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Upstream from the Massachusetts State line the Hoosic River drains a total of 205 mi<sup>2</sup> (531 km<sup>2</sup>) of which 164 mi<sup>2</sup> (425 km<sup>2</sup>) are in Massachusetts, 29 mi<sup>2</sup> (101 km<sup>2</sup>) are in Vermont, and 2 mi<sup>2</sup> (5 km<sup>2</sup>) are in New York. This report contains hydrologic data for that part inside Massachusetts and includes all, or parts of, the towns of Adams, Cheshire, Clarksburg, Dalton, Florida, Hancock, Lanesborough, New Ashford, North Adams, Savoy, Williamstown, and Windsor.</p><p>The data tabulated here were collected during an investigation of the water resources of the Hoosic River basin in Massachusetts by the U.S. Geological Survey in cooperation with the Massachusetts Water Resources Commission. This report is released to make available to the public basic hydrologic and related information that will facilitate the planning of water-resources development and complements an interpretive report of the area (Hansen and others, 1973).</p><p>Data presented include selected information on wells, test borings, springs, seismic surveys, streamflow records, chemical analyses of surface and ground water and of rainfall, and suspended-sediment concentrations of surface water. (See Plate 1 for locations of all hydrologic-data collection sites.)</p><p>The authors wish to acknowledge the public officials, consulting firms, industrial concerns, well drillers, and individual homeowners who have given their time and information to this study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74368","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Hansen, B.P., Gay, F.B., and Toler, L., 1974, Hydrologic data of the Hoosic River basin, Massachusetts: U.S. Geological Survey Open-File Report 74-368, Report: 33 p.; 1 Plate: 27.53 x 21.03 inches, https://doi.org/10.3133/ofr74368.","productDescription":"Report: 33 p.; 1 Plate: 27.53 x 21.03 inches","costCenters":[],"links":[{"id":431328,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0368/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431327,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0368/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148218,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0368/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Hoosic River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.29894453570657,\n              42.8800886208854\n            ],\n            [\n              -73.29894453570657,\n              42.40327840740747\n            ],\n            [\n              -72.34313398883154,\n              42.40327840740747\n            ],\n            [\n              -72.34313398883154,\n              42.8800886208854\n            ],\n            [\n              -73.29894453570657,\n              42.8800886208854\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60786f","contributors":{"authors":[{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":168738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":168740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toler, L.G.","contributorId":98710,"corporation":false,"usgs":true,"family":"Toler","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":168739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4840,"text":"pp383 - 1974 - Hydrology of volcanic-rock terranes","interactions":[{"subject":{"id":39019,"text":"pp383C - 1969 - Effect of tectonic structure on the occurrence of ground water in the basalt of the Columbia River Group of The Dalles area, Oregon and Washington","indexId":"pp383C","publicationYear":"1969","noYear":false,"chapter":"C","title":"Effect of tectonic structure on the occurrence of ground water in the basalt of the Columbia River Group of The Dalles area, Oregon and Washington"},"predicate":"IS_PART_OF","object":{"id":4840,"text":"pp383 - 1974 - Hydrology of volcanic-rock terranes","indexId":"pp383","publicationYear":"1974","noYear":false,"title":"Hydrology of volcanic-rock terranes"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:52","indexId":"pp383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"383","title":"Hydrology of volcanic-rock terranes","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp383","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrology of volcanic-rock terranes: U.S. Geological Survey Professional Paper 383, NA, https://doi.org/10.3133/pp383.","productDescription":"NA","costCenters":[],"links":[{"id":117267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0383/report-thumb.jpg"},{"id":31777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0383/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7a7","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":528386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15814,"text":"ofr74357 - 1974 - Streamflow measurement network review for hydroelectric power applications in Brazil","interactions":[],"lastModifiedDate":"2023-08-21T18:51:30.61942","indexId":"ofr74357","displayToPublicDate":"1994-01-01T00:00:00","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":"74-357","title":"Streamflow measurement network review for hydroelectric power applications in Brazil","docAbstract":"<p>This review of selected segments of the stream-gaging network of Brazil was undertaken by the writer in March and April, 1973, pursuant to an agreement between Companhia de Pesquisa de Recursos Minerais (CPRM) and Centrais Eletricas Brasileiras S.A. (ELETROBRAS) as a part of the cooperative program of the U.S. Geological Survey (USGS) and CPRM under the auspices of the Ministerio das Minas e Energia (MME) and the U.S. Agency for International Development (USAID). Its primary purpose is to provide an evaluation of the adequacy of streamflow data on streams which are being considered for or are already being utilized for hydroelectric power sources. Some comments are included pertaining to the general coverage hydrologic network. These comments were generated by the examination of the streamflow data useful for power purposes because all gaging stations form a part of the total network for hydrologic investigations. Present plans are that the entire network will eventually be operated by or under the jurisdiction of the MME through the Departamento National de Aguas e Energia Eletrica (DNAEE).</p><p>Brazil is a large country, larger than the conterminous United States, and it has been engaged in hydrologic investigations for more than 50 years. The network has been maintained by Federal agencies, State agencies, power companies, and consulting firms and until recently no organizational mechanism existed to coordinate the various activities or to establish uniform standards of data collection, computation, and publication.</p><p>It is estimated that stage and/or discharge data have been collected at 2,500 or more sites in Brazil. Because there has been no centralized publication system, it has not been possible to locate with assurance all measurement sites or to ascertain precisely the types and quality of the data collected or available.</p><p>For these reasons the suggestions outlined in this report are expected to be modified on the basis of local need and site information, which may not have been evident at the time of the review. For example, specific suggestions have been made to discontinue some stations which appear superfluous or which essentially duplicate other stations. In other instances additions to the network have been proposed. There may be reasons for the continued operation of a given station which cannot be discerned from the available literature. Also coverage may have been established in an area but the evidence has not yet appeared in print. DEAEE is currently (1973) working diligently to overcome a backlog of data computation and publication. Brazil is currently developing at a rapid rate with electric power demands increasing at a 12% annually, a reflection of the tremendous growth of the economy. With this rate of increase likely to continue for the foreseable future, it goes without saying that hydrologic information needed tomorrow must be collected today.