{"pageNumber":"386","pageRowStart":"9625","pageSize":"25","recordCount":11004,"records":[{"id":70232798,"text":"70232798 - 1976 - Revision of Mississippian stratigraphy, eastern Idaho and northeastern Utah","interactions":[],"lastModifiedDate":"2022-07-12T16:54:39.308298","indexId":"70232798","displayToPublicDate":"1976-07-01T11:45:33","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":"Revision of Mississippian stratigraphy, eastern Idaho and northeastern Utah","docAbstract":"<p>New paleontologic evidence requires a revision of previous interpretations of the stratigraphy of Mississippian sequences in the Cordilleran miogeosyncline of eastern Idaho and northeastern Utah. A postulated unconformity between rocks of early Osagean age and rocks of middle Meramecian age is no longer tenable in the light of new data. The new evidence supports continuous deposition from the Lodgepole Limestone (Kinderhookian and early Osagean age) into the Little Flat Formation (early Osagean to middle Meramecian age) and its equivalents, and the interpretation of a phosphatic siltstone and shale interval in the lower part of the Little Flat Formation as a starved-basin facies. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Sando, W.J., Dutro, J.T., Sandberg, C., and Mamet, B.L., 1976, Revision of Mississippian stratigraphy, eastern Idaho and northeastern Utah: Journal of Research of the U.S. Geological Survey, v. 4, no. 4, p. 467-479.","productDescription":"13 p.","startPage":"467","endPage":"479","costCenters":[],"links":[{"id":403550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403547,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue4/report.pdf","size":"21912 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.08203125,\n              39.90973623453719\n            ],\n            [\n              -109.0283203125,\n              39.90973623453719\n            ],\n            [\n              -109.09423828125,\n              41.0130657870063\n            ],\n            [\n              -111.005859375,\n              41.04621681452063\n            ],\n            [\n              -111.07177734375,\n              44.55916341529182\n            ],\n            [\n              -111.20361328125,\n              44.66865287227321\n            ],\n            [\n              -112.3681640625,\n              44.62175409623324\n            ],\n            [\n              -112.91748046874999,\n              44.5435052132082\n            ],\n            [\n              -113.02734374999999,\n              44.824708282300236\n            ],\n            [\n              -113.40087890624999,\n              45.120052841530544\n            ],\n            [\n              -114.01611328125,\n              45.72152152227954\n            ],\n            [\n              -114.08203125,\n              39.90973623453719\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sando, William Jasper","contributorId":8524,"corporation":false,"usgs":true,"family":"Sando","given":"William","email":"","middleInitial":"Jasper","affiliations":[],"preferred":true,"id":846411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutro, J. Thomas Jr.","contributorId":102878,"corporation":false,"usgs":true,"family":"Dutro","given":"J.","suffix":"Jr.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":846412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandberg, Charles sandberg@usgs.gov","contributorId":199124,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":846413,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mamet, Bernard L.","contributorId":32524,"corporation":false,"usgs":true,"family":"Mamet","given":"Bernard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":846414,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70232795,"text":"70232795 - 1976 - Mississippi carbonate shelf margins, western United States","interactions":[],"lastModifiedDate":"2022-07-12T16:43:20.340036","indexId":"70232795","displayToPublicDate":"1976-07-01T11:34:30","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":"Mississippi carbonate shelf margins, western United States","docAbstract":"<p>Regional linear carbonate shelf margins, or stratigraphic reefs, are postulated to have developed during Mississippian time along the eastern flank of the Cordilleran miogeosyncline in the Western United States. These shelf margins are analogous to well-documented ancient and modern geologic counterparts, such as the Guadalupian reef of the West Texas Permian basin, the Lower Cretaceous Edwards shelf margin of the Gulf Coast, and the modern Florida reef tract-Straits of Florida province. Two Mississippian shelf margins are believed to have existed: The lower one developed as an integral part of a widespread carbonate depositional complex of Kinderhookian through early Meramecian age; the upper shelf margin developed west of the earlier stratigraphic reef as part of a regional carbonate depositional complex of middle Meramecian to late Chesterian age. Evidence for both shelf margins consists of (1) a linear physical barrier, (2) restricted sediments in the shelf interior, (3) abrupt basinward thinning of sediments and basin-starvation just seaward of the shelf edge, (4) profound fades-changes coincident with the basinward thinning from light-colored, skeletal, shelf carbonate rocks to dark, fine-grained, silty, basinal carbonate rocks, and (5) the consistent regional occurrence of the first four patterns. Seaward topographic relief along the front edge of the lower shelf margin was probably about 200-400 m, and maximum relief along the central sector of the upper shelf margin may have approached 1,000 m. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Rose, P.R., 1976, Mississippi carbonate shelf margins, western United States: Journal of Research of the U.S. Geological Survey, v. 4, no. 4, p. 449-466.","productDescription":"18 p.","startPage":"449","endPage":"466","costCenters":[],"links":[{"id":403543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403539,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue4/report.pdf","size":"21912 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Colorado, Idaho, Montana, Nevada, New Mexico, Oregon, Utah, Washington, Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-104.053249,41.001406],[-102.124972,41.002338],[-102.051292,40.749591],[-102.04192,37.035083],[-102.979613,36.998549],[-103.002247,36.911587],[-103.064423,32.000518],[-106.565142,32.000736],[-106.577244,31.810406],[-106.750547,31.783706],[-108.208394,31.783599],[-108.208573,31.333395],[-111.000643,31.332177],[-114.813613,32.494277],[-114.722746,32.713071],[-117.118868,32.534706],[-117.50565,33.334063],[-118.088896,33.729817],[-118.428407,33.774715],[-118.519514,34.027509],[-119.159554,34.119653],[-119.616862,34.420995],[-120.441975,34.451512],[-120.608355,34.556656],[-120.644311,35.139616],[-120.873046,35.225688],[-120.884757,35.430196],[-121.851967,36.277831],[-121.932508,36.559935],[-121.788278,36.803994],[-121.880167,36.950151],[-122.140578,36.97495],[-122.419113,37.24147],[-122.511983,37.77113],[-122.425942,37.810979],[-122.168449,37.504143],[-122.144396,37.581866],[-122.385908,37.908136],[-122.301804,38.105142],[-122.484411,38.11496],[-122.492474,37.82484],[-122.972378,38.020247],[-123.103706,38.415541],[-123.725367,38.917438],[-123.851714,39.832041],[-124.373599,40.392923],[-124.063076,41.439579],[-124.536073,42.814175],[-124.150267,43.91085],[-123.962887,45.280218],[-123.996766,46.20399],[-123.548194,46.248245],[-124.029924,46.308312],[-124.06842,46.601397],[-123.97083,46.47537],[-123.84621,46.716795],[-124.022413,46.708973],[-124.108078,46.836388],[-123.86018,46.948556],[-124.138035,46.970959],[-124.425195,47.738434],[-124.672427,47.964414],[-124.727022,48.371101],[-123.981032,48.164761],[-122.748911,48.117026],[-122.637425,47.889945],[-123.15598,47.355745],[-122.527593,47.905882],[-122.578211,47.254804],[-122.725738,47.33047],[-122.691771,47.141958],[-122.796646,47.341654],[-122.863732,47.270221],[-122.67813,47.103866],[-122.364168,47.335953],[-122.429841,47.658919],[-122.230046,47.970917],[-122.425572,48.232887],[-122.358375,48.056133],[-122.512031,48.133931],[-122.424102,48.334346],[-122.689121,48.476849],[-122.425271,48.599522],[-122.796887,48.975026],[-104.048736,48.999877],[-104.053249,41.001406]]],[[[-119.789798,34.05726],[-119.5667,34.053452],[-119.795938,33.962929],[-119.916216,34.058351],[-119.789798,34.05726]]],[[[-118.524531,32.895488],[-118.573522,32.969183],[-118.369984,32.839273],[-118.524531,32.895488]]],[[[-118.500212,33.449592],[-118.32446,33.348782],[-118.593969,33.467198],[-118.500212,33.449592]]],[[[-122.519535,48.288314],[-122.66921,48.240614],[-122.400628,48.036563],[-122.419274,47.912125],[-122.744612,48.20965],[-122.664928,48.374823],[-122.519535,48.288314]]],[[[-122.800217,48.60169],[-122.883759,48.418793],[-123.173061,48.579086],[-122.949116,48.693398],[-122.743049,48.661991],[-122.800217,48.60169]]]]},\"properties\":{\"name\":\"Arizona\",\"nation\":\"USA  \"}}]}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rose, Peter R.","contributorId":19958,"corporation":false,"usgs":true,"family":"Rose","given":"Peter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":846410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232782,"text":"70232782 - 1976 - Fission-track ages of sphene and apatite of granitic rocks of the Salinian block, Coast Ranges, California","interactions":[],"lastModifiedDate":"2022-07-12T16:07:14.153611","indexId":"70232782","displayToPublicDate":"1976-07-01T10:56:59","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":"Fission-track ages of sphene and apatite of granitic rocks of the Salinian block, Coast Ranges, California","docAbstract":"<p>Fission-track ages have been determined on apatite and sphene from granitic rocks of the Salinian block, California Coast Ranges. The 26 age determinations on sphene range between 68 and 93 m.y. The 24 age determinations on apatite have a greater variation, ranging from 3 to 74 m.y. None of the fission-track ages appear to reflect times of intrusion. The Pinnacles volcanic field of Miocene age apparently has thermally affected apatite ages in the central Gabilan and eastern Santa Lucia Ranges. Reduced apatite ages in the area between the Farallon Islands and the Monterey Peninsula may also be the result of Miocene volcanic activity, but the evidence is less conclusive. Fission-track ages on sphene correlate closely with previously determined potassium-argon ages on hornblende and biotite but show an unexplained \"bimodal\" age distribution, the ages in the Gabilan and Santa Lucia Ranges being slightly, but consistently, lower (avg 75 m.y.) than the ages for terrane to the north and south (avg 85 m.y.) The overall pattern of the sphene and apatite fission-track ages, distinctly different from that of the central Sierra Nevada, may be a \"fingerprint\" of correlative value in locating the parent terrane of the \"ripped-off\" Salinian block.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Naeser, C.W., and Ross, D.C., 1976, Fission-track ages of sphene and apatite of granitic rocks of the Salinian block, Coast Ranges, California: Journal of Research of the U.S. Geological Survey, v. 4, no. 4, p. 415-420.","productDescription":"6 p.","startPage":"415","endPage":"420","costCenters":[],"links":[{"id":403516,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403515,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue4/report.pdf","size":"21912 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Coast Ranges, Salinian block, San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.04687499999999,\n              38.048091067457236\n            ],\n            [\n              -122.54150390625,\n              37.61423141542417\n            ],\n            [\n              -122.51953124999999,\n              37.16031654673677\n            ],\n            [\n              -122.16796875,\n              36.914764288955936\n            ],\n            [\n              -122.01416015625,\n              36.27970720524017\n            ],\n            [\n              -121.2451171875,\n              35.53222622770337\n            ],\n            [\n              -119.267578125,\n              34.74161249883172\n            ],\n            [\n              -118.45458984375,\n              34.813803317113155\n            ],\n            [\n              -122.23388671874999,\n              37.87485339352928\n            ],\n            [\n              -123.662109375,\n              38.94232097947902\n            ],\n            [\n              -123.04687499999999,\n              38.048091067457236\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":846402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, D. C.","contributorId":103681,"corporation":false,"usgs":true,"family":"Ross","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":846403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232758,"text":"70232758 - 1976 - Geology of the Brysch uranium mine, Karnes County, Texas","interactions":[],"lastModifiedDate":"2022-07-12T15:36:53.642205","indexId":"70232758","displayToPublicDate":"1976-07-01T09:56:04","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":"Geology of the Brysch uranium mine, Karnes County, Texas","docAbstract":"<p>Approximately 13,700 tons (12,400 tonnes) of oxidized uranium ore, averaging about 0.1 percent U<sub>2</sub>O<sub>8</sub>, was mined during 1966 and 1967 from the lower unit of the Deweesville Sandstone Member of the upper Eocene Whitsett Formation, from depths of 75 to 90 feet (23-27 m). The mine is in the Karnes County uranium area, 3 miles (5 km) east of Falls City, Tex. Meta-autunite, Ca(UO<sub>2</sub>)<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>2-6H<sub>2</sub>O, and meta-tyuyamunite, Ca(UO<sub>2</sub>)<sub>2</sub>(PO<sub>4</sub>)<sub>2</sub>3-5H<sub>2</sub>O, were identified in samples of the ore. The host rock is light-colored, medium-grained, well-sorted feldspathic sandstone that contains fossil wood and <i>Ophiomorpha</i>. It also contains clinoptilolite, cristobalite, and montmorillonite that probably formed as alteration products of volcanic grains in the original sediment. The host rock was deposited in a beach environment near or on a delta formed at the mouth of a stream channel oriented roughly normal to the beach. The Deweesville can be traced for many miles on the surface and represents in general the point of maximum transgression in a transgressive-regressive cycle. The upper unit of the Deweesville, which overlies the host rock, is now exposed in the mine and contains, in ascending order, storm-beach, shoreface, beach, and tidal-flat facies. The shape of the ore body suggests that it originated as an unoxidized ore roll. The ore-bearing fluids may have entered through porous fluvial rock extending updip. Plant material, abundant in the original host sediment, probably supplied reductant necessary for the roll formation.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Dickinson, K.A., and Sullivan, M.W., 1976, Geology of the Brysch uranium mine, Karnes County, Texas: Journal of Research of the U.S. Geological Survey, v. 4, no. 4, p. 397-404.","productDescription":"8 p.","startPage":"397","endPage":"404","costCenters":[],"links":[{"id":403507,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403502,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue4/report.pdf","size":"21912 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Karnes County","otherGeospatial":"Brysch uranium mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.06164741516113,\n              28.879251532390377\n            ],\n            [\n              -98.05967330932617,\n              28.884737829480123\n            ],\n            [\n              -98.05838584899902,\n              28.925763133251827\n            ],\n            [\n              -98.06859970092773,\n              28.925838256288348\n            ],\n            [\n              -98.06868553161621,\n              28.928016800669653\n            ],\n            [\n              -98.07675361633301,\n              28.92313379268237\n            ],\n            [\n              -98.10224533081055,\n              28.907130939803995\n            ],\n            [\n              -98.11391830444336,\n              28.901796106917587\n            ],\n            [\n              -98.11975479125977,\n              28.89548411948549\n            ],\n            [\n              -98.1049919128418,\n              28.872863013115218\n            ],\n            [\n              -98.1053352355957,\n              