{"pageNumber":"360","pageRowStart":"8975","pageSize":"25","recordCount":10959,"records":[{"id":70011810,"text":"70011810 - 1982 - Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2017-09-06T10:27:51","indexId":"70011810","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts","docAbstract":"<p>Present conditions and sedimentary evolution of the shallow offshore region near Nauset Inlet on Cape Cod, Massachusetts were clarified using high-resolution seismic-reflection profiles, sidescan-sonar records, surface grab samples and current meter measurements. The study area contains three provinces: (1) a nearshore province (shallower than 18 m) with a relatively steep slope (0.6°) and a cover of medium sand; (2) a northern offshore province covered with coarse sand, gravel, and boulders, interpreted to be glacial drift; and (3) a southern offshore province with a gentle seaward-dipping slope (0.3°) and a surface sediment of coarse sand. The glacial drift exposed in the northern offshore province can be traced southward under the coarse sand province. The overlying fill is comprised of either outwash sediment derived from the Pleistocene South Channel ice lobe to the east or Holocene-aged marine sediments eroded from seacliffs to the north. Latest Holocene sediment appears to be limited to the zone shoreward of 18 m where the medium sand occurs.</p><p>Near-bottom mean flows (measured over two winter months in 10 m water depth) average 6 cm sec<sup>−1</sup><span>&nbsp;</span>to the south. Mean flows exceeded 20 cm sec<sup>−1</sup>approx. 23% of the time. Ninety percent of the flows exceeding 20 cm sec<sup>−1</sup>were directed to the south, reflecting the dominant atmospheric forcing during these winter months. Waves had an average variance of 650 cm<sup>2</sup><span>&nbsp;</span>with variance exceeding 5000 cm<sup>2</sup>, 3% of the time, indicating moderate wave activity.</p><p>Present processes are actively reshaping the nearshore province, which is characterized by many east to northeast-trending shore-oblique channels that do not extend seaward of the 18-m contour. Coarse sand in the floors of these channels suggests they may be erosional features, and the presence of megaripples oriented perpendicular to the channel axes indicates active transport in these channels. Megaripple orientation and the current and wave regime of the study area support a rip-current origin for these channels.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0025-3227(82)90071-8","issn":"00253227","usgsCitation":"Aubrey, D., Twichell, D., and Pfirman, S., 1982, Holocene sedimentation in the shallow nearshore zone off Nauset Inlet, Cape Cod, Massachusetts: Marine Geology, v. 47, no. 3-4, p. 243-259, https://doi.org/10.1016/0025-3227(82)90071-8.","productDescription":"17 p.","startPage":"243","endPage":"259","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachussetts","otherGeospatial":"Cape Cod, Nauset Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              41.693424216151314\n            ],\n            [\n              -69.9224853515625,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              42.10229818948117\n            ],\n            [\n              -70.68878173828125,\n              41.693424216151314\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a31f4e4b0c8380cd5e3b3","contributors":{"authors":[{"text":"Aubrey, D.G.","contributorId":73336,"corporation":false,"usgs":true,"family":"Aubrey","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":362010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":362011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pfirman, S.L.","contributorId":40281,"corporation":false,"usgs":true,"family":"Pfirman","given":"S.L.","affiliations":[],"preferred":false,"id":362009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011586,"text":"70011586 - 1982 - Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons","interactions":[],"lastModifiedDate":"2017-09-13T14:34:57","indexId":"70011586","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons","docAbstract":"<p><span>The distribution and morphology of submarine canyons off the eastern United States between Hudson and Baltimore Canyons have been mapped by long-range sidescan sonar. In this area canyons are numerous, and their spacing correlates with overall slope gradient; they are absent where the gradient is less than 3°, are 2 to 10 km apart where the gradient is 3° to 5°, and are 1.5 to 4 km apart where the gradient exceeds 6°. Canyons range from straight to sinuous; those having sinuous axes indent the edge of the continental shelf and appear to be older than those that head on the upper slope and have straighter axes. A difference in canyon age would suggest that canyons are initiated on the continental slope and only with greater age erode headward to indent the shelf. Shallow gullies on the middle and upper slope parts of the canyon walls suggest that submarine erosion has been a major process in a recent phase of canyon development.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<408:MDADOS>2.0.CO;2","issn":"00917613","usgsCitation":"Twichell, D.C., and Roberts, D.G., 1982, Morphology, distribution, and development of submarine canyons on the United States Atlantic continental slope between Hudson and Baltimore Canyons: Geology, v. 10, no. 8, p. 408-412, https://doi.org/10.1130/0091-7613(1982)10<408:MDADOS>2.0.CO;2.","productDescription":"5 p.","startPage":"408","endPage":"412","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":221597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Baltimore Canyon, Hudson Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.1357421875,\n              37.55764242679524\n            ],\n            [\n              -74.1357421875,\n              39.5633531658293\n            ],\n            [\n              -70.7794189453125,\n              39.5633531658293\n            ],\n            [\n              -70.7794189453125,\n              37.55764242679524\n            ],\n            [\n              -74.1357421875,\n              37.55764242679524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e5de4b0c8380cd709b2","contributors":{"authors":[{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":361470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, David G.","contributorId":39937,"corporation":false,"usgs":false,"family":"Roberts","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":361469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185628,"text":"70185628 - 1982 - Acid rain, air pollution, and tree growth in southeastern New York","interactions":[],"lastModifiedDate":"2020-01-26T09:55:04","indexId":"70185628","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Acid rain, air pollution, and tree growth in southeastern New York","docAbstract":"<p><span>Whether dendroecological analyses could be used to detect changes in the relationship of tree growth to climate that might have resulted from chronic exposure to components of the acid rain-air pollution complex was determined. Tree-ring indices of white pine (</span><i>Pinus strobus</i><span> L.), eastern hemlock (</span><i>Tsuga canadensis</i><span> (L.) Cart.), pitch pine (</span><i>Pinus rigida</i><span> Mill.), and chestnut oak (</span><i>Quercus prinus</i><span> L.) were regressed against orthogonally transformed values of temperature and precipitation in order to derive a response-function relationship. Results of the regression analyses for three time periods, 1901–1920, 1926–1945, and 1954–1973 suggest that the relationship of tree growth to climate has been altered. Statistical tests of the temperature and precipitation data suggest that this change was nonclimatic. Temporally, the shift in growth response appears to correspond with the suspected increase in acid rain and air pollution in the Shawangunk Mountain area of southeastern New York in the early 1950's. This change could be the result of physiological stress induced by components of the acid rain-air pollution complex, causing climatic conditions to be more limiting to tree growth.</span></p>","language":"English","publisher":"Alliance of Crop, Soil, and Environmental Science Societies ","doi":"10.2134/jeq1982.00472425001100030011x","usgsCitation":"Puckett, L., 1982, Acid rain, air pollution, and tree growth in southeastern New York: Journal of Environmental Quality, v. 11, no. 3, p. 376-381, https://doi.org/10.2134/jeq1982.00472425001100030011x.","productDescription":"6 p.","startPage":"376","endPage":"381","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338329,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.19091796875,\n              43.34116005412307\n            ],\n            [\n              -73.32275390625,\n              43.628123412124616\n            ],\n            [\n              -77.431640625,\n              42.06560675405716\n            ],\n            [\n              -75.3662109375,\n              41.95131994679697\n            ],\n            [\n              -74.99267578125,\n              41.57436130598913\n            ],\n            [\n              -73.828125,\n              40.96330795307353\n            ],\n            [\n              -73.47656249999999,\n              41.32732632036622\n            ],\n            [\n              -73.19091796875,\n              43.34116005412307\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63042e4b05ec799131127","contributors":{"authors":[{"text":"Puckett, L.J.","contributorId":27503,"corporation":false,"usgs":true,"family":"Puckett","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":686156,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169269,"text":"70169269 - 1982 - Volcanic hazard alert issued for the Long Valley-Mono Lake area of California","interactions":[],"lastModifiedDate":"2016-04-07T15:58:46","indexId":"70169269","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Volcanic hazard alert issued for the Long Valley-Mono Lake area of California","docAbstract":"<p>The ski resort of Mammoth Lakes, nestled against the east front of the Sierra Nevada just east of Yosemite National Park, knows about natural hazards. It is still being shaken by an unusual sequence of earthquakes that started in 1978 and included four earthquakes of magnitude 6 within 48 hours of each other in May 1980. An earthquake hazard watch is still in effect.