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,{"id":47079,"text":"ofr6470 - 1964 - Geologic map of the Mud Springs quadrangle, Carbon and Natrona Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:24","indexId":"ofr6470","displayToPublicDate":"1994-01-01T00:00:00","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":"64-70","title":"Geologic map of the Mud Springs quadrangle, Carbon and Natrona Counties, Wyoming","language":"ENGLISH","doi":"10.3133/ofr6470","usgsCitation":"Harshman, E., 1964, Geologic map of the Mud Springs quadrangle, Carbon and Natrona Counties, Wyoming: U.S. Geological Survey Open-File Report 64-70, 1 map, https://doi.org/10.3133/ofr6470.","productDescription":"1 map","costCenters":[],"links":[{"id":106343,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8068.htm","linkFileType":{"id":5,"text":"html"},"description":"8068"},{"id":170246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84051,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0070/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6963ad","contributors":{"authors":[{"text":"Harshman, E.N.","contributorId":84827,"corporation":false,"usgs":true,"family":"Harshman","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":234601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16451,"text":"ofr64161 - 1964 - Seismic refraction survey in the Great Miami River Valley and vicinity, Montgomery, Warren, and Butler Counties, Ohio","interactions":[],"lastModifiedDate":"2025-07-24T16:32:53.565544","indexId":"ofr64161","displayToPublicDate":"1994-01-01T00:00:00","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":"64-161","title":"Seismic refraction survey in the Great Miami River Valley and vicinity, Montgomery, Warren, and Butler Counties, Ohio","docAbstract":"<p>As part of a continuing program to define the thickness and extent of water-bearing sand and gravel deposits in southwestern Ohio, the U.S. Geological Survey, in cooperation with the Ohio Division of Water and The Miami Conservancy District, completed a seismic refraction survey of the Great Miami River valley and adjacent areas between Dayton and Hamilton, Ohio, in the fall of 1963. A similar survey of the adjoining lower Great Miami River and Whitewater River valleys was completed in 1962 (Watkins, 1963; Spieker and Watkins, unpublished data).</p><p>The area of the survey includes known or inferred portions of an interglacial drainage system which is deeply entrenched into bedrock. Ohio was covered by glaciers at least three times during the Pleistocene epoch. As each glacier melted, rock fragments absorbed by the glacier were transported and deposited in these buried valleys by torrents of meltwater. The total thickness of glacial drift is over 300 feet in some places. </p><p>Much of the glacial material is highly permeable and saturated with large quantities of water of good quality. The underlying bedrock is virtually impermeable and yields only meager quantities of water. The cities of Dayton, Middletown, Hamilton, and many industries in the Miami River valley rely on wells in the glacial deposits as their principal source of water. The purpose of the present survey is to define the thickness and extent of these important water-bearing formations. Such information will make possible a more accurate evaluation of the area's water resources than has previously have been possible.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbus, OH","doi":"10.3133/ofr64161","usgsCitation":"Watkins, J.S., and Spieker, A.M., 1964, Seismic refraction survey in the Great Miami River Valley and vicinity, Montgomery, Warren, and Butler Counties, Ohio: U.S. Geological Survey Open-File Report 64-161, Report: iii, 6 p.; 3 Figures: 20.02 x 26.16 inches or smaller, https://doi.org/10.3133/ofr64161.","productDescription":"Report: iii, 6 p.; 3 Figures: 20.02 x 26.16 inches or smaller","numberOfPages":"21","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":330795,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0161/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330794,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0161/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330793,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0161/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330792,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0161/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148595,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":492836,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8056.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","county":"Butler County, Montgomery County, Warren County","otherGeospatial":"Great Miami River Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.3529,39.2916],[-84.3881,39.2969],[-84.4292,39.2981],[-84.4358,39.2994],[-84.4644,39.3026],[-84.4834,39.3009],[-84.5049,39.306],[-84.5239,39.303],[-84.5633,39.3082],[-84.599,39.3085],[-84.6306,39.3121],[-84.6376,39.3092],[-84.6417,39.3051],[-84.7029,39.3049],[-84.8191,39.3056],[-84.8186,39.3531],[-84.8181,39.3673],[-84.8166,39.4134],[-84.8159,39.4692],[-84.8154,39.5218],[-84.8154,39.5296],[-84.815,39.5677],[-84.7026,39.5675],[-84.591,39.5676],[-84.4788,39.5685],[-84.4788,39.5898],[-84.4806,39.6573],[-84.4818,39.7448],[-84.4836,39.8305],[-84.4854,39.9184],[-84.4261,39.9193],[-84.3691,39.9207],[-84.3008,39.9217],[-84.2558,39.9218],[-84.1629,39.9226],[-84.1646,39.895],[-84.1656,39.8859],[-84.051,39.8801],[-84.0539,39.8501],[-84.055,39.8424],[-84.0554,39.8361],[-84.0602,39.8365],[-84.0926,39.8379],[-84.097,39.7938],[-84.0989,39.7725],[-84.0994,39.7657],[-84.1052,39.7039],[-84.1119,39.6282],[-84.1118,39.6263],[-84.1094,39.6259],[-84.1137,39.5778],[-84.03,39.5725],[-83.9769,39.5691],[-83.9798,39.5396],[-83.9813,39.5264],[-83.9818,39.5187],[-83.9838,39.5001],[-84.0004,39.3249],[-84.0067,39.2554],[-84.2602,39.2703],[-84.2573,39.2735],[-84.2574,39.2775],[-84.2604,39.2789],[-84.2652,39.2802],[-84.2659,39.2829],[-84.2624,39.2883],[-84.3339,39.2932],[-84.3529,39.2916]]]},\"properties\":{\"name\":\"Butler\",\"state\":\"OH\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb686","contributors":{"authors":[{"text":"Watkins, Joel