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74357","collaboration":"Prepared in cooperation with the Brazilian Ministry of Mines and Energy National Department of Water and Electrical Energy under the auspices of the United States Agency for International Development","usgsCitation":"Schaefer, F.T., 1974, Streamflow measurement network review for hydroelectric power applications in Brazil: U.S. Geological Survey Open-File Report 74-357, 63 p., https://doi.org/10.3133/ofr74357.","productDescription":"63 p.","costCenters":[],"links":[{"id":148318,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0357/report-thumb.jpg"},{"id":419982,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Brazil","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.5719146888472,\n              3.7969492210477824\n            ],\n            [\n              -74.5719146888472,\n              -33.611048620406706\n            ],\n            [\n              -27.13000244975086,\n              -33.611048620406706\n            ],\n            [\n              -27.13000244975086,\n              3.7969492210477824\n            ],\n            [\n              -74.5719146888472,\n              3.7969492210477824\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d89","contributors":{"authors":[{"text":"Schaefer, Francis T.","contributorId":48184,"corporation":false,"usgs":true,"family":"Schaefer","given":"Francis","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":171778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15649,"text":"ofr74328 - 1974 - Proposed hydrologic analyses of streamflow for Brazil","interactions":[],"lastModifiedDate":"2023-11-24T20:40:38.133808","indexId":"ofr74328","displayToPublicDate":"1994-01-01T00:00:00","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":"74-328","title":"Proposed hydrologic analyses of streamflow for Brazil","docAbstract":"<p>The objective of my assignment was to recommend what hydrologic analyses might be made using the records of stream discharge soon to be available at the gaging stations in Brazil. To attain this objective I (1) examined the streamflow records in part of the Rio Jacui basin in the state of Rio Grande do Sul for quality, length of record, and density of areal coverage; (2) locked at the available topographic maps; (3) spent one day in the field visiting gaging stations and observing general hydrologic conditions and (4) examined an isohyetal map of Brazil. The assignment was accomplished May 6-24, 1974.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74328","usgsCitation":"Riggs, H.C., 1974, Proposed hydrologic analyses of streamflow for Brazil: U.S. Geological Survey Open-File Report 74-328, 18 p., https://doi.org/10.3133/ofr74328.","productDescription":"18 p.","costCenters":[],"links":[{"id":422945,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0328/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0328/report-thumb.jpg"}],"country":"Brazil","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -35.43653638656767,\n              6.476173966316765\n            ],\n            [\n              -72.07106531715064,\n              6.476173966316765\n            ],\n            [\n              -72.07106531715064,\n              -33.11926593714407\n            ],\n            [\n              -35.43653638656767,\n              -33.11926593714407\n            ],\n            [\n              -35.43653638656767,\n              6.476173966316765\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d67b","contributors":{"authors":[{"text":"Riggs, Henry Chiles","contributorId":44129,"corporation":false,"usgs":true,"family":"Riggs","given":"Henry","email":"","middleInitial":"Chiles","affiliations":[],"preferred":false,"id":171492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12517,"text":"ofr74331 - 1974 - Summary appraisals of the Nation's ground-water resources; Texas Gulf region","interactions":[],"lastModifiedDate":"2016-08-10T16:11:59","indexId":"ofr74331","displayToPublicDate":"1994-01-01T00:00:00","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":"74-331","title":"Summary appraisals of the Nation's ground-water resources; Texas Gulf region","docAbstract":"<p>Ground water in the Texas-Gulf Region is a large and important resource that can provide a more significant percentage of the total water supply of the region. Total water requirements within the region are projected to rise sharply from 14 million acre-feet (17 cubic kilometres) in 1970 to nearly 26 million acre-feet (32.cubic kilometres) in 2020. About half of the water used in 1970 was ground water.</p>\n<p>An estimated total of 1.04 billion acre-feet (1,280 cubic kilometres) of recoverable water containing less than 3,000 milligrams per litre dissolved solids is stored above a depth of 400 feet (122 metres) in the aquifers of the region. In addition, part of an estimated 3.28 billion acre-feet (4,040 cubic kilometres) of water in storage below 400 feet (122 metres) is recoverable. Although not all of the ground water in storage is recoverable, a significant amount is available for development, and an enormous quantity is accessible should occasions prompt its use on a time-limited basis.</p>\n<p>The total steady-state yield (amount of water that approximates the maximum perennial replenishment from precipitation) of the region's aquifers is about 4.6 million acre-feet (5.7 cubic kilometres) annually, or about 2.3 times the ground-water usage in 1970 if the large mining draft on the High Plains is not considered as part of the total steady-state yield. Because of the large quantity of recoverable ground water in storage, the steady-state yield can be augmented for a very long time on a 'deferred' basis, whereby the economic use of the water that is withdrawn from storage in excess of the steady-state yield may result in a strengthened economy.</p>\n<p>An important goal in programs for meeting future water needs should be to identify the full potential of the available ground-water resources. The subsurface reservoirs may be utilized not only as sources of fresh and treatable water, but as storage facilities for other fresh-water-supplies and as possible sources of geothermal energy. Some saline-water reservoirs may be suitable for liquid-waste storage or disposal.</p>\n<p>Large-scale and unregulated ground-water pumping may result in hydrologic problems such as declining water levels, streamflow depletion, and land-surface subsidence; but studies on proper development of the groundwater reservoirs could provide solutions to many of the problems. Water rights and other legal concepts should be based on sound hydrologic principles to assist development of water resources in an orderly and efficient manner.</p>\n<p>Because significant amounts of ground water are available, the opportunities for expanded and conjunctive use of ground water and surface water should be considered in regional plans for water development and conservation. The complexities of water management and the difficulties of achieving an integrated system of total water management will require additional technical information.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74331","usgsCitation":"Baker, E.T., and Wall, J.R., 1974, Summary appraisals of the Nation's ground-water resources; Texas Gulf region: U.S. Geological Survey Open-File Report 74-331, Report: iv, 61 p.; 11 Figures: 30.32 x 41.39 inches or smaller, https://doi.org/10.3133/ofr74331.","productDescription":"Report: iv, 61 p.; 11 Figures: 30.32 x 41.39 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":146488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0331/report-thumb.jpg"},{"id":40760,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-01.pdf","text":"Figure 1","size":"950.37 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 1"},{"id":40761,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-02.pdf","text":"Figure 10","size":"735.75 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 10"},{"id":40762,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-03.pdf","text":"Figure 11","size":"325.46 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 11"},{"id":40763,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-04.pdf","text":"Figure 2","size":"935.74 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 2"},{"id":40764,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-05.pdf","text":"Figure 3","size":"457.42 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 3"},{"id":40765,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-06.pdf","text":"Figure 4","size":"2.30 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 4"},{"id":40766,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-07.pdf","text":"Figure 5","size":"2.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":40767,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-08.pdf","text":"Figure 5","size":"2.23 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":40768,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-09.pdf","text":"Figure 6","size":"2.