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,{"id":70175515,"text":"70175515 - 1974 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1972","interactions":[],"lastModifiedDate":"2017-06-14T11:11:06","indexId":"70175515","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175515","usgsCitation":"Steger, R., 1974, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1972: Open-File Report, 102 p., https://doi.org/10.3133/70175515.","productDescription":"102 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326538,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43951e4b03bcb01039ff9","contributors":{"authors":[{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":645546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70175503,"text":"70175503 - 1974 - Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972","interactions":[],"lastModifiedDate":"2021-11-09T20:27:51.682147","indexId":"70175503","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972","docAbstract":"<p>The U.S. Soil Conservation Service is actively engaged in the installation of flood- and soil-erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of approximately 3,500 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1972, 1,551 of these structures had been built.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175503","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Hampton, B., 1974, Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972: Open-File Report, 26 p., https://doi.org/10.3133/70175503.","productDescription":"26 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":391527,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70175503/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":326500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70175503/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Pin Oak Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bde4b03bcb0102e8ef","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":645512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010061,"text":"70010061 - 1974 - Water quality effects of seepage from earthen dams","interactions":[],"lastModifiedDate":"2025-04-10T15:22:23.400638","indexId":"70010061","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Water quality effects of seepage from earthen dams","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>Analyses of surface and seepage waters from selected floodwater retarding structures in west-central Oklahoma, U.S.A. show the salinity of seepage to be several times greater than that of the impounded waters. The increases in concentration of the several chemical components are not proportional. This phenomenon appears to be caused largely by simple solution, which is closely related to the chemical character of the geologic formation that provides the reservoir site and the earth fill of the dam. Concentration of certain chemical components in the seepage water progressively decreases as the structure ages. This is probably a function of depletion, which is related to the amounts and solubility of the parent materials subjected to solution. In contrast, the concentration of certain other components, such as iron and calcium, increases with time. The chemical activities within the accumulating mud on the bottom of the reservoir apparently cause these increases.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(74)90059-6","issn":"00221694","usgsCitation":"Yost, C., and Naney, J., 1974, Water quality effects of seepage from earthen dams: Journal of Hydrology, v. 21, no. 1, p. 15-26, https://doi.org/10.1016/0022-1694(74)90059-6.","productDescription":"12 p.","startPage":"15","endPage":"26","costCenters":[],"links":[{"id":219126,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"west-central Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.16259765625,\n              34.27083595165\n            ],\n            [\n              -97.05322265625,\n              34.27083595165\n            ],\n            [\n              -97.05322265625,\n              35.782170703266075\n            ],\n            [\n              -99.16259765625,\n              35.782170703266075\n            ],\n            [\n              -99.16259765625,\n              34.27083595165\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"21","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc894e4b08c986b32c9d9","contributors":{"authors":[{"text":"Yost, C. Jr.","contributorId":39514,"corporation":false,"usgs":true,"family":"Yost","given":"C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Naney, J.W.","contributorId":48308,"corporation":false,"usgs":true,"family":"Naney","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":357808,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42456,"text":"ofr741023 - 1974 - Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","interactions":[{"subject":{"id":42456,"text":"ofr741023 - 1974 - Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","indexId":"ofr741023","publicationYear":"1974","noYear":false,"title":"Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","indexId":"70046305","publicationYear":"1977","noYear":false,"title":"Ground-water resources of Griggs and Steele Counties, North Dakota"},"id":1}],"supersededBy":{"id":70046305,"text":"70046305 - 1977 - Ground-water resources of Griggs and Steele Counties, North Dakota","indexId":"70046305","publicationYear":"1977","noYear":false,"title":"Ground-water resources of Griggs and Steele Counties, North Dakota"},"lastModifiedDate":"2023-03-06T14:04:34.585183","indexId":"ofr741023","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"74-1023","title":"Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota","docAbstract":"<p>This investigation is part of a statewide program to determine the location, extent, and hydrologic characteristics of the ground-water reservoirs (aquifers).