28.871134287431143\n            ],\n            [\n              -98.0903148651123,\n              28.85527376633892\n            ],\n            [\n              -98.06164741516113,\n              28.879251532390377\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dickinson, Kendall A.","contributorId":293002,"corporation":false,"usgs":false,"family":"Dickinson","given":"Kendall","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":846391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sullivan, Michael W.","contributorId":86428,"corporation":false,"usgs":true,"family":"Sullivan","given":"Michael","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":846392,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232748,"text":"70232748 - 1976 - Thin-skinned tectonics and potential hydrocarbon traps: Illustrated by a seismic profile in the Valley and Ridge province of Tennessee","interactions":[],"lastModifiedDate":"2022-07-12T14:37:51.225396","indexId":"70232748","displayToPublicDate":"1976-07-01T09:25:42","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":"Thin-skinned tectonics and potential hydrocarbon traps: Illustrated by a seismic profile in the Valley and Ridge province of Tennessee","docAbstract":"<p>Seismic data, although limited to a small part of the western half of the Valley and Ridge province in Tennessee, confirm that the structural style is thin-skinned and that there is a fundamental change from west to east in both the total section preserved and the structural complexities that exist in the subsurface. Cambrian to Upper Ordovician rocks in the Valley and Ridge province have been thrust westward over a 4-mile (6.4-km) projection of Cambrian through Mississippian rocks of the Appalachian Plateau. Structure within the plateau projection is characterized by splay anticlines, whereas structure in the Valley and Ridge is dominated by a series of imbricate thrust sheets containing isolated fault-bound masses of Cambrian sandstone and shale. Both splay anticlines and large fault-bound masses of rocks preserved in the subsurface in east Tennessee may be favorable fracture-porosity traps for the accumulation of hydrocarbons.</p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Harris, L.D., 1976, Thin-skinned tectonics and potential hydrocarbon traps: Illustrated by a seismic profile in the Valley and Ridge province of Tennessee: Journal of Research of the U.S. Geological Survey, v. 4, no. 4, p. 379-386.","productDescription":"8 p.","startPage":"379","endPage":"386","costCenters":[],"links":[{"id":403491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403489,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue4/report.pdf","size":"21912 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Valley and Ridge province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.74853515625,\n              34.994003757575776\n            ],\n            [\n              -84.29809570312499,\n              35.47856499535729\n            ],\n            [\n              -83.990478515625,\n              35.71083783530009\n            ],\n            [\n              -83.023681640625,\n              36.12900165569652\n            ],\n            [\n              -82.342529296875,\n              36.61552763134925\n            ],\n            [\n              -83.70483398437499,\n              36.59788913307022\n            ],\n            [\n              -83.990478515625,\n              36.39475669987386\n            ],\n            [\n              -84.210205078125,\n              36.19109202182454\n            ],\n            [\n              -84.473876953125,\n              35.94243575255426\n            ],\n            [\n              -84.83642578125,\n              35.69299463209881\n            ],\n            [\n              -85.352783203125,\n              34.994003757575776\n            ],\n            [\n              -84.74853515625,\n              34.994003757575776\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harris, Leonard D.","contributorId":25567,"corporation":false,"usgs":true,"family":"Harris","given":"Leonard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":846377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175437,"text":"70175437 - 1976 - Hydrogeology of a drift-filled bedrock valley near Lino Lakes, Anoka County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:09:22","indexId":"70175437","displayToPublicDate":"1976-06-15T11:30:00","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":"Hydrogeology of a drift-filled bedrock valley near Lino Lakes, Anoka County, Minnesota","docAbstract":"<div class=\"publication-abstract\" data-reactid=\"65\">\n<div class=\"nova-e-text nova-e-text--size-l nova-e-text--family-sans-serif nova-e-text--spacing-auto\" data-reactid=\"68\">The bedrock surface of east-central Minnesota is dissected by an intricate network of valleys. Outside the bedrock valley at site B, 3 mi (4. 8 km) from site A, 100 ft (30 m) of drift overlies the bedrock surface. Observation wells were installed at the two sites to determine the vertical ground-water movement between the various aquifer units and the lateral movement between the two sites. An aquifer test of the lowest valley-fill aquifer at site A showed that the observation well completed in the same aquifer as the pumping well responded immediately; whereas a lag of about 100 min occurred between the lower valley fill and uppermost body of sand and gravel. This indicates that the hydraulic connection between these two layers is poor at the immediate site. Test results show that the lower sand-and-gravel aquifer has a transmissivity between 14,000 and 27,000 ft<sup>2</sup>/d (1,300 and 2,500 m<sup>2</sup>/d). Although the hydraulic gradient is vertically downward in the valley, much of the drift fill is poorly permeable. This suggests that the quantity of downward-percolating water reaching the lowest valley-fill aquifer is relatively small at the test site. Because valley cut through a number of bedrock aquifers in the region, they could potentially be an important avenue of contamination from land-surface waste. In addition, the vast network of bedrock valleys in the Twin Cities area might cause contaminants to disseminate rather rapidly throughout a large area.</div>\n</div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","usgsCitation":"Winter, T.C., and Pfannkuch, H., 1976, Hydrogeology of a drift-filled bedrock valley near Lino Lakes, Anoka County, Minnesota: Journal of Research of the U.S. Geological Survey, v. 4, no. 3, p. 267-276.","productDescription":"10 p.","startPage":"267","endPage":"276","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":326393,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Anoka County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.5093,45.4163],[-93.1289,45.4153],[-93.0186,45.4131],[-93.0188,45.2984],[-93.0207,45.1258],[-93.2262,45.1255],[-93.2272,45.0373],[-93.2814,45.0374],[-93.2807,45.0498],[-93.2814,45.0539],[-93.2826,45.0584],[-93.2826,45.063],[-93.282,45.0666],[-93.282,45.0689],[-93.2813,45.0717],[-93.2794,45.0753],[-93.2781,45.0794],[-93.2787,45.0835],[-93.28,45.0867],[-93.28,45.0913],[-93.2799,45.0959],[-93.2786,45.1],[-93.2786,45.1036],[-93.2793,45.1064],[-93.2812,45.1077],[-93.2863,45.1119],[-93.2915,45.1155],[-93.2934,45.1187],[-93.2947,45.1215],[-93.296,45.1251],[-93.296,45.1274],[-93.296,45.1297],[-93.2985,45.1329],[-93.3011,45.1356],[-93.3024,45.1388],[-93.3056,45.1416],[-93.3076,45.1429],[-93.3127,45.1448],[-93.3179,45.1466],[-93.3211,45.1484],[-93.3257,45.1512],[-93.3302,45.1539],[-93.3328,45.1544],[-93.3347,45.1549],[-93.3373,45.1558],[-93.3399,45.1576],[-93.3431,45.1599],[-93.3463,45.1626],[-93.3495,45.1663],[-93.3528,45.1699],[-93.3553,45.1727],[-93.3579,45.1745],[-93.3618,45.1759],[-93.3663,45.1768],[-93.3709,45.1777],[-93.3767,45.1805],[-93.3812,45.1832],[-93.3838,45.1855],[-93.3864,45.1878],[-93.3889,45.1892],[-93.3928,45.1914],[-93.3967,45.1933],[-93.4025,45.1956],[-93.4084,45.1965],[-93.4116,45.1983],[-93.4142,45.2001],[-93.4161,45.2038],[-93.418,45.2088],[-93.4193,45.2116],[-93.4226,45.2134],[-93.4252,45.2152],[-93.4264,45.2157],[-93.4297,45.2161],[-93.4362,45.217],[-93.4426,45.2166],[-93.4472,45.2161],[-93.4517,45.2157],[-93.4543,45.2175],[-93.4575,45.2203],[-93.4614,45.2234],[-93.4653,45.2257],[-93.4698,45.2257],[-93.4763,45.2253],[-93.4821,45.2248],[-93.4847,45.2257],[-93.4879,45.2271],[-93.4912,45.2289],[-93.4964,45.2344],[-93.5022,45.239],[-93.5035,45.2399],[-93.5073,45.2417],[-93.5113,45.2431],[-93.5138,45.2454],[-93.5093,45.4163]]]},\"properties\":{\"name\":\"Anoka\",\"state\":\"MN\"}}]}","volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ada1d1e4b0f412a62dfa87","contributors":{"authors":[{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":645230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pfannkuch, H.O.","contributorId":79228,"corporation":false,"usgs":true,"family":"Pfannkuch","given":"H.O.","affiliations":[],"preferred":false,"id":645231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70232669,"text":"70232669 - 1976 - Mississippian history of the northern Rocky Mountains region","interactions":[],"lastModifiedDate":"2022-07-11T16:28:04.733861","indexId":"70232669","displayToPublicDate":"1976-05-01T11:11:04","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":"Mississippian history of the northern Rocky Mountains region","docAbstract":"<p>The Mississippian history of the northern Cordilleran region of the United States consists of two principal depositional cycles separated by a cycle of epeirogenic uplift and erosion. Each depositional cycle is divisible into phases that represent significant changes in depositional patterns. During Cycle I (early Kinderhookian-early Meramecian), predominantly carbonate and evaporite deposition took place on a broad cratonic shelf bordered on the east by land and on the west by a deep trough that received terrigenous sediments from an adjacent western landmass. Kinderhookian transgression was followed by regression during the Osagean and early Meramecian. Regional uplift during latest early Meramecian time (Cycle II) drained the shelf area and caused the sea to be confined to the western trough. During Cycle III (middle Meramecian-Chesterian), the sea again transgressed onto the craton, which was differentiated into the Big Snowy-Williston, Wyoming, and Uinta basins, where terrigenous and carbonate sediments were deposited. The Big Snowy-Williston basin was uplifted during latest Chesterian time and lost its identity, but the Wyoming basin continued to expand into the Pennsylvanian, when it engulfed most of the Cordilleran platform and breached the Transcontinental arch. Application of generalized carbonate, terrigenous, and evaporite depositional models results in specific models that explain the Mississippian depositional patterns. </p>","language":"English","publisher":"U. S. Geological Survey","usgsCitation":"Sando, W.J., 1976, Mississippian history of the northern Rocky Mountains region: Journal of Research of the U.S. Geological Survey, v. 4, no. 3, p. 317-338.","productDescription":"22 p.","startPage":"317","endPage":"338","costCenters":[],"links":[{"id":403405,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403402,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue3/report.pdf","size":"16265 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Idaho, Montana, Nebraska, Nevada, North Dakota, South Dakota, Utah, Wyoming","otherGeospatial":"Rocky Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.6748046875,\n              40.413496049701955\n            ],\n            [\n              -102.3486328125,\n              40.413496049701955\n            ],\n            [\n              -102.3486328125,\n              49.06666839558117\n            ],\n            [\n              -116.6748046875,\n              49.06666839558117\n            ],\n            [\n              -116.6748046875,\n              40.413496049701955\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sando, William Jasper","contributorId":8524,"corporation":false,"usgs":true,"family":"Sando","given":"William","email":"","middleInitial":"Jasper","affiliations":[],"preferred":true,"id":846220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232654,"text":"70232654 - 1976 - Factors affecting declining water levels in a sewered area of Nassau County, New York","interactions":[],"lastModifiedDate":"2022-07-12T13:37:45.149132","indexId":"70232654","displayToPublicDate":"1976-05-01T09:21:03","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":"Factors affecting declining water levels in a sewered area of Nassau County, New York","docAbstract":"<p> Double-mass-curve analysis of ground-water levels in Nassau County, Long Island, N.Y., shows that the average-weighted ground-water levels in a 32-mi<sup>2</sup> (83-km<sup>2</sup>) segment of a sewered area declined 11.8 ft (3.6 m) relative to an adjacent unsewered area to the east during 1953-72. Electric-analog-model analysis indicates that 4.9 ft (1.5 m) of the decline is due to pumping in nearby Queens County, west of the sewered area. Most of the remaining 6.9 ft (2.1 m) of the decline is due to sewering. Streamflow within the sewered area has also declined because of the lowered ground-water levels.</p>","language":"English","publisher":"U. S. Geological Survey","collaboration":"Prepared in cooperation with the Nassau County Department of Public Works","usgsCitation":"Garber, M.S., and Sulam, D.J., 1976, Factors affecting declining water levels in a sewered area of Nassau County, New York: Journal of Research of the U.S. Geological Survey, v. 4, no. 3, p. 255-265.","productDescription":"11 p.","startPage":"255","endPage":"265","costCenters":[],"links":[{"id":403377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":403375,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue3/report.pdf","size":"16265 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Nassau County","city":"Hempstead, North Hempstead","otherGeospatial":"Long Island, Sewer District 2","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": 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,{"id":70232224,"text":"70232224 - 1976 - Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado","interactions":[],"lastModifiedDate":"2022-06-15T16:09:05.601311","indexId":"70232224","displayToPublicDate":"1976-03-01T11:01:35","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":"Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado","docAbstract":"<p>Radiocarbon dates and stratigraphic cores from bogs, kettle ponds, and former ice-marginal lakes on the east and west sides of the Front Range, Colo., between lat 40°00' and 40°24' N. suggest that (1) valley glaciers of Pinedale age began to recede from their terminal positions between about 14,600 and 13,000 yr ago, (2) revegetation of glaciated areas at altitudes of 2,600-2,900 m (8,600-9,500 ft) was complete by 11,000-10,000 yr ago, (3) at one site, 3,500±1,000 yr elapsed before peat began to form after deglaciation, (4) the formation of bogs within the glaciated areas kept pace with glacier recession in a general way, beginning at progressively later times as deglaciation proceeded upward, (5) Pinedale glaciers had disappeared or were reduced to small remnants by about 8,000 yr ago, (6) moraines that have been mapped as belonging to the early stade of Pinedale Glaciation are no younger than 13,000 yr B.P. and may be older than 14,600 yr, and those delimiting what has been mapped as late stade are no younger than about 7,600 yr B.P. and are probably older than 7,800 yr, and (7) most of the till mapped as Pinedale was deposited between about 14,600 and 8,000 yr ago.</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Madole, R.F., 1976, Bog stratigraphy, radiocarbon dates, and Pinedale to Holocene glacial history in the Front Range, Colorado: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 163-169.","productDescription":"7 p.","startPage":"163","endPage":"169","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":402212,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":402211,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf"}],"country":"United States","state":"Colorado","otherGeospatial":"Front Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106,\n              40\n            ],\n            [\n              -105,\n              40\n            ],\n            [\n              -105,\n              40.4\n            ],\n            [\n              -106,\n              40.4\n            ],\n            [\n              -106,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Madole, Richard F. 0000-0002-9081-570X madole@usgs.gov","orcid":"https://orcid.org/0000-0002-9081-570X","contributorId":1340,"corporation":false,"usgs":true,"family":"Madole","given":"Richard","email":"madole@usgs.gov","middleInitial":"F.