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,{"id":62543,"text":"gq1332 - 1976 - Geologic map of the Colfax quadrangle, east-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:45","indexId":"gq1332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"1332","title":"Geologic map of the Colfax quadrangle, east-central Kentucky","language":"ENGLISH","doi":"10.3133/gq1332","usgsCitation":"McDowell, R.C., 1976, Geologic map of the Colfax quadrangle, east-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1332, 1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1332.","productDescription":"1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107759,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10867.htm","linkFileType":{"id":5,"text":"html"},"description":"10867"},{"id":248704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1332/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":254014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1332/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b889","contributors":{"authors":[{"text":"McDowell, Robert Carter","contributorId":81985,"corporation":false,"usgs":true,"family":"McDowell","given":"Robert","email":"","middleInitial":"Carter","affiliations":[],"preferred":false,"id":267522,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67276,"text":"i951 - 1976 - Geologic map of northern part of Ruby Range, Madison County, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:19","indexId":"i951","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"951","subseriesTitle":"NONE","title":"Geologic map of northern part of Ruby Range, Madison County, Montana","language":"ENGLISH","doi":"10.3133/i951","usgsCitation":"Tysdal, R.G., 1976, Geologic map of northern part of Ruby Range, Madison County, Montana: U.S. Geological Survey IMAP 951, 1 map :col. ;70 x 82 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i951.","productDescription":"1 map :col. ;70 x 82 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107069,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9835.htm","linkFileType":{"id":5,"text":"html"},"description":"9835"},{"id":187976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.36749999999999,45.25 ], [ -112.36749999999999,45.3675 ], [ -112.11749999999999,45.3675 ], [ -112.11749999999999,45.25 ], [ -112.36749999999999,45.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a28f4","contributors":{"authors":[{"text":"Tysdal, R. G.","contributorId":8823,"corporation":false,"usgs":true,"family":"Tysdal","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":275900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62982,"text":"gq1330 - 1976 - Geologic map of the Franklinton quadrangle, Henry County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:40","indexId":"gq1330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"1330","title":"Geologic map of the Franklinton quadrangle, Henry County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1330","usgsCitation":"Gibbons, A.B., 1976, Geologic map of the Franklinton quadrangle, Henry County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1330, 1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1330.","productDescription":"1 map :col. ;58 x 46 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107757,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10865.htm","linkFileType":{"id":5,"text":"html"},"description":"10865"},{"id":180028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.11749999999999,38.3675 ], [ -85.11749999999999,38.5 ], [ -85,38.5 ], [ -85,38.3675 ], [ -85.11749999999999,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698f9b","contributors":{"authors":[{"text":"Gibbons, A. B.","contributorId":12016,"corporation":false,"usgs":true,"family":"Gibbons","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":268131,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35378,"text":"b1398 - 1976 - Recent landslides in Alameda County, California (1940-71): An estimate of economic losses and correlations with slope, rainfall, and ancient landslide deposits","interactions":[],"lastModifiedDate":"2021-12-02T22:53:47.566342","indexId":"b1398","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1398","title":"Recent landslides in Alameda County, California (1940-71): An estimate of economic losses and correlations with slope, rainfall, and ancient landslide deposits","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/b1398","usgsCitation":"Nilsen, T.H., Taylor, F.A., and Brabb, E.E., 1976, Recent landslides in Alameda County, California (1940-71): An estimate of economic losses and correlations with slope, rainfall, and ancient landslide deposits: U.S. Geological Survey Bulletin 1398, Report: iii, 21 p.; 1 Plate: 54.50 × 38.00 inches, https://doi.org/10.3133/b1398.","productDescription":"Report: iii, 21 p.; 1 Plate: 54.50 × 38.00 inches","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":167353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1398/report-thumb.jpg"},{"id":63231,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1398/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1398/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392424,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21519.htm"}],"country":"United States","state":"California","county":"Alameda County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.314,\n              37.48\n            ],\n            [\n              -121.4690,\n              37.48\n            ],\n            [\n              -121.4690,\n              37.904\n            ],\n            [\n              -122.314,\n              37.904\n            ],\n            [\n              -122.314,\n              37.48\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648540","contributors":{"authors":[{"text":"Nilsen, Tor Helge","contributorId":89864,"corporation":false,"usgs":true,"family":"Nilsen","given":"Tor","email":"","middleInitial":"Helge","affiliations":[],"preferred":false,"id":214539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Fred A.","contributorId":38142,"corporation":false,"usgs":true,"family":"Taylor","given":"Fred","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214538,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30654,"text":"wri7622 - 1976 - Geohydrology of the lowland lakes area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2019-07-16T12:01:01","indexId":"wri7622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-22","title":"Geohydrology of the lowland lakes area, Anchorage, Alaska","docAbstract":"Unconsolidated deposits, chiefly of glacial origin, make up the surficial geologic materials in the Anchorage lowland lakes area , the western part of the Anchorage glacial outwash plain. Postglacial accumulation