{"pageNumber":"381","pageRowStart":"9500","pageSize":"25","recordCount":11004,"records":[{"id":70009981,"text":"70009981 - 1977 - Structure and sediment distribution in the western Bering Sea","interactions":[],"lastModifiedDate":"2025-04-18T13:55:21.623452","indexId":"70009981","displayToPublicDate":"2003-04-15T00:00:00","publicationYear":"1977","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":"Structure and sediment distribution in the western Bering Sea","docAbstract":"<p><span>Eleven seismic reflection profiles across Shirshov Ridge and the adjacent deep-water sedimentary basins (Komandorsky and Aleutian Basins) are presented to illustrate the sediment distribution in the western Bering Sea. A prominent seismic reflecting horizon, Reflector P (Middle—Late Miocene in age), is observed throughout both the Aleutian and Komandorsky Basins at an approximate subbottom depth of 1 km. This reflector is also present, in places, on the flanks and along the crest of Shirshov Ridge. The thickness of sediments beneath Reflector P is significantly different within the two abyssal basins. In the Aleutian Basin, the total subbottom depth to acoustic basement (basalt?) is about 4 km, while in the Komandorsky Basin the depth is about 2 km.</span></p><p><span>Shirshov Ridge, a Cenozoic volcanic feature that separates the Aleutian and Komandorsky Basins, is an asymmetric bathymetric ridge characterized by thick sediments along its eastern flank and steep scarps on its western side. The southern portion of the ridge has more structural relief that includes several deep, sediment-filled basins along its summit.</span></p><p><span>Velocity data from sonobuoy measurements indicate that acoustic basement in the Komandorsky Basin has an average compressional wave velocity of 5.90 km/sec. This value is considerably larger than the velocities measured for acoustic basement in the northwestern Aleutian Basin (about 5.00 km/sec) and in the central Aleutian Basin (5.40–5.57 km/sec). In the northwestern Aleutian Basin, the low-velocity acoustic basement may be volcaniclastic sediments or other indurated sediments that are overlying true basaltic basement. A refracting horizon with similar velocities (4.6–5.0 km/sec) as acoustic basement dips steeply beneath the Siberian continental margin, reaching a maximum subbottom depth of about 8 km. The thick welt of sediment at the base of the Siberian margin may be the result of sediment loading or tectonic depression prior to Late Cenozoic time.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(77)90074-3","issn":"00253227","usgsCitation":"Rabinowitz, P.D., and Cooper, A., 1977, Structure and sediment distribution in the western Bering Sea: Marine Geology, v. 24, no. 4, p. 309-320, https://doi.org/10.1016/0025-3227(77)90074-3.","productDescription":"12 p.","startPage":"309","endPage":"320","costCenters":[],"links":[{"id":219662,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska","otherGeospatial":"western Bering Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -179.9,\n              56.285168320056385\n            ],\n            [\n              -179.9,\n              51.00071364602036\n            ],\n            [\n              -174.83958193767174,\n              51.00071364602036\n            ],\n            [\n              -174.83958193767174,\n              56.285168320056385\n            ],\n            [\n              -179.9,\n              56.285168320056385\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              56.28905975329704\n            ],\n            [\n              164.84405712674976,\n              56.28905975329704\n            ],\n            [\n              164.84405712674976,\n              50.95540695542479\n            ],\n            [\n              179.9,\n              50.95540695542479\n            ],\n            [\n              179.9,\n              56.28905975329704\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9c2ce4b08c986b31d2fe","contributors":{"authors":[{"text":"Rabinowitz, P. D.","contributorId":102624,"corporation":false,"usgs":true,"family":"Rabinowitz","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":357579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, A.","contributorId":47517,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","affiliations":[],"preferred":false,"id":357578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60434,"text":"mf865C - 1977 - Map showing original (pre-mining) distribution of coal in Kentucky River Area Development District and vicinity, Eastern Kentucky","interactions":[],"lastModifiedDate":"2022-08-08T22:21:58.230925","indexId":"mf865C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"865","chapter":"C","title":"Map showing original (pre-mining) distribution of coal in Kentucky River Area Development District and vicinity, Eastern Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf865C","usgsCitation":"Newell, W.L., and Rice, C.L., 1977, Map showing original (pre-mining) distribution of coal in Kentucky River Area Development District and vicinity, Eastern Kentucky: U.S. Geological Survey Miscellaneous Field Studies Map 865, 1 Plate: 43.12 × 40.44 inches, https://doi.org/10.3133/mf865C.","productDescription":"1 Plate: 43.12 × 40.44 inches","costCenters":[],"links":[{"id":180256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404959,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4053.htm","linkFileType":{"id":5,"text":"html"}},{"id":276402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0865c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Kentucky","otherGeospatial":"Kentucky River Area Development District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.9478,\n              36.8647\n            ],\n            [\n              -82.5583,\n              36.8647\n            ],\n            [\n              -82.5583,\n              37.8514\n            ],\n            [\n              -83.9478,\n              37.8514\n            ],\n            [\n              -83.9478,\n              36.8647\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b14e4b07f02db6a47a1","contributors":{"authors":[{"text":"Newell, Wayne L. wnewell@usgs.gov","contributorId":99114,"corporation":false,"usgs":true,"family":"Newell","given":"Wayne","email":"wnewell@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":263746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, C. L.","contributorId":60658,"corporation":false,"usgs":true,"family":"Rice","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":263745,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47280,"text":"ofr77169B - 1977 - Generalized geologic map of the eastern part of southern Alaska","interactions":[],"lastModifiedDate":"2022-04-06T21:40:06.202474","indexId":"ofr77169B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-169","chapter":"B","title":"Generalized geologic map of the eastern part of southern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77169B","usgsCitation":"Beikman, H.M., Holloway, C.D., and MacKevett, E., 1977, Generalized geologic map of the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169, 1 Plate: 58.00 × 37.00 inches, https://doi.org/10.3133/ofr77169B.","productDescription":"1 Plate: 58.00 × 37.00 inches","costCenters":[],"links":[{"id":170935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398278,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14324.htm"},{"id":99895,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0169b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153,\n              59\n            ],\n            [\n              -138,\n              59\n            ],\n            [\n              -138,\n              65\n            ],\n            [\n              -153,\n              65\n            ],\n            [\n              -153,\n              59\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee6f","contributors":{"authors":[{"text":"Beikman, Helen M.","contributorId":76290,"corporation":false,"usgs":true,"family":"Beikman","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":234971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holloway, C. D.","contributorId":78374,"corporation":false,"usgs":true,"family":"Holloway","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":234972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacKevett, E. M.","contributorId":32910,"corporation":false,"usgs":true,"family":"MacKevett","given":"E. M.","affiliations":[],"preferred":false,"id":234970,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":46520,"text":"ofr77169D - 1977 - Map showing coal fields and distribution of coal-bearing rocks in the eastern part of southern Alaska","interactions":[],"lastModifiedDate":"2024-09-24T18:37:13.734374","indexId":"ofr77169D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-169","chapter":"D","title":"Map showing coal fields and distribution of coal-bearing rocks in the eastern part of southern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77169D","usgsCitation":"Holloway, C.D., 1977, Map showing coal fields and distribution of coal-bearing rocks in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169, 1 Plate: 66.00 x 38.00 inches, https://doi.org/10.3133/ofr77169D.","productDescription":"1 Plate: 66.00 x 38.00 inches","costCenters":[],"links":[{"id":99725,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0169d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":462213,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14326.htm","linkFileType":{"id":5,"text":"html"}},{"id":172509,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135.1073670439423,\n              