{"pageNumber":"5199","pageRowStart":"129950","pageSize":"25","recordCount":165485,"records":[{"id":37356,"text":"ssrw212 - 1978 - Metabolism of pesticides, an update II","interactions":[],"lastModifiedDate":"2012-02-02T00:09:44","indexId":"ssrw212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"212","title":"Metabolism of pesticides, an update II","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Menzie, C.M., 1978, Metabolism of pesticides, an update II (Updates and supplements Special Scientific Report-Wildlife 127 and 184 (1969 and 1974, respectively).): Special Scientific Report  - Wildlife 212, xvi, 381 p. : ill. ; 27 cm.","productDescription":"xvi, 381 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":167102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":112196,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486884?urlappend=%3Bseq=387"}],"edition":"Updates and supplements Special Scientific Report-Wildlife 127 and 184 (1969 and 1974, respectively).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625559","contributors":{"authors":[{"text":"Menzie, Calvin M.","contributorId":79146,"corporation":false,"usgs":true,"family":"Menzie","given":"Calvin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":217921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39570,"text":"pp712D - 1978 - Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2025-04-15T20:26:16.195733","indexId":"pp712D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"712","chapter":"D","title":"Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp712D","usgsCitation":"Claassen, H., 1978, Hydrologic processes and radionuclide distribution in a cavity and chimney produced by the Cannikin nuclear explosion, Amchitka Island, Alaska: U.S. Geological Survey Professional Paper 712, Report: 27 p.; 1 Plate: 34.50 x 22.50 inches, https://doi.org/10.3133/pp712D.","productDescription":"Report: 27 p.; 1 Plate: 34.50 x 22.50 inches","costCenters":[],"links":[{"id":484616,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113900.htm","linkFileType":{"id":5,"text":"html"}},{"id":67152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0712d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67151,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0712d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122231,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0712d/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.25275267331563,\n              51.33956315534962\n            ],\n            [\n              179.49112175917583,\n              51.36223420066128\n            ],\n            [\n              179.39553212575987,\n              51.421126430176\n            ],\n            [\n              178.84982421853886,\n              51.64392567497552\n            ],\n            [\n              178.6150851187565,\n              51.677701728838\n            ],\n            [\n              178.59814518372121,\n              51.63266139516509\n            ],\n            [\n              178.76996452479904,\n              51.5620081900241\n            ],\n            [\n              179.2261327754033,\n              51.341074907368835\n            ],\n            [\n              179.25275267331563,\n              51.33956315534962\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056d6","contributors":{"authors":[{"text":"Claassen, H.C.","contributorId":74028,"corporation":false,"usgs":true,"family":"Claassen","given":"H.C.","affiliations":[],"preferred":false,"id":221686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40071,"text":"ofr78247 - 1978 - Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"ofr78247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-247","title":"Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr78247","usgsCitation":"Roehler, H.W., 1978, Correlations of coal beds in the Rock Springs Formation in measured sections on the east flank of the Rock Springs Uplift, Sweetwater County, Wyoming: U.S. Geological Survey Open-File Report 78-247, 1 map., https://doi.org/10.3133/ofr78247.","productDescription":"1 map.","costCenters":[],"links":[{"id":165781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":97489,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0247/plate-1.pdf","size":"4705","linkFileType":{"id":1,"text":"pdf"}},{"id":97490,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0247/plate-2.pdf","size":"2026","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842b7","contributors":{"authors":[{"text":"Roehler, Henry W.","contributorId":48529,"corporation":false,"usgs":true,"family":"Roehler","given":"Henry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":222943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36076,"text":"b1448 - 1978 - Geology of the Juazohn Quadrangle, Liberia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:29","indexId":"b1448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1448","title":"Geology of the Juazohn Quadrangle, Liberia","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1448","usgsCitation":"Tysdal, R.G., 1978, Geology of the Juazohn Quadrangle, Liberia: U.S. Geological Survey Bulletin 1448, iv, 39 p. :maps ;23 cm. , https://doi.org/10.3133/b1448.","productDescription":"iv, 39 p. :maps ;23 