of peat, commonly 5 to 10 feet thick, and the presence of ground water at or very near the surface combine to create the swamp-muskeg terrane of much of the area. Deeper, confined ground water is also present beneath thick silt and clay layers that underlie the surficial deposits. Domestic water supply for the lowland lakes area is provided largely by public-supply wells completed in the deep, confined aquifers. No large perennial streams traverse the area, thus streamflow is not a major parameter in the area 's natural water balance. The major uses of surface water are recreational, including fishing and boating at several of the larger lakes, and private and commercial aircraft operations at Hood-Spenard Lakes floatplane base. The hydrology and water balance of these lakes is complex. Water levels in some lakes appear to be closely related to adjacent ground-water levels. Other lakes are evidently perched above the local water table. The relation of lake level to adjacent ground-water level may vary along the shoreline of a single lake. The effect of residential development practices on lake basin water balance is not completely understood. At Sand Lake, the largest lake in this area of rapid urbanization, the water level has declined about 6 feet since the early 1960's. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7622","usgsCitation":"Zenone, C., 1976, Geohydrology of the lowland lakes area, Anchorage, Alaska: U.S. Geological Survey Water-Resources Investigations Report 76-22, 2 Plates: 27.49 x 28.65 inches and 27.31 x 28.52 inches, https://doi.org/10.3133/wri7622.","productDescription":"2 Plates: 27.49 x 28.65 inches and 27.31 x 28.52 inches","costCenters":[],"links":[{"id":159970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0022/report-thumb.jpg"},{"id":365608,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0022/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365609,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.93041992187497,\n              61.15383794909113\n            ],\n            [\n              -149.776611328125,\n              61.15383794909113\n            ],\n            [\n              -149.776611328125,\n              61.227957176677876\n            ],\n            [\n              -149.93041992187497,\n              61.227957176677876\n            ],\n            [\n              -149.93041992187497,\n              61.15383794909113\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a883e","contributors":{"authors":[{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":203612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19779,"text":"ofr76498 - 1976 - Changes in the water supply in the Upper Republican Natural Resources District, Southwest Nebraska, from 1952-75","interactions":[],"lastModifiedDate":"2019-06-11T15:08:49","indexId":"ofr76498","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-498","title":"Changes in the water supply in the Upper Republican Natural Resources District, Southwest Nebraska, from 1952-75","docAbstract":"<p>Use of ground water for irrigation has increased rapidly in the Upper Republican Natural Resources District in southwestern Nebraska in recent years. The principal aquifer being developed is composed of saturated and gravel of the Ogallala Formation of Tertiary age. Water-level declines of as much as 16 feet (4.9 meters) have occurred. Base flow of major streams draining the aquifer was reduced by as much as 19 percent between 1967 and 1975. Recoverable ground water in storage was reduced by about 1 percent. New withdrawal of ground water in 1975 was about 250 ,000 acre-feet (308 million cubic meters), compared with estimated recharge from precipitation of 176,000 acre-feet (217 million cubic meters). Water levels and streamflow will continue to decline if ground-water withdrawals continue at or greater than the 1975. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr76498","usgsCitation":"Lappala, E., 1976, Changes in the water supply in the Upper Republican Natural Resources District, Southwest Nebraska, from 1952-75: U.S. Geological Survey Open-File Report 76-498, iv, 17 p., https://doi.org/10.3133/ofr76498.","productDescription":"iv, 17 p.","numberOfPages":"28","costCenters":[],"links":[{"id":153362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e671e","contributors":{"authors":[{"text":"Lappala, E.G.","contributorId":17996,"corporation":false,"usgs":true,"family":"Lappala","given":"E.G.","affiliations":[],"preferred":false,"id":181496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3107,"text":"wsp2103 - 1976 - Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 3, Basins from Maryland to York River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp2103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2103","title":"Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 3, Basins from Maryland to York River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2103","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Surface water supply of the United States, 1966-70, Part 1, North Atlantic slope basins, v. 3, Basins from Maryland to York River: U.S. Geological Survey Water Supply Paper 2103, x, 971 p. :tables ;23 cm., https://doi.org/10.3133/wsp2103.","productDescription":"x, 971 p. :tables ;23 cm.","costCenters":[],"links":[{"id":139352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2103/report-thumb.jpg"},{"id":30019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692419","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":528084,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24967,"text":"pp933 - 1976 - Geology and resources of fluorine in the United States","interactions":[],"lastModifiedDate":"2018-10-23T17:58:50","indexId":"pp933","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"933","title":"Geology and resources of fluorine in the United States","language":"ENGLISH","publisher":"for sale by the Supt. of Docs., U.S. Govt. Print. Off.,","doi":"10.3133/pp933","usgsCitation":"Van Alstine, R., Worl, R.G., Heyl, A.V., Trace, R.D., Parker, R., Griffitts, W.R., Sainsbury, C., and Cathcart, J., 1976, Geology and resources of fluorine in the United States: U.S. Geological Survey Professional Paper 933, 99 p., https://doi.org/10.3133/pp933.","productDescription":"99 p.","costCenters":[],"links":[{"id":118843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0933/report-thumb.jpg"},{"id":53936,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0933/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684284","contributors":{"editors":[{"text":"Shawe, D. R.","contributorId":48819,"corporation":false,"usgs":true,"family":"Shawe","given":"D. R.","affiliations":[],"preferred":false,"id":749525,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Van Alstine, R. E.","contributorId":54459,"corporation":false,"usgs":true,"family":"Van Alstine","given":"R. E.","affiliations":[],"preferred":false,"id":192889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worl, R. G.","contributorId":13984,"corporation":false,"usgs":true,"family":"Worl","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":192885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heyl, A. V.","contributorId":70032,"corporation":false,"usgs":true,"family":"Heyl","given":"A.