S.","contributorId":10788,"corporation":false,"usgs":true,"family":"Watkins","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":172872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spieker, Andrew M.","contributorId":41492,"corporation":false,"usgs":true,"family":"Spieker","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":172873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16450,"text":"ofr64160 - 1964 - Refraction seismic survey of parts of the Little Miami River and Scioto River valleys, Ohio","interactions":[],"lastModifiedDate":"2025-06-12T15:04:56.642705","indexId":"ofr64160","displayToPublicDate":"1994-01-01T00:00:00","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":"64-160","title":"Refraction seismic survey of parts of the Little Miami River and Scioto River valleys, Ohio","docAbstract":"<p>The U. S. Geological Survey and the Ohio Division of Water conducted a refraction seismic survey of the Little Miami River valley near Xenia, Ohio, and the Scioto River valley between Columbus and Chillicothe, Ohio, in the fall of 1963.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64160","usgsCitation":"Watkins, J.S., and Bailey, N.G., 1964, Refraction seismic survey of parts of the Little Miami River and Scioto River valleys, Ohio: U.S. Geological Survey Open-File Report 64-160, Report: 6 p.; 3 Plates: 8.76 x 14.07 inches or smaller, https://doi.org/10.3133/ofr64160.","productDescription":"Report: 6 p.; 3 Plates: 8.76 x 14.07 inches or 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6350bc","contributors":{"authors":[{"text":"Watkins, Joel S.","contributorId":10788,"corporation":false,"usgs":true,"family":"Watkins","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":172870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":172871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12938,"text":"ofr6433 - 1964 - Geology of the Andover Granite and surrounding rocks, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr6433","displayToPublicDate":"1994-01-01T00:00:00","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":"64-33","title":"Geology of the Andover Granite and surrounding rocks, Massachusetts","docAbstract":"Field and petrographic studies of the Andover Granite and surrounding rocks have afforded an opportunity for an explanation of its emplacement and crystallization. The investigation has contributed secondarily to an understanding of the geologic history of southeastern New England, particularly as it is revealed in the Lawrence, Wilmington, South Groveland, and Reading quadrangles of Massachusetts. \r\n\r\nThe Andover Granite and Sharpners Pond Tonalite together comprise up to 90 percent of the Acadian(?) subalkaline intrusive series cropping out within the area of study. The subalkaline series locally invades a sequence of early to middle Paleozoic and possibly Precambrian metasedimentary and metavolcanic rocks. Much of the subalkaline series and most of the Andover Granite is confined between two prominent east-northeast trending faults or fault systems. The northern fault separates the mildly metamorphosed Middle Silurian(?) Merrimack Group on the north from a highly metamorphosed and thoroughly intruded Ordovician(?) sequence on the south. The southern 'boundary '' fault is a major structural discontinuity characterized by penetrative, diffuse shearing over a zone one-half mile or more in width. \r\n\r\nThe magmatic nature of the Andover Granite is demonstrated by: (1) sharply crosscutting relationships with surrounding rocks; (2) the occurrence of tabular-shaped xenoliths whose long directions parallel the foliation within the granite and whose internal foliation trends at a high angle to that of the granite; (3) continuity with the clearly intrusive Sharpners Pond Tonalite; (4) the compositional uniformity of the granite as contrasted with the compositional diversity of the rocks it invades; (5) its modal and normative correspondence with (a) calculated norms of salic extrusives and (b) that of the ternary (\u001Cgranite\u001D) minimum for the system NaAlSi3O8-KAlSi3O8-SiO2. \r\n\r\nOrogenic granites, as represented by the Andover, contrast with post-orogenic granites, represented locally by the Peabody Granite, in their phase composition and texture. Unlike the Peabody, the Andover Granite is thought to have been thoroughly recrystallized through the unmixing of initially homogeneous phases with the concomitant development of extremely intricate, allotriomorphic textures. Textural relationships between potassium and plagioclase feldspars and among quartz and the two feldspars, suggest that the Andover Granite has evolved through exsolution of a single hypersolvus feldspar (or two coexisting subsolvus feldspars of only slightly disparate compositions) into discrete grains of plagioclase and potassium feldspar, much along the lines proposed by Tuttle (1952). \r\n\r\nA hypothesis is proposed for the origin of myrmekite whereby it is evolved indirectly through exsolution of a homogeneous, hypersolvus, calcalkali feldspar in the presence of a silica reservoir. Where the An 'molecule' is contained in the primary mix crystal, exsolution into potassium and plagioclase feldspar phases normally requires a paired exchange between Ca-Al and K-Si. Should the silicon requirements of the developing potassium feldspar be met by the matrix silica reservoir, the concomitantly evolving plagioclase may become stoichiometrically enriched in silicon and ultimately develop into myrmekite. Discrete unmixing of pure alkali feldspar proceeds through simple alkali ion exchange; ternary compostions high in An are more apt to fall initially in the two-feldspar field, thereby reducing the unmixing potential. General restriction of myrmekite to plagioclase of calcic albite to oligoclase composition is explained accordingly.