This report presents and discusses the quantitative and qualitative data obtained during a pumping test at the Levittown housing development in Nassau County, N. Y. One of the ten principal supply wells, screened in the sands of the Magothy (?) formation which is overlain unconformably by the sand and gravel of the upper Pleistocene deposits, was pumped for more than 24 hours at a rate of 790 gallons per minute. During this time the development of the cone of depression extended a distance of more than 1,000 feet from the pumping well. A coefficient of transmissibility of 245,0W gallons per day per foot was computed and a coefficient of storage of 0.13 was determined at the site of the pumping test.
The qualitative results show that the two aquifers at the pumping-test site, that is, the sand and gravel of the upper Pleistocene deposits and the underlying sands of the Magothy (?) formation, function essentially as one hydrologic unit. Such information, together with other data of this kind, assumes importance when it is realized that the New York rater Power and Control Commission by regulation considers every aquifer as a separate and distinct hydrologic unit. It thus requires the return of water pumped for cooling and other similar uses to the same aquifer from which the water taken, unless sufficient evidence is obtained to show that two adjacent aquifers function as a single hydrologic unit.
Sufficient data were obtained during the test to suggest that perhaps about 14 feet of the 19.7 feet measured as drawdown in the pumped well is attributable to well and screen losses.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr51131","usgsCitation":"Lusczynski, N., 1951, Pumping test at Levittown, Nassau County, New York, September 16-18, 1949: U.S. Geological Survey Open-File Report 51-131, Report: 8 p., 10 Plates: 9.36 x 7.93 inches or smaller, 3 Tables: 10.27 x 7.40 inches or smaller, https://doi.org/10.3133/ofr51131.","productDescription":"Report: 8 p., 10 Plates: 9.36 x 7.93 inches or smaller, 3 Tables: 10.27 x 7.40 inches or smaller","costCenters":[],"links":[{"id":383997,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383996,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383995,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383994,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383993,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0131/report-thumb.jpg"},{"id":383992,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383991,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383990,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383989,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383988,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0131/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383987,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1951/0131/Table-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383986,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1951/0131/Table-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383985,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1951/0131/Table-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383984,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0131/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Nassau County","city":"Levittown","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.53080749511717,\n 40.7189000170401\n ],\n [\n -73.49716186523438,\n 40.7189000170401\n ],\n [\n -73.49716186523438,\n 40.72982797782921\n ],\n [\n -73.53080749511717,\n 40.72982797782921\n ],\n [\n -73.53080749511717,\n 40.7189000170401\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655ad9","contributors":{"authors":[{"text":"Lusczynski, N.J.","contributorId":10779,"corporation":false,"usgs":true,"family":"Lusczynski","given":"N.J.","affiliations":[],"preferred":false,"id":242776,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1324,"text":"wsp1134A - 1951 - Flood of August 4-5, 1943, in central West Virginia, with a summary of flood stages and discharges in West Virginia","interactions":[],"lastModifiedDate":"2022-02-16T21:59:34.297557","indexId":"wsp1134A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"1134","chapter":"A","title":"Flood of August 4-5, 1943, in central West Virginia, with a summary of flood stages and discharges in West Virginia","docAbstract":"During the night of August 4-5, 1943, a violent, thunderstorm of unusual intensity occurred in parts of Braxton, Calhoun, Gilmer, Ritchie, and Wirt Counties in the Little Kanawha River Basin in central West Virginia. Precipitation amounted to as much as 15 inches in 2 hours in some sections. As a result, many small streams and a reach of the Little Kanawha River in the vicinity of Burnsville and Gilmer reached the highest stages known. Computations based on special surveys made at suitable sites on representative small streams in the areas of intense flooding indicate that peak discharges closely approach 50 percent of the Jarvis scale.