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":192890,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trace, R. D.","contributorId":47004,"corporation":false,"usgs":true,"family":"Trace","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":192887,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parker, R. L.","contributorId":19170,"corporation":false,"usgs":true,"family":"Parker","given":"R. L.","affiliations":[],"preferred":false,"id":192886,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Griffitts, W. R.","contributorId":10428,"corporation":false,"usgs":true,"family":"Griffitts","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":192884,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":192892,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Cathcart, J.B.","contributorId":83533,"corporation":false,"usgs":true,"family":"Cathcart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":192891,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":25967,"text":"wri7651 - 1976 - Technical manual for estimating low-flow frequency characteristics of streams in the Susquehanna River basin","interactions":[],"lastModifiedDate":"2017-07-07T08:52:18","indexId":"wri7651","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-51","title":"Technical manual for estimating low-flow frequency characteristics of streams in the Susquehanna River basin","docAbstract":"<p>This report presents procedures for estimating low-flow frequency characteristics for streams in the Susquehanna River basin. The techniques can be used at ungaged sites as well as sites where insufficient data are available to make a reliable estimate. Streams have been divided intp two types--major and minor. Major streams are the Susquehanna, West Branch Susquehanna, Juniata, and Chemung Rivers. Points on these streams with drainage areas of more than 2,000 mi 2 (5,180 km 2 ) are included in this category. Points on these streams with drainage areas of less than 2,000 mi 2 fall into the minor stream category. Generally minor streams are herein defined as those draining less than 2,000 mi 2 (5,180 km 2 ). Multiple -regression techniques have been used to develop relations for estimating the 1-, 3-, 7-, 30-, and 183-day duration low flows at recurrence intervals of 10, 20, SO and 100 years for annual series data and the 1 - , 3-, 7-, and 30-day duration low flows, at the same recurrence intervals, for six individual months, May through October, inclusive. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7651","usgsCitation":"Armbruster, J.T., 1976, Technical manual for estimating low-flow frequency characteristics of streams in the Susquehanna River basin: U.S. Geological Survey Water-Resources Investigations Report 76-51, 71 p. :ill., map (fold. in pocket) ;26 cm., https://doi.org/10.3133/wri7651.","productDescription":"71 p. :ill., map (fold. in pocket) ;26 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":157928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":267199,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0051/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa31f","contributors":{"authors":[{"text":"Armbruster, Jeffrey T.","contributorId":37707,"corporation":false,"usgs":true,"family":"Armbruster","given":"Jeffrey","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":195559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43135,"text":"ofr7635 - 1976 - Land use and land cover and associated maps for Clarksburg, W. Va., and Pa.","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr7635","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-35","title":"Land use and land cover and associated maps for Clarksburg, W. Va., and Pa.","language":"ENGLISH","doi":"10.3133/ofr7635","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Clarksburg, W. Va., and Pa.: U.S. Geological Survey Open-File Report 76-35, 5 maps., https://doi.org/10.3133/ofr7635.","productDescription":"5 maps.","costCenters":[],"links":[{"id":135596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b15eb","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":530983,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46437,"text":"ofr76788 - 1976 - Map showing altitude of the bedrock surface in Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:02:05","indexId":"ofr76788","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-788","title":"Map showing altitude of the bedrock surface in Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr76788","usgsCitation":"1976, Map showing altitude of the bedrock surface in Minnesota: U.S. Geological Survey Open-File Report 76-788, 1 Plate: 25.26 x 32.82 inches, https://doi.org/10.3133/ofr76788.","productDescription":"1 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,{"id":60907,"text":"mf767E - 1976 - Mineral resources map of the Tanacross Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-04-17T19:24:04.542673","indexId":"mf767E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"767","chapter":"E","title":"Mineral resources map of the Tanacross Quadrangle, Alaska","docAbstract":"<p>Areas favorable for the occurrence of two types of mineral deposits are delineated on the map. Known deposits and occurrences are also shown on the map and available data on them are provided in table 1. Information from the known deposits combined with geologic, geochemical, geophysical, and earth satellite data presented in the other components of the Tanacross folio provide the basis for the selection of favorable areas. However because bedrock exposure is poor in the Tanacross quadrangle, types of deposits other than those now known to occur may eventually be found, and boundaries of the area delineated as favorable may change as more information, particularly from drilling, is obtained.