</p><p>The investigation was made cooperatively by the U.S. Geological Survey, North Dakota State Water Commission, North Dakota Geological Survey, and Griggs and Steele Counties Water Management Districts.</p><p>This preliminary map is the first product of an intensive study of Griggs and Steele Counties. A well inventory provided data on depth, construction, and productivity of private and public wells. Test drilling by the North Dakota State Water Commission, Federal agencies, and commercial well drillers provided information regarding the thickness, grain size, and extent of the aquifers. Potential well yields were estimated from the thickness and hydraulic conductivity of the water-bearing materials logged at each test hole, and from aquifer tests. Generally, the yield of a well is proportional to the hydraulic conductivity and thickness of the aquifer.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741023","collaboration":"Prepared in cooperation with the North Dakota State Water Commission, North Dakota Geological Survey, and Griggs and Steele Counties Water Management Districts","usgsCitation":"Downey, J.S., 1974, Preliminary map showing availability of ground water from major glacial-drift aquifers in Griggs and Steele Counties, North Dakota: U.S. Geological Survey Open-File Report 74-1023, 1 Plate: 35.29  21.60 inches, https://doi.org/10.3133/ofr741023.","productDescription":"1 Plate: 35.29  21.60 inches","costCenters":[],"links":[{"id":136614,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1023/report-thumb.jpg"},{"id":412566,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"126720","country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4504,47.6742 ], [ -97.4504,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696910","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":226526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58919,"text":"mf607 - 1974 - Map showing areas serviced by public water-supply agencies in 1973 greater Pittsburgh region, southwestern Pennsylvania","interactions":[],"lastModifiedDate":"2023-08-31T21:11:30.427931","indexId":"mf607","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"607","title":"Map showing areas serviced by public water-supply agencies in 1973 greater Pittsburgh region, southwestern Pennsylvania","docAbstract":"Urban water planning, development, and management are many sectored, costly efforts, subject to a multitude of controls and demands including those imposed by nature. One primary concern in development is for providing a dependable and safe water supply. In spite of a bountiful natural availability, the process of satisfying consumer needs involves the resolution of a variety of problems, not the least of which are cooperation and coordination among suppliers. One of the fundamental requisites in seeking sound solutions to developmental and environmental problems is inventory documentation. This map is one facet of documentation; the data listing, given on sheet 2, is the companion inventory. These supplement State, regional, and local efforts directed toward both long-range planning and current evaluation programs. Such documentation also assists the assessment of the effect of one water-management subsystem on hydrologic characteristics.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf607","usgsCitation":"Beall, R.M., 1974, Map showing areas serviced by public water-supply agencies in 1973 greater Pittsburgh region, southwestern Pennsylvania: U.S. Geological Survey Miscellaneous Field Studies Map 607, 2 Plates: 45.40 x 48.57 inches and 31.65 x 36.09 inches, https://doi.org/10.3133/mf607.","productDescription":"2 Plates: 45.40 x 48.57 inches and 31.65 x 36.09 inches","costCenters":[],"links":[{"id":183412,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0607/report-thumb.jpg"},{"id":278824,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0607/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":278823,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0607/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420388,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19237.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"125000","country":"United States","state":"Pennsylvania","otherGeospatial":"greater Pittsburgh Region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.5,39.916667 ], [ -80.5,41.2 ], [ -79.0,41.2 ], [ -79.0,39.916667 ], [ -80.5,39.916667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db659433","contributors":{"authors":[{"text":"Beall, Robert M.","contributorId":90695,"corporation":false,"usgs":true,"family":"Beall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":261097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68081,"text":"ha535 - 1974 - Ground-water favorability and surficial geology of the Machias-Lubec area, Washington County, Maine","interactions":[],"lastModifiedDate":"2023-03-13T19:05:59.086712","indexId":"ha535","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"535","title":"Ground-water favorability and surficial geology of the Machias-Lubec area, Washington County, Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha535","usgsCitation":"Prescott, G., 1974, Ground-water favorability and surficial geology of the Machias-Lubec area, Washington County, Maine: U.S. Geological Survey Hydrologic Atlas 535, 3 Plates: 32.00 x 44.00 inches or smaller, https://doi.org/10.3133/ha535.","productDescription":"3 Plates: 32.00 x 44.00 inches or