cm. ","costCenters":[],"links":[{"id":165562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1448/report-thumb.jpg"},{"id":64017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fddd","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":215723,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38697,"text":"pp813I - 1978 - Summary appraisals of the nation's ground-water resources – Mid-Atlantic region","interactions":[],"lastModifiedDate":"2021-12-14T21:53:16.272671","indexId":"pp813I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"I","title":"Summary appraisals of the nation's ground-water resources – Mid-Atlantic region","docAbstract":"<p>The Mid-Atlantic Region covers a total area of about 108,000 square miles. It includes parts of Vermont, Massachusetts, New York, Pennsylvania, Maryland, West Virginia, and Virginia, the entire States of New Jersey and Delaware, and the District of Columbia. It encompasses the entire drainage basins (within the United States) of the Hudson, Delaware, Susquehanna, Potomac, and the James River and includes Long Island and the coastal drainage of New Jersey, Delaware, Maryland, and Virginia.</p>\n<p>Ground water in the region occurs in three broad types of geologic terrane: (1) unconsolidated deposits in the Coastal Plain seaward of the Fall Line; (2) hard, consolidated sedimentary rocks and crystalline igneous and metamorphic rocks in the remainder of the region; and (3) unconsolidated sand, gravel, and other deposits of glacial origin that overlie the older rocks extensively in the glaciated northern part of the region.</p>\n<p>Ground water is derived primarily from precipitation; it can be intercepted for use by pumping from wells before it reaches the streams or before it drains into coastal wetlands or the ocean.</p>\n<p>The natural discharge from the aquifers in the region is estimated to be at about 38.6 billion gallons per day; in addition, at least 140-350 trillion gallons is stored in the rocks.</p>\n<p>About 949 billion gallons of fresh ground water was withdrawn in 1970. This quantity represents about 9 percent of the total freshwater use of 10,220 billion gallons. Available ground-water reserves indicate that a considerable part of the additional supplies needed for the anticipated increase in economic activity in the region could be developed from ground water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813I","usgsCitation":"Sinnott, A., and Cushing, E.M., 1978, Summary appraisals of the nation's ground-water resources – Mid-Atlantic region: U.S. Geological Survey Professional Paper 813, iv, 32 p., https://doi.org/10.3133/pp813I.","productDescription":"iv, 32 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":392895,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","interactions":[{"subject":{"id":10803,"text":"ofr77565 - 1977 - Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region","indexId":"ofr77565","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Souris-Red-Rainy region"},"predicate":"SUPERSEDED_BY","object":{"id":38698,"text":"pp813K - 1978 - Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","indexId":"pp813K","publicationYear":"1978","noYear":false,"chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region"},"id":1}],"lastModifiedDate":"2021-12-14T22:08:19.164288","indexId":"pp813K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"K","title":"Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region","docAbstract":"<p>A broad-perspective analysis of the ground-water resources and present and possible future water development and management in the Souris-Red-Rainy Region is presented. The region includes the basins of the Souris River within Montana and North Dakota; the Red River of the North in South Dakota, North Dakota, and Minnesota; and the Rainy River within Minnesota. The region includes 59,645 square miles, mostly in North Dakota and Minnesota.</p>\n<p>The terrain is relatively flat, but ranges in altitude from 2,541 to 750 feet. Annual average precipitation ranges from 14 inches in the west to 28 inches in the east and about 75 percent of it is rain. The mean annual snowfall ranges from 32 inches in the west to 64 inches in the east. Temperatures range from -55&deg; to 118&deg; F (-48.3&deg; to 47.8&deg; C). Irrigation is needed at least part of the time to assure crop production, particularly in the western part of the region.</p>\n<p>Sand and gravel deposits in the drift form the most important freshwater aquifers. Other aquifers are found in at least parts of the region in the Precambrian, Paleozoic, Cretaceous, and Tertiary rocks. The potentiometric surface in the bedrock aquifers generally decreases in altitude toward the Red River of the North, indicating that the general direction of ground-water movement is toward the river. Ground water with less than 3,000 milligrams per liter dissolved solids is available throughout the region. Ground water with less than 1,000 milligrams per liter occurs in most of the region east of the Red River of the North and in most of the shallow aquifers west of the river. The total volume of water available from storage having less than 3,000 milligrams per liter dissolved solids is estimated to be 5x10<sup>8</sup> acre-feet. In addition to the fresh and slightly saline water, the region has abundant highly mineralized water that can be considered as a resource. Yields of wells in individual bedrock aquifers are generally less than 100 gallons per minute but locally yields may be as much as 500 gallons per minute and more. Yields in drift aquifers are frequently less than 100 gallons per minute but range from 5 to 1,000 gallons per minute. In a few places outwash yields more than 1,000 gallons per minute.