56.60676719906883\n            ],\n            [\n              -132.9089896971182,\n              57.246509922812095\n            ],\n            [\n              -135.4706601476653,\n              59.63239164833158\n            ],\n            [\n              -137.4913490578516,\n              59.085167883927994\n            ],\n            [\n              -140.68400439488084,\n              60.45081730015744\n            ],\n            [\n              -140.86255730634022,\n              65\n            ],\n            [\n              -153,\n              65\n            ],\n            [\n              -153,\n              58.81341104096671\n            ],\n            [\n              -146.5545073060723,\n              59.56471586005253\n            ],\n            [\n              -142.48784636046838,\n              59.42513256723976\n            ],\n            [\n              -138.37720969119894,\n              58.36479993082949\n            ],\n            [\n              -135.1073670439423,\n              56.60676719906883\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659c5f","contributors":{"authors":[{"text":"Holloway, Carleen D.","contributorId":105719,"corporation":false,"usgs":true,"family":"Holloway","given":"Carleen","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":233485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44535,"text":"wri773 - 1977 - Water resources of the Umatilla Indian Reservation, Oregon","interactions":[],"lastModifiedDate":"2019-02-14T15:14:12","indexId":"wri773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-3","title":"Water resources of the Umatilla Indian Reservation, Oregon","docAbstract":"<p>Water resources of the Umatilla Indian Reservation are poorly distributed both geographically and in time. On the reservation, only the Umatilla River and one of its principal tributaries, Meacham Creek, have significant perennial flows. Runoff of the principal streams is largely from snowmelt in the Blue Mountains and is highly variable. The principal aquifers are the Columbia River Basalt Group and the Quaternary alluvium. The basalt underlies the entire reservation to a depth of a few thousand feet, and most wells tap this source. The Quaternary alluvium is present only in the valleys of the principal streams. The alluvium averages about 12 feet (ft) in thickness in the Umatilla River valley, where it has the greatest extent; elsewhere it is generally thinner.</p><p>Surface-water outflow from the reservation averages about 600 cubic feet per second (ft<sup>3</sup>/s), and the total stream inflow is about 540 ft<sup>3</sup>/s. About 480 ft<sup>3</sup>/s of the outflow is in the Umatilla River, 106 ft<sup>3</sup>/s is in McKay Creek, and 14 ft<sup>3</sup>/s is in other streams.</p><p>Dependable streamflow, defined here as the 7-day mean low flow that will occur once every 50 years, on the average, is 30 ft<sup>3</sup>/s in Umatilla River above Meacham Creek near Gibbon, 5 ft<sup>3</sup>/s in Meacham Creek below Line Creek at the east boundary, 33 ft<sup>3</sup>/s in Umatilla River at Cayuse, and 14 ft<sup>3</sup>/s in Umatilla River at Pendleton. Monthly mean flows in Umatilla River above Meacham Creek near Gibbon in summer and fall frequently are less than the published recommended minimum flows for spawning and rearing of trout; in the reach of the Umatilla River near Pendleton the summer and fall flows generally are below those recommended minimum flows.</p><p>Wells in the Columbia River Basalt Group range in depth from a few to 1,910 ft, and their yields range from less than 1 to more than 1,200 gallons per minute (gal/min). Small yields adequate for domestic needs can generally be obtained from the basalt. The depths required for successful wells may be&nbsp;extremely variable. Evaluation of specific-capacity data from wells in the basalt in four geographic areas suggests that the basalt is more permeable beneath the south reservation and the Umatilla River valley, that the permeability decreases on the north reservation, and that it is least in the Blue Mountains.&nbsp;</p><p>Surface and ground waters generally are of good quality and suitable for most uses. Surface water is soft and generally contains less than 120 milligrams per liter (ug/L) of dissolved solids. Dissolved oxygen in streams is generally at or close to saturation levels at most stream temperatures and discharge rates. Ground water ranges from soft to very hard (28 to 280 mg/L), but it generally ranges between moderately hard to hard (61 to 180 mg/L). Dissolved solids in ground water range from 88 to 561 mg/L, but generally are between 200 and about 250 mg/L.</p><p>During 1975, an estimated 11 million gallons per day (Mgal/d) of surface and ground water was withdrawn from the reservation for all uses. About 4 Mgal/d was from surface-water sources and 60 percent, or 7 Mgal/d, was from ground-water sources. About 7.2 Mgal/d was used for irrigation, 3.6 Mgal/d for public supply, and the remainder was for domestic and industrial use. About 4 Mgal/d, or 40 percent of the total water withdrawn, was for public supply and for irrigation use outside the reservation boundaries.</p><p>Local seasonal declines of ground-water levels of 100 ft or more occur in shallow basalt wells in the Umatilla River valley between Mission and the west boundary. The declines are due chiefly to pumping from many small-capacity shallow wells in the basalt for irrigation of lawns and small acreages of pasture or hay.</p><p>Future potential problems on the reservation include regional decline of ground-water levels in the basalt aquifer and local contamination of surface and ground water from accidental spills of deleterious substances. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri773","collaboration":"Prepared in cooperation with the Confederated Tribes of the Umatilla Indian Reservation","usgsCitation":"Gonthier, J.B., and Harris, D., 1977, Water resources of the Umatilla Indian Reservation, Oregon: U.S. Geological Survey Water-Resources Investigations Report 77-3, vi, 112 p., https://doi.org/10.3133/wri773.","productDescription":"vi, 112 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":134823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0003/report-thumb.jpg"},{"id":361270,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":361269,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Oregon","otherGeospatial":"Umatilla Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.8,\n              45.25\n            ],\n            [\n              -118.25,\n              45.25\n            ],\n            [\n              -118.25,\n              45.8\n            ],\n            [\n              -118.8,\n              45.8\n            ],\n            [\n              -118.8,\n              45.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698600","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":229957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, D.D.","contributorId":59002,"corporation":false,"usgs":true,"family":"Harris","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":229956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62846,"text":"gq1444 - 1977 - Geologic map of the North Middletown quadrangle, east-central Kentucky","interactions":[],"lastModifiedDate":"2021-11-10T20:47:13.712531","indexId":"gq1444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1444","title":"Geologic map of the North Middletown quadrangle, east-central Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1444","usgsCitation":"Helfrich, C.T., 1977, Geologic map of the North Middletown quadrangle, east-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1444, Report: 1 p.; Plate, https://doi.org/10.3133/gq1444.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":107868,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10978.htm","linkFileType":{"id":5,"text":"html"},"description":"10978"},{"id":248994,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1444/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1444/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"North Middletown quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.125,38.125 ], [ -84.125,38.25 ], [ -84,38.25 ], [ -84,38.125 ], [ -84.125,38.