{"pageNumber":"356","pageRowStart":"8875","pageSize":"25","recordCount":10959,"records":[{"id":70000682,"text":"70000682 - 1982 - Channel systems and lobe construction in the Mississippi Fan","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000682","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Channel systems and lobe construction in the Mississippi Fan","docAbstract":"Morphological features on the Mississippi Fan in the eastern Gulf of Mexico were mapped using GLORIA II, a long-range side-scan sonar system. Prominent is a sinuous channel flanked by well-developed levees and occasional crevasse splays. The channel follows the axis and thickest part of the youngest fan lobe; seismic-reflection profiles offer evidence that its course has remained essentially constant throughout lobe development. Local modification and possible erosion of levees by currents indicates a present state of inactivity. Superficial sliding has affected part of the fan lobe, but does not appear to have been a factor in lobe construction. ?? 1982 A. M. Dowden, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462797","issn":"02760460","usgsCitation":"Garrison, L.E., Kenyon, N.H., and Bouma, A., 1982, Channel systems and lobe construction in the Mississippi Fan: Geo-Marine Letters, v. 2, no. 1-2, p. 31-39, https://doi.org/10.1007/BF02462797.","startPage":"31","endPage":"39","costCenters":[],"links":[{"id":203652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19001,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462797"}],"volume":"2","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e607b","contributors":{"authors":[{"text":"Garrison, L. E.","contributorId":66676,"corporation":false,"usgs":true,"family":"Garrison","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":346471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kenyon, Neil H.","contributorId":89535,"corporation":false,"usgs":false,"family":"Kenyon","given":"Neil","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bouma, A.H.","contributorId":107281,"corporation":false,"usgs":true,"family":"Bouma","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":346473,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221735,"text":"5221735 - 1982 - Distribution and status of Vicia menziesii Spreng. (Leguminosae): Hawai'i's first officially listed endangered plant species","interactions":[],"lastModifiedDate":"2023-09-14T17:58:14.286759","indexId":"5221735","displayToPublicDate":"2010-06-16T12:19:29","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1015,"text":"Biological Conservation","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Distribution and status of <i>Vicia menziesii</i> Spreng. (Leguminosae): Hawai'i's first officially listed endangered plant species","title":"Distribution and status of Vicia menziesii Spreng. (Leguminosae): Hawai'i's first officially listed endangered plant species","docAbstract":"<p id=\"simple-para.0010\"><i>Vicia menziesii</i><span>&nbsp;</span>Spreng., Hawai'i's first officially listed endangered plant species, formerly occurred across a large area in the upper montane-mesic forest habitat on the windward side of the island of Hawai'i. Until this species was ‘rediscovered’ in 1974, it had last been seen in 1915, and it was presumed to be extinct. The population is presently thought to number 150–300 plants, most of which are seedlings. These are located within a 200 ha area on the eastern flank of Mauna Loa volcano.</p><p id=\"simple-para.0015\">The primary factors responsible for the decline of<span>&nbsp;</span><i>V. menziesii</i><span>&nbsp;</span>are habitat loss and excessive predation on the plants by introduced ungulates. Continued logging and cattle grazing within its remnant range are major threats to its existence. Enhancing the survival of<span>&nbsp;</span><i>V. menziesii</i><span>&nbsp;</span>may best be accomplished by stabilizing its remaining habitat and allowing the population to reestablish itself naturally.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0006-3207(82)90034-9","usgsCitation":"Warshauer, F.R., and Jacobi, J., 1982, Distribution and status of Vicia menziesii Spreng. (Leguminosae): Hawai'i's first officially listed endangered plant species: Biological Conservation, v. 23, no. 2, p. 111-126, https://doi.org/10.1016/0006-3207(82)90034-9.","productDescription":"16 p.","startPage":"111","endPage":"126","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197305,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Hawai'i, Mauna Loa Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.6622740700458,\n              19.363812612335536\n            ],\n            [\n              -155.51105380670714,\n              19.235551369951082\n            ],\n            [\n              -155.45509564758615,\n              19.244356822861917\n            ],\n            [\n              -155.38581411724607,\n              19.350613895081167\n            ],\n            [\n              -155.3178649240277,\n              19.438585143126204\n            ],\n            [\n              -155.3585012062466,\n              19.472504188046685\n            ],\n            [\n              -155.3798186001973,\n              19.501392590816337\n            ],\n            [\n              -155.47774537865888,\n              19.54283215872283\n            ],\n            [\n              -155.57100897719386,\n              19.504532323951167\n            ],\n            [\n              -155.60498357380297,\n              19.481924885668775\n            ],\n            [\n              -155.62896564199755,\n              19.397747263253564\n            ],\n            [\n              -155.6622740700458,\n              19.363812612335536\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64959a","contributors":{"authors":[{"text":"Warshauer, F. R.","contributorId":39873,"corporation":false,"usgs":true,"family":"Warshauer","given":"F.","middleInitial":"R.","affiliations":[],"preferred":false,"id":334559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobi, J.D.","contributorId":13570,"corporation":false,"usgs":true,"family":"Jacobi","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":334558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223719,"text":"5223719 - 1982 - Anarbylus switaki Murphy: An addition to the herpetofauna of the United States with comments on relationships with Coleonyx","interactions":[],"lastModifiedDate":"2024-12-10T16:54:33.202718","indexId":"5223719","displayToPublicDate":"2010-06-16T12:19:23","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2334,"text":"Journal of Herpetology","active":true,"publicationSubtype":{"id":10}},"title":"Anarbylus switaki Murphy: An addition to the herpetofauna of the United States with comments on relationships with Coleonyx","docAbstract":"Anarbys switaki, a species previously known only from Baja California Sur, Mexico, occurs in eastern San Diego and southwestern Imperial Counties in California. In California, specimens tend to have continuous transverse bars on the body, are lighter in color, and more slender in body form than in southern Baja California. California populations appear to be confined to extremely rocky habitats in desert foothill situations between 200 and 600 m. The species appears to be secretive, and occurs in low densities within rock crevices and subterranean cavities. The morphological gap between Anarbylus and Coleonyx species may not warrant generic recognition. Anarbylus is part of a diverse lizard fauna in southern California and occurs in sympatry with 15 lizard species in a small area of southern California.","language":"English","publisher":"Society for the Study of Amphibians and Reptiles","doi":"10.2307/1563903","usgsCitation":"Fritts, T.H., Snell, H., and Martin, R., 1982, Anarbylus switaki Murphy: An addition to the herpetofauna of the United States with comments on relationships with Coleonyx: Journal of Herpetology, v. 16, no. 1, p. 39-52, https://doi.org/10.2307/1563903.","productDescription":"14 p.","startPage":"39","endPage":"52","numberOfPages":"14","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200341,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c40f","contributors":{"authors":[{"text":"Fritts, T. H.","contributorId":40147,"corporation":false,"usgs":true,"family":"Fritts","given":"T.","middleInitial":"H.","affiliations":[],"preferred":false,"id":339336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snell, H.L.","contributorId":49314,"corporation":false,"usgs":false,"family":"Snell","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":339337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, R.L.","contributorId":85296,"corporation":false,"usgs":true,"family":"Martin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":339338,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9966,"text":"ofr82493 - 1982 - The geology of the Kutztown and Hamburg 7 1/2-minute quadrangles, eastern Pennsylvania","interactions":[],"lastModifiedDate":"2026-01-21T17:27:28.454679","indexId":"ofr82493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-493","title":"The geology of the Kutztown and Hamburg 7 1/2-minute quadrangles, eastern Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82493","usgsCitation":"Lash, G.G., 1982, The geology of the Kutztown and Hamburg 7 1/2-minute quadrangles, eastern Pennsylvania: U.S. Geological Survey Open-File Report 82-493, 3 Plates: 9.08 x 11.46 inches or