smaller","costCenters":[],"links":[{"id":89342,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/535/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398648,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15926.htm"},{"id":89341,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/535/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89340,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/535/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","country":"United States","state":"Maine","county":"Washington County","otherGeospatial":"Machias-Lubec area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.5,\n              44.55\n            ],\n            [\n              -66.917,\n              44.55\n            ],\n            [\n              -66.917,\n              44.917\n            ],\n            [\n              -67.5,\n              44.917\n            ],\n            [\n              -67.5,\n              44.55\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce1a","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68078,"text":"ha529 - 1974 - Ground-water favorability and surficial geology of the Cherryfield-Jonesboro area, Maine","interactions":[],"lastModifiedDate":"2023-03-13T19:06:51.921127","indexId":"ha529","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"529","title":"Ground-water favorability and surficial geology of the Cherryfield-Jonesboro area, Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha529","usgsCitation":"Prescott, G., 1974, Ground-water favorability and surficial geology of the Cherryfield-Jonesboro area, Maine: U.S. Geological Survey Hydrologic Atlas 529, 1 Plate: 37.00 × 41.25 inches, https://doi.org/10.3133/ha529.","productDescription":"1 Plate: 37.00 × 41.25 inches","costCenters":[],"links":[{"id":89339,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/529/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187923,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398606,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15919.htm"}],"scale":"62500","country":"United States","state":"Maine","otherGeospatial":"Cherryfield-Jonesboro area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -68,\n              44.423\n            ],\n            [\n              -67.5,\n              44.423\n            ],\n            [\n              -67.5,\n              44.75\n            ],\n            [\n              -68,\n              44.75\n            ],\n            [\n              -68,\n              44.423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce57","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48119,"text":"ofr7365 - 1973 - Reconnaissance of the water resources in the vicinity of proposed deep-well injection sites in southeast Dade County, Florida","interactions":[],"lastModifiedDate":"2025-04-14T17:15:52.972634","indexId":"ofr7365","displayToPublicDate":"2022-01-03T22:15:00","publicationYear":"1973","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":"73-65","title":"Reconnaissance of the water resources in the vicinity of proposed deep-well injection sites in southeast Dade County, Florida","docAbstract":"<p>Deep-well injection has been selected by the Dade County Water and Sewer Authority as a means of disposing treated waste water in southeast Dade County. Preliminary plans call for the construction of a county-owned sanitary sewage treatment plant and several 3,000-foot deep injection wells at 1,000-foot intervals on Levee 31E. As a first stage, drilling of seven wells, capable of accepting, in the aggregate, 30 mgd (million gallons per day) of treated liquid waste, is planned. The locations of the proposed sites (fig. 1) were selected by the consultants for the Authority.</p><p>A reconnaissance was made in the vicinity of the proposed well sites to determine the chloride content of surface and ground water because this information is needed to formulate plans for the safe disposal of salt water during drilling and testing of the injection wells. The reconnaissance was part of a cooperative program with the Dade County Water and Sewer Authority to investigate the hydrologic effects of injecting treated waste water into a deep-saline aquifer.</p><p>The area of investigation is near Cutler Ridge in southeast Dade County. It occupies about 51/2 square miles bounded on the east by S.W. 77th Avenue extended, on the west by S.W. 97th Avenue, on the south by Coconut Palm Drive, and on the north by Old Cutler Road (fig. 1). The area for the investigation was selected by the Authority and their consultants.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr7365","collaboration":"Prepared in cooperation with the Dade County Water and Sewer Authority","usgsCitation":"Earle, J., and Meyer, F., 1973, Reconnaissance of the water resources in the vicinity of proposed deep-well injection sites in southeast Dade County, Florida: U.S. Geological Survey Open-File Report 73-65, 20 p., https://doi.org/10.3133/ofr7365.","productDescription":"20 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":484522,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0065/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0065/report-thumb.jpg"}],"country":"United 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 \"}}]}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6369cc","contributors":{"authors":[{"text":"Earle, J.E.","contributorId":41037,"corporation":false,"usgs":true,"family":"Earle","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":236839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, F.W.","contributorId":25150,"corporation":false,"usgs":true,"family":"Meyer","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":236838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70178885,"text":"70178885 - 1973 - Hydrologic reconnaissance of Pilot Valley, Utah and Nevada","interactions":[],"lastModifiedDate":"2016-12-10T10:11:09","indexId":"70178885","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"41","title":"Hydrologic reconnaissance of Pilot Valley, Utah and Nevada","docAbstract":"<p>This report, prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, is the twelfth in a series of reports that describe the water resources of the western basins of Utah. (See fig. 1.) Its purpose is to present available hydrologic data on the Pilot Valley area, to provide an evaluation of the potential for water-resource development in the area, and to identify studies that would improve understanding of the area's water supply.