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Kerr, R.A., 1982, Volcanic hazard alert issued for the Long Valley-Mono Lake area of California: Earthquake Information Bulletin (USGS), v. 14, no. 3, p. 84-93.","productDescription":"10 p.","startPage":"84","endPage":"93","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.1412353515625,\n              38.39764411353181\n            ],\n            [\n              -119.31427001953125,\n              38.25974980039479\n            ],\n            [\n              -119.014892578125,\n              37.74031329210266\n            ],\n            [\n              -118.79241943359374,\n              37.590295170521955\n            ],\n            [\n              -118.6083984375,\n              37.38761749978395\n            ],\n            [\n              -118.40240478515624,\n              37.86618078529668\n            ],\n            [\n              -119.1412353515625,\n              38.39764411353181\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be56e4b0f59b85e02f62","contributors":{"authors":[{"text":"Kerr, R. A.","contributorId":152674,"corporation":false,"usgs":false,"family":"Kerr","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":623419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70169161,"text":"70169161 - 1982 - Earthquakes, November-December 1981","interactions":[],"lastModifiedDate":"2016-03-24T16:22:31","indexId":"70169161","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes, November-December 1981","docAbstract":"<p>The last 2 months of the year were somewhat active, seismically speaking, including three major earthquakes (7.0-7.9) during the month of December. The first of the major quakes was in the Aegean Sea on December 19, and the other two were in the South Pacific in the Kermadee Islands on December 24 and 26.</p>\n<p>Earthquake fatalities were experienced in Pakistan on December 12, and consdierable damage was reported in the eastern Caucasus.</p>\n<p>In the United States, a number of earthquakes were experienced, but no significant damage occurred.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1982, Earthquakes, November-December 1981: Earthquake Information Bulletin (USGS), v. 14, no. 3, p. 115-118.","productDescription":"4 p.","startPage":"115","endPage":"118","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be36e4b0f59b85e02e00","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":623270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001580,"text":"1001580 - 1982 - Nocturnal activity and foraging of prairie raccoons (Procyon lotor) in North Dakota","interactions":[],"lastModifiedDate":"2023-02-15T16:08:23.583256","indexId":"1001580","displayToPublicDate":"1982-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Nocturnal activity and foraging of prairie raccoons (<i>Procyon lotor</i>) in North Dakota","title":"Nocturnal activity and foraging of prairie raccoons (Procyon lotor) in North Dakota","docAbstract":"<p>Nocturnal activity and foraging of 39 radio-equipped raccoons (<i>Procyon lotor</i>) in eastern North Dakota were studied from April-July in 1974-1976. Sixteen of the raccoons were collected after foraging bouts for stomach content analysis. Raccoon activity consisted of running (13%), walking (49%) and local movement in confined areas (38%). Local movement was foraging on large or locally abundant food items. Adult males traveled farther in a night, ran twice as often, and moved locally only half as often as adult females and yearlings. Differences in activity patterns between adult females and yearlings were not detected. There was no difference among age-sex groups in use of foraging habitats. All raccoons foraged extensively in farmyards and wetlands. Stomach content analysis substantiated foraging determinations obtained by radiotelemetry. Principal foods were grain, aquatic animals, rodents, birds and bird eggs.</p>","language":"English","publisher":"University of Notre Dame","doi":"10.2307/2425374","usgsCitation":"Greenwood, R.J., 1982, Nocturnal activity and foraging of prairie raccoons (Procyon lotor) in North Dakota: American Midland Naturalist, v. 107, no. 2, p. 238-243, https://doi.org/10.2307/2425374.","productDescription":"6 p.","startPage":"238","endPage":"243","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133841,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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,{"id":8672,"text":"ofr82893 - 1982 - Tilt measurements at Long Valley caldera, California, May-August 1982","interactions":[],"lastModifiedDate":"2023-03-17T20:35:01.955162","indexId":"ofr82893","displayToPublicDate":"1982-01-01T00:00:00","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":"82-893","title":"Tilt measurements at Long Valley caldera, California, May-August 1982","docAbstract":"The Mammoth Lakes area in east-central California has experienced unusual seismicity and ground deformation since 1978, highlighted by four M>6 earthquakes in May 1980 and by the discovery soon thereafter of a broad uplift within Long Valley caldera. Recurrent seismic swarms during June 1980-May 1982 raised concern over the possibility of renewed volcanic activity in the foreseeable future, prompting a USGS Notice of Potential Volcanic Hazard on 28 May 1982. As part of an intensified Long Valley monitoring effort sponsored by the USGS Volcanic Hazards Program, a network of nine tilt sites was established near Mammoth Lakes in May and July 1982. This report describes those stations and presents results from three tilt resurveys during July-August 1982.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82893","usgsCitation":"Dzurisin, D., Cashman, K.V., Johnston, D.A., and Sylvester, A.G., 1982, Tilt measurements at Long Valley caldera, California, May-August 1982: U.S. Geological Survey Open-File Report 82-893, 34 p., https://doi.org/10.3133/ofr82893.","productDescription":"34 p.","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":414351,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13850.htm","linkFileType":{"id":5,"text":"html"}},{"id":36267,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0893/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142843,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0893/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.833,\n              37.733\n            ],\n            [\n              -118.95,\n              37.733\n            ],\n            [\n              -118.95,\n              37.617\n            ],\n            [\n              -118.833,\n              37.617\n            ],\n            [\n              -118.833,\n              37.733\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b753","contributors":{"authors":[{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":158128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cashman, K. V.","contributorId":16831,"corporation":false,"usgs":true,"family":"Cashman","given":"K.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":158129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, D. A.","contributorId":18109,"corporation":false,"usgs":true,"family":"Johnston","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158130,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sylvester, Arthur G.","contributorId":23953,"corporation":false,"usgs":true,"family":"Sylvester","given":"Arthur","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158131,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10524,"text":"ofr82674 - 1982 - Sedimentology and stratigraphy of the Kanayut Conglomerate, central and western Brooks Range, Alaska: Report of 1981 field season","interactions":[],"lastModifiedDate":"2022-12-14T20:40:31.129842","indexId":"ofr82674","displayToPublicDate":"1982-01-01T00:00:00","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":"82-674","title":"Sedimentology and stratigraphy of the Kanayut Conglomerate, central and western Brooks Range, Alaska: Report of 1981 field season","docAbstract":"The Upper Devonian and Lower Mississippian(?) Kanayut Conglomerate forms a major stratigraphic unit along the crest of the Brooks Range of northern Alaska. It crops out for an east-west distance of about 900 km and a north-south distance of about 65 km. The Kanayut is wholly allochthonous and has probably been transported northward on a series of thrust plates. \r\n\r\nThe Kanayut is as thick as 2,600 m in the east-central Brooks Range. It thins and fines to the south and west. The Kanayut forms the middle part of the allochthonous sequence of the Endicott Group, an Upper Devonian and Mississippian clastic sequence underlain by platform limestones of the Baird Group and overlain by platform limestone, carbonaceous shale, and black chert of the Lisburne Group. The Kanayut overlies the marine Upper Devonian Noatak Sandstone or, where it is missing, the marine Upper Devonian Hunt Fork Shale. It is overlain by the marine Mississippian Kayak Shale. The Kanayut Conglomerate forms the fluvial part of a large, coarse-grained delta that prograded to the southwest in Late Devonian time and retreated in Early Mississippian time. \r\n\r\nFour