A common method of publication for Soviet scientists, which partly supplants periodicals, is the publication of a collection of articles on a general area of research, frequently by members of a given institution. An extensive sampling of world geologic literature for 1961 (Hawkes, 1966) showed that 33 percent of Soviet titles appeared in periodicals whereas 55 percent of North American and 70 percent of Western European literature appeared in this form.
\nThe Soviet predilection for symposia and collections of papers makes searching for information on a given subject more difficult for Westerners because the monographs in question are often not included in exchange agreements (except informal personal ones) with Western libraries and institutions, because they may be primed in small editions, and because such publications frequently escape the notice of Western abstract journals.
\nUnless one is fortunate enough to have many personal contacts in the Soviet Union, there seems to be little alternative to at least a rudimentary knowledge of Russian in order to stay abreast of work published as monographs and in collections.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water Resources Division Bulletin","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70047729","usgsCitation":"Manheim, F., 1966, Soviet books and publications on hydrology (continental) and hydrogeology: titles and some notes on obtaining Soviet monographs, 4 p., https://doi.org/10.3133/70047729.","productDescription":"4 p.","startPage":"22","endPage":"25","costCenters":[],"links":[{"id":276871,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047729/report-thumb.jpg"},{"id":279945,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047729/report.pdf"}],"country":"Armenia;Azerbaijan;Belarus;Estonia;Georgia;Kazakhstan;Kyrgyzstan;Latvia;Lithuania;Moldova;Russia;Tajikistan;Turkmenistan","otherGeospatial":"Union Of Soviet Socialist Republics","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 23.0,35.5 ], [ 23.0,77.7 ], [ 179.9,77.7 ], [ 179.9,35.5 ], [ 23.0,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5215e164e4b02034073ad416","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":482836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70263595,"text":"70263595 - 1966 - Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands","interactions":[],"lastModifiedDate":"2025-02-14T21:16:24.403461","indexId":"70263595","displayToPublicDate":"1966-01-01T16:16:03","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands","docAbstract":"Moderate supplies of potable ground water are believed to be available in the Roadtown and Paraquita Bay areas, and small, possibly brackish supplies in the Long Look and West End areas of Tortola. Two water bearing units of the same hydrologic system have the potential of yielding water to wells: 1) alluvial deposits, possibly as thick as 60 feet and locally containing beds and lenses of gravel 1 to 5 feet thick; and 2) fractured and jointed bedrock, especially where it is overlain by alluvium.
The most productive ground-water areas are expected to be the lower reaches of the larger valleys. Here the alluvial deposits are thickest and the valleys often follow the trace of fault or fracture systems in the bedrock. A potential yield of 195,000 gpd (U.S. gallons per day) is estimated to be available in the Road Bay area, 55,000 gpd in the Long Look area, and 8,000 gpd in the West End area.
Sites are suggested for test and monitoring wells in the lower courses of six of the valleys on the south coast.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70263595","collaboration":"Work Done in Cooperation with the Government of the Virgin Islands, Ralph M. Paiewonsky, Governor","usgsCitation":"Jordan, D., 1966, Test well sites and preliminary evaluation of ground-water potential in Tortola, British Virgin Islands, 35 p., https://doi.org/10.3133/70263595.","productDescription":"35 p.","costCenters":[],"links":[{"id":482116,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70263595/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":482115,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70263595/report-thumb.jpg"}],"country":"United States","state":"Virgin Islands","otherGeospatial":"Tortola","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -64.51309561955642,\n 18.51802619929059\n ],\n [\n -64.74978261433117,\n 18.51802619929059\n ],\n [\n -64.74978261433117,\n 18.336353177581245\n ],\n [\n -64.51309561955642,\n 18.336353177581245\n ],\n [\n -64.51309561955642,\n 18.51802619929059\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jordan, Donald G.","contributorId":9519,"corporation":false,"usgs":true,"family":"Jordan","given":"Donald G.","affiliations":[],"preferred":false,"id":927458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048291,"text":"70048291 - 1966 - Soviet books and publications on geological and chemical oceanography, hydrology, and other subjects acquired during the second international oceanographic congress, Moscow, June 1966: titles and some translated contents and notes","interactions":[],"lastModifiedDate":"2019-12-19T15:46:21","indexId":"70048291","displayToPublicDate":"1966-01-01T13:57:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Soviet books and publications on geological and chemical oceanography, hydrology, and other subjects acquired during the second international oceanographic congress, Moscow, June 1966: titles and some translated contents and notes","docAbstract":"The listed publications represent a selection, by no means complete, of recent Soviet work in geological and chemical oceanography. Some works on hydrogeology and hydrochemistry of the continents, as well as a few publications on other subjects, such as geology, geophysics, and biology, also are included.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Woods Hole, Massachusetts","doi":"10.3133/70048291","usgsCitation":"Manheim, F., 1966, Soviet books and publications on geological and chemical oceanography, hydrology, and other subjects acquired during the second international oceanographic congress, Moscow, June 1966: titles and some translated contents and notes, 37 p., https://doi.org/10.3133/70048291.","productDescription":"37 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":277934,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70048291.jpg"},{"id":284817,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70048291/report.pdf"}],"otherGeospatial":"Soviet Union","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cfae4b024b60d407399","contributors":{"authors":[{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":484253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221257,"text":"70221257 - 1966 - Hydrology of limestone terranes in the coastal plain of the Southeastern United States","interactions":[],"lastModifiedDate":"2021-06-09T14:56:52.390317","indexId":"70221257","displayToPublicDate":"1966-01-01T12:42:46","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of limestone terranes in the coastal plain of the Southeastern United States","docAbstract":"The very productive limestone aquifers of Tertiary and Quaternary age in the Coastal Plain of the Southeastern States contain a water-table circulation system where aquifers are at or near the land surface; the Tertiary limestone unit is a homoclinal artesian system confined beneath younger beds in coastal areas.
The Tertiary limestone has a total thickness of several thousand feet and ranges in age from Paleocene to Pliocene. The part of the limestone that represents a hydrologic unit, as much as 1000 feet thick, ranges in age from middle Eocene to middle Miocene. That unit is the principal artesian aquifer in Florida and southeastern Georgia. It is also an aquifer, but of lesser importance, in South Carolina, North Carolina, and Alabama. In southeastern Florida the Quaternary limestone forms a shallow, although highly productive, aquifer.
In general, the Tertiary formations dip gently toward the coast, except where the regional dip is interrupted by folds such as the Cape Fear arch, the Ocala uplift, and the Chattahoochee anticline, or by faults such as those on the Ocala uplift.
A piezometric map showing the head of water in the principal artesian aquifer in Florida and southeastern Georgia reveals chief areas of recharge where limestone crops out in interstream areas and where sinkholes breach overlying beds; it reveals principal discharge areas in certain stream valleys, springs, and offshore.
Lateral movement of the water in the limestone is generally controlled by the hydraulic gradient to the nearest discharge area. The movement may be either controlled by or independent of faults and folds; it may be along joints for short distances. Solution by downward movement of water in the zone of aeration to the water table has formed vertical tubular openings or shafts. Lateral movement of the water from areas of recharge to areas of discharge has formed caves and other solution channels, chiefly in the upper part of the zone of saturation. Since they were formed, some caves have been drowned, and others have been exposed in the zone of aeration as the water rose and fell, chiefly in Pleistocene time. The principal aquifer in Florida probably has caves and solution channels comparable in size and extent to those of Mammoth Cave, Kentucky; however, only a small percentage of these are above the water table at the present time.
In a large part of the region the most noticeable change in chemical quality of the water in the limestone resulting from circulation of water is the freshening accompanying removal of salty water from the aquifer.