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf767E","usgsCitation":"Singer, D., Curtin, G., and Foster, H., 1976, Mineral resources map of the Tanacross Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 767, 1 Plate: 40.46 x 33.85 inches, https://doi.org/10.3133/mf767E.","productDescription":"1 Plate: 40.46 x 33.85 inches","costCenters":[],"links":[{"id":415868,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0767-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0767-E/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Tanacross Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -144,63 ], [ -144,64 ], [ -141,64 ], [ -141,63 ], [ -144,63 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69bd16","contributors":{"authors":[{"text":"Singer, D.A.","contributorId":69128,"corporation":false,"usgs":true,"family":"Singer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":264594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Curtin, G.C.","contributorId":89501,"corporation":false,"usgs":true,"family":"Curtin","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":264595,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, H.L.","contributorId":34894,"corporation":false,"usgs":true,"family":"Foster","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":264593,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15275,"text":"ofr76220 - 1976 - Uranium and trace elements in stream sediments as an exploration tool","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr76220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-220","title":"Uranium and trace elements in stream sediments as an exploration tool","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76220","usgsCitation":"Otton, J.K., 1976, Uranium and trace elements in stream sediments as an exploration tool: U.S. Geological Survey Open-File Report 76-220, ii, 19 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr76220.","productDescription":"ii, 19 leaves :ill., maps ;27 cm.","costCenters":[],"links":[{"id":148194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605c8a","contributors":{"authors":[{"text":"Otton, James K. jkotton@usgs.gov","contributorId":1170,"corporation":false,"usgs":true,"family":"Otton","given":"James","email":"jkotton@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":170867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26260,"text":"wri76118 - 1976 - Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming","interactions":[],"lastModifiedDate":"2023-01-11T19:49:02.96036","indexId":"wri76118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-118","title":"Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming","docAbstract":"<p>The Albin and La Grange areas in southeastern Wyoming are two adjoining different hydrologic areas. Since ground water is the only source of water for irrigation in the Albin area, 34 irrigation wells have been drilled since 1968 and developed in conjunction mostly with center-pivot sprinkler systems that in 1974 irrigated about 6,980 acres. Most irrigation wells are developed in channel deposits of the Ogallala Formation of late Miocene. Water levels in parts of these channel deposits have declined about 4 to 7 feet since pumping began in 1968. In the La Grange area, lands are irrigated by surface water, ground water or a combination of both. The best producing wells are those completed in both the Brule Formation of Oligocene age and the alluvium. Secondary porosity was located and elevated in the Brule using caliper logs, an Acoustic Borehole Televiewer and geophysical logs. From the spring of 1970 to the spring of 1974, hydrographs of wells in parts of the La Grange area show water-level rises of about 5 feet resulting from the net effect of surface-water recharge and groundwater pumpage. Throughout the La Grange area no significant annual water-table declines have occurred. It is unlikely that irrigation wells pumping near Horse Creek have caused significant direct streamflow depletion.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76118","usgsCitation":"Borchert, W.B., 1976, Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 76-118, Report: v, 72 p.; 6 Plates: 33.00 x 27.25 inches or smaller, https://doi.org/10.3133/wri76118.","productDescription":"Report: v, 72 p.; 6 Plates: 33.00 x 27.25 inches or smaller","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":411732,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35026.htm","linkFileType":{"id":5,"text":"html"}},{"id":55066,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55065,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55062,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55061,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55067,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118958,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0118/report-thumb.jpg"},{"id":55063,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55064,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Albin and La Grande areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.482,\n              41.565\n            ],\n            [\n              -104.482,\n              41.317\n            ],\n            [\n              -104.057,\n              41.317\n            ],\n            [\n              -104.057,\n              41.565\n            ],\n            [\n              -104.482,\n              41.565\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89dd","contributors":{"authors":[{"text":"Borchert, W. B.","contributorId":34965,"corporation":false,"usgs":true,"family":"Borchert","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":196076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25390,"text":"wri7652 - 1976 - Analysis of historical water-quality data and a network plan for the Central and Southern Florida Flood Control District","interactions":[],"lastModifiedDate":"2018-11-29T13:37:14","indexId":"wri7652","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-52","title":"Analysis of historical water-quality data and a network plan for the Central and Southern Florida Flood Control District","docAbstract":"<p>Historical water quality data from about 100 sampling stations on streams, canals and lakes in central and southern Florida were analyzed for areal and temporal variations in water quality, statistical measures of the data, relationships between water quality variables, and long term changes or trends in water quality. Included in the analysis were data on the major inorganic chemical constituents, temperature, nitrogen and phosphorus species, trace metals, pesticides, organic carbon and biochemical oxygen demand. Based on the results of the analysis, a network was designed which would provide data to meet six specific objectives: (1) water quality accounting, (2) areal assessments (3) detection of gross long-term trends, (4) detection of toxic and deleterious substances, (5) establish a limnological data base on lakes and (6) furnish data on chemical inputs from the atmosphere.