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6433","usgsCitation":"Castle, R.O., 1964, Geology of the Andover Granite and surrounding rocks, Massachusetts: U.S. Geological Survey Open-File Report 64-33, 550 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr6433.","productDescription":"550 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":146979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0033/report-thumb.jpg"},{"id":41382,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41383,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41384,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41385,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41386,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41387,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41388,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41389,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41390,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0033/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68353e","contributors":{"authors":[{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":166992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35516,"text":"b1158D - 1964 - Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts","interactions":[{"subject":{"id":51927,"text":"ofr5697 - 1956 - Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts","indexId":"ofr5697","publicationYear":"1956","noYear":false,"title":"Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":35516,"text":"b1158D - 1964 - Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts","indexId":"b1158D","publicationYear":"1964","noYear":false,"chapter":"D","title":"Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts"},"id":1}],"lastModifiedDate":"2022-01-14T19:53:11.607447","indexId":"b1158D","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":"1158","chapter":"D","title":"Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of selected quadrangles in Rhode Island","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1158D","usgsCitation":"Pollock, S.J., 1964, Bedrock geology of the Tiverton quadrangle, Rhode Island-Massachusetts: U.S. Geological Survey Bulletin 1158, Report: 16 p.; 1 Plate: 26.00 × 29.25 inches, https://doi.org/10.3133/b1158D.","productDescription":"Report: 16 p.; 1 Plate: 26.00 × 29.25 inches","costCenters":[],"links":[{"id":109431,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20909.htm","linkFileType":{"id":5,"text":"html"},"description":"20909"},{"id":63424,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1158d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1158d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1158d/report-thumb.jpg"}],"country":"United States","state":"Massachusetts, Rhode Island","otherGeospatial":"Tiverton quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.25,\n              41.5\n            ],\n            [\n              -71.125,\n              41.5\n            ],\n            [\n              -71.125,\n              41.625\n            ],\n            [\n              -71.25,\n              41.625\n            ],\n            [\n              -71.25,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db633f85","contributors":{"authors":[{"text":"Pollock, Samuel Joseph","contributorId":69210,"corporation":false,"usgs":true,"family":"Pollock","given":"Samuel","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":214777,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35518,"text":"b1043E - 1964 - Recognition criteria of igneous and metamorphic rocks on aerial photographs of Chichagof and Kruzof Islands, southeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b1043E","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":"1043","chapter":"E","title":"Recognition criteria of igneous and metamorphic rocks on aerial photographs of Chichagof and Kruzof Islands, southeastern Alaska","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1043E","usgsCitation":"Pomeroy, J.S., 1964, Recognition criteria of igneous and metamorphic rocks on aerial photographs of Chichagof and Kruzof Islands, southeastern Alaska: U.S. Geological Survey Bulletin 1043, p. 87-110  plates. ;24 cm., https://doi.org/10.3133/b1043E.","productDescription":"p. 87-110  plates. ;24 cm.","costCenters":[],"links":[{"id":96952,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1043e/report.pdf","size":"6434","linkFileType":{"id":1,"text":"pdf"}},{"id":165803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1043e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64494c","contributors":{"authors":[{"text":"Pomeroy, John S.","contributorId":18329,"corporation":false,"usgs":true,"family":"Pomeroy","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":214780,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35069,"text":"b1161C - 1964 - Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1161C","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":"1161","chapter":"C","title":"Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1161C","usgsCitation":"Mapel, W.J., Chisholm, W.A., and Bergenback, R.E., 1964, Nonopaque heavy minerals in sandstone of Jurassic and Cretaceous age in the Black Hills, Wyoming and South Dakota: U.S. Geological Survey Bulletin 1161, p. C1-C59, ill., maps (2 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1161C.","productDescription":"p. C1-C59, ill., maps (2 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":166988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1161c/report-thumb.jpg"},{"id":63015,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1161c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63016,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1161c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1161c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e97","contributors":{"authors":[{"text":"Mapel, W. J.","contributorId":92225,"corporation":false,"usgs":true,"family":"Mapel","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":214067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chisholm, Wayne A.","contributorId":43343,"corporation":false,"usgs":true,"family":"Chisholm","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergenback, Richard E.","contributorId":65897,"corporation":false,"usgs":true,"family":"Bergenback","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":214066,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2983,"text":"wsp1499E - 1964 - Water resources of the Flint area, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T15:45:12","indexId":"wsp1499E","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":"1499","chapter":"E","title":"Water resources of the Flint area, Michigan","docAbstract":"<p>This report describes the water resources of Genesee County, Mich., whose principal city is Flint. The sources of water available to the county are the Flint and Shiawassee Rivers and their tributaries, inland lakes, ground water, and Lake Huron. The withdrawal use of water in the county in 1958 amounted to about 45 mgd. Of this amount, 36 mgd was withdrawn from the Flint River by the Flint public water-supply system. The rest was supplied by wells. At present (1959) the Shiawassee River and its tributaries and the inland lakes are not used for water supply.</p><p>&nbsp;Flint River water is used for domestic, industrial, and waste-dilution requirements in Flint. About 60 percent of the water supplied by the Flint public water system is used by Flint industry. At least 30 mgd of river water is needed for waste dilution in the Flint River during warm weather.</p><p>Water from Holloway Reservoir, which has a storage capacity of 5,760 million gallons, is used to supplement low flows in the Flint River to meet water-supply and waste-dilution requirements. About 650 million gallons in Kearsley Reservoir, on a Flint River tributary, is held in reserve for emergency use. Based on records for the lowest flows during the period 1930-52, the Flint River system, with the two reservoirs in operation, is capable of supplying about 60 mgd at Flint, less evaporation and seepage losses. The 1958 water demands exceeded this amount. Development of additional storage in the Flint River basin is unlikely because of lack of suitable storage sites. Plans are underway to supply Flint and most of Genesee County with water from Lake Huron.</p><p>The principal tributaries of the Flint River in and near Flint could furnish small supplies of water. Butternut Creek, with the largest flow of those studied, has an estimated firm yield of 0.054 mgd per sq mi for 95 percent of the time. The Shiawassee River at Byron is capable of supplying at least 29 mgd for 95 percent of the time.</p><p>Floods are a serious problem in Flint. The April 1947 flood, the largest on record, caused nearly $4 million flood damage in Flint. A proposed flood-control plan for Flint calls for channel, floodwall, and levee improvements and the removal or modification of some bridges.</p><p>Analyses of water samples taken from selected streams and lakes in the Flint area indicate that the waters are of the calcium bicarbonate type and generally hard to very hard. Flint River water is relatively uniform in quality although a progressive increase in iron, sodium, and chloride concentrations was noted between Otisville and Montrose. Downstream from Flint, the dissolved oxygen</p><p>content may be low during low flows. At times, concentrations of iron, manganese, phenols, color, and turbidity in Flint River water exceed the limits recommended in drinking water standards. Water temperatures ranged from freezing to 86°F in a 4-year period. The finished water supplied by the Flint water-treatment plant is fairly uniform in quality, moderately soft, alkaline, and low in color and turbidity. The pH is nearly always above 10. Further softening and removal of iron and related minerals would be desirable for certain industrial uses.</p><p>The quality of the water sampled in the Flint River tributaries was generally similar to that of the Flint River. However, no phenols or oils and waxes were found. Softening and other treatment dependent upon use would be required if these streams were developed for water supply.</p><p>Waters sampled in the Shiawassee River and selected lakes were generally less mineralized than Flint River water. Water from the lakes showed the lowest concentrations of dissolved solids. Softening would be required for nearly all uses. Additional treatment would depend upon contemplated use.</p><p>Shallow deposits of sand and gravel deposited as outwash along glacial meltwater streams and as deltas in the glacial lakes that covered the northwestern part of the county are sources of water to moderate- and large-capacity wells. Thick deposits of sand and gravel also fill some of the valleys in the bedrock surface and yield moderate to large supplies of water. Production from public supply wells tapping the drift aquifers in the area ranges from about 50 to 1,200 gpm. The water from the drift aquifer is hard or very hard and commonly contains objectionable amounts of iron.