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,{"id":68426,"text":"ha414 - 1971 - Floods in the Guayanilla-Yauco area, Puerto Rico","interactions":[{"subject":{"id":70203695,"text":"70203695 - 1969 - Floods in the Guayanilla-Yauco area, Puerto Rico","indexId":"70203695","publicationYear":"1969","noYear":false,"title":"Floods in the Guayanilla-Yauco area, Puerto Rico"},"predicate":"SUPERSEDED_BY","object":{"id":68426,"text":"ha414 - 1971 - Floods in the Guayanilla-Yauco area, Puerto Rico","indexId":"ha414","publicationYear":"1971","noYear":false,"title":"Floods in the Guayanilla-Yauco area, Puerto Rico"},"id":1}],"lastModifiedDate":"2024-05-29T20:13:09.553174","indexId":"ha414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"414","title":"Floods in the Guayanilla-Yauco area, Puerto Rico","docAbstract":"<p><span>This report is a compilation of data pertaining to floods in Rios Guayanilla and Yauco and is based principally upon information obtained from residents in the study area. This information is a useful tool in making land-use and development decisions.</span></p><p><span>The Guayanilla and Yauco basins lie in the southwestern part of Puerto Rico. The streams flow southward from the rugged Cordillera Central and empty into Bahia de Guayanilla. The lower basins are devoted principally to the production of sugarcane and are subject to destructive floods. Details pertaining to basin features, flood frequency, flood profiles, and inundated areas are discussed by individual basins. All elevations given are in meters above mean sea level.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha414","collaboration":"Prepared in cooperation with the Commonwealth of Puerto Rico Department of Public Works","usgsCitation":"Fields, F.K., 1971, Floods in the Guayanilla-Yauco area, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 414, 1 Plate: 43.57 x 36.94 inches, https://doi.org/10.3133/ha414.","productDescription":"1 Plate: 43.57 x 36.94 inches","costCenters":[],"links":[{"id":89951,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/414/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":429364,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15798.htm","linkFileType":{"id":5,"text":"html"}},{"id":186613,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/414/report-thumb.jpg"}],"scale":"20000","datum":"Mean Sea Level","country":"United States","state":"Puerto Rico","otherGeospatial":"Guayanilla-Yauco area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.875,\n              17.93333333\n            ],\n            [\n              -66.75,\n              17.93333333\n            ],\n            [\n              -66.75,\n              18.05833333\n            ],\n            [\n              -66.875,\n              18.05833333\n            ],\n            [\n              -66.875,\n              17.93333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e116f","contributors":{"authors":[{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63196,"text":"gq1021 - 1971 - Geologic map of the Sonora quadrangle, Pinal and Gila Counties, Arizona","interactions":[],"lastModifiedDate":"2013-02-14T10:32:21","indexId":"gq1021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1021","title":"Geologic map of the Sonora quadrangle, Pinal and Gila Counties, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/gq1021","usgsCitation":"Cornwall, H.R., Banks, N.G., and Phillips, C.H., 1971, Geologic map of the Sonora quadrangle, Pinal and Gila Counties, Arizona: U.S. Geological Survey Geologic Quadrangle 1021, 1 map., https://doi.org/10.3133/gq1021.","productDescription":"1 map.","costCenters":[],"links":[{"id":107465,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10566.htm","linkFileType":{"id":5,"text":"html"},"description":"10566"},{"id":262771,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://ngmdb.usgs.gov/ngm-bin/pdp/download.pl?q=967_10566_3","linkFileType":{"id":1,"text":"pdf"}},{"id":249316,"rank":300,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/gq/1021/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1021/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,33.1175 ], [ -111,33.25 ], [ -110.86749999999999,33.25 ], [ -110.86749999999999,33.1175 ], [ -111,33.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a70b","contributors":{"authors":[{"text":"Cornwall, Henry Rowland","contributorId":68304,"corporation":false,"usgs":true,"family":"Cornwall","given":"Henry","email":"","middleInitial":"Rowland","affiliations":[],"preferred":false,"id":268475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banks, Norman G.","contributorId":89524,"corporation":false,"usgs":true,"family":"Banks","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":268476,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, C. H.","contributorId":37414,"corporation":false,"usgs":true,"family":"Phillips","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268474,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","interactions":[{"subject":{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","indexId":"ofr71291","publicationYear":"1971","noYear":false,"title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"id":1}],"supersededBy":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"lastModifiedDate":"2022-06-06T19:51:44.388865","indexId":"ofr71291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-291","title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71291","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho: U.S. Geological Survey Open-File Report 71-291, 1 Plate: 29.41 x 42.51 inches, https://doi.org/10.3133/ofr71291.","productDescription":"1 Plate: 29.41 x 42.51 