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7652","collaboration":"Prepared in cooperation with Central and Southern Florida Flood Control District","usgsCitation":"Goolsby, D.A., Mattraw, H.C., Lamonds, A.G., Maddy, D., and Rollo, J., 1976, Analysis of historical water-quality data and a network plan for the Central and Southern Florida Flood Control District: U.S. Geological Survey Water-Resources Investigations Report 76-52, vi, 124 p., https://doi.org/10.3133/wri7652.","productDescription":"vi, 124 p.","costCenters":[],"links":[{"id":158170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0052/report-thumb.jpg"},{"id":359801,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82,\n              25\n            ],\n            [\n              -80,\n              25\n            ],\n            [\n              -80,\n              28.5\n            ],\n            [\n              -82,\n              28.5\n            ],\n            [\n              -82,\n              25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680374","contributors":{"authors":[{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mattraw, H. C. Jr.","contributorId":21996,"corporation":false,"usgs":true,"family":"Mattraw","given":"H.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":193494,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":193492,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maddy, D.V.","contributorId":86354,"corporation":false,"usgs":true,"family":"Maddy","given":"D.V.","affiliations":[],"preferred":false,"id":193496,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rollo, J.R.","contributorId":15662,"corporation":false,"usgs":true,"family":"Rollo","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":193493,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":2079,"text":"wsp2038 - 1976 - Hydrology and environmental aspects of Erie Canal (1817-99)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2038","title":"Hydrology and environmental aspects of Erie Canal (1817-99)","docAbstract":"As the first major water project in the United States, the old Erie Canal provides an example of the hydrological and environmental consequences of water development. The available record shows that the project aroused environmental fears that the canal might be impaired by the adverse hydrologic effects of land development induced by the canal. Water requirements proved greater than anticipated, and problems of floods and hydraulic inefficiencies beset navigation throughout its history. The Erie Canal proved the practicality of major hydraulic works to the extent that operations and maintenance could cope with the burdens of deficiencies in design. \r\n\r\nThe weight of prior experience that upland streams, such as the Potomac and Mohawk Rivers, had proved unsatisfactory for dependable navigation, led to a decision to build an independent canal which freed the location from the constraints of river channels and made possible a cross-country water route directly to Lake Erie. \r\n\r\nThe decision on dimensioning the canal prism--chiefly width and depth-involved balance between a fear of building too small and thus not achieving the economic potentials, and a fear of building too expensively. The constraints proved effective, and for the first part of its history the revenues collected were sufficient to repay all costs. So great was the economic advantage of the canal that the rising trend in traffic soon induced an enlargement of the canal cross section, based upon a new but riskier objective-build as large as the projected trend in toll revenues would finance. The increased revenues did not materialize. \r\n\r\nWater supplies were a primary concern for both the planners and the operators of the canal. Water required for lockage, although the most obvious to the planners, proved to be a relatively minor item compared with the amounts of water that were required to compensate for leakage through the bed and banks of the canal. Leakage amounted to about 8 inches of depth per day. The total quantities of water taken into the canal made it the largest hydraulic undertaking of the 19th century in the United States. The diversion of water to factories that were attracted to the canal as a source of hydraulic power added to the water requirements. Although new feeders and reservoirs to extend the supply were built throughout the canal's history, these efforts to cope with water shortages were never fully successful. The primary cause of the persistent deficiencies in supply was the method used to estimate the available flow of the. streams during extended dry spells. Ad hoc, spot measurements of streamflow consistently led to overestimation of the dependable supply. \r\n\r\nThere was a persistent hydraulic problem as well. The cross section of the canal, especially when obstructed by many barges, was inadequate to convey the large volumes of water needed to maintain navigable depths over the long distances between feeders. \r\n\r\nThe major flood problem was caused by cross-drainage--the small creeks that crossed under the canal in culverts. Washout of culverts was a never-ending source of sporadic disruption of traffic of 1 or 2 weeks duration. Repairs and replacements could not cope with the problem created by deficiency in information ,about the flood potentials of 'the small streams. \r\n\r\nA fortunate occurrence of severe floods in 1817 at the start of canal construction provided such clear and persuasive evidence of the flood potentials of the, Mohawk River, which the canal followed for about 110 miles, so as to compel putting the canal at a high level in difficult terrain. \r\n\r\nEnvironmental anxieties, broached early in the planning of the canal, centered on the potentially adverse effects of land development and deforestation on floods, water supply, and erosion. The flow of rivers did not decrease as originally feared. Land use did not increase the intensity of flooding and so endanger the canal. Viewed first as a conveyor of pure water from Lake ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2038","usgsCitation":"Langbein, W.B., 1976, Hydrology and environmental aspects of Erie Canal (1817-99): U.S. Geological Survey Water Supply Paper 2038, vi, 92 p. :ill., maps ;23 cm. --, https://doi.org/10.3133/wsp2038.","productDescription":"vi, 92 p. :ill., maps ;23 cm. --","costCenters":[],"links":[{"id":138347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2038/report-thumb.jpg"},{"id":27639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6050f0","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":144647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3124,"text":"wsp2160 - 1976 - Quality of surface waters of the United States, 1970, Parts 12-16, North Pacific slope basins, Alaska, and Hawaii and other Pacific areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp2160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2160","title":"Quality of surface waters of the United