{"pageNumber":"5573","pageRowStart":"139300","pageSize":"25","recordCount":184828,"records":[{"id":24794,"text":"ofr80906 - 1980 - Bibliography for topical studies of ground motion, fault mechanics, and seismic engineering (January 1977 - September 1979)","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"ofr80906","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-906","title":"Bibliography for topical studies of ground motion, fault mechanics, and seismic engineering (January 1977 - September 1979)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80906","issn":"0094-9140","usgsCitation":"Walz, K.M., 1980, Bibliography for topical studies of ground motion, fault mechanics, and seismic engineering (January 1977 - September 1979): U.S. Geological Survey Open-File Report 80-906, 56 p.  ;28 cm., https://doi.org/10.3133/ofr80906.","productDescription":"56 p.  ;28 cm.","costCenters":[],"links":[{"id":157499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6299b1","contributors":{"authors":[{"text":"Walz, Kaye M.","contributorId":81525,"corporation":false,"usgs":true,"family":"Walz","given":"Kaye","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25890,"text":"wri806 - 1980 - The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California","interactions":[],"lastModifiedDate":"2022-11-08T15:08:51.222669","indexId":"wri806","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-6","title":"The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California","docAbstract":"<p>Adequate supplies of ground water for municipal use generally are not available within a 3-mile radius of Pescadero, San Mateo County, California. The required quantity of 100 gallons per minute probably could be obtained from one or more wells in the alluvium along Pescadero Creek; however, the quality of the water probably would deteriorate with time and might not be suitable for public supply for more than 20 or 30 years. Sand and gravel beds below 60 feet in the alluvium near the junction of Honsinger and Pescadero Creeks offer the best potential for developing domestic water supplies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri806","usgsCitation":"Akers, J.P., 1980, The potential for developing ground-water supplies in the Pescadero area, San Mateo County, California: U.S. Geological Survey Water-Resources Investigations Report 80-6, iii, 8 p., https://doi.org/10.3133/wri806.","productDescription":"iii, 8 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":158544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0006/report-thumb.jpg"},{"id":365516,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Mateo County","otherGeospatial":"Pescadero area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.4254857433479,\n              37.36201737722473\n            ],\n            [\n              -122.4254857433479,\n              37.16890736555864\n            ],\n            [\n              -122.0913656434631,\n              37.16890736555864\n            ],\n            [\n              -122.0913656434631,\n              37.36201737722473\n            ],\n            [\n              -122.4254857433479,\n              37.36201737722473\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db641d5d","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25124,"text":"cir840 - 1980 - Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"cir840","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981","language":"ENGLISH","doi":"10.3133/cir840","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Catalog of selected offices of the Office of Surface Mining, Bureau of Land Management, and Geological Survey relating to coal, 1981: U.S. Geological Survey Circular 840, 41 p., https://doi.org/10.3133/cir840.","productDescription":"41 p.","costCenters":[],"links":[{"id":156886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0840/report-thumb.jpg"},{"id":54104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0840/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef372","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24780,"text":"ofr80846 - 1980 - Mineral resources of the Lost Forest Instant Wilderness Study Area, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr80846","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-846","title":"Mineral resources of the Lost Forest Instant Wilderness Study Area, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80846","issn":"0094-9140","usgsCitation":"Walker, G.W., and McHugh, E.L., 1980, Mineral resources of the Lost Forest Instant Wilderness Study Area, Oregon: U.S. Geological Survey Open-File Report 80-846, iii, 22 p.  :maps ;28 cm., https://doi.org/10.3133/ofr80846.","productDescription":"iii, 22 p.  :maps ;28 cm.","costCenters":[],"links":[{"id":156110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0846/report-thumb.jpg"},{"id":53802,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0846/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0846/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a238","contributors":{"authors":[{"text":"Walker, George Walton","contributorId":14801,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"Walton","affiliations":[],"preferred":false,"id":192554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McHugh, Edward L.","contributorId":77157,"corporation":false,"usgs":true,"family":"McHugh","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24779,"text":"ofr80989 - 1980 - Mineral resource potential of the Pine Creek (RARE II) area, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr80989","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-989","title":"Mineral resource potential of the Pine Creek (RARE II) area, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80989","issn":"0094-9140","usgsCitation":"Walker, G.W., 1980, Mineral resource potential of the Pine Creek (RARE II) area, Oregon: U.S. Geological Survey Open-File Report 80-989, i,10 p. :map ;28 cm., https://doi.org/10.3133/ofr80989.","productDescription":"i,10 p. :map ;28 cm.","costCenters":[],"links":[{"id":156381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c116","contributors":{"authors":[{"text":"Walker, George Walton","contributorId":14801,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"Walton","affiliations":[],"preferred":false,"id":192553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25681,"text":"wri8021 - 1980 - Nitrogen in ground water and surface water from sewered and unsewered areas, Nassau County, Long Island, New York","interactions":[],"lastModifiedDate":"2019-11-25T16:04:25","indexId":"wri8021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-21","title":"Nitrogen in ground water and surface water from sewered and unsewered areas, Nassau County, Long Island, New York","docAbstract":"Data on nitrogen in groundwater and surface waters in the sewered and unsewered parts of Nassau County were analyzed to evaluate the principal sources of nitrogen and to determine what factors significantly affect its concentration in the upper glacial aquifer and the underlying Magothy aquifer. Nitrate data for water samples collected during 1952-76 show that: (1) median nitrate concentration of water in the sewered part of the entire thickness of the upper glacial aquifer is not significantly different (at the 0.95 confidence limit, N = 1400) from that in the unsewered area, (2) median nitrate concentrations in the upper 3 meters of the upper glacial aquifer are significantly lower (at the 0.90 confidence limit, N = 15) in the sewered area than in the unsewered area, (3) in the sewered area, water from 8 of 10 wells in the upper glacial aquifer shows significantly decreasing nitrate concentration with time, (4) total nitrogen concentrations in streams draining the sewered area are significantly lower than in those draining the unsewered area, (5) from more than 2,000 nitrate analyses of water in the Magothy aquifer collected from 1952-76, it was found that nitrate is present at all depths but that nitrate concentrations decrease with depth, and (6) although water from most Magothy wells having long-term nitrate records shows no significant change in nitrate concentration with time, where the change is significant, nitrate is increasing. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8021","usgsCitation":"Ragone, S.E., Katz, B., Kimmel, G., and Lindner, J., 1980, Nitrogen in ground water and surface water from sewered and unsewered areas, Nassau County, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 80-21, vii, 64 p. , https://doi.org/10.3133/wri8021.","productDescription":"vii, 64 p. ","costCenters":[],"links":[{"id":156196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0021/report-thumb.jpg"},{"id":369596,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.0423583984375,\n              40.588928169693745\n            ],\n            [\n              -73.9324951171875,\n              40.52423878069866\n            ],\n            [\n              -73.39691162109375,\n              40.5930995321649\n            ],\n            [\n              -73.2403564453125,\n              40.61186744303007\n            ],\n            [\n              -72.872314453125,\n              40.70979201243495\n            ],\n            [\n              -72.257080078125,\n              40.89482963261175\n            ],\n            [\n              -71.8011474609375,\n              41.0565730874647\n            ],\n            [\n              -72.2735595703125,\n              41.168316941075766\n            ],\n            [\n              -72.66632080078125,\n              41.008920735004885\n            ],\n            [\n              -73.2073974609375,\n              40.994410999439516\n            ],\n            [\n              -73.212890625,\n              40.94048973170136\n            ],\n            [\n              -73.41064453125,\n              40.97160353279909\n            ],\n            [\n              -73.68255615234375,\n              40.91351257612758\n            ],\n            [\n              -73.79241943359375,\n              40.79925662005228\n            ],\n            [\n              -73.87138366699219,\n              40.79613778833378\n            ],\n            [\n              -73.90159606933594,\n              40.79717741518766\n            ],\n            [\n              -73.93867492675781,\n              40.7737818731648\n            ],\n            [\n              -73.96614074707031,\n              40.73529128534676\n            ],\n            [\n              -73.97420883178711,\n              40.709141393000124\n            ],\n            [\n              -73.99944305419922,\n              40.70471701226026\n            ],\n            [\n              -74.00733947753906,\n              40.692483371144434\n            ],\n            [\n              -74.02399063110352,\n              40.67686269237614\n            ],\n            [\n              -74.02090072631836,\n              40.662800951382906\n            ],\n            [\n              -74.03841018676758,\n              40.643265836603\n            ],\n            [\n              -74.04544830322264,\n              40.63089063912002\n            ],\n            [\n              -74.04356002807617,\n              40.605742384748446\n            ],\n            [\n              -74.0423583984375,\n              40.588928169693745\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697257","contributors":{"authors":[{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":194636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Katz, B. G.","contributorId":82702,"corporation":false,"usgs":true,"family":"Katz","given":"B. G.","affiliations":[],"preferred":false,"id":194637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimmel, G.E.","contributorId":23976,"corporation":false,"usgs":true,"family":"Kimmel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":194634,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindner, J.B.","contributorId":48975,"corporation":false,"usgs":true,"family":"Lindner","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":194635,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24672,"text":"ofr80754 - 1980 - Weather forecast needs from the viewpoint of hydrology","interactions":[],"lastModifiedDate":"2013-08-02T08:03:16","indexId":"ofr80754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-754","title":"Weather forecast needs from the viewpoint of hydrology","docAbstract":"Hydrologists now depend on directly observed data in their forecasting and only infrequently use meteorological forecasts. Case studies show how reliable meteorological forecasts could be beneficial in flood and drought situations. Hydrologists need meteorological forecasts that recognize spatial variability, that are unbiased, and that have a specified degree of uncertainty. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80754","issn":"0094-9140","usgsCitation":"Thomas, D., and Buchanan, T.J., 1980, Weather forecast needs from the viewpoint of hydrology: U.S. Geological Survey Open-File Report 80-754, 9 p.  ;27 cm., https://doi.org/10.3133/ofr80754.","productDescription":"9 p.  ;27 cm.","costCenters":[],"links":[{"id":157737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0754/report-thumb.jpg"},{"id":275931,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0754/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eecf1","contributors":{"authors":[{"text":"Thomas, Donald M.","contributorId":89569,"corporation":false,"usgs":true,"family":"Thomas","given":"Donald M.","affiliations":[],"preferred":false,"id":192362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan, Thomas J.","contributorId":6842,"corporation":false,"usgs":true,"family":"Buchanan","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11652,"text":"ofr801018 - 1980 - Chemical character of water in the Red River alluvial aquifer, Louisiana","interactions":[],"lastModifiedDate":"2023-03-14T22:44:57.106324","indexId":"ofr801018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1018","title":"Chemical character of water in the Red River alluvial aquifer, Louisiana","docAbstract":"<p>The Red River alluvial aquifer of Louisiana underlies approximately 2,000 square miles in the Red River Valley of Louisiana. The aquifer is Pleistocene in age and consists of clay, silt, sand, and gravel deposited by the Red River. Sand and gravel constitute the lower two-thirds of the deposit, the most productive part of the aquifer. The aquifer ranges from 40 to 150 feet in thickness and reaches its maximum thickness in Avoyelles and Catahoula Parishes. Fine sand, silt, and clay of Holocene age overlie and generally confine the aquifer. These fine-grained deposits generally do not exceed 50 feet in thickness.</p><p>The aquifer is recharged by downward seepage of rainfall in the valley, by lateral movement of water from adjacent Pleistocene and Tertiary formations, and by upward movement of water from underlying formations of Tertiary age. When large quantities of seepage occur locally within short periods of time, a temporary reduction in mineralization takes place in the upper part of the aquifer. Lateral recharge from Pleistocene and Tertiary formations generally upgrades water in the alluvial aquifer near the edge of the valley. Recharge from underlying aquifers may upgrade or downgrade the quality of water in the lower part of the alluvial aquifer.</p><p>The Red River and its major tributaries recharge the Red River alluvial aquifer in local zones near the river during high stream stages, but noticeable water-quality changes occur only following periods of prolonged high stages.</p><p>Ground water in the alluvium generally moves toward the streams and down the valley. Water levels fluctuate seasonally and are generally less than 30 feet below land surface. Annual water-level fluctuations have a maximum range of about 30 feet near the Red River, and a minimum range of only a few feet in some interstream areas.</p><p>The Red River alluvial aquifer can yield 2,000 gallons per minute or more of water to individual wells where thick beds of coarse sand and gravel occur in the southern part of the study area. Aquifer tests indicate that the transmissivity ranges from 2,000 to 27,000 feet squared per day. The hydraulic conductivity ranges from 100 to 300 feet per day. Storage coefficients range from 6.0x10<sup>-4</sup> to 1.0x10<sup>-3</sup>.