Changes in sea level during Pleistocene time have raised and lowered the water table; thus the position of the upper part of the zone of saturation, in which conditions were most favorable for solution and for the formation of cavities, has changed repeatedly. At the lowest stand of the Pleistocene sea, it is conceivable that the water level in part of the limestone in north-central Florida was a few hundred feet lower than at present. The present pattern of solution openings probably was developed in Pleistocene time.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE93-p1","usgsCitation":"Stringfield, V.T., and LeGrand, H.E., 1966, Hydrology of limestone terranes in the coastal plain of the Southeastern United States: Special Paper of the Geological Society of America, v. 93, p. 1-46, https://doi.org/10.1130/SPE93-p1.","productDescription":"46 p.","startPage":"1","endPage":"46","costCenters":[],"links":[{"id":386303,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Southeastern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.1748046875,\n 25.085598897064752\n ],\n [\n -73.2568359375,\n 25.085598897064752\n ],\n [\n -73.2568359375,\n 36.42128244364947\n ],\n [\n -83.75976562499999,\n 36.421282443649496\n ],\n [\n -94.1748046875,\n 36.42128244364947\n ],\n [\n -94.1748046875,\n 25.085598897064752\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"93","noUsgsAuthors":false,"publicationDate":"1966-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":817177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeGrand, H. E.","contributorId":54571,"corporation":false,"usgs":true,"family":"LeGrand","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171424,"text":"70171424 - 1966 - Glacier mass budget measurements by hydrologic means","interactions":[],"lastModifiedDate":"2018-02-04T14:15:36","indexId":"70171424","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Glacier mass budget measurements by hydrologic means","docAbstract":"Ice storage changes for the South Cascade Glacier drainage basin were determined for the 1957–1964 period using basin runoff and precipitation measurements. Measurements indicate that evaporation and condensation are negligible compared with the large runoff and precipitation values. Runoff, measured by a stream discharge station, averaged 4.04 m/yr; precipitation, determined by snow accumulation measurements at a central point on the glacier and by storage gages, averaged 3.82 m/yr, resulting in a basin net loss of about 0.22 m/yr. During the same period, South Cascade Glacier net budgets were determined by ablation stakes, snow density-depth profiles, and maps. The average glacier net budget for the period was −0.61sol;yr of water. This amount is equivalent to −0.26 m of water when averaged over the drainage basin (43% glacier-covered), which is in fair agreement with the net storage change measured by hydrologic methods. Agreement between the two methods for individual years is slightly less perfect.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR002i001p00105","usgsCitation":"Tangborn, W.V., 1966, Glacier mass budget measurements by hydrologic means: Water Resources Research, v. 2, no. 1, p. 105-110, https://doi.org/10.1029/WR002i001p00105.","productDescription":"6 p.","startPage":"105","endPage":"110","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321910,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"South Cascade Glacier","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.09182357788086,\n 48.34118976566224\n ],\n [\n -121.0370635986328,\n 48.34118976566224\n ],\n [\n -121.0370635986328,\n 48.3807678494171\n ],\n [\n -121.09182357788086,\n 48.3807678494171\n ],\n [\n -121.09182357788086,\n 48.34118976566224\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"1","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"574eb5cbe4b0ee97d51a83c1","contributors":{"authors":[{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70190812,"text":"70190812 - 1966 - Hydrologic and climatologic data collected through 1964, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T16:51:21","indexId":"70190812","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Hydrologic and climatologic data collected through 1964, Salt Lake County, Utah","docAbstract":"An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed equally by the State of Utah and the Federal Government in accordance with an agreement between the State Engineer and the Geological Survey. The Utah Water and Power Board, Utah Fish and Game Commission, Salt Lake County Water Conservancy District, Metropolitan Water District of Salt Lake City, Salt Lake County, Kennecott Copper Corporation, Utah Power and Light Company, and Salt Lake City Chamber of Commerce contributed funds to the State Engineer's office toward support of the project.