States, 1970, Parts 12-16, North Pacific slope basins, Alaska, and Hawaii and other Pacific areas","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2160","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Quality of surface waters of the United States, 1970, Parts 12-16, North Pacific slope basins, Alaska, and Hawaii and other Pacific areas: U.S. Geological Survey Water Supply Paper 2160, xiv, 501 p. ;23 cm., https://doi.org/10.3133/wsp2160.","productDescription":"xiv, 501 p. ;23 cm.","costCenters":[],"links":[{"id":139457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2160/report-thumb.jpg"},{"id":30036,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65184c","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":528100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4383,"text":"cir717B - 1976 - Seismic engineering program report, April-June 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir717B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"717","chapter":"B","title":"Seismic engineering program report, April-June 1975","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir717B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Seismic engineering program report, April-June 1975: U.S. Geological Survey Circular 717, v, p B1-B6; 26 cm., https://doi.org/10.3133/cir717B.","productDescription":"v, p B1-B6; 26 cm.","costCenters":[],"links":[{"id":120953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0717b/report-thumb.jpg"},{"id":31492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0717b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8e2","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":528201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2085,"text":"wsp2039B - 1976 - An appraisal of ground water for irrigation in the Appleton area, west-central Minnesota","interactions":[{"subject":{"id":14609,"text":"ofr7532 - 1975 - An appraisal of groundwater for irrigation in the Appleton area, west-central Minnesota","indexId":"ofr7532","publicationYear":"1975","noYear":false,"title":"An appraisal of groundwater for irrigation in the Appleton area, west-central Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2085,"text":"wsp2039B - 1976 - An appraisal of ground water for irrigation in the Appleton area, west-central Minnesota","indexId":"wsp2039B","publicationYear":"1976","noYear":false,"chapter":"B","title":"An appraisal of ground water for irrigation in the Appleton area, west-central Minnesota"},"id":1}],"lastModifiedDate":"2018-03-12T13:00:16","indexId":"wsp2039B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2039","chapter":"B","title":"An appraisal of ground water for irrigation in the Appleton area, west-central Minnesota","docAbstract":"<p>Supplemental irrigation of well-drained sandy soils has prompted an evaluation of ground water in the Appleton area. Glacial drift aquifers are the largest source of ground water. The surficial outwash sand and gravel is the most readily available and the most areally extensive drift aquifer, and it underlies much of the sandy soil area. Saturated thickness of the outwash is more than 80 feet (24 m) in places, and potential well yields may exceed 1,200 gal/min (76 1/s) in some areas. In about 17 percent of the area, yields of more than 300 gal/min (19 1/s) are obtainable.</p>\n<p>Recharge to the outwash aquifer occurs primarily during the spring thaw and averages about 5 inches (12.7 cm) annually. Most discharge from the aquifer appears as base flow in the Pomme de Terre River. Despite dissolved-solids concentrations ranging from 280 to 1,350 mg/1, the water is chemically suitable for irrigation.</p>\n<p>Mathematical models of a part of the aquifer were made to evaluate the effects of 20 successive years of ground-water withdrawal for three irrigation-development patterns. It was estimated that the present annual withdrawal rate of 1,410 acre-ft (1.74 hm<sup>3</sup>) would result in water-level declines of less than 3 feet (0.9 m). However, annual withdrawals of 8,450 acre-ft (10.4 hm<sup>3</sup>) would cause aquifer dewatering and decreased well yields in some places. After a new state of equilibrium was established in response to withdrawals, most of the withdrawal would be supplied by diverted base flow from the Pomme de Terre River.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2039B","collaboration":"Prepared in cooperation with the WesMin Resource Conservation and Development Project Committee and the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Larson, S.P., 1976, An appraisal of ground water for irrigation in the Appleton area, west-central Minnesota: U.S. Geological Survey Water Supply Paper 2039, Document: v, 34 p.; 3 Plates: 43.27 x 19.00 inches or smaller, https://doi.org/10.3133/wsp2039B.","productDescription":"Document: v, 34 p.; 3 Plates: 43.27 x 19.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":1634,"text":"wsp2114 - 1976 - Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 2, Upper Mississippi River basin above Keokuk, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp2114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2114","title":"Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 2, Upper Mississippi River basin above Keokuk, Iowa","language":"ENGLISH","publisher":"USGS,","doi":"10.3133/wsp2114","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Surface water supply of the United States, 1966-70, Part 5, Hudson Bay and upper Mississippi River basins, v. 2, Upper Mississippi River basin above Keokuk, Iowa: U.S. Geological Survey Water Supply Paper 2114, 785 p. ;23 cm., https://doi.org/10.3133/wsp2114.","productDescription":"785 p. ;23 cm.","costCenters":[],"links":[{"id":137209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2114/report-thumb.jpg"},{"id":26701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dd2","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":527993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3072,"text":"wsp1608Q - 1976 - Hydrologic evaluation of salinity control and reclamation projects in the Indus Plain, Pakistan--A summary","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"wsp1608Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1608","chapter":"Q","title":"Hydrologic evaluation of salinity control and reclamation projects in the Indus Plain, Pakistan--A summary","docAbstract":"This report summarizes the observations and findings of a team of four specialists from the U.S. Geological Survey assigned to Pakistan under the auspices of the U.S. Agency for International Development during May to August 1972 for a hydrologic evaluation of Salinity Control and Reclamation Projects in the Indus Plain Individual members of the team undertook comprehensive studies related to