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Stephens, J.C., and Hood, J.W., 1973, Hydrologic reconnaissance of Pilot Valley, Utah and Nevada: Technical Publication 41, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331853,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-100"},{"id":331852,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-100"}],"country":"United States","state":"Nevada, Utah","county":"Box Elder County, Elko County, Tooele County","otherGeospatial":"Pilot Valley","geographicExtents":" {\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.510498046875,\n              39.90973623453719\n            ],\n            [\n              -114.510498046875,\n              41.15384235711447\n            ],\n            [\n              -113.08227539062499,\n              41.15384235711447\n            ],\n            [\n              -113.08227539062499,\n              39.90973623453719\n            ],\n            [\n              -114.510498046875,\n              39.90973623453719\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584d222fe4b0f574cb6e9607","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":655454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156922,"text":"70156922 - 1973 - Bibliography of published reports by the U.S. Geological Survey personnel on the geology and hydrology of the Amchitka Supplementary Test Area, Aleutian Islands, Alaska, 1969-1972","interactions":[],"lastModifiedDate":"2019-11-12T16:17:02","indexId":"70156922","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Bibliography of published reports by the U.S. Geological Survey personnel on the geology and hydrology of the Amchitka Supplementary Test Area, Aleutian Islands, Alaska, 1969-1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156922","usgsCitation":"1973, Bibliography of published reports by the U.S. Geological Survey personnel on the geology and hydrology of the Amchitka Supplementary Test Area, Aleutian Islands, Alaska, 1969-1972, 15 p., https://doi.org/10.3133/70156922.","productDescription":"15 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308062,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156922.JPG"},{"id":308544,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156922/report.pdf","text":"Report","size":"2,389 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Islands, Amchitka Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              178.584136963,\n              51.63677159243599\n            ],\n            [\n              178.592376709,\n              51.61290019118336\n            ],\n            [\n              179.21585083,\n              51.3254629443313\n            ],\n            [\n             179.508361816,\n              51.37520943448463\n            ],\n            [\n              179.057922363,\n              51.587309751245456\n            ],\n            [\n              178.628082275,\n              51.67936786087718\n            ],\n            [\n              178.584136963,\n              51.63677159243599\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f2a9ace4b0dacf699ec6aa","contributors":{"compilers":[{"text":"Ohl, Jane P.","contributorId":104062,"corporation":false,"usgs":true,"family":"Ohl","given":"Jane","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571146,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":70047488,"text":"70047488 - 1973 - Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","interactions":[{"subject":{"id":24343,"text":"ofr71241 - 1971 - A preliminary evaluation of hydrologic conditions of the Lakeland Ridge area of Polk County, Florida","indexId":"ofr71241","publicationYear":"1971","noYear":false,"title":"A preliminary evaluation of hydrologic conditions of the Lakeland Ridge area of Polk County, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047488,"text":"70047488 - 1973 - Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","indexId":"70047488","publicationYear":"1973","noYear":false,"title":"Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:59:54","indexId":"70047488","displayToPublicDate":"2013-01-01T15:31:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":283,"text":"Florida Bureau of Geology Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"64","title":"Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","docAbstract":"The Lakeland ridge area of this investigation covers about 300 square miles in northwest Polk County in central Florida. The growth of industry, phosphate mining, and citrus production as well as population growth during the last two decades has resulted in an increase in ground-water pumpage from about 11 billion gallons in 1950 to 27 billion gallons in 1970.