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696166","contributors":{"authors":[{"text":"Helfrich, Charles T.","contributorId":22847,"corporation":false,"usgs":true,"family":"Helfrich","given":"Charles","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":267951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47635,"text":"wri7739 - 1977 - Estimating the magnitude and frequency of floods on natural-flow streams in Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:10:24","indexId":"wri7739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-39","title":"Estimating the magnitude and frequency of floods on natural-flow streams in Massachusetts","docAbstract":"The magnitude and frequency of floods on natural-flow streams in Massachusetts, with drainage areas between 0.25 square mile and 497 square miles, may be estimated from drainage area, main channel slope, a precipitation index, and a storage factor. Multiple-regression techniques were used to define the relationship between basin and climatic characteristics, and flood peaks for 113 gaging stations. Flood-frequency and magnitude data at the gaging stations were computed using the guidelines recommended by the U.S. Water Resources Council. It was found that flood peaks of rural, unregulated Massachusetts streams can best be defined by dividing the State into an EASTERN MASSACHUSETTS and a WESTERN MASSACHUSETTS flood-frequency region. The regression equations relate peak discharges with 0.5, 0.2, 0.1, 0.04, 0.02, 0.01, 0.005, and 0.002 exceedance probabilities to basin and climatic parameters. Standard errors of estimate ranged from 42 to 70 percent for the eastern river basins and from 32 to 68 percent for the western river basins. The defined estimating relations do not apply to streams where the flood flows are significantly affected by regulation where the usable man-made storage is over 4.5 million cubic feet per square mile, or by diversions or urbanization, or where the basin indices are outside a specified range. Also, these equations should not be used for basins in eastern Plymouth County, or Barnstable, Dukes, or Nantucket Counties where the available data are insufficient to determine the influence of high infiltration and storage capacities of drainage basins on flood flows. (Woodard-USGS)","language":"ENGLISH","doi":"10.3133/wri7739","usgsCitation":"Wandle, S.W., 1977, Estimating the magnitude and frequency of floods on natural-flow streams in Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 77-39, 26 p., 1 plate, https://doi.org/10.3133/wri7739.","productDescription":"26 p., 1 plate","costCenters":[],"links":[{"id":170028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc68a","contributors":{"authors":[{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":235933,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59512,"text":"mf863 - 1977 - Gamma aeroradioactivity map of parts of Norfolk and Eastville quadrangles, outer Coastal Plain, North Carolina and Virginia","interactions":[],"lastModifiedDate":"2022-08-17T21:41:11.835793","indexId":"mf863","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"863","title":"Gamma aeroradioactivity map of parts of Norfolk and Eastville quadrangles, outer Coastal Plain, North Carolina and Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf863","usgsCitation":"Force, E.R., and Bose, S.K., 1977, Gamma aeroradioactivity map of parts of Norfolk and Eastville quadrangles, outer Coastal Plain, North Carolina and Virginia: U.S. Geological Survey Miscellaneous Field Studies Map 863, 1 Plate: 32.94 × 26.96 inches, https://doi.org/10.3133/mf863.","productDescription":"1 Plate: 32.94 × 26.96 inches","costCenters":[],"links":[{"id":184963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0863/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405289,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4049.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Norfolk and Eastville quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77,\n              36\n            ],\n            [\n              -75.7167,\n              36\n            ],\n            [\n              -75.7167,\n              36.625\n            ],\n            [\n              -77,\n              36.625\n            ],\n            [\n              -77,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1416","contributors":{"authors":[{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":262141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bose, S. K.","contributorId":92919,"corporation":false,"usgs":true,"family":"Bose","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":262142,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56276,"text":"wdrWA762 - 1977 - Water resources data for Washington, water year 1976, Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-23T18:28:09.946631","indexId":"wdrWA762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-76-2","title":"Water resources data for Washington, water year 1976, Vol. 2 - Eastern Washington","docAbstract":"<p>Water resources data for the 1976 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of ground water. This report contains discharge records for 248 gaging stations; stage only records for 3 gaging stations; stage and contents for 44 lakes and reservoirs; water quality for 123 gaging stations, 1 partial-record station, and 7 lakes; and water levels for 108 observations wells. Also included are 172 crest-stage partial-record stations and 1 low-flow partial-record station. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA762","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data for Washington, water year 1976, Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-76-2, x, 344 p., https://doi.org/10.3133/wdrWA762.","productDescription":"x, 344 p.","costCenters":[],"links":[{"id":410999,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1976/wa-76-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174641,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1976/wa-76-2/report-thumb.jpg"}],"country":"United 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,{"id":10158,"text":"ofr77672 - 1977 - Shelled benthic fauna of the eastern Chukchi Sea","interactions":[],"lastModifiedDate":"2024-02-28T22:32:29.743817","indexId":"ofr77672","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-672","title":"Shelled benthic fauna of the eastern Chukchi Sea","docAbstract":"<p>The purposes of this study were to identify the benthic shelled infauna and epifauna of the eastern Chukchi Sea, compile species lists and distribution maps, determine recurrent groups of species (communities), and examine the environmental parameters that may control the distribution of the faunal groups. The study was partly supported by the Bureau of Land Management through an interagency agreement with the National Oceanic and Atmospheric Administration, under which a multi-year program responding to the needs of petroleum development of the Alaskan continental shelf is managed by the Outer Continental Shelf Environmental Assessment Program (OCSEAP) Office. The objective of this study is to provide an assessment of the biological patterns of the region as related to petroleum development. Future offshore oil leases proposed by the State of Alaska and the Federal Government require a biological data base from which impact statements can be derived.</p><p>Samples used in this report were collected by the U.S. Geological Survey in August 1974 from the U.S. Coast Guard Cutter Burton Island under the direction of Arthur Grantz. Sampling was conducted using van Veen grabs, gravity cores, dart cores, and bottom dredges. Only the van Veen grabs contained material useful for this study. At present 103 samples containing 90 species have been examined.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77672","usgsCitation":"Mann, D.M., 1977, Shelled benthic fauna of the eastern Chukchi Sea: U.S. Geological Survey Open-File Report 77-672, i, 112 p., https://doi.org/10.3133/ofr77672.","productDescription":"i, 112 p.","costCenters":[],"links":[{"id":426093,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411645,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14495.htm","linkFileType":{"id":5,"text":"html"}},{"id":144283,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0672/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"eastern Chukchi Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -156,\n              72.5\n            ],\n            [\n              -170,\n              72.5\n            ],\n            [\n              -170,\n              66.25\n            ],\n            [\n              -156,\n              66.25\n            ],\n            [\n              -156,\n              72.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c55","contributors":{"authors":[{"text":"Mann, Dennis M.","contributorId":50528,"corporation":false,"usgs":true,"family":"Mann","given":"Dennis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9035,"text":"ofr77492 - 1977 - Hydrologic reconnaissance of the eastern North Slope, Alaska, 1975","interactions":[],"lastModifiedDate":"2019-10-01T15:34:21","indexId":"ofr77492","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-492","title":"Hydrologic reconnaissance of the eastern North Slope, Alaska, 1975","docAbstract":"The part of the Arctic coast of Alaska between the Colville River and the Canadian boundary was visited in April, August, and November 1975. The study area is characterized by its cold climate and is largely uninhabited, but oil and gas discoveries have spurred development of parts of the area. Sensible, coordinated development requires information about water resources. The purpose of the April reconnaissance was to locate winter streamflow and describe its quantity and quality. A followup summer trip was made in August to determine the flood characteristics of selected streams by measuring channel geometry in relation to bankfull discharge and the maximum evident flood and by estimating channel roughness. In addition, one lake was sampled, the discharge of a few springs was measured, and samples of spring water were taken. Because streamflow in August was assumed to be representative of normal summer flow, water quality was examined in streams for which flood surveys had been made. Samples of aquatic invertebrate populations were taken from most sites on the April and August trips. Another reconnaissance trip from Prudhoe Bay east to Canada was made in November to measure discharge in selected streams and springs, to measure ice thickness and water depth in selected lakes, and to collect water samples for water-quality analyses. Tables of data, photographs, and maps are included. 