climatology, surface-water hydrology, and the canal system; streamflow and sediment yields of the rivers; computer applications to hydrologic data; aquifer characteristics; hydrologic evaluation of Salinity Control and Reclamation Projects (SCARPs); tubewell performance; hydrology of shallow versus deep tubewells; well and well-screen design in the Indus Plain; evaluation of observed and anticipated trends in both private and public tubewell development; evaluation of water-quality programs, data analysis, and records, and computer coding of special water-quality data; and evaluation of water-level data, well discharge and specific-capacity tests and aquifer tests. \r\n\r\nThe reclamation program, by pumping from tubewells, has been notably successful in lowering the water table, in providing supplemental water for irrigation and for leaching of salinized soils, and in improving crop production. Some changes in water quality have been observed in SCARP-I and the Mona Scheme of SCARP-II, but these have not as yet (1972) significantly affected the utility of the water for irrigation. Problems associated with reclamation include control of deterioration in performance of tubewells and their rehabilitation, local brackish or saline-water encroachment, and maintenance of a favorable salt balance in the ground-water system. \r\n\r\nRapid and as yet (1972) unregulated growth of shallow private tubewell development in the past decade has introduced complicating factors to the reclamation planning of the early 1960's which had emphasized public tubewell development through the SCARP program. In comparing shallow (0-200 feet) with deep (200-400 feet} tubewell development, it is concluded that long-term response of the water table is the same, whether many shallow wells of small capacity or fewer deeper wells of large capacity pump the same total volume of water in the same area. Moreover, it is concluded that there is no definite advantage for either type of pumping regime with respect to water quality. \r\n\r\nUtilization of the Punjab aquifer could be greatly enhanced by recharge of high-quality water diverted from the Chenab and Jhelum Rivers to the Ravi and Sutlej Rivers by way of the link and irrigation canals during periods of surplus flow. Recharge to the aquifer could also be improved by diversion of high-quality water from the Chenab and the Jhelum to natural nalas and other surface drainageways during periods of surplus flow. Such recharge would be of much better quality than water leaching downward from irrigated fields. Continued monitoring of the hydrologic system and research on problems engendered by reclamation are essential to the viability of the SCARP program and related water-resources development in the Indus River Basin.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1608Q","usgsCitation":"Mundorff, M.J., Carrigan, P., Steele, T., and Randall, A., 1976, Hydrologic evaluation of salinity control and reclamation projects in the Indus Plain, Pakistan--A summary: U.S. Geological Survey Water Supply Paper 1608, v, 59 p. :ill., maps (some fold. col. in pocket) ;24 cm. --, https://doi.org/10.3133/wsp1608Q.","productDescription":"v, 59 p. :ill., maps (some fold. col. in pocket) ;24 cm. --","costCenters":[],"links":[{"id":139328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608q/report-thumb.jpg"},{"id":29939,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608q/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29940,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608q/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29941,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608q/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698575","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":146239,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrigan, P.H. Jr.","contributorId":21935,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":146237,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steele, T.D.","contributorId":38976,"corporation":false,"usgs":true,"family":"Steele","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":146238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Randall, A. D.","contributorId":81077,"corporation":false,"usgs":true,"family":"Randall","given":"A. D.","affiliations":[],"preferred":false,"id":146240,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3068,"text":"wsp2004 - 1976 - Artificial recharge through a well in fissured carbonate rock, west St. Paul, Minnesota","interactions":[{"subject":{"id":15589,"text":"ofr74367 - 1974 - Artificial recharge through a well in fissured carbonate rock, West St. Paul, Minnesota","indexId":"ofr74367","publicationYear":"1974","noYear":false,"title":"Artificial recharge through a well in fissured carbonate rock, West St. Paul, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":3068,"text":"wsp2004 - 1976 - Artificial recharge through a well in fissured carbonate rock, west St. Paul, Minnesota","indexId":"wsp2004","publicationYear":"1976","noYear":false,"title":"Artificial recharge through a well in fissured carbonate rock, west St. Paul, Minnesota"},"id":1}],"lastModifiedDate":"2018-03-19T11:07:09","indexId":"wsp2004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2004","title":"Artificial recharge through a well in fissured carbonate rock, west St. Paul, Minnesota","docAbstract":"<p>The Prairie du Chien Group was injected with 2,754,000 gallons (368,200 cubic feet), or 10,430 cubic metres, of municipally treated water at about 100 gallons per minute (13.4 cubic feet per minute), or 6.3 litres per second, for 20 days. The injection-pipe system was designed to utilize pipe friction rather than a remote-controlled valve in the well to maintain positive pressure and eliminate air entrainment in the injection water and the escape cf dissolved gasses from the water. During the 20-day injection period the temperature of the injection water declined gradually from 15.0<span>&deg;</span> to 11.2<span>&deg;</span>C, and the flow rate decreased from 108 to 90 gallons per minute (6.8 to 5.7 litres per second).</p>\n<p>Analyses of test data were, in some instances, based upon hydrologic judgement as well as observations. Results of aquifer tests before and after injections indicated that the transmissivity had decreased 18 percent during the intervening injection periods; however, the specific capacity remained the same, indicating no change in transmissivity during pumping. Analysis of water-level changes in observation wells during injection indicated a reduction in transmissivity of more than 50 percent; however, the specific capacity of the injection well decreased only about 5 percent during injection.