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 6"},{"id":40769,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-10.pdf","text":"Figure 7","size":"821.78 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 7"},{"id":40770,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-11.pdf","text":"Figure 8","size":"310.10 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 8"},{"id":40771,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0331/plate-12.pdf","text":"Figure 9","size":"3.01 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 9"},{"id":40772,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0331/report.pdf","text":"Report","size":"1.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Louisiana, New Mexico, Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n       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T. Jr.","contributorId":88366,"corporation":false,"usgs":true,"family":"Baker","given":"E.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":166264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wall, James Ray","contributorId":14830,"corporation":false,"usgs":true,"family":"Wall","given":"James","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":166263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15535,"text":"ofr74339 - 1974 - Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73","interactions":[],"lastModifiedDate":"2024-02-23T19:33:40.536288","indexId":"ofr74339","displayToPublicDate":"1994-01-01T00:00:00","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":"74-339","title":"Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73","docAbstract":"<p>The Reedy Creek Improvement District (hereinafter called the RCID) is an area of about 43 square miles (111. square kilometres) in southwest Orange and northwest Osceola Counties. Before development of Walt Disney World began (mid-1967), all of this tract of land was scrubby flatlands and swamp. Walt Disney World facilities now (1974) occupy slightly less than 10 percent of the area. Hydrologic data are available for most of the area for the 6-year period July 1967-June 1973, with some records starting before July 1967.</p><p>The potentiometric surface of the Floridan aquifer near Bay Lake has declined 8 feet (2 metres) on the average. Seventy-five percent of the decline is attributed to water use in the RCID; the remaining decline is attributed to deficient rainfall since the records began in March 1966. The discharge of streams in the RCID has apparently increased. However, the hydrologic conditions were changing locally as the development of the area progressed. Because of this change, the magnitude and seasonal distribution of any eventual change in streamflow cannot be accurately appraised until additional data are obtained after the development has stabilized. Some changes in water quality have occurred, but none can be attributed to urbanization.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74339","collaboration":"Prepared in cooperation with the Reedy Creek Improvement District","usgsCitation":"Putnam, A.L., 1974, Summary of hydrologic conditions and effects of Walt Disney World development in the Reedy Creek Improvement District, 1966-73: U.S. Geological Survey Open-File Report 74-339, ix, 129 p., https://doi.org/10.3133/ofr74339.","productDescription":"ix, 129 p.","costCenters":[],"links":[{"id":425959,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0339/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0339/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Orange County, Osceola County","otherGeospatial":"Reedy Creek Improvement District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.60730309556335,\n              28.489196384290096\n            ],\n            [\n              -81.60730309556335,\n              28.395006686287886\n            ],\n            [\n              -81.50978150298498,\n              28.395006686287886\n            ],\n            [\n              -81.50978150298498,\n              28.489196384290096\n            ],\n            [\n              -81.60730309556335,\n              28.489196384290096\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69919c","contributors":{"authors":[{"text":"Putnam, Arthur L.","contributorId":25170,"corporation":false,"usgs":true,"family":"Putnam","given":"Arthur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171288,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15512,"text":"ofr74352 - 1974 - Hydrologic reconnaissance of the southern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":15512,"text":"ofr74352 - 1974 - Hydrologic reconnaissance of the southern Uinta Basin, Utah and Colorado","indexId":"ofr74352","publicationYear":"1974","noYear":false,"title":"Hydrologic reconnaissance of the southern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042869,"text":"70042869 - 1954 - Progress report on selected ground-water basins in Utah","indexId":"70042869","publicationYear":"1954","noYear":false,"title":"Progress report on selected ground-water basins in Utah"},"id":1}],"supersededBy":{"id":70042869,"text":"70042869 - 1954 - Progress report on selected ground-water basins in Utah","indexId":"70042869","publicationYear":"1954","noYear":false,"title":"Progress report on selected ground-water basins in Utah"},"lastModifiedDate":"2016-12-12T11:37:04","indexId":"ofr74352","displayToPublicDate":"1994-01-01T00:00:00","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":"74-352","title":"Hydrologic reconnaissance of the southern Uinta Basin, Utah and Colorado","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr74352","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Price, D., and Miller, L.L., 1974, Hydrologic reconnaissance of the southern Uinta Basin, Utah and Colorado: U.S. Geological Survey Open-File Report 74-352, 92 leaves :ill., maps (1 col.) ;27 cm., https://doi.org/10.3133/ofr74352.","productDescription":"92 leaves :ill., maps (1 col.) ;27 cm.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":148298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605437","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":171242,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Louise L.","contributorId":74759,"corporation":false,"usgs":true,"family":"Miller","given":"Louise","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14153,"text":"ofr74237 - 1974 - Hydrology of the abandoned coal mines in the Wyoming Valley, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-27T11:12:05","indexId":"ofr74237","displayToPublicDate":"1994-01-01T00:00:00","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":"74-237","title":"Hydrology of the abandoned coal mines in the Wyoming Valley, Pennsylvania","docAbstract":"Mine-water discharge, into the Susquehanna River degrades the river's quality during periods of low flow to a point critical for subsistence of aquatic life. To determine what measures are required to provide a better quality mine-water discharge in the Wyoming Valley, mine hydrology and mine-water quality are related to mine-pool management. The addition of mine-pool outlets at several locations would increase the rate of discharge and reduce interpool flow, which would reduce the total mineral load discharged to the river. Additional outlets would act as relief overflows to reduce the maximum fluctuation of mine-pool levels, decrease related mine-surface instability, and eliminate surface flooding.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74237","usgsCitation":"Hollowell, J.R., 1974, Hydrology of the abandoned coal mines in the Wyoming Valley, Pennsylvania: U.S. Geological Survey Open-File Report 74-237, 47 [i.e. 50] leaves :ill. (some folded), folded maps ;27 cm., https://doi.org/10.3133/ofr74237.","productDescription":"47 [i.e. 50] leaves :ill. (some folded), folded maps ;27 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":95206,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0237/plate-1.pdf","size":"2280","linkFileType":{"id":1,"text":"pdf"}},{"id":95207,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0237/plate-2.pdf","size":"10808","linkFileType":{"id":1,"text":"pdf"}},{"id":42801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0237/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0237/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbdf","contributors":{"authors":[{"text":"Hollowell, Jerrald R.","contributorId":51278,"corporation":false,"usgs":true,"family":"Hollowell","given":"Jerrald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":169010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10144,"text":"ofr75612 - 1974 - A program to compute aquifer-response coefficients","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr75612","displayToPublicDate":"1994-01-01T00:00:00","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":"75-612","title":"A program to compute aquifer-response coefficients","docAbstract":"An alternating direction technique is used to solve finite difference equations approximating the flow of water in an aquifer. The solutions produce response coefficients relating pumping from wells to drawdowns within those wells. The product of the response coefficient with the pumping values produces a linear algebraic technological function that can be used for integrating hydrologic phenomena into planning and management models.