{"pageNumber":"590","pageRowStart":"14725","pageSize":"25","recordCount":16498,"records":[{"id":68368,"text":"ha533 - 1975 - Floods in the Carolina-Rio Grande area, northeastern Puerto Rico","interactions":[],"lastModifiedDate":"2023-03-07T22:22:29.648059","indexId":"ha533","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"533","title":"Floods in the Carolina-Rio Grande area, northeastern Puerto Rico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha533","usgsCitation":"Haire, W.J., 1975, Floods in the Carolina-Rio Grande area, northeastern Puerto Rico: U.S. Geological Survey Hydrologic Atlas 533, 1 Plate: 58.00 x 41.63 inches, https://doi.org/10.3133/ha533.","productDescription":"1 Plate: 58.00 x 41.63 inches","costCenters":[],"links":[{"id":185795,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89853,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/533/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413798,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15924.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"20000","country":"United States","state":"Puerto Rico","otherGeospatial":"Carolina-Rio Grande area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.025,\n              18.333\n            ],\n            [\n              -66.025,\n              18.467\n            ],\n            [\n              -65.758,\n              18.467\n            ],\n            [\n              -65.758,\n              18.333\n            ],\n            [\n              -66.025,\n              18.333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b117e","contributors":{"authors":[{"text":"Haire, William J.","contributorId":70482,"corporation":false,"usgs":true,"family":"Haire","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68369,"text":"ha545 - 1975 - Floods in the Fajardo-Luquillo area, northeastern Puerto Rico","interactions":[],"lastModifiedDate":"2022-08-23T20:08:09.132258","indexId":"ha545","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"545","title":"Floods in the Fajardo-Luquillo area, northeastern Puerto Rico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha545","usgsCitation":"Haire, W.J., 1975, Floods in the Fajardo-Luquillo area, northeastern Puerto Rico: U.S. Geological Survey Hydrologic Atlas 545, 1 Plate: 47.00 × 35.50 inches, https://doi.org/10.3133/ha545.","productDescription":"1 Plate: 47.00 × 35.50 inches","costCenters":[],"links":[{"id":185796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405488,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15936.htm","linkFileType":{"id":5,"text":"html"}},{"id":89854,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/545/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"Puerto Rico","otherGeospatial":"Fajarido - Luguillo area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.787,\n              18.275\n            ],\n            [\n              -65.625,\n              18.275\n            ],\n            [\n              -65.625,\n              18.417\n            ],\n            [\n              -65.787,\n              18.417\n            ],\n            [\n              -65.787,\n              18.275\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0ec2","contributors":{"authors":[{"text":"Haire, William J.","contributorId":70482,"corporation":false,"usgs":true,"family":"Haire","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27621,"text":"wri759 - 1975 - Hydrology of the Albemarle-Pamlico region, North Carolina : A preliminary report on the impact of agricultural developments","interactions":[],"lastModifiedDate":"2017-01-20T11:33:32","indexId":"wri759","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-9","title":"Hydrology of the Albemarle-Pamlico region, North Carolina : A preliminary report on the impact of agricultural developments","docAbstract":"<p>Extensive agricultural land clearing and drainage operations underway in a 650 square mile part of the Albemarle-Pamlico region--a 1,634 square mile peninsula in North Carolina lying between Albemarle Sound on the North and the Pamlico River on the south--are changing the hydrology of the area.</p>\n<p>The artificial drainage system being constructed in the region, although it will probably result in only a slight modification of the natural annual evapotranspiration, overland runoff, and ground-water discharge, will likely result in several important problems.</p>\n<p>First, changes in the water quality of the sounds and estuaries resulting from the rapid runoff of storm waters may prove harmful to the fishery resources. Second, lowering of the water table may cause relatively rapid subsidence of the land surface in an irregular pattern in the extensive areas underlain by thick peat deposits as a result of biochemical oxidation, peat fires, and wind.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Raleigh, NC","doi":"10.3133/wri759","collaboration":"Prepared in cooperation with the North Carolina Department of Natural and Economic Resources","usgsCitation":"Heath, R., 1975, Hydrology of the Albemarle-Pamlico region, North Carolina : A preliminary report on the impact of agricultural developments: U.S. Geological Survey Water-Resources Investigations Report 75-9, vi, 98 p., https://doi.org/10.3133/wri759.","productDescription":"vi, 98 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri759.jpg"},{"id":323463,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":" Albemarle-Pamlico region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.23388671874999,\n              34.57895241036945\n            ],\n            [\n              -77.23388671874999,\n              36.54053616262899\n            ],\n            [\n              -75.322265625,\n              36.54053616262899\n            ],\n            [\n              -75.322265625,\n              34.57895241036945\n            ],\n            [\n              -77.23388671874999,\n              34.57895241036945\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f02","contributors":{"authors":[{"text":"Heath, Ralph C.","contributorId":53359,"corporation":false,"usgs":true,"family":"Heath","given":"Ralph C.","affiliations":[],"preferred":false,"id":198424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68417,"text":"ha541 - 1975 - Flood of June 22-23, 1972, at Lock Haven, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"541","title":"Flood of June 22-23, 1972, at Lock Haven, Pennsylvania","language":"ENGLISH","doi":"10.3133/ha541","usgsCitation":"Flippo, H.N., 1975, Flood of June 22-23, 1972, at Lock Haven, Pennsylvania: U.S. Geological Survey Hydrologic Atlas 541, 1 map., https://doi.org/10.3133/ha541.","productDescription":"1 map.","costCenters":[],"links":[{"id":188899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89939,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/541/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,41.08416666666667 ], [ -77.5,41.166666666666664 ], [ -77.36749999999999,41.166666666666664 ], [ -77.36749999999999,41.08416666666667 ], [ -77.5,41.08416666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed5c","contributors":{"authors":[{"text":"Flippo, Herbert N. Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":278184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26695,"text":"wri753 - 1975 - Hydrologic analysis of the valley-fill aquifer, North Platte River Valley, Goshen County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:18:26","indexId":"wri753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-3","title":"Hydrologic analysis of the valley-fill aquifer, North Platte River Valley, Goshen County, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri753","usgsCitation":"Crist, M.A., 1975, Hydrologic analysis of the valley-fill aquifer, North Platte River Valley, Goshen County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 75-3, v, 129 p. :ill., maps(part fold. in pocket) ;27 cm., https://doi.org/10.3133/wri753.","productDescription":"v, 129 p. :ill., maps(part fold. in pocket) ;27 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":119064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0003/report-thumb.jpg"},{"id":55558,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55559,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0003/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55560,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0003/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55561,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db61190a","contributors":{"authors":[{"text":"Crist, Marvin A.","contributorId":63376,"corporation":false,"usgs":true,"family":"Crist","given":"Marvin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12459,"text":"ofr7527 - 1975 - Hydrology of three sinkhole basins in southwestern Seminole County, Florida","interactions":[],"lastModifiedDate":"2024-07-31T20:08:21.251923","indexId":"ofr7527","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-27","title":"Hydrology of three sinkhole basins in southwestern Seminole County, Florida","docAbstract":"<p>The southwestern part of Seminole County--in east-central Florida-is characterized by sinkholes formed by the subsidence of surficial deposits into solution cavities in the underlying limestone deposits. The area includes three sinkhole basins created by such subsidence: Cranes Roost, Palm Springs, and Grace Lake.</p><p>Cranes Roost basin (drainage area, 5.02 square miles) contains a closed drainage system of lakes and swamps--including Lakes Adelaide, Florida, and Mobile--that terminates at Cranes Roost sink. It also contains Lake Orienta and two unnamed sinks which do not overflow into Cranes Roost sink.</p><p>Palm Springs basin (drainage area, 1.77 square miles) includes Lake Marion, Eleventh Hole Pond, and several small unconnected sinks.</p><p>Grace Lake basin (drainage area, 1.64 square miles) includes Island Lake which overflows into Grace Lake.</p><p>The recent spread of urban development has tended to encroach on the flood plains of lakes in these sinkhole basins and cause concern over the flood hazard that results. An investigation was made of the area to document the highest known lake levels, to examine possible effects of urbanization with regard to increasing the flood hazard, and to appraise the possibilities of controlling lake levels to reduce or limit the flood hazard.</p><p>The highest lake stages of record in the three sinkhole basins occurred in September 1960. Analyses of the hydrologic relations between lake stages, ground-water levels, stream discharges, and rainfall in the area indicated that the lake stages of September 1960 probably were the highest attained since at least 1895.</p><p>Cultural development that increases the percentage of a sink basin covered by impervious materials will cause more rapid runoff of a larger part of the rainfall in the basin. Thus, as development progresses, lake stages seldom reached under natural conditions may be reached more frequently unless the lake levels are controlled.</p><p>In Crane Roost basin, the levels of Lakes Mobile, Adelaide, and Florida could be controlled by enlarging their surface outlets and adding control structures; however, such measures might be ineffective unless the level of Cranes Roost also was controlled. The level of Cranes Roost could be controlled by removal of water by pumping or by providing a surface outlet; pumping might be ineffective during extreme wet periods because of the potential for inflow from upstream lakes and the potential for ground-water inflow from the Floridan aquifer. The level of Lake Orienta could be Controlled by removal of water by pumping or by providing a surface outlet.</p><p>In the Palm Springs sink basin, the levels of Lake Marion and the several small sinks could be controlled by removal of water by pumping or by providing surface outlets. For the several sinks, however, providing a surface outlet would require an extensive excavation and pumping might prove impractical because of seepage induced from the Floridan aquifer.</p><p>The level of Island Lake--in Grace Lake sink basin-could be controlled by enlarging its surface outlet and providing a control structure. The peak stage of Grace Lake could be reduced by lowering its outlet to the north, but release of water during wet periods might cause downstream flooding.