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1953 - Photogeologic map, Agathla Peak 2, Navajo County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr5359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-59","title":"Photogeologic map, Agathla Peak 2, Navajo County, Arizona","language":"ENGLISH","doi":"10.3133/ofr5359","usgsCitation":"Eckstein, W., 1953, Photogeologic map, Agathla Peak 2, Navajo County, Arizona: U.S. Geological Survey Open-File Report 53-59, 1 map, https://doi.org/10.3133/ofr5359.","productDescription":"1 map","costCenters":[],"links":[{"id":178583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":86495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f9c3","contributors":{"authors":[{"text":"Eckstein, W.H.","contributorId":79872,"corporation":false,"usgs":true,"family":"Eckstein","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":243205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51228,"text":"ofr5345 - 1953 - Steel tubular products in general use as water-well pipe","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr5345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-45","title":"Steel tubular products in general use as water-well pipe","language":"ENGLISH","doi":"10.3133/ofr5345","usgsCitation":"Conklin, H., 1953, Steel tubular products in general use as water-well pipe: U.S. Geological Survey Open-File Report 53-45, 7 p., https://doi.org/10.3133/ofr5345.","productDescription":"7 p.","costCenters":[],"links":[{"id":176821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4637","contributors":{"authors":[{"text":"Conklin, H.L.","contributorId":80745,"corporation":false,"usgs":true,"family":"Conklin","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":243189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51241,"text":"ofr5361 - 1953 - Preliminary structure contour map of Blaine, northern Choteau, and Hill Counties and adjoining areas in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr5361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-61","title":"Preliminary structure contour map of Blaine, northern Choteau, and Hill Counties and adjoining areas in Montana","language":"ENGLISH","doi":"10.3133/ofr5361","usgsCitation":"Erdman, C., and Koskinen, V., 1953, Preliminary structure contour map of Blaine, northern Choteau, and Hill Counties and adjoining areas in Montana: U.S. Geological Survey Open-File Report 53-61, 1 map, https://doi.org/10.3133/ofr5361.","productDescription":"1 map","costCenters":[],"links":[{"id":178585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":100128,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0061/plate-1.pdf","size":"6135","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a75a","contributors":{"authors":[{"text":"Erdman, C.E.","contributorId":86843,"corporation":false,"usgs":true,"family":"Erdman","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":243207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koskinen, V.E.","contributorId":90817,"corporation":false,"usgs":true,"family":"Koskinen","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":243208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51774,"text":"ofr54305 - 1953 - Progress report on the Killigwa anticlinorium, 1953","interactions":[],"lastModifiedDate":"2023-10-02T19:15:19.021243","indexId":"ofr54305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"54-305","title":"Progress report on the Killigwa anticlinorium, 1953","docAbstract":"