</p><p>Water in the aquifer typically is of the calcium magnesium bicarbonate type. The water is hard to very hard, ranging in hardness from about 100 to 2,300 mg/L (milligrams per liter). However, hardness generally is in the 200- to 600-mg/L range. The ions that appear to be most variable in occurrence and sensitive to change with time are calcium, magnesium, iron, sulfate, and chloride. Iron concentrations range from less than 0.3 mg/L to as high as 49 mg/L but generally are 1 to 10 mg/L. In areas where rapid recharge occurs, shallow wells may have iron concentrations of less than 0.3 mg/L. Sulfate concentrations generally range from 0.5 to 50 mg/L but locally exceed 250 mg/L. The highest concentration detected was 1,900 mg/L. Chloride concentrations typically are less than 50 Mg/L. However, concentrations of chloride exceed 250 mg/L locally and are as high as 4,400 mg/L in a few areas. For this report, water with chloride concentrations greater than 250 mg/L is considered salty.</p><p>The base of freshwater in the Red River Valley generally coincides with the base of the alluvium at depths of 80 to 150 feet. However, locally, the aquifer contains salty water, and the base of freshwater occurs within the aquifer; in parts of Rapides, Caddo, and Natchitoches Parishes, the base of freshwater extends below the alluvium. The largest occurrence of salty water is in Natchitoches Parish, with other smaller bodies occurring in Red River, Caddo, and Bossier Parishes.</p><p>Water quality in the aquifer varies both areally and with depth; the quality also varies with time, depending on the quantity and chemical character of the recharge water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801018","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Whitfield, M., 1980, Chemical character of water in the Red River alluvial aquifer, Louisiana: U.S. Geological Survey Open-File Report 80-1018, Report: v, 94 p.; 21 Plates: 25.02 x 18.81 inches or smaller, https://doi.org/10.3133/ofr801018.","productDescription":"Report: v, 94 p.; 21 Plates: 25.02 x 18.81 inches or 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,{"id":42619,"text":"ofr80793 - 1980 - Preliminary map and tables describing metalliferous and selected nonmetalliferous mineral deposits in the Petersburg and eastern Port Alexander quadrangles, Alaska","interactions":[],"lastModifiedDate":"2022-07-21T21:40:46.490604","indexId":"ofr80793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-793","title":"Preliminary map and tables describing metalliferous and selected nonmetalliferous mineral deposits in the Petersburg and eastern Port Alexander quadrangles, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80793","usgsCitation":"Karl, S.M., Berg, H.C., Grybeck, D., and Abramson, B.S., 1980, Preliminary map and tables describing metalliferous and selected nonmetalliferous mineral deposits in the Petersburg and eastern Port Alexander quadrangles, Alaska: U.S. Geological Survey Open-File Report 80-793, Report: 17 p.; 4 Plates: 34.56 × 31.86 inches or smaller, https://doi.org/10.3133/ofr80793.","productDescription":"Report: 17 p.; 4 Plates: 34.56 × 31.86 inches or smaller","costCenters":[],"links":[{"id":404295,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75434.htm","linkFileType":{"id":5,"text":"html"}},{"id":80398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0793/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80397,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80396,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80395,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80394,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0793/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0793/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Petersburg and Port Alexander quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -134.5,\n              56\n            ],\n            [\n              -132,\n              56\n            ],\n            [\n              -132,\n              57\n            ],\n            [\n              -134.5,\n              57\n            ],\n            [\n              -134.5,\n              56\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d90b","contributors":{"authors":[{"text":"Karl, Susan M. 0000-0003-1559-7826 skarl@usgs.gov","orcid":"https://orcid.org/0000-0003-1559-7826","contributorId":502,"corporation":false,"usgs":true,"family":"Karl","given":"Susan","email":"skarl@usgs.gov","middleInitial":"M.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":226836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berg, H. C.","contributorId":36130,"corporation":false,"usgs":true,"family":"Berg","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":226839,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grybeck, Donald","contributorId":8066,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","affiliations":[],"preferred":false,"id":226837,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Abramson, B. S.","contributorId":29045,"corporation":false,"usgs":true,"family":"Abramson","given":"B.