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7527","collaboration":"Prepared in cooperation with the Board of County Commissioners of Seminole County","usgsCitation":"Anderson, W., and Hughes, G., 1975, Hydrology of three sinkhole basins in southwestern Seminole County, Florida: U.S. Geological Survey Open-File Report 75-27, Report: 59 p.; 6 Figures: 17.73 x 23.92 inches or smaller, https://doi.org/10.3133/ofr7527.","productDescription":"Report: 59 p.; 6 Figures: 17.73 x 23.92 inches or smaller","costCenters":[],"links":[{"id":431759,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431758,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431757,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431756,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431755,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431754,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431753,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146526,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0027/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Seminole County","otherGeospatial":"southwestern Seminole County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.53839079697836,\n              28.867357027113812\n            ],\n            [\n              -81.53839079697836,\n              28.66338961826405\n            ],\n            [\n              -81.14420156315663,\n              28.66338961826405\n            ],\n            [\n              -81.14420156315663,\n              28.867357027113812\n            ],\n            [\n              -81.53839079697836,\n              28.867357027113812\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc746","contributors":{"authors":[{"text":"Anderson, Warren","contributorId":7712,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","affiliations":[],"preferred":false,"id":166171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":166172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13293,"text":"ofr75105 - 1975 - Hydrology for land-use planning: The Hillside area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2023-12-11T21:50:42.482764","indexId":"ofr75105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-105","title":"Hydrology for land-use planning: The Hillside area, Anchorage, Alaska","docAbstract":"<p>Rapid residential growth of the Hillside area, Anchorage, Alaska, may cause depletion of aquifers and a change in quality of water resources as a result of extensive development of small-lot tracts. Ground-water yields are low and may be locally inadequate for single family requirements where wells produce from bedrock in the eastern Hillside region. At lower altitudes single family water requirements of 3 to 10 gallons per minute or 0.2 to 0.6 litre per second usually can be obtained, but aquifers capable of being pumped at larger yields for public supplies are uncommon. However, in a few localities, wells do produce 40 to 300 gallons per minute or 2.5 to 19 litres per second from sand and gravel aquifers lying within thick sequences of glacial till. Streamflow within the Hillside area is inadequate as a significant source of water for public supply. Springs, swamps, and water-logged surficial sediments in the Hillside area are mainly caused by hilly terrain and low permeability of surficial materials.</p><p>The relative vulnerability of streams, lakes, and ground water to pollution caused by the discharge of liquid waste, particularly from onsite sewage-disposal systems, is moderate to high in about half the study area. At higher altitudes contamination of bedrock aquifers may occur if discharge of liquid wastes is not regulated. The deep sedimentary aquifers at lower altitudes are less susceptible to contamination. However, shallow groundwater bodies may become polluted by discharge of sewage effluent and, consequently, some deep wells may be contaminated by seepage down the outside of casings or through leaky casing joints and underground seals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75105","collaboration":"Prepared in cooperation with the Greater Anchorage Area Borough","usgsCitation":"Dearborn, L.L., and Barnwell, W.W., 1975, Hydrology for land-use planning: The Hillside area, Anchorage, Alaska: U.S. Geological Survey Open-File Report 75-105, 45 p., https://doi.org/10.3133/ofr75105.","productDescription":"45 p.","costCenters":[],"links":[{"id":146731,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0105/report-thumb.jpg"},{"id":393069,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15092.htm"},{"id":423406,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Anchorage","otherGeospatial":"Hillside area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.803,\n              61.081\n            ],\n            [\n              -149.697,\n              61.081\n            ],\n            [\n              -149.697,\n              61.139\n            ],\n            [\n              -149.803,\n              61.139\n            ],\n            [\n              -149.803,\n              61.081\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604bdd","contributors":{"authors":[{"text":"Dearborn, Larry L.","contributorId":66687,"corporation":false,"usgs":true,"family":"Dearborn","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167555,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnwell, William W.","contributorId":73621,"corporation":false,"usgs":true,"family":"Barnwell","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":167556,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14128,"text":"ofr75573 - 1975 - Interpretation of geologic and hydrologic data from the Ray-1 Well, City of Gallup, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr75573","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-573","title":"Interpretation of geologic and hydrologic data from the Ray-1 Well, City of Gallup, McKinley County, New Mexico","docAbstract":"The Ray-1 well was to be the third production well completed in the city of Gallup Yah-ta-hey well field located about 7 miles (11 km) north of the city. The first string of casing collapsed during completion, however, and the well was abandoned before it could be tested. The lithology of the Upper Cretaceous Dalton Sandstone and Dilco Coal Members of the Crevasse Canyon Formation and the Gallup Sandstone was interpreted from geophysical logs and examination of the drill cuttings. These units appear to be similar to correlative strata encountered in the first two wells. A yield of approximately 700 gallons per minute (44 l/s), similar to the other wells in the Yah-ta-hey well field, is anticipated from the same aquifers when the Ray-1 replacement well is completed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75573","usgsCitation":"Hiss, W.L., and Marshall, J.G., 1975, Interpretation of geologic and hydrologic data from the Ray-1 Well, City of Gallup, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 75-573, 58 p. :maps ;29 cm.; (67 p. - PGS), https://doi.org/10.3133/ofr75573.","productDescription":"58 p. :maps ;29 cm.; (67 