inches","costCenters":[],"links":[{"id":175557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0291/report-thumb.jpg"},{"id":401700,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Idaho","otherGeospatial":"Challis Quadrangle, Doublespring Quadrangle, Lone Pine Peak Quadrangle, May Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.8895263671875,\n              44.209772586984485\n            ],\n            [\n              -113.7579345703125,\n              44.209772586984485\n            ],\n            [\n              -113.7579345703125,\n              44.67646564865964\n            ],\n            [\n              -114.8895263671875,\n              44.67646564865964\n            ],\n            [\n              -114.8895263671875,\n              44.209772586984485\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69704b","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":530820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35210,"text":"b1311B - 1971 - Stratigraphy and potassium-argon ages of some Tertiary tuffs from Lander and Churchill Counties, central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b1311B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1311","chapter":"B","title":"Stratigraphy and potassium-argon ages of some Tertiary tuffs from Lander and Churchill Counties, central Nevada","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1311B","usgsCitation":"McKee, E.H., and Stewart, J.H., 1971, Stratigraphy and potassium-argon ages of some Tertiary tuffs from Lander and Churchill Counties, central Nevada: U.S. Geological Survey Bulletin 1311, iv, B28 p. :illus., maps (1 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1311B.","productDescription":"iv, B28 p. :illus., maps (1 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":166131,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1311b/report-thumb.jpg"},{"id":63083,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1311b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63084,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1311b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63085,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1311b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b05","contributors":{"authors":[{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":214255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, John Harris","contributorId":63790,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"Harris","affiliations":[],"preferred":false,"id":214256,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63366,"text":"gq918 - 1971 - Geologic map of the Ashland quadrangle, Columbia and Schuylkill Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq918","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"918","title":"Geologic map of the Ashland quadrangle, Columbia and Schuylkill Counties, Pennsylvania","language":"ENGLISH","doi":"10.3133/gq918","usgsCitation":"Arndt, H.H., 1971, Geologic map of the Ashland quadrangle, Columbia and Schuylkill Counties, Pennsylvania: U.S. Geological Survey Geologic Quadrangle 918, 1 map., https://doi.org/10.3133/gq918.","productDescription":"1 map.","costCenters":[],"links":[{"id":103633,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2219.htm","linkFileType":{"id":5,"text":"html"},"description":"2219"},{"id":249467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0918/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252949,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0918/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.36749999999999,40.75 ], [ -76.36749999999999,40.8675 ], [ -76.25,40.8675 ], [ -76.25,40.75 ], [ -76.36749999999999,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a23ce","contributors":{"authors":[{"text":"Arndt, Harold H.","contributorId":14412,"corporation":false,"usgs":true,"family":"Arndt","given":"Harold","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68622,"text":"ha363 - 1971 - Floods in Hebron Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"363","title":"Floods in Hebron Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha363","usgsCitation":"Allen, H., and Grant, R.S., 1971, Floods in Hebron Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 363, 1 col. map ;58 x 43 cm., on sheet 77 x 122 cm., https://doi.org/10.3133/ha363.","productDescription":"1 col. map ;58 x 43 cm., on sheet 77 x 122 cm.","costCenters":[],"links":[{"id":185646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90283,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/363/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,42.3675 ], [ -88.5,42.5 ], [ -88.36749999999999,42.5 ], [ -88.36749999999999,42.3675 ], [ -88.5,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70dd","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, R. Stephen","contributorId":83125,"corporation":false,"usgs":true,"family":"Grant","given":"R.","email":"","middleInitial":"Stephen","affiliations":[],"preferred":false,"id":278587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66309,"text":"i662 - 1971 - Geologic map of the Scenic area, Pennington, Shannon and Custer Counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-10T00:11:04","indexId":"i662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"662","subseriesTitle":"NONE","title":"Geologic map of the Scenic area, Pennington, Shannon and Custer Counties, South Dakota","language":"ENGLISH","doi":"10.3133/i662","usgsCitation":"King, R., and Raymond, W.H., 1971, Geologic map of the Scenic area, Pennington, Shannon and Custer Counties, South Dakota: U.S. Geological Survey IMAP 662, 1 map :col. ;88 x 96 cm. on sheet 101 x 103 cm. folded to 26 x 21 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i662.","productDescription":"1 map :col. ;88 x 96 cm. on sheet 101 x 103 cm. folded to 26 x 21 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106899,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9440.htm","linkFileType":{"id":5,"text":"html"},"description":"9440"},{"id":190234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.86749999999999,43.6175 ], [ -102.86749999999999,43.8675 ], [ -102.5,43.8675 ], [ -102.5,43.6175 ], [ -102.86749999999999,43.