Twenty-three lives were lost on the small tributaries as numerous homes were swept away by the flood, which developed with incredible rapidity during the early morning hours. Damage estimated at $1,300,000 resulted to farm buildings, crops, land, livestock, railroads, highways, and gas- and oil-producing facilities. Considerable permanent land damage resulted from erosion and deposition of sand and gravel.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Notable local floods of 1942-43","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1134A","collaboration":"Prepared in cooperation with the Corps of Engineers and the State of West Virginia","usgsCitation":"Erskine, H.M., 1951, Flood of August 4-5, 1943, in central West Virginia, with a summary of flood stages and discharges in West Virginia: U.S. Geological Survey Water Supply Paper 1134, iv, 57 p., https://doi.org/10.3133/wsp1134A.","productDescription":"iv, 57 p.","costCenters":[],"links":[{"id":396054,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24221.htm"},{"id":137976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1134a/report-thumb.jpg"},{"id":26371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1134a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.5,\n 38.667\n ],\n [\n -80.5,\n 38.667\n ],\n [\n -80.5,\n 39.333\n ],\n [\n -81.5,\n 39.333\n ],\n [\n -81.5,\n 38.667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee9a2","contributors":{"authors":[{"text":"Erskine, Harlan Mercer","contributorId":25135,"corporation":false,"usgs":true,"family":"Erskine","given":"Harlan","email":"","middleInitial":"Mercer","affiliations":[],"preferred":false,"id":143565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51027,"text":"ofr51130 - 1951 - Pumping test at Levittown, New York, at well N3488 (Hicksville Water District well 5)","interactions":[],"lastModifiedDate":"2021-02-22T18:45:27.332276","indexId":"ofr51130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-130","title":"Pumping test at Levittown, New York, at well N3488 (Hicksville Water District well 5)","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr51130","usgsCitation":"Lusczynski, N., 1951, Pumping test at Levittown, New York, at well N3488 (Hicksville Water District well 5): U.S. Geological Survey Open-File Report 51-130, Report: 3 p.; 2 Plates: 9.81 x 7.66 inches and 9.54 x 7.64 inches, https://doi.org/10.3133/ofr51130.","productDescription":"Report: 3 p.; 2 Plates: 9.81 x 7.66 inches and 9.54 x 7.64 inches","costCenters":[],"links":[{"id":383443,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383445,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383444,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0130/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0130/report-thumb.jpg"}],"country":"United States","state":"New York","city":"Levittown","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.52806091308594,\n 40.72202247464282\n ],\n [\n -73.50059509277344,\n 40.72202247464282\n ],\n [\n -73.50059509277344,\n 40.72878729696505\n ],\n [\n -73.52806091308594,\n 40.72878729696505\n ],\n [\n -73.52806091308594,\n 40.72202247464282\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db6557b6","contributors":{"authors":[{"text":"Lusczynski, N.J.","contributorId":10779,"corporation":false,"usgs":true,"family":"Lusczynski","given":"N.J.","affiliations":[],"preferred":false,"id":242775,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50996,"text":"ofr5198 - 1951 - Ground-water data on certain areas in Baltimore County, Maryland","interactions":[],"lastModifiedDate":"2021-02-04T19:49:52.800103","indexId":"ofr5198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-98","title":"Ground-water data on certain areas in Baltimore County, Maryland","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5198","usgsCitation":"Bennett, R., 1951, Ground-water data on certain areas in Baltimore County, Maryland: U.S. Geological Survey Open-File Report 51-98, Report: 3 p.; 1 Plate: 9.99 x 6.61 inches, https://doi.org/10.3133/ofr5198.","productDescription":"Report: 3 p.; 1 Plate: 9.99 x 6.61 inches","costCenters":[],"links":[{"id":383029,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1951/0098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383028,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0098/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0098/report-thumb.jpg"}],"country":"United States","state":"Maryland","county":"Baltimore County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.81640625,\n 39.20246222588238\n ],\n [\n -76.475830078125,\n 39.20246222588238\n ],\n [\n -76.475830078125,\n 39.37677199661635\n ],\n [\n -76.81640625,\n 39.37677199661635\n ],\n [\n -76.81640625,\n 39.20246222588238\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf25","contributors":{"authors":[{"text":"Bennett, R.R.","contributorId":104880,"corporation":false,"usgs":true,"family":"Bennett","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":242732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51012,"text":"ofr51115 - 1951 - Progress report on sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana (revised)","interactions":[{"subject":{"id":51012,"text":"ofr51115 - 1951 - Progress report on sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana (revised)","indexId":"ofr51115","publicationYear":"1951","noYear":false,"title":"Progress report on sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana (revised)"},"predicate":"SUPERSEDED_BY","object":{"id":3818,"text":"cir170 - 1952 - Sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana","indexId":"cir170","publicationYear":"1952","noYear":false,"title":"Sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana"},"id":1}],"supersededBy":{"id":3818,"text":"cir170 - 1952 - Sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana","indexId":"cir170","publicationYear":"1952","noYear":false,"title":"Sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana"},"lastModifiedDate":"2012-02-02T00:11:30","indexId":"ofr51115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-115","title":"Progress report on sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana (revised)","language":"ENGLISH","doi":"10.3133/ofr51115","usgsCitation":"Hembree, C., Colby, B.R., Swenson, H.A., and Davis, J., 1951, Progress report on sedimentation and chemical quality of water in the Powder River drainage basin, Wyoming and Montana (revised) (Superceded by: Circular 170): U.S. Geological Survey Open-File Report 51-115, 127 p., https://doi.org/10.3133/ofr51115.","productDescription":"127 p.","costCenters":[],"links":[{"id":178795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: Circular 170","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de7b","contributors":{"authors":[{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":242754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colby, B. R.","contributorId":59776,"corporation":false,"usgs":true,"family":"Colby","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242752,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swenson, H. A.","contributorId":58618,"corporation":false,"usgs":true,"family":"Swenson","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":242751,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, J.R.","contributorId":83907,"corporation":false,"usgs":true,"family":"Davis","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":242753,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":51014,"text":"ofr51117 - 1951 - Investigations of seepage gains and losses in the Atascosa, Frio, and Nueces rivers from Potett, Texas to Mikeska, Texas, during January, April, August, and September 1951","interactions":[],"lastModifiedDate":"2023-11-24T21:35:47.416553","indexId":"ofr51117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-117","title":"Investigations of seepage gains and losses in the Atascosa, Frio, and Nueces rivers from Potett, Texas to Mikeska, Texas, during January, April, August, and September 1951","docAbstract":"These investigations were undertaken at the request of the Texas State Board of Water Engineers and engineers of the Lower Nueces River Water Supply District. The purpose of the investigations was to determine seepage gains or losses along the river and losses in transmission of water from the District's artesian wells near Campbellton to Lake Corpus Christi. The channels of the Atascosa, Frio, Nueces rivers were used to transport the water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr51117","collaboration":"Prepared in cooperation with the Texas State Board of Water Engineers","usgsCitation":"Holland, P.H., 1951, Investigations of seepage gains and losses in the Atascosa, Frio, and Nueces rivers from Potett, Texas to Mikeska, Texas, during January, April, August, and September 1951: U.S. Geological Survey Open-File Report 51-117, 26 p., https://doi.org/10.3133/ofr51117.","productDescription":"26 p.","costCenters":[],"links":[{"id":178797,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0117/report-thumb.jpg"},{"id":422947,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Mikeska, Potett","otherGeospatial":"Atascosa River, Frio River, Nueces River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.54531753804604,\n 29.162750368519113\n ],\n [\n -98.54531753804604,\n 28.864916151721474\n ],\n [\n -96.05691421773348,\n 28.864916151721474\n ],\n [\n -96.05691421773348,\n 29.162750368519113\n ],\n [\n -98.54531753804604,\n 29.162750368519113\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f81","contributors":{"authors":[{"text":"Holland, Pat H.","contributorId":64690,"corporation":false,"usgs":true,"family":"Holland","given":"Pat","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":242756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2848,"text":"wsp1107 - 1951 - Geology and water resources of the Santa Ynez River basin, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"1107","title":"Geology and water resources of the Santa Ynez River basin, Santa Barbara County, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1107","usgsCitation":"Upson, J., and Thomasson, H., 1951, Geology and water resources of the Santa Ynez River basin, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1107, vii, 194 p. :ill. ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1107.","productDescription":"vii, 194 p. :ill. ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":138699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1107/report-thumb.jpg"},{"id":29428,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29429,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29430,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29431,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29432,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29433,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29434,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1107/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68405f","contributors":{"authors":[{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":145901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomasson, H.G. Jr.","contributorId":45694,"corporation":false,"usgs":true,"family":"Thomasson","given":"H.G.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":145900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50951,"text":"ofr5191 - 1951 - Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","interactions":[],"lastModifiedDate":"2021-03-18T21:28:50.810463","indexId":"ofr5191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-91","title":"Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota","docAbstract":"The Mohall area includes about 120 square miles in Bottineau and Renville Counties in northwestern North Dakota. Mohall, whose 1950 population was 1,073, is the only town in the area.