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,{"id":9426,"text":"ofr77209 - 1977 - Floods in the Big Creek basin, Linn County, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T15:12:42","indexId":"ofr77209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-209","title":"Floods in the Big Creek basin, Linn County, Iowa","docAbstract":"<p>Flood information for the Big Creek basin in Linn County, Iowa, should be of use to those concerned with the design of bridges and other structures on the flood plains of the streams. Water-surface profiles for the flood of May 1974 are given for Big Creek and its major tributaries, East Big, Crabapple, Elbow, and Abbe Creeks. The May 1974 flood was at least a 50-year flood on East Big Creek and along certain reaches of Big and Abbe Creeks. Also included for Big Creek are a profile of the December 1971 medium-stage flow and a partial profile for the minor flood of July 1971. Profiles for the low-water condition of October 26, 1972, are shown for all reaches. Water-surface profiles for the 25- and 50-year floods are estimated in relation to the May 1974 flood.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr77209","collaboration":"Prepared in cooperation with Linn County, Iowa","usgsCitation":"Heinitz, A.J., 1977, Floods in the Big Creek basin, Linn County, Iowa: U.S. Geological Survey Open-File Report 77-209, iv, 35 p., https://doi.org/10.3133/ofr77209.","productDescription":"iv, 35 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318295,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77209.JPG"},{"id":286617,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0209/report.pdf"}],"country":"United States","state":"Iowa","county":"Linn County","otherGeospatial":"Big Creek Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.3649,42.2964],[-91.3651,42.2082],[-91.3653,42.1215],[-91.3661,42.0343],[-91.3669,41.948],[-91.3677,41.8603],[-91.4836,41.8608],[-91.5989,41.8612],[-91.716,41.862],[-91.8318,41.8617],[-91.8329,41.9485],[-91.8338,42.0366],[-91.8342,42.1242],[-91.8328,42.2087],[-91.8319,42.2987],[-91.7153,42.2971],[-91.5969,42.2959],[-91.4809,42.296],[-91.3649,42.2964]]]},\"properties\":{\"name\":\"Linn\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0e18","contributors":{"authors":[{"text":"Heinitz, Albert J.","contributorId":43355,"corporation":false,"usgs":true,"family":"Heinitz","given":"Albert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43162,"text":"ofr77169C - 1977 - Gravity map of the eastern part of southern Alaska","interactions":[],"lastModifiedDate":"2021-10-14T18:11:11.186883","indexId":"ofr77169C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-169","chapter":"C","title":"Gravity map of the eastern part of southern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77169C","usgsCitation":"Barnes, D., 1977, Gravity map of the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169, 1 Plate: 37.90 × 34.00 inches, https://doi.org/10.3133/ofr77169C.","productDescription":"1 Plate: 37.90 × 34.00 inches","costCenters":[],"links":[{"id":176388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390523,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14325.htm"},{"id":80953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0169c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153,\n              59\n            ],\n            [\n              -138,\n              59\n            ],\n            [\n              -138,\n              65\n            ],\n            [\n              -153,\n              65\n            ],\n            [\n              -153,\n              59\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2807","contributors":{"authors":[{"text":"Barnes, David F.","contributorId":72787,"corporation":false,"usgs":true,"family":"Barnes","given":"David F.","affiliations":[],"preferred":false,"id":227815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16185,"text":"ofr78124 - 1977 - Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey","interactions":[],"lastModifiedDate":"2024-05-08T18:23:11.015031","indexId":"ofr78124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"78-124","title":"Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey","docAbstract":"<p>This report contains the results of triaxial and consolidation-compression testing on selected cores taken by the Atlantic Margin Coring Project, a 60-day expedition to obtain core samples by drilling beneath the Continental Shelf and Slope of the eastern United States. The coring took place in July, August and September, 1976 aboard the D/V GLOMAR CONCEPTION, and penetrated as much as 310 meters below the sea floor at 19 sites (Figure 1) along the continental margin from Georgia to Georges Bank off New England in water depth ranging from 20 to 300 meters.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78124","usgsCitation":"Swanson, P.G., and Brown, R.E., 1977, Triaxial and consolidation testing of cores from the 1976 Atlantic Margin Coring Project of the United States Geological Survey: U.S. Geological Survey Open-File Report 78-124, iv, 144 p., https://doi.org/10.3133/ofr78124.","productDescription":"iv, 144 p.","costCenters":[],"links":[{"id":428537,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0124/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Georgia to Georges Bank","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.75683968804638,\n              41.66992961819466\n            ],\n            [\n              -81.24003722734089,\n              41.66992961819466\n            ],\n            [\n              -81.24003722734089,\n              31.17169868819218\n            ],\n            [\n              -70.75683968804638,\n              31.17169868819218\n            ],\n            [\n              -70.75683968804638,\n              41.66992961819466\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6246ce","contributors":{"authors":[{"text":"Swanson, Paul G.","contributorId":97376,"corporation":false,"usgs":true,"family":"Swanson","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":172388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Ralph E.","contributorId":15882,"corporation":false,"usgs":true,"family":"Brown","given":"Ralph","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":172387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8019,"text":"ofr77631 - 1977 - Chemical composition of Precambrian, Paleozoic, Mesozoic and Tertiary rocks from east-central Alaska","interactions":[],"lastModifiedDate":"2024-01-24T20:29:45.316054","indexId":"ofr77631","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-631","title":"Chemical composition of Precambrian, Paleozoic, Mesozoic and Tertiary rocks from east-central Alaska","docAbstract":"<p>The purpose of this report is to make available 108 analyses of a variety of igneous, sedimentary, and metamorphic rocks from east-central Alaska. The rocks were collected by the senior author, Michael Churkin, Jr., G. Donald Eberlein, Reuben J. Ross, Jr., and James Melik from 1960 to 1963.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77631","usgsCitation":"Brabb, E.E., and Hamachi, B.R., 1977, Chemical composition of Precambrian, Paleozoic, Mesozoic and Tertiary rocks from east-central Alaska: U.S. Geological Survey Open-File Report 77-631, ii, 166 p., https://doi.org/10.3133/ofr77631.","productDescription":"ii, 166 p.","costCenters":[],"links":[{"id":424900,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0631/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141577,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0631/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"east-central 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,{"id":9778,"text":"ofr77545 - 1977 - Late Pleistocene and Recent geology of the Housatonic River region in northwestern Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr77545","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-545","title":"Late Pleistocene and Recent geology of the Housatonic River region in northwestern Connecticut","docAbstract":"An investigation of Late Pleistocene and Recent surficial deposits in western Connecticut and adjacent areas was undertaken, to determine characteristics of Wisconsin glaciation and the history and chronology of deglaciation in part of the finely dissected New England Uplands. \r\n\r\nThe study area lies along the midreach of the Housatonic River in western Connecticut, and has local relief exceeding 1,200 feet. Surface morphology and internal characteristics of glacial and glaciofluvial erosional and depositional features were examined and mapped in detail in the Kent and Ellsworth, Connecticut, USGS 7? minute quadrangles, and by reconnaissance in the surrounding quadrangles. This study contributes to the expanding detailed knowledge of glaciation and geomorphology in western New England and eastern New York state. \r\n\r\nIce along the lateral east margin of the southward-waxing, Wisconsin-age, Hudson-Champlain Valley ice lobe successively overran ridges trending northeast-to-southwest. Late Wisconsin ice flow was consistently toward the southeast in the study area. Glacial erosion on the upland surfaces was weak, and several early or pre-Wisconsin meltwater channels persist, which evidence little late Wisconsin glacial or glaciofluvial modification. Deeply weathered rock has been locally preserved beneath unweathered till. \r\n\r\nTill deposits are generally thin, averaging from 10 to 15 feet in thickness, but till deposits exceeding 200 feet in thickness have been observed. Direct evidence for two or more cycles of till deposition is lacking, although multiple glaciations can be inferred from drainage derangement of the Housatonic River and from anomalies in configuration of old, upland melt-water channels which were re-occupied and eroded by melt water during subsequent deglaciations. \r\n\r\nThe orientation of ridges and the local terrain relief exerted minor control on ice flow during waxing phases of glaciation. Local relief and