The investigation encompasses the collection and interpretation of a large variety of climatologic, hydrologic, and geologic data in and near Salt Lake County. This basic-data report sets forth climatologic and surface-water data collected by project personnel and others during the water year beginning October 1, 1963, and ending September 30, 1964, and ground-water data collected by project personnel and others for the period July 1, 1963, through December 31, 1964. Included also are some earlier ground-water data not previously published. Organizations that furnished data are acknowledged in station descriptions and footnotes to tables. Data collected during the period of investigation will be published in annual basic-data releases and an interpretative report will be published at the completion of the investigation.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with The State of Utah and local organizations","usgsCitation":"Iorns, W., Mower, R.W., and Horr, C.A., 1966, Hydrologic and climatologic data collected through 1964, Salt Lake County, Utah: Utah Basic-Data Release 11, ii, 91 p.","productDescription":"ii, 91 p.","numberOfPages":"96","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345783,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-220&Title=Basic+Data+Report+11"}],"country":"United States","state":"Utah","county":"Salt Lake 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A.","contributorId":63940,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":710530,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70190813,"text":"70190813 - 1966 - Hydrologic and climatologic data, 1965, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2018-03-26T15:44:09","indexId":"70190813","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Hydrologic and climatologic data, 1965, Salt Lake County, Utah","docAbstract":"An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed equally by the State of Utah and the Federal Government in accordance with an agreement between the State Engineer and the Geological Survey. The Utah Water and Power Board, Utah Fish and Game Commission, Salt Lake County Water Conservancy District, Metropolitan Water District of Salt Lake City, Salt Lake County, Kennecott Copper Corporation, Utah Power and Light Company, Salt Lake City Chamber of Commerce, and the Central Utah Water Conservancy District. contributed funds to the State Engineer's office toward support of the project.
The investigation encompasses the collection and interpretation of a large variety of climatologic, hydrologic, and geologic data in and near Salt Lake County. Utah Basic-Data Release No. 11 contains data collected through 1964. This release contains climatologic and surface-water data for the 1965 water year (October 1964 to September 1965) and ground-water data collected during the 1965 calendar year. Similar annual releases will contain data collected during the remainder of the investigation, and interpretive reports will be prepared as the investigation proceeds. Organizations that furnished data are acknowledged in station descriptions and footnotes to tables.
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A.","contributorId":63940,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":710533,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185640,"text":"70185640 - 1966 - Waste injection into a deep limestone in northwestern Florida","interactions":[],"lastModifiedDate":"2020-01-26T10:23:28","indexId":"70185640","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Waste injection into a deep limestone in northwestern Florida","docAbstract":"During a three-month trial period, 70 million gallons of industrial wastes were successfully injected at moderate pressures into a deep limestone in the westernmost part of Florida. The movement of these wastes is expected to be predominantly southward toward the natural discharge area which is presumed to be far out in the Gulf of Mexico. The limestone lies between two thick beds of clay (aquicludes) and contains 13,000 parts per million salty water. A series of aquifers and aquicludes appear capable of preventing contamination of the overlying fresh-water aquifers.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1966.tb01588.x","usgsCitation":"Barraclough, J., 1966, Waste injection into a deep limestone in northwestern Florida: Groundwater, v. 4, no. 1, p. 22-24, https://doi.org/10.1111/j.1745-6584.1966.tb01588.x.","productDescription":"3 p. ","startPage":"22","endPage":"24","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338341,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"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 -87.9345703125,\n 29.611670115197377\n ],\n [\n -83.0126953125,\n 29.611670115197377\n ],\n [\n -83.0126953125,\n 31.203404950917395\n ],\n [\n -87.9345703125,\n 31.203404950917395\n ],\n [\n -87.9345703125,\n 29.611670115197377\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"58d63044e4b05ec799131139","contributors":{"authors":[{"text":"Barraclough, J.T.","contributorId":16003,"corporation":false,"usgs":true,"family":"Barraclough","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":686181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68346,"text":"ha167 - 1966 - Availability of ground water in the Crutchfield quadrangle, Jackson Purchase region, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:34:25.686293","indexId":"ha167","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"167","title":"Availability of ground water in the Crutchfield quadrangle, Jackson Purchase region, Kentucky-Tennessee","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha167","usgsCitation":"Hansen, A., 1966, Availability of ground water in the Crutchfield quadrangle, Jackson Purchase region, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 167, 1 Plate: 48.00 x 38.50 inches, https://doi.org/10.3133/ha167.","productDescription":"1 Plate: 48.00 x 38.50 inches","costCenters":[],"links":[{"id":188893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89822,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/167/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413582,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15528.