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b4a8","contributors":{"authors":[{"text":"King, R.U.","contributorId":7692,"corporation":false,"usgs":true,"family":"King","given":"R.U.","email":"","affiliations":[],"preferred":false,"id":274329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raymond, W. H.","contributorId":83919,"corporation":false,"usgs":true,"family":"Raymond","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274330,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63273,"text":"gq927 - 1971 - Geologic map of the Webbville quadrangle, eastern Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq927","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"927","title":"Geologic map of the Webbville quadrangle, eastern Kentucky","language":"ENGLISH","doi":"10.3133/gq927","usgsCitation":"Carlson, J.E., 1971, Geologic map of the Webbville quadrangle, eastern Kentucky: U.S. Geological Survey Geologic Quadrangle 927, 1 map., https://doi.org/10.3133/gq927.","productDescription":"1 map.","costCenters":[],"links":[{"id":103641,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2227.htm","linkFileType":{"id":5,"text":"html"},"description":"2227"},{"id":249379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0927/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0927/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.86749999999999,38.1175 ], [ -82.86749999999999,38.25 ], [ -82.75,38.25 ], [ -82.75,38.1175 ], [ -82.86749999999999,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689fa9","contributors":{"authors":[{"text":"Carlson, John Edward","contributorId":49803,"corporation":false,"usgs":true,"family":"Carlson","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":268588,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41946,"text":"ofr7175 - 1971 - Analytical data from samples of surficial deposits, Hampden Quadrangle, Massachusetts-Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr7175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-75","title":"Analytical data from samples of surficial deposits, Hampden Quadrangle, Massachusetts-Connecticut","language":"ENGLISH","doi":"10.3133/ofr7175","usgsCitation":"Colton, R.B., and Mallory, M.J., 1971, Analytical data from samples of surficial deposits, Hampden Quadrangle, Massachusetts-Connecticut: U.S. Geological Survey Open-File Report 71-75, 1 map +1 data sheet., https://doi.org/10.3133/ofr7175.","productDescription":"1 map +1 data sheet.","costCenters":[],"links":[{"id":136798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0075/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79705,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0075/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fbd0","contributors":{"authors":[{"text":"Colton, R. B.","contributorId":40186,"corporation":false,"usgs":true,"family":"Colton","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":225759,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mallory, M. J.","contributorId":10398,"corporation":false,"usgs":true,"family":"Mallory","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":225758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2853,"text":"wsp1899J - 1971 - Ground water for irrigation near Lake Emily, Pope County, west-central Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:01:12","indexId":"wsp1899J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1899","chapter":"J","title":"Ground water for irrigation near Lake Emily, Pope County, west-central Minnesota","docAbstract":"<p>In the Lake Emily area, thickness of the glacial drift ranges from about 200 feet to more than 400 feet. Within the drift are sand and gravel aquifers, some of which can yield adequate water supplies for irrigation. Outwash, as much as 60 feet thick, lies at the surface. The outwash has saturated thicknesses of more than 40 feet and transmissivities of more than 50,000 gallons per day per foot locally in the northern and western parts of the area. In the places of large saturated thickness and high hydraulic conductivity, the aquifer should yield more than 600 gallons per minute to wells. Theoretical maximum yields to wells in most of the area are more than 100 gallons per minute.</p>\n<p>Chemically, water in the buried and surficial aquifers is mainly of a calcium magnesium bicarbonate type and is suitable for irrigation. Calculated and estimated sodium adsorption ratios and salinity and boron concentrations are below the limits recommended by the U.S. Department of Agriculture.