</p>\n<p>Ground water is the sole or a primary source of water supply in much of the region, including supplies for irrigation, domestic and livestock, municipal, and industrial needs. Reportedly, the potential irrigation development is 1,550,000 acres, as compared with 50,200 acres in 1975. Both ground- and surface-water supplies would be required to meet these demands. Rural domestic and livestock water supplies are derived almost entirely from ground-water sources. Smaller communities and towns generally rely on ground water, and the cities and industries use ground water, surface water, or both. The municipalities using surface water generally depend upon reservoir storage. Water quality rather than quantity is the greater water-supply problem for many communities in the region.</p>\n<p>Increased demands on both ground-water and surface-water supplies likely will be made in the future. Storage of surface water in the ground-water reservoirs during times of surplus for withdrawal during times of scarcity would aid in meeting these demands. The surplus (flood) water is of better chemical quality than underlying ground water in parts of the western half of the region. Freshwater could be stored in saline- or freshwater aquifers, and pumped out later, as needed. Thus, the ground-water reservoirs have a definite present and potential role in water management.</p>\n<p>To understand the hydrologic system for management purposes there is a need to determine more adequately the geologic and hydrologic characteristics of existing aquifers and the location of new aquifers. Also, as pumping and other stresses on any part of the hydrologic system affect other parts of the system, monitoring programs ideally should be started and maintained to detect changes and determine effects of the stresses.</p>\n<p>Many alternatives are available for managing water in the region. Some of these are operational and others are undergoing research. Adequate hydrologic information is needed to aid in solving problems of water supply, use, and pollution.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813K","usgsCitation":"Reeder, H.O., 1978, Summary appraisals of the nation's ground-water resources – Souris-Red-Rainy region: U.S. Geological Survey Professional Paper 813, vi, 25 p., https://doi.org/10.3133/pp813K.","productDescription":"vi, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":392905,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5066.htm"},{"id":122128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813k/report-thumb.jpg"},{"id":65552,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813k/report.pdf","text":"Report","size":"8.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Minnesota, Montana, North Dakota, South Dakota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ],\n            [\n              -95.185546875,\n              49.06666839558117\n            ],\n            [\n              -95.1416015625,\n              49.52520834197442\n            ],\n            [\n              -94.74609375,\n              49.32512199104001\n            ],\n            [\n              -94.482421875,\n              48.864714761802794\n            ],\n            [\n              -93.69140625,\n              48.69096039092549\n            ],\n            [\n              -93.0322265625,\n              48.719961222646276\n            ],\n            [\n              -92.28515625,\n              48.516604348867475\n            ],\n            [\n              -91.845703125,\n              48.40003249610685\n            ],\n            [\n              -91.3623046875,\n              48.19538740833338\n            ],\n            [\n              -90.7470703125,\n              48.28319289548349\n            ],\n            [\n              -89.384765625,\n              48.1367666796927\n            ],\n            [\n              -90,\n              47.724544549099676\n            ],\n            [\n              -91.2744140625,\n              47.15984001304432\n            ],\n            [\n              -92.373046875,\n              46.70973594407157\n            ],\n            [\n              -94.5703125,\n              45.73685954736049\n            ],\n            [\n              -95.712890625,\n              45.398449976304086\n            ],\n            [\n              -97.0751953125,\n              45.30580259943578\n            ],\n            [\n              -98.525390625,\n              45.82879925192134\n            ],\n            [\n              -99.5361328125,\n              46.10370875598026\n            ],\n            [\n              -100.81054687499999,\n              46.89023157359399\n            ],\n            [\n              -101.953125,\n              47.07012182383309\n            ],\n            [\n              -103.3154296875,\n              47.54687159892238\n            ],\n            [\n              -104.150390625,\n              47.84265762816538\n            ],\n            [\n              -105.2490234375,\n              48.3416461723746\n            ],\n            [\n              -105.40283203124999,\n              49.03786794532644\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996cc","contributors":{"authors":[{"text":"Reeder, Harold