This report was prepared to assist in the planning of seismic profiles to be run across the anticlinorium in the vicinity of the Kiligwa River. The stratigraphy and structure of the mapped area south of the anticlinorium are reviewed. Two facies of the Lisburne formation, a calcarenite-hydroclastic limestone facies and a black shale, black chert and dark limestone facies, have been distinguished. In the southern foothills, the black shale facies appears to have been thrust from the south over the limestone facies. The available evidence indicates that the Lisburne formation, as limestone or a more proximal facies was doposited over the area of the anticlinorium. Following a redefinition of the Torok formation in the type area, strata formerly mapped as Torok have here been designated Castle Mountain formation. The depositional history of the Castle Mountain formation reflects active orogeny. Lenses of coarse clastics appear to have been dumped in local basins; equivalent beds to the north are much finer. A basal zone of sandstone may be more extensive and may correlate with the sandstones noted along and north of the anticlinorium.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54305","usgsCitation":"Trailleur, I.L., and Kent, B.H., 1953, Progress report on the Killigwa anticlinorium, 1953: U.S. Geological Survey Open-File Report 54-305, Report: 17 p.; 1 Plate: 69.28 x 27.07 inches, https://doi.org/10.3133/ofr54305.","productDescription":"Report: 17 p.; 1 Plate: 69.28 x 27.07 inches","costCenters":[],"links":[{"id":174320,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1954/0305/report-thumb.jpg"},{"id":421483,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1954/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":421482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96000","country":"United States","state":"Alaska","otherGeospatial":"Kiligwa River vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -158.51398670378427,\n 69.47752552167404\n ],\n [\n -158.51398670378427,\n 69.17711978354669\n ],\n [\n -157.87002212311705,\n 69.17711978354669\n ],\n [\n -157.87002212311705,\n 69.47752552167404\n ],\n [\n -158.51398670378427,\n 69.47752552167404\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688483","contributors":{"authors":[{"text":"Trailleur, Irvin L.","contributorId":24422,"corporation":false,"usgs":true,"family":"Trailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":244275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kent, Bion H.","contributorId":63389,"corporation":false,"usgs":true,"family":"Kent","given":"Bion","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":244276,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51210,"text":"ofr5316 - 1953 - Photogeologic map, Tidwell 9 quadrangle, Emery and Grand Counties, Utah","interactions":[{"subject":{"id":51210,"text":"ofr5316 - 1953 - Photogeologic map, Tidwell 9 quadrangle, Emery and Grand Counties, Utah","indexId":"ofr5316","publicationYear":"1953","noYear":false,"title":"Photogeologic map, Tidwell 9 quadrangle, Emery and Grand Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":64700,"text":"i114 - 1955 - Photogeologic map of the Tidwell-9 quadrangle, Emery and Grand Counties, Utah","indexId":"i114","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Tidwell-9 quadrangle, Emery and Grand Counties, Utah"},"id":1}],"supersededBy":{"id":64700,"text":"i114 - 1955 - Photogeologic map of the Tidwell-9 quadrangle, Emery and Grand Counties, Utah","indexId":"i114","publicationYear":"1955","noYear":false,"title":"Photogeologic map of the Tidwell-9 quadrangle, Emery and Grand Counties, Utah"},"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr5316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-16","title":"Photogeologic map, Tidwell 9 quadrangle, Emery and Grand Counties, Utah","language":"ENGLISH","doi":"10.3133/ofr5316","usgsCitation":"Bates, C., and Hosley, V., 1953, Photogeologic map, Tidwell 9 quadrangle, Emery and Grand Counties, Utah (Superceded by: I-114): U.S. Geological Survey Open-File Report 53-16, 1 map, https://doi.org/10.3133/ofr5316.","productDescription":"1 map","costCenters":[],"links":[{"id":178527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: I-114","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685f27","contributors":{"authors":[{"text":"Bates, C.E.","contributorId":48237,"corporation":false,"usgs":true,"family":"Bates","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":243157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hosley, V.M.","contributorId":33372,"corporation":false,"usgs":true,"family":"Hosley","given":"V.M.","email":"","affiliations":[],"preferred":false,"id":243156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51219,"text":"ofr5327 - 1953 - Supplement to the effect of a well on the flow of a nearby stream, by C. F. Theis, in American Geophysical Union Transactions, pt. 3, p. 734-438, August, 1941","interactions":[],"lastModifiedDate":"2020-09-22T16:54:43.795844","indexId":"ofr5327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-27","title":"Supplement to the effect of a well on the flow of a nearby stream, by C. F. Theis, in American Geophysical Union Transactions, pt. 3, p. 734-438, August, 1941","docAbstract":"

No abstract available.