sections of the Kanayut Conglomerate in the central Brooks Range and five in the western Brooks Range were measured in 1981. The sections from the western Brooks Range document the presence of fluvial cycles in the Kanayut as far west as the shores of the Chukchi Sea. The Kanayut in this area is generally finer grained than it is in the central and eastern Brooks Range, having a maximum clast size of 3 cm. It is probably about 300 m thick. The upper and lower contacts of the Kanayut are gradational. The lower Kanayut contains calcareous, marine-influenced sandstone within channel deposits, and the upper Kanayut contains probable marine interdistributary-bay shale sequences. The members of the Kanayut Conglomerate cannot be differentiated in this region. \r\n\r\nIn the central Brooks Range, sections of the Kanayut Conglomerate at Siavlat Mountain and Kakivilak Creek are typically organized into fining-upward fluvial cycles. The maximum clast size is about 3 cm in this area. The Kanayut in this region is 200-500 m thick and can be divided into the Ear Peak, Shainin Lake, and Stuver Members. The upper contact of the Kanayut with the Kayak Shale is very gradational at Kakivilak Creek and very abrupt at Siavlat Mountain. \r\n\r\nPaleocurrents from fluvial strata of the Kanayut indicate sediment transport toward the west and south in both the western and central Brooks Range. The maximum clast size distribution generally indicates westward fining from the Shainin Lake region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82674","usgsCitation":"Nilsen, T.H., and Moore, T., 1982, Sedimentology and stratigraphy of the Kanayut Conglomerate, central and western Brooks Range, Alaska: Report of 1981 field season: U.S. Geological Survey Open-File Report 82-674, iii, 64 p., https://doi.org/10.3133/ofr82674.","productDescription":"iii, 64 p.","costCenters":[],"links":[{"id":410492,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75645.htm","linkFileType":{"id":5,"text":"html"}},{"id":38371,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0674/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0674/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"central and western Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -142,\n              67.3333\n            ],\n            [\n              -163.5,\n              67.3333\n            ],\n            [\n              -163.5,\n              68.75\n            ],\n            [\n              -142,\n              68.75\n            ],\n            [\n              -142,\n              67.3333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d4d","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Thomas E. 0000-0002-0878-0457","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":85592,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas E.","affiliations":[],"preferred":false,"id":161539,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70188759,"text":"70188759 - 1982 - Impact of Mount St. Helens eruption on hydrology and water quality","interactions":[],"lastModifiedDate":"2018-02-15T13:08:42","indexId":"70188759","displayToPublicDate":"1981-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":295,"text":"Technical Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"N-8311538","title":"Impact of Mount St. Helens eruption on hydrology and water quality","docAbstract":"<p><span>The 1980 eruptions of Mount St. Helens in southeast Washington resulted in a pronounced effect on the surface and ground water resources of the state. In response to the volcanic activity, the U.S. Geological Survey intensified statewide surface and ground water sampling programs to determine the nature and magnitude of the volcanic-induced variations. Streams to the east of Mount St. Helens received the major ash fallout. Chemical effects were best noted in smaller streams sampled 60 to 70 miles northeast of Mount St. Helens. The chemical variations observed were pronounced but short lived. Sulfate and chloride increases in anionic composition were prevalent immediately following the eruption however, the original bicarbonate predominance was again attained within several days. Suspended iron and aluminum concentrations were similarly elevated during the period of greatest ash deposition (highest turbidity) however, the dissolved concentrations remained relatively constant. Depressions of pH were minor and short lived. Streams draining to the south, tributaries to the Columbia river, showed little observable changes in water chemistry. Streams draining to the west (Toutle river and its tributaries) were compositionally affected by the various volcanic activities. Chloride and sulfate anion percentage exceeded the bicarbonate percentage up to one month following the eruption</span><span> period. Streams and lakes sampled in the immediate vicinity of Mount St. Helens, in addition to trace metals, contained organic compounds derived from decomposing wood buried in the debris deposits. This organic material may constitute a significant source of organic compounds to surface and ground water for some time to come.</span></p>","language":"English","publisher":"U.S. Department of Energy","usgsCitation":"Bonelli, J.E., Taylor, H.E., and Klein, J., 1982, Impact of Mount St. Helens eruption on hydrology and water quality: Technical Report N-8311538, 4 p.","productDescription":"4 p.","startPage":"261","endPage":"264","costCenters":[],"links":[{"id":342794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.9425048828125,\n              45.71385093029221\n            ],\n            [\n              -121.51702880859374,\n              45.71385093029221\n            ],\n            [\n              -121.51702880859374,\n              46.69089949154197\n            ],\n            [\n              -122.9425048828125,\n              46.69089949154197\n            ],\n            [\n              -122.9425048828125,\n              45.71385093029221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd743e4b062508e3951f7","contributors":{"authors":[{"text":"Bonelli, J. E.","contributorId":35064,"corporation":false,"usgs":true,"family":"Bonelli","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":699775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":699776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, J.M.","contributorId":44550,"corporation":false,"usgs":true,"family":"Klein","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":699777,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176179,"text":"70176179 - 1981 - Assessing the risk of earthquakes in the eastern United States","interactions":[],"lastModifiedDate":"2016-08-31T11:52:18","indexId":"70176179","displayToPublicDate":"2016-03-15T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Assessing the risk of earthquakes in the eastern United States","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1981, Assessing the risk of earthquakes in the eastern United States: Earthquake Information Bulletin (USGS), v. 13, no. 5, p. 175-178.","productDescription":"4 p.","startPage":"175","endPage":"178","numberOfPages":"4","costCenters":[],"links":[{"id":328122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Central and eastern United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.55859375,\n              49.03786794532644\n            ],\n            [\n              -90.966796875,\n              49.1242192485914\n            ],\n            [\n              -86.7041015625,\n              48.10743118848039\n            ],\n            [\n              -81.5185546875,\n              45.27488643704894\n            ],\n            [\n              -81.474609375,\n              42.97250158602597\n            ],\n            [\n              -78.1787109375,\n              44.33956524809713\n            ],\n            [\n              -69.43359375,\n              47.635783590864854\n            ],\n            [\n              -67.4560546875,\n              47.517200697839414\n            ],\n            [\n              -66.796875,\n              44.77793589631623\n            ],\n            [\n              -69.3896484375,\n              41.475660200278234\n            ],\n            [\n              -75.3662109375,\n              34.95799531086792\n            ],\n            [\n              -78.79394531249999,\n              30.14512718337613\n            ],\n            [\n              -79.716796875,\n              25.20494115356912\n            ],\n            [\n              -82.0458984375,\n              24.16680208530324\n            ],\n            [\n              -85.4296875,\n              28.304380682962783\n            ],\n            [\n              -88.5498046875,\n              28.497660832963472\n            ],\n            [\n              -93.55957031249999,\n              28.57487404744697\n            ],\n            [\n              -95.8447265625,\n              27.800209937418252\n            ],\n            [\n              -96.50390625,\n              27.644606381943326\n            ],\n            [\n              -97.55859375,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c7ffafe4b0f2f0cebfc222","contributors":{"editors":[{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":647620,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":70162203,"text":"70162203 - 1981 - Shorebirds of the eastern Bering Sea","interactions":[],"lastModifiedDate":"2018-12-21T13:19:12","indexId":"70162203","displayToPublicDate":"2016-01-15T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"41","title":"Shorebirds of the eastern Bering Sea","docAbstract":"<p>Largely on the basis of work conducted in western Alaska since 1975, we present an overview of the shorebird resources of the region and discuss their relationship to the littoral and supralittoral habitats of the area. Thirty species of shorebirds occur regularly and comprise an important component of the eastern Bering Sea ecosystem. For a third of these species the region supports the main Alaska population-for several species, the main North American population. In winter and spring littoral areas are generally ice-fast and little used by shorebirds. After breeding, there is a pronounced movement of shorebirds to coastal areas throughout the region. Populations regularly swell into the millions, many relying entirely on littoral habitats while undergoing molt and premigratory fat deposition. The extensive intertidal of the Yukon Delta and lagoons of the Alaska Peninsula are used by more species, in greater numbers, and for longer periods than other areas within the region. The timing of fall migration shows considerable variation by area, species, and age. The susceptibility of the most common shorebird species to disturbances from petroleum development is discussed.