O.","contributorId":14381,"corporation":false,"usgs":true,"family":"Reeder","given":"Harold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":220306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38699,"text":"pp813L - 1978 - Summary appraisals of the nation's ground-water resources – Tennessee region","interactions":[{"subject":{"id":49320,"text":"ofr77609 - 1977 - Summary appraisals of the Nation's ground-water resources; Tennessee region, including part of Tennessee and adjacent areas","indexId":"ofr77609","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Tennessee region, including part of Tennessee and adjacent areas"},"predicate":"SUPERSEDED_BY","object":{"id":38699,"text":"pp813L - 1978 - Summary appraisals of the nation's ground-water resources – Tennessee region","indexId":"pp813L","publicationYear":"1978","noYear":false,"chapter":"L","title":"Summary appraisals of the nation's ground-water resources – Tennessee region"},"id":1}],"lastModifiedDate":"2021-12-14T22:10:25.510843","indexId":"pp813L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"L","title":"Summary appraisals of the nation's ground-water resources – Tennessee region","docAbstract":"<p>Ground water is an abundant and little-used resource in the Tennessee Region, a 41,000 square mile area dominated by the Tennessee River system and including parts of Alabama, Georgia, Kentucky, Mississippi, North Carolina, Tennessee, and Virginia. One-fifth to one-fourth of the precipitation that falls on the region enters the ground-water reservoirs. During the year approximately the same amount of water leaves the ground-water system, sustaining the dry-weather flow of streams. Recharge for the region is about 22,000 million gallons per day or 0.5 million gallons per day per square mile. The major types of aquifers in the region are unconsolidated material (including sand and regolith), carbonate rocks, and fractured noncarbonate rocks. One or more of these aquifer types occurs in each of the six physiographic subdivisions of the region. The productivity of these aquifers depends on their hydraulic properties and on the distribution of these properties. The unconsolidated sand aquifers are the most homogeneous in composition and most predictable in occurrence. These aquifers commonly yield 200 to 600 gallons per minute per well depending on the thickness of sand penetrated.</p>\n<p>The most difficult aquifers to predict in regard to depth and yield are the carbonate rocks. In these aquifers it is possible to drill dry holes within a few hundred feet of wells capable of producing several thousand gallons per minute. However, with an adequate reconnaissance study to determine the occurrence of ground water and a planned test drilling program, yields of up to 300 gallons per minute per well can be expected in the carbonate aquifers. Potential yields from the fractured noncarbonate aquifers are lower than in the carbonate rocks.</p>\n<p>The chemical and physical properties of ground water in the Tennessee Region are usually within the limits recommended by the Environmental Protection Agency for drinking water, and the ground water in all but some very shallow aquifers tends to be free of pathogenic microorganisms. Saline water is not known to occur in significant quantities in the region.</p>\n<p>In 1970, 173 million gallons per day of ground water were used in the Tennessee Region. This was less than 8 percent of the total quantity of water used in the region and only 0.8 percent of the estimated ground-water recharge. Ground water is used chiefly as a source of water supply for rural areas and small towns. A lesser amount is used by industries and commercial establishments located beyond the limits of municipal water-supply systems. However, there is potential for significantly increased use in order to augment surface-water supplies and to utilize the total water resource more efficiently.</p>\n<p>Hydrologic studies and adequate test drilling would greatly increase the chances of locating large amounts of ground water, especially in the nine-tenths of the Tennessee Region that is underlain by either carbonate rocks or fractured noncarbonate rocks which have highly variable water-bearing properties. Collectively, such studies are useful in developing a concept of the hydrologic system which would permit the development of criteria for selecting well sites in other areas with a similar geological and hydrological setting. Hydrologic studies that include test drilling have been conducted in all parts of the region except the Cumberland Plateau.</p>\n<p>Some of the basic data necessary for hydrologic studies, such as geologic maps, well records, and streamflow records are available throughout the region. However, detailed information on groundwater levels, ground-water quality, and aquifer characteristics are not equally available throughout the region. This type of information cannot be obtained quickly when it is needed; it must be the product of a continuing program of studies designed to evaluate the Tennessee Region's ground-water resource.