p. - PGS)","costCenters":[],"links":[{"id":146785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0573/report-thumb.jpg"},{"id":42768,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0573/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42769,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0573/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0573/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2b0","contributors":{"authors":[{"text":"Hiss, William L.","contributorId":8064,"corporation":false,"usgs":true,"family":"Hiss","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":168970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marshall, Jane G.","contributorId":6459,"corporation":false,"usgs":true,"family":"Marshall","given":"Jane","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168969,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14734,"text":"ofr75214 - 1975 - Hydrologic effects of reducing irrigation to maintain a permanent pool in John Martin Reservoir, Arkansas River Valley, Colorado","interactions":[],"lastModifiedDate":"2017-09-29T08:15:45","indexId":"ofr75214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-214","title":"Hydrologic effects of reducing irrigation to maintain a permanent pool in John Martin Reservoir, Arkansas River Valley, Colorado","docAbstract":"<p>The U.S. Geological Survey has evaluated a plan by the Colorado Division of Wildlife to maintain a permanent pool of 10,000 acre-feet (1.2x10<sup>7</sup> cubic metres) in John Martin Reservoir on the Arkansas River. The proposed pool would be maintained through the use of water formerly diverted by the Catlin Canal Company to irrigate land in the Arkansas River valley. This plan was evaluated using a mathematical simulation model developed to test management alternatives in a stream-aquifer system. A 25-year period from 1949 through 1973 was simulated using monthly time intervals. Based on this simulation, it is concluded that (1) the proposed change in water use would be adequate to maintain a permanent pool of the proposed size, (2) surface-water diversions by most other canals in the study area would increase slightly under the proposed plan, (3) the flow of the Arkansas River at the Colorado-Kansas State line would increase slightly under the proposed plan, and (4) the ground-water system would not be significantly affected by the proposed change in water-use plan.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75214","collaboration":"Prepared in cooperation with the Colorado Water Conservation Board","usgsCitation":"Luckey, R.R., 1975, Hydrologic effects of reducing irrigation to maintain a permanent pool in John Martin Reservoir, Arkansas River Valley, Colorado: U.S. Geological Survey Open-File Report 75-214, iv, 13 p., https://doi.org/10.3133/ofr75214.","productDescription":"iv, 13 p.","costCenters":[],"links":[{"id":148982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0214/report-thumb.jpg"},{"id":346207,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0214/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas River Valley, John Martin Reservoir","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.7445,37.6428],[-103.0766,37.6417],[-103.183,37.6424],[-103.2917,37.6426],[-103.4039,37.6423],[-103.5092,37.6432],[-103.5778,37.6432],[-103.6016,37.6437],[-103.8109,37.644],[-103.8929,37.644],[-103.9661,37.6439],[-104.0591,37.6436],[-104.0597,37.7316],[-104.3518,37.8148],[-104.3889,37.8248],[-104.4978,37.8556],[-104.6074,37.886],[-104.6527,37.8982],[-104.7175,37.8949],[-104.9375,37.8834],[-104.9545,37.8822],[-104.9737,37.881],[-105.0017,37.8794],[-105.0041,37.8794],[-105.0093,37.879],[-105.0122,37.8799],[-105.0209,37.8859],[-105.0313,37.8919],[-105.0295,37.8964],[-105.03,37.9],[-105.0346,37.9055],[-105.0468,37.9115],[-105.0474,37.9967],[-105.0481,38.0855],[-105.0481,38.173],[-105.0483,38.202],[-105.0487,38.2582],[-104.9391,38.2587],[-104.9402,38.3448],[-104.9392,38.4178],[-104.939,38.43],[-104.9397,38.5003],[-104.9427,38.5003],[-104.943,38.5175],[-104.8295,38.5183],[-104.736,38.5183],[-104.7171,38.5186],[-104.6071,38.5187],[-104.4971,38.5192],[-104.3759,38.52],[-104.2836,38.5201],[-104.2794,38.5205],[-104.2759,38.5204],[-104.1629,38.5215],[-104.054,38.523],[-103.9411,38.523],[-103.8328,38.523],[-103.7228,38.5223],[-103.6116,38.5225],[-103.6118,38.5171],[-103.5089,38.5159],[-103.508,38.4366],[-103.5066,38.3409],[-103.5019,38.3408],[-103.5004,38.2646],[-103.3972,38.2647],[-103.2787,38.2649],[-103.1691,38.2647],[-103.0571,38.2647],[-102.741,38.2654],[-102.6154,38.2661],[-102.5075,38.2662],[-102.396,38.2662],[-102.2858,38.2665],[-102.1749,38.2668],[-102.0443,38.2676],[-102.0443,38.2627],[-102.0432,37.7384],[-102.043,37.6429],[-102.089,37.643],[-102.199,37.6429],[-102.3071,37.6435],[-102.4182,37.6432],[-102.5281,37.6432],[-102.6363,37.6435],[-102.7445,37.6428]]]},\"properties\":{\"name\":\"Bent\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ec9","contributors":{"authors":[{"text":"Luckey, Richard R.","contributorId":17980,"corporation":false,"usgs":true,"family":"Luckey","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":169924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48228,"text":"ofr741028 - 1975 - Hydrologic data processing system for Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"ofr741028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"74-1028","title":"Hydrologic data processing system for Brazil","language":"ENGLISH","doi":"10.3133/ofr741028","usgsCitation":"Edwards, M.D., 1975, Hydrologic data processing system for Brazil: U.S. Geological Survey Open-File Report 74-1028, 201 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr741028.","productDescription":"201 p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":172596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6072a0","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":237002,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48229,"text":"ofr741029 - 1975 - Implementation of a hydrologic data processing system in Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"ofr741029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"74-1029","title":"Implementation of a hydrologic data processing system in Brazil","language":"ENGLISH","doi":"10.3133/ofr741029","usgsCitation":"Edwards, M.D., 1975, Implementation of a hydrologic data processing system in Brazil: U.S. Geological Survey Open-File Report 74-1029, 201 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr741029.","productDescription":"201 