lower elevations, eventually forming Lake Agassiz, which flooded part of eastern Steele County.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared by the North Dakota Geological Survey in cooperation with the North Dakota State Water Commission, the water management districts of Griggs and Steele Counties, and the United States Geological Survey; this report was also published as North Dakota County Ground-Water Studies 21-1","usgsCitation":"Bluemle, J.P., 1975, Geology of Griggs and Steele Counties: Bulletin 64-1, vii, 49 p.; Maps: 2 Sheets: 36 x 18 inches.","productDescription":"vii, 49 p.; Maps: 2 Sheets: 36 x 18 inches","numberOfPages":"50","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":273368,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046307.png"},{"id":273366,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-251/GriggsSteele_Part_1.pdf"},{"id":273367,"type":{"id":17,"text":"Plate"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-252/GriggsSteele_Part_1_Plates.pdf"}],"country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4504,47.6742 ], [ -97.4504,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd2e4b022a6a540f9cb","contributors":{"authors":[{"text":"Bluemle, John P.","contributorId":104375,"corporation":false,"usgs":true,"family":"Bluemle","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":479433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70042868,"text":"70042868 - 1975 - A model for earthquakes near Palisades Reservoir, southeast Idaho","interactions":[{"subject":{"id":15832,"text":"ofr7512 - 1975 - A model for earthquakes near Palisades Reservoir, southeast Idaho","indexId":"ofr7512","publicationYear":"1975","noYear":false,"title":"A model for earthquakes near Palisades Reservoir, southeast Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70042868,"text":"70042868 - 1975 - A model for earthquakes near Palisades Reservoir, southeast Idaho","indexId":"70042868","publicationYear":"1975","noYear":false,"title":"A model for earthquakes near Palisades Reservoir, southeast Idaho"},"id":1}],"lastModifiedDate":"2013-01-26T21:23:44","indexId":"70042868","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","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 model for earthquakes near Palisades Reservoir, southeast Idaho","docAbstract":"The Palisades Reservoir seems to be triggering earthquakes: epicenters are concentrated near the reservoir, and quakes are concentrated in spring, when the reservoir level is highest or is rising most rapidly, and in fall, when the level is lowest. Both spring and fall quakes appear to be triggered by minor local stresses superposed on regional tectonic stresses; faulting is postulated to occur when the effective normal stress across a fault is decreased by a local increase in pore-fluid pressure. The spring quakes tend to occur when the reservoir level suddenly rises: increased pore pressure pushes apart the walls of the graben flooded by the reservoir, thus decreasing the effective normal stress across faults in the graben. The fall quakes tend to occur when the reservoir level is lowest: water that gradually infiltrated poorly permeable (fault-gouge?) zones during high reservoir stands is then under anomalously high pressure, which decreases the effective normal stress across faults in the poorly permeable zones.","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":"Schleicher, D., 1975, A model for earthquakes near Palisades Reservoir, southeast Idaho: Journal of Research of the U.S. Geological Survey, v. 3, no. 4, p. 393-400.","productDescription":"8 p.","startPage":"393","endPage":"400","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":266569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue4/report.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Palisades Reservoir","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":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51050907e4b091226576e99e","contributors":{"authors":[{"text":"Schleicher, David","contributorId":49350,"corporation":false,"usgs":true,"family":"Schleicher","given":"David","affiliations":[],"preferred":false,"id":472446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046195,"text":"70046195 - 1975 - Simple Bouguer gravity anomaly map of Utah","interactions":[{"subject":{"id":40281,"text":"ofr72297 - 1972 - Complete Bouguer gravity anomaly map of parts of Beaver, Iron, and Millard counties, southwestern Utah","indexId":"ofr72297","publicationYear":"1972","noYear":false,"title":"Complete Bouguer gravity anomaly map of parts of Beaver, Iron, and Millard counties, southwestern Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70046195,"text":"70046195 - 1975 - Simple Bouguer gravity anomaly map of Utah","indexId":"70046195","publicationYear":"1975","noYear":false,"title":"Simple Bouguer gravity anomaly map of Utah"},"id":1}],"lastModifiedDate":"2013-05-30T12:53:23","indexId":"70046195","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":264,"text":"Map","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"37","title":"Simple Bouguer gravity anomaly map of Utah","language":"English","publisher":"Utah Geological and Mineral Survey","publisherLocation":"Salt Lake City, UT","usgsCitation":"Cook, K.L., and Utah Geological and Mineralogical Survey, 1975, Simple Bouguer gravity anomaly map of Utah: Map 37, Map: 1 Sheet.","productDescription":"Map: 1 Sheet","costCenters":[],"links":[{"id":273019,"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\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -109.0,42.0 ], [ -109.