</p>\n<p>Because of the interdependence of ground water and surface water, water management efforts can be fully effective only if they involve the whole water resource. In the Tennessee Region, surface water is highly controlled, but there is at present no regionwide water-resources management plan that includes ground water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813L","usgsCitation":"Zurawski, A., 1978, Summary appraisals of the nation's ground-water resources – Tennessee region: U.S. Geological Survey Professional Paper 813, iv., 35 p., https://doi.org/10.3133/pp813L.","productDescription":"iv., 35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392908,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5067.htm"},{"id":65553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813l/report.pdf","text":"Report","size":"5.82 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,{"id":38701,"text":"pp813P - 1978 - Summary appraisals of the Nation's ground-water resources; Alaska","interactions":[],"lastModifiedDate":"2016-01-11T18:44:45","indexId":"pp813P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"P","title":"Summary appraisals of the Nation's ground-water resources; Alaska","docAbstract":"<p>Alaska has enormous surface-water resources, but many of the streams are frozen for most of the year and most contain glacial silt that makes them unacceptable for human use. These factors lend special significance to ground water as a water-supply source, even though perennially frozen ground (permafrost) profoundly modifies ground-water flow systems in much of Alaska north of the maritime southern coast and southeastern panhandle areas. Frozen ground is a virtually impermeable layer that restricts recharge, discharge, and movement of ground water, acts as a confining layer and limits the volume of unconsolidated deposits and bedrock in which water may be stored.</p>\n<p>Ground water is an untested resource in most of Alaska, but in many areas potential development of ground water far exceeds current use. Alluvium of major river valleys, such as the Yukon, Tanana, Kuskokwim and Susitna Rivers, probably contains the most extensive aquifers in the State. Large amounts of ground water are also stored in glacial outwash aquifers that underlie coastal basins and valleys, such as those at Kenai and Anchorage in the Cook Inlet lowland. Individual wells yielding more than 1,000 gallons per minute have been developed in the Tanana River valley, Cook Inlet lowland, and the coastal valleys at Seward and Juneau. Comparable yields should be possible in other areas that have similar geohydrologic environments. No major aquifers have been identified in glacial and glaciolacustrine deposits of interior valleys or in deltaic deposits. Major bedrock aquifers have been identified only in carbonate rocks of the Brooks Range and on the north side of the Alaska Range. Springs issuing from the carbonate rocks of the Brooks Range have discharges as great as 16,000 gallons per minute.</p>\n<p>Most ground-water recharge occurs beneath reaches of stream channels that are losing flow to the ground-water system. Most ground-water discharge also takes place along reaches of stream channels. This discharge augments streamflows during summer and maintains low flows during winter when there is no surface-water runoff. On the basis of a streamflow hydrograph separation technique and using the 60 percent flow-duration value as an indicator of ground-water discharge, it is estimated that 25 percent of the total volume of streamflow in Alaska (exclusive of coastal, maritime environments) is contributed by ground-water discharge.</p>\n<p>The thawing of frozen ground in the permafrost regions of Alaska causes construction and engineering problems. Disturbance of the ground surface disrupts the natural thermal equilibrium and tends to thaw part of the permafrost. Thawing can cause loss of strength, a decrease in volume, and an increase in erosion potential, particularly if the frozen ground is fine grained and poorly drained.</p>\n<p>Present deficiencies in the ground-water information base are obvious limiting factors to ground-water development in Alaska. There is a need to extend the ground-water data-collection network and to pursue special research into the quantitative aspects of ground-water hydrology in cold regions, particularly the continuous permafrost zone.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813P","usgsCitation":"Zenone, C., and Anderson, G.S., 1978, Summary appraisals of the Nation's ground-water resources; Alaska: U.S. Geological Survey Professional Paper 813, vi., 28 p., https://doi.org/10.3133/pp813P.","productDescription":"vi., 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":119943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813p/report-thumb.jpg"},{"id":65555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813p/report.pdf","text":"Report","size":"8.84 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,{"id":36075,"text":"b1449 - 1978 - Geology of the Buchanan quadrangle, Liberia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:29","indexId":"b1449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1449","title":"Geology of the Buchanan quadrangle, Liberia","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1449","usgsCitation":"Tysdal, R.G., 1978, Geology of the Buchanan quadrangle, Liberia: U.S. Geological Survey Bulletin 1449, iv, 31 p. :maps ;23 cm. , https://doi.org/10.3133/b1449.","productDescription":"iv, 31 p. :maps ;23 cm. ","costCenters":[],"links":[{"id":163152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1449/report-thumb.jpg"},{"id":64016,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1449/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683210","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":215722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38702,"text":"pp813Q - 1978 - Summary appraisals of the nation's ground-water resources – Missouri basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:56:38.395429","indexId":"pp813Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"Q","title":"Summary appraisals of the nation's ground-water resources – Missouri basin region","docAbstract":"<p>The Missouri Basin Region lies in the north-central part of the United States and southern Canada. It includes parts of Alberta and Saskatchewan in Canada; parts of Montana, Wyoming, North Dakota, South Dakota, Minnesota, Iowa, Colorado, Kansas, and Missouri, and all of Nebraska in the United States. The region includes about one-sixth of the contiguous United States and requires large water supplies for irrigation, industrial, public, and rural uses. Climate ranges from semiarid to subhumid. Normal annual precipitation increases generally eastward in the downstream direction, but precipitation is not a dependable source of supply. The Missouri River and its tributaries furnish water to many users, but surface water is often inadequate to meet large demands. Numerous surface reservoirs help to regulate streamflow and provide storage, but they also allow an increase in evapotranspiration, which in some areas exceeds normal precipitation. Ground water occurs in aquifers classified as alluvial deposits of sand and gravel, glacial deposits, dune-sand deposits, basin-fill deposits of sand and gravel, sandstone, siltstone, fractured sandy clay, limestone, and dolomite. Ground water can be developed and managed in an orderly manner provided adequate geologic and hydrologic data are available to determine aquifer characteristics and response to pumping and other hydraulic stresses. These data and determinations are essential to design, testing, and implementation of water management plans.</p>\n<p>Unconsolidated and semiconsolidated aquifers include valley-fill alluvium, areally extensive alluvium, glacial deposits, and basin-fill deposits. The aquifers normally consist of alluvial sand and gravel that contain unconfined ground water that lies near the land surface. Many wells completed in the alluvial aquifers have high yields of good-quality water because most alluvial aquifers are highly transmissive and hydraulically connected to streams. Aquifers in glacial deposits may be difficult to locate and in some areas contain saline water; nevertheless, these aquifers are sources of water supply for many users. Basin-fill aquifers are as much as several thousand feet thick, and many contain large ground-water supplies. Ground-water mining has occurred in semiconsolidated aquifers because of withdrawals from wells.&nbsp;Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.</p>\n<p>Sandstone aquifers lie near the land surface and in structural basins. Interbasin movement of ground water occurs in the Virgelle (Milk River aquifer), Fox Hills-basal Hell Creek, and Dakota aquifers. Sandstone aquifers are less transmissive than unconsolidated and semiconsolidated aquifers in general. Confined sandstone aquifers are common, and flowing wells are obtained in many areas. However, flowing wells may cause large declines in water levels if uncontrolled. Water quality is variable in sandstone aquifers but is adequate for most needs.&nbsp;Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.</p>\n<p>Limestone and dolomite aquifers are extensive in the region, but in some areas they lie deep below the land surface. The occurrence of ground water in small pores, fractures, or large caverns causes yields from wells to range widely. Large flows through cavern systems in the aquifers are indicated by large springs in some areas. Water quality is extremely variable and must be considered in any water-development plan.&nbsp;Limestone and dolomite aquifers have potential for development of large water supplies in some areas. The development may be aided by induced recharge and interaquifer leakage.</p>\n<p>Saline ground water occurs throughout the Missouri Basin Region. Dissolved-solids concentration as much as 30,000 milligrams per liter has been measured in aquifers in glacial deposits in Montana. Saline water is common in sandstone aquifers in Wyoming, North Dakota, and South Dakota; maximum reported concentration is 280,000 milligrams per liter in water from the Tensleep Sandstone in Wyoming. Limestone contains saline water in many areas; maximum dissolved-solids concentration is about 350,000 milligrams per liter for the Madison Group in the Williston Basin in North Dakota.</p>\n<p>Comprehensive water-management planning in the Missouri Basin Region will require periodic or continuing inventory of precipitation, streamflow, surface-water storage, and ground water. Water demands for irrigation, industrial, public supply, and rural use are increasing rapidly. Reliance on ground-water supplies is increasing even though in many areas the ground water is still mostly undeveloped. Optimal use of water supplies will require the establishment of realistic goals and carefully conceived water-management plans, each of which will necessarily be based on an adequate baseline of hydrologic data and knowledge of the highly variable hydrologic systems in the region.