The area is part of the Drift Prairie section of the Central Lowland physiographic province. It is characterized by the gently undulating ground moraine plain which slopes regionally to the northeast. It is drained by several southeast-trending intermittent streams which run almost at right angles to the regional slope.
The geologic formations in the Mohall area may be conveniently grouped into three units: the alluvium or alluvial deposits, which are found in the valleys of the intermittent streams, the till and associated glaciofluvial deposits, and the bedrock formations.
Ground water of reasonably good quality is obtained in the area only from the alluvial deposits. Because of the limited areal extent of these deposits, only a small number of farms obtain water supplies from them. However, the municipal water supply of the town of Mohall is obtained from these deposits in Spring Coulee northeast of the town, and much water for rural domestic use is hauled from the Becker well southwest of the town, in Little Deep Creek.
The principal source of recharge to the alluvial deposits is seepage during the spring runoff period. Natural discharge occurs by underflow down the stream valleys, by evaporation from open water and marshy areas and transpiration by plants.
The coefficient of transmissibility of the alluvium, n the basis of short pumping tests on Mohan wells 3 and 4, is indicated to be about 6,000 gallons a day per foot at well 3 and about 20,000 gallons a day per foot at well 4. The specific yield was computed as 0.25 from the pumping test on well 3. No gravel of importance was encountered in the two cross sections that were drilled across Spring Coulee near the municipal wells, and the greatest thickness of saturated alluvial deposits found was only about 10 feet.
A Saturated thickness of 20 feet of sand and gravel was penetrated in test drilling along Cut Bank Creek. This is the greatest thickness of saturated alluvial deposits penetrated anywhere in the area. Ground water in storage in these alluvial deposits has been estimated to be about 150 million gallons per mile. These deposits are favorably situated to receive recharge, as Cut Bank Creek drains a rather large area and contains long stretches of open water perennially, Therefore, it is believed that the alluvial deposits of Cut Bank Creek offer the best promise for the development of moderately large perennial ground-water supplies for the present and probable future needs of the town of Mohall.
Test drilling in West Cut Bank Creek and in Little Deep Creek did not reveal alluvial deposits of such character and saturated thickness as to be considered favorable for the development of moderate to large water supplies, though some of the material encountered should yield adequate quantities for farm supplies.
The till with its associated glaciofluvial deposits is the surface formation in the area except where covered by the alluvial deposits in the stream valleys. In the Mohall areas, this formation is not an important aquifer and fewer than half a dozen wells are known to obtain water from it. The glaciofluvial deposits penetrated by the test holes are not considered adequate sources for permanent municipal or industrial supplies because they are likely to have small-areal extent and the overlying, relatively impermeable till makes seasonal recharge to them practically impossible.
Test drilling in the Souris River Valley about 12 miles west of Mohall penetrated as mutt as 58 feet of fluvial sediments, but practi-cally all the material is clay and silt. No important aquifers were found there.
At least 50 percent of all the farm water supplies in the area are obtained from wells in the bedrock formations, which probably consist of the Fox Hills sandstone, the Cannonball formation, and the Ludlow and Tongue Rtter members of the Fort Union formation.
Underlying these formations is approximately 2,600 feet of Cretaceous shale, which'is not water bearing. Water from the \"Dakota\" sandstone (including the possible equivalent of the Fuson shale and Lakota sandstone) may be obtained at depths of about 3,200 to 3,300 feet. The \"Dakota sandstone\" probably would yield water in sufficient quantity for municipal and many industrial purposes in this areas but the water is likely to be too highly mineralized for most domestic uses.
Jurassic formations underlie the Cretaceous formations in the area. They do not constitute aquifers of importance, and, any water found in them is likely to be too highly mineralized for most purposes.
In the Mohall area, by far the most suitable water for general purposes is obtained from the shallow alluvial deposits in the stream valleys. Of the seven samples of this water water analyzed, the highest concentration of dissolved solids was 1,242 parts per million and the lowest, 317 parts. The iron content was higher than desirable in two samples but satisfactory in all the others. Total hardness ranged from 196 to 570, which is higher than desirable. Nitrate was present in all samples analyzed and was excessively high in two samples.