p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":172597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c37e","contributors":{"authors":[{"text":"Edwards, Melvin D.","contributorId":94305,"corporation":false,"usgs":true,"family":"Edwards","given":"Melvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":237003,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16171,"text":"ofr75268 - 1975 - Hydrologic reconnaissance of the Montezuma Creek-Aneth area, southeastern Utah","interactions":[],"lastModifiedDate":"2017-09-03T14:08:56","indexId":"ofr75268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-268","title":"Hydrologic reconnaissance of the Montezuma Creek-Aneth area, southeastern Utah","docAbstract":"The Montezuma Creek-Aneth area is in the northeastern part of the Navajo Indian Reservation in southeastern Utah. It is a semiarid area along the San Juan River near the communities of Montezuma Creek and Aneth. Within the Blanding Basin, geologic formations exposed are of Jurassic and Quaternary age. The rock strata are nearly horizontal, dipping gently northeastward. Wells derive small quantities of mater for domestic use from aquifers in the Morrison Formation and the Bluff Sandstone of Jurassic age, but aquifers in deeper formations contain saline mater or brine. Alluvium consisting of sand and gravel along the San Juan River is a potential source of additional moderately large quantities of water to shallow wells for industrial use and public supply. The chemical quality of water in the alluvium is good and varies directly with the discharge of the San Juan River.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr75268","usgsCitation":"Sumsion, C.T., 1975, Hydrologic reconnaissance of the Montezuma Creek-Aneth area, southeastern Utah: U.S. Geological Survey Open-File Report 75-268, Report: 32 p.; 4 Tables: 18.48 in x 15.49 in. or smaller; 1 Figure: 23.43 in. x 18.66 in., https://doi.org/10.3133/ofr75268.","productDescription":"Report: 32 p.; 4 Tables: 18.48 in x 15.49 in. or smaller; 1 Figure: 23.43 in. x 18.66 in.","numberOfPages":"30","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":45112,"rank":303,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0268/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45107,"rank":403,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1975/0268/plate-1.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"General description and water-bearing characteristics of geologic units in the Montezuma Creek-Aneth area"},{"id":45109,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1975/0268/plate-3.pdf","text":"Table 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Records of selected wells in alluvium"},{"id":45110,"rank":6,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1975/0268/plate-4.pdf","text":"Table 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Chemical analyses of water from selected wells"},{"id":45111,"rank":4,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1975/0268/plate-5.pdf","text":"Table 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Records of selected wells in consolidated formations"},{"id":148816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0268/report-thumb.jpg"},{"id":45108,"rank":404,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0268/plate-2.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing locaitons of selected wells and alluvium along the San Juan River, Montezuma Creek-Aneth area"}],"publicComments":"Prepared for the U.S. Public Health Service","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055c4","contributors":{"authors":[{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":172353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68498,"text":"ha513 - 1975 - Ground-water levels on Boston peninsula, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha513","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"513","title":"Ground-water levels on Boston peninsula, Massachusetts","language":"ENGLISH","doi":"10.3133/ha513","usgsCitation":"Cotton, J.E., and Delaney, D.F., 1975, Ground-water levels on Boston peninsula, Massachusetts: U.S. Geological Survey Hydrologic Atlas 513, 4 maps :col. ;93 x 108 fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha513.","productDescription":"4 maps :col. ;93 x 108 fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90059,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/513/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90060,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/513/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90061,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/513/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90062,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/513/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"6000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.10111111111111,42.31805555555556 ], [ -71.10111111111111,42.38361111111111 ], [ -71.05,42.38361111111111 ], [ -71.05,42.31805555555556 ], [ -71.10111111111111,42.31805555555556 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674a5","contributors":{"authors":[{"text":"Cotton, John E.","contributorId":99106,"corporation":false,"usgs":true,"family":"Cotton","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Delaney, David F.","contributorId":41797,"corporation":false,"usgs":false,"family":"Delaney","given":"David","email":"","middleInitial":"F.","affiliations":[{"id":27261,"text":"U.S. Army Construction Engineering Research Laboratory, Champaig","active":true,"usgs":false}],"preferred":false,"id":278330,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68253,"text":"ha502 - 1975 - Hydrogeology along the proposed barrier-recharge-well alinement in southern Nassau County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"502","title":"Hydrogeology along the proposed barrier-recharge-well alinement in southern Nassau County, Long Island, New York","language":"ENGLISH","doi":"10.3133/ha502","usgsCitation":"Ku, H.F., Vecchioli, J., and Cerrillo, L.A., 1975, Hydrogeology along the proposed barrier-recharge-well alinement in southern Nassau County, Long Island, New York: U.S. Geological Survey Hydrologic Atlas 502, 1 map :col. ;40 x 49 cm. on sheet 106 x 104 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha502.","productDescription":"1 map :col. ;40 x 49 cm. on sheet 106 x 104 