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Eastern Bering Sea Shelf: Oceanography and Resources","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"U.S. Deptartment of Commerce, National Oceanic and Atmospheric Administration, Office of Marine Pollution Assessment","publisherLocation":"Seattle, WA","doi":"10.5962/bhl.title.61718","usgsCitation":"Calder, J., and Hood, D.W., 1981, Shorebirds of the eastern Bering Sea, chap. 41 <i>of</i> The Eastern Bering Sea Shelf: Oceanography and Resources, p. 719-738, https://doi.org/10.5962/bhl.title.61718.","productDescription":"20 p.","startPage":"719","endPage":"738","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":480278,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.biodiversitylibrary.org/item/125430","text":"External Repository"},{"id":314427,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Eastern Bearing Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -186.15234374999997,\n              52.32191088594773\n            ],\n            [\n              -186.15234374999997,\n              67.87554134672945\n            ],\n            [\n              -150.205078125,\n              67.87554134672945\n            ],\n            [\n              -150.205078125,\n              52.32191088594773\n            ],\n            [\n              -186.15234374999997,\n              52.32191088594773\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569a182de4b0ec051295ef9d","contributors":{"authors":[{"text":"Calder, J.A.","contributorId":152283,"corporation":false,"usgs":false,"family":"Calder","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":646081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, Donald W.","contributorId":111881,"corporation":false,"usgs":false,"family":"Hood","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":646082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038303,"text":"70038303 - 1981 - Water resources inventory of Connecticut Part 7: upper Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T14:07:44","indexId":"70038303","displayToPublicDate":"2012-04-29T10:03:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Water resources inventory of Connecticut Part 7: upper Connecticut River basin","docAbstract":"<p>The 508 square miles of the upper Connecticut River basin in north-central Connecticut include the basins of four major tributaries: the Scantic, Park, and Hockanum Rivers, and the Farmington River downstream from Tariffville. Precipitation over this area averaged 44 inches per year during 1931-60. In this period, an additional 3,800 billion gallons of water per year entered the basin in the main stem of the Connecticut River at the Massachusetts state line, about 230 billion gallons per year in the Farmington River at Tariffville, and about 10 billion gallons per year in the Seantic River at the Massachusetts state line. Some water was also imported from outside the basin by water-supply systems. About half the precipitation, 22.2 inches, was lost from the basin by evapotranspiration; the remainder flowed out of the study area in the Connecticut River at Portland.</p>\n<br/>\n<p>Variations in streamflow at 41 long-term continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean-flow and two low-flow characteristics: (1) the 7-day annual minimum flow for 2-year and (2) 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.</p>\n<br/>\n<p>Of the 30 principal lakes, ponds, and reservoirs, two have usable storage capacities of more than 1 billion gallons. The maximum safe draft rate (regulated flow) of the largest of these, Shenipsit Lake at Rockville, is 6.5 million gallons per day for the 2-year and 30-year recurrence intervals (median and lowest annual flow).</p>\n<br/>\n<p>Floods have occurred within each month of the year but in different years. The greatest known flood on the Connecticut River was in March 1936; it had a peak flow of 130,000 cubic feet per second at Hartford. Since then, major floods have been reduced by flood-control measures.</p>\n<br/>\n<p>The major aquifers underlying the basin are composed of unconsolidated materials (stratified drift and till) and bedrock. Stratified drift overlies till and bedrock in valleys and lowlands in the eastern and western parts and in most of the broad central valley. The stratified drift generally ranges in thickness from 10 feet in small valleys to more than 200 feet in the Connecticut River Valley. Bedrock underlies the entire basin and is composed of (1) interbedded sedimentary and igneous rocks and (2) crystalline rocks.</p>\n<br/>\n<p>Ground-water sources yield from several million gallons per day from large well fields to 1 gallon per minute from single wells. Yields of 100 gal/min or more are most commonly obtained from screened wells tapping stratified-drift aquifers; amounts can be calculated by use of a series of graphs in conjunction with estimates of aquifer transmissivity and thickness. Eighteen areas underlain by good aquifers are selected as the most favorable locations for large-scale development of ground water. Selection of these areas is based on estimates of aquifer characteristics and the amount of water potentially available from induced infiltration of streamflow at low-flow conditions.</p>\n<br/>\n<p>Small to moderate water supplies can generally be obtained from any of the aquifers. Wells in bedrock yield at least a few gallons per minute at most sites. The probability of obtaining an adequate yield for domestic supply is greater in sedimentary than in crystalline bedrock and is also greater in stratified-drift overburden than in till.</p>\n<br/>\n<p>Where unaffected by man's activities, the water is of the calcium magnesium bicarbonate type, is generally low to moderate in dissolved-solids concentration, and ranges from soft to hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streams become more highly mineralized during low-flow conditions, when most flow consists of more highly mineralized water discharged from aquifers. The median dissolved-solids concentration in water from 25 stream sites was 113 mg/L (milligrams per liter) during high flow, and 148 mg/L during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in some streams draining swamps and in some waters draining from sedimentary bedrock which contains iron- and manganese-bearing minerals.</p>\n<br/>\n<p>Man's activities have affected the water quality of streams in much of the area, particularly in the Hockanum and Park River basins. The degradation in quality in these streams is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of trace elements, a low dissolved-oxygen content, and abnormally high temperatures. Ground water within this area is degraded principally by induced infiltration of surface water that contains chemical wastes, by leachate from wastes stored or disposed of on the ground, and by effluents discharged from septic tanks.</p>\n<br/>\n<p>The quantity and quality of water are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. The total amount of water used in 1968 was more than 100 billion gallons. About 80 percent of this was used for industrial purposes, and 90 percent of the industrial water was obtained from surface-water sources. About 85 percent of the population was supplied with water for domestic use by 15 major public and municipal systems and 25 private associations. Analyses of water from the 13 largest systems show generally good quality.</p>","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Ryder, R.B., Thomas, M.P., and Weiss, L.A., 1981, Water resources inventory of Connecticut Part 7: upper Connecticut River basin: Connecticut Water Resources Bulletin 24, Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller.","productDescription":"Report: vii, 76 p.; 4 Plates: 37.33 x 50.45 inches and smaller","numberOfPages":"83","costCenters":[],"links":[{"id":258813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0024/report.pdf","size":"17112","linkFileType":{"id":1,"text":"pdf"}},{"id":258814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0024/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.533333 ], [ -72.833333,42.058333 ], [ -72.366667,42.058333 ], [ -72.366667,41.533333 ], [ -72.833333,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc907e4b08c986b32cc15","contributors":{"authors":[{"text":"Ryder, Robert B. rryder@usgs.gov","contributorId":68294,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":463828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463830,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463829,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221635,"text":"5221635 - 1981 - Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin","interactions":[],"lastModifiedDate":"2022-11-03T16:39:56.804404","indexId":"5221635","displayToPublicDate":"2010-06-16T12:19:18","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3111,"text":"Prairie Naturalist","active":true,"publicationSubtype":{"id":10}},"displayTitle":"<i>Eustrongylides</i> and pesticide levels in a great blue heron shot in Wisconsin","title":"Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin","docAbstract":"<p>The parasitic roundworm, <i>Eustrongylides ignotus</i> Jagersk, has been known to cause mortality and morbidity in members of the heron family in the eastern states of North America. To date no previous records exist for this nematode in Wisconsin. Even though eustrongylidiosis was first detected in the District of Columbia in 1926 by Chapin (1926), it was not until 1976 that this parasite was found in the midwest, in central Indiana (Winterfield and Kazacos 1977). The purpose of this report is to document the occurrence of this nematode even further westward in Wisconsin, and to show the debilitating effect it can have on herons.