ridges which were oriented transverse to ice flow became the dominant control factors for ice flow during late phases of deglaciation and ultimately initiated marginal stagnation zones. \r\n\r\nLate Wisconsin deglaciation evolved in three stages. First, the active ice margin receded rapidly northwestward across, and almost transverse to, the upland ridge crests in response to factors of both backwasting and downwasting. Second, local terrain relief restricted active ice flow, initiated stagnation, diverted melt-water flow and controlled deposition of small active ice-marginal deposits on the northwest slopes of ridges. Third, melting and thinning of stagnant ice tongues in valleys with ice surfaces which were low gradient and southward-sloping caused rapid northward recession of the stagnant ice margin. \r\n\r\nSequences of related outwash deposits have been correlated with inferred ice-marginal, recessional positions. In this region, the zone of stagnant ice distal to active ice ranged from 6 to 15 miles in average width. \r\n\r\nLacustrine sediments accumulated as stagnant ice blocks melted in isolated basins and other depressions where through-flowing melt-water drainage was restricted or absent. The paucity of ice-contact and outwash deposits in the isolated basins indicates that little entrained debris was present in the stagnant ice. Prograding outwash along the Housatonic River and other major drainage routes infilled glacially overdeepened \r\nunderlying lacustrine sediments sand and gravel. rock basins and buried beneath upward-coarsening \r\n\r\nUpland bogs, which have developed postglacially, contain as much as 22 feet of organic material mixed with silt and clay. An age of 12,750 ? 230 years B.P. was determined for materials immediately above three feet of older organic-rich clay layers. This dated material correlates with the upper part of the pollen T zone reported elsewhere in Connecticut and New York.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77545","usgsCitation":"Kelley, G.C., 1977, Late Pleistocene and Recent geology of the Housatonic River region in northwestern Connecticut: U.S. Geological Survey Open-File Report 77-545, [12], 222 leaves :ill., maps, plates (fold. in envelope) ;28 cm.; (222 p., 9 sheets - PGS), https://doi.org/10.3133/ofr77545.","productDescription":"[12], 222 leaves :ill., maps, plates (fold. in envelope) ;28 cm.; (222 p., 9 sheets - PGS)","costCenters":[],"links":[{"id":142786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0545/report-thumb.jpg"},{"id":37540,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37541,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37542,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37543,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37544,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37545,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37546,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0545/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b71","contributors":{"authors":[{"text":"Kelley, George C.","contributorId":51294,"corporation":false,"usgs":true,"family":"Kelley","given":"George","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10583,"text":"ofr77264 - 1977 - January 1977 water levels, and data related to water-level changes since 1950, western Kansas","interactions":[],"lastModifiedDate":"2017-09-29T08:07:58","indexId":"ofr77264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-264","title":"January 1977 water levels, and data related to water-level changes since 1950, western Kansas","docAbstract":"<p>This report contains basic data on water-level measurements in observation wells in western Kansas. Most of the measurements were made in January 1977; a few were made in December 1976 and in February 1977. The measurements were made in mid-winter when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also contains basic hydrologic data for 1950-77 that are provided for consideration in relation to the January 1977 water-level measurements.</p><p>The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.</p><p>Wells in this report are numbered according to the Bureau of Land Management's system of land subdivision. In this system, the first set of digits of a well number indicates the township; the second set, the range east or west of the sixth prinicipal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract, the second, the 40-acre tract, and the third, the 10-acre tract. The letters are designated in a counterclockwise direction beginning in the northeast quarter of the section. Where there is more than one well in a 10-acre tract, consecutive numbers, beginning with \"2\", are added in the order in which the wells are inventoried.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77264","usgsCitation":"Pabst, M.E., 1977, January 1977 water levels, and data related to water-level changes since 1950, western Kansas: U.S. Geological Survey Open-File Report 77-264, 209 p., https://doi.org/10.3133/ofr77264.","productDescription":"209 p.","numberOfPages":"213","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346201,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0264/report-thumb.jpg"}],"country":"United States","state":"Kansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fc7","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42273,"text":"ofr77523 - 1977 - Bedrock map of Fairfax County, Virginia","interactions":[{"subject":{"id":42273,"text":"ofr77523 - 1977 - Bedrock map of Fairfax County, Virginia","indexId":"ofr77523","publicationYear":"1977","noYear":false,"title":"Bedrock map of Fairfax County, Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":41234,"text":"ofr79398 - 1979 - Preliminary geologic map of Fairfax County, Virginia","indexId":"ofr79398","publicationYear":"1979","noYear":false,"title":"Preliminary geologic map of Fairfax County, Virginia"},"id":1}],"supersededBy":{"id":41234,"text":"ofr79398 - 1979 - Preliminary geologic map of Fairfax County, Virginia","indexId":"ofr79398","publicationYear":"1979","noYear":false,"title":"Preliminary geologic map of Fairfax County, Virginia"},"lastModifiedDate":"2016-10-12T09:59:15","indexId":"ofr77523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-523","title":"Bedrock map of Fairfax County, Virginia","docAbstract":"<p>The generalized rock-type of lithologic map separates the firm consolidated bedrock that underlies most of Fairfax County into thirteen (13) major rock types; each type groups rock units with grossly similar physical characteristics. &nbsp;Although crystalline bedrock underlies the Coastal Plain deposits of Eastern Fairfax County, it was not subdivided on this map. &nbsp;The only available information is based on interpretations from a few widely scattered deep drill holes and aeromagnetic and gravity surveys. Three sedimentary and ten (10) crystalline rocks on the Explanation are arranged in order from softest, best bedded, most foliated and readily splittable - to hardest, most massive, and least readily splittable.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77523","usgsCitation":"Drake, A.A., and Froelich, A., 1977, Bedrock map of Fairfax County, Virginia: U.S. Geological Survey Open-File Report 77-523, 46.46 x 56.34 inches, https://doi.org/10.3133/ofr77523.","productDescription":"46.46 x 56.34 inches","costCenters":[],"links":[{"id":172743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77523.PNG"},{"id":329402,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0523/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Virginia","county":"Fairfax 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Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":650633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":650634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","interactions":[{"subject":{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","indexId":"ofr77565","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region"},"predicate":"SUPERSEDED_BY","object":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"id":1}],"supersededBy":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"lastModifiedDate":"2016-01-15T16:15:22","indexId":"ofr77565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-565","title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","docAbstract":"<p>A broad-perspective analysis of the ground-water resources and present and possible future water development and management in the Souris-Red-Rainy Region is presented. The region includes the basins of the Souris River within Montana and North Dakota; the Red River of the North in South Dakota, North Dakota, and Minnesota; and the Rainy River within Minnesota. The region includes 59,645 square miles, mostly in North Dakota and Minnesota.</p>\n<p>The terrain is relatively flat, but ranges in altitude from 2,541 to 750 feet. Annual average precipitation ranges from 14 inches in the west to 28 inches in the east and about 75 percent of it is rain. The mean annual snow fall ranges from 32 inches in the west to 64 inches in the east. Temperatures range from -55&deg; to 118&deg;F (-48.3&deg; to 47.8&deg;C). Irrigation is needed at least part of the time to assure crop production, particularly in the western part of the region.</p>\n<p>Sand and gravel deposits in the drift form the most important fresh-water aquifers. Other aquifers are found in at least parts of the region in the Precambrian, Paleozoic, Cretaceous, and Tertiary rocks. The potentiometric surface in the bedrock generally decreases in altitude toward the Red River of the North, indicating that the general direction of ground-water movement is toward the river. Ground-water with less than 3,000 milligrams per liter dissolved solids is available throughout the region.