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1899J","collaboration":"Prepared in cooperation with the West-Central Minnesota Resource Conservation and Development Committee and the Minnesota Department of Conservation, Division of Waters, Soils, and Minerals","usgsCitation":"Van Voast, W.A., 1971, Ground water for irrigation near Lake Emily, Pope County, west-central Minnesota: U.S. Geological Survey Water Supply Paper 1899, iv, 28 p., https://doi.org/10.3133/wsp1899J.","productDescription":"iv, 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":139076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899j/report-thumb.jpg"},{"id":29444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Pope County","otherGeospatial":"Lake Emily","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-95.1388,45.7602],[-95.1384,45.5864],[-95.1319,45.5856],[-95.1322,45.4128],[-95.2549,45.4122],[-95.7451,45.4122],[-95.7483,45.585],[-95.7574,45.5853],[-95.7595,45.76],[-95.1388,45.7602]]]},\"properties\":{\"name\":\"Pope\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbc5","contributors":{"authors":[{"text":"Van Voast, Wayne A.","contributorId":91846,"corporation":false,"usgs":true,"family":"Van Voast","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2852,"text":"wsp1899E - 1971 - Ground water for irrigation in the Brooten-Belgrade area, west-central Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:00:47","indexId":"wsp1899E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1899","chapter":"E","title":"Ground water for irrigation in the Brooten-Belgrade area, west-central Minnesota","docAbstract":"<p>Water for irrigation is needed to improve crop yields from sandy soils in the Brooten-Belgrade area. Ground-water supplies of sufficient quantity and suitable quality for irrigation are available in much of the area.</p>\n<p>Quaternary glacial drift, as much as 300 feet thick, is underlain by Precambrian crystalline rocks and possibly by Cretaceous sedimentary rocks. Sand and gravel aquifers are buried at various depths in the drift and can be located by test drilling. One buried aquifer, possibly capable of high yields, is within 250 feet of the land surface in the vicinity of Belgrade.</p>\n<p>Glacial outwash comprises the upper part of the drift in most of the project area and is locally more than 100 feet thick. The outwash is made up of crossbedded sand and gravel that is interbedded in places with silt and clay deposits and has a saturated thickness of as much as 65 feet. Locally, the transmissivity of the surficial aquifer is as much as 60,000 gallons per day per foot, but elsewhere is generally less than 30,000 gallons per day per foot. The aquifer should yield more than 300 gallons per minute and locally more than 1,000 gallons per minute to individual wells in much of the northern and southwestern parts of the area.</p>\n<p>Recharge to the surficial aquifer is almost entirely from precipitation. Significant ground-water losses occur as base flow and underflow, and through evaporation and transpiration.</p>\n<p>Water in the buried and surficial aquifers is of the calcium magnesium bicarbonate type and is of suitable quality for irrigation.</p>\n<p>An analog model, simulating yearly 30-day pumping periods and hypothetical volumes and distributions of withdrawals, showed the effects on the surficial aquifer of withdrawals of about 20,000 acre-feet per pumping season for 20 years. Predicted water-level declines caused by withdrawals of 20,000 acre-feet per pumping season were generally less than 5 feet in the surficial aquifer and years Predicted water-level declines caused by withdrawals of 20,000 acre-feet pumping season caused predicted water-table declines of more than 10 feet in large parts of the area and caused lake-level declines of as much as 8 feet. The model indicated that water removed from aquifer and lake storage accounted for less than 50 percent of all withdrawals; the remainder was accounted for by water recovered from stream base flow and by water diverted from evaporation and transpiration.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1899E","collaboration":"Prepared in cooperation with the West-Central Minnesota Resource Conservation and Development Committee and the Minnesota Department of Conservation, Division of Waters, Soils, and Minerals","usgsCitation":"Van Voast, W.A., 1971, Ground water for irrigation in the Brooten-Belgrade area, west-central Minnesota: U.S. Geological Survey Water Supply Paper 1899, Document: iv, 24 p.; 2 Plates: 35 x 40 inches and 37 x 39 inches, https://doi.org/10.3133/wsp1899E.","productDescription":"Document: iv, 24 p.; 2 Plates: 35 x 40 inches and 37 x 39 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,{"id":2717,"text":"wsp1869G - 1971 - Techniques and equipment required for precise stream gaging in tide-affected fresh-water reaches of the Sacramento River, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1869G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1869","chapter":"G","title":"Techniques and equipment required for precise stream gaging in tide-affected fresh-water reaches of the Sacramento River, California","docAbstract":"Current-meter measurements of high accuracy will be required for calibration of an acoustic flow-metering system proposed for installation in the Sacramento River at Chipps Island in California. This report presents an analysis of the problem of making continuous accurate current-meter measurements in this channel where the flow regime is changing constantly in response to tidal action. Gaging-system requirements are delineated, and a brief description is given of the several applicable techniques that have been developed by others. None of these techniques provides the accuracies required for the flowmeter calibration. A new system is described--one which has been assembled and tested in prototype and which will provide the matrix of data needed for accurate continuous current-meter measurements. \r\n\r\nAnalysis of a large quantity of data on the velocity distribution in the channel of the Sacramento River at Chipps Island shows that adequate definition of the velocity can be made during the dominant flow periods--that is, at times other than slack-water periods--by use of current meters suspended at elevations 0.2 and 0.8 of the depth below the water surface. However, additional velocity surveys will be necessary to determine whether or not small systematic corrections need be applied during periods of rapidly changing flow. \r\n\r\nIn the proposed system all gaged parameters, including velocities, depths, position