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Crutchfield quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89,\n 36.5\n ],\n [\n -89,\n 36.625\n ],\n [\n -88.875,\n 36.625\n ],\n [\n -88.875,\n 36.5\n ],\n [\n -89,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de02","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":278069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68240,"text":"ha168 - 1966 - Availability of ground water in the Heath quadrangle, Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2023-11-28T21:59:12.573943","indexId":"ha168","displayToPublicDate":"1966-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"168","title":"Availability of ground water in the Heath quadrangle, Jackson Purchase region, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha168","usgsCitation":"Lambert, T.W., 1966, Availability of ground water in the Heath quadrangle, Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 168, 1 Plate: 48.00 x 36.00 inches, https://doi.org/10.3133/ha168.","productDescription":"1 Plate: 48.00 x 36.00 inches","costCenters":[],"links":[{"id":423023,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15529.htm","linkFileType":{"id":5,"text":"html"}},{"id":89620,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/168/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":189568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Heath quadrangle, Jackson Purchase region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.875,\n 37.125\n ],\n [\n -88.875,\n 37\n ],\n [\n -88.75,\n 37\n ],\n [\n -88.75,\n 37.125\n ],\n [\n -88.875,\n 37.125\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d975","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68153,"text":"ha190 - 1965 - Flood on Big Fossil Creek at Haltom City near Fort Worth, Texas, in 1962","interactions":[],"lastModifiedDate":"2016-08-16T16:11:44","indexId":"ha190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"190","title":"Flood on Big Fossil Creek at Haltom City near Fort Worth, Texas, in 1962","docAbstract":"The approximate area inundated near Fort Worth, Texas, by Big Fossil Creek, during the flood of September 7, 1962, is shown on a topographic map to record the flood hazard in graphic form. Big Fossil Creek, which drains an area of 74.7 square miles, flows generally southeastward along the northeast edge of Fort Worth through Richland Hills and Haltom City, into West Fork Trinity River. The flood of September 7, 1962, the greatest in Richland Hills since at least 1900 was the result of a high rate of discharge from the area upstream from the confluence of Big Fossil Creek and Whites Branch. Greater floods are possible, but no attempt has been made to show their probable overflow limits. Future protective works may reduce the frequency of flooding in the area but will not necessarily eliminate flooding. Changes in culture such as new highways and bridges and changes in land use may influence the inundation pattern of future floods. Mapping of the West Fork Trinity River flood was beyond the scope of the Big Fossil Creek study, and is not shown.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha190","usgsCitation":"Montgomery, J.H., Ruggles, F., and Patterson, J.L., 1965, Flood on Big Fossil Creek at Haltom City near Fort Worth, Texas, in 1962: U.S. Geological Survey Hydrologic Atlas 190, Plate: 40.50 x 31.76 inches, https://doi.org/10.3133/ha190.","productDescription":"Plate: 40.50 x 31.76 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha190.JPG"},{"id":89455,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/190/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Texas","otherGeospatial":"Big Fossil Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.375,\n 32.875\n ],\n [\n -97.375,\n 32.75\n ],\n [\n -97.195833,\n 32.75\n ],\n [\n -97.195833,\n 32.875\n ],\n [\n -97.375,\n 32.875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e74d5","contributors":{"authors":[{"text":"Montgomery, John H.","contributorId":102151,"corporation":false,"usgs":true,"family":"Montgomery","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, Frederick H.","contributorId":96665,"corporation":false,"usgs":true,"family":"Ruggles","given":"Frederick H.","affiliations":[],"preferred":false,"id":277736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, James Lee","contributorId":24329,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":277735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68152,"text":"ha155 - 1965 - Availability of ground water in the parts of the Little Cypress and Calvert City quadrangles in the Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2022-11-28T20:03:41.431948","indexId":"ha155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"155","title":"Availability of ground water in the parts of the Little Cypress and Calvert City quadrangles in the Jackson Purchase region, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha155","usgsCitation":"Morgan, J.H., 1965, Availability of ground water in the parts of the Little Cypress and Calvert City quadrangles in the Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 155, 1 Plate: 39.50 × 44.25 inches, https://doi.org/10.3133/ha155.","productDescription":"1 Plate: 39.50 × 44.25 inches","costCenters":[],"links":[{"id":188910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409747,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15515.htm","linkFileType":{"id":5,"text":"html"}},{"id":89454,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/155/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Little Cypress and Calvert City quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.5,\n 37\n ],\n [\n -88.5,\n 37.064\n ],\n [\n -88.25,\n 37.064\n ],\n [\n -88.25,\n 37\n ],\n [\n -88.5,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8bc","contributors":{"authors":[{"text":"Morgan, J. H.","contributorId":9243,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52503,"text":"ofr65151 - 1965 - Water resources appraisal of the Anchorage area, Alaska","interactions":[],"lastModifiedDate":"2023-10-20T20:27:13.82275","indexId":"ofr65151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-151","title":"Water resources appraisal of the Anchorage area, Alaska","docAbstract":"At the present, water use in the Anchorage area amounts to about 21 mgd (million gallons per day); of this amount ground water accounts for about 10 mgd. By 1980, 60 mgd may be required to meet the demand.
