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,{"id":5696,"text":"pp652 - 1971 - Ore deposits of the Kokomo-Tenmile District, Colorado","interactions":[{"subject":{"id":55428,"text":"ofr4216 - 1942 - Topographic and geologic map of the Kokomo-Robinson area, Summit County, Colorado","indexId":"ofr4216","publicationYear":"1942","noYear":false,"title":"Topographic and geologic map of the Kokomo-Robinson area, Summit County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5696,"text":"pp652 - 1971 - Ore deposits of the Kokomo-Tenmile District, Colorado","indexId":"pp652","publicationYear":"1971","noYear":false,"title":"Ore deposits of the Kokomo-Tenmile District, Colorado"},"id":1},{"subject":{"id":55432,"text":"ofr4452 - 1944 - Geologic map of the Kokomo mining district, Colorado","indexId":"ofr4452","publicationYear":"1944","noYear":false,"title":"Geologic map of the Kokomo mining district, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5696,"text":"pp652 - 1971 - Ore deposits of the Kokomo-Tenmile District, Colorado","indexId":"pp652","publicationYear":"1971","noYear":false,"title":"Ore deposits of the Kokomo-Tenmile District, Colorado"},"id":2},{"subject":{"id":55522,"text":"ofr4552 - 1945 - Preliminary report on Kokomo mining district, Colorado","indexId":"ofr4552","publicationYear":"1945","noYear":false,"title":"Preliminary report on Kokomo mining district, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5696,"text":"pp652 - 1971 - Ore deposits of the Kokomo-Tenmile District, Colorado","indexId":"pp652","publicationYear":"1971","noYear":false,"title":"Ore deposits of the Kokomo-Tenmile District, Colorado"},"id":3},{"subject":{"id":55609,"text":"ofr4834 - 1948 - Map of the Kokomo (Tenmile) zinc-lead mining district, Colorado","indexId":"ofr4834","publicationYear":"1948","noYear":false,"title":"Map of the Kokomo (Tenmile) zinc-lead mining district, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":5696,"text":"pp652 - 1971 - Ore deposits of the Kokomo-Tenmile District, Colorado","indexId":"pp652","publicationYear":"1971","noYear":false,"title":"Ore deposits of the Kokomo-Tenmile District, Colorado"},"id":4}],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp652","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"652","title":"Ore deposits of the Kokomo-Tenmile District, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp652","usgsCitation":"Bergendahl, M., and Koschmann, A.H., 1971, Ore deposits of the Kokomo-Tenmile District, Colorado: U.S. Geological Survey Professional Paper 652, 53 p., https://doi.org/10.3133/pp652.","productDescription":"53 p.","costCenters":[],"links":[{"id":104708,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4972.htm","linkFileType":{"id":5,"text":"html"},"description":"4972"},{"id":140757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0652/report-thumb.jpg"},{"id":112556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0652/report.pdf","size":"11032","linkFileType":{"id":1,"text":"pdf"}},{"id":112557,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0652/plate-1.pdf","size":"6281","linkFileType":{"id":1,"text":"pdf"}},{"id":112558,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0652/plate-2.pdf","size":"3773","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691285","contributors":{"authors":[{"text":"Bergendahl, M.H.","contributorId":23538,"corporation":false,"usgs":true,"family":"Bergendahl","given":"M.H.","affiliations":[],"preferred":false,"id":151452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koschmann, Albert Herbert","contributorId":77525,"corporation":false,"usgs":true,"family":"Koschmann","given":"Albert","email":"","middleInitial":"Herbert","affiliations":[],"preferred":false,"id":151453,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4318,"text":"cir662 - 1971 - Index of surface-water records to September 30, 1970; Part 12, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"662","title":"Index of surface-water records to September 30, 1970; Part 12, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir662","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970; Part 12, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Circular 662, 40 p. :ill. ;27 cm., https://doi.org/10.3133/cir662.","productDescription":"40 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":117104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0662/report-thumb.jpg"},{"id":31428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2c77","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":528180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5839,"text":"pp732A - 1971 - Channel movement of meandering Indiana streams","interactions":[],"lastModifiedDate":"2016-05-13T10:41:13","indexId":"pp732A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"732","chapter":"A","title":"Channel movement of meandering Indiana streams","docAbstract":"<p>The process of channel movement in a meander system involves rotation and translation of meander loops and an increasing path length. The amount of path-length increase is directly proportional to the impulse supplied by discharge and is inversely proportional to the silt-clay percentage of the material composing the channel perimeter.