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89639,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/502/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.75,40.56777777777778 ], [ -73.75,40.75 ], [ -73.41666666666667,40.75 ], [ -73.41666666666667,40.56777777777778 ], [ -73.75,40.56777777777778 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627845","contributors":{"authors":[{"text":"Ku, Henry F. H.","contributorId":11258,"corporation":false,"usgs":true,"family":"Ku","given":"Henry","email":"","middleInitial":"F. H.","affiliations":[],"preferred":false,"id":277914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":277915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cerrillo, Lawrence A.","contributorId":106374,"corporation":false,"usgs":true,"family":"Cerrillo","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68236,"text":"ha514 - 1975 - Water resources of the Huron River Basin, southeastern Michigan","interactions":[],"lastModifiedDate":"2017-01-11T12:25:45","indexId":"ha514","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"514","title":"Water resources of the Huron River Basin, southeastern Michigan","docAbstract":"<p>This hydrologic atlas represents a part of a comprehensive study of the water resources of southeastern Michigan. Its purpose is to provide information on (1) physical features of the Huron River and its tributaries, (2) characteristics of streamflow, (3) quality of ground and surface water, and (4) availability of ground water. This atlas is one in a series of atlases on several river basins in southeastern Michigan.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha514","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Larson, R., Allen, W.B., and Hanson, S., 1975, Water resources of the Huron River Basin, southeastern Michigan: U.S. Geological Survey Hydrologic Atlas 514, Document: 22 p.; 2 Plates: 49 x 41 inches and 45.5 x 41.0 inches , https://doi.org/10.3133/ha514.","productDescription":"Document: 22 p.; 2 Plates: 49 x 41 inches and 45.5 x 41.0 inches ","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":68658,"text":"ha543 - 1975 - Water resources of the Zumbro River watershed, southeastern Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T10:20:49","indexId":"ha543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"543","title":"Water resources of the Zumbro River watershed, southeastern Minnesota","docAbstract":"<p>The Zumbro River drains 1,428 square miles and falls from about 1,300 feet altitude in its headwaters to 665 feet at its mouth. The remaining 248 square miles included in the watershed is drained by small creeks flowing directly into the Mississippi River. Distribution of water use is about as follows: domestic, 50 percent; farm (for irrigation and livestock), 18 percent; and industrial, 32 percent. Total usage, in water-budget terms, is 0.24 inch over the entire watershed, or less than 1 percent of inflow (average annual precipitation). Total quantity of water, thus, is of lesser concern than local availability and quality of water. The dominant ions (calcium, magnesium, and bicarbonate) and dissolved solids are reduced by dilution during periods of high water discharge in the Zumbro River at Zumbro Falls. Similarly, in the South Fork Zumbro River near Rochester, dominant ions, dissolved solids, and those ions that are increased by waste disposal (sodium, chloride, and nitrates) are all reduced by dilution at high water discharge. For the Zumbro River the smallest monthly range and the most uniform daily mean discharge usually occurs in January, whereas the greatest range usually occurs in March. The lowest flows usually occur in the winter and the highest during the spring ice breakup. The lowest observed flow, 47 cfs, occurred on February 18, 1961 and the highest, 23,600 cfs, occurred on March 29, 1962. Seventeen of 22 municipalities obtain at least part of their water supply from the Prairie du Chien-Jordan aquifer. Although only one town uses the Galena aquifer, a large number of private domestic wells are completed in it in the western part of the watershed. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ha543","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Anderson, H.W., Farrell, D., Broussard, W., and Hult, M.F., 1975, Water resources of the Zumbro River watershed, southeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 543, 3 Plates: 41.50 x 34.00 inches, https://doi.org/10.3133/ha543.","productDescription":"3 Plates: 41.50 x 34.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":189899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90362,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/543/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90363,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/543/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90364,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/543/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Minnesota","otherGeospatial":"Zumbro River watershed","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.53097534179686, 44.577752058683366 ], [ -92.47329711914062, 44.57286088638149 ], [ -92.44720458984375, 44.56503415498704 ], 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,{"id":68655,"text":"ha548 - 1975 - Water resources of the Root River watershed, southeastern Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T11:30:19","indexId":"ha548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"548","title":"Water resources of the Root River watershed, southeastern Minnesota","docAbstract":"<p>This Hydrologic Atlas is one of a series describing the 39 watersheds in Minnesota. The Root River watershed includes Houston, Winona, and parts of the surrounding counties. The 2 ,570 square miles in the watershed varies from gently rolling prairie in the west to an area of plateaus separated by valleys deeply incised into bedrock in the north and east. The average annual water budget for 30 years shows 29.5 inches of precipitation, 7.2 inches of surface runoff, and 22.3 inches of evapotranspiration. Water use in millions of gallons for 1970 was established at 7,310 of ground water and 6,700 of surface water. Domestic supplies accounted for less than one fourth and thermoelectric power for about one half of the total use. All 33 municipalities use ground water from bedrock aquifers, and 21 of those obtain at least part of their supply from the Prairie du Chien-Jordan aquifer. Many private domestic wells are completed in a shallow limestone aquifer. The ground-water system is recharged primarily by infiltrating precipitation in upland areas Ground-water movement is indicated by water-table and potentiometric maps and section diagrams. Water from bedrock and glacial aquifers generally is of acceptable quality for domestic use, dissolved solids generally less than 400 mg/liter very hard , and locally high iron content. The Mount Simon-Red clastics aquifer is locally saline. Runoff is greatest during the spring when snowmelt occurs and the soils are generally saturated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha548","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Broussard, W., Farrell, D., Anderson, H.W., and Felsheim, P., 1975, Water resources of the Root River watershed, southeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 548, 3 Plates: 52.25 x 38.50 inches or smaller, https://doi.org/10.3133/ha548.","productDescription":"3 Plates: 52.25 x 38.