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":226838,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":11526,"text":"ofr801234 - 1980 - Where on Earth is all the lithium?; with a section on uranium isotope studies","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr801234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1234","title":"Where on Earth is all the lithium?; with a section on uranium isotope studies","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801234","usgsCitation":"Vine, J.D., and Dooley, J.R., 1980, Where on Earth is all the lithium?; with a section on uranium isotope studies: U.S. Geological Survey Open-File Report 80-1234, iii, 114 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801234.","productDescription":"iii, 114 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1234/report-thumb.jpg"},{"id":39389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e491e","contributors":{"authors":[{"text":"Vine, James David","contributorId":52147,"corporation":false,"usgs":true,"family":"Vine","given":"James","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":163303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dooley, J. R. Jr.","contributorId":8110,"corporation":false,"usgs":true,"family":"Dooley","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41293,"text":"ofr80424 - 1980 - Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr80424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-424","title":"Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska","docAbstract":"Preliminary bathymetry (at 1:20,000 scale) and other scientific studies of McCarty Fiord, Alaska, Conducted by the Research Vessel Growler in 1978, showed this 15 mile-long waterway to be a narrow, deeply scoured basin enclosed by a terminal-moraine shoal. This valley was formerly filled by McCarty Glacier, which began a drastic retreat shortly after 1909; the glacier reached shallow water at the head of the fiord around 1960. The relative rate of retreat in deep water and on land is disclosed by the slower melting of stagnent ice left in a side valley. Soundings and profiles show the main channel to extend to a depth as great as 957 feet and to have the typical ' U ' shape of a glacier-eroded valley; since the glacier 's retreat, sediments have formed a nearly level deposit in the deepest part of the fiord. Old forest debris dated by carbon-14 indicates that a neoglacial advance of the glacier began before 3,395 years B.P. (before present); by 1,500 B.P. the glacier filled most of the fiord, and before the glacier culminated its advance around 1860 , two glacier-dammed lakes were formed in side valleys. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80424","usgsCitation":"Post, A., 1980, Preliminary bathymetry of McCarty Fiord and Neoglacial changes of McCarty Glacier, Alaska: U.S. Geological Survey Open-File Report 80-424, 4 maps ;89 x 67 cm., https://doi.org/10.3133/ofr80424.","productDescription":"4 maps ;89 x 67 cm.","costCenters":[],"links":[{"id":171520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19998,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19999,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20000,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0424/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c836","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":224787,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24046,"text":"ofr80952 - 1980 - Hydrogeology of the Seldovia area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:10","indexId":"ofr80952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-952","title":"Hydrogeology of the Seldovia area, Alaska","docAbstract":"Surficial materials in the Seldovia area, Alaska, are mapped as glacial drift over sedimentary bedrock, glacial drift over igneous and metamorphic bedrock, valley-bottom, alluvium, alluvial fan deposits, beach and intertidal deposits, and peat. Unconsolidated materials are generally less than 10 feet thick except in well-drained glacial deposits along the Seldovia-Jakolof Bay Road and in depressions in the bedrock surface. These depressions are poorly drained and commonly contain peat bogs. Development of domestic wells (1-15 gallons per minute) may be possible from unconsolidated materials and sedimentary bedrock, but larger water requirements must be met from surface-water sources. In areas having the water table or top of bedrock at shallow depths, effluent from sewage disposal systems may cause pollution of the land surface and nearby surface water. Seepage from hillside aquifers and unstable land along the coast of Kachemak Bay may adversely affect roads and structures. (USGS)","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr80952","issn":"0094-9140","usgsCitation":"Nelson, G.L., and Danskin, W.R., 1980, Hydrogeology of the Seldovia area, Alaska (WRI/OFR): U.S. Geological Survey Open-File Report 80-952, 1 map ;63 x 35 cm., in envelope 31 x 23 cm., https://doi.org/10.3133/ofr80952.","productDescription":"1 map ;63 x 35 cm., in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":108085,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11840.htm","linkFileType":{"id":5,"text":"html"},"description":"11840"},{"id":156318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":53215,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0952/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53216,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0952/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614d21","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danskin, Wesley