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":844715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5223543,"text":"5223543 - 1976 - Establishment of the black-tailed jackrabbit on the Virginia eastern shore","interactions":[],"lastModifiedDate":"2025-03-10T16:38:18.767277","indexId":"5223543","displayToPublicDate":"1976-02-27T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Establishment of the black-tailed jackrabbit on the Virginia eastern shore","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1379525","usgsCitation":"Clapp, R.B., Weske, J., and Clapp, T., 1976, Establishment of the black-tailed jackrabbit on the Virginia eastern shore: Journal of Mammalogy, v. 57, no. 1, p. 180-181, https://doi.org/10.2307/1379525.","productDescription":"2 p.","startPage":"180","endPage":"181","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.53318689722039,\n              37.98487341318935\n            ],\n            [\n              -76.53318689722039,\n              36.62076603430651\n            ],\n            [\n              -75.79097825485586,\n              36.62076603430651\n            ],\n            [\n              -75.79097825485586,\n              37.98487341318935\n            ],\n            [\n              -76.53318689722039,\n              37.98487341318935\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd5a","contributors":{"authors":[{"text":"Clapp, R. B.","contributorId":9371,"corporation":false,"usgs":true,"family":"Clapp","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":338952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weske, J.S.","contributorId":102423,"corporation":false,"usgs":true,"family":"Weske","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":338954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clapp, T.C.","contributorId":45812,"corporation":false,"usgs":true,"family":"Clapp","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":338953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11039,"text":"ofr76713 - 1976 - Geologic data from test drilling in Palm Beach County, Florida since 1970","interactions":[],"lastModifiedDate":"2022-01-05T16:46:35.547986","indexId":"ofr76713","displayToPublicDate":"1976-01-01T22:10:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-713","title":"Geologic data from test drilling in Palm Beach County, Florida since 1970","docAbstract":"Test hole data, in Palm Beach County, Florida, include lithologic logs from 66 test wells and geophysical logs from 54 test wells. The purpose of the study is to provide the geohydrologic information needed for water management and land use decisions, with emphasis on the urbanized eastern part of the county and the readily developable area in the central part. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr76713","collaboration":"Prepared in cooperation with Palm Beach County and the South Florida Water Management District","usgsCitation":"Schneider, J.J., 1976, Geologic data from test drilling in Palm Beach County, Florida since 1970: U.S. Geological Survey Open-File Report 76-713, iii, 99 p., https://doi.org/10.3133/ofr76713.","productDescription":"iii, 99 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":142586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0713/coverthb.jpg"},{"id":967,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0713/ofr76713.pdf","text":"Report","size":"5.36 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","county":"Palm Beach 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href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8e8","contributors":{"authors":[{"text":"Schneider, James J.","contributorId":22356,"corporation":false,"usgs":true,"family":"Schneider","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28673,"text":"wri7629 - 1976 - Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff","interactions":[],"lastModifiedDate":"2022-01-05T18:52:24.717791","indexId":"wri7629","displayToPublicDate":"1976-01-01T21:35:00","publicationYear":"1976","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":"76-29","title":"Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff","docAbstract":"In much of the water pumped into the northern Everglades, Florida, concentrations of inorganic nitrogen and phosphorus are relatively high. These nutrients are transported in the canals or into the peripheral marshes. Concentrations decrease sharply within 330 feet or less of the canals, whereas specific conductance remains essentially unchanged within this distance. The sharp decrease in inorganic nitrogen and phosphorus near the canal edge indicates net uptake in these shallow waters. Concentrations of nitrogen and phosphorus also decrease as water moves through the conservation areas in canals. This decrease is due partly to dilution by rainfall and runoff, and partly to net uptake in the canals and their peripheral marsh. The large canals of the northern and eastern parts of the conservation areas often have relatively low concentrations of dissolved oxygen which show little fluctuation within 24 hours. Backpumping 50 percent of the total annual canal runoff in southeast Florida would add from 990 to 6,160 tons of nitrogen and from 10 to 62 tons of phosphorus to the conservation areas. The bottom sediments of the Everglades are a sink for nitrogen and phosphorus. They can, however, be a source of these nutrients when anaerobic conditions exist at the water-sediment interface or when bottom material becomes resuspended. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7629","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"McPherson, B.F., Waller, B.G., and Mattraw, H., 1976, Nitrogen and phosphorus uptake in the Everglades Conservation Areas, Florida, with special reference to the effects of backpumping runoff: U.S. Geological Survey Water-Resources Investigations Report 76-29, 120 p., https://doi.org/10.3133/wri7629.","productDescription":"120 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2265,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0029/wri7629.pdf","text":"Report","size":"2.47 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":158277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0029/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.09832763671875,\n              26.966141794817037\n            ],\n            [\n              -81.3372802734375,\n              26.88288045572338\n            ],\n            [\n              -81.23291015625,\n              26.703906250401882\n            ],\n            [\n              -81.05987548828125,\n              26.73089302213736\n            ],\n            [\n              -80.99945068359375,\n              26.73334604773261\n            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          -80.88409423828125,\n              26.78729922215609\n            ],\n            [\n              -80.97198486328125,\n              26.944108009688595\n            ],\n            [\n              -81.09832763671875,\n              26.966141794817037\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c02b","contributors":{"authors":[{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":200209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200211,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mattraw, H. C.","contributorId":45712,"corporation":false,"usgs":true,"family":"Mattraw","given":"H. C.","affiliations":[],"preferred":false,"id":200210,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5220984,"text":"5220984 - 1976 - Some characteristics of fall migration of female woodcock","interactions":[],"lastModifiedDate":"2025-02-18T17:51:57.587802","indexId":"5220984","displayToPublicDate":"1976-01-01T12:19:14","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Some characteristics of fall migration of female woodcock","docAbstract":"<p>Nine female woodcock (<i>Philohela minor</i>) were radio-tagged in central Pennsylvania before fall migration to monitor premigratory and migratory movements. Within 15 days of departure, 5 of the birds moved 0.8 to 8.0 km from their normally used area, but the remaining 4 did not move. In 1973 five marked woodcock began migration between 30 November and 8 December. In 1974, four birds departed between 18 and 29 November. Departures coincided with high pressure centers approaching from the north and west or low pressure centers retreating to the north and east, or both. Eight of the 9 woodcock departed 2.5 or more hours after sunset and at least 7 left before midnight. Two hatching-year birds were tracked for up to 201 km SSW of the study area during 2 nights. Their air speeds (mean + SD) were 36 + 2 and 45 + 3 km/h.