smaller, https://doi.org/10.3133/ofr82493.","productDescription":"3 Plates: 9.08 x 11.46 inches or smaller","costCenters":[],"links":[{"id":426552,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0493/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426551,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0493/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426550,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0493/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142425,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0493/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Pennsylvania","city":"Kutztown","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.79625118853856,\n              40.531669801963176\n            ],\n            [\n              -75.79625118853856,\n              40.50144072971335\n            ],\n            [\n              -75.74910540374503,\n              40.50144072971335\n            ],\n            [\n              -75.74910540374503,\n              40.531669801963176\n            ],\n            [\n              -75.79625118853856,\n              40.531669801963176\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d649","contributors":{"authors":[{"text":"Lash, G. G.","contributorId":60648,"corporation":false,"usgs":true,"family":"Lash","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":160585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7978,"text":"ofr82585 - 1982 - The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","interactions":[{"subject":{"id":7978,"text":"ofr82585 - 1982 - The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","indexId":"ofr82585","publicationYear":"1982","noYear":false,"title":"The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations"},"predicate":"SUPERSEDED_BY","object":{"id":38521,"text":"pp1355 - 1988 - The Giles County, Virginia, seismic zone– Seismological results and geological interpretations","indexId":"pp1355","publicationYear":"1988","noYear":false,"title":"The Giles County, Virginia, seismic zone– Seismological results and geological interpretations"},"id":1}],"supersededBy":{"id":38521,"text":"pp1355 - 1988 - The Giles County, Virginia, seismic zone– Seismological results and geological interpretations","indexId":"pp1355","publicationYear":"1988","noYear":false,"title":"The Giles County, Virginia, seismic zone– Seismological results and geological interpretations"},"lastModifiedDate":"2026-01-21T17:27:41.443217","indexId":"ofr82585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-585","title":"The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","docAbstract":"<p>This paper describes and interprets a newly-recognized 40-km-long seismogenic zone, which is inferred to have been the locus of a damaging earthquake in 1897. That shock was the second largest known to have occurred in the southeastern United States (MMI VIII, m<sup>b</sup> estimated at 5.8, felt over 725,000 km<sub>2</sub>). It struck Giles County in southwestern Virginia, and a recurrence would affect populous regions on and near the central Atlantic seaboard. This paper attempts to aid in evaluating that hazard by presenting and synthesizing new seismological data with geological inferences and deductions.</p><p>A five-station, 60-km aperture seismic network has been in operation in the Giles County locale since early 1978. For the subsequent 3-year monitoring period, 10 microearthquakes (M &lt; 2) have been detected. Eight of those 10 events, plus an additional 4 relocated felt earthquakes (3.2 &lt; M &lt; 4.1; 1959-1976) have a tabular distribution centered at Pearisburg, Virginia. That distribution is about 40 km long, 10 km wide, strikes N. 43° E., and has a nearly vertical extent of from 5 km to 25 km in depth. Thus, a Giles County seismogenic zone is defined presently by 12 earthquakes that span 4 orders of magnitude (0 &lt; M &lt; 4) and 2 decades of time (1959-1980). We conclude that the 1897 earthquake occurred on that seismogenic zone. From the orientation of the tabular zone, from evidence that greatest horizontal compressive stress trends east-northeasterly at seismogenic depths in and near Giles County and from sparse P-wave first-motion data, we infer that the monitored microseismicity probably occurs by right-reverse motion on the seismogenic zone, with the southeast side dropping down with respect to the northwest side.</p><p>In the Giles County locale, the upper 3-6 km of the crust are Paleozoic sedimentary rocks that have moved some tens of kilometers northwest on nearly horizontal detachment faults. The above-mentioned reliable hypocenters for the region lie below the deepest likely detachment, indicating that Giles County seismicity probably has no simple relationship to surface geology.</p><p>Since Precambrian time, three deformational episodes could have formed steep faults under today's surface structures, at the observed hypocentral depths. These episodes were as follows: (1) As the Iapetus Ocean (Atlantic's predecessor) opened in late Precambrian or early Paleozoic time, northeast-striking normal faults formed, probably at the inferred Iapetan continental edge in central Virginia and at least as far northwest of that locus as Giles County. (2) In late Paleozoic time, detachment faults loaded the crust with several kilometers of overthrust sedimentary rocks, perhaps forming northeast-striking thrust-load faults in a brittle analogue of isostatic depression caused by thrust masses and much lighter continental glaciers. (3) As the Atlantic Ocean opened in Mesozoic time, other northeast-striking normal faults formed on the present continental margin and inland of it.</p><p>The N. 43° E.-striking seismogenic zone seems most likely to have resulted from compressional reactivation of an Iapetan normal fault, which also may have been reactivated by late Paleozoic compression and Mesozoic extension. First, the seismogenic zone probably does not occur on a thrust-load fault. The zone underlies detached structures of southern Appalachian orientations (east-northeast), but those structures are not known to be displaced where they cross the zone. Thus, if the zone occurs on a thrust-load fault, the fault and its coeval causative central Appalachian detachments would pre-date the southern Appalachian structures. That deduction contradicts stratigraphic and structural estimates of relative ages of southern and central Appalachian detachments. Second, the zone probably does not result from a Mesozoic normal fault, because known locations of Mesozoic normal faults and grabens are well to the southeast of Giles County.</p><p>Not yet known is where else in the East reactivated Iapetan normal faults might generate shocks similar to that of 1897. However, our analysis enables us to suggest specific geological and geophysical investigations that may produce results useful in answering that question. Such investigations can concentrate on defining the area of probable occurrence of other Iapetan normal faults, and on determining whether the one inferred to underlie Giles County is uniquely active or is typical of others that might exist elsewhere.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82585","usgsCitation":"Bollinger, G.A., and Wheeler, R.L., 1982, The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations: U.S. Geological Survey Open-File Report 82-585, iv, 136 p., https://doi.org/10.3133/ofr82585.","productDescription":"iv, 136 p.","costCenters":[],"links":[{"id":412470,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0585/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140332,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0585/report-thumb.jpg"}],"country":"United States","state":"Virginia","county":"Giles County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-80.4761,37.4269],[-80.4506,37.3704],[-80.4417,37.3506],[-80.428,37.3194],[-80.4481,37.3088],[-80.4756,37.2905],[-80.4912,37.2822],[-80.5049,37.273],[-80.5147,37.2688],[-80.5302,37.2633],[-80.5551,37.2608],[-80.5787,37.2542],[-80.6075,37.2467],[-80.6219,37.2425],[-80.6724,37.2239],[-80.6828,37.2197],[-80.7051,37.209],[-80.7218,37.2039],[-80.7794,37.1888],[-80.804,37.1786],[-80.8286,37.1615],[-80.856,37.1476],[-80.8678,37.157],[-80.8824,37.1686],[-80.8624,37.1797],[-80.8725,37.1928],[-80.8947,37.1798],[-81.0099,37.2746],[-80.9785,37.294],[-80.9777,37.2934],[-80.9772,37.2932],[-80.9756,37.2931],[-80.9686,37.2927],[-80.9651,37.2932],[-80.9595,37.294],[-80.9566,37.2948],[-80.949,37.2971],[-80.9394,37.2999],[-80.9347,37.3015],[-80.9209,37.307],[-80.9111,37.3107],[-80.8985,37.3171],[-80.8916,37.3218],[-80.8859,37.3264],[-80.8813,37.33],[-80.8795,37.3312],[-80.8767,37.3332],[-80.8735,37.3352],[-80.8709,37.3368],[-80.8646,37.3401],[-80.8627,37.3411],[-80.859,37.3434],[-80.8544,37.3453],[-80.8516,37.3476],[-80.8504,37.3495],[-80.8532,37.3533],[-80.8705,37.371],[-80.8736,37.3737],[-80.8782,37.3777],[-80.8817,37.3817],[-80.8824,37.3848],[-80.8808,37.3889],[-80.8778,37.3926],[-80.8643,37.4096],[-80.8655,37.4132],[-80.8661,37.4159],[-80.8662,37.4184],[-80.8661,37.4189],[-80.8633,37.423],[-80.8627,37.4239],[-80.8575,37.4304],[-80.853,37.4278],[-80.8484,37.4256],[-80.8451,37.4257],[-80.842,37.4257],[-80.8367,37.4248],[-80.8321,37.4222],[-80.8244,37.4168],[-80.8157,37.4115],[-80.8097,37.4062],[-80.8051,37.4012],[-80.8021,37.3981],[-80.8004,37.3963],[-80.7986,37.3954],[-80.7968,37.395],[-80.7963,37.3948],[-80.7939,37.3946],[-80.7934,37.3945],[-80.7899,37.3945],[-80.7864,37.3936],[-80.7834,37.3923],[-80.7793,37.3878],[-80.7757,37.382],[-80.7709,37.3729],[-80.7629,37.3748],[-80.7531,37.3776],[-80.7507,37.3784],[-80.7423,37.3812],[-80.7307,37.3849],[-80.7248,37.3874],[-80.7198,37.3895],[-80.7052,37.3958],[-80.7048,37.396],[-80.684,37.4056],[-80.6696,37.4116],[-80.6518,37.4199],[-80.6363,37.4282],[-80.6276,37.4328],[-80.6219,37.4361],[-80.6176,37.4385],[-80.613,37.4404],[-80.6077,37.4427],[-80.6052,37.4439],[-80.603,37.445],[-80.5986,37.4473],[-80.5899,37.4523],[-80.5807,37.4583],[-80.5732,37.4628],[-80.5673,37.4661],[-80.5563,37.4707],[-80.55,37.4729],[-80.5407,37.4752],[-80.5309,37.4768],[-80.5182,37.4796],[-80.5156,37.48],[-80.5124,37.4806],[-80.5083,37.481],[-80.5054,37.4802],[-80.5026,37.4789],[-80.5002,37.4761],[-80.4984,37.473],[-80.4954,37.4666],[-80.4932,37.4596],[-80.4931,37.4528],[-80.4937,37.4487],[-80.4939,37.4467],[-80.4942,37.4446],[-80.4936,37.4419],[-80.4919,37.4396],[-80.4905,37.4379],[-80.4901,37.4374],[-80.4884,37.4356],[-80.486,37.4333],[-80.4831,37.4319],[-80.4802,37.4283],[-80.4761,37.4269]]]},\"properties\":{\"name\":\"Giles\",\"state\":\"VA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c56e","contributors":{"authors":[{"text":"Bollinger, G. A.","contributorId":55809,"corporation":false,"usgs":true,"family":"Bollinger","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":156925,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7503,"text":"ofr82916 - 1982 - Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","interactions":[],"lastModifiedDate":"2017-09-01T14:57:41","indexId":"ofr82916","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-916","title":"Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980","docAbstract":"<p>The Price River basin in east-central Utah includes a significant part of the Wasatch Plateau and Book Cliffs coal-fields area (pi. 1) and currently (1980) is part of the most active coal-mining areas in the State.</p><p>This report presents data gathered by the U.S. Geological Survey as part of a hydrologic study carried out during the water years 1979 and 1980 in cooperation with the U.S. Bureau of Land Management. The data were obtained in the field or from private, State, and other Federal agencies. The purpose of this report is to make the data available to those engaged in coal mining, to those assessing water resources that may possibly be affected by coal mining, and to supplement two interpretive reports that will be published at a later date. Other sources of hydrologic data in the Price River basin include Waddell and others, 1978 and Sumsion, 1979.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82916","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Waddell, K., Dodge, J., Darby, D., and Theobald, S., 1982, Selected hydrologic data, Price River basin, Utah, water years 1979 and 1980: U.S. Geological Survey Open-File Report 82-916, Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in., https://doi.org/10.3133/ofr82916.","productDescription":"Report: iv, 73 p.; Plate: 23.85 in. x 22.64 in.","numberOfPages":"77","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":34957,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0916/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0916/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0916/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8830","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":155918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dodge, J.E.","contributorId":21133,"corporation":false,"usgs":true,"family":"Dodge","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":155915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darby, D.W.","contributorId":49333,"corporation":false,"usgs":true,"family":"Darby","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":155916,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Theobald, S.M.","contributorId":51270,"corporation":false,"usgs":true,"family":"Theobald","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":155917,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9314,"text":"ofr82148 - 1982 - Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana","interactions":[],"lastModifiedDate":"2022-08-17T19:26:33.808343","indexId":"ofr82148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-148","title":"Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82148","usgsCitation":"Hammarstrom, J.M., 1982, Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana: U.S. Geological Survey Open-File Report 82-148, ii, 177 p., https://doi.org/10.3133/ofr82148.","productDescription":"ii, 177 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":405276,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75619.htm","linkFileType":{"id":5,"text":"html"}},{"id":37034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0148/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0148/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.125,\n              45.35\n            ],\n            [\n              -112.75,\n              45.35\n            ],\n            [\n              -112.75,\n              45.75\n            ],\n            [\n              -113.125,\n              45.75\n            ],\n            [\n              -113.125,\n              45.35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e487a","contributors":{"authors":[{"text":"Hammarstrom, J. M.","contributorId":34513,"corporation":false,"usgs":true,"family":"Hammarstrom","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35861,"text":"b1531 - 1982 - Mineral resources of the Big Frog Wilderness Study Area and additions, Polk County, Tennessee and Fannin County, Georgia","interactions":[{"subject":{"id":40483,"text":"ofr79129 - 1979 - Coal resource occurrence and coal development potential maps of the southeast quarter of the Superior 15-minute quadrangle, Sweetwater County, Wyoming","indexId":"ofr79129","publicationYear":"1979","noYear":false,"title":"Coal resource occurrence and coal development potential maps of the southeast quarter of the Superior 15-minute quadrangle, Sweetwater County, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":35861,"text":"b1531 - 1982 - Mineral resources of the Big Frog Wilderness Study Area and additions, Polk County, Tennessee and Fannin County, Georgia","indexId":"b1531","publicationYear":"1982","noYear":false,"title":"Mineral resources of the Big Frog Wilderness Study Area and additions, Polk County, Tennessee and Fannin County, Georgia"},"id":1}],"lastModifiedDate":"2021-09-24T14:00:44.169799","indexId":"b1531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1531","title":"Mineral resources of the Big Frog Wilderness Study Area and additions, Polk County, Tennessee and Fannin County, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. G.P.O.,","doi":"10.3133/b1531","usgsCitation":"Slack, J.F., Gazdik, G.C., and Dunn, M.L., 1982, Mineral resources of the Big Frog Wilderness Study Area and additions, Polk County, Tennessee and Fannin County, Georgia: U.S. Geological Survey Bulletin 1531, vi, 25 p., https://doi.org/10.3133/b1531.","productDescription":"vi, 25 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":63817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1531/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1531/report-thumb.jpg"},{"id":389712,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21615.htm"}],"country":"United States","state":"Georgia, Tennessee","otherGeospatial":"Big Frog Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.5580,\n              34.9830\n            ],\n            [\n              -84.4850,\n              34.9830\n            ],\n            [\n              -84.4850,\n              35.058104573869024\n            ],\n            [\n              -84.5580,\n              35.058104573869024\n            ],\n            [\n              -84.5580,\n              34.9830\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69b072","contributors":{"authors":[{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":215345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gazdik, Gertrude C.","contributorId":56220,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":215346,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Maynard L. Jr.","contributorId":70457,"corporation":false,"usgs":true,"family":"Dunn","given":"Maynard","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":215347,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9660,"text":"ofr8220 - 1982 - Gulf of Alaska and Lower Cook Inlet summary report 3: Second revision of Outer Continental Shelf oil and gas activities in the Gulf of Alaska (including Lower Cook Inlet) and their onshore impacts: A summary report, September 1980","interactions":[],"lastModifiedDate":"2022-09-19T22:18:48.794983","indexId":"ofr8220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-20","title":"Gulf of Alaska and Lower Cook Inlet summary report 3: Second revision of Outer Continental Shelf oil and gas activities in the Gulf of Alaska (including Lower Cook Inlet) and their onshore impacts: A summary report, September 1980","docAbstract":"<p>Five Outer Continental Shelf (OCS) lease sales have been held in the Gulf of Alaska subregion of Alaska. Lease Sale 39, in the northern Gulf of Alaska, was held on April 13, 1976, and it resulted in the leasing of 76 tracts. Lease Sale CI, held on October 27, 1977, resulted in the leasing of 87 tracts in Lower Cook Inlet. Lease Sale 55 in the eastern Gulf of Alaska, held on October 21, 1980, leased 35 tracts. The first Reoffering Sale (RS-1), held on June 30, 1981, resulted in the leasing of one tract in the eastern Gulf of Alaska. Lease Sale 60, the most recent sale in the subregion, was held on September 29, 1981. It resulted in the leasing of 13 tracts in the Lower Cook Inlet and the Shelikof Strait. Exploratory drilling has been conducted on tracts leased in Lease Sales 39 and CI. No commercial discoveries were made, and no further exploratory drilling is anticipated on tracts leased in either sale. ARCO has plans to explore a tract leased in Lease Sale 55 in January 1983. Chevron has conducted geohazard studies on tracts leased in Lease Sale 60. The results of these studies will determine if exploratory wells will be drilled. Exploratory drilling, if it does take place, is not anticipated before the summer of 1983.