</p><p>The Saginaw formation is a source of water to wells supplying some of the small communities and industries in the county. The Saginaw, which is the uppermost bedrock formation in the area, underlies most of the county. It is composed of layers of sandstone, shale, and limestone and some beds of coal. The formation is composed principally of sandstone in some areas of the county, and shale in others. Production from wells tapping the Saginaw ranges from a few to about 500 gpm. The water produced is generally moderately hard or hard and commonly contains objectionable amounts of chloride. The quality of the water limits its development for water supply. Overdrafts from the Saginaw result in a lowering of the piezometric surface and commonly cause an upward migration of water high in chloride.</p><p>The Michigan and Marshall formations are generally not sources of fresh water where they are overlain by the Saginaw formation. In the southern and eastern parts of the county where they are overlain by glacial deposits, they are a source of water of good quality. The quantity of water obtainable from these formations is not fully known. However, the Marshall may be a source of large supplies of water in the southeastern part of the county.</p><p>An ample supply of water is available in lakes, ponds, and streams in the metropolitan area of Flint to meet requirements for domestic, sanitary, and firefighting use in civil defense emergencies. The extent of emergency use of water from these sources would depend upon the pumping, distribution, and treatment facilities available. Enough private industrial and commercial, and public wells are present in the area normally supplied by the Flint public water system to meet emergency requirements for domestic and sanitary use. Use of these wells would also depend upon available pumping and distribution facilities. Water from many of these wells contains objectionable amounts of chloride, but it could be used without treatment in an emergency.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1499E","usgsCitation":"Wiitala, S.W., Vanlier, K., and Krieger, R.A., 1964, Water resources of the Flint area, Michigan: U.S. Geological Survey Water Supply Paper 1499, Document: viii, 86 p.; 6 Plates: 20.00 x 18.29 inches or smaller, https://doi.org/10.3133/wsp1499E.","productDescription":"Document: viii, 86 p.; 6 Plates: 20.00 x 18.29 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":139431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499e/report-thumb.jpg"},{"id":29743,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29744,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29745,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29746,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29747,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29748,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499e/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Genesee County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.4607,43.2235],[-83.4593,43.1425],[-83.4589,43.1365],[-83.455,42.9681],[-83.4553,42.9617],[-83.4546,42.8798],[-83.4541,42.8766],[-83.5737,42.8744],[-83.6902,42.871],[-83.6863,42.7822],[-83.9225,42.7812],[-83.928,42.8677],[-83.9309,42.9574],[-83.9283,43.0451],[-83.9294,43.1334],[-83.9318,43.2204],[-83.8154,43.2212],[-83.694,43.2223],[-83.5809,43.2226],[-83.4607,43.2235]]]},\"properties\":{\"name\":\"Genesee\",\"state\":\"MI\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602df3","contributors":{"authors":[{"text":"Wiitala, Sulo Werner","contributorId":20315,"corporation":false,"usgs":true,"family":"Wiitala","given":"Sulo","email":"","middleInitial":"Werner","affiliations":[],"preferred":false,"id":146097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vanlier, K.E.","contributorId":24332,"corporation":false,"usgs":true,"family":"Vanlier","given":"K.E.","affiliations":[],"preferred":false,"id":146098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krieger, Robert A.","contributorId":99954,"corporation":false,"usgs":true,"family":"Krieger","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146099,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68643,"text":"ha106 - 1964 - Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"106","title":"Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware","language":"ENGLISH","doi":"10.3133/ha106","usgsCitation":"Adams, J.K., Boggess, D.H., and Coskery, O.J., 1964, Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware: U.S. Geological Survey Hydrologic Atlas 106, 1 map., https://doi.org/10.3133/ha106.","productDescription":"1 map.","costCenters":[],"links":[{"id":186592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90317,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/106/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.61749999999999,38.6175 ], [ -75.61749999999999,38.75 ], [ -75.5,38.75 ], [ -75.5,38.6175 ], [ -75.61749999999999,38.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ca8","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coskery, O. J.","contributorId":8440,"corporation":false,"usgs":true,"family":"Coskery","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278626,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":34178,"text":"b1173 - 1964 - Bedrock geology of the Evitts Creek and Pattersons Creek quadrangles, Maryland, Pennsylvania, and West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:09:25","indexId":"b1173","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":"1173","title":"Bedrock geology of the Evitts Creek and Pattersons Creek quadrangles, Maryland, Pennsylvania, and West Virginia","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1173","usgsCitation":"De Witt, W., and Colton, G.W., 1964, Bedrock geology of the Evitts Creek and Pattersons Creek