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3800159","usgsCitation":"Coon, R., Caldwell, P., and Storm, G., 1976, Some characteristics of fall migration of female woodcock: Journal of Wildlife Management, v. 40, no. 1, p. 91-95, https://doi.org/10.2307/3800159.","productDescription":"5 p.","startPage":"91","endPage":"95","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193422,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70171425,"text":"70171425 - 1976 - Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","interactions":[],"lastModifiedDate":"2018-02-04T14:32:02","indexId":"70171425","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","docAbstract":"<p>On the basis of a linear relationship between winter (October-April) precipitation and annual runoff from a drainage basin (Rasmussen and Tangborn, 1976) a physically reasonable model for predicting summer (May-September) streamflow from drainages in the North Cascades region was developed. This hydrometeorological prediction method relates streamflow for a season beginning on the day of prediction to the storage (including snow, ice, soil moisture, and groundwater) on that day. The spring storage is inferred from an input-output relationship based on the principle of conservation of mass: spring storage equals winter precipitation on the basin less winter runoff from the basin and less winter evapotranspiration, which is presumed to be small. The method of prediction is based on data only from the years previous to the one for which the prediction is made, and the system is revised each year as data for the previous year become available. To improve the basin storage estimate made in late winter or early spring, a short-season runoff prediction is made. The errors resulting from this short-term prediction are used to revise the storage estimate and improve the later prediction. This considerably improves the accuracy of the later prediction, especially for periods early in the summer runoff season. The optimum length for the test period appears to be generally less than a month for east side basins and between 1 and 2 months for those on the west side of the Cascade Range. The time distribution of the total summer runoff can be predicted when this test season is used so that on May 1 monthly streamflow for the May-September season can be predicted. It was found that summer precipitation and the time of minimum storage are two error sources that were amenable to analysis. For streamflow predictions in seasons beginning in early spring the deviation of the subsequent summer precipitation from a long-period average will contribute up to 53% of the prediction error. This contribution decreases to nearly zero during the summer and then rises slightly for late summer predictions. The reason for the smaller than expected effect of summer precipitation is thought to be due to the compensating effect of increased evaporative losses and increased infiltration when precipitation is greater than normal during the summer months. The error caused by the beginning winter month (assumed to be October in this study) not coinciding with the time of minimum storage was examined; it appears that October may be the best average beginning winter month for most drainages but that a more detailed study is needed. The optimum beginning of the winter season appears to vary from August to October when individual years are examined. These results demonstrate that standard precipitation and runoff measurements in the North Cascades region are adequate for constructing a predictive hydrologic model. This model can be used to make streamflow predictions that compare favorably with current multiple regression methods based on mountain snow surveys. This method has the added advantages of predicting the space and time distributions of storage and summer runoff.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR012i002p00203","usgsCitation":"Tangborn, W.V., and Rasmussen, L.A., 1976, Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method: Water Resources Research, v. 12, no. 2, p. 203-216, https://doi.org/10.1029/WR012i002p00203.","productDescription":"14 p.","startPage":"203","endPage":"216","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321911,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cascade 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,{"id":70162479,"text":"70162479 - 1976 - Earthquake history of Oregon","interactions":[],"lastModifiedDate":"2019-11-13T14:55:40","indexId":"70162479","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake history of Oregon","docAbstract":"<p>Although situated between two States (California and Washington) that have has many violent earthquakes, Oregon is noticeably less active seismically. the greatest damage experienced resulted from a major shock near Olympia, Wash., in 1949. During the short history record available (since 1841), 34 earthquakes of intensity V, Modified Mercalli Scale, or greater have centered within Oregon or near its borders. Only 13 of the earthquakes had an intensity above V, and many of the shocks were local. However, a 1936 earthquake in the eastern Oregon-Washington region caused extensive damage and was felt over an area of 272,000 square kilometers.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"von Hake, C., 1976, Earthquake history of Oregon: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 30-33.","productDescription":"4 p.","startPage":"30","endPage":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a7554ee4b0b28f1184d7ff","contributors":{"authors":[{"text":"von Hake, C. A.","contributorId":7699,"corporation":false,"usgs":true,"family":"von Hake","given":"C. A.","affiliations":[],"preferred":false,"id":589668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011146,"text":"70011146 - 1976 - Aseismic uplift in Southern California","interactions":[],"lastModifiedDate":"2017-03-15T16:40:13","indexId":"70011146","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Aseismic uplift in Southern California","docAbstract":"<p><span>Preliminary examination of the historic geodetic record has disclosed crustal uplift of 0.15 to 0.25 meter that apparently began around 1960 and has since grown to include at least 12,000 square kilometers of southern California. This uplift extends at least 150 kilometers west-northwestward along the San Andreas Fault from Cajon to Maricopa, southward from the San Andreas into the northern Transverse Ranges, and eastward from Lebec into and including much of western Mojave block. It seems to have grown spasmodically eastward from a center near the junction of the San Andreas and Garlock faults and has occurred largely within an area that has remained virtually aseismic since at least 1932. Although much of this area has been characterized by crustal mobility since at least the turn the century, the described uplift seems to be an unusually large and probably unique event superimposed the existing pattern of continuing deformation.