</p><p>In March 1982, the Department of the Interior prepared new resource estimates for the Gulf of Alaska subregion. The risked mean resource estimates for tracts leased in Lease Sale 55 and Lease Sale RS-1 are 12.1 million barrels of oil and 46.2 billion cubic feet of gas. The risked mean resource estimates for tracts leased in Lease Sale 60 are 5.6 million barrels of oil and 5 billion cubic feet of gas.</p><p>The onshore impacts from previous OCS exploration in the Gulf of Alaska and the Lower Cook Inlet were minimal. Yakutat will be used to support exploratory drilling on any Lease Sale 55 or Lease Sale RS-1 tracts. If exploratory drilling takes place on Lease Sale 60 tracts, support facilities are expected to be located in Kenai or on Kodiak Island.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8220","collaboration":"Prepared for the U.S. Department of the Interior, Minerals Management Service, in cooperation with the U.S. Geological Survey","usgsCitation":"Jackson, J.B., and Kurz, F.N., 1982, Gulf of Alaska and Lower Cook Inlet summary report 3: Second revision of Outer Continental Shelf oil and gas activities in the Gulf of Alaska (including Lower Cook Inlet) and their onshore impacts: A summary report, September 1980: U.S. Geological Survey Open-File Report 82-20, viii, 79 p., https://doi.org/10.3133/ofr8220.","productDescription":"viii, 79 p.","costCenters":[],"links":[{"id":407019,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0020/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0020/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Gulf of Alaska, Outer Continental Shelf","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -176.923828125,\n              50.680797145321655\n            ],\n            [\n              -140.712890625,\n              50.680797145321655\n            ],\n            [\n              -140.712890625,\n              60.1524422143808\n            ],\n            [\n              -176.923828125,\n              60.1524422143808\n            ],\n            [\n              -176.923828125,\n              50.680797145321655\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a236","contributors":{"authors":[{"text":"Jackson, Joanne Barnes","contributorId":31752,"corporation":false,"usgs":true,"family":"Jackson","given":"Joanne","email":"","middleInitial":"Barnes","affiliations":[],"preferred":false,"id":160075,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurz, Frederick N.","contributorId":47785,"corporation":false,"usgs":true,"family":"Kurz","given":"Frederick","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":160076,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36629,"text":"fwsobs80_67 - 1982 - A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"fwsobs80_67","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"80/67","title":"A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Nawrot, J.R., Woolf, A., and Klimstra, W., 1982, A guide for enhancement of fish and wildlife on abandoned mine lands in the eastern United States: FWS/OBS 80/67, x, 101 p. : ill., 1 map; 28 cm.","productDescription":"x, 101 p. : ill., 1 map; 28 cm.","costCenters":[],"links":[{"id":162174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5d5","contributors":{"authors":[{"text":"Nawrot, Jack R.","contributorId":60283,"corporation":false,"usgs":true,"family":"Nawrot","given":"Jack","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woolf, A.","contributorId":18421,"corporation":false,"usgs":true,"family":"Woolf","given":"A.","affiliations":[],"preferred":false,"id":216688,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klimstra, W.D.","contributorId":59084,"corporation":false,"usgs":true,"family":"Klimstra","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":216689,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40899,"text":"ofr82562 - 1982 - Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:57:58.601919","indexId":"ofr82562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-562","title":"Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Judith River Formation occurs under water-table and artesian conditions. The direction of regional ground-water movement is from west to east. Water is discharged from the Judith River Formation to the Milk River from near Havre, Montana, to Malta and to the Missouri River south of the Bearpaw and Little Rocky Mountains. The average discharge from 236 wells is about 10 gallons per minute, and the specific capacity of 186 wells averages 0.66 gallon per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82562","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-562, 1 Plate: 40.47 × 23.06 inches, https://doi.org/10.3133/ofr82562.","productDescription":"1 Plate: 40.47 × 23.06 inches","costCenters":[],"links":[{"id":407485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75640.htm","linkFileType":{"id":5,"text":"html"}},{"id":78781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              45\n            ],\n            [\n              -104.0418,\n              45\n            ],\n            [\n              -104.0418,\n              49\n            ],\n            [\n              -111,\n              49\n            ],\n            [\n              -111,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2f5","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38648,"text":"pp813T - 1982 - Summary appraisals of the nation's ground-water resources – New England region","interactions":[],"lastModifiedDate":"2021-12-14T21:58:30.42222","indexId":"pp813T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"813","chapter":"T","title":"Summary appraisals of the nation's ground-water resources – New England region","docAbstract":"<p>The New England Region has a total area of about 62,400 square miles (160,000 km<sup>2</sup>) and includes the States of Maine and New Hampshire, eastern Vermont, most of Massachusetts and Connecticut, all of Rhode Island, and a small part of southeastern New York. The longest stream is the Connecticut River, which extends from northern Vermont and New Hampshire, through western Massachusetts and central Connecticut, and drains into Long Island Sound. Other major streams are the Penobscot and Kennebec Rivers in Maine, the Androscoggin in Maine and New Hampshire, the Merrimack in New Hampshire and Massachusetts, and the Housatonic in western Massachusetts and Connecticut. Of the smaller streams, some, like the Charles River in the Boston area, are widely known because of their proximity to large population centers.</p>\n<p>Ground water occurs in two types of geologic materials: consolidated rocks and unconsolidated sedimentary rocks. The consolidated rocks underlie the entire region. They include crystalline igneous and metamorphic rocks and consolidated sedimentary rocks-shale, sandstone, and limestone and other carbonate rocks. The most productive unconsolidated rocks are sand and gravel of glacial origin. These deposits occur all over Cape Cod and nearby islands in southeastern Massachusetts and in many valleys throughout the region.</p>\n<p>Ground water is derived from precipitation. It can be intercepted for use by pumping from wells (1) before it discharges to the streams as base flow and (2) before it drains directly into coastal wetlands, bays, Long Island Sound, or the ocean.</p>\n<p>Withdrawals of fresh ground water in 1975 aggregated about 220 billion gallons (830 hm<sup>3</sup>), or about 12 percent of the total freshwater withdrawals (from all sources) of 1,800 billion gallons (6,800 hm<sup>3</sup>). In view of the available ground-water reserves, considerable additional water, for the anticipated continuing increase in population and economic activity, could be developed.