</p>","language":"English","publisher":"Great Plains Natural Science Society","usgsCitation":"Windingstad, R.M., and Swineford, D.M., 1981, Eustrongylides and pesticide levels in a great blue heron shot in Wisconsin: Prairie Naturalist, v. 13, no. 2, p. 161-162.","productDescription":"2 p.","startPage":"161","endPage":"162","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":409097,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://digitalcommons.unl.edu/tpn/"}],"country":"United States","state":"Wisconsin","county":"Oneida County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.0477,45.8953],[-89.047,45.8097],[-89.0469,45.7265],[-89.0475,45.6391],[-89.0468,45.5518],[-89.0467,45.4668],[-89.174,45.4681],[-89.3013,45.4692],[-89.4274,45.4707],[-89.4286,45.5553],[-89.5489,45.5562],[-89.6725,45.5556],[-89.7961,45.5559],[-89.9197,45.5551],[-90.0433,45.5551],[-90.0434,45.6443],[-90.0434,45.7302],[-90.0448,45.8176],[-90.0428,45.8972],[-89.9846,45.8974],[-89.9212,45.8981],[-89.8199,45.8984],[-89.797,45.898],[-89.7571,45.8985],[-89.6741,45.8987],[-89.5498,45.8988],[-89.4256,45.8987],[-89.3628,45.8987],[-89.3007,45.9014],[-89.3008,45.8606],[-89.1754,45.859],[-89.1752,45.8993],[-89.1091,45.8973],[-89.0477,45.8953]]]},\"properties\":{\"name\":\"Oneida\",\"state\":\"WI\"}}]}","volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb126","contributors":{"authors":[{"text":"Windingstad, R. M.","contributorId":71124,"corporation":false,"usgs":true,"family":"Windingstad","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":334325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swineford, D. M.","contributorId":106839,"corporation":false,"usgs":true,"family":"Swineford","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":334326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011738,"text":"70011738 - 1981 - Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska","interactions":[],"lastModifiedDate":"2025-07-10T16:29:25.653401","indexId":"70011738","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska","docAbstract":"<p><span>The Canyon Creek vertebrate-fossil locality is an extensive road cut near Fairbanks that exposes sediments that range in age from early Wisconsin to late Holocene. Tanana River gravel at the base of the section evidently formed during the Delta Glaciation of the north-central Alaska Range. Younger layers and lenses of fluvial sand are interbedded with arkosic gravel from Canyon Creek that contains tephra as well as fossil bones of an interstadial fauna about 40,000 years old. Solifluction deposits containing ventifacts, wedge casts, and rodent burrows formed during a subsequent period of periglacial activity that took place during the maximum phase of Donnelly Glaciation about 25,000–17,000 years ago. Overlying sheets of eolian sand are separated by a 9500-year-old paleosol that may correlate with a phase of early Holocene spruce expansion through central Alaska. The Pleistocene fauna from Canyon Creek consists of rodents (indicated by burrows),&nbsp;</span><i>Mammuthus primigenius</i><span>&nbsp;(woolly mammoth),&nbsp;</span><i>Equus lambei</i><span>&nbsp;(Yukon wild ass),&nbsp;</span><i>Camelops hesternus</i><span>&nbsp;(western camel),&nbsp;</span><i>Bison</i><span>&nbsp;sp. cf.&nbsp;</span><i>B. crassicornis</i><span>&nbsp;(large-horned bison),&nbsp;</span><i>Ovis</i><span>&nbsp;sp. cf.</span><i>O. dalli</i><span>&nbsp;(mountain sheep),&nbsp;</span><i>Canis</i><span>&nbsp;sp. cf.&nbsp;</span><i>C. lupus</i><span>&nbsp;(wolf),&nbsp;</span><i>Lepus</i><span>&nbsp;sp. cf.&nbsp;</span><i>L. othus</i><span>&nbsp;or&nbsp;</span><i>L. arcticus</i><span>&nbsp;(tundra hare), and&nbsp;</span><i>Rangifer</i><span>&nbsp;sp. (caribou). This assemblage suggests an open landscape in which trees and tall shrubs were either absent or confined to sheltered and moist sites.&nbsp;</span><i>Camelops</i><span>&nbsp;evidently was present in eastern Beringia during the middle Wisconsin interstadial interval but may have disappeared during the following glacial episode. The stratigraphic section at Canyon Creek appears to demonstrate that the Delta Glaciation of the north-central Alaska Range is at least in part of early Wisconsin age and was separated from the succeeding Donnelly Glaciation by an interstadial rather than interglacial episode.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(81)90043-0","issn":"00335894","usgsCitation":"Weber, F.R., Hamilton, T.D., Hopkins, D., Repenning, C., and Haas, H., 1981, Canyon Creek: A late Pleistocene vertebrate locality in interior Alaska: Quaternary Research, v. 16, no. 2, p. 167-180, https://doi.org/10.1016/0033-5894(81)90043-0.","productDescription":"14 p.","startPage":"167","endPage":"180","costCenters":[],"links":[{"id":220787,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"north-central Alaska Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -150.32186007264718,\n              65.94098893598314\n            ],\n            [\n              -150.32186007264718,\n              64.33338352969466\n            ],\n            [\n              -145.35284620275706,\n              64.33338352969466\n            ],\n            [\n              -145.35284620275706,\n              65.94098893598314\n            ],\n            [\n              -150.32186007264718,\n              65.94098893598314\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059f347e4b0c8380cd4b6eb","contributors":{"authors":[{"text":"Weber, F. R.","contributorId":105303,"corporation":false,"usgs":true,"family":"Weber","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":361847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":361844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":361846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Repenning, C.A.","contributorId":56700,"corporation":false,"usgs":true,"family":"Repenning","given":"C.A.","affiliations":[],"preferred":false,"id":361845,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haas, H.","contributorId":27192,"corporation":false,"usgs":true,"family":"Haas","given":"H.","email":"","affiliations":[],"preferred":false,"id":361843,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70011989,"text":"70011989 - 1981 - Contemporary doming of the Adirondack Mountains: Further evidence from releveling","interactions":[],"lastModifiedDate":"2025-08-28T16:33:24.753325","indexId":"70011989","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Contemporary doming of the Adirondack Mountains: Further evidence from releveling","docAbstract":"<p><span>The Adirondack Mountains constitute an anomalously large, domical uplift on the Appalachian foreland. The dome has a NNE—SSW axis about 190 km long, and an east—west dimension of about 140 km. It has a structural relief of at least 1600 m, and a local topographic relief of up to 1200 m. First-order leveling in 1955, and again in 1973 along a north—south line at the eastern margin of the Adirondack shows an uplift rate of 2.2 mm/yr at the latitude of the center of the dome and a subsidence rate of 2.8 mm/yr at the northern end of the line near the Canadian border. The net amount of arching along this releveled line is 9&nbsp;</span><i>cm</i><span>&nbsp;± 2&nbsp;</span><i>cm</i><span>&nbsp;(Isachsen, 1975). To test the idea that this arching represented an “edge effect” of contemporary doming of the Adirondacks as a whole, the National Geodetic Survey was encouraged to relevel a 1931 north—south line between Utica and Fort Covington (near the Canadian border) which crosses the center of the dome. The releveling showed that the mountain mass is undergoing contemporary domical uplift at a rate which reaches 3.7 mm/yr near the center of the dome (compare with 1 mm/yr for the Swiss Alps). Three other releveled lines in the area support this conclusion.