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75612","usgsCitation":"Maddock, T., 1974, A program to compute aquifer-response coefficients: U.S. Geological Survey Open-File Report 75-612, 39 leaves (in various foliations) :ill. ;27 cm.; (18 p. - PGS), https://doi.org/10.3133/ofr75612.","productDescription":"39 leaves (in various foliations) :ill. ;27 cm.; (18 p. - PGS)","costCenters":[],"links":[{"id":143463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0612/report-thumb.jpg"},{"id":37991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0612/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8957","contributors":{"authors":[{"text":"Maddock, Thomas","contributorId":79892,"corporation":false,"usgs":true,"family":"Maddock","given":"Thomas","affiliations":[],"preferred":false,"id":160887,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15092,"text":"ofr74257 - 1974 - Hydrologic effects of the Tampa Bypass Canal","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr74257","displayToPublicDate":"1994-01-01T00:00:00","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":"74-257","title":"Hydrologic effects of the Tampa Bypass Canal","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr74257","usgsCitation":"Motz, L.H., 1974, Hydrologic effects of the Tampa Bypass Canal: U.S. Geological Survey Open-File Report 74-257, 48 leaves :22 folded maps ;28 cm.; (68 p. - PGS), https://doi.org/10.3133/ofr74257.","productDescription":"48 leaves :22 folded maps ;28 cm.; (68 p. - PGS)","costCenters":[],"links":[{"id":148059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e15","contributors":{"authors":[{"text":"Motz, Louis H.","contributorId":6934,"corporation":false,"usgs":true,"family":"Motz","given":"Louis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5920,"text":"pp908 - 1974 - Simulated effects of oil-shale development on the hydrology of Piceance Basin, Colorado","interactions":[{"subject":{"id":16469,"text":"ofr74255 - 1974 - Simulated effects of oil-shale development on the hydrology of Piceance basin, Colorado","indexId":"ofr74255","publicationYear":"1974","noYear":false,"title":"Simulated effects of oil-shale development on the hydrology of Piceance basin, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5920,"text":"pp908 - 1974 - Simulated effects of oil-shale development on the hydrology of Piceance Basin, Colorado","indexId":"pp908","publicationYear":"1974","noYear":false,"title":"Simulated effects of oil-shale development on the hydrology of Piceance Basin, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"pp908","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"908","title":"Simulated effects of oil-shale development on the hydrology of Piceance Basin, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp908","usgsCitation":"Weeks, J., Leavesley, G., Welder, F., and Saulnier, G., 1974, Simulated effects of oil-shale development on the hydrology of Piceance Basin, Colorado: U.S. Geological Survey Professional Paper 908, 84 p.; 1 plate in pocket, https://doi.org/10.3133/pp908.","productDescription":"84 p.; 1 plate in pocket","costCenters":[],"links":[{"id":117534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0908/report-thumb.jpg"},{"id":32803,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0908/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32804,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0908/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f37aa","contributors":{"authors":[{"text":"Weeks, John B.","contributorId":36123,"corporation":false,"usgs":true,"family":"Weeks","given":"John B.","affiliations":[],"preferred":false,"id":151812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leavesley, G.H.","contributorId":93895,"corporation":false,"usgs":true,"family":"Leavesley","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":151814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welder, F.A.","contributorId":104878,"corporation":false,"usgs":true,"family":"Welder","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":151815,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saulnier, G.J. Jr.","contributorId":45299,"corporation":false,"usgs":true,"family":"Saulnier","given":"G.J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":151813,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14686,"text":"ofr7439 - 1974 - Hydrology of the Dismal Swamp, Virginia-North Carolina","interactions":[],"lastModifiedDate":"2023-11-23T00:04:19.391593","indexId":"ofr7439","displayToPublicDate":"1994-01-01T00:00:00","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":"74-39","title":"Hydrology of the Dismal Swamp, Virginia-North Carolina","docAbstract":"<p>The Dismal Swamp, on the border between eastern Virginia and North Carolina is one of the few remaining large (approximately 210,000 acres) areas of wet wilderness in the eastern United States. There has been much speculation concerning the hydrologic conditions that led to the formation of the swamp.</p><p>Oaks and Coch (1973) recently completed a detailed investigation of the geology and morphology of the area. An analysis of their geology and the pollen work of Whitehead (1972) has lead the authors to the following hypothesis concerning the hydrologic conditions that led to the formation of the peat in the swamp.</p><p>A permeable sand facies of the Norfolk Formation underlies Dismal Swamp. This facies was originally completely covered by the Sand Bridge Formation, which is a confining layer, and underlain by the impermeable Yorktown Formation. Movement of water eastward within the Norfolk Formation from the outcrop area on the top of the Suffolk Scarp was further restricted by a less permeable facies of the Norfolk east of the swamp; thereby creating an artesian head within the permeable sand facies of the Norfolk Formation.</p><p>Erosion during the Pleistocene age breached the Sand Bridge confining layer and allowed upward seepage of water along the shallow stream valleys. This seepage, combined with the abundant rainfall and naturally sluggish surface drainage, may have been sufficient to trigger the formation of peat along stream valleys about 9,000 years ago. The peat further inhibited surface drainage, which in turn, accelerated the accumulation of peat until the interfluve areas were covered. The present role of the Norfolk Formation in the hydrology of the swamp is not clear, but it is considered to be one of the most important aspects of the hydrology to be studied in future investigations.</p><p>Surface inflow is from small streams draining from the west. The flow of these streams varies widely, being generally less in the summer than in winter. Outflow is primarily through the Feeder Ditch-Dismal Swamp Canal system, which discharges at South Mills and Deep Creek locks.</p><p>Rates and direction of surface flow within the swamp are partly controlled by gates on many of the ditches. Inadequately controlled ditches penetrating the Norfolk Formation plus withdrawal of water from wells along Suffolk Scarp have altered the flow of ground water under the swamp. These modifications and the loss of water through the Dismal Swamp Canal have probably resulted in a generally drier swamp as indicated by changes in the vegetation. It is feasible to preserve Dismal Swamp, but more detailed studies of the hydrology are needed to aid in future management.