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813T","usgsCitation":"Sinnott, A., 1982, Summary appraisals of the nation's ground-water resources – New England region: U.S. Geological Survey Professional Paper 813, vi, 23 p., https://doi.org/10.3133/pp813T.","productDescription":"vi, 23 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5074.htm"},{"id":65480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813t/report.pdf","text":"Report","size":"6.64 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-68.6865234375,\n              47.30903424774781\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69967f","contributors":{"authors":[{"text":"Sinnott, Allen","contributorId":15995,"corporation":false,"usgs":true,"family":"Sinnott","given":"Allen","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":220217,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9854,"text":"ofr82849 - 1982 - Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-849","title":"Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","docAbstract":"Linear features are relatively short, distinct, non-cultural linear elements mappable on Landsat multispectral scanner images (MSS). Most linear features are related to local topographic features, such as cliffs, slope breaks, narrow ridges, and stream valley segments that are interpreted as reflecting directed aspects of local geologic structure including faults, zones of fracturing (joints), and the strike of tilted beds. \r\n\r\n6,050 linear features were mapped on computer-enhanced Landsat MSS images of 11 Landsat scenes covering an area from the Rio Grande rift zone on the east to the Grand Canyon on the west and from the San Juan Mountains, Colorado, on the north to the Mogollon Rim on the south. Computer-aided statistical analysis of the linear feature data revealed 5 statistically important trend intervals: 1.) N. 10W.-N.16E., 2.) N.35-72E., 3.) N.33-59W., 4.) N. 74-83W., and 5.) N.89-9-W. and N. 89-90E. Subsequent analysis of the distribution of the linear features indicated that only the first three trend intervals are of regional geologic significance. Computer-generated maps of the linear features in each important trend interval were prepared, as well as contour maps showing the relative concentrations of linear features in each trend interval. These maps were then analyzed for patterns suggestive of possible regional tectonic lines. \r\n\r\n20 possible tectonic lines, or lineaments, were interpreted from the maps. One lineament is defined by an obvious change in overall linear feature concentrations along a northwest-trending line cutting across northeastern Arizona. Linear features are abundant northeast of the line and relatively scarce to the southwest. The remaining 19 lineaments represent the axes of clusters of parallel linear features elongated in the direction of the linear feature trends. Most of these lineaments mark previously known structural zones controlled by linear features in the Precambrian basement or show newly recognized relationships to geological and/or geophysical patterns that suggest probable influence by buried basement features. The remaining few lineaments are not strongly correlative with geological or geophysical patterns, but on the basis of existing data they cannot be dismissed as being possible expressions of basement features.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82849","usgsCitation":"Knepper, D.H., 1982, Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States: U.S. Geological Survey Open-File Report 82-849, 81 p., 1 over-size sheet, ill., maps ;30 cm., https://doi.org/10.3133/ofr82849.","productDescription":"81 p., 1 over-size sheet, ill., maps ;30 cm.","costCenters":[],"links":[{"id":141873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0849/report-thumb.jpg"},{"id":37635,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0849/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0849/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50c8","contributors":{"authors":[{"text":"Knepper, Daniel H. dknepper@usgs.gov","contributorId":1242,"corporation":false,"usgs":true,"family":"Knepper","given":"Daniel","email":"dknepper@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":160411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11230,"text":"ofr821019 - 1982 - A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr821019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1019","title":"A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations","docAbstract":"Most stations in the U.S. Geological Survey's National Stream Quality Accounting Network show no significant trend in either dissolved oxygen concentration or fecal coliform bacteria population for the period October 1974. through October 1981. Of the stations which do show trends, however, most show improved water quality: thirty-one of a total of 276 stations show rising dissolved oxygen concentrations, while only 17 show decreasing concentrations. Decreases in fecal coliform populations have occurred at 21 stations while increases have occurred at only 12 stations. \r\n\r\nApproximately half of the stations showing improving trends in dissolved oxygen and fecal coliform bacteria are in the Missouri-Mississippi-Ohio River system. Decreases in dissolved oxygen have occurred at scattered locations in the Western and South-Central States. Rising bacterial populations occur most frequently in the Eastern and Central States \r\n\r\nTrends in dissolved oxygen concentration resulting from temperature changes occurring during the study period can be separated from trends caused by chemical or biological processes by analyzing computed values of dissolved oxygen deficit. About half of the observed trends in dissolved oxygen appear to be the result of changes in water temperature.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821019","usgsCitation":"Smith, R.A., and Alexander, R.B., 1982, A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations: U.S. Geological Survey Open-File Report 82-1019, [i], 8 p. maps ;28 cm., https://doi.org/10.3133/ofr821019.","productDescription":"[i], 8 p. maps ;28 cm.","costCenters":[],"links":[{"id":143993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1019/report-thumb.jpg"},{"id":39020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6120","contributors":{"authors":[{"text":"Smith, Richard A. 0000-0003-2117-2269 rsmith1@usgs.gov","orcid":"https://orcid.org/0000-0003-2117-2269","contributorId":580,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rsmith1@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":162771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, Richard B. 0000-0001-9166-0626 ralex@usgs.gov","orcid":"https://orcid.org/0000-0001-9166-0626","contributorId":541,"corporation":false,"usgs":true,"family":"Alexander","given":"Richard","email":"ralex@usgs.gov","middleInitial":"B.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":162770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60223,"text":"mf1342C - 1982 - Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho","interactions":[],"lastModifiedDate":"2018-10-22T14:19:58","indexId":"mf1342C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1342","chapter":"C","title":"Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho","docAbstract":"<p>Parts of both the Targhee and Beaverhead National Forests are within the study area. Four contiguous parcels of land, totaling about 96,176 acres (38,922 ha) make up the area. The first of these encompasses about 46,126 acres (18,667 ha), is wholly in Montana, and includes an addition by the Bureau of Land Management. The second area, in the Targhee National Forest, consists of some 38,750 acres (15,682 ha) within Idaho. The third and fourth parcels include about 11,300 acres (4,573 ha) in the Beaverhead..and Targhee National Forests that overlies the Mt. Jefferson and Sawtell Peak areas in the eastern part of the Centennial Mountains.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1342C","usgsCitation":"Martin, R., 1982, Geophysical survey of the Centennial Mountains Wilderness Study Area and contiguous areas, Beaverhead County, Montana and Clark and Fremont counties, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1342, 33.80 x 40.03 inches, https://doi.org/10.3133/mf1342C.","productDescription":"33.80 x 40.03 inches","costCenters":[],"links":[{"id":358634,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1342-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1342-C/report-thumb.jpg"}],"scale":"0","country":"United States","state":"Idaho, Montana","county":"Beaverhead County, Clark County, Fremont County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25,\n              44.5\n            ],\n            [\n              -112.25,\n              44.6667\n            ],\n            [\n              -111.25,\n              44.6667\n            ],\n            [\n              -111.25,\n              44.5\n            ],\n            [\n              -112.25,\n              44.