{"pageNumber":"6666","pageRowStart":"166625","pageSize":"25","recordCount":184900,"records":[{"id":70197609,"text":"70197609 - 1964 - Specific yield - laboratory experiments showing the effect of time on column drainage","interactions":[],"lastModifiedDate":"2022-05-25T18:43:50.318517","indexId":"70197609","displayToPublicDate":"1999-12-27T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Specific yield - laboratory experiments showing the effect of time on column drainage","docAbstract":"<p>The increasing use of ground water from many major aquifers in the United States has required a more thorough understanding of gravity drainage, or specific yield. This report describes one phase of specific yield research by the U.S. Geological Survey's Hydrologic Laboratory in cooperation with the California Department of Water Resources.</p><p>An earlier phase of the research concentrated on the final distribution of moisture retained after drainage of saturated columns of porous media. This report presents the phase that concentrated on the distribution of moisture retained in similar columns after drainage for various periods of time.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70197609","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Prill, R., Johnson, A., and Morris, D.A., 1964, Specific yield - laboratory experiments showing the effect of time on column drainage: Open-File Report, iv, 55 p., https://doi.org/10.3133/70197609.","productDescription":"iv, 55 p.","costCenters":[],"links":[{"id":401064,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70197609/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":355004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70197609/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Prill, R.C.","contributorId":27034,"corporation":false,"usgs":true,"family":"Prill","given":"R.C.","affiliations":[],"preferred":false,"id":737898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":737899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":737900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70189329,"text":"70189329 - 1964 - Water quality of the Swatara Creek Basin, PA","interactions":[],"lastModifiedDate":"2017-07-12T14:56:41","indexId":"70189329","displayToPublicDate":"1999-12-26T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Water quality of the Swatara Creek Basin, PA","docAbstract":"<p>The Swatara Creek of the Susquehanna River Basin is the farthest downstream sub-basin that drains acid water (pH of 4.5 or less) from anthracite coal mines. The Swatara Creek drainage area includes 567 square miles of parts of Schuylkill, Berks, Lebanon, and Dauphin Counties in Pennsylvania.</p><p>To learn what environmental factors and dissolved constituents in water were influencing the quality of Swatara Creek, a reconnaissance of the basin was begun during the summer of 1958. Most of the surface streams and the wells adjacent to the principal tributaries of the Creek were sampled for chemical analysis. Effluents from aquifers underlying the basin were chemically analyzed because ground water is the basic source of supply to surface streams in the Swatara Creek basin. When there is little runoff during droughts, ground water has a dominating influence on the quality of surface water. Field tests showed that all ground water in the basin was non-acidic. However, several streams were acidic. Sources of acidity in these streams were traced to the overflow of impounded water in unworked coal mines.</p><p>Acidic mine effluents and washings from coal breakers were detected downstream in Swatara Creek as far as Harper Tavern, although the pH at Harper Tavern infrequently went below 6.0. Suspended-sediment sampling at this location showed the mean daily concentration ranged from 2 to 500 ppm. The concentration of suspended sediment is influenced by runoff and land use, and at Harper Tavern it consisted of natural sediments and coal wastes. The average daily suspended-sediment discharge there during the period May 8 to September 30, 1959, was 109 tons per day, and the computed annual suspended-sediment load, 450 tons per square mile. </p><p>Only moderate treatment would be required to restore the quality of Swatara Creek at Harper Tavern for many uses. Above Ravine, however, the quality of the Creek is generally acidic and, therefore, of limited usefulness to public supplies, industries and recreation. </p><p>In general, the quality of Swatara Creek improves after it mixes with water from the Upper Little and Lower Little Swatara Creeks, which converge with the main stream near Pine Grove. Jonestown is the first downstream location where Swatara Creek contains bicarbonate ion most of the time, and for the remaining downstream length of the stream, the concentration of bicarbonate progressively increases. Before the stream enters the Susquehanna River, chemical and diluting processes contributed by tributaries change the acidic calcium sulfate water, which characterizes the upper Swatara, to a calcium bicarbonate water.