Water samples for analysis were not obtained from the till and associated glaciofluvial deposits but the water from these aquifers is likely to be more highly mineralized than the water from the alluvial. deposits.
The water from the upper part of the bedrock is highly mineralized, but its mineral content varies considerably. The chloride concentration of the samples analyzed ranges from 608 to 3,740 parts per million and the bicarbonate concentration ranges from 160 to 860 parts per million. The specific conductance ranges from 3,190 to 11,120 micromhos and may represent total mineralization on the order of 1,500 to more than 6,000 parts per million in the water with high chloride and bicarbonate content.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5191","usgsCitation":"Akin, P., 1951, Ground water in the Mohall area, Bottineau and Renville Counties, North Dakota: U.S. Geological Survey Open-File Report 51-91, Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches, https://doi.org/10.3133/ofr5191.","productDescription":"Report: 90 p.; 2 Plates: 8.00 x 7.80 inches and 10.30 x 5.66 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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(1 folded) :ill., 2 maps ;27 cm., https://doi.org/10.3133/ofr5242.","productDescription":"141 p. (1 folded) :ill., 2 maps ;27 cm.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":154730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho","county":"Cassia County","otherGeospatial":"Raft River Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6356b9","contributors":{"authors":[{"text":"Fader, Stuart Wesley","contributorId":68742,"corporation":false,"usgs":true,"family":"Fader","given":"Stuart","email":"","middleInitial":"Wesley","affiliations":[],"preferred":false,"id":189276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51054,"text":"ofr51155 - 1951 - Ground-water resources of Baker Valley, Baker County, Oregon","interactions":[],"lastModifiedDate":"2025-11-25T16:22:40.063158","indexId":"ofr51155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-155","title":"Ground-water resources of Baker Valley, Baker County, Oregon","docAbstract":"The Baker Valley is the southern part of a small oval-shaped inter-montane structural basin located near tie southeastern edge of the Blue Mountains of northeastern Oregon. The Powder River enters and leaves the valley through narrow rock gorges. The alluviated basin floor at an altitude of about 3,400 feet is bounded by high, Alpine-type mountains on the west and by lover hilly ridges on the north, east, and south. Creeks descend across alluvial fans from the higher western margin of the valley to the Powder River on the valley floor.
The valley floor and the contiguous alluvial slopes are formed of unconsolidated deposits of Quaternary age having a thickness of more than 700 feet in the central part of the valley. The surrounding higher lands are formed of consolidated rocks composed of volcanic flows, tuffs, and partly consolidated deposits of Tertiary age, and sedimentary, igneous, and metamorphic roots of late Paleozoic age. The unconsolidated materials underlying the alluvial slopes are mostly fanglomerates - composed of partly consolidated angular rock fragments imbedded in assorted finer materials - and fine-grained sedimentary deposits having much inter-bedded gravel and sand along the valley floor.
The unconsolidated deposits contain a body of ground water, the upper surface of which is called the water table. The water table slopes down gradient approximately parallel to tile land surface. Variations in the general inclination of that water table indicate that drainage on different segments of the alluvial slope is influent and effluent to the ground water body. Yields from wells in the fanglomerate along the rest side of the valley are not large, but large yields are obtained from wells on the valley floor just north of Baker. Properly constructed test wells have not been drilled over much of the northern part of the valley floor.
The Tertiary rocks of both volcanic and sedimentary origin along the margin of the valley east of Baker contain some ground water under sufficient pressure to cause wells to flow at the surface, but generally those strata are not highly productive. Some water occurring along fault lines in these rocks has all abnormally high temperature.