","language":"English","doi":"10.3133/ofr5327","usgsCitation":"Brown, R.H., and Reed, E.W., 1953, Supplement to the effect of a well on the flow of a nearby stream, by C. F. Theis, in American Geophysical Union Transactions, pt. 3, p. 734-438, August, 1941 (Superceded by: W-1545-C): U.S. Geological Survey Open-File Report 53-27, 3 p., https://doi.org/10.3133/ofr5327.","productDescription":"3 p.","costCenters":[],"links":[{"id":176720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: W-1545-C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985d2","contributors":{"authors":[{"text":"Brown, R. H.","contributorId":19931,"corporation":false,"usgs":false,"family":"Brown","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":243169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, E. W.","contributorId":69640,"corporation":false,"usgs":true,"family":"Reed","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":243170,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51242,"text":"ofr5362 - 1953 - Kyanite quartzite in the Baker Mountain Madisonville area, Prince Edward and Charlotte Counties, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr5362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-62","title":"Kyanite quartzite in the Baker Mountain Madisonville area, Prince Edward and Charlotte Counties, Virginia","language":"ENGLISH","doi":"10.3133/ofr5362","usgsCitation":"Espenshade, G., and Potter, D., 1953, Kyanite quartzite in the Baker Mountain Madisonville area, Prince Edward and Charlotte Counties, Virginia: U.S. Geological Survey Open-File Report 53-62, 1 map, https://doi.org/10.3133/ofr5362.","productDescription":"1 map","costCenters":[],"links":[{"id":178586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4773","contributors":{"authors":[{"text":"Espenshade, G.H.","contributorId":49374,"corporation":false,"usgs":true,"family":"Espenshade","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":243209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, D.B.","contributorId":96748,"corporation":false,"usgs":true,"family":"Potter","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":243210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51243,"text":"ofr5363 - 1953 - Kyanite quartzite in the Willis Mountain-Woods Mountain area, Buckingham County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr5363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-63","title":"Kyanite quartzite in the Willis Mountain-Woods Mountain area, Buckingham County, Virginia","language":"ENGLISH","doi":"10.3133/ofr5363","usgsCitation":"Espenshade, G., and Potter, D., 1953, Kyanite quartzite in the Willis Mountain-Woods Mountain area, Buckingham County, Virginia: U.S. Geological Survey Open-File Report 53-63, 1 map, https://doi.org/10.3133/ofr5363.","productDescription":"1 map","costCenters":[],"links":[{"id":178691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4775","contributors":{"authors":[{"text":"Espenshade, G.H.","contributorId":49374,"corporation":false,"usgs":true,"family":"Espenshade","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":243211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, D.B.","contributorId":96748,"corporation":false,"usgs":true,"family":"Potter","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":243212,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1509,"text":"wsp1183 - 1953 - Surface water supply of the United States, 1950, Part XIII, Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1183","title":"Surface water supply of the United States, 1950, Part XIII, Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1183","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Surface water supply of the United States, 1950, Part XIII, Snake River basin: U.S. Geological Survey Water Supply Paper 1183, viii, 250 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1183.","productDescription":"viii, 250 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1183/report-thumb.jpg"},{"id":26570,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69655d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51743,"text":"ofr54246 - 1953 - Second memorandum on the flow of Aqua Caliente Spring after road construction at Palm Springs, California","interactions":[],"lastModifiedDate":"2014-06-18T10:12:07","indexId":"ofr54246","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"54-246","title":"Second memorandum on the flow of Aqua Caliente Spring after road construction at Palm Springs, California","docAbstract":"This memorandum was prepared at the request of Henry Harris, Acting Area Director, Bureau of Indian Affairs, Sacramento, Calif., to report on recent conditions at the Agua Caliente Spring, Palm Springs, Calif., and to suggest further possibilities for restoring the spring discharge to its pre-road-construction condition.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Long Beach, CA","doi":"10.3133/ofr54246","collaboration":"Prepared at the request of the Bureau of Indian Affairs","usgsCitation":"Poland, J.F., and Dutcher, L., 1953, Second memorandum on the flow of Aqua Caliente Spring after road construction at Palm Springs, California: U.S. Geological Survey Open-File Report 54-246, 8 p., https://doi.org/10.3133/ofr54246.","productDescription":"8 p.","numberOfPages":"10","costCenters":[],"links":[{"id":288764,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0246/report.pdf"},{"id":288765,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","city":"Palm Springs","otherGeospatial":"Agua Caliente Spring","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.684848,33.611126 ], [ -116.684848,33.932139 ], [ -116.443046,33.932139 ], [ -116.443046,33.611126 ], [ -116.684848,33.611126 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc274","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":244224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1352,"text":"wsp1229 - 1953 - Ground-water conditions in the Milwaukee-Waukesha area, Wisconsin","interactions":[],"lastModifiedDate":"2024-05-29T20:56:49.407766","indexId":"wsp1229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1229","title":"Ground-water conditions in the Milwaukee-Waukesha area, Wisconsin","docAbstract":"