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7439","usgsCitation":"Lichtler, W.F., and Walker, P.N., 1974, Hydrology of the Dismal Swamp, Virginia-North Carolina: U.S. Geological Survey Open-File Report 74-39, v, 50 p., https://doi.org/10.3133/ofr7439.","productDescription":"v, 50 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":148364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0039/report-thumb.jpg"},{"id":422873,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Dismal Swamp","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    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,{"id":2725,"text":"wsp1850D - 1974 - Floods of June 1965 in Arkansas River basin, Colorado, Kansas, and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1850D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"1850","chapter":"D","title":"Floods of June 1965 in Arkansas River basin, Colorado, Kansas, and New Mexico","docAbstract":"Maximum discharges during the floods of June 1965 in the Arkansas River basin in Colorado, Kansas, and New Mexico were greater than those previously known at 49 of the 137 locations where flood information was obtained. Property damage exceeded $60 million, and 16 lives were lost. At many sites, peak discharges exceeded by severalfold the discharges that may be expected, on the average, once in 50 years; yet, the 1965 discharges could be exceeded in the near future. \r\n\r\nHeavy rainfall of more than 12 inches in several areas and more than 18 inches near Two Buttes, Colo., caused severe flooding in the Arkansas River basin in Colorado and Kansas and the Canadian River basin in New Mexico. Snowmelt runoff added only token amounts to the flood peaks. The 1965 peak discharges along the main stem of the Arkansas River in Colorado were less than those in 1921, but tributary peaks were probably greater at many sites In New Mexico the peak discharges exceeded those for the destructive floods of 1904 at some locations, by manyfold at some sites. \r\n\r\nDescriptions of the storms and floods, detailed streamflow records, and information on \r\ndamages and flood frequency are included in this report. Comparisons of the magnitude of the floods are made, and all indicate that an outstanding hydrologic event occurred.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1850D","usgsCitation":"Snipes, R., 1974, Floods of June 1965 in Arkansas River basin, Colorado, Kansas, and New Mexico: U.S. Geological Survey Water Supply Paper 1850, iv, 97 p. :ill., maps (2 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1850D.","productDescription":"iv, 97 p. :ill., maps (2 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1850d/report-thumb.jpg"},{"id":29130,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29131,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1850d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4884e4b07f02db51858a","contributors":{"authors":[{"text":"Snipes, R.J.","contributorId":16813,"corporation":false,"usgs":true,"family":"Snipes","given":"R.J.","affiliations":[],"preferred":false,"id":145671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14386,"text":"ofr74113 - 1974 - Analog-model studies of ground-water hydrology in the Houston District, Texas","interactions":[],"lastModifiedDate":"2016-08-10T16:05:38","indexId":"ofr74113","displayToPublicDate":"1994-01-01T00:00:00","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":"74-113","title":"Analog-model studies of ground-water hydrology in the Houston District, Texas","docAbstract":"<p>The major water-bearing units in the Houston district are the Chicot and the Evangeline aquifers. The Chicot aquifer overlies the Evangeline aquifer, which is underlain by the Burkeville confining layer. Both aquifers consist of unconsolidated and discontinuous layers of sand and clay that dip toward the Gulf of Mexico. Heavy pumping of fresh water has caused large declines in the altitudes of the potentiometric surfaces in both aquifers and has created large cones of depression around Houston. The declines have caused compaction of clay layers, which has resulted in land surface subsidence and the movement of saline ground water toward the centers of the cones of depression. An electric analog model was used to study the hydrologic system and to simulate the declines in the altitudes of the potentiometric surfaces for several alternative plans of ground-water development. The results indicate that the largest part. of the pumped water comes from storage in the water-table part of the Chicot aquifer. Vertical leakage from the aquifers and water derived from the compaction of clay layers in the aquifers are also large sources of the water being pumped. The response of the system, as observed on the model, indicates that development of additional ground-water supplies from the water-table part of the Chicot aquifer north of Houston would result in a minimum decline of the altitudes of the potentiometric surfaces. Total withdrawals of about 1,000 million gallons (5.8 million cubic meters) per day may be possible without seriously, increasing subsidence or salt-water encroachment. Analyses of the recovery of water levels indicate that both land-surface subsidence and salt-water encroachment could be reduced by artificially recharging the artesian part of the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74113","usgsCitation":"Jorgensen, D.G., 1974, Analog-model studies of ground-water hydrology in the Houston District, Texas: U.S. Geological Survey Open-File Report 74-113, Report: x, 86 p.; 33 Plates, https://doi.org/10.3133/ofr74113.","productDescription":"Report: x, 86 p.; 33 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":95252,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-18.pdf","size":"2911","linkFileType":{"id":1,"text":"pdf"}},{"id":95253,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-19.pdf","size":"3452","linkFileType":{"id":1,"text":"pdf"}},{"id":95254,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-20.pdf","size":"3790","linkFileType":{"id":1,"text":"pdf"}},{"id":95255,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-21.pdf","size":"2695","linkFileType":{"id":1,"text":"pdf"}},{"id":95256,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-22.pdf","size":"1868","linkFileType":{"id":1,"text":"pdf"}},{"id":95257,"rank":422,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-23.pdf","size":"1740","linkFileType":{"id":1,"text":"pdf"}},{"id":95258,"rank":423,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-24.pdf","size":"2007","linkFileType":{"id":1,"text":"pdf"}},{"id":95259,"rank":424,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-25.pdf","size":"1731","linkFileType":{"id":1,"text":"pdf"}},{"id":95260,"rank":425,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-26.pdf","size":"3503","linkFileType":{"id":1,"text":"pdf"}},{"id":95261,"rank":426,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-27.pdf","size":"2932","linkFileType":{"id":1,"text":"pdf"}},{"id":95262,"rank":427,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-28.pdf","size":"3048","linkFileType":{"id":1,"text":"pdf"}},{"id":95263,"rank":428,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-29.pdf","size":"3884","linkFileType":{"id":1,"text":"pdf"}},{"id":95264,"rank":429,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-30.pdf","size":"3176","linkFileType":{"id":1,"text":"pdf"}},{"id":95265,"rank":430,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-31.pdf","size":"3093","linkFileType":{"id":1,"text":"pdf"}},{"id":95266,"rank":431,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-32.pdf","size":"3280","linkFileType":{"id":1,"text":"pdf"}},{"id":95267,"rank":432,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-33.pdf","size":"1261","linkFileType":{"id":1,"text":"pdf"}},{"id":95235,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-01.pdf","size":"9012","linkFileType":{"id":1,"text":"pdf"}},{"id":95236,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-02.pdf","size":"4740","linkFileType":{"id":1,"text":"pdf"}},{"id":95237,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-03.pdf","size":"3451","linkFileType":{"id":1,"text":"pdf"}},{"id":95238,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-04.pdf","size":"2351","linkFileType":{"id":1,"text":"pdf"}},{"id":95239,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-05.pdf","size":"2992","linkFileType":{"id":1,"text":"pdf"}},{"id":95234,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0113/report.pdf","size":"26972","linkFileType":{"id":1,"text":"pdf"}},{"id":95240,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-06.pdf","size":"3022","linkFileType":{"id":1,"text":"pdf"}},{"id":148804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0113/report-thumb.jpg"},{"id":95241,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-07.pdf","size":"2938","linkFileType":{"id":1,"text":"pdf"}},{"id":95242,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-08.pdf","size":"3099","linkFileType":{"id":1,"text":"pdf"}},{"id":95243,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-09.pdf","size":"3491","linkFileType":{"id":1,"text":"pdf"}},{"id":95244,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-10.pdf","size":"3185","linkFileType":{"id":1,"text":"pdf"}},{"id":95245,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-11.pdf","size":"3569","linkFileType":{"id":1,"text":"pdf"}},{"id":95246,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-12.pdf","size":"3311","linkFileType":{"id":1,"text":"pdf"}},{"id":95247,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-13.p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Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":169367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68228,"text":"ha488 - 1974 - Water resources of the Snake River watershed, east-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:17:05","indexId":"ha488","displayToPublicDate":"1994-01-01T00:00:00","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":"488","title":"Water resources of the Snake River watershed, east-central Minnesota","docAbstract":"<p>Glacial drift overlies sedimentary, igneous, and metamorphic rocks in the Snake River watershed.