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.192.4236.251","issn":"00368075","usgsCitation":"Castle, R.O., Church, J.P., and Elliot, M.R., 1976, Aseismic uplift in Southern California: Science, v. 192, no. 4236, p. 251-253, https://doi.org/10.1126/science.192.4236.251.","productDescription":"3 P.","startPage":"251","endPage":"253","costCenters":[],"links":[{"id":220820,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      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,{"id":24994,"text":"pp891 - 1976 - The February 1969 east rift eruption of Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2023-04-05T18:17:39.633331","indexId":"pp891","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"891","title":"The February 1969 east rift eruption of Kilauea Volcano, Hawaii","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp891","usgsCitation":"Swanson, D., Jackson, D.B., Koyanagi, R.Y., and Wright, T.L., 1976, The February 1969 east rift eruption of Kilauea Volcano, Hawaii: U.S. Geological Survey Professional Paper 891, Report: iv, 30 p.; 1 Plate: 39.00 x 25.40 inches, https://doi.org/10.3133/pp891.","productDescription":"Report: iv, 30 p.; 1 Plate: 39.00 x 25.40 inches","costCenters":[],"links":[{"id":104749,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5102.htm","linkFileType":{"id":5,"text":"html"},"description":"5102"},{"id":53983,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0891/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53982,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0891/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118995,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0891/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.25,\n              19.4583\n            ],\n            [\n              -155.25,\n              19.333\n            ],\n            [\n              -155.0417,\n              19.333\n            ],\n            [\n              -155.0417,\n              19.4583\n            ],\n            [\n              -155.25,\n              19.4583\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c842","contributors":{"authors":[{"text":"Swanson, Donald A. 0000-0002-1680-3591","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":22303,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","affiliations":[],"preferred":false,"id":192968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, D. B.","contributorId":27057,"corporation":false,"usgs":true,"family":"Jackson","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":192969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koyanagi, R. Y.","contributorId":35719,"corporation":false,"usgs":true,"family":"Koyanagi","given":"R.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":192970,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wright, T. L.","contributorId":11188,"corporation":false,"usgs":true,"family":"Wright","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192967,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70230341,"text":"70230341 - 1976 - Water-quality data for canals in eastern Broward County, Florida 1969-1974","interactions":[],"lastModifiedDate":"2025-04-25T15:16:23.144223","indexId":"70230341","displayToPublicDate":"1976-01-01T00:00:00","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}},"seriesNumber":"FL 75-009","displayTitle":"Water-Quality Data for Canals in Eastern Broward County, Florida 1969-1974","title":"Water-quality data for canals in eastern Broward County, Florida 1969-1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70230341","collaboration":"Prepared in cooperation with Broward County Environmental Quality Control Board and Central and Southern Florida Flood Control District","usgsCitation":"Waller, B., Miller, W.L., and Beaven, T., 1976, Water-quality data for canals in eastern Broward County, Florida 1969-1974: Open-File Report FL 75-009, 156 p., https://doi.org/10.3133/70230341.","productDescription":"156 p.","numberOfPages":"156","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":398315,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70230341/coverthb.jpg"},{"id":398316,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70230341/ofr-fl-75009.pdf","text":"Report","size":"5.22 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR FL 75-009"}],"country":"United States","state":"Florida","county":"Broward County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.54569321020263,\n              26.280939961326084\n            ],\n            [\n              -80.54569321020263,\n              26.023977390206696\n            ],\n            [\n              -80.07917922157858,\n              26.023977390206696\n            ],\n            [\n              -80.07917922157858,\n              26.280939961326084\n            ],\n            [\n              -80.54569321020263,\n              26.280939961326084\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1975-10-01","noUsgsAuthors":false,"publicationDate":"1975-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Waller, B.G.","contributorId":75970,"corporation":false,"usgs":true,"family":"Waller","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":840031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. L.","contributorId":79128,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":840032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beaven, T.R.","contributorId":84757,"corporation":false,"usgs":true,"family":"Beaven","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":840033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157471,"text":"70157471 - 1975 - Ground-water resources and geology of Waukesha County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:36:47","indexId":"70157471","displayToPublicDate":"2015-05-11T09:00:00","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":"29","title":"Ground-water resources and geology of Waukesha County, Wisconsin","docAbstract":"<p>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.&nbsp;</p>","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":"<p>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.</p>","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":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":70039598,"text":"70039598 - 1975 - Norfolk and environs: A land use perspective","interactions":[],"lastModifiedDate":"2012-08-15T01:02:00","indexId":"70039598","displayToPublicDate":"2012-01-01T11:18:48","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}},"seriesNumber":"Volume 2, Part A","title":"Norfolk and environs: A land use perspective","docAbstract":"The Norfolk-Portsmouth Standard Metropolitan Statistical Area (SMSA) in southeastern Virginia was the site of intensive testing of a number of land resources assessment methods, built around the availability of remotely sensed data from the Earth Resources Technology Satellite (ERTS-I), later renamed LANDSAT I. The Norfolk tests were part of a larger experiment known as the Central Atlantic Regional Ecological Test Site (CARETS), designed to test the extent to which LANDSAT and associated high-altitude aircraft data could be used as cost-effective inputs to a regional land use information system. The Norfolk SMSA contains a variety of land uses typical of the urbanized eastern seaboard, along with typical associated problems: rapid urbanization; heavy recreational, commercial, and residential demands on fragile beaches and coastal marsh environments; industrial, transportation, and governmental land and water uses impacting on residential and agricultural areas; drainage and land stability difficulties affecting construction and other uses; and increasing difficulties in maintaining satisfactory air and water quality.