Three major aquifers underlie the Milwaukee-Waukesha area: sandstones of Cambrian and Ordovician age, Niagara dolomite of Silurian age, and sand and gravel deposits of Pleistocene age. The Maquoketa shale of Ordovician age acts as a more or less effective seal between the Pleistocene deposits and Niagara dolomite above and the sandstone aquifer below. Crystalline rocks of pre-Cambrian age form an impermeable basement complex below the Paleozoic sedimentary rocks. The Paleozoic strata dip east at 25 to 30 feet to the mile. There is no evidence that any of the faults and folds known or surmised to be present acts as a barrier to the movement of ground water.

\n

The bedrock surface underlying the Milwaukee-Waukesha area is formed by the Niagara dolomite except in northeastern Milwaukee County, where it is dolomite and shale of the Milwaukee formation of Devonian age, and in some of the preglacial valleys where the uppermost bedrock formation is the Maquoketa shale. Unconsolidated deposits of glacial drift cover the surface of the bedrock almost completely.

\n

Buried valleys in the bedrock surface contain as much as 150 feet of water-bearing sand and gravel deposits. These deposits, along with the Niagara dolomite, could be developed as sources of water supplemental to that of the sandstone aquifer. The Niagara dolomite is an important aquifer; it yields water from crevices and solution channels.

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The sandstone aquifer consists of the Galena dolomite, the Platteville limestone, and the St. Peter sandstone of Ordovician age, and the Eau Claire and Mount Simon sandstones of Cambrian age. The St. Peter and Mount Simon are the most productive formations but the others supply some water to wells.

\n

Static water levels in the shallow aquifers have not declined to any great extent except in downtown Milwaukee, where a 50-foot-deep cone of depression exists. Static water levels in the sandstone aquifer declined as much as 350 feet in the Milwaukee area from 1880 through 1950.

\n

Recharge to the two shallow aquifers occurs locally from precipitation within the area. The major recharge area of the sandstone aquifer lies about 25 miles west of Wauwatosa. Some ground water is recharged to the sandstone aquifer locally by leakage from the Niagara dolomite, mostly through deep uncased wells.

\n

Ground water is the source of six municipal supplies and many industrial and commercial supplies in the area. Pumpage from deep wells has increased from about 2.5 mgd in 1900 to about 25 mgd in 1949, of which 6.0 mgd was derived from the shallow aquifers. The total withdrawal from the shallow aquifers, including the 6.0 mgd from the deep wells, was about 19.5 mgd in 1949. Thus the total in 1949 was 38.5 mgd for the area as a whole.

\n

Coefficients of transmissibility and storage for the sandstone aquifer were obtained by means of controlled pumping tests at Wauwatosa, Waukesha, Greendale, Town of Lake, and Jefferson. The coefficients were used to calculate the amount of water recharged from the Niagara dolomite to the sandstone aquifer in the area. About 5.5 mgd of the 23 mgd pumped from deep wells in 1950 was supplied locally by leakage from the Niagara dolomite. The coefficients, with corrections for boundaries, were also applied to past records of pumpage to calculate the water-level decline in the sandstone aquifer at Wauwatosa from 1880 through 1950. The calculated decline was 317 feet, and the actual decline was 307 feet.

\n

The future water-level decline in the sandstone aquifer at Wauwatosa resulting from estimated future pumping conditions was computed. If the pumpage in the area as ?. whole increases from about 23 mgd in 1950 to about 28 mgd in 1960, the water levels at Wauwatosa will decline as much as 65 feet more by 1960.

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It is estimated that the available recharge to the sandstone aquifer underlying the Milwaukee-Waukesha area is approximately 60 mgd.

\n

It is recommended that new deep wells be located to the west toward the recharge area and that the shallow aquifers be used as auxiliary sources to void excessive lowering of water levels in the sandstone aquifers.

\n

Conservation should be practiced by all users of ground water to avoid waste resulting in lower water levels and higher pumping costs.

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