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(81)90051-2","issn":"00401951","usgsCitation":"Isachsen, Y., 1981, Contemporary doming of the Adirondack Mountains: Further evidence from releveling: Tectonophysics, v. 71, no. 1-4, p. 95-96, https://doi.org/10.1016/0040-1951(81)90051-2.","productDescription":"2 p.","startPage":"95","endPage":"96","costCenters":[],"links":[{"id":220732,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Adirondack Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.08632613930284,\n              44.849722542694394\n            ],\n            [\n              -75.68357029846126,\n              44.12534350539521\n            ],\n            [\n              -75.11834401539436,\n              43.137593153404055\n            ],\n            [\n              -73.6455352174284,\n              43.04799214874441\n            ],\n            [\n              -73.31377725183206,\n              44.32023495222312\n            ],\n            [\n              -73.6455352174284,\n              44.89509467289085\n            ],\n            [\n              -75.08632613930284,\n              44.849722542694394\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"71","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fa4ce4b0c8380cd4da21","contributors":{"authors":[{"text":"Isachsen, Y.W.","contributorId":100528,"corporation":false,"usgs":true,"family":"Isachsen","given":"Y.W.","affiliations":[],"preferred":false,"id":362460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60612,"text":"mf1201B - 1981 - Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2014-04-25T06:45:57","indexId":"mf1201B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1201","chapter":"B","title":"Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California","docAbstract":"<p>The aeromagnetic map consists of parts of two surveys flown at an altitude of 300 m above the average ground surface. One survey (west park of the map_ centered over the Mokelumne Wilderness was flowing in a northeast-southwest direction along slight lines spaced at a horizontal interval of about 800 m (U>S> Geological Survey, 1979b). The survey to the east is part of a regional survey flown in an east-west direction along flight lines spaced at an interval of about 1,600 m (U.S. Geological Survey, 1979a). The join of the aeromagnetic contours along the border between the two surveys is generally conformable. The contour datum of the eastern regional survey, however, is about 650 nT (nanotesla) lower than the Mokelumne Wilderness survey because of difference in data reduction.</p>\n<br>\n<p>The aeromagnetic pattern reflects variations of magnetization within the underlying rocks, but the pattern is complicated by strong topographic effects. That is, magnetic anomaly maxima tend to occur over ridges and hilltops and minima over canyons and depressions. The topographic effect exists mostly because a constant ground clearance could not be maintained at normal aircraft speeds in this area of rugged topographic relief. The recorded flight altitude varied from 30 m to nearly 1,500 m above the ground with local changes that approard 1,000 m in distances of less than 5,000 m.</p>\n<br>\n<p>Four magnetic anomalies that can be related to geologic features are discusses., Magnetic highs or lows cause by topography are not discussed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1201B","usgsCitation":"Plouff, D., and McKee, E.H., 1981, Aeromagnetic map of the Mokelumne Wilderness and contiguous Rare II further planning areas, central Sierra Nevada, California: U.S. Geological Survey Miscellaneous Field Studies Map 1201, Map: 37.01 x 33.97 inches, https://doi.org/10.3133/mf1201B.","productDescription":"Map: 37.01 x 33.97 inches","costCenters":[],"links":[{"id":286554,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286553,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1201-B/plate-1.pdf"}],"scale":"62500","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.25,38.416667 ], [ -120.25,38.75 ], [ -119.75,38.75 ], [ -119.75,38.416667 ], [ -120.25,38.416667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d73","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":264079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":264078,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60711,"text":"mf1270 - 1981 - Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States","interactions":[],"lastModifiedDate":"2016-08-23T09:18:06","indexId":"mf1270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1270","title":"Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States","docAbstract":"<p>This map was prepared as part of a study of geologic hazards to resource exploration and development on the Continental Slope in the Baltimore Canyon Trough area, off southern New Jersey. &nbsp;Detailed bathymetric maps are required for enfineering studies of bottom stability and for geologic &nbsp;interpretation of the nature of the submarine topography. &nbsp;This map presents the morphology of the Continental Slope in greater detail than do other available bathymetic maps (Veatch and Smith, 1939; Uchupi, 1965, sheet 2; U.S. Coast and Geodetic Survey, 1967; Belding and Holland, 1970, sheet 1; National Ocean Survey, 1977).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1270","usgsCitation":"Robb, J.M., Kirby, J., and Hampson, J., 1981, Bathymetric map of the continental slope and uppermost continental rise between Lindenkohl Canyon and South Toms Canyon, offshore Eastern United States: U.S. Geological Survey Miscellaneous Field Studies Map 1270, 30.76 x 36.75 inches, https://doi.org/10.3133/mf1270.","productDescription":"30.76 x 36.75 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1270.PNG"},{"id":327469,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1270/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Lindenkohl Canyon, South Toms Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73,\n              38.583333333333336\n            ],\n            [\n              -73,\n              39.083333333333336\n            ],\n            [\n              -72.28333333333335,\n              39.083333333333336\n            ],\n            [\n              -72.28333333333335,\n              38.583333333333336\n            ],\n            [\n              -73,\n              38.583333333333336\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640710","contributors":{"authors":[{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirby, John R.","contributorId":91826,"corporation":false,"usgs":true,"family":"Kirby","given":"John R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":264268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampson, John C.","contributorId":173186,"corporation":false,"usgs":false,"family":"Hampson","given":"John C.","affiliations":[],"preferred":false,"id":264269,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68748,"text":"oc113 - 1981 - Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","interactions":[],"lastModifiedDate":"2019-12-26T07:46:24","indexId":"oc113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"113","title":"Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/oc113","usgsCitation":"O'Sullivan, R., 1981, Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah: U.S. Geological Survey Oil and Gas Investigation Chart 113, HTML, https://doi.org/10.3133/oc113.","productDescription":"HTML","costCenters":[],"links":[{"id":188260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104771,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5139.htm","linkFileType":{"id":5,"text":"html"},"description":"5139"}],"scale":"5000","country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.046551,41.251716],[-111.046723,40.997959],[-110.750727,40.996847],[-110.715026,40.996347],[-110.539819,40.996346],[-110.500718,40.994746],[-110.375714,40.994947],[-110.250709,40.996089],[-110.237848,40.995427],[-110.125709,40.99655],[-110.121639,40.997101],[-110.048476,40.997555],[-110.006495,40.997815],[-110.000708,40.997352],[-109.999838,40.99733],[-109.97553,40.997912],[-109.855299,40.997614],[-109.854302,40.997661],[-109.715409,40.998191],[-109.713877,40.998266],[-109.676421,40.998395],[-109.534926,40.998143],[-109.500694,40.999127],[-109.250735,41.001009],[-109.231985,41.002059],[-109.173682,41.000859],[-109.050076,41.000659],[-109.048455,40.826081],[-109.049088,40.714562],[-109.048373,40.662602],[-109.048249,40.653601],[-109.048044,40.619231],[-109.050074,40.540358],[-109.049955,40.539901],[-109.050698,40.499963],[-109.050314,40.495092],[-109.050946,40.444368],[-109.050969,40.222662],[-109.050973,40.180849],[-109.050944,40.180712],[-109.050813,40.059579],[-109.050873,40.058915],[-109.050615,39.87497],[-109.05104,39.660472],[-109.051363,39.497674],[-109.050765,39.366677],[-109.051512,39.126095],[-109.052436,38.999985],[-109.053292,38.942878],[-109.053233,38.942467],[-109.053797,38.905284],[-109.053943,38.904414],[-109.054189,38.874984],[-109.057388,38.795456],[-109.059541,38.719888],[-109.060253,38.599328],[-109.059962,38.499987],[-109.060062,38.275489],[-109.054648,38.244921],[-109.041762,38.16469],[-109.041837,38.153022],[-109.04282,37.999301],[-109.042819,37.997068],[-109.043121,37.97426],[-109.041058,37.907236],[-109.041653,37.88117],[-109.041844,37.872788],[-109.041723,37.842051],[-109.041754,37.835826],[-109.041461,37.800105],[-109.042098,37.74999],[-109.041636,37.74021],[-109.04176,37.713182],[-109.041732,37.711214],[-109.042269,37.666067],[-109.042089,37.623795],[-109.042131,37.617662],[-109.041806,37.604171],[-109.041865,37.530726],[-109.041915,37.530653],[-109.043137,37.499992],[-109.043464,37.484711],[-109.04581,37.374993],[-109.046039,37.249993],[-109.045584,37.249351],[-109.045487,37.210844],[-109.045978,37.201831],[-109.045995,37.177279],[-109.045156,37.112064],[-109.045203,37.111958],[-109.045173,37.109464],[-109.045189,37.096271],[-109.044995,37.086429],[-109.045058,37.074661],[-109.045166,37.072742],[-109.045223,36.999084],[-109.181196,36.999271],[-109.233848,36.999266],[-109.246917,36.999346],[-109.26339,36.999263],[-109.268213,36.999242],[-109.270097,36.999266],[-109.378039,36.999135],[-109.381226,36.999148],[-109.495338,36.999105],[-109.625668,36.998308],[-109.875673,36.998504],[-110.000677,36.997968],[-110.000876,36.998502],[-110.021778,36.998602],[-110.47019,36.997997],[-110.490908,37.003566],[-110.50069,37.00426],[-110.599512,37.003448],[-110.625605,37.003416],[-110.62569,37.003721],[-110.75069,37.003197],[-111.066496,37.002389],[-111.133718,37.000779],[-111.254853,37.001077],[-111.278286,37.000465],[-111.405517,37.001497],[-111.405869,37.001481],[-111