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813Q","usgsCitation":"Taylor, O., 1978, Summary appraisals of the nation's ground-water resources – Missouri basin region: U.S. Geological Survey Professional Paper 813, Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller, https://doi.org/10.3133/pp813Q.","productDescription":"Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":11156,"text":"ofr78224 - 1978 - Water-quality conditions in southern Rockingham County, New Hampshire","interactions":[],"lastModifiedDate":"2026-02-04T17:34:48.242142","indexId":"ofr78224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-224","title":"Water-quality conditions in southern Rockingham County, New Hampshire","docAbstract":"<p>Physical, chemical, and biological characteristics of water were measured at 26 surface-water sites, 17 ground-water sites, and in effluent from two sanitary landfills as part of planning for area-wide waste management in four watersheds within the Southern Rockingham Regional Planning District in Southern New Hampshire.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78224","collaboration":"Prepared in cooperation with the Southern Rockingham Regional Planning District Commission","usgsCitation":"Silvey, W.D., and Wheeler, R.L., 1978, Water-quality conditions in southern Rockingham County, New Hampshire: U.S. Geological Survey Open-File Report 78-224, iv, 51 p., https://doi.org/10.3133/ofr78224.","productDescription":"iv, 51 p.","costCenters":[],"links":[{"id":144958,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0224/report-thumb.jpg"},{"id":499520,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0224/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Hampshire","county":"Rockingham 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,{"id":36825,"text":"fwsobs78_48 - 1978 - Impacts of transmission lines on birds in flight: Proceedings of a workshop","interactions":[],"lastModifiedDate":"2018-02-26T09:06:56","indexId":"fwsobs78_48","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78/48","title":"Impacts of transmission lines on birds in flight: Proceedings of a workshop","docAbstract":"Progress to alleviate the national and world energy problem will come as individual issues are identified and acceptable solutions implemented. One of the specific issues to emerge in the last few years in the United States is the impact of electric power transmission lines on birds in flight. Therefore, the National Power Plant Team, Office of Biological Services, U.S. Fish and Wildlife Service, requested Oak Ridge Associated Universities (ORAU) to organized and convene a workshop of knowledgeable experts to examine this issue and options for dealing with it. The participants are listed at the end of this report.","conferenceTitle":"Impacts of transmission lines on birds in flight","conferenceDate":"January 31 - February 2, 1978","conferenceLocation":"Oak Ridge, TN","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","collaboration":"This study was conducted as part of the Federal Interagency Energy/Environment Research and Development Program, Office of Research and Development, U.S. Environmental Protection Agency","usgsCitation":"1978, Impacts of transmission lines on birds in flight: Proceedings of a workshop: FWS/OBS 78/48, 151 p.","productDescription":"151 p.","numberOfPages":"155","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":289592,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":289591,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fwsobs/1978/0048/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a04e4b07f02db5f8560","contributors":{"editors":[{"text":"Avery, Michael L.","contributorId":89945,"corporation":false,"usgs":true,"family":"Avery","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":726030,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
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,{"id":39607,"text":"pp988AB - 1978 - Geology and resources of uranium deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp988AB","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"988","chapter":"A,B","title":"Geology and resources of uranium deposits","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.; [for sale by the Supt. of Docs., U.S. Govt. Print. Office],","doi":"10.3133/pp988AB","usgsCitation":"Cathcart, J., Butler, A., and Fischer, R.P., 1978, Geology and resources of uranium deposits: U.S. Geological Survey Professional Paper 988, 28 p., https://doi.org/10.3133/pp988AB.","productDescription":"28 p.","costCenters":[],"links":[{"id":170131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0988a-b/report-thumb.jpg"},{"id":67192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0988a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684276","contributors":{"authors":[{"text":"Cathcart, J.B.","contributorId":83533,"corporation":false,"usgs":true,"family":"Cathcart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":221780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, A.P. Jr.","contributorId":22414,"corporation":false,"usgs":true,"family":"Butler","given":"A.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":221779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fischer, R. P.","contributorId":89958,"corporation":false,"usgs":true,"family":"Fischer","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":221781,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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