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":189896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90353,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/548/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90354,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/548/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90355,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/548/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Minnesota","otherGeospatial":"Root River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.92192077636719,\n              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W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":626918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Felsheim, P.E.","contributorId":39395,"corporation":false,"usgs":true,"family":"Felsheim","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":626919,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68666,"text":"ha521 - 1975 - Water resources of Gove, Logan, and Wallace Counties, west-central Kansas","interactions":[],"lastModifiedDate":"2018-12-10T15:07:54","indexId":"ha521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"521","title":"Water resources of Gove, Logan, and Wallace Counties, west-central Kansas","docAbstract":"<p>This atlas presents information on the geology and water resources of a three-county area in west-central Kansas (index map). The report is intended promarily as a guide to the availability of ground water, which is the main source of supply for domestic, stock, inductrial, irrigation, and municipal uses.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha521","usgsCitation":"McClain, T.J., Jenkins, E., Keene, K.M., and Pabst, M.E., 1975, Water resources of Gove, Logan, and Wallace Counties, west-central Kansas: U.S. Geological Survey Hydrologic Atlas 521, 2 Plates: 37.28 x 23.87 inches and 39.74 x 33.32 inches, https://doi.org/10.3133/ha521.","productDescription":"2 Plates: 37.28 x 23.87 inches and 39.74 x 33.32 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha521.PNG"},{"id":360122,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/521/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327452,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/521/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Kansas","county":"Gove County, Logan County, Wallace County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102,38.7 ], [ -102,39.11666666666667 ], [ -100.16666666666667,39.11666666666667 ], [ -100.16666666666667,38.7 ], [ -102,38.7 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0804","contributors":{"authors":[{"text":"McClain, Thomas J.","contributorId":104981,"corporation":false,"usgs":true,"family":"McClain","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenkins, Edward D.","contributorId":17972,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward D.","affiliations":[],"preferred":false,"id":643066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keene, Katherine M.","contributorId":17994,"corporation":false,"usgs":true,"family":"Keene","given":"Katherine","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":643067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":643068,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68334,"text":"ha534 - 1975 - Water resources of the Mississippi and Sauk Rivers Watershed, central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:55:30","indexId":"ha534","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"534","title":"Water resources of the Mississippi and Sauk Rivers Watershed, central Minnesota","docAbstract":"<p>A variety of glacial landforms (moraines, till plains, drumlin fields and outwash plains) characterized the 3,890-square mile Mississippi and Sauk Rivers watershed.</p>\n<p>Underlying the glacial drift are Cambrian and Precambrian sedimentary rocks in the southeastern part of the watershed and Precambrian igneous and metamorphic rocks elsewhere.</p>\n<p>Surface drainage is entirely to the Mississippi River, the largest tributary being the Sauk River, which drains an area of about 970 square miles. The Mississippi follows a regional topographic low and transects the watershed from north to south. Greatest relief is in the morainal area in the west-central part of the watershed. The outwash plain in the southeastern part of the watershed and associated terrace deposits along the Mississippi River form a large area of relatively low relief. Details of topography are shown on 7 &frac12; and 15&rsquo; U.S. Geological Survey quadrangle maps, as indexed.</p>\n<p>Agriculture is the major economic activity. Small communities are scattered throughout the watershed; most larger municipalities and related development are concentrated along the Mississippi River.</p>\n<p>Lakes and streams offer good recreational opportunities.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha534","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Helgesen, J.O., Ericson, D.W., and Lindholm, G.F., 1975, Water resources of the Mississippi and Sauk Rivers Watershed, central Minnesota: U.S. Geological Survey Hydrologic Atlas 534, 3 Plates: 52.0 x 39.5 inches, https://doi.org/10.3133/ha534.","productDescription":"3 Plates: 52.0 x 39.