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by United States Geological Survey in cooperation with Southwest Florida Water Management District the City of Lakeland, Florida and the Bureau of Geology Florida Department of Natural Resources","usgsCitation":"Robertson, A.F., 1973, Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida: Florida Bureau of Geology Report of Investigations 64, vii, 48 p.","productDescription":"vii, 48 p.","costCenters":[],"links":[{"id":276182,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047488.PNG"},{"id":276181,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001251/00001/pdf?search=report+%3dinvestigations"}],"country":"United States","state":"Florida","county":"Polk County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.1062,27.6432 ], [ -82.1062,28.3619 ], [ -81.131,28.3619 ], [ -81.131,27.6432 ], [ -82.1062,27.6432 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37ae4b02bdb1bc63fbc","contributors":{"authors":[{"text":"Robertson, Alton F.","contributorId":71177,"corporation":false,"usgs":true,"family":"Robertson","given":"Alton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":482174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047603,"text":"70047603 - 1973 - Ground-water resources of Brazoria County, Texas","interactions":[{"subject":{"id":57139,"text":"ofr70377 - 1970 - Ground-water resources of Brazoria County, Texas","indexId":"ofr70377","publicationYear":"1970","noYear":false,"title":"Ground-water resources of Brazoria County, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047603,"text":"70047603 - 1973 - Ground-water resources of Brazoria County, Texas","indexId":"70047603","publicationYear":"1973","noYear":false,"title":"Ground-water resources of Brazoria County, Texas"},"id":1}],"lastModifiedDate":"2013-08-14T12:56:02","indexId":"70047603","displayToPublicDate":"2013-01-01T10:55:28","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"163","title":"Ground-water resources of Brazoria County, Texas","docAbstract":"The Chicot and Evangeline aquifers are the only hydrologic units bearing fresh (less than 1,000 milligrams per liter dissolved solids) or slightly saline water (1,000-3,000 milligrams per liter dissolved solids in Brazoria County. These aquifers are composed of gravel, sand, silt, and clay of Pliocene, Pleistocene, and Holocene age.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Water Development Board; Reprinted by the Texas Department of Water Resources December 1982","usgsCitation":"Sandeen, W.M., and Wesselman, J.B., 1973, Ground-water resources of Brazoria County, Texas: Report 163, v, 64 p.","productDescription":"v, 64 p.","numberOfPages":"40","costCenters":[],"links":[{"id":276596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047603.png"},{"id":276595,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.state.tx.us/publications/reports/numbered_reports/doc/R163/report163.asp"}],"country":"United States","state":"Texas","county":"Brazoria County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.8721,28.8214 ], [ -95.8721,29.5991 ], [ -95.0561,29.5991 ], [ -95.0561,28.8214 ], [ -95.8721,28.8214 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e6e4b081fa6136d3f1","contributors":{"authors":[{"text":"Sandeen, William M.","contributorId":32533,"corporation":false,"usgs":true,"family":"Sandeen","given":"William","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":482507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wesselman, John B.","contributorId":52154,"corporation":false,"usgs":true,"family":"Wesselman","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":482508,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047244,"text":"70047244 - 1973 - A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen","interactions":[],"lastModifiedDate":"2013-07-26T10:37:43","indexId":"70047244","displayToPublicDate":"2013-01-01T10:25:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":301,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"32","title":"A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen","docAbstract":"The results of drilling test holes to depths of approximately 1,000 feet in the Mud Lake region show that a large part of the region is underlain by both sedimentary deposits and basalt flows. At some locations, predominantly sedimentary deposits were penetrated; at others, basalt flows predominated. The so-called Mud Lake-Market Lake barrier denotes a change in geology. From the vicinity of the barrier area, as described by Stearns, Crandall, and Steward (1938, p. 111), up the water-table gradient for at least a few tens of miles, the saturated geologic section consists predominantly of beds of sediments that are intercalated with numerous basalt flows. Downgradient from the barrier, sedimentary deposits are not common and practically all the water-bearing formations are basalt, at least to the depths explored so far. Thus, the barrier is a transition zone from a sedimentary-basaltic sequence to a basaltic sequence. The sedimentary-basaltic sequence forms a complex hydrologic system in which water occurs under water-table conditions in the upper few tens of feet of saturated material and under artesian conditions in the deeper material in the southwest part of the region. The well data indicate that southwest of the barrier, artesian pressures are not significant. Southwest of the barrier, few sedimentary deposits occur in the basalt section and, as described by Mundorff, Crosthwaite, and Kilburn (1964). ground water occurs in a manner typical of the Snake Plain aquifer. In several wells, artesian pressures are higher in the deeper formations than in the shallower ones, but the reverse was found in a few wells. The available data are not adequate to describe the water-bearing characteristics of the artesian aquifer nor the effects that pumping in one zone would have on adjacent zones. The water-table aquifer yields large quantities of water to irrigation wells.","language":"English","publisher":"Idaho Department of Water Administration","publisherLocation":"Boise City, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with Idaho Department of Water Administration","usgsCitation":"Crosthwaite, E., 1973, A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen: Water Information Bulletin 32, vii, 60 p.; Figures.","productDescription":"vii, 60 p.; Figures","numberOfPages":"73","costCenters":[],"links":[{"id":275431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047244.png"},{"id":275430,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib32-mud_lake_arco_aberdeen.