The growing season in this area is short and the use of shallow water for irrigation may aid materially in securing the maximum returns of which the valley is capable.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8c8","contributors":{"authors":[{"text":"Trauger, F.D.","contributorId":102520,"corporation":false,"usgs":true,"family":"Trauger","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":242810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51015,"text":"ofr51118 - 1951 - Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida","interactions":[],"lastModifiedDate":"2019-11-14T14:36:42","indexId":"ofr51118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-118","title":"Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr51118","usgsCitation":"Hoy, N., 1951, Occurrence of fresh-water limestones restricts Pliocene deposits in southeastern Florida: U.S. Geological Survey Open-File Report 51-118, 5 p., https://doi.org/10.3133/ofr51118.","productDescription":"5 p.","costCenters":[],"links":[{"id":369223,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0118/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.58447265624999,\n 25.16517336866393\n ],\n [\n -79.91455078125,\n 25.16517336866393\n ],\n [\n -79.91455078125,\n 28.22697003891834\n ],\n [\n -81.58447265624999,\n 28.22697003891834\n ],\n [\n -81.58447265624999,\n 25.16517336866393\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69249f","contributors":{"authors":[{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":242757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3891,"text":"cir122 - 1951 - Index of surface-water records, part 2, South Atlantic and eastern Gulf of Mexico basins, to September 30, 1950","interactions":[],"lastModifiedDate":"2012-02-02T00:05:41","indexId":"cir122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"122","title":"Index of surface-water records, part 2, South Atlantic and eastern Gulf of Mexico basins, to September 30, 1950","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir122","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Index of surface-water records, part 2, South Atlantic and eastern Gulf of Mexico basins, to September 30, 1950: U.S. Geological Survey Circular 122, 20 p. ;27 cm., https://doi.org/10.3133/cir122.","productDescription":"20 p. ;27 cm.","costCenters":[],"links":[{"id":120944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0122/report-thumb.jpg"},{"id":30981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2a22","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":528139,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3378,"text":"cir96 - 1951 - Ground-water resources of the Paintrock irrigation project, Wyoming, with a section on the quality of the water","interactions":[],"lastModifiedDate":"2022-07-07T21:24:00.785636","indexId":"cir96","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96","title":"Ground-water resources of the Paintrock irrigation project, Wyoming, with a section on the quality of the water","docAbstract":"The ground-water conditions of the area covered by the Paintrock irrigation project, in north-central Wyoming, were investigated during the summer of 1947. The purpose of the study was to obtain a general evaluation of ground-water recharge, discharge, and storage in the area now irrigated and in the adjacent areas where additional lands are to be irrigated.
Much of the area covered by this report consists of flat to gently sloping stream terraces and alluvial-bottoms along Nowood, Paintrock, and Medicine Lodge Creeks. The stream-terrace materials consist of fluviatile sand, clay, and gravel. The alluvium is very fine grained and in general has low permeability. The materials underlying the stream terraces and the bottomlands became progressively finer grained and less permeable downstream.
The bedrock formations underlying the area studied range from the Madison limestone of Mississippian age to the Fort Union formation of Paleocene age. Beds have been folded into several prominent structures which trend northwest-southeast across the area. Several of the formations exposed in the area serve as aquifers and yield water to domestic and stock wells. The most important bedrock aquifers are the Fort Union, Lance, Meeteetee, Mesaverde, Frontier, Cloverly and Morrison formations , the Tensleep sandstone, the Amsden formation, and the Madison limestone. More than 7,000 feet of strata are exposed in the area, the older beds being exposed on the western flank of the Big Horn Range near the eastern end of the area.
The quality of the water in the project ranges within wide limits. The concentration of dissolved solids in seven samples of ground water ranges from 279 parts per million for a water in the Tensleep sandstone to 4,590 parts per million for a water in the Morrison formation. The hardness as calcium carbonate (CaCO3) ranges from 13 to 1,680 parts per million. Limited data on the quality of water in Nowood and Paintrock Creeks indicate that these waters are suitable for irrigation. The water in Paintrock Creek near Tensleep is higher in mineral content and hardness than the water upstream at Hyattville as a result of return flow of the irrigation water that is applied to farm lands above Tensleep.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir96","usgsCitation":"Swenson, F.A., Bach, W.K., and Swenson, H.A., 1951, Ground-water resources of the Paintrock irrigation project, Wyoming, with a section on the quality of the water: U.S. Geological Survey Circular 96, Report: ii, 45 p.; Plate: 26.50 x 10.60 inches, https://doi.org/10.3133/cir96.","productDescription":"Report: ii, 45 p.; Plate: 26.50 x 10.60 inches","costCenters":[],"links":[{"id":123573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0096/report-thumb.jpg"},{"id":30391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0096/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":30390,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1951/0096/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":403240,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23947.