quadrangles, Maryland, Pennsylvania, and West Virginia: U.S. Geological Survey Bulletin 1173, iv, 90 p. :illus., maps (2 col.) ;24 cm., https://doi.org/10.3133/b1173.","productDescription":"iv, 90 p. :illus., maps (2 col.) ;24 cm.","costCenters":[],"links":[{"id":109461,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20940.htm","linkFileType":{"id":5,"text":"html"},"description":"20940"},{"id":163502,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1173/report-thumb.jpg"},{"id":62078,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1173/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62079,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1173/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62080,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1173/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62081,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1173/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1173/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634407","contributors":{"authors":[{"text":"De Witt, Wallace Jr.","contributorId":87521,"corporation":false,"usgs":true,"family":"De Witt","given":"Wallace","suffix":"Jr.","affiliations":[],"preferred":false,"id":212567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colton, G. W.","contributorId":97468,"corporation":false,"usgs":true,"family":"Colton","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":212568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68272,"text":"ha131 - 1964 - Availability of ground water in Hall County, Nebraska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"131","title":"Availability of ground water in Hall County, Nebraska","language":"ENGLISH","doi":"10.3133/ha131","usgsCitation":"Keech, C.F., and Dreeszen, V., 1964, Availability of ground water in Hall County, Nebraska: U.S. Geological Survey Hydrologic Atlas 131, 4 maps ;31 x 29 cm., on sheet 122 x 105 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha131.","productDescription":"4 maps ;31 x 29 cm., on sheet 122 x 105 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":188556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89678,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ], [ -98.58333333333333,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66724c","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":277947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreeszen, V. H.","contributorId":8825,"corporation":false,"usgs":true,"family":"Dreeszen","given":"V. H.","affiliations":[],"preferred":false,"id":277946,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32726,"text":"pp458B - 1964 - Rocks, structure, and geologic history of Steamboat Springs thermal area, Washoe County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"pp458B","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":"458","chapter":"B","title":"Rocks, structure, and geologic history of Steamboat Springs thermal area, Washoe County, Nevada","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and geochemistry of the Steamboat Springs area, Nevada","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp458B","usgsCitation":"White, D., Thompson, G.A., and Sandberg, C., 1964, Rocks, structure, and geologic history of Steamboat Springs thermal area, Washoe County, Nevada: U.S. Geological Survey Professional Paper 458, p. B1-B63, https://doi.org/10.3133/pp458B.","productDescription":"p. B1-B63","costCenters":[],"links":[{"id":113063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0458b/report.pdf","size":"17443","linkFileType":{"id":1,"text":"pdf"}},{"id":113064,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0458b/plate-1.pdf","size":"7458","linkFileType":{"id":1,"text":"pdf"}},{"id":113065,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0458b/plate-2.pdf","size":"2697","linkFileType":{"id":1,"text":"pdf"}},{"id":113066,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0458b/plate-3.pdf","size":"2685","linkFileType":{"id":1,"text":"pdf"}},{"id":113067,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0458b/plate-4.pdf","size":"2611","linkFileType":{"id":1,"text":"pdf"}},{"id":113068,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0458b/plate-5.pdf","size":"2334","linkFileType":{"id":1,"text":"pdf"}},{"id":160594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0458b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd37","contributors":{"authors":[{"text":"White, D. E.","contributorId":20729,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":209038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, G. A.","contributorId":90332,"corporation":false,"usgs":true,"family":"Thompson","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":209040,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandberg, C.H.","contributorId":47421,"corporation":false,"usgs":true,"family":"Sandberg","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":209039,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32723,"text":"pp454L - 1964 - Stratigraphy of the Niobrara Formation at Pueblo, Colorado","interactions":[],"lastModifiedDate":"2026-02-18T21:10:56.453519","indexId":"pp454L","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":"L","title":"Stratigraphy of the Niobrara Formation at Pueblo, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp454L","usgsCitation":"Scott, G., and Cobban, W.A., 1964, Stratigraphy of the Niobrara Formation at Pueblo, Colorado: U.S. Geological Survey Professional Paper 454, 30 p., https://doi.org/10.3133/pp454L.","productDescription":"30 