</p>\n<p>The Snake River, which drains an area of about 1,030 square miles, originates in an extensive area of peat bogs in the northern part of the watershed. It flows southward across gently rolling glacial terrain in which the major relief is near the river. Near the southern boundary of the watershed, the Snake River turns eastward to its confluence with the St. Croix River. The northwest half of the watershed is heavily forested, whereas much of the southeast half has been cleared. The largest communities in the watershed, Mora and Pine City, had 1970 populations of 2,582 and 2,143, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha488","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Lindholm, G.F., Helgesen, J.O., Broussard, W., and Ericson, D., 1974, Water resources of the Snake River watershed, east-central Minnesota: U.S. Geological Survey Hydrologic Atlas 488, 3 Plates: 44 x 35 inches, https://doi.org/10.3133/ha488.","productDescription":"3 Plates: 44 x 35 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":628993,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broussard, W.L.","contributorId":35334,"corporation":false,"usgs":true,"family":"Broussard","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":628994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ericson, D.W.","contributorId":80295,"corporation":false,"usgs":true,"family":"Ericson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":628995,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68227,"text":"ha490 - 1974 - Water resources of the lower St. Croix river watershed, east-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:16:38","indexId":"ha490","displayToPublicDate":"1994-01-01T00:00:00","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":"490","title":"Water resources of the lower St. Croix river watershed, east-central Minnesota","docAbstract":"<p>The lower St. Croix River watershed is an elongate area of about 930 square miles bounded on the east by the St. Croix River.</p>\n<p>The St. Croix River forms the Minnesota-Wisconsin boundary along the eastern side of the watershed. Additional drainage to the St. Croix River includes areas of about 2,500 square miles upstream in Minnesota and about 4,340 square miles in Wisconsin. At the southern tip of the watershed, the St. Croix joins the Mississippi River.</p>\n<p>Because part of the St. Croix River is deeply entrenched, topography in the watershed ranges from relatively rugged in highly dissected areas near the river to nearly flat in the west-central area.</p>\n<p>In the southern third of the watershed and along the St. Croix River, many outcrops of Ordovician, Cambrian, and Precambrian bedrock occur. The remainder of the watershed is covered by glacial deposits whose maximum thickness is about 400 feet.</p>\n<p>Much of the original forest cover, primarily hardwoods, has been removed; the largest concentrations remaining are long the St. Croix River and in the west-central area.</p>\n<p>The proximity of the watershed to the expanding Minneapolis-St. Paul metropolitan area emphasizes the importance of defining water resources essential for future growth.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha490","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Lindholm, G.F., Helgesen, J.O., Broussard, W., and Farrell, D., 1974, Water resources of the lower St. Croix river watershed, east-central Minnesota: U.S. Geological Survey Hydrologic Atlas 490, 3 Plates: 48 x 38 inches or smaller, https://doi.org/10.3133/ha490.","productDescription":"3 Plates: 48 x 38 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":187952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89592,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/490/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89593,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/490/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89594,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/490/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Minnesota","otherGeospatial":"Lower St. Croix River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": 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,{"id":68226,"text":"ha528 - 1974 - Water resources of the Crow River watershed, south-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:16:20","indexId":"ha528","displayToPublicDate":"1994-01-01T00:00:00","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":"528","title":"Water resources of the Crow River watershed, south-central Minnesota","docAbstract":"<p>The Crow River watershed, an area of about 2,760 square miles, is covered entirely by glacial deposits. A topographically high, east-west-trending end moraine divides most of the watershed into two drainage areas of approximately equal size. The North Fork Crow River drains a mixture of glacial outwash and till deposits, whereas the South Fork Crow River drains chiefly till deposits. Local relief is greatest in morainal areas and least in surficial outwash areas.</p>\n<p>Cambrian and Precambrian sedimentary rocks underlie the glacial drift in the eastern part of the watershed. Cretaceous sedimentary rocks, though discontinuous, are present in part of the western two-thirds of the watershed. Where sedimentary bedrock is absent, the glacial drift is directly underlain by Precambrian igneous or metamorphic rocks.</p>\n<p>Forested areas are sparse and occur mainly in steeply sloping morainal areas. Most land is used for agriculture, and slightly more than half the total population is rural.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha528","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters","usgsCitation":"Lindholm, G.F., Farrell, D., and Helgesen, J.O., 1974, Water resources of the Crow River watershed, south-central Minnesota: U.S. Geological Survey Hydrologic Atlas 528, 3 Plates: 54 x 35 inches or smaller, https://doi.org/10.3133/ha528.","productDescription":"3 Plates: 54 x 35 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":66112,"text":"i855C - 1974 - Map showing availability of hydrologic data, Boulder-Fort Collins-Greeley area, Front Range Urban Corridor, Colorado","interactions":[],"lastModifiedDate":"2025-08-13T17:09:33.250239","indexId":"i855C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"855","chapter":"C","title":"Map showing availability of hydrologic data, Boulder-Fort Collins-Greeley area, Front Range Urban Corridor, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i855C","usgsCitation":"Hampton, E.R., Clark, G.A., and McNutt, M.H., 1974, Map showing availability of hydrologic data, Boulder-Fort Collins-Greeley area, Front Range Urban Corridor, Colorado: U.S. Geological Survey IMAP 855, 1 Plate: 32.76 x 36.73 inches, https://doi.org/10.3133/i855C.","productDescription":"1 Plate: 32.76 x 36.73 inches","costCenters":[],"links":[{"id":494034,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9730.htm","linkFileType":{"id":5,"text":"html"}},{"id":255609,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0855c/report-thumb.jpg"},{"id":255608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0855c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255607,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0855c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Colorado","otherGeospatial":"Boulder-Fort Collins-Greeley area, Front Range Urban Corridor","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.625,\n              40\n            ],\n            [\n              -104.625,\n              40.625\n            ],\n            [\n              -105.375,\n              40.625\n            ],\n            [\n              -105.375,\n              40\n            ],\n            [\n              -104.625,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659765","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":273990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, G. A.","contributorId":97197,"corporation":false,"usgs":true,"family":"Clark","given":"G.","middleInitial":"A.","affiliations":[],"preferred":false,"id":273991,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McNutt, M. H.","contributorId":49053,"corporation":false,"usgs":true,"family":"McNutt","given":"M.","middleInitial":"H.","affiliations":[],"preferred":false,"id":273989,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67902,"text":"ha524 - 1974 - Water resources of Wisconsin--Lake Superior basin","interactions":[],"lastModifiedDate":"2015-10-05T16:30:08","indexId":"ha524","displayToPublicDate":"1994-01-01T00:00:00","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":"524","title":"Water resources of Wisconsin--Lake Superior basin","docAbstract":"<p><span>This report describes the physical environment, availability, distribution, movement, quality, and use of water in the upper Wisconsin River basin as an aid in planning and water management. The report presents general information on the basin derived from data obtained from Federal, State, and local agencies, New field data were collected in areas where information was lacking. More detailed studies of problem areas may be required in the future, as water needs and related development increase.</span></p>\n<p><span>The upper Wisconsin River basin is the headwaters of the Wisconsin River drainage and includes about 2,730 square miles in northern Wisconsin (upstream from the gage on the Wisconsin River at Merrill). An additional 50 square miles of the basin lies in Michigan and is not covered by this report. The report area includes parts of Forest, Langlade, Lincoln, Marathon, Oneida, Price, Taylor, and Vilas Counties,</span></p>\n<p><span>Many organizations and persons assisted the study by providing data. Among the contributors were the University of Wisconsin-Extension, Geological and Natural History Survey, the Wisconsin Department of Natural Resources, the Public Service Commission of Wisconsin, and the Wisconsin Valley Improvement Company, Municipal water officials furnished water-supply information and well records, Many individuals allowed access to their wells for water-level measurements and collection of water samples for chemical analysis.</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha524","usgsCitation":"Young, H.L., and Skinner, E.L., 1974, Water resources of Wisconsin--Lake Superior basin: U.S. Geological Survey Hydrologic Atlas 524, 3 Sheets: 38.5 x 45 inches, https://doi.org/10.3133/ha524.","productDescription":"3 Sheets: 38.5 x 45 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":188816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89076,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/524/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89077,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/524/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89075,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/524/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Wisconsin","county":"Ashland County, Bayfield County, Douglas County, Iron County, Vilas County","otherGeospatial":"Lake Superior","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.49414062499999,\n              47.025206001585396\n            ],\n            [\n              -91.7138671875,\n              47.18224592701489\n            ],\n            [\n              -92.61474609375,\n              46.73233101286786\n            ],\n            [\n              -92.40600585937499,\n              46.55886030311719\n            ],\n            [\n              -92.26318359375,\n              46.22545288226939\n            ],\n            [\n              -90.780029296875,\n              45.66012730272194\n            ],\n            [\n              -90.1318359375,\n              45.706179285330855\n            ],\n            [\n              -89.47265625,\n              45.706179285330855\n            ],\n            [\n              -88.857421875,\n              45.90529985724799\n            ],\n            [\n              -89.07714843749999,\n              46.33175800051563\n            ],\n            [\n              -89.58251953125,\n              46.53619267489863\n            ],\n            [\n              -90.263671875,\n              46.90524554642923\n            ],\n            [\n              -90.428466796875,\n              47.18224592701489\n            ],\n            [\n              -91.19750976562499,\n              47.07012182383309\n            ],\n            [\n              -91.49414062499999,\n              47.025206001585396\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f06b0","contributors":{"authors":[{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, Earl L.","contributorId":73191,"corporation":false,"usgs":true,"family":"Skinner","given":"Earl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277285,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67920,"text":"ha504 - 1974 - Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha504","displayToPublicDate":"1994-01-01T00:00:00","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":"504","title":"Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston","language":"ENGLISH","doi":"10.3133/ha504","usgsCitation":"Williams, J.R., and Tasker, G.D., 1974, Water resources of the coastal drainage basins of Southeastern Massachusetts: Weir River, Hingham to Jones River, Kingston: U.S. Geological Survey Hydrologic Atlas 504, 2 col. maps ;87-113 x 107-146 cm., https://doi.org/10.3133/ha504.","productDescription":"2 col. maps ;87-113 x 107-146 cm.","costCenters":[],"links":[{"id":189451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89114,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/504/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89115,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/504/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -70.95083333333334,41.950833333333335 ], [ -70.95083333333334,42.266666666666666 ], [ -70.58416666666666,42.266666666666666 ], [ -70.58416666666666,41.950833333333335 ], [ -70.95083333333334,41.950833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0240","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":277324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67932,"text":"ha507 - 1974 - Water resources of the coastal drainage basins of Southeastern Massachusetts, Plymouth to Weweantic River, Wareham","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"ha507","displayToPublicDate":"1994-01-01T00:00:00","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":"507","title":"Water resources of the coastal drainage basins of Southeastern Massachusetts, Plymouth to Weweantic River, Wareham","language":"ENGLISH","doi":"10.3133/ha507","usgsCitation":"Williams, J.R., and Tasker, G.D., 1974, Water resources of the coastal drainage basins of Southeastern Massachusetts, Plymouth to Weweantic River, Wareham: U.S. Geological Survey Hydrologic Atlas 507, 2 col. maps ;86-103 x 100-113 cm., https://doi.org/10.3133/ha507.","productDescription":"2 col. maps ;86-103 x 100-113 cm.","costCenters":[],"links":[{"id":187697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89132,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/507/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89133,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/507/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -70.86749999999999,41.700833333333335 ], [ -70.86749999999999,42 ], [ -70.5,42 ], [ -70.5,41.700833333333335 ], [ -70.86749999999999,41.700833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03c6","contributors":{"authors":[{"text":"Williams, John R.","contributorId":107260,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":277348,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68219,"text":"ha516 - 1974 - Water resources of Hamilton County, southwestern Kansas","interactions":[],"lastModifiedDate":"2017-02-13T16:43:40","indexId":"ha516","displayToPublicDate":"1994-01-01T00:00:00","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":"516","title":"Water resources of Hamilton County, southwestern Kansas","docAbstract":"<p>According to records of the National Weather Service (formerly the U.S. Weather Bureau) for a station near Syracuse, the average annual precipitation in Hamilton County is about 16 inches. Of this amount, 83 percent occurs during the growing season (March 15 to October 15). A part of the precipitation runs off as surface flow, part is evaporated, part is used by vegetation, and a small part percolates downward to recharge the ground-water reservoir. The average recharge from precipitation for Hamilton County is estimated to be 0.1 inch per year. Owing to the limited supply of water in most of the upland area of the county, dryland farming and grazing are the predominant land uses.