The greatest potential problem is overpumping the ground-water reservoir resulting in excessive declines in water levels, which, in turn, might lead to salt-water intrusion. A well-laid plan for conjunctive use of surface and ground water seems to be the most promising means of supplying the expected need of 60 mgd, and of preventing saltwater intrusion of the aquifers.
Total inflow into the Anchorage hydrologic system amounts to about 180 mgd. Of this amount Ship and South Fork Campbell Creeks contribute about 130 mgd, North Fork Campbell Creek and other streams contribute an estimated 24 mgd, and precipitation and ground-water inflow contribute an estimated 26 mgd.
Of the total outflow, which must be equivalent to the inflow, Ship and Chester Creeks contribute about 94 mgd, Campbell Creek about 25 mgd, and ground-water pumpage contributes an assumed amount of approximately 10 mgd. The difference of 50 mgd between inflow and outflow presumably is accounted for; by submarine discharge beneath Cook Inlet and evapotranspiration.
Surface and subsurface storage of excess stream discharge during periods of high flow can overcome the problem of water shortages during periods of greatest demand. Surface storage can be accomplished by construction of an additional dam on Ship Creek. Natural ground-water storage can be supplemented by spreading techniques to increase the amount of ground-water recharge. Additional recharge can be provided by returning air-conditioning water to the aquifer through recharge wells. Recharge along the coastline would be a means of maintaining a fresh-water barrier against salt-water intrusion.
The area with the greatest potential for ground-water development is along Ship Creek east and north of Mountain View. The alluvial fan east of Mountain View seems favorable for installation of deep wells; and withdrawal of ground water in this area is not likely to result in salt-water intrusion. Similar favorable conditions exist in the alluvial fan areas of North and South Forks Campbell Creek. Infiltration galleries in alluvial deposits along Ship Creek are a relatively inexpensive and convenient means of withdrawing water.
To plan for orderly and economical development of the Anchorage area's water resources, geologic and hydrologic studies are needed. An expanded network of stream-gaging stations and observation wells is needed. Deep wells near the coastline are needed to monitor any changes in chemical quality of ground water that would indicate impending salt-water intrusion. Borehole geophysical studies and pumping tests are needed to define the boundaries and hydraulic characteristics of the aquifers. The primary goal of these and other supplementing studies would be to provide the information needed to construct an electric-analog model of the Anchorage hydrologic system. Such a model would provide a means of assessing quantitatively alternative methods of water development.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65151","usgsCitation":"Sommers, D.A., and Marcher, M.V., 1965, Water resources appraisal of the Anchorage area, Alaska: U.S. Geological Survey Open-File Report 65-151, 34 p., https://doi.org/10.3133/ofr65151.","productDescription":"34 p.","costCenters":[],"links":[{"id":422019,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0151/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -150.0148756092472,\n 61.267767521656054\n ],\n [\n -150.0148756092472,\n 61.119542274353336\n ],\n [\n -149.69627209362233,\n 61.119542274353336\n ],\n [\n -149.69627209362233,\n 61.267767521656054\n ],\n [\n -150.0148756092472,\n 61.267767521656054\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8302","contributors":{"authors":[{"text":"Sommers, David A.","contributorId":96761,"corporation":false,"usgs":true,"family":"Sommers","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":245454,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52491,"text":"ofr65125 - 1965 - Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts","interactions":[],"lastModifiedDate":"2019-06-04T14:52:43","indexId":"ofr65125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-125","title":"Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts","docAbstract":"The Assabet River, located in Worcester and Middlesex Counties in eastern Massachusetts, drains an area of approximately 177 square miles. The area includes all or a portion of the following towns: Acton, Boxborough, Carlisle, Concord, Hudson, Littleton, Marlborough, Maynard, Stow, Sudbury, and Westford in Middlesex County; Berlin, Bolton, Boylston, Clinton, Grafton, Harvard, Northborough, Shrewsbury, and Westborough in Worcester County (see plate 1 in pocket).