</p>\n<p>Ground water with less than 1,000 milligrams per liter occurs in most of the region east of the Red River of the North and in most of the shallow aquifers west of the river. The total volume of water available from storage having less than 3,000 milligrams per liter dissolved solids is estimated to be 5 x 10<sup>8</sup> acre-feet. In addition to the fresh and slightly saline water, the region has abundant highly mineralized water that can be considered as a resource. Yields of wells in individual bedrock aquifers are generally less than 100 gallons per minute but locally yields may be as much as 500 gallons per minute and more. Yields in drift aquifers are frequently less than 100 gallons per minute but range from 5 to 1,000 gallons per minute. In a few places outwash yields more than 1,000 gallons per minute.</p>\n<p>Ground water is the sole or a primary source of water supply in much of the region, including supplies for irrigation, domestic and livestock, municipal, and industrial needs. Reportedly, the potential irrigation development is 1,550,000 acres, as compared with 50,200 acres in 1975. Both ground- and surface-water supplies would be required to meet these demands. Rural domestic and livestock water supplies are derived almost entirely from ground-water sources. Smaller communities and towns generally rely on ground water, and the cities and industries use ground water, surface water, or both. The municipalities using surface water generally depend upon reservoir storage. Water quality rather than quantity is the greater water-supply problem for many communities in the region.</p>\n<p>Increased demands on both ground-water and surface-water supplies likely will be made in the future. Storage of surface water in the ground-water reservoirs during times of surplus for withdrawal during times of scarcity would aid in meeting these demands. The surplus (flood) water is of better chemical quality than underlying ground water in parts of the western half of the region. Fresh water could be stored in saline- or fresh-water aquifers, and pumped out later, as needed. Thus, the ground-water reservoirs have a definite present and potential role in water management.</p>\n<p>To understand the hydrologic system for management purposes there is a need to determine more adequately the geologic and hydrologic characteristics of existing aquifers and the location of new aquifers. Also, as pumping and other stresses on any part of the hydrologic system affect other parts of the system, monitoring programs ideally should be started and maintained to detect changes and determine effects of the stresses.</p>\n<p>Many alternatives are available for managing water in the region. Some of these are operational and others are undergoing research. Adequate hydrologic information is needed to aid in solving problems of water supply, use and pollution.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77565","usgsCitation":"Reeder, H.O., 1977, Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region: U.S. Geological Survey Open-File Report 77-565, 125 p., https://doi.org/10.3133/ofr77565.","productDescription":"125 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0565/report-thumb.jpg"},{"id":38598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0565/report.pdf","text":"Report","size":"2.98 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Minnesota, Montana, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ],\n            [\n              -95.185546875,\n              49.06666839558117\n            ],\n            [\n              -95.1416015625,\n              49.52520834197442\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -94.482421875,\n              48.864714761802794\n            ],\n            [\n              -93.69140625,\n              48.69096039092549\n            ],\n            [\n              -93.0322265625,\n              48.719961222646276\n            ],\n            [\n              -92.28515625,\n              48.516604348867475\n            ],\n            [\n              -91.845703125,\n              48.40003249610685\n            ],\n            [\n              -91.3623046875,\n              48.19538740833338\n            ],\n            [\n              -90.7470703125,\n              48.28319289548349\n            ],\n            [\n              -89.384765625,\n              48.1367666796927\n            ],\n            [\n              -90,\n              47.724544549099676\n            ],\n            [\n              -91.2744140625,\n              47.15984001304432\n            ],\n            [\n              -92.373046875,\n              46.70973594407157\n            ],\n            [\n              -94.5703125,\n              45.73685954736049\n            ],\n            [\n              -95.712890625,\n              45.398449976304086\n            ],\n            [\n              -97.0751953125,\n              45.30580259943578\n            ],\n            [\n              -98.525390625,\n              45.82879925192134\n            ],\n            [\n              -99.5361328125,\n              46.10370875598026\n            ],\n            [\n              -100.81054687499999,\n              46.89023157359399\n            ],\n            [\n              -101.953125,\n              47.07012182383309\n            ],\n            [\n              -103.3154296875,\n              47.54687159892238\n            ],\n            [\n              -104.150390625,\n              47.84265762816538\n            ],\n            [\n              -105.2490234375,\n              48.3416461723746\n            ],\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6995d7","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":161995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30633,"text":"wri77108 - 1977 - Reconnaissance of ground-water resources in the Mountain Home plateau area, southwest Idaho","interactions":[],"lastModifiedDate":"2020-11-09T13:38:47.733454","indexId":"wri77108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-108","title":"Reconnaissance of ground-water resources in the Mountain Home plateau area, southwest Idaho","docAbstract":"<p><span>The Mountain Home plateau area occupies approximately </span><span>1,220 square miles of the western Snake River Plain in </span><span>southwestern Idaho. About 40,000 acres are presently (1977) </span><span>irrigated with ground water, about 30,000 acres with surface </span><span>water. An estimated 450,000 acres are potentially irrigable, </span><span>if water is available. Development of ground-water re-</span><span>sources has caused water-level declines in several places. </span><span>Largest declines are south of Mountain Home, where water </span><span>levels dropped more than 20 feet in the last 9 years.</span></p><p><span>Ground water in the area occurs primarily under water-table conditions. Perched-water zones are present in several locations. The most productive aquifer in the eastern part of the plateau is basalt of the Bureau Formation of the Idaho Group. In the western part, the most productive aquifers are sand and gravel of the older terrace gravel lithologic unit and the Idaho Group.</span></p><p><span>Recharge to the ground-water system is water from the </span><span>Boise River drainage basin, precipitation on the plateau and </span><span>adjacent mountains, and leakage from irrigation structures. </span><span>Ground-water movement is generally south or southwest. </span><span>Natural ground-water discharge from the plateau is about </span><span>18,000 acre-feet annually. </span></p><p><span>The chemical composition of the ground water generally reflects water characteristics in the area of the source of recharge and, for the most part, is good. Deuterium and oxygen-18 isotope analyses suggest that the water at the lower end of the ground-water flow system underlying the plateau was recharged a long time ago, although climatic conditions then were similar to current conditions in the Boise River basin. </span></p><p><span>Additional large-scale ground-water development will probably result in economically prohibitive pumping lifts, which also would consume excessive amounts of energy. Therefore, large-scale new agricultural development would depend heavily on the availability of surface water. However, one or several deep test holes, in selected places, could help answer some questions about the occurrence of ground water and perhaps encourage further exploration for untapped deep artesian aquifers.</span></p><p><span>The occurrence of perched-water zones beneath lands irrigated by surface water suggests that more zones of this type could develop if water is imported into the area to irrigate additional lands, and if the efficiency of the present distribution systems remains unchanged. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri77108","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources","usgsCitation":"Young, H., 1977, Reconnaissance of ground-water resources in the Mountain Home plateau area, southwest Idaho: U.S. Geological Survey Water-Resources Investigations Report 77-108, Report: iv, 40 p.; 5 Figures, https://doi.org/10.3133/wri77108.","productDescription":"Report: iv, 40 p.; 5 Figures","costCenters":[],"links":[{"id":380232,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1977/0108/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 3"},{"id":380231,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1977/0108/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 4"},{"id":380230,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1977/0108/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":380229,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1977/0108/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 6"},{"id":380228,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1977/0108/figure-9.