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039598","collaboration":"Sponsored jointly by the National Aeronautics and Space Administration and the U.S. Geological Survey","usgsCitation":"Alexander, R.H., Buzzanell, P.J., Fitzpatrick, K.A., Lins, H.F., and McGinty, H.K., 1975, Norfolk and environs: A land use perspective: Final Report Volume 2, Part A, viiii, 348 p., https://doi.org/10.3133/70039598.","productDescription":"viiii, 348 p.","numberOfPages":"363","costCenters":[{"id":296,"text":"Geography Program","active":false,"usgs":true}],"links":[{"id":259601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Delaware;Maryl;New Jersey;North Carolina;Pennsylvania;Virginia","city":"Norfolk;Portsmouth;Washington D.C.","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78,36 ], [ -78,38 ], [ -75,38 ], [ -75,36 ], [ -78,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a67bae4b0c8380cd7347b","contributors":{"authors":[{"text":"Alexander, Robert H.","contributorId":53807,"corporation":false,"usgs":true,"family":"Alexander","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buzzanell, Peter J.","contributorId":30083,"corporation":false,"usgs":true,"family":"Buzzanell","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":466533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzpatrick, Katherine A.","contributorId":54846,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Katherine","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466536,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":466532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McGinty, Herbert K. III","contributorId":43214,"corporation":false,"usgs":true,"family":"McGinty","given":"Herbert","suffix":"III","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":466534,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70039597,"text":"70039597 - 1975 - Norfolk and environs: A land use perspective","interactions":[],"lastModifiedDate":"2012-08-15T01:02:00","indexId":"70039597","displayToPublicDate":"2012-01-01T10:44:03","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}},"seriesNumber":"Volume 2, Part A","title":"Norfolk and environs: A land use perspective","docAbstract":"The Norfolk-Portsmouth Standard Metropolitan Statistical Area (SMSA) in southeastern Virginia was the site of intensive testing of a number of land resources assessment methods, built around the availability of remotely sensed data from the Earth Resources Technology Satellite (ERTS-I), later renamed LANDSAT I. The Norfolk tests were part of a larger experiment known as the Central Atlantic Regional Ecological Test Site (CARETS), designed to test the extent to which LANDSAT and associated high-altitude aircraft data could be used as cost-effective inputs to a regional land use information system. The Norfolk SMSA contains a variety of land uses typical of the urbanized eastern seaboard, along with typical associated problems: rapid urbanization; heavy recreational, commercial, and residential demands on fragile beaches and coastal marsh environments; industrial, transportation, and governmental land and water uses impacting on residential and agricultural areas; drainage and land stability difficulties affecting construction and other uses; and increasing difficulties in maintaining satisfactory air and water quality.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039597","collaboration":"Sponsored jointly by the National Aeronautics and Space Administration and the U.S. Geological Survey","usgsCitation":"Alexander, R.H., Buzzanell, P.J., Fitzpatrick, K.A., Lins, H.F., and McGinty, H.K., 1975, Norfolk and environs: A land use perspective: Final Report Volume 2, Part A, viii, 348 p.; 11 Plates: 85 x 104 cm. or smaller, https://doi.org/10.3133/70039597.","productDescription":"viii, 348 p.; 11 Plates: 85 x 104 cm. or smaller","numberOfPages":"363","costCenters":[{"id":296,"text":"Geography Program","active":false,"usgs":true}],"links":[{"id":259603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Delaware;Maryl;New Jersey;North Carolina;Pennsylvania;Virginia","city":"Norfolk;Portsmouth;Washinton;D.C.","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78,36 ], [ -78,38 ], [ -75,38 ], [ -75,36 ], [ -78,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a67b9e4b0c8380cd73475","contributors":{"authors":[{"text":"Alexander, Robert H.","contributorId":53807,"corporation":false,"usgs":true,"family":"Alexander","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buzzanell, Peter J.","contributorId":30083,"corporation":false,"usgs":true,"family":"Buzzanell","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":466528,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzpatrick, Katherine A.","contributorId":54846,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Katherine","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":466527,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McGinty, Herbert K. III","contributorId":43214,"corporation":false,"usgs":true,"family":"McGinty","given":"Herbert","suffix":"III","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":466529,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":5224810,"text":"5224810 - 1975 - Emperor penguins nesting on Inaccessible Island","interactions":[],"lastModifiedDate":"2012-02-02T00:15:10","indexId":"5224810","displayToPublicDate":"2010-06-16T12:19:11","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":812,"text":"Antarctic Journal of the United States","active":true,"publicationSubtype":{"id":10}},"title":"Emperor penguins nesting on Inaccessible Island","docAbstract":"Emperor penguins were observed nesting on Inaccessible I. during the 1973 winter. This is the southernmost nesting of emperor penguins thus far recorded; it also could be the first record of emperors attempting to start a new rookery. This site, however, may have been used by emperors in the past. The closest reported nesting of these penguins to Inaccessible I. is on the Ross Ice Shelf east of Cape Crozier. With the exception of the Inaccessible I. record, there is little evidence that emperor penguins breed in McMurdo Sound proper.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Antarctic Journal of the United States","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"6806_Jonkel.pdf","usgsCitation":"Jonkel, G., and Llano, G., 1975, Emperor penguins nesting on Inaccessible Island: Antarctic Journal of the United States, v. 9, no. 3, p. 93-95.","productDescription":"93-95","startPage":"93","endPage":"95","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056db","contributors":{"authors":[{"text":"Jonkel, G.M.","contributorId":55104,"corporation":false,"usgs":true,"family":"Jonkel","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":342748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Llano, G.A.","contributorId":56335,"corporation":false,"usgs":true,"family":"Llano","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":342749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70164431,"text":"70164431 - 1975 - Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2016-02-03T17:15:44","indexId":"70164431","displayToPublicDate":"2008-12-28T00:00:00","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":"Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana","docAbstract":"<p>A gravity survey of the Henrys Lake quadrangle shows that a gravity low with about 10 milligals of closure coincides with the Henrys Lake basin. The low is interpreted to reflect a basin fill of 1,100 m or more of Cenozoic sediments and volcanic rock. The data indicate that on the east and probably on the west the basin is bounded by northwest- and north-trending faults, and near its waist by the east-trending Centennial fault. A model constructed across the Henrys Lake basin suggests a northwest-trending fault, located near the southeast corner of Henrys Lake and concealed beneath the basin fill. The sparse gravity data east of the Centennial Mountains are not sufficient to provide any evidence on the extension of the Centennial fault across the Henrys Lake basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Peterson, D.L., and Witkind, I.J., 1975, Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana: Journal of Research of the U.S. Geological Survey, v. 3, no. 2.","productDescription":"6 p.","startPage":"228","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":316565,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue2/report.pdf","text":"Report","size":"28.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho, Montana, Wyoming","otherGeospatial":"Henrys Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              44.25\n            ],\n            [\n              -111,\n              45\n            ],\n            [\n              -111.75,\n              45\n            ],\n            [\n              -111.75,\n              44.25\n            ],\n            [\n              -111,\n              44.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"2","edition":"223","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b33320e4b0cc79997f3420","contributors":{"authors":[{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":597214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkind, Irving J.","contributorId":14469,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":597215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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