p.","startPage":"L1","endPage":"L30","costCenters":[],"links":[{"id":500150,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92893.htm","linkFileType":{"id":5,"text":"html"}},{"id":119493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0454l/report-thumb.jpg"},{"id":60644,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0454l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Pueblo","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.930419921875,\n              38.06106741381201\n            ],\n            [\n              -104.30419921875,\n              38.06106741381201\n            ],\n            [\n              -104.30419921875,\n              38.453588708941375\n            ],\n            [\n              -104.930419921875,\n              38.453588708941375\n            ],\n            [\n              -104.930419921875,\n              38.06106741381201\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5d7d","contributors":{"authors":[{"text":"Scott, G. R.","contributorId":61398,"corporation":false,"usgs":true,"family":"Scott","given":"G. R.","affiliations":[],"preferred":false,"id":209027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobban, W. A.","contributorId":21577,"corporation":false,"usgs":true,"family":"Cobban","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":209026,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1023,"text":"wsp1669U - 1964 - Ground-water resources of Waupaca County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:05:28","indexId":"wsp1669U","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":"1669","chapter":"U","title":"Ground-water resources of Waupaca County, Wisconsin","docAbstract":"<p>Waupaca County is in east-central Wisconsin. No serious ground-water problems existed in 1960 except in a few localities where crystalline rock is near land surface or is covered by nearly impermeable till. The use of ground water for irrigation has not appreciably affected ground-water levels.</p>\n<p>The county is covered by Pleistocene till, glaciolacustrine (lake), glaciofluvial (stream), and eolian (wind) deposits. In the northern three-quarters of the county these deposits overlie Precambrian crystalline rocks; in the remainder, they overlie sandstone of Cambrian age and, to a minor extent, dolomite of the Prairie du Chien Group of Ordovician age. The deposits of Pleistocene age, particularly outwash, are the principal sources of ground water except in those areas where the saturated thickness is slight or the permeability low. The sandstone of Cambrian age is an important aquifer in the southeastern part of the county. The crystalline rocks of Precambrian age yield little water except from fractures, joints, and weathered zones, and they are a source of water only in areas where better aquifers are absent.</p>\n<p>Ground water in Waupaca County occurs under both water-table and artesian conditions. The source of this ground water is precipitation that falls on the county and percolates downward to the zone of saturation. Regional movement of ground water is to the Wolf River. In most of the county the direction of movement is eastward or southeastward, except in the southeastern corner of the county, where the movement is westward.</p>\n<p>&nbsp;Water-level fluctuations reflect the variations of ground-water storage or artesian pressure in response to variations in recharge and discharge. Declining water levels from 1956 to 1959 reflect a period of below-normal precipitation, and rising water levels in late 1959 and 1960 reflect above-normal precipitation. Average precipitation, runoff, and evapotranspiration in 1959 are estimated to be 1,000, 400, and 600 mgd (million gallons per day) respectively. Pumpage in the county was estimated to be about 4 mgd in 1959, and about half of this amount was used for public supplies.</p>\n<p>A pumping test of a well in outwash deposits near Waupaca indicated that at that point the coefficient of transmissibility is about 100,000 gpd (gallons per day) per ft, the permeability is about 1,000 gpd per sq ft, the coefficient of storage is about 0.2, and the specific capacity is 41 gpm (gallons per minute) per ft of drawdown. These hydraulic characteristics are probably in the same order of magnitude as the characteristics of outwash deposits in the county in general.</p>\n<p>The water from wells in Waupaca County, although hard and generally containing iron, is good for most purposes.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1669U","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey, University of Wisconsin","usgsCitation":"Berkstresser, C., 1964, Ground-water resources of Waupaca County, Wisconsin: U.S. Geological Survey Water Supply Paper 1669, Report: iv, 38 p.; 7 Plates: 32.00 x 34.06 inches or smaller, https://doi.org/10.3133/wsp1669U.","productDescription":"Report: iv, 38 p.; 7 Plates: 32.00 x 34.06 inches or smaller","numberOfPages":"42","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":137935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669u/report-thumb.jpg"},{"id":25641,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25642,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25643,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25644,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25645,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25646,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25647,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25648,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Waupaca County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6062,44.5903],[-88.6152,44.5903],[-88.7371,44.5906],[-88.7368,44.5021],[-88.7365,44.4164],[-88.7381,44.3307],[-88.7397,44.2432],[-88.7658,44.2434],[-88.8609,44.2425],[-88.8871,44.2426],[-88.9821,44.243],[-89.007,44.2426],[-89.104,44.243],[-89.1288,44.243],[-89.2245,44.2433],[-89.2242,44.3308],[-89.2238,44.4174],[-89.2235,44.504],[-89.2231,44.5916],[-89.2234,44.6814],[-88.982,44.6798],[-88.8587,44.6797],[-88.7367,44.6791],[-88.6051,44.6783],[-88.6062,44.5903]]]},\"properties\":{\"name\":\"Waupaca\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d523","contributors":{"authors":[{"text":"Berkstresser, Charles