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51a874eae4b082d85d5ed8ea","contributors":{"authors":[{"text":"Cook, Kenneth L.","contributorId":91099,"corporation":false,"usgs":true,"family":"Cook","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":479135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Utah Geological and Mineralogical Survey","contributorId":128186,"corporation":true,"usgs":false,"organization":"Utah Geological and Mineralogical Survey","id":535522,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70006806,"text":"70006806 - 1975 - You asked for it! Answers to questions about fish farming: Part III","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"70006806","displayToPublicDate":"2012-08-08T16:36:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Answers to questions about fish farming: Part III","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None","usgsCitation":"Martin, M., 1975, You asked for it! Answers to questions about fish farming: Part III: Commercial Fish Farmer and Aquaculture News, v. 2, no. 1, p. 35-35.","productDescription":"1 p.","startPage":"35","endPage":"35","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd227e4b08c986b32f66e","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":355277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006807,"text":"70006807 - 1975 - You asked for it! Answers to questions from persons interested in fish farming: Part III","interactions":[],"lastModifiedDate":"2013-01-18T14:50:51","indexId":"70006807","displayToPublicDate":"2012-08-08T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Answers to questions from persons interested in fish farming: Part III","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None","usgsCitation":"Martin, M., 1975, You asked for it! Answers to questions from persons interested in fish farming: Part III: Commercial Fish Farmer and Aquaculture News, v. 1, no. 4, p. 51-51.","productDescription":"1 p.","startPage":"51","endPage":"51","numberOfPages":"1","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":259782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bd229e4b08c986b32f674","contributors":{"authors":[{"text":"Martin, M.","contributorId":103217,"corporation":false,"usgs":true,"family":"Martin","given":"M.","affiliations":[],"preferred":false,"id":355278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038737,"text":"wri5175 - 1975 - Flood of July 21, 1975 in Mercer County, New Jersey","interactions":[],"lastModifiedDate":"2012-06-19T01:01:45","indexId":"wri5175","displayToPublicDate":"2012-06-18T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"51-75","title":"Flood of July 21, 1975 in Mercer County, New Jersey","docAbstract":"Intense rainfall during the evening of July 20 and early morning hours of July 21, 1975 caused flooding of unprecedented magnitude in highly urbanized Mercer County, New Jersey. Over 6 inches (152 millimetres) of rainfall was recorded during a 10-hour period at Trenton, the capital of New Jersey. No lives were lost but damages to highways and bridges, to industrial, business, and residential buildings, to farmlands and crops, and to water supply systems were severe. This report illustrates the magnitude of the flood and provides hydrologic data needed for planning and design to control or lessen damages from future floods. It includes discussions of the antecedent conditions and meteorological aspects of the storm; a description of the flood and comparison to previous floods; a summary of flood stages and discharges; a discussion of flood frequency; and photomosaics which show inundated areas. 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Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Lee R. Peterson, district chief. These data represent that portion of the National Water Data System collected by the Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA7411","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for California, 1974; Part 1: Surface water records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-74-1-1, xv, 495 p., https://doi.org/10.3133/wdrCA7411.","productDescription":"xv, 495 p.","temporalStart":"1973-10-01","temporalEnd":"1974-09-30","costCenters":[],"links":[{"id":257493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/ca-74/WDR-1974-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_74_1_1.jpg"}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc958e4b08c986b32cce7","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":535195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038343,"text":"70038343 - 1975 - Hydrogeologic data for the lower Connecticut River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-05-15T09:38:29","indexId":"70038343","displayToPublicDate":"2012-05-01T11:21:00","publicationYear":"1975","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":"30","title":"Hydrogeologic data for the lower Connecticut River basin, Connecticut","docAbstract":"This report contains geologic, ground-water, and miscellaneous data on the quality of surface water collected for a water-resources inventory of the lower Connecticut River basin, Connecticut. The study was made by the U.S. Geological Survey in fiscal cooperation with the Connecticut Department of Environmental Protection. A companion report (Connecticut Water Resources Bulletin No. 31, in preparation) interprets the factual information presented here or otherwise collected for the study.","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":"Bingham, J., Paine, F., and Weiss, L., 1975, Hydrogeologic data for the lower Connecticut River basin, Connecticut: Connecticut Water Resources Bulletin 30, Report: 59 p.; 1 Plate: 22.24 x 29.00 inches.","productDescription":"Report: 59 p.; 1 Plate: 22.24 x 29.00 inches","numberOfPages":"62","costCenters":[],"links":[{"id":287223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287222,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038343/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Lower Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.85,41.241667 ], [ -72.85,41.8 ], [ -72.2,41.8 ], [ -72.2,41.241667 ], [ -72.85,41.241667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b0e4b0c8380cd5f1a8","contributors":{"authors":[{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":463915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paine, F.D.","contributorId":20830,"corporation":false,"usgs":true,"family":"Paine","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":463914,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, L.A.","contributorId":95098,"corporation":false,"usgs":true,"family":"Weiss","given":"L.A.","affiliations":[],"preferred":false,"id":463916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}