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake Plain Aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a62e4b0a32220222f52","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":481487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046308,"text":"70046308 - 1973 - Ground-water basic data for Griggs and Steele Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-05-23T12:56:45","indexId":"70046308","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64-2","title":"Ground-water basic data for Griggs and Steele Counties, North Dakota","docAbstract":"The objectives of the hydrologic investigation in Griggs and Steele Counties, N. Dak. (fig. 1) were to: (1) determine the location, extent, and nature of the major aquifers; (2) evaluate the occurrence and movement of ground water, including recharge and discharge; (3) estimate the quantities of water stored in the aquifers; (4) estimate the potential yields of wells tapping the major aquifers; and (5) determine the chemical quality of the ground water.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the North Dakota Geological Survey, North Dakota State Water Commission, Griggs County Water Management District and the Steele County Water Management District; this report was also published as North Dakota County Ground-Water Studies 21-2","usgsCitation":"Downey, J.S., 1973, Ground-water basic data for Griggs and Steele Counties, North Dakota: Bulletin 64-2, ii, 468 p.","productDescription":"ii, 468 p.","numberOfPages":"470","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":273371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046308.png"},{"id":273369,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-253/GriggsSteele_Part_2.pdf"},{"id":273370,"type":{"id":17,"text":"Plate"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-254/Griggs_and_Steele_Part2_Plates.pdf"}],"country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4505,47.6742 ], [ -97.4505,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd2e4b022a6a540f9cf","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":479434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48111,"text":"ofr7334 - 1973 - Hydrology of the Bayou Bartholomew alluvial aquifer-stream system, Arkansas","interactions":[],"lastModifiedDate":"2013-07-16T12:53:22","indexId":"ofr7334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-34","title":"Hydrology of the Bayou Bartholomew alluvial aquifer-stream system, Arkansas","docAbstract":"The study area comprises about 3,200 square miles of the Mississippi Alluvial Plain in southeast Arkansas. About 90 percent of the area drains south to the Ouachita River in Louisiana. The alluvial aquifer and the streams are hydraulically connected and are studied as an aquifer-stream system. Bayou Bartholomew is a principal stream of the system. The aquifer is underlain by confining strata of the Jackson Group and Cockfield Formation. The mean annual surface-water yield of the area that drains to the Ouachita River basin is nearly 2 million acre-feet. Flood-control projects have significantly reduced flooding in the area. Basin boundaries and low-flow characteristics of streams have been altered as a result of the flood-control projects and streamflow diversion for irrigation. The direction of ground-water flow generally is southward. Bayou Bartholomew functions mostly as a drain for ground-water flow from the west and as a recharge source to the aquifer east of the bayou. As a result of navigation pools, the Arkansas River is mostly a steady-recharge source to the aquifer. Pumpage from the aquifer and streams increased from about 20,000 acre-feet in 1941 to 237,000 acre-feet in 1970. Estimates of flow, derived from analog analysis but lacking field verification, indicate that recharge to the aquifer in 1970 was about 161,000 acre-feet. About 70 percent of the recharge was by capture from streams as a result of ground-water pumpage. Discharge from the aquifer was about 233,000 acre-feet. About 80 percent of the discharge was through wells. Stream diversion in 1970 from capture and open channel, excluding capture from the Arkansas and Mississippi Rivers, was about 110,000 acre-feet. Return flow to streams from rice irrigation and fishponds was about 60,000 acre-feet. The chemical quality of streamflows is excellent for irrigation. Water from the aquifer generally ranges from permissible to excellent for irrigation. The use of water from the aquifer in the flood-plain area, exclusive of irrigation, is severely limited unless it is treated to remove the iron and reduce the hardness.