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha516","usgsCitation":"Lobmeyer, D.H., and Sauer, C.G., 1974, Water resources of Hamilton County, southwestern Kansas: U.S. Geological Survey Hydrologic Atlas 516, 2 Sheets: 28.0 x 28.0 and 28. x 31.0 inches, https://doi.org/10.3133/ha516.","productDescription":"2 Sheets: 28.0 x 28.0 and 28. x 31.0 inches","costCenters":[],"links":[{"id":187474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89572,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/516/plate-2.pdf","text":"Sheet 2 of 2","linkFileType":{"id":1,"text":"pdf"}},{"id":89571,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/516/plate-1.pdf","text":"Sheet 1 of 2","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Kansas","county":"Hamilton County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-101.5405,38.2631],[-101.5401,37.8282],[-101.5256,37.8281],[-101.527,37.7364],[-102.0432,37.7384],[-102.0443,38.2627],[-101.5669,38.2633],[-101.5405,38.2631]]]},\"properties\":{\"name\":\"Hamilton\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0864","contributors":{"authors":[{"text":"Lobmeyer, David H.","contributorId":85156,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, C. G.","contributorId":52548,"corporation":false,"usgs":true,"family":"Sauer","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69530,"text":"hu29 - 1974 - Hydrologic Unit Map — 1974, States of New Hampshire and Vermont","interactions":[],"lastModifiedDate":"2022-01-05T22:36:41.234722","indexId":"hu29","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"29","subseriesTitle":"New Hamshire & Vermont 1974","title":"Hydrologic Unit Map — 1974, States of New Hampshire and Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu29","isbn":"607767871","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map — 1974, States of New Hampshire and Vermont: U.S. Geological Survey Hydrologic Unit 29, 1 Plate: 28.47 × 27.17 inches, https://doi.org/10.3133/hu29.","productDescription":"1 Plate: 28.47 × 27.17 inches","costCenters":[],"links":[{"id":252480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/29/report-thumb.jpg"},{"id":251555,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/29/plate-1.pdf","size":"4130","linkFileType":{"id":1,"text":"pdf"}},{"id":251554,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/hu/29/report.pdf","size":"26","linkFileType":{"id":1,"text":"pdf"}},{"id":393946,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16240.htm"}],"scale":"500000","country":"United States","state":"New Hampshire, Vermont","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.4326171875,\n              42.71473218539458\n            ],\n            [\n              -70.83984375,\n              42.71473218539458\n            ],\n            [\n              -70.83984375,\n              45.3444241045224\n            ],\n            [\n              -73.4326171875,\n              45.3444241045224\n            ],\n            [\n              -73.4326171875,\n              42.71473218539458\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614369","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":534620,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68064,"text":"ha487 - 1974 - Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2022-12-01T20:26:08.272857","indexId":"ha487","displayToPublicDate":"1994-01-01T00:00:00","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":"487","title":"Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming","docAbstract":"<p>The Great Basin Region is defined to include the drainage of the Great Basin physiographic section (Fennman, 1931) in Idaho, Nevada, Utah, and Wyoming. In October 1966, the President’s Water Resources Council requested that a comprehensive framework study be made in the Great Basin Region under the leadership of the Pacific Southwest Interagency Committee. The study, which included evaluation of the water resources of the region and guidelines for future study and development, was completed June 30, 1971. Results of the study received limited distribution.</p><p>The purpose of this atlas is to make available to the public the hydrologic data (including a general appraisal) that were compiled for the comprehensive framework study. Most of the work was done by a water-resources work group consisting of members from several Federal and State agencies under the chairmanship of Thomas E. Eakin of the U.S. Geological Survey. This atlas contains some data not included in the framework study.</p><p>The data presented herein are reconnaissance in nature and should be used with discretion. The maps are highly generalized and are intended only to illustrate the regional distribution of the supply and general chemical quality of the water. Sources of more detailed information on the hydrology of specific parts of the Great Basin region are listed in the selected references.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha487","collaboration":"Prepared in cooperation with the states of Idaho, Nevada, Utah, and Wyoming","usgsCitation":"Price, D., and Eakin, T., 1974, Water in the Great Basin region; Idaho, Nevada, Utah, and Wyoming: U.S. Geological Survey Hydrologic Atlas 487, 3 Plates: 47.0 x 40.0 inches or smaller, https://doi.org/10.3133/ha487.","productDescription":"3 Plates: 47.0 x 40.0 inches or smaller","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":91819,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Ground Water"},{"id":185540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89331,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Surface Water"},{"id":89330,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/487/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Physical Setting"},{"id":409947,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15876.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"2000000","country":"United States","state":"Idaho, Nevada, Utah, Wyoming","otherGeospatial":"Great Basin region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              35\n            ],\n            [\n              -110.5,\n              35\n            ],\n            [\n              -110.5,\n             43\n            ],\n            [\n              -120,\n              43\n            ],\n            [\n              -120,\n              35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9de8","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":277591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eakin, Thomas E.","contributorId":95449,"corporation":false,"usgs":true,"family":"Eakin","given":"Thomas E.","affiliations":[],"preferred":false,"id":277592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69534,"text":"hu12 - 1974 - Hydrologic Unit Map -- 1974, Idaho","interactions":[],"lastModifiedDate":"2018-12-10T14:14:44","indexId":"hu12","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"12","subseriesTitle":"Idaho 1974","title":"Hydrologic Unit Map -- 1974, Idaho","docAbstract":"<p>This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). The previous U.S. Geological Survey Catalog-Indexing System was by map number and letter, such as 49M. The boundaries as shown have been adapted from \"The Catalog of Information on Water Data\" (1972), \"Water Resources Regions and Subregions for the National Assessment of Water and Related Land Resources\" by the U.S. Water Resources Council (1970), \"River Basins of the United States\" by the U.S. Soil Conservation Service (1963, 1970), \"River Basin Maps Showing Hydrologic Stations\" by the Inter-Agency Committee on Water Resources, Subcommittee on Hydrology (1961), and State planning maps.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu12","isbn":"607767707","collaboration":"Prepared in cooperation with the U.S. Water Resources Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, Idaho: U.S. Geological Survey Hydrologic Unit 12, 42.80 x 67.48 inches, https://doi.org/10.3133/hu12.","productDescription":"42.80 x 67.48 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