R. 0000-0001-8672-5501 wdanskin@usgs.gov","orcid":"https://orcid.org/0000-0001-8672-5501","contributorId":1034,"corporation":false,"usgs":true,"family":"Danskin","given":"Wesley","email":"wdanskin@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23933,"text":"ofr801195 - 1980 - Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T08:00:06","indexId":"ofr801195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1195","title":"Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","docAbstract":"This report describes the observation-well network in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough Counties, Florida. Data obtained in 1978 from the network in and adjacent to the two well fields, as well as rainfall and pumpage records, are presented. The Southwest Florida Water Management District has established regulatory water-level limits in four observation wells and water-quality limits in three observation wells. Water levels dropped below regulatory limits in the spring of 1978 in three wells. Chloride concentrations in 1978 remained above regulatory limits for the entire year in one well and exceeded the limit during the late spring in the other two deep wells, both west of Eldridge-Wilde well field. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr801195","issn":"0094-9140","usgsCitation":"Mills, L.R., 1980, Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978: U.S. Geological Survey Open-File Report 80-1195, iv, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801195.","productDescription":"iv, 27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":156575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1195/report-thumb.jpg"},{"id":275925,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1195/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606973","contributors":{"authors":[{"text":"Mills, L. R.","contributorId":26281,"corporation":false,"usgs":true,"family":"Mills","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42673,"text":"ofr801270 - 1980 - Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","interactions":[{"subject":{"id":42673,"text":"ofr801270 - 1980 - Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"ofr801270","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"i1445","publicationYear":"1983","noYear":false,"title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah"},"id":1}],"supersededBy":{"id":66445,"text":"i1445 - 1983 - Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah","indexId":"i1445","publicationYear":"1983","noYear":false,"title":"Geologic map of the northwest-quarter of the Beaver Quadrangle, Beaver County, Utah"},"lastModifiedDate":"2022-04-07T17:46:28.532055","indexId":"ofr801270","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1270","title":"Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801270","usgsCitation":"Machette, M., and Steven, T., 1980, Preliminary geologic map of the northwest quarter of the Beaver Quadrangle, Beaver County, Utah: U.S. Geological Survey Open-File Report 80-1270, 1 Plate: 42.74 x 27.50 inches, https://doi.org/10.3133/ofr801270.","productDescription":"1 Plate: 42.74 x 27.50 inches","costCenters":[],"links":[{"id":398325,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1270/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1270/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,38.3675 ], [ -112.75,38.5 ], [ -112.61749999999999,38.5 ], [ -112.61749999999999,38.3675 ], [ -112.75,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db67426e","contributors":{"authors":[{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":226916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, Thomas A.","contributorId":57529,"corporation":false,"usgs":true,"family":"Steven","given":"Thomas A.","affiliations":[],"preferred":false,"id":226917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23957,"text":"ofr80581 - 1980 - Ground-water models for water resources planning","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr80581","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-581","title":"Ground-water models for water resources planning","docAbstract":"In the past decade hydrologists have emphasized the development of computer-based mathematical models to aid in the understanding of flow, the transport of solutes, transport of heat, and deformation in the groundwater system. These models have been used to provide information and predictions for water managers. Too frequently, groundwater was neglected in water-resource planning because managers believed that it could not be adequately evaluated in terms of availability, quality, and effect of development on surface water supplies. Now, however, with newly developed digital groundwater models, effects of development can be predicted. Such models have been used to predict hydrologic and quality changes under different stresses. These models have grown in complexity over the last 10 years from simple one-layer flow models to three-dimensional simulations of groundwater flow which may include solute transport, heat transport, effects of land subsidence, and encroachment of salt water. This paper illustrates, through case histories, how predictive groundwater models have provided the information needed for the sound planning and management of water resources in the United States. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80581","issn":"0094-9140","usgsCitation":"Moore, J.E., 1980, Ground-water models for water resources planning: U.S. Geological Survey Open-File Report 80-581, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr80581.","productDescription":"25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0581/report-thumb.jpg"},{"id":53155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0581/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69807b","contributors":{"authors":[{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23998,"text":"ofr802039 - 1980 - Surficial geology of Central Square quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-09-14T21:50:01.013787","indexId":"ofr802039","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-2039","title":"Surficial geology of Central Square quadrangle, Oswego County, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802039","usgsCitation":"Muller, E.H., and Miller, T.S., 1980, Surficial geology of Central Square quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-2039, 1 Plate: 24.25 × 27.36 inches, https://doi.org/10.3133/ofr802039.","productDescription":"1 Plate: 24.25 × 27.36 inches","costCenters":[],"links":[{"id":156306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397652,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75392.htm","linkFileType":{"id":5,"text":"html"}},{"id":53180,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/2039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Central Square quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.125,\n              43.25\n            ],\n            [\n              -76.25,\n              43.25\n            ],\n            [\n              -76.25,\n              43.375\n            ],\n            [\n              -76.125,\n              43.375\n            ],\n            [\n              -76.125,\n              43.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c15","contributors":{"authors":[{"text":"Muller, Ernest Hathaway","contributorId":96297,"corporation":false,"usgs":true,"family":"Muller","given":"Ernest","email":"","middleInitial":"Hathaway","affiliations":[],"preferred":false,"id":191119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24116,"text":"ofr80958 - 1980 - January 1980 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2017-09-29T08:45:22","indexId":"ofr80958","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-958","title":"January 1980 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"<p>This report contains hydrologic data on water-level measurements in observation wells in western and south-central Kansas. The measurements were made in mid-winter, mostly in January, when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also provides basic hydrologic data for relating water-level changes from a \"base-reference year\" (pre-development year), a year of abnormally high rainfall and minimum pumpage (1966), and the previous year (1979). The \"base-reference year\" i s designated as 1950 for the northwestern and west-central areas, 1940 for the southwestern area, and 1944 for the south-central area. Water-level data in the south-central area also are compared with data for 1974. \"Base-reference-year\" water levels are based on measurements made during that year and on interpretation of water-table-contour maps.</p><p>Tables in the report show the depths to water level in 1940, 1944, or 1950 (pre-development years), 1966, 1974, 1979, and 1980; water-level changes from 1940-80,1944-80,1950-80,1966-80,1974-80, and 1979-80; and the average annual changes from 1940-80, 1944-80, 1950-80, 1966-80, and 1974-80. Also shown are saturated thicknesses of the deposits in 1940, 1944, or 1950, and in 1980, as well as the percentage change in saturated thickness from 1940-80, 1944-80, or 1950-80.</p><p>Maps in the report, drawn by digital plotter, show the location of observation wells where water-level measurements are made. The water-level rise or decline, 1979-80, is given to the nearest 0.01 foot; two values at the same location indicate separate wells in the same 10-acre tract.</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 Manage- ment'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 principal meridian; and the third set, the section in which the well is situated. The first letter denotes the 160-acre tract within the section; the second, the 40-acre tract, and the third, the 10-acre tract. The letters, A, B, C, or D, are designated in a counterclockwise direction beginning in the northeast quadrant. Because there may be more than one well in a 10-acre tract, consecutive numbers, beginning with \"1\", are added in the order in which the data from the wells are collect.</p><p>Explanation of geologic units in tables 1 and 2 are: QA, Quaternary alluvium; QU, undifferentiated Quaternary deposits; TO, Ogallala Formation; KN, Niobrara Formation; KU, undifferentiated Lower Cretaceous rocks; KJ, undiffer-rentiated Lower Cretaceous and Upper Jurassic rocks.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80958","issn":"0094-9140","usgsCitation":"Pabst, M., 1980, January 1980 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 80-958, 166 p., https://doi.org/10.3133/ofr80958.","productDescription":"166 p.","numberOfPages":"170","costCenters":[{"id":353,"text":"Kansas Water Science 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