.412784,37.001478],[-112.35769,37.001025],[-112.368946,37.001125],[-112.534545,37.000684],[-112.538593,37.000674],[-112.540368,37.000669],[-112.545094,37.000734],[-112.558974,37.000692],[-112.609787,37.000753],[-112.899366,37.000319],[-112.966471,37.000219],[-113.965907,36.999976],[-113.965907,37.000025],[-114.0506,37.000396],[-114.051749,37.088434],[-114.051822,37.090976],[-114.052827,37.103961],[-114.051867,37.134292],[-114.052179,37.14711],[-114.051673,37.172368],[-114.051405,37.233854],[-114.051974,37.283848],[-114.051974,37.284511],[-114.0518,37.293044],[-114.0518,37.293548],[-114.051927,37.370459],[-114.051927,37.370734],[-114.051765,37.418083],[-114.052448,37.43144],[-114.052701,37.492014],[-114.052685,37.502513],[-114.052718,37.517264],[-114.052689,37.517859],[-114.052962,37.592783],[-114.052472,37.604776],[-114.051728,37.745997],[-114.051785,37.746249],[-114.05167,37.746958],[-114.051109,37.756276],[-114.049919,37.765586],[-114.048473,37.809861],[-114.049677,37.823645],[-114.049928,37.852508],[-114.049658,37.881368],[-114.050423,37.999961],[-114.049903,38.148601],[-114.050138,38.24996],[-114.049417,38.2647],[-114.05012,38.404536],[-114.050091,38.404673],[-114.050485,38.499955],[-114.049834,38.543784],[-114.049862,38.547764],[-114.050154,38.57292],[-114.049883,38.677365],[-114.049749,38.72921],[-114.049168,38.749951],[-114.049465,38.874949],[-114.048521,38.876197],[-114.048054,38.878693],[-114.049104,39.005509],[-114.047079,39.499943],[-114.047728,39.542742],[-114.047273,39.759413],[-114.047783,39.79416],[-114.047214,39.821024],[-114.047134,39.906037],[-114.046555,39.996899],[-114.046835,40.030131],[-114.046386,40.097896],[-114.046741,40.104231],[-114.046683,40.116931],[-114.046153,40.231971],[-114.046178,40.398313],[-114.045826,40.424823],[-114.045218,40.430282],[-114.045518,40.494474],[-114.045577,40.495801],[-114.045281,40.506586],[-114.043505,40.726292]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,{"id":61501,"text":"mf1217 - 1981 - Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","interactions":[{"subject":{"id":24125,"text":"ofr80662 - 1980 - Preliminary map showing recently active breaks along the Maacama fault zone between Hopland and Laytonville, Mendocino County, California","indexId":"ofr80662","publicationYear":"1980","noYear":false,"title":"Preliminary map showing recently active breaks along the Maacama fault zone between Hopland and Laytonville, Mendocino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":61501,"text":"mf1217 - 1981 - Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","indexId":"mf1217","publicationYear":"1981","noYear":false,"title":"Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California"},"id":1}],"lastModifiedDate":"2018-12-06T15:29:01","indexId":"mf1217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1217","title":"Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","docAbstract":"<p>The southernmost 15 km of this map is a product of a study that began in 1975 as part of a study of recency of faulting in coastal California (Ziony and others, 1974; Buchanan-Banks and others, 1978; Pampeyan , 1979). In February 1975, after being shown evidence of recent faulting in the vicinity of Ukiah by E. C. Winterhalder, Principal Engineering Geologist for Harding - Lawson Associates, Pampeyan extended the study area northward to the vicinity of Willits . After the Willits earthquake of November 22, 1977 (Simon and others, 1978; Warren and others, 1979), field investigations in the epicentral area revealed a series of distressed pavements, curbs, and sidewalks all showing right-lateral offset (Harsh and others, 1978; 1981). These features traverse the city of Willits and define a line coincident with a photolineament extending southeastward from Willits. Subsequently, additional sites of distressed pavements discovered both east and north of Ukiah alone; other lineaments of the photogeologic study verified the existence of tectonic creep in the Maacama fault zone.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1217","usgsCitation":"Pampeyan, E., Harsh, P., and Coakley, J., 1981, Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1217, 3 Sheets: 58.01 x 42.00 inches or smaller, https://doi.org/10.3133/mf1217.","productDescription":"3 Sheets: 58.01 x 42.00 inches or smaller","costCenters":[],"links":[{"id":180223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1217/report-thumb.jpg"},{"id":360001,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360002,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360003,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"Mendcino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.5,38.8675 ], [ -123.5,39.75 ], [ -123,39.75 ], [ -123,38.8675 ], [ -123.5,38.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf7f","contributors":{"authors":[{"text":"Pampeyan, E. H.","contributorId":14493,"corporation":false,"usgs":true,"family":"Pampeyan","given":"E. H.","affiliations":[],"preferred":false,"id":265828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harsh, Philip W.","contributorId":18028,"corporation":false,"usgs":true,"family":"Harsh","given":"Philip W.","affiliations":[],"preferred":false,"id":265829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coakley, J.M.","contributorId":32557,"corporation":false,"usgs":true,"family":"Coakley","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":265830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61158,"text":"mf1271B - 1981 - Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia","interactions":[],"lastModifiedDate":"2016-08-23T10:09:28","indexId":"mf1271B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1271","chapter":"B","title":"Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the President and the Congress. This map presents an analysis&nbsp;of the oil and gas resources&nbsp;of the&nbsp;Cheat Mountain Further Planning Area in the Monongahela National Forest,&nbsp;Randolph County, West Virginia. The area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>Cheat Mountain Further Planning Area comprises about 7,720 acres in the&nbsp;Monongahela National Forest in east-central West Virginia, southeast of Elkins. The study area lies on a northeast-trending linear ridge bordered on the west by the Right Fork of Tygart River and on the east by Shavers Fork. It averages about 2 mi in length and 1</span>&frac12; mi in width. Altitudes on Cheat Mountain range from about 2,550 to 3,900 ft.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1271B","usgsCitation":"Weed, E.G., 1981, Oil and gas resources of the Cheat Mountain Further Planning Area (RARE II), Randolph County, West Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 1271, 32.75 x 42.23 inches, https://doi.org/10.3133/mf1271B.","productDescription":"32.75 x 42.23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1271B.PNG"},{"id":327558,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1271-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West Virginia","county":"Randolph County","otherGeospatial":"Monongahela National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80,38.25 ], [ -80,39.25 ], [ -79.25,39.25 ], [ -79.25,38.25 ], [ -80,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d74","contributors":{"authors":[{"text":"Weed, E. G.","contributorId":55267,"corporation":false,"usgs":true,"family":"Weed","given":"E.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":265093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50766,"text":"ofr811004 - 1981 - Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","interactions":[],"lastModifiedDate":"2017-12-06T14:00:43","indexId":"ofr811004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1004","title":"Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","docAbstract":"<p>The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming.&nbsp; The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State.&nbsp; This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits.&nbsp; In western Kansas, the High Plains aquifer consists principally of the Ogallala Formation of late Tertiary age and the overlying deposits of Quaternary age.&nbsp; In south-central Kansas, the aquifer consists of unconsolidated deposits principally of the Quaternary age.&nbsp; Valley alluvium of Quaternary age also is included in the deposits in both areas.&nbsp; The High Plains aquifer is delimited on the east by outcrops of Permian or Cretaceous rocks and by unsaturated deposits of Quaternary age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811004","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1981, Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980: U.S. Geological Survey Open-File Report 81-1004, 43.21 x 31.20 inches, https://doi.org/10.3133/ofr811004.","productDescription":"43.21 x 31.20 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349811,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1004/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"High Plains Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102,\n              40\n            ],\n            [\n              -102,\n              37\n            ],\n            [\n              -97,\n              37\n            ],\n            [\n              -97,\n              39\n            ],\n            [\n              -99,\n              39\n            ],\n            [\n              -99,\n              40\n            ],\n            [\n              -102,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686ac3","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46165,"text":"ofr81804 - 1981 - Maps showing ground-water conditions in the Agua Fria area, Yavapai and Maricopa Counties, Arizona","interactions":[],"lastModifiedDate":"2022-04-20T22:41:44.364897","indexId":"ofr81804","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-804","title":"Maps showing ground-water conditions in the Agua Fria area, Yavapai and Maricopa Counties, Arizona","docAbstract":"<p>The Aqua Fria area includes about 1,500 mi<sup>2&nbsp;</sup>in central Arizona. The area is bounded by the Prescott National Forest on the west, north, and east; by the Tonto National Forest on the southeast; and by the Bradshaw Mountains and Lake Pleasant on the southwest. Ground-water development has been slight, and in 1978 about 3,200 acre-ft of groundwater was withdrawn; of this, about 2,200 acres-ft was used for irrigation, 600 acre-ft for public supply, and 400 acre-ft for domestic and stock supplies. Public-supply use has increased nearly 30 percent (data in files of Arizona Corporation Commission Phoenix, Ariz.) Many small-capacity wells have been drilled in the area, and only selected areas are shown on the maps in areas of high well density.