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b49f","contributors":{"authors":[{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":263344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7457,"text":"ofr821033 - 1982 - Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr821033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1033","title":"Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States","docAbstract":"Maximum horizontal accelerations and velocities caused by earthquakes are mapped for exposure times of 10, 50 and 250 years at the 90-percent probability level of nonexceedance for the contiguous United States. In many areas these new maps differ significantly from the 1976 probabilistic acceleration map by Algermlssen and Perkins because of the increase in detail, resulting from greater emphasis on the geologic basis for seismic source zones. This new emphasis is possible because of extensive data recently acquired on Holocene and Quaternary faulting in the western United States and new interpretations of geologic structures controlling the seismicity pattern in the central and eastern United States. ","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821033","usgsCitation":"Algermissen, S.T., Perkins, D.M., Thenhaus, P., Hanson, S., and Bender, B., 1982, Probabilistic estimates of maximum acceleration and velocity in rock in the contiguous United States: U.S. Geological Survey Open-File Report 82-1033, 107 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr821033.","productDescription":"107 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1033/report-thumb.jpg"},{"id":34868,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34869,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34870,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34871,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34872,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34873,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1033/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660d58","contributors":{"authors":[{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":155704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, D. M.","contributorId":83922,"corporation":false,"usgs":true,"family":"Perkins","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thenhaus, P.C.","contributorId":46089,"corporation":false,"usgs":true,"family":"Thenhaus","given":"P.C.","affiliations":[],"preferred":false,"id":155701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, S.L.","contributorId":47361,"corporation":false,"usgs":true,"family":"Hanson","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":155702,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bender, B.L.","contributorId":99976,"corporation":false,"usgs":true,"family":"Bender","given":"B.L.","email":"","affiliations":[],"preferred":false,"id":155705,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7738,"text":"ofr821023 - 1982 - Selected hydrologic data for northern Utah Valley, Utah, 1935-82","interactions":[],"lastModifiedDate":"2022-09-19T22:17:45.843729","indexId":"ofr821023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1023","title":"Selected hydrologic data for northern Utah Valley, Utah, 1935-82","docAbstract":"<p>This report contains hydrologic data collected in northern Utah Valley from 1935 to 1982. Northern Utah Valley is approximately the northern half of an alluvial-filled basin partly occupied by Utah Lake in north-central Utah. The report area is bounded by the Wasatch Range on the east, the Lake Mountains on the west, and the Traverse Mountains on the north. Its southern boundary is the boundary between Townships 7 and 8 south, Salt Lake Base Line and Meridian.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821023","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Appel, C.L., Clark, D.W., and Fairbanks, P.E., 1982, Selected hydrologic data for northern Utah Valley, Utah, 1935-82: U.S. Geological Survey Open-File Report 82-1023, Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches, https://doi.org/10.3133/ofr821023.","productDescription":"Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":407017,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407016,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1023/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Utah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"This report was also published as Utah Hydrologic Data Report 39","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a144","contributors":{"authors":[{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fairbanks, Paul E.","contributorId":66254,"corporation":false,"usgs":true,"family":"Fairbanks","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156518,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","interactions":[{"subject":{"id":41283,"text":"ofr82583 - 1982 - Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada","indexId":"ofr82583","publicationYear":"1982","noYear":false,"title":"Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","indexId":"cir877","publicationYear":"1982","noYear":false,"title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment"},"id":1}],"lastModifiedDate":"2021-10-04T12:00:46.023373","indexId":"cir877","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"877","title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir877","usgsCitation":"Miller, C.D., Mullineaux, D.R., Crandell, D.R., and Bailey, R., 1982, Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment: U.S. Geological Survey Circular 877, iii, 10 p., https://doi.org/10.3133/cir877.","productDescription":"iii, 10 p.","costCenters":[],"links":[{"id":31475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0877/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0877/report-thumb.jpg"},{"id":390138,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23969.htm"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Long Valley - Mono Lake area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.50927734374999,\n              37.33522435930639\n            ],\n            [\n              -118.27880859375001,\n              37.33522435930639\n            ],\n            [\n              -118.27880859375001,\n              38.40194908237822\n            ],\n            [\n              -119.50927734374999,\n              38.40194908237822\n            ],\n            [\n              -119.50927734374999,\n              37.33522435930639\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683625","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":148957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148958,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148959,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":148960,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25963,"text":"wri8247 - 1982 - Ground-water resources of the White River basin, Delaware County, Indiana","interactions":[],"lastModifiedDate":"2020-11-05T21:15:00.164788","indexId":"wri8247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-47","title":"Ground-water resources of the White River basin, Delaware County, Indiana","docAbstract":"<p><span>The ground-water resources of the White River basin in and near Delaware </span><span>County, Indiana, were investigated by mapping the aquifers, calculating their </span><span>hydraulic properties, determining the distribution of potentiometric head, and </span><span>determining some of the components of the ground-water budget from data collect</span><span>ed in the field. This information was used to construct and calibrate a seven-</span><span>layer, digital ground-water-flow model. The model, constructed and calibrated </span><span>to water-level and seepage data collected during the study, simulates conditions </span><span>for the autumn of 1977. The model was used to assess ground-water potential in </span><span>terms of yield, drawdown, and streamflow depletion. </span></p><p><span>Drift covers nearly the entire area and generally ranges in thickness from 0 to 500 feet. Beneath the drift lie Silurian and Ordovician limestone, dolomite, and shale. A bedrock valley trends east-west through the center of the area. Bedrock surface relief is about 400 feet. </span></p><p><span>Six confined sand and gravel aquifers interbedded in the drift, a bedrock aquifer, and an unconfined outwash aquifer are the three major aquifer systems. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers generally range in thickness from 5 to 40 feet and have an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying all of Delaware County has a permeable thickness estimated to be 150 feet and an average transmissivity of 1,000 square feet per day. </span></p><p><span>Observation-well records indicate that water-level fluctuation is seasonal and has no long-term trends. Municipal and industrial ground-water pumpage for 1976 was 3.1 million gallons per day (4.8 cubic feet per second). On October 29, 1977, when the flow duration in the White River at Muncie was 80 percent, ground-water seepage to streams was 81 cubic feet per second. The water budget simulated in the model indicated that the rate of inflow to the ground-water system in the modeled area is 102 cubic feet per second: 80 percent from effective areal recharge of precipitation and 20 percent from ground-water flow across the area boundaries. Two percent of the ground-water discharge is pump-age, 66 percent is seepage to streams, and the remaining 32 percent is flow across the area boundaries. </span></p><p><span>Simulations of seven pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems. Model results indicate that as much as 3 million gallons per day can be developed from well fields where the average drawdown is 20 feet. Model simulations also indicate that 7 million gallons per day is available from a potential well field around Muncie. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8247","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Arihood, L.D., and Lapham, W.W., 1982, Ground-water resources of the White River basin, Delaware County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 82-47, vi, 69 p., https://doi.org/10.3133/wri8247.","productDescription":"vi, 69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380218,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0047/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Delaware County","otherGeospatial":"White River basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.4451,40.3792],[-85.2205,40.379],[-85.2182,40.3073],[-85.2168,40.2198],[-85.2165,40.135],[-85.2157,40.0765],[-85.5763,40.0769],[-85.5784,40.3794],[-85.4451,40.3792]]]},\"properties\":{\"name\":\"Delaware\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696a92","contributors":{"authors":[{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8829,"text":"ofr82888 - 1982 - Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2020-04-30T16:28:14.587118","indexId":"ofr82888","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-888","title":"Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","docAbstract":"<p>The Mariano Lake uranium deposit, hosted by the Brushy Basin Member of the Jurassic Morrison Formation, occurs in the trough of an east-west trending syncline at the western end of the Smith Lake-Mariano Lake group of uranium deposits near Crownpoint, New Mexico. The orebody, which contains abundant amorphous organic material, is situated on the reduced side of a regional reduction-oxidation (redox) interface. The presence of amorphous organic material suggests the orebody may represent a tabular (primary) deposit, whereas the close proximity of the orebody to the redox interface is suggestive that uranium was secondarily redistributed by oxidative processes from pre-existing tabular orebodies. Uranium contents correlate positively with both organic carbon and vanadium contents. Petrographic evidence and scanning electron microscope-energy dispersive analyses point to uranium residence in the epigentically introduced amorphous organic material, which coats detrital grains and fills voids. Uranium mineralization was preceded by the following diagenetic alterations: precipitation of pyrite (ẟ<sup>34</sup>S values ranging from-11.0 to-38.2 per mil); precipitation of mixed-layer smectite-illite clays; partial dissolution of some of the detrital feldspar population; and precipitation of quartz and adularia overgrowths. Alterations associated with uranium mineralization include emplacement of amorphous organic material (possibly uranium bearing); destruction of detrital iron-titanium oxide grains; coprecipitation of chlorite and microcrystalline quartz, and precipitation of pyrite and marcasite (ẟ<sup>34</sup>S values for these sulfides ranging from -29.4 to -41.6 per mil). After mineralization, calcite, dolomite, barite, and kaolinite precipitated, and authigenic iron disulfides were replaced by ferric oxides and hydroxides. Geochemical data (primarily the positive correlation of uranium content to both organic carbon and vanadium contents) and petrographic observations (epigentically introduced amorphous organic matter and uranium residence in this organic matter) indicate that the Mariano Lake orebody is a tabular-type uranium deposit. Oxidative processes have not noticeably redistributed and reconcentrated primary uranium in the immediate vicinity of the deposit nor have they greatly modified geochemical characteristics in the ore. Preservation of the Mariano Lake deposit may not only be related to its position along the synclinal trough, where oxidative destruction of the orebody has been inhibited by stagnation of oxidizing ground waters by the structure, but also due to the deflection of ground waters (resulting from low orebody porosity) around the orebody.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82888","usgsCitation":"Fishman, N.S., and Reynolds, R.L., 1982, Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 82-888, iii, 52 p., https://doi.org/10.3133/ofr82888.","productDescription":"iii, 52 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":141608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0888/report-thumb.jpg"},{"id":36405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.0452,36.006],[-108.7687,36.0063],[-108.3738,36.0044],[-108.2646,36.0038],[-108.1559,36.0027],[-108.1468,36.0028],[-108.1411,36.0029],[-108.1224,36.0028],[-107.8738,36.0034],[-107.8351,36.0035],[-107.6776,36.0031],[-107.66,36.0034],[-107.6423,36.0032],[-107.6247,36.0034],[-107.6213,36.003],[-107.6042,36.0032],[-107.5866,36.003],[-107.5718,36.0027],[-107.5541,36.0025],[-107.5513,36.0026],[-107.5161,36.0026],[-107.4421,36.0008],[-107.4068,36.0007],[-107.3875,36.0009],[-107.3397,36.0006],[-107.317,36.0008],[-107.3056,36.0005],[-107.3054,35.991],[-107.3058,35.9765],[-107.3055,35.9311],[-107.3051,35.8744],[-107.3049,35.8295],[-107.3047,35.8168],[-107.3053,35.7864],[-107.3054,35.7573],[-107.3057,35.7419],[-107.3049,35.7301],[-107.3052,35.7151],[-107.305,35.6997],[-107.3053,35.6852],[-107.305,35.6707],[-107.3048,35.6552],[-107.3046,35.6439],[-107.3041,35.6139],[-107.3032,35.5277],[-107.3035,35.4787],[-107.3025,35.4247],[-107.3016,35.3021],[-107.518,35.3036],[-107.5231,35.3036],[-107.6183,35.3059],[-107.6229,35.3059],[-107.6231,35.3159],[-107.6243,35.3485],[-107.7287,35.3489],[-107.7295,35.3366],[-107.7288,35.3062],[-107.7812,35.3063],[-107.8111,35.3063],[-107.8297,35.3065],[-107.8336,35.3064],[-107.9159,35.3065],[-107.9351,35.3066],[-107.9396,35.3065],[-107.974,35.3064],[-107.992,35.3066],[-108.0473,35.307],[-108.143,35.3057],[-108.151,35.307],[-108.2558,35.3077],[-108.364,35.3065],[-108.4661,35.3081],[-108.4644,35.2214],[-108.4659,35.1623],[-108.4661,35.1355],[-108.4673,35.0501],[-108.4678,34.9597],[-108.497,34.96],[-108.52,34.96],[-108.7809,34.9595],[-109.0458,34.9611],[-109.0458,35.166],[-109.0457,35.1796],[-109.0457,35.1941],[-109.0457,35.2078],[-109.0457,35.2228],[-109.0457,35.2359],[-109.0456,35.3531],[-109.0457,35.6637],[-109.0452,36.006]]]},\"properties\":{\"name\":\"McKinley\",\"state\":\"NM\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e15","contributors":{"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30462,"text":"wri8169 - 1982 - Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","interactions":[],"lastModifiedDate":"2017-06-07T12:25:54","indexId":"wri8169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-69","title":"Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","docAbstract":"<p>Parts of the East Branch Mahoning Creek basin, a forested area of 29.6 square miles in west-central Pennsylvania, are disturbed by farming, surface mining, unpaved haul roads, eroding reclaimed areas, and logging. Streamflow was measured and water samples collected at a site upstream from the mouth from June 1979 to June 1980 during base flow and storm periods to evaluate sediment discharges. An additional site on a tributary draining mostly farmland was sampled from December 1979 to June 1980. Samples were analyzed for suspended sediment, turbidity, and specific conductance. Daily mean suspended-sediment concentrations and discharges were computed.</p>\n<p>From June 1979 to June 1980, 3,570 tons of suspended sediment was transported from the basin. This was an average yield of 121 tons per square mile per year. From December 1979 to June 1980, a tributary draining 2.21 square miles of a predominantly agricultural area discharged 328 tons of sediment which was 12 percent of the sediment load transported from the entire basin.</p>\n<p>Monthly sediment discharges averaged 298 tons ranged from 32 tons in July to 1,250 tons in March. The highest daily mean suspended-sediment concentration was 712 milligrams per liter on June 8, 1980. On that date, 267 tons of sediment was discharged from the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8169","collaboration":"Prepared in cooperation with the  Pennsylvania Department of Environmental Resources, Bureau of Mining and Reclamation","usgsCitation":"Wetzel, K.L., 1982, Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980: U.S. Geological Survey Water-Resources Investigations Report 81-69, iv, 33 p., https://doi.org/10.3133/wri8169.","productDescription":"iv, 33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":159817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri8169.jpg"},{"id":318653,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0069/report.pdf"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"East Branch Mahoning Creek 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Kim L.","contributorId":104884,"corporation":false,"usgs":true,"family":"Wetzel","given":"Kim","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10641,"text":"ofr82158 - 1982 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80","interactions":[],"lastModifiedDate":"2017-03-29T14:28:14","indexId":"ofr82158","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-158","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80","docAbstract":"<p>Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year.</p>\n<p>The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.</p>\n<p>The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Sal ado Creek (lower station) at San Antonio are funded by the San Antonio River Authority in conjunction with the Texas Department of Water Resources and the U.S. Geological Survey.</p>\n<p>The operation and maintenance and collection of water-quality data at station 08178720, Lorence Creek at Thousand Oaks Blvd., San Antonio, station 08178640, West Elm Creek at San Antonio, and station 08178645, East Eln Creek at San Antonio, are funded by the Edwards Underground Water District in cooperation with the Texas Department of Water Resources and the U.S. Geological Survey. Station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio will provide hydrologic data on similar and adjacent watersheds. The West Elm watershed is still predominately rural but is undergoing extensive urbanization in some areas. The East Elm watershed is relatively stable and undeveloped.</p>\n<p>The objectives of the San Antonio urban hydrology study are:</p>\n<ol>\n<li>To provide data showing the effects of various stages of urbanization on flood discharge and runoff.