This report presents data collected as part of an investigation of the ground-water resources in the Assabet River basin by the U.S. Geological Survey in cooperation with the Massachusetts Water Resources Commission. The data have been prepared for release in order to make available to the public basic ground-water data that will be useful in the planning of water-resources development.
The data in this report were collected intermittently from 1939 to 1964 by H. A. Wilde, H. L. Pree, H. N. Halberg, J. A. Baker, R. W. Macomber, W. B. Fleck, and S. J. Pollock. The selected data in tables 2, 3, 4, and 5 represent those wells, test wells, and borings that were deemed representative of any given location. Data of some one hundred wells and test wells and over one thousand bridge and roadway borings are not included in this report, but may be inspected at the U.S. Geological Survey, Ground Water Branch, 211 Congress Street, Boston, Massachusetts. Tables 6-9 include data on chemical analyses of water samples, physical and hydrologic properties of materials samples, and water-table measurements made during the years 1961 through 1964. The geologic units used in tables 2 and 3 are described in table 1.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65125","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Pollock, S., and Fleck, W.B., 1965, Records of wells and test holes, materials tests, and chemical analyses of water in the Assabet River basin, Massachusetts: U.S. Geological Survey Open-File Report 65-125, Report: 45 p.; 1 Plate: 41.16 x 54.13 inches, https://doi.org/10.3133/ofr65125.","productDescription":"Report: 45 p.; 1 Plate: 41.16 x 54.13 inches","costCenters":[],"links":[{"id":364337,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364338,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0125/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0125/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","otherGeospatial":"Assabet River basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635624","contributors":{"authors":[{"text":"Pollock, Samuel J.","contributorId":27555,"corporation":false,"usgs":true,"family":"Pollock","given":"Samuel J.","affiliations":[],"preferred":false,"id":245432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":245431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52470,"text":"ofr6568 - 1965 - Description and analysis of the geohydrologic system in western Pinal County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:23","indexId":"ofr6568","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-68","title":"Description and analysis of the geohydrologic system in western Pinal County, Arizona","docAbstract":"Western Pinal County is between Phoenix and Tucson in the Basin and Range physiographic province of southern Arizona and consists of about 2,000 square miles of valley floor with low relief surrounded by mountains. It is the second largest agricultural area in the State, and about 25 percent of the ground water pumped in the State is from this area. \r\n\r\nThe study area has been divided into four parts. Three of these--the Casa Grande-Florence area, the Eloy area, and the Stanfield-Maricopa area--are in the lower Santa Cruz basin; the fourth--the Gila River area--is a long narrow strip along the Gila River from the Ashurst-Hayden Dam to the confluence of the Gila and Santa Cruz Rivers. The project was undertaken to provide a better understanding of the ground-water supply in relation to the present and potential water use in this area of extensive ground-water development. The arid climate of western Pinal County--combining high temperatures and low humidity--causes most of the precipitation to be returned to the atmosphere by evapotranspiration, which leaves only a very small part for recharge to the ground-water reservoir. The computed potential evapotranspiration--44. 97 inches--is five times greater than the average precipitation. \r\n\r\nIn general, the subsurface materials in western Pinal County are unconsolidated alluvial deposits underlain by consolidated alluvium and crystalline rocks and bounded by mountains consisting of crystalline and minor sedimentary rocks. The crystalline and sedimentary rocks of the mountains are not known to be water bearing in western Pinal County. The impermeable rocks underlying the basin are called the hydrologic bedrock unit in this report. Although the unit may consist of several different rock types, the distinction between them is relatively unimportant in this study because none of them yield appreciable amounts of water. The lower Santa Cruz basin in western Pinal County is divided into two sections by a buried ridge of the hydrologic bedrock unit, referred to in this report as the Casa Grande ridge. The ridge trends in a north-south direction from the Sacaton to the Silver Reef Mountains. \r\n\r\nThe unconsolidated deposits constitute the main storage reservoir for ground water in western Pins/ County. The deposits are divided into four units---the local gravel unit, the lower sand and gravel unit, the silt and clay unit, and the upper sand and gravel unit--all of which are major water-yielding units except the silt and clay unit. The local gravel unit, which is present only in the western section of the lower Santa Cruz basin, ranges in thickness from 0 to nearly 1,000 feet and is generally a productive aquifer. The lower sand and gravel unit, Which is a heterogeneous mixture of sand, gravel, and clay, ranges in thickness from 0 