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","county":"Big Horn County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.052,\n 44.188\n ],\n [\n -107.497,\n 44.188\n ],\n [\n -107.497,\n 44.312\n ],\n [\n -108.052,\n 44.312\n ],\n [\n -108.052,\n 44.188\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a852","contributors":{"authors":[{"text":"Swenson, Frank Albert","contributorId":71958,"corporation":false,"usgs":true,"family":"Swenson","given":"Frank","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bach, W. Kenneth","contributorId":20312,"corporation":false,"usgs":true,"family":"Bach","given":"W.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":146750,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146752,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3354,"text":"cir105 - 1951 - Some aspects of the water supply in the South Coastal basin, California","interactions":[{"subject":{"id":51057,"text":"ofr518 - 1951 - Some aspects of the water supply in the South Coastal Basin, California","indexId":"ofr518","publicationYear":"1951","noYear":false,"title":"Some aspects of the water supply in the South Coastal Basin, California"},"predicate":"SUPERSEDED_BY","object":{"id":3354,"text":"cir105 - 1951 - Some aspects of the water supply in the South Coastal basin, California","indexId":"cir105","publicationYear":"1951","noYear":false,"title":"Some aspects of the water supply in the South Coastal basin, California"},"id":1},{"subject":{"id":52983,"text":"ofr50102 - 1950 - Some aspects of the water supply in the South Coastal Basin, California","indexId":"ofr50102","publicationYear":"1950","noYear":false,"title":"Some aspects of the water supply in the South Coastal Basin, California"},"predicate":"SUPERSEDED_BY","object":{"id":3354,"text":"cir105 - 1951 - Some aspects of the water supply in the South Coastal basin, California","indexId":"cir105","publicationYear":"1951","noYear":false,"title":"Some aspects of the water supply in the South Coastal basin, California"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"105","title":"Some aspects of the water supply in the South Coastal basin, California","docAbstract":"The observation well network in Alabama was started in 1940. Unpublished water-level data collected periodically at 254 observation wells are listed in this report with the location, description, and general information on construction of the observation wells. Publications containing water-level data from selected observation wells are also listed. (USGS)","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir105","usgsCitation":"Troxell, H.C., Poland, J.F., and and others, 1951, Some aspects of the water supply in the South Coastal basin, California: U.S. Geological Survey Circular 105, 10 p. :illus. ;27cm., https://doi.org/10.3133/cir105.","productDescription":"10 p. :illus. ;27cm.","costCenters":[],"links":[{"id":123140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0105/report-thumb.jpg"},{"id":30364,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b3e4b07f02db5321c1","contributors":{"authors":[{"text":"Troxell, Harold Coble","contributorId":48166,"corporation":false,"usgs":true,"family":"Troxell","given":"Harold","email":"","middleInitial":"Coble","affiliations":[],"preferred":false,"id":146712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":146713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528122,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3904,"text":"cir112 - 1951 - Index of surface-water records, part 8, Western Gulf of Mexico basins, to September 30, 1950","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"cir112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"112","title":"Index of surface-water records, part 8, Western Gulf of Mexico basins, to September 30, 1950","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir112","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Index of surface-water records, part 8, Western Gulf of Mexico basins, to September 30, 1950: U.S. Geological Survey Circular 112, 21 p. ;27 cm., https://doi.org/10.3133/cir112.","productDescription":"21 p. ;27 cm.","costCenters":[],"links":[{"id":117431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1951/0112/report-thumb.jpg"},{"id":30991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1951/0112/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f28cd","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":528152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2454,"text":"wsp1116 - 1951 - Surface water supply of the United States, 1948, Part VI, Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"1116","title":"Surface water supply of the United States, 1948, Part VI, Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1116","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Surface water supply of the United States, 1948, Part VI, Missouri River basin: U.S. Geological Survey Water Supply Paper 1116, xiii, 703 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1116.","productDescription":"xiii, 703 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1116/report-thumb.jpg"},{"id":28530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69675a","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":528012,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2462,"text":"wsp1159 - 1951 - Water levels and artesian pressure in observation