in the stream, and related times, are monitored continuously as a boat moves across the river on the selected cross section. Data are recorded photographically and transferred later onto punchcards for computer processing. \r\n\r\nComputer programs have been written to permit computation of instantaneous discharges at any selected time interval throughout the period of the current meter measurement program. It is anticipated that current-meter traverses will be made at intervals of about one-half hour over periods of several days. Capability of performance for protracted periods was, consequently, one of the important elements in system design. \r\n\r\nAnalysis of error sources in the proposed system indicates that errors in individual computed discharges can be kept smaller than 1.5 percent if the expected precision in all measured parameters is maintained.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1869G","usgsCitation":"Smith, W., 1971, Techniques and equipment required for precise stream gaging in tide-affected fresh-water reaches of the Sacramento River, California: U.S. Geological Survey Water Supply Paper 1869, vi, 46 p. ;24 cm., https://doi.org/10.3133/wsp1869G.","productDescription":"vi, 46 p. ;24 cm.","costCenters":[],"links":[{"id":139024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869g/report-thumb.jpg"},{"id":29101,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1869g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29102,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a321","contributors":{"authors":[{"text":"Smith, Winchell","contributorId":20311,"corporation":false,"usgs":true,"family":"Smith","given":"Winchell","email":"","affiliations":[],"preferred":false,"id":145658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2179,"text":"wsp1532D - 1971 - Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1532D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1532","chapter":"D","title":"Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66","docAbstract":"An intensive study of the effect of grazing on the hydrologic and biotic characteristics of small drainage basins on the Colorado Plateau was begun in the fall of 1953. This report presents data obtained during the first 13 years of the proposed 20-year study. \r\n\r\nFor the period of record 1954-66, runoff from grazed watersheds has averaged about 33 acre-feet per square mile per year. Runoff from ungrazed watersheds averaged from 71 to 76 percent of that from grazed watersheds. During the last 6 years of the period, however, ungrazed watersheds produced 69 to 71 percent as much runoff as grazed watersheds. The sediment yield frown grazed watersheds during the same period was about 3 acre-feet per square mile per year. Sediment yield from ungrazed watersheds ranged from 51 to 75 percent of that from grazed watersheds and averaged 66 percent. The largest change in these relations occurred about 2 years after livestock were excluded from certain watersheds. The causative factors for changes in the runoff and sediment yield relations are not entirely clear. At the end of 13 years, a significant change had occurred in the amount of bare soil and rock. in the ground-cover index, and in the litter and moss on the grazed watersheds. These items remained essentially unchanged on ungrazed watersheds. The changes in ground-cover factors were not of large magnitude and did not occur at the same rate as the changes in runoff and sediment yield. A large part of the difference appears to have been caused by a change in the structure of surface soil. which was brought about by the elimination of trampling by livestock. \r\n\r\nDeer mice were the most common rodent present on the experimental watersheds, but even their population was not great enough to affect the composition of range vegetation. Deer mice populations remained comparable on grazed and ungrazed watersheds during the study. Other rodents were not present in sufficient numbers to allow their comparison on grazed and ungrazed range. Desert cottontail rabbits and black-tailed jackrabbits were more plentiful in ungrazed watersheds but were not present in large enough numbers to affect range vegetation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1532D","usgsCitation":"Lusby, G.C., and Knipe, O., 1971, Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66: U.S. Geological Survey Water Supply Paper 1532, v, 90 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1532D.","productDescription":"v, 90 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":109968,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24708.htm","linkFileType":{"id":5,"text":"html"},"description":"24708"},{"id":138202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532d/report-thumb.jpg"},{"id":27799,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db5460de","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knipe, O.D.","contributorId":90158,"corporation":false,"usgs":true,"family":"Knipe","given":"O.D.","email":"","affiliations":[],"preferred":false,"id":144779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56527,"text":"wdrMO711 - 1971 - Water resources data for Missouri, water year 1971","interactions":[],"lastModifiedDate":"2025-09-02T16:07:32.843051","indexId":"wdrMO711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-71-1","title":"Water resources data for Missouri, water year 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMO711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Water resources data for Missouri, water year 1971: U.S. Geological Survey Water Data Report MO-71-1, xi, 375 p., https://doi.org/10.3133/wdrMO711.","productDescription":"xi, 375 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