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 9"},{"id":159946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0108/report-thumb.jpg"},{"id":380227,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0108/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho","otherGeospatial":"Mountain Home plateau area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117,\n              42\n            ],\n            [\n              -115,\n              42\n            ],\n            [\n              -115,\n              44\n            ],\n            [\n              -117,\n              44\n            ],\n            [\n              -117,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63be41","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":203574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10352,"text":"ofr77428 - 1977 - Progress report on uranium investigations in the Zane Hills area, west-central Alaska","interactions":[],"lastModifiedDate":"2023-08-29T20:45:06.015711","indexId":"ofr77428","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-428","title":"Progress report on uranium investigations in the Zane Hills area, west-central Alaska","docAbstract":"<p>The Zane Hills pluton underlies a mountainous area of about 460 km<sup>2</sup> in west-central Alaska and is locally enriched in uranium and thorium (Miller and Ferrians, 1968; Miller, 1970; Staatz and Miller, 1976). While over 90 percent of the pluton consists of granodiorite with average contents of uranium and thorium, zones of porphyritic to gneissic monzonite along the southern and eastern margins of the pluton (fig. 1) contain as much as 100 ppm (parts per million) uranium and 269 ppm thorium (Staatz and Miller, 1976; table 1, this report). This report presents information obtained in 1976 on the relationship of the uraniferous monzonite to the granodiorite and on uranium enrichment outside the pluton as part of an on-going study of the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77428","usgsCitation":"Miller, T.P., and Elliott, R.L., 1977, Progress report on uranium investigations in the Zane Hills area, west-central Alaska: U.S. Geological Survey Open-File Report 77-428, 12 p., https://doi.org/10.3133/ofr77428.","productDescription":"12 p.","costCenters":[],"links":[{"id":420265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0428/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143550,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0428/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Zane Hills area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.67015825439097,\n              66.36915590077189\n            ],\n            [\n              -152.67015825439097,\n              65.57079937978608\n            ],\n            [\n              -150.11332818389027,\n              65.57079937978608\n            ],\n            [\n              -150.11332818389027,\n              66.36915590077189\n            ],\n            [\n              -152.67015825439097,\n              66.36915590077189\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699043","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":161239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161240,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5636,"text":"pp1028 - 1977 - Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report","interactions":[],"lastModifiedDate":"2024-11-19T14:26:59.152609","indexId":"pp1028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1028","title":"Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report","docAbstract":"<p>PART A: The seismic history of the southeastern United States is dominated by the 1886 earthquake near Charleston, S.C. An understanding of the specific source and the uniqueness of the neotectonic setting of this large earthquake is essential in order to properly assess seismic hazards in the southeastern United States. Such knowledge will also contribute to the fundamental understanding of intraplate earthquakes and will aid indirectly in deciphering the evolution of Atlantic-type continental margins. The 15 chapters in this volume report on the first stage of an ongoing multidisciplinary study of the Charleston earthquake of 1886. The Modified Mercalli intensity for the 1886 earthquake was X in the meizoseismal area, an elliptical area 35 by 50 km, the center of which was Middleton Place. Seismic activity is continuing today in the Middleton Place-Summerville area at a higher level than prior to 1886. The present seismicity is originating at depths of 1 to 8 km, mostly in the crystalline basement beneath sedimentary rocks of the Coastal Plain. The crystalline basement beneath the Charleston-Summerville area is not simply a seaward extension of crystalline rocks of the Appalachian orogen that are exposed in the Piedmont to the northwest, but has a distinctive magnetic signature that does not reflect Appalachian orogenic trends. The area underlain by this distinctive geophysical basement, the Charleston block, may represent a broad zone of Triassic and (or) Jurassic crustal extension formed during the early stages of the opening of the Atlantic Ocean. The Charleston block is characterized in part by prominent, roughly circular magnetic and gravity highs that are thought to reflect maflc or ultramafic plutons. A continuously cored borehole put down over the shallowest (about 1.5 km deep) of these magnetic anomalies on the edge of the meizoseismal area bottomed at 792 m in amygdaloidal basalt. Although the K-Ar ages of about 100 m.y. for the basalt are consistent with the Late Cretaceous (Cenomanian) age of the overlying Cape Fear Formation, this must be a minimum age as a result of chemical alteration. The interpreted magmatic composition of the basalt most closely resembles the high-Ti quartz-normative tholeiites of Late Triassic and Early Jurassic age from eastern North America; age of the basalt is probably similar. Various geophysical surveys suggest that Coastal Plain sedimentary rocks do not simply dip homoclinally to the southeast on a gently dipping basement surface but are disturbed by structures not yet clearly deciphered. The present stress regime of the Charleston-Summerville area appears to be one of NE-SW. compression rather than of extension as it presumably was in the Mesozoic. The present stress regime seems similar to that of much of the eastern United States. Comparison of several seismic source areas in eastern North America shows that epicenters are typically near the periphery of positive gravity features interpreted to represent mafic or ultramafic bodies. Earthquakes may be caused by the concentration of regional stress around the peripheries of these inhomogeneities in an otherwise more homogeneous plate. Whether the inhomogeneities are more or less rigid than the. surrounding material is uncertain. PART B: In 1889, C. E. Dutton published all his basic intensity data for the 1886 Charleston, S.C., shock but did not list what intensity values he assigned to each report, nor did he show the distribution of the locations of these data reports on his isoseismal map. The writer and two other seismologists have each independently evaluated Dutton's 1,300 intensity reports (at least two of the. three interpreters agreed on intensity values for 90 percent of the reports), and the consensus values were plotted and contoured. One map was prepared on which contours emphasized the broad regional pattern of effects (with results similar to Dutton's) ; another map was contoured to depict the more</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1028","usgsCitation":"Rankin, D., 1977, Studies related to the Charleston, South Carolina, earthquake of 1886: A preliminary report: U.S. Geological Survey Professional Paper 1028, iii, 204 p., https://doi.org/10.3133/pp1028.","productDescription":"iii, 204 p.","costCenters":[],"links":[{"id":464242,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92981.htm","text":"Biostratigraphy of the deep corehole (Clubhouse Crossroads corehole 1) near Charleston, South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":140112,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1028/report-thumb.jpg"},{"id":32134,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402866,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92975.htm","text":"Lithostratigraphy of the deep corehole (Clubhouse Crossroads corehole 1) near Charleston, South Carolina","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","city":"Charleston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.17822265625,\n              32.637061996573436\n            ],\n            [\n              -79.79095458984375,\n              32.637061996573436\n            ],\n            [\n              -79.79095458984375,\n              32.95567280997862\n            ],\n            [\n              -80.17822265625,\n              32.95567280997862\n            ],\n            [\n              -80.17822265625,\n              32.637061996573436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d3b","contributors":{"authors":[{"text":"Rankin, Douglas W. dwrankin@usgs.gov","contributorId":1770,"corporation":false,"usgs":true,"family":"Rankin","given":"Douglas W.","email":"dwrankin@usgs.gov","affiliations":[],"preferred":true,"id":151342,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8579,"text":"ofr77308 - 1977 - Municipal, industrial, and irrigation water use in Washington, 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr77308","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-308","title":"Municipal, industrial, and irrigation water use in Washington, 1975","docAbstract":"An assessment of water use in 1975 in the 39 counties and 62 Water Resources Inventory Areas of Washington, indicated that 2.49 trillion gallons of water was used for municipal, industrial, and irrigation purposes. That amount represents a 10-percent increase over a similar water-use assessment in 1965, but a slight decrease from that of 1970. Total municipal water use, which includes municipally supplied industrial water, was 283 billion gallons. Industry used 442 billion gallons, of which 121 billion gallons was from municipal systems and 321 billion gallons was for self-suppled systems. Of the 604 billion gallons of water used for municipal and industrial supplies 145 billion gallons was ground water, 444 billion gallons was fresh surface water, and 14.8 billion gallons was saline surface water. A compilation of statewide industrial use as categorized by SIC (Lumber and Wood Products), SIC 28 (Chemicals and Allied Products), and SIC 20 (Food and Kindred Products)--accounted for about 65 percent of the total water used in industrial processes , In 1975, 5.79 million acre-feet of irrigation water (1,890 billion gallons) as applied to 1.52 million acres. This water was 95 percent surface water and 5 percent ground water. About 97 percent of the irrigation water was supplied in eastern Washington, to about 94 percent of the irrigated acreage in the State. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77308","usgsCitation":"Dion, N.P., and Lum, W., 1977, Municipal, industrial, and irrigation water use in Washington, 1975: U.S. Geological Survey Open-File Report 77-308, vi, 18, [23] leaves :ill., 6 maps (col.) ;33 cm.; (24 p. - PGS), https://doi.org/10.3133/ofr77308.","productDescription":"vi, 18, [23] leaves :ill., 6 maps (col.) ;33 cm.; (24 p. - PGS)","costCenters":[],"links":[{"id":141030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698a84","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157974,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lum, W. E.","contributorId":57847,"corporation":false,"usgs":true,"family":"Lum","given":"W. E.","affiliations":[],"preferred":false,"id":157975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10478,"text":"ofr77592 - 1977 - Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","interactions":[],"lastModifiedDate":"2021-12-08T22:09:56.728257","indexId":"ofr77592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-592","title":"Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation","docAbstract":"<p>Bedrock geology of about 12 km<sup>2</sup> near the Midnite mine has been mapped at the surface, in mine exposures, and from drilling, at scales from 1:600 to 1:12,000 and is presented here at 1:12,000 to provide description of the setting of uranium deposits. Oldest rocks in the area are metapelitic and metacarbonate rocks of the Precambrian (Y) Togo Formation. The chief host for uranium deposits is graphitic and pyritic mica phyllite and muscovite schist. Ore also occurs in calc-silicate hornfels and marble at the western edge of a calcareous section about 1,150 m thick. Calcareous rocks of the Togo are probably older than the pelitic as they are interpreted to be near the axis of a broad anticline. The composition and structural position of the calcareous unit suggests correlation with less metamorphosed carbonate-bearing rocks of the Lower Wallace Formation, Belt Supergroup, about 200 km to the east. Basic sills intrusive into the Togo have been metamorphosed to amphibolite.</p><p> Unmetamorphosed rocks in the mine area are Cretaceous(?) and Eocene igneous rocks. Porphyritic quartz monzonite of Cretaceous age, part of the Loon Lake batholith, is exposed over one third of the mine area. It underlies the roof pendant of Precambrian rocks in which the Midnite mine occurs at depths of generally less than 300 m. The pluton is a two-mica granite and exhibits pegmatitic and aplitic textural features indicative of water saturation and pressure quenching. Eocene intrusive and extrusive rocks in the area provide evidence that the Eocene surface was only a short distance above the present uranium deposits. </p><p>Speculative hypotheses are presented for penesyngenetic, hydrothermal, and supergene modes of uranium emplacement. The Precambrian Stratigraphy, similar in age and pre-metamorphic lithology to that of rocks hosting large uranium deposits in Saskatchewan and Northern Territory, Australia, suggests the possibility of uranium accumulation along with diagenetic pyrite in carbonaceous muds in a marine shelf environment. This hypothesis is not favored by the author because there is no evidence for stratabound uranium such as high regional radioactivity in the Togo. A hydrothermal mode of uranium emplacement is supported by the close apparent ages of mineralization and plutonism, and by petrology of the pluton. I speculate that uranium may have become enriched in postmagmatic fluids at the top of the pluton, possibly by hydrothermal leaching of soluble uranium associated with magnetite, and diffused outward into metasedimentary wall rocks to create an aureole about 100 m thick containing about 100 ppm uranium. Chemistry of the hydrothermal process is not understood, but uranium does not appear to have been transported by an oxidizing fluid, and the fluid did not produce veining and alteration comparable to that of base-metal sulfide deposits. Uranium in the low-grade protore is believed to have been redistributed into permeable zones in the Tertiary to create ore grades. Geologic and isotopic ages of uranium mineralization, and the small volume of porphyritic quartz monzonite available for leaching, are not supportive of supergene emplacement of uranium.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77592","usgsCitation":"Nash, J.T., 1977, Geology of the Midnite uranium mine area, Washington — Maps, description, and interpretation: U.S. Geological Survey Open-File Report 77-592, Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches, https://doi.org/10.3133/ofr77592.","productDescription":"Report: ii, 39 p.; 2 Plates: 15.00 × 20.00 inches and 16.00 × 17.00 inches","costCenters":[],"links":[{"id":392655,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14485.htm"},{"id":38343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0592/report-thumb.jpg"},{"id":94974,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94973,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0592/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Washington","otherGeospatial":"Midnite uranium mine area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.118,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.933\n            ],\n            [\n              -118.0670,\n              47.962\n            ],\n            [\n              -118.118,\n              47.962\n            ],\n            [\n              -118.118,\n              47.933\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9da","contributors":{"authors":[{"text":"Nash, J. Thomas","contributorId":26306,"corporation":false,"usgs":true,"family":"Nash","given":"J.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":161468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26265,"text":"wri7742 - 1977 - Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976","interactions":[],"lastModifiedDate":"2018-11-16T09:42:19","indexId":"wri7742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-42","title":"Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976","docAbstract":"<p>The northern High Plains of Colorado is an area of about 9,500 mi<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\"> (24,600 km<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"true\">) in the eastern part of the State (index map). The boundaries of the High Plains of Colorado are the State line and the limit of the Ogallala Formation of late Tertiary age. The Ogallala Formation is an unconsolidated or partly consolidated deposit of sand, gravel, clay, and silt and is the major aquifer in the northern High Plains.</span></span></span></span><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7742","usgsCitation":"Borman, R.G., and Major, T.J., 1977, Water-level changes in the northern high plains of Colorado, 1964 to 1976 and 1972 to 1976: U.S. Geological Survey Water-Resources Investigations Report 77-42, 35.92 x 30.55 inches, https://doi.org/10.3133/wri7742.","productDescription":"35.92 x 30.55 inches","costCenters":[],"links":[{"id":157802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0042/report-thumb.jpg"},{"id":359486,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.7,\n              38.33\n            ],\n            [\n              -102.04376220703125,\n              38.33\n            ],\n            [\n              -102.04376220703125,\n              41\n            ],\n            [\n              -103.7,\n              41\n            ],\n            [\n              -103.7,\n              38.33\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e776a","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":196083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Major, Thomas J.","contributorId":32529,"corporation":false,"usgs":true,"family":"Major","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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