F.","contributorId":33697,"corporation":false,"usgs":true,"family":"Berkstresser","given":"Charles F.","affiliations":[],"preferred":false,"id":143042,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","interactions":[{"subject":{"id":51650,"text":"ofr5480 - 1954 - The \"slug test\" for estimating transmissibility","indexId":"ofr5480","publicationYear":"1954","noYear":false,"title":"The \"slug test\" for estimating transmissibility"},"predicate":"SUPERSEDED_BY","object":{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","indexId":"wsp1536I","publicationYear":"1964","noYear":false,"chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown"},"id":1},{"subject":{"id":51779,"text":"ofr54310 - 1954 - Estimating transmissibility from specific capacity","indexId":"ofr54310","publicationYear":"1954","noYear":false,"title":"Estimating transmissibility from specific capacity"},"predicate":"SUPERSEDED_BY","object":{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","indexId":"wsp1536I","publicationYear":"1964","noYear":false,"chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1536I","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":"1536","chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown","docAbstract":"If the Theis graphical method is used for determining the hydraulic constants of an aquifer under water-table conditions, the observed drawdowns should be corrected for the decrease in saturated thickness. This is especially true if the drawdown is a large fraction of the original saturated thickness, for then the computed coefficient of permeability is highly inaccurate if based on observed, rather than corrected, water levels. Wenzel's limiting formula, a modification of the Theis graphical method, is useful where u=r2s/4Tt is less than about 0.01. However, a shorter procedure for determination of the coefficient of transmissibility, as well as the coefficient of storage, consists of plotting the values of the corrected drawdowns against the values of the logarithm of r. \r\n\r\nWenzel (1942) suggested that observation wells be situated on lines that extend upgradient and downgradient from the pumped well. However, a detailed analysis of aquifer-test results indicates that such a restriction is unnecessary. The gradient method for determining permeability should yield the same results as the Thies method. The former, when applied for a distance within the range of applicability of the latter, is merely a duplication of effort or, at best, a crude check. Because of the limitations of accuracy in plotting, the gradient method is much less satisfactory. That Wenzel (1942) obtained identical results from the two methods is regarded as a coincidence. \r\n\r\nFailure to take into consideration the fact that the pumped well does not tap the full thickness of the aquifer leads to an apparent coefficient of permeability that is much too low, especially if the aquifer consists of stratified sediments. The average coefficient of permeability computed from uncorrected drawdowns may be only a little more than half of the true value.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1536I","usgsCitation":"Bentall, R., 1964, Methods of determining permeability, transmissibility and drawdown: U.S. Geological Survey Water Supply Paper 1536, vi, 99 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1536I.","productDescription":"vi, 99 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1536i/report-thumb.jpg"},{"id":25635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bcc6","contributors":{"authors":[{"text":"Bentall, Ray","contributorId":78711,"corporation":false,"usgs":true,"family":"Bentall","given":"Ray","email":"","affiliations":[],"preferred":false,"id":143040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32764,"text":"pp420B - 1964 - Geology and oil resources of the eastern Puente Hills area, southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"pp420B","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":"420","chapter":"B","title":"Geology and oil resources of the eastern Puente Hills area, southern California","language":"ENGLISH","doi":"10.3133/pp420B","usgsCitation":"Durham, D., and Yerkes, R.F., 1964, Geology and oil resources of the eastern Puente Hills area, southern California: U.S. Geological Survey Professional Paper 420, p. B1-B62, https://doi.org/10.3133/pp420B.","productDescription":"p. B1-B62","costCenters":[],"links":[{"id":113073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0420b/report.pdf","size":"14606","linkFileType":{"id":1,"text":"pdf"}},{"id":113074,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0420b/plate-1.pdf","size":"13386","linkFileType":{"id":1,"text":"pdf"}},{"id":113075,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0420b/plate-2.pdf","size":"1410","linkFileType":{"id":1,"text":"pdf"}},{"id":113076,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0420b/plate-3.pdf","size":"4449","linkFileType":{"id":1,"text":"pdf"}},{"id":113077,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0420b/plate-4.pdf","size":"2695","linkFileType":{"id":1,"text":"pdf"}},{"id":161241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0420b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684751","contributors":{"authors":[{"text":"Durham, D.L.","contributorId":62257,"corporation":false,"usgs":true,"family":"Durham","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":209119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":209118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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