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":68332,"text":"ha544 - 1975 - Water resources of the Lake of the Woods watershed, north-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T11:57:00","indexId":"ha544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"544","title":"Water resources of the Lake of the Woods watershed, north-central Minnesota","docAbstract":"<p>The Lake of the Woods watershed is an area of about 2,900 square miles (7,500 km), the northern limit of which is part of the boundary between the United States and Canada. Drainage is to Lake of the Woods, either directly or by the Rainy River. The watershed includes about 470 square miles (1,220 km2) of Lake of the Woods, one-third of the lake&rsquo;s total area.</p>\n<p>The watershed, a part of the plain of glacial Lake Agassiz, is an area of low relief and slopes generally northward. Details of topography may be obtained from U.S. Geological Survey 7 1/2-minute quadrangle maps, as indexed.</p>\n<p>Surficial materials consist mainly of peat, lake-washed till, and beach deposits. Extensive wetlands typify much of the watershed. Bedrock is exposed in places near Lake of the Woods and the Rainy River.</p>\n<p>Except where cleared for cultivation, most of the watershed is covered by coniferous forests. Harvest of forest products, agriculture, and fishing are major economic activities.</p>\n<p>The 1970 population of the watershed was bout 6,600, concentrated chiefly along the Rainy River and the south shore of Lake of the Woods.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha544","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Helgesen, J.O., Lindholm, G.F., and Ericson, D.W., 1975, Water resources of the Lake of the Woods watershed, north-central Minnesota: U.S. Geological Survey Hydrologic Atlas 544, 2 Plates: 39.5 x 58.0 inches and 35.5 x 40.0 inches, https://doi.org/10.3133/ha544.","productDescription":"2 Plates: 39.5 x 58.0 inches and 35.5 x 40.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":186604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89803,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/544/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89804,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/544/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Minnesota","otherGeospatial":"Lake of the Woods watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.15396118164062,\n              49.00004203215395\n            ],\n            [\n              -95.39978027343749,\n              48.99733908118444\n            ],\n        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,{"id":68215,"text":"ha539 - 1975 - Water resources of the thrust belt of western Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha539","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"539","title":"Water resources of the thrust belt of western Wyoming","language":"ENGLISH","doi":"10.3133/ha539","usgsCitation":"Lines, G.C., and Glass, W.R., 1975, Water resources of the thrust belt of western Wyoming: U.S. Geological Survey Hydrologic Atlas 539, 6 maps :part col. ;on 3 sheets 92 x 132 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha539.","productDescription":"6 maps :part col. ;on 3 sheets 92 x 132 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89566,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/539/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89567,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/539/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89568,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/539/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41 ], [ -111,43.5 ], [ -110.5,43.5 ], [ -110.5,41 ], [ -111,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4b53","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glass, William R.","contributorId":107304,"corporation":false,"usgs":true,"family":"Glass","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":277856,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68649,"text":"ha552 - 1975 - Water resources of the Cedar River watershed, southeastern Minnesota","interactions":[{"subject":{"id":44063,"text":"ofr74191 - 1974 - Water resources of the Cedar River watershed, southeastern Minnesota","indexId":"ofr74191","publicationYear":"1974","noYear":false,"title":"Water resources of the Cedar River watershed, southeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68649,"text":"ha552 - 1975 - Water resources of the Cedar River watershed, southeastern Minnesota","indexId":"ha552","publicationYear":"1975","noYear":false,"title":"Water resources of the Cedar River watershed, southeastern Minnesota"},"id":1}],"lastModifiedDate":"2018-03-12T11:05:22","indexId":"ha552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"552","title":"Water resources of the Cedar River watershed, southeastern Minnesota","docAbstract":"<p>The Cedar River Watershed Unit (as established by the states of Minnesota) consists of 1,204 square miles (3,118 square kilometres) of flat or gently undulating plain.</p>\n<p>The watershed is drained by the Cedar River and several smaller streams that flow south into Iowa and eventually into the Mississippi River.</p>\n<p>Its easternmost neck is part of a broad, flat, well-drained plain, covered by a thin sheet of glacial drift. Sinkholes have formed in the near surface carbonate bedrock, and a karst topography is developing. Farther north, along the east boundary, the drift is more than 200 feet (61 m) thick, and the land surface reaches altitudes of more than 1,450 feet (442 m) &ndash; the highest area in southeastern Minnesota. In the central part of the watershed in the southern flood plain of the Cedar River, the drift is less than 100 feet (30 m) thick, and the land surface altitude is less than 1,140 feet (347 m). The western part is dominated by a terminal moraine of the last Wisconsin glacier. Here the drift is more than 300 feet (91 m) thick, is poorly drained, and has numerous lakes.</p>\n<p>The watershed is mostly prairie and is well suited for farming, which is the dominant economic activity.</p>\n<p>Topographic quadrangle maps published by the U.S. Geological Survey are available for the entire watershed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha552","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, Division of Waters, Soils, and Minerals","usgsCitation":"Farrell, D., Broussard, W., Anderson, H.W., and Hult, M.F., 1975, Water resources of the Cedar River watershed, southeastern Minnesota: U.S. Geological Survey Hydrologic Atlas 552, 3 Plates: 51.50 x 36.50 inches or smaller, https://doi.org/10.3133/ha552.","productDescription":"3 Plates: 51.50 x 36.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota 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