&nbsp;</p><p><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81804","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Littin, G.R., 1981, Maps showing ground-water conditions in the Agua Fria area, Yavapai and Maricopa Counties, Arizona: U.S. Geological Survey Open-File Report 81-804, 2 Plates: 33.09 x 39.38 inches and 32.60 x 39.48 inches, https://doi.org/10.3133/ofr81804.","productDescription":"2 Plates: 33.09 x 39.38 inches and 32.60 x 39.48 inches","costCenters":[],"links":[{"id":397225,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12172.htm"},{"id":172689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0804/report-thumb.jpg"},{"id":399368,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0804/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399367,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0804/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Maricopa County, Yavapai County","otherGeospatial":"Agua Fria area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.73071289062499,\n              34.06176136129718\n            ],\n            [\n              -112.203369140625,\n              34.06176136129718\n            ],\n            [\n              -112.203369140625,\n              34.72355492704221\n            ],\n            [\n              -112.73071289062499,\n              34.72355492704221\n            ],\n            [\n              -112.73071289062499,\n              34.06176136129718\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605967","contributors":{"authors":[{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":232737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46379,"text":"ofr81698 - 1981 - Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, and dissolved-solids concentrations, 1970-80","interactions":[],"lastModifiedDate":"2021-10-29T20:19:02.863423","indexId":"ofr81698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-698","title":"Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, and dissolved-solids concentrations, 1970-80","docAbstract":"A map (scale 1:125,000) shows ground-water subunits and areas and graphs of dissolved-solids concentrations, 1970-80, in the Antelope Valley-East Kern Water Agency area, California. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81698","usgsCitation":"Lamb, C.E., and Hadley, T.L., 1981, Map of the Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, and dissolved-solids concentrations, 1970-80: U.S. Geological Survey Open-File Report 81-698, 1 Plate: 38.00 × 40.00 inches, https://doi.org/10.3133/ofr81698.","productDescription":"1 Plate: 38.00 × 40.00 inches","costCenters":[],"links":[{"id":391184,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12118.htm"},{"id":20157,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0698/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley - East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.854,\n              34.383\n            ],\n            [\n              -117.626,\n              34.383\n            ],\n            [\n              -117.626,\n              35.361\n            ],\n            [\n              -118.854,\n              35.361\n            ],\n            [\n              -118.854,\n              34.383\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6582cc","contributors":{"authors":[{"text":"Lamb, Charles Edwin","contributorId":33318,"corporation":false,"usgs":true,"family":"Lamb","given":"Charles","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":233187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, Tamara L.","contributorId":108168,"corporation":false,"usgs":true,"family":"Hadley","given":"Tamara","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":233188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46430,"text":"ofr81333 - 1981 - Map of water table in Graham County, northwestern Kansas, March 1979","interactions":[],"lastModifiedDate":"2017-09-29T08:23:27","indexId":"ofr81333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-333","title":"Map of water table in Graham County, northwestern Kansas, March 1979","docAbstract":"<p>A map of the water table in Graham County, prepared in collaboration with the U.S. Bureau of Reclamation, provides current (1980) information on water levels in the unconsolidated deposits. Graham County, an area of 900 square miles in northwestern Kansas, is within the rolling, moderately to well-dissected terrain on the eastern edge of the High Plains. &nbsp;The eastward-flowing South Fork Solomon River separates the county into nearly equal parts.</p><p>The principal source of water for domestic, stock, municipal, and irrigation use if from wells in the shallow unconsolidated deposits. The aquifers occur chiefly in the Ogallala Formation of Miocene age and in deposits of Quaternary age. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81333","usgsCitation":"Spinazola, J.M., 1981, Map of water table in Graham County, northwestern Kansas, March 1979: U.S. Geological Survey Open-File Report 81-333, 23.85 x 20.34 inches., https://doi.org/10.3133/ofr81333.","productDescription":"23.85 x 20.34 inches.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":134661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0333/report-thumb.jpg"},{"id":346212,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","county":"Graham County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.6019,39.5672],[-99.6024,39.4806],[-99.6035,39.3949],[-99.6039,39.3074],[-99.6044,39.2194],[-99.6054,39.1329],[-99.7027,39.1329],[-99.7157,39.1323],[-99.8142,39.1322],[-99.8279,39.132],[-99.9251,39.1323],[-99.9388,39.1326],[-100.0355,39.1324],[-100.0521,39.1326],[-100.1488,39.1318],[-100.1642,39.1321],[-100.1638,39.2187],[-100.1635,39.3062],[-100.1637,39.3927],[-100.1639,39.4793],[-100.1635,39.5673],[-100.0788,39.5675],[-100.0507,39.5674],[-99.9642,39.5671],[-99.9373,39.5669],[-99.852,39.5665],[-99.8251,39.5668],[-99.7398,39.5672],[-99.7135,39.567],[-99.6282,39.5674],[-99.6019,39.5672]]]},\"properties\":{\"name\":\"Graham\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db6586b0","contributors":{"authors":[{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":233303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47060,"text":"ofr81870 - 1981 - Geologic map and coal sections of the Pearl School quadrangle and the easternmost part of the Bar V Ranch quadrangle, Big Horn County, Montana","interactions":[],"lastModifiedDate":"2021-09-14T19:23:20.718351","indexId":"ofr81870","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-870","title":"Geologic map and coal sections of the Pearl School quadrangle and the easternmost part of the Bar V Ranch quadrangle, Big Horn County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81870","usgsCitation":"Galyardt, G.L., and Murray, F.N., 1981, Geologic map and coal sections of the Pearl School quadrangle and the easternmost part of the Bar V Ranch quadrangle, Big Horn County, Montana: U.S. Geological Survey Open-File Report 81-870, Report: 8 p.; 3 Plates: 36.15 × 52.94 inches, https://doi.org/10.3133/ofr81870.","productDescription":"Report: 8 p.; 3 Plates: 36.15 × 52.94 inches","costCenters":[],"links":[{"id":108185,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12192.htm","linkFileType":{"id":5,"text":"html"},"description":"12192"},{"id":84037,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0870/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84036,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0870/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84035,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0870/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0870/report-thumb.jpg"},{"id":84038,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0870/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Big Horn County","otherGeospatial":"Bar V Ranch quadrangle, Pearl School quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.002,\n              45.00\n            ],\n            [\n              -106.875,\n              45.00\n            ],\n            [\n              -106.875,\n              45.125\n            ],\n            [\n              -107.002,\n              45.125\n            ],\n            [\n              -107.002,\n              45.00\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ee1","contributors":{"authors":[{"text":"Galyardt, Gary L.","contributorId":59505,"corporation":false,"usgs":true,"family":"Galyardt","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, F. N.","contributorId":30679,"corporation":false,"usgs":true,"family":"Murray","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":234574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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