</p><p>A major tributary to Swatara Creek is Quittapahilla Creek, which drains a limestone region and has alkaline characteristics. Effluents from a sewage treatment plant are discharged into this stream west of Lebanon. Adjacent to the Creek are limestone quarries and during the recovery of limestone, ground water seeps into the mining areas. This water is pumped to upper levels and flows over the land surface into Quittapahilla Creek. </p><p>As compared with the 1940's, the quality of Swatara Creek is better today, and the water is suitable for more uses. In large part, this improvement is due to curtailment of anthracite coal mining and because of the controls imposed on new mines, stripping mines, and the related coal mining operations, by the Pennsylvania Sanitary Water Board. Thus, today (1962) smaller amounts of coal mine wastes are more effectively flushed and scoured away with each successive runoff during storms that affect the drainage basin. Natural processes neutralizing acid water in the stream by infiltration of alkaline ground water through springs and through the streambed are also indicated. </p>","language":"English","publisher":" U.S. Geological Survey","doi":"10.3133/70189329","collaboration":"Prepared in cooperation with the Pennsylvania Department of Forests and Waters","usgsCitation":"McCarren, E.F., Wark, J., and George, J., 1964, Water quality of the Swatara Creek Basin, PA: Open-File Report, 88 p., https://doi.org/10.3133/70189329.","productDescription":"88 p.","costCenters":[],"links":[{"id":343575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70189329/report-thumb.jpg"},{"id":343749,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70189329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Swatara Creek Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.80841064453125,\n              41.03585891144301\n            ],\n            [\n              -75.82763671875,\n              41.03378713521864\n            ],\n            [\n              -76.102294921875,\n              41.02964338716638\n            ],\n            [\n              -76.70379638671874,\n              40.84498264925404\n            ],\n            [\n              -76.81915283203125,\n              40.670222795307346\n            ],\n            [\n              -76.84661865234375,\n              40.54511315470123\n            ],\n            [\n              -76.89605712890625,\n              40.287906612507406\n            ],\n            [\n              -76.871337890625,\n              40.18516846826054\n            ],\n            [\n              -76.73126220703125,\n              40.13899044275822\n            ],\n            [\n              -76.6790771484375,\n              40.11799004890473\n            ],\n            [\n              -75.948486328125,\n              40.21873275657034\n            ],\n            [\n              -75.73699951171875,\n              40.30466538259176\n            ],\n            [\n              -75.5859375,\n              40.48455955508278\n            ],\n            [\n              -75.62164306640625,\n              40.65563874006118\n            ],\n            [\n              -75.65185546874999,\n              40.83874913796459\n            ],\n            [\n              -75.74249267578125,\n              40.96952973563832\n            ],\n            [\n              -75.80841064453125,\n              41.03585891144301\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5965e3afe4b0d1f9f05c1d98","contributors":{"authors":[{"text":"McCarren, Edward F.","contributorId":106472,"corporation":false,"usgs":true,"family":"McCarren","given":"Edward","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":704194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wark, J.W.","contributorId":194454,"corporation":false,"usgs":false,"family":"Wark","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":704195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"George, J.R.","contributorId":15277,"corporation":false,"usgs":true,"family":"George","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":704196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62847,"text":"gq351 - 1964 - Geology of the Mammoth Cave quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq351","displayToPublicDate":"1995-06-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"351","title":"Geology of the Mammoth Cave quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq351","usgsCitation":"Haynes, D., 1964, Geology of the Mammoth Cave quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 351, 1 map :col. ;58 x 46 cm., on sheet 77 x 87 cm., folded in envelope 30 x 24 cm.; Reprinted in 1995, https://doi.org/10.3133/gq351.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 77 x 87 cm., folded in envelope 30 x 24 cm.; Reprinted in 1995","costCenters":[],"links":[{"id":102363,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_812.htm","linkFileType":{"id":5,"text":"html"},"description":"812"},{"id":180607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0351/report-thumb.jpg"},{"id":89027,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0351/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.11749999999999,37.1175 ], [ -86.11749999999999,37.25 ], [ -86,37.25 ], [ -86,37.1175 ], [ -86.11749999999999,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea6a","contributors":{"authors":[{"text":"Haynes, Donald D.","contributorId":78400,"corporation":false,"usgs":true,"family":"Haynes","given":"Donald D.","affiliations":[],"preferred":false,"id":267952,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13372,"text":"ofr708 - 1964 - Measurement of the remanent magnetization of igneous rocks","interactions":[],"lastModifiedDate":"2012-04-15T17:28:15","indexId":"ofr708","displayToPublicDate":"1994-01-01T17:27:00","publicationYear":"1964","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":"708","title":"Measurement