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7334","collaboration":"Prepared in cooperation with the Arkansas Geological Commission","usgsCitation":"Broom, M., and Reed, J., 1973, Hydrology of the Bayou Bartholomew alluvial aquifer-stream system, Arkansas: U.S. Geological Survey Open-File Report 73-34, vi, 91 p., https://doi.org/10.3133/ofr7334.","productDescription":"vi, 91 p.","costCenters":[],"links":[{"id":162201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0034/report-thumb.jpg"},{"id":271060,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0034/report.pdf"}],"country":"United States","state":"Arkansas","otherGeospatial":"Mississippi Alluvial Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6448,36.4997 ], [ -89.6448,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f26","contributors":{"authors":[{"text":"Broom, M.E.","contributorId":91147,"corporation":false,"usgs":true,"family":"Broom","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":236828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":236827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27646,"text":"wri7329 - 1973 - Electric-analog simulation network of unconsolidated aquifers in the upper Wabash River basin, Indiana","interactions":[],"lastModifiedDate":"2018-11-02T10:30:32","indexId":"wri7329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-29","title":"Electric-analog simulation network of unconsolidated aquifers in the upper Wabash River basin, Indiana","docAbstract":"<p>The ground-water budget of the unconsolidated deposits in the upper Wabash River basin was modeled. An electrical-simulation network was used to determine an integrated storage coefficient of 0.003 for the basin. Two practical problems were investigated: a municipal pumping problem and the change in flow regime due to the addition of surface-water reservoirs to the basin. Because these are demonstration exercises, the information presented is not intended to be used for construction justification. The network is available and can be used to determine the effect on basin hydrology due to local development of the ground-water resource.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7329","usgsCitation":"Heisel, J.E., 1973, Electric-analog simulation network of unconsolidated aquifers in the upper Wabash River basin, Indiana: U.S. Geological Survey Water-Resources Investigations Report 73-29, iv, 26 p., https://doi.org/10.3133/wri7329.","productDescription":"iv, 26 p.","costCenters":[],"links":[{"id":158810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0029/report-thumb.jpg"},{"id":359112,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Upper Wabash River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.5,\n              40.25\n            ],\n            [\n              -84.5,\n              40.25\n            ],\n            [\n              -84.5,\n              41.25\n            ],\n            [\n              -86.5,\n              41.25\n            ],\n            [\n              -86.5,\n              40.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60734a","contributors":{"authors":[{"text":"Heisel, James E.","contributorId":68378,"corporation":false,"usgs":true,"family":"Heisel","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27662,"text":"wri738 - 1973 - Hydrology and recreation of selected cold-water rivers of the Saint Lawrence River Basin in Michigan, New York, and Wisconsin","interactions":[],"lastModifiedDate":"2019-07-10T09:53:16","indexId":"wri738","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-8","title":"Hydrology and recreation of selected cold-water rivers of the Saint Lawrence River Basin in Michigan, New York, and Wisconsin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri738","usgsCitation":"Hendrickson, G.E., Knutilla, R., and Doonan, C.J., 1973, Hydrology and recreation of selected cold-water 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E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knutilla, R. L.","contributorId":65451,"corporation":false,"usgs":true,"family":"Knutilla","given":"R. L.","affiliations":[],"preferred":false,"id":198490,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198489,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41943,"text":"ofr73138 - 1973 - Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas","interactions":[],"lastModifiedDate":"2016-08-23T16:37:52","indexId":"ofr73138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-138","title":"Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas","docAbstract":"<p>Because of increasing concern about the continuing decline of water levels in the Houston area, an electric analog model was used to determine the effects on the potentiometric surfaces resulting from recharging water through wells along the Houston Ship Channel into the two major aquifers, the Chicot and Evangeline.</p><p>The model conditions simulated for this study are too complex to be described in detail. The upper model layer simulated the hydrologic conditions in the lower unit of the Chicot aquifer undifferentiated. The simulation included clay compaction and vertical leakage as well as transmissivity and storage. The lower model layer simulated the hydrologic conditions in the Evangeline aquifer which underlies the Chicot aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73138","collaboration":"Prepared in cooperation with the City of Houston and Texas Water Development Board","usgsCitation":"Jorgensen, D.G., 1973, Analog-model studies of the effects of recharge wells along the Houston Ship Channel on potentiometric surfaces of the Chicot and Evangeline aquifers, Houston, Texas: U.S. Geological Survey Open-File Report 73-138, 2 Plates: 15.48 x 21.26 inches x 15.78 x 21.23 inches, https://doi.org/10.3133/ofr73138.","productDescription":"2 Plates: 15.48 x 21.26 inches x 15.78 x 21.23 inches","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr73138.JPG"},{"id":79670,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79671,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0138/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683991","contributors":{"authors":[{"text":"Jorgensen, D. G.","contributorId":104527,"corporation":false,"usgs":true,"family":"Jorgensen","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":225753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27037,"text":"wri7313 - 1973 - Ground-water hydrology of northern Napa Valley, California","interactions":[],"lastModifiedDate":"2020-08-08T00:26:00.663327","indexId":"wri7313","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-13","title":"Ground-water hydrology of northern Napa Valley, California","docAbstract":"<p><span>The alluvium of northern Napa Valley is the principal aquifer of the </span><span>area and is capable of yielding as much as 3,000 gallons per minute to wells. </span><span>Generally the larger-yielding wells are along the Napa River where the </span><span>alluvium is thickest and most permeable. Recharge to the alluvium is chiefly </span><span>by percolation from streams and infiltration of precipitation. Discharge is </span><span>chiefly flow to the Napa River, evapotranspiration, and pumpage from wells. </span><span>Both recharge to, and discharge from, the alluvial aquifer are sensitively </span><span>influenced by rainfall. About 190,000 acre-feet of water is presently (1972) </span><span>stored in the alluvium of northern Napa Valley. Future annual water use in </span><span>the project area will probably vary between 12,000 and 35,000 acre-feet and, </span><span>for most purposes, can be supplied by the alluvial aquifer even during </span><span>extended periods of limited rainfall. Generally low transmissivities in the </span><span>alluvium, however, limit the opportunity for obtaining sustained, large yields </span><span>from wells in much of the valley and require that large-scale development and </span><span>operation of wells in much of the area be planned and synchronized.</span></p><p><span>Sustained drought conditions in the Napa Valley accompanied by expected increases in the use of ground water will probably cause significant reductions in the base flow of the Napa River and cause many shallow wells in the area to dry up. </span></p><p><span>Sodium chloride ground water occurs near Calistoga and in the vicinity of Oakville and in some places is not suitable for irrigation. Model studies indicate that limited migration of sodium chloride water into intensively pumped parts of the aquifer probably will not be a serious problem.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7313","collaboration":"Prepared in cooperation with the Napa County Flood Control and Water Conservation District","usgsCitation":"Faye, R.E., 1973, Ground-water hydrology of northern Napa Valley, California: U.S. Geological Survey Water-Resources Investigations Report 73-13, Report: vi, 64 p.; 1 Figure: 32.18 x 21.92 inches, https://doi.org/10.3133/wri7313.","productDescription":"Report: vi, 64 p.; 1 Figure: 32.18 x 21.92 inches","costCenters":[],"links":[{"id":158580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0013/report-thumb.jpg"},{"id":377248,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/wri/1973/0013/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377247,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Napa Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.66666667,\n              38.33333333\n            ],\n            [\n              -122.25,\n              38.33333333\n            ],\n            [\n              -122.25,\n              38.61666667\n            ],\n            [\n              -122.66666667,\n              38.61666667\n            ],\n            [\n              -122.66666667,\n              38.33333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d497","contributors":{"authors":[{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24797,"text":"ofr73358 - 1973 - Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"ofr73358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-358","title":"Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","docAbstract":"This is a study of the feasibility of recharging, in the Waterman Canyon-East Twin Creek area, imported water from northern California by way of the State Water Project beginning in 1972. \r\n\r\nThe feasibility of recharging 30,000 acre-feet of water a year in the Waterman Canyon-East Twin Creek area will depend on the effectiveness of fault K as a barrier to ground-water movement near the land surface. The results of test drilling and an infiltration test indicate that the subsurface material at the spreading grounds is permeable enough to allow recharged water to percolate to the water table. The data indicate that fault K extends into the Waterman Canyon-East Twin Creek area and may impede the lateral movement of recharged water. Fault K has no known surface expression and therefore probably does not affect the highly permeable younger alluvium. If that is so, fault K will be less effective as a barrier to ground-water movement as the recharge mound rises. Monitoring of the observation wells near the spreading grounds as the planned recharge operation proceeds should provide data about the hydrologic effects of fault K near the land surface.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr73358","issn":"0094-9140","usgsCitation":"Warner, J.W., and Moreland, J.A., 1973, Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California: U.S. Geological Survey Open-File Report 73-358, iv, 44 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr73358.","productDescription":"iv, 44 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0358/report-thumb.jpg"},{"id":53810,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0358/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c47","contributors":{"authors":[{"text":"Warner, J. W.","contributorId":42996,"corporation":false,"usgs":true,"family":"Warner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moreland, J. A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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