</li>\n<li>To provide water-quality data on surface-water runoff from floods of various magnitudes, during all seasons of the year from areas with different types of urban development.</li>\n</ol>\n<p>Annual publication of the San Antonio urban studies was initiated in 1969.</p>\n<p>A defination of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in the U.S. Geological Survey's 1979 and 1980 \"Water resources data for Texas\" reports.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82158","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1982, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1979-80: U.S. Geological Survey Open-File Report 82-158, 125 p., https://doi.org/10.3133/ofr82158.","productDescription":"125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0158/report.pdf","text":"Report","size":"2.41 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":144072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0158/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607eb9","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161727,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40934,"text":"ofr82565 - 1982 - Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:51:53.126062","indexId":"ofr82565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-565","title":"Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of water in the Upper Cretaceous Eagle Sandstone and equivalent units (Virgelle Sandstone and Telegraph Creek Formation) is shown on a base map at a scale of 1:1,000,000. The map is one of a series of maps produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great plains of Montana. The contour interval is 200 feet. The map shows that the directions of regional ground-water movement is from west to east except in the extreme northwestern corner where the movement is from east to west. Water is discharged from the Eagle Sandstone to the Missouri River south of the Bearpaw Mountains. In the area north of the Bearpaw Mountains, depressurization from gas production may account for the decline in the potentiometric surface. The average discharge from 115 wells is about 23 gallons per minute and the specific capacity of 85 wells averages 1.4 gallons per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82565","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-565, 1 Plate: 40.81 × 22.83 inches, https://doi.org/10.3133/ofr82565.","productDescription":"1 Plate: 40.81 × 22.83 inches","costCenters":[],"links":[{"id":78824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407484,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75643.htm","linkFileType":{"id":5,"text":"html"}},{"id":171535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              45\n            ],\n            [\n              -104.0417,\n              45\n            ],\n            [\n              -104.0417,\n              49\n            ],\n            [\n              -112.5,\n              49\n            ],\n            [\n              -112.5,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b88","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4156,"text":"cir855 - 1982 - The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","interactions":[],"lastModifiedDate":"2021-11-18T20:54:59.200928","indexId":"cir855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"855","title":"The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska","docAbstract":"The Ketchikan and Prince Rupert 1-degree by 2-degree quadrangles, which encompass about 16,000 km2 at the south tip of southeastern Alaska, have been investigated by integrated field and laboratory studies in the disciplines of geology, geochemistry, geophysics, and Landsat data interpretation to determine their mineral-resource potential. Mineral deposits in the study area have been mined or prospected intermittently since about 1900, and production of small tonnages of ores containing gold, silver, copper, lead, zinc, and tungsten has been recorded. Extensive exploration and development currently (1981) is underway at a molybdenum prospect about 65 km east of Ketchikan. Our mineral-resource assessment indicates that the area contains potentially significant amounts of those metallic commodities, as well as of molybdenum, iron, antimony, and barite. The results of these studies have been published in a folio of maps accompanied by descriptive texts, diagrams, tables, and pertinent references. The present report serves as a guide to these investigations, provides relevant background information, and integrates the component maps and reports. It also describes revisions to the geology based on studies completed since the folio was published and includes a list of specific and general references on the geology and mineral deposits of the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir855","usgsCitation":"Berg, H., 1982, The Alaska Mineral Resource Assessment Program: Guide to information about the geology and mineral resources of the Ketchikan and Prince Rupert quadrangles, southeastern Alaska: U.S. Geological Survey Circular 855, iii, 24 p., https://doi.org/10.3133/cir855.","productDescription":"iii, 24 p.","costCenters":[],"links":[{"id":391884,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23951.htm"},{"id":139234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0855/report-thumb.jpg"},{"id":31265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0855/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Ketchikan and Prince Rupert quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132,\n              54.717\n            ],\n            [\n              -130,\n              54.717\n            ],\n            [\n              -130,\n              56\n            ],\n            [\n              -132,\n              56\n            ],\n            [\n              -132,\n              54.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835c1","contributors":{"authors":[{"text":"Berg, Henry C.","contributorId":73176,"corporation":false,"usgs":true,"family":"Berg","given":"Henry C.","affiliations":[],"preferred":false,"id":148308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58611,"text":"mf1240E - 1982 - Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon","interactions":[],"lastModifiedDate":"2018-11-05T10:16:37","indexId":"mf1240E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1240","chapter":"E","title":"Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon","docAbstract":"<p>Under the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint conference Report on Senate Bill 4, 88th Congress, the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of wilderness and primitive areas. Areas officially designated as \"wilderness,\" wild,\" or \"canoe\" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. The act provided that areas under consideration for wilderness designation should be studied for suitability for incorporation into the Wilderness System. The mineral surveys constitute one aspect of the suitability studies. The act directs that the results of such surveys are to be made available to the public and be submitted to the President and the Congress. This report discusses the results of a mineral survey of the Kalmiopsis Wilderness, Siskiyou National Forest, Josephine and Curry Counties, Oregon. The area was established as a wilderness by Public Law 88-577, September 1964.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1240E","usgsCitation":"Page, N.J., Miller, M.S., Grimes, D.J., Leinz, R.W., Blakely, R.J., Lipin, B.R., Foose, M.P., and Gray, F., 1982, Mineral resource potential map of the Kalmiopsis Wilderness, southwestern Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1240, Report: 7 p.; Plate: 37.46 x 45.21 inches, https://doi.org/10.3133/mf1240E.","productDescription":"Report: 7 p.; Plate: 37.46 x 45.21 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":183623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1240E.jpg"},{"id":310115,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1240-E/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310116,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1240-E/plate-1.pdf","text":"Plate 1"}],"scale":"62","country":"United States","state":"Oregon","otherGeospatial":"Kalmiopsis Wilderness","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.25,42 ], [ -124.25,42.5 ], [ -123.75,42.5 ], [ -123.75,42 ], [ -124.25,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade15","contributors":{"authors":[{"text":"Page, Norman J.","contributorId":46492,"corporation":false,"usgs":true,"family":"Page","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":260053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Michael S.","contributorId":52588,"corporation":false,"usgs":true,"family":"Miller","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":260056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576285,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":576286,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":576287,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lipin, Bruce R. blipin@usgs.gov","contributorId":5723,"corporation":false,"usgs":true,"family":"Lipin","given":"Bruce","email":"blipin@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":576288,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":576289,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":576290,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
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