wells in the United States in 1949, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"1159","title":"Water levels and artesian pressure in observation wells in the United States in 1949, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1159","isbn":"pbk","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1951, Water levels and artesian pressure in observation wells in the United States in 1949, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 1159, vi, 230 p. :ill., tables ;24 cm., https://doi.org/10.3133/wsp1159.","productDescription":"vi, 230 p. :ill., tables ;24 cm.","costCenters":[],"links":[{"id":138211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1159/report-thumb.jpg"},{"id":28538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa17a","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":528020,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13966,"text":"ofr51113 - 1951 - Preliminary report on the ground-water resources of the Navajo and Hopi Indian Reservations, Arizona, New Mexico and Utah","interactions":[{"subject":{"id":13966,"text":"ofr51113 - 1951 - Preliminary report on the ground-water resources of the Navajo and Hopi Indian Reservations, Arizona, New Mexico and Utah","indexId":"ofr51113","publicationYear":"1951","noYear":false,"title":"Preliminary report on the ground-water resources of the Navajo and Hopi Indian Reservations, Arizona, New Mexico and Utah"},"predicate":"SUPERSEDED_BY","object":{"id":38852,"text":"pp521A - 1969 - Regional hydrogeology of the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah, with a section on vegetation","indexId":"pp521A","publicationYear":"1969","noYear":false,"chapter":"A","title":"Regional hydrogeology of the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah, with a section on vegetation"},"id":1}],"supersededBy":{"id":38852,"text":"pp521A - 1969 - Regional hydrogeology of the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah, with a section on vegetation","indexId":"pp521A","publicationYear":"1969","noYear":false,"title":"Regional hydrogeology of the Navajo and Hopi Indian Reservations, Arizona, New Mexico, and Utah, with a section on vegetation"},"lastModifiedDate":"2012-02-02T00:07:01","indexId":"ofr51113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","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":"51-113","title":"Preliminary report on the ground-water resources of the Navajo and Hopi Indian Reservations, Arizona, New Mexico and Utah","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr51113","usgsCitation":"Halpenny, L.C., and Harshbarger, J.W., 1951, Preliminary report on the ground-water resources of the Navajo and Hopi Indian Reservations, Arizona, New Mexico and Utah (Superseded by: P-521-A): U.S. Geological Survey Open-File Report 51-113, 13 p. ;27 cm., https://doi.org/10.3133/ofr51113.","productDescription":"13 p. ;27 cm.","costCenters":[],"links":[{"id":95183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1951/0113/report.pdf","size":"7725","linkFileType":{"id":1,"text":"pdf"}},{"id":147771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1951/0113/report-thumb.jpg"}],"edition":"Superseded by: P-521-A","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c83e","contributors":{"authors":[{"text":"Halpenny, Leonard Cameron","contributorId":66698,"corporation":false,"usgs":true,"family":"Halpenny","given":"Leonard","email":"","middleInitial":"Cameron","affiliations":[],"preferred":false,"id":168712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harshbarger, John William","contributorId":53765,"corporation":false,"usgs":true,"family":"Harshbarger","given":"John","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":168711,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3745,"text":"cir133 - 1951 - Detroit River group in the Michigan basin","interactions":[],"lastModifiedDate":"2017-01-11T10:51:30","indexId":"cir133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1951","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"133","title":"Detroit River group in the Michigan basin","docAbstract":"This report attempts to correlate the outcropping rocks in the type locality of the Detroit River group with the thick sequence of rocks that has been explored by many drilled wells in the Michigan Basin during the last twenty years. The surface nomenclature as recently revised (Ehlers, 1950) is suggested for the subsurface section in place of the heterogeneous collection of names now used. The present work revises earlier reports by the writer (1945, a, b, c).
During the preparation of this report the samples have been examined from more than 300 wells and cores from 9 wells. The writer has also drawn upon the work of Enyert (1949) who wrote a Doctoral thesis on the sandstones of the Detroit River group, and upon Master's theses on various phases of Detroit River stratigraphy written by Cooley (1947), Saunders .(1948), and Tharp (1944). Finally the writer has had the advantage of many consultations in office and field with George V. Cohee of the U. S. Geological Survey, Professors G. M. Ehlers and E. C. Stumm of the University of Michigan, and with other geologists of Michigan and Ontario, especially George D. Lindberg (Sun Oil Company, Toledo), E. J. Baltrusaitis and K. A. Gravelle (Gulf Refining Company, Saginaw), Willard A. Sanger (Pure Oil Company, Clare), Joseph Lindsay and George WinSton (Carter Oil Co. , Grand Rapids), and Charles S. Evans (Union Gas Co. , Chatham, Ontario). It is a pleasure to acknowledge the help received from these geologists and to thank them for it.
The surface and subsurface sections through the Detroit River group in Canada are not included in this report.
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