to about 500 feet. Where the lower sand and gravel unit is overlain by the silt and clay unit, it generally contains water under artesian conditions; where it is not overlain by the silt and clay unit, it is indistinguishable from the upper sand and gravel unit, and the water is under water-table conditions. The silt and clay unit is the least permeable deposit of the unconsolidated alluvium, and ranges in thickness from 0 to about 2, 000 feet. Generally it is less productive than the other units of the unconsolidated alluvium, although it yields moderate amounts of water from numerous thin stringers and lenses of highly permeable sand and gravel. The upper sand and gravel unit is at the land surface in most of the area; it ranges in thickness from less than 50 to about 600 feet. The unit has the highest average permeability of all the unconsolidated alluvial units; however, the permeability of the unit varies vertically and laterally, which results in a wide range of well yields. As of 1964, the static water levels in most wells in the basin were still in the upper sand and gravel unit. However, the unit is being dewatered in most of the basin, and water levels in","language":"ENGLISH","doi":"10.3133/ofr6568","usgsCitation":"Hardt, W.F., and Cattany, R., 1965, Description and analysis of the geohydrologic system in western Pinal County, Arizona: U.S. Geological Survey Open-File Report 65-68, 111 p., https://doi.org/10.3133/ofr6568.","productDescription":"111 p.","costCenters":[],"links":[{"id":179267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0068/report-thumb.jpg"},{"id":86900,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86901,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86902,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86903,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86904,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86905,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86906,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86907,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86908,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86909,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86910,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86911,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86912,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86913,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86914,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86915,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86916,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86917,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86918,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86919,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86920,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86921,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0068/plate-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86922,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dce1","contributors":{"authors":[{"text":"Hardt, W. 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H.","contributorId":9243,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68148,"text":"ha163 - 1965 - Availability of ground water in the Hickory quadrangle, Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"163","title":"Availability of ground water in the Hickory quadrangle, Jackson Purchase region, Kentucky","language":"ENGLISH","doi":"10.3133/ha163","usgsCitation":"Morgan, J.H., 1965, Availability of ground water in the Hickory quadrangle, Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 163, 1 map., https://doi.org/10.3133/ha163.","productDescription":"1 map.","costCenters":[],"links":[{"id":186458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/163/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.75,36.75 ], [ -88.75,36.8675 ], [ -88.61749999999999,36.8675 ], [ -88.61749999999999,36.75 ], [ -88.75,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d939","contributors":{"authors":[{"text":"Morgan, J. H.","contributorId":9243,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277730,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52469,"text":"ofr6563 - 1965 - Summary of ground-water conditions in Michigan in 1964","interactions":[],"lastModifiedDate":"2017-07-12T10:35:03","indexId":"ofr6563","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-63","title":"Summary of ground-water conditions in Michigan in 1964","docAbstract":"The purpose of this report is to make available records of groundwater level changes in the principal aquifers of the State during 1964 and compile other related data, such as ground-water pumpage, data on municipal, public and industrial water supply facilities, and the effects of precipitation on ground-water levels. Records of water level changes in areas of heavy pumpage and in areas where changes are principally from natural influences are illustrated or tabulated (table 2) to allow comparison between these two types of water-level fluctuations. The water-level and related data prOvide a day-to-day evaluation of available ground-water supplies. These long-term records serve as a framework to which many short-term records collected during an intensive investigation may be related.
This report is written for those persons, municipalities, industries, institutions, consultants, drillers and hydrologists interested in the_groundwater resources of the State.
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