</p>\n<p>A comparison of water-level changes with the discharge or recharge rates of the three tests showed that the water-level changes in the two observation wells tapping the Prairie du Chien Group during the injection test were greater than those projected from the two aouifer pumping tests. The deviations in the water-level changes and in the analysis of aquifer-test data indicate that the methods used to analyze data from these wells may not be wholly applicable, inasmuch as anisotropic and nonhomogeneous conditions prevail in at least the Prairie du Chien part of the aquifer.</p>\n<p>The native water and the injected water averaged 0.8 and 25 milligrams per litre chloride, respectively. The chloride, utilized as a tracer, showed that the injected water was detected only in the lower part of the nearest observation well, 99 feet (30.2 metres) from the injection well. The chemistry of the water and the rock formation showed little likelihood of plugging of the recharge well by chemical precipitation. Microbiological phenomena apparently did not become a significant factor in the recharge test.</p>\n<p>The hydraulic gradient of the aquifer in October and December 1971 (before and after injection) was estimated to be N. 36<span>&deg;</span> E., 0.0013, and N. 39<span>&deg;</span> E., 0.0012, respectively, on the basis of measurements of water levels in the three wells in the Prairie du Chien Group. The single-well tracer-dilution method of calculation showed a hydraulic gradient of 0.0016. A longitudinal dispersivity of 280 feet (85 metres) was calculated. Such a value of dispersivity is typical of fractured reservoirs and shows that the Prairie du Chien Group is a heterogeneous aquifer.</p>\n<p>The injection test demonstrated that it is hydrologically feasible to recharge the Prairie du Chien Group and the Jordan Sandstone artificially through wells completed in the Prairie du Chien Group. The fissures in the Prairie du Chien Group act as conduits through which water spreads. The water passes into the Jordan Sandstone from the Prairie du Chien over a larger area than it would if it were injected directly into the Jordan.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2004","usgsCitation":"Reeder, H.O., Wood, W., Ehrlich, G.G., and Sun, R.J., 1976, Artificial recharge through a well in fissured carbonate rock, west St. Paul, Minnesota: U.S. Geological Survey Water Supply Paper 2004, vi, 80.p., https://doi.org/10.3133/wsp2004.","productDescription":"vi, 80.p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":29926,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2004/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"West St. Paul","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bf0","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":146230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":629817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ehrlich, G. G.","contributorId":89126,"corporation":false,"usgs":true,"family":"Ehrlich","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":146232,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sun, Ren Jen","contributorId":68721,"corporation":false,"usgs":true,"family":"Sun","given":"Ren","email":"","middleInitial":"Jen","affiliations":[],"preferred":false,"id":146231,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26349,"text":"wri7669 - 1976 - Availability and chemical characteristics of ground water in central La Plata County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri7669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-69","title":"Availability and chemical characteristics of ground water in central La Plata County, Colorado","docAbstract":"The central part of La Plata County, Colo., has undergone rapid population growth in recent years. This growth has resulted in an increased demand for information for additional domestic, industrial, and municipal water supplies. A knowledge of the occurrence of ground water will permit a more efficient allocation of the resource. Aquifers in central La Plata County include: alluvium, Animas Formation of Quaternary and Tertiary age, Fruitland Formation, Pictured Cliffs Sandstone, three formations of the Mesa Verde Group, the Mancos Shale, Dakota Sandstone, Morrison Formation of Cretaceous and Jurassic age, and undifferentiated formations. Well yields generally are low, usually less than 25 gallons per minute. However, higher yields, 25 to 50 gallons per minute may be found locally in aquifers in the alluvium and the Animas Formation. The quality of water from the aquifers is dependent on rock type. Most of the water is a calcium bicarbonate type. However, aquifers that are predominantly fine-grained or contain interbeds of shale may contain sodium bicarbonate type water. The dissolution of minerals in the coal beds, which are present in the Mesa Verde Group and the Dakota Sandstone, can contribute high concentrations of iron, sulfate, and chloride to ground water. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7669","usgsCitation":"Brogden, R., and Giles, T., 1976, Availability and chemical characteristics of ground water in central La Plata County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 76-69, 2 maps (1 col.) ;on sheet 82 x 95 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/wri7669.","productDescription":"2 maps (1 col.) ;on sheet 82 x 95 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":158459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":55145,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0069/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f34","contributors":{"authors":[{"text":"Brogden, R. E.","contributorId":43356,"corporation":false,"usgs":true,"family":"Brogden","given":"R. E.","affiliations":[],"preferred":false,"id":196228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giles, T.F.","contributorId":83096,"corporation":false,"usgs":true,"family":"Giles","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":196229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43570,"text":"ofr7627 - 1976 - Land use and land cover and associated maps for Savannah, Georgia; Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr7627","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-27","title":"Land use and land cover and associated maps for Savannah, Georgia; Alabama","language":"ENGLISH","doi":"10.3133/ofr7627","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Savannah, Georgia; Alabama: U.S. Geological Survey Open-File Report 76-27, 4 maps., https://doi.org/10.3133/ofr7627.","productDescription":"4 maps.","costCenters":[],"links":[{"id":167850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5a9","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":531245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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