of the remanent magnetization of igneous rocks","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr708","usgsCitation":"Doell, R.R., and Cox, A., 1964, Measurement of the remanent magnetization of igneous rocks: U.S. Geological Survey Open-File Report 708, iii, 51 p. :ill. ;27 cm., https://doi.org/10.3133/ofr708.","productDescription":"iii, 51 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":258467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/708/report.pdf","size":"3762","linkFileType":{"id":1,"text":"pdf"}},{"id":258468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/708/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f5d3","contributors":{"authors":[{"text":"Doell, Richard Rayman","contributorId":59089,"corporation":false,"usgs":true,"family":"Doell","given":"Richard","email":"","middleInitial":"Rayman","affiliations":[],"preferred":false,"id":167696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Allan","contributorId":89949,"corporation":false,"usgs":true,"family":"Cox","given":"Allan","email":"","affiliations":[],"preferred":false,"id":167697,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5828,"text":"pp454J - 1964 - Geology of Bullfrog quadrangle and ore deposits related to Bullfrog Hills caldera, Nye County, Nevada, and Inyo County, California","interactions":[],"lastModifiedDate":"2026-02-18T21:05:43.349025","indexId":"pp454J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"454","chapter":"J","title":"Geology of Bullfrog quadrangle and ore deposits related to Bullfrog Hills caldera, Nye County, Nevada, and Inyo County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp454J","usgsCitation":"Cornwall, H.R., and Kleinhampl, F., 1964, Geology of Bullfrog quadrangle and ore deposits related to Bullfrog Hills caldera, Nye County, Nevada, and Inyo County, California: U.S. Geological Survey Professional Paper 454, Report: iv, 25 p.; 10 Plates: 38.00 × 19.00 inches or smaller, https://doi.org/10.3133/pp454J.","productDescription":"Report: iv, 25 p.; 10 Plates: 38.00 × 19.00 inches or smaller","costCenters":[],"links":[{"id":104462,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4458.htm","linkFileType":{"id":5,"text":"html"},"description":"4458"},{"id":32527,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32528,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32529,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32537,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0454j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121678,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0454j/report-thumb.jpg"},{"id":32530,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32531,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32532,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32533,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32534,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32535,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32536,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0454j/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","county":"Inyo County, Nye County","otherGeospatial":"Bullfrog quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117,\n              36.75\n            ],\n            [\n              -116.75,\n              36.75\n            ],\n            [\n              -116.75,\n              37\n            ],\n            [\n              -117,\n              37\n            ],\n            [\n              -117,\n              36.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683fec","contributors":{"authors":[{"text":"Cornwall, Henry Rowland","contributorId":68304,"corporation":false,"usgs":true,"family":"Cornwall","given":"Henry","email":"","middleInitial":"Rowland","affiliations":[],"preferred":false,"id":151640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinhampl, Frank J.","contributorId":105297,"corporation":false,"usgs":true,"family":"Kleinhampl","given":"Frank J.","affiliations":[],"preferred":false,"id":151641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":37128,"text":"rr66 - 1964 - Effects of accumulated excretory products on hatchery-reared salmonids:","interactions":[],"lastModifiedDate":"2012-02-02T00:09:52","indexId":"rr66","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"66","title":"Effects of accumulated excretory products on hatchery-reared salmonids:","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Burrows, R., 1964, Effects of accumulated excretory products on hatchery-reared salmonids:: Research Report 66, 12 p.","productDescription":"12 p.","costCenters":[],"links":[{"id":94584,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009784562?urlappend=%3Bseq=59"},{"id":165095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624d6c","contributors":{"authors":[{"text":"Burrows, R.E.","contributorId":59497,"corporation":false,"usgs":true,"family":"Burrows","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":217531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":35033,"text":"b1171 - 1964 - Hawaiian volcanoes during 1955","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"b1171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1171","title":"Hawaiian volcanoes during 1955","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1171","usgsCitation":"Macdonald, G.A., and Eaton, J.P., 1964, Hawaiian volcanoes during 1955: U.S. Geological Survey Bulletin 1171, vi, 170 p. :ill., maps ;24 cm., https://doi.org/10.3133/b1171.","productDescription":"vi, 170 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":93044,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1171/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93045,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1171/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93046,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1171/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93047,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1171/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93048,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1171/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1171/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1171/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d71a","contributors":{"authors":[{"text":"Macdonald, G. A.","contributorId":86824,"corporation":false,"usgs":true,"family":"Macdonald","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214014,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":214015,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2114,"text":"wsp1619X - 1964 - Geology and ground-water resources of Rock County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T14:37:26","indexId":"wsp1619X","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","chapter":"X","title":"Geology and ground-water resources of Rock County, Wisconsin","docAbstract":"<p>Rock County is in south-central Wisconsin adjacent to the Illinois State line. The county has an area of about 723 square miles and had a population of about 113,000 in 1957 ; it is one of the leading agricultural and industrial counties in the State. The total annual precipitation averages about 32 inches, and the mean annual temperature is about 48 ? F. Land-surface altitudes are generally between 800 and 00 feet, but range from 731 feet, where the Rock River flows into Illinois, to above 1,080 feet, at several places in the northwestern part of the county. The northern part of Rock County consists of the hills and kettles of a terminal moraine which slopes southward to a flat, undissected outwash plain. The southeastern part of the county is an area of gentle slopes, whereas the southwestern part consists of steep-sided valleys and ridges. Rock County is within the drainage basin of the Rock River, which flows southward through the center of the county. The western and southwestern parts of ,the county are drained by the Sugar River und Coon Creek, both of which flow into the Pecatonica River in Illinois and thence into the Rock River. The southeastern part of the county is drained by Turtle Creek, which also flows into Illinois before joining the Rock River. Nearly all the lakes and ponds are in the northern one-third of the county, the area of most recent glaciation. The aquifers in Rock County are of sedimentary origin and include deeply buried sandstones, shales, and dolomites of the Upper Cambrian series. This series overlies crystalline rocks of Precambrian age and supplies water to all the cities and villages in the county. The St. Peter sandstone of Ordovician age underlies all Rock County except where the formation has been removed by erosion in the Rock and Sugar River valleys, and perhaps in Coon Creek valley. The St. Peter sandstone is the principal source of water for domestic, stock, and small industrial wells in the western half of the county. This sandstone also yields some water to uncased wells that tap the deeper rocks of the Upper Cambrian series. East of the Rock River the Platteville, Decorah, and Galena formations undifferentiated, or Platteville-Galena unit, is the principal source of water for domestic and stock wells. Unconsolidated deposits of glacial origin cover most of Rock County and supply water to many small wells. In the outwash deposits along the Rock River, wells of extremely high capacity have been developed for industrial and municipal use. The most significant feature of the bedrock surface in Rock County is the ancestral Rock River valley, which has been filled with glacial outwash to a depth of at least 396 feet below the present land surface. East of the buried valley the bedrock has a fiat, relatively undissected surface. West of the valley the bedrock surface is rugged and greatly dissected. Ground water in Rock County occurs under both water-table and artesian conditions; however, because of the interconnection and close relation of all ground water in the county, the entire system is considered to be a single groundwater body whose surface may be represented by one piezometric map. Recharge occurs locally, throughout the county. Nearly all recharge is derived directly from precipitation that percolates downward to become a part of the groundwater body. Natural movement of water in the consolidated water-bearing units is generally toward the buried Rock and Sugar River valleys. Movement of water in the sandstones of Cambrian age was calculated to be about 44 million gallons a day toward the Rock River. Discharge from wells in Rock County in 1957 was about 23 million gallons a day. Nearly 90 percent of this water was drawn from the area along the Rock River. Drilled wells, most of which were drilled by the cable-tool method, range in diameter from 3 to 26 inches, and in depth from 46 to 1,225 feet. 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