</p>\n<p>Comparable paths have been obtained by standardizing measurements with a sine-generated curve and a moving reference axis. Analysis of previous investigations and time-of-travel data indicates that the discharge effective in channel formation consists of the range beginning just higher than the average and continuing throughout all higher discharges. Of six field sites investigated, three meander systems had path-length increases of sufficient magnitude to correlate with above-average discharge volume, one had no discernible change over a 30-year period, and two had changes which were too small for correlation owing to the short period of time covered by the available data.</p>\n<p>Because of the consistency of yearly above-average discharge volumes, it was possible to develop a general relation between path-length increase per thousand cubic-feet-per-second-days per square mile of drainage area above average discharge and the width-depth ratio of the channel. Little progress was made toward defining relationships for rotation and translation.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp732A","collaboration":"State of Indiana Department of  Natural Resources","usgsCitation":"Daniel, J.F., 1971, Channel movement of meandering Indiana streams: U.S. Geological Survey Professional Paper 732, 17 p., https://doi.org/10.3133/pp732A.","productDescription":"17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":32598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0732a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0732a/report-thumb.jpg"}],"country":"United 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,{"id":37198,"text":"rp100 - 1971 - Blackbirds and the southern rice crop","interactions":[],"lastModifiedDate":"2020-09-24T18:30:25.34991","indexId":"rp100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"100","title":"Blackbirds and the southern rice crop","docAbstract":"<p>Blackbirds have been a problem to the rice grower since colonial times. The problem has existed wherever rice is grown because man, by his culture of rice (Oryza sativa), creates food-rich ricefield marshes that apparently are more attractive to blackbirds than the natural marshes in which they have flourished for centuries.</p>\n<p>In the 1700's and 1800's, rice was grown in the lowlands of South Carolina, Georgia, and North Carolina - on the major migratory route of the bobolink (<i>Dolichonyx oryzivorus</i>), the historic \"ricebird\" of that area because of its consumption of ripening rice. By the late 1800's the rice-growing industry had largely shifted to the coastal prairies of Louisiana and Texas, which are bordered by some 5 million acres of marshland-breeding habitat for the redwinged blackbird (<i>Agelaius phoeniceus</i>) and the boat-tailed grackle (<i>Cassidix mexicanus</i>). By 1900, rice was being grown on the Grand Prairie of eastern Arkansas, which bestrides the largest blackbird flyway in the country. In recent decades, rice culture has spread to other sections of Arkansas and thence to contiguous areas in Louisiana, Mississippi, Tennesee, and Missouri. In effect, then, man has taken the rice to the blackbirds.</p>","language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, DC","usgsCitation":"Meanley, B., 1971, Blackbirds and the southern rice crop: Resource Publication 100, iv, 64 p.","productDescription":"iv, 64 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":165017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/rp100.jpg"},{"id":317894,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/rp/100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608277","contributors":{"authors":[{"text":"Meanley, Brooke","contributorId":79938,"corporation":false,"usgs":true,"family":"Meanley","given":"Brooke","email":"","affiliations":[],"preferred":false,"id":217651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6517,"text":"pp655D - 1971 - Geology and ground-water system in the Gila River Phreatophyte Project area, Graham County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp655D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"655","chapter":"D","title":"Geology and ground-water system in the Gila River Phreatophyte Project area, Graham County, Arizona","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp655D","usgsCitation":"Weist, W.G., 1971, Geology and ground-water system in the Gila River Phreatophyte Project area, Graham County, Arizona: U.S. Geological Survey Professional Paper 655, 21 p., https://doi.org/10.3133/pp655D.","productDescription":"21 p.","costCenters":[],"links":[{"id":118024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0655d/report-thumb.jpg"},{"id":33990,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0655d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33991,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0655d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33992,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0655d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0655d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b466a","contributors":{"authors":[{"text":"Weist, William G. Jr.","contributorId":21527,"corporation":false,"usgs":true,"family":"Weist","given":"William","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":152856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22475,"text":"ofr7141 - 1971 - Determination of channel capacity of the Fresno River downstream from Hidden Damsite, Madera County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:08","indexId":"ofr7141","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":"71-41","title":"Determination of channel capacity of the Fresno River downstream from Hidden Damsite, Madera County, California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr7141","issn":"0094-9140","usgsCitation":"Bertoldi, G., and Blodgett, J.C., 1971, Determination of channel capacity of the Fresno River downstream from Hidden Damsite, Madera County, California: U.S. Geological Survey Open-File Report 71-41, 38 p.  :ill., maps ;27 cm., https://doi.org/10.3133/ofr7141.","productDescription":"38 p.  :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6678d3","contributors":{"authors":[{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":188321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":188322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42874,"text":"ofr71217 - 1971 - Preliminary photointerpretation and damage maps of landslide and other surficial deposits in northeastern San Jose, California","interactions":[],"lastModifiedDate":"2021-09-29T19:21:00.413404","indexId":"ofr71217","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":"71-217","title":"Preliminary photointerpretation and damage maps of landslide and other surficial deposits in northeastern San Jose, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71217","usgsCitation":"Nilsen, T.H., and Brabb, E.E., 1971, Preliminary photointerpretation and damage maps of landslide and other surficial deposits in northeastern San Jose, California: U.S. Geological Survey Open-File Report 71-217, 1 Plate: 34.92 × 23.67 inches, https://doi.org/10.3133/ofr71217.","productDescription":"1 Plate: 34.92 × 23.67 inches","costCenters":[],"links":[{"id":169150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389982,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8617.htm"},{"id":80697,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0217/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","city":"San Jose","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.852,\n              37.375\n            ],\n            [\n              -121.771,\n              37.375\n            ],\n            [\n              -121.771,\n              37.425\n            ],\n            [\n              -121.852,\n              37.425\n            ],\n            [\n              -121.852,\n              37.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd0b","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":227305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42890,"text":"ofr71335 - 1971 - Preliminary geologic map of the Malibu Beach Quadrangle, Los Angeles County, California","interactions":[{"subject":{"id":42890,"text":"ofr71335 - 1971 - Preliminary geologic map of the Malibu Beach Quadrangle, Los Angeles County, California","indexId":"ofr71335","publicationYear":"1971","noYear":false,"title":"Preliminary geologic map of the Malibu Beach Quadrangle, Los Angeles County, California"},"predicate":"SUPERSEDED_BY","object":{"id":64481,"text":"i1146 - 1980 - Geologic map of east-central Santa Monica Mountains, Los Angeles County, California","indexId":"i1146","publicationYear":"1980","noYear":false,"title":"Geologic map of east-central Santa Monica Mountains, Los Angeles County, California"},"id":1}],"supersededBy":{"id":64481,"text":"i1146 - 1980 - Geologic map of east-central Santa Monica Mountains, Los Angeles County, California","indexId":"i1146","publicationYear":"1980","noYear":false,"title":"Geologic map of east-central Santa Monica Mountains, Los Angeles County, California"},"lastModifiedDate":"2022-06-07T17:34:12.462143","indexId":"ofr71335","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":"71-335","title":"Preliminary geologic map of the Malibu Beach Quadrangle, Los Angeles County, California","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71335","collaboration":"Prepared in cooperation with Los Angeles County, California","usgsCitation":"Yerkes, R.F., Campbell, R.H., Blackerby, B., Wentworth, C., Birkeland, P.W., and Schoellhamer, J.E., 1971, Preliminary geologic map of the Malibu Beach Quadrangle, Los Angeles County, California: U.S. Geological Survey Open-File Report 71-335, 2 Plates: 41.52 x 50.44 inches and 42.00 x 49.73 inches, https://doi.org/10.3133/ofr71335.","productDescription":"2 Plates: 41.52 x 50.44 inches and 42.00 x 49.73 inches","costCenters":[],"links":[{"id":401852,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0335/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401851,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0335/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0335/report-thumb.jpg"}],"scale":"12000","country":"United States","state":"California","county":"Los Angeles County","otherGeospatial":"Malibu Beach Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.75,34.0 ], [ -118.75,34.125 ], [ -118.625,34.125 ], [ -118.625,34.0 ], [ -118.75,34.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b0ab","contributors":{"authors":[{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":227337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, R. H.","contributorId":52160,"corporation":false,"usgs":true,"family":"Campbell","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blackerby, B.A.","contributorId":95947,"corporation":false,"usgs":true,"family":"Blackerby","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":227340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wentworth, C. M. 0000-0003-2569-569X","orcid":"https://orcid.org/0000-0003-2569-569X","contributorId":106466,"corporation":false,"usgs":true,"family":"Wentworth","given":"C. M.","affiliations":[],"preferred":false,"id":227342,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Birkeland, P. W.","contributorId":44215,"corporation":false,"usgs":false,"family":"Birkeland","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":227338,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schoellhamer, J. E.","contributorId":106086,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":227341,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":16181,"text":"ofr72371 - 1971 - Preliminary description of Apollo 15 sample environments","interactions":[{"subject":{"id":16181,"text":"ofr72371 - 1971 - Preliminary description of Apollo 15 sample environments","indexId":"ofr72371","publicationYear":"1971","noYear":false,"title":"Preliminary description of Apollo 15 sample environments"},"predicate":"SUPERSEDED_BY","object":{"id":70042577,"text":"70042577 - 1972 - Preliminary geologic investigation of the Apollo 15 landing site","indexId":"70042577","publicationYear":"1972","noYear":false,"title":"Preliminary geologic investigation of the Apollo 15 landing site"},"id":1}],"supersededBy":{"id":70042577,"text":"70042577 - 1972 - Preliminary geologic investigation of the Apollo 15 landing site","indexId":"70042577","publicationYear":"1972","noYear":false,"title":"Preliminary geologic investigation of the Apollo 15 landing site"},"lastModifiedDate":"2013-01-12T17:05:19","indexId":"ofr72371","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":"72-371","title":"Preliminary description of Apollo 15 sample environments","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr72371","usgsCitation":"Swann, G., Hait, M., Schaber, G.G., Freeman, V.L., Ulrich, G., Wolfe, E., Reed, V.S., and Sutton, R.L., 1971, Preliminary description of Apollo 15 sample environments: U.S. Geological Survey Open-File Report 72-371, 2, xii, 219 p. :ill., maps ;27 cm.; 12 sheets, https://doi.org/10.3133/ofr72371.","productDescription":"2, xii, 219 p. :ill., maps ;27 cm.; 12 sheets","costCenters":[],"links":[{"id":148349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c636","contributors":{"authors":[{"text":"Swann, G.A.","contributorId":8859,"corporation":false,"usgs":true,"family":"Swann","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":172375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hait, M. H.","contributorId":59052,"corporation":false,"usgs":true,"family":"Hait","given":"M. H.","affiliations":[],"preferred":false,"id":172380,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schaber, G. G.","contributorId":68300,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":172381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Freeman, V. L.","contributorId":52958,"corporation":false,"usgs":true,"family":"Freeman","given":"V.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":172377,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":172382,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wolfe, E.W.","contributorId":57470,"corporation":false,"usgs":true,"family":"Wolfe","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":172378,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Reed, V. S.","contributorId":58255,"corporation":false,"usgs":true,"family":"Reed","given":"V.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":172379,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sutton, R. L.","contributorId":24364,"corporation":false,"usgs":true,"family":"Sutton","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":172376,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"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":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":24817,"text":"ofr71320 - 1971 - Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr71320","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":"71-320","title":"Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado","docAbstract":"An evaluation of the ground-water supply potential at 30 sites within the Rocky Mountain National Park and Shadow Mountain National Recreation Area was made by the U.S. Geological Survey in 1967 and 1968. The work consisted of a geohydrologic reconnaissance, well inventory, and test drilling. \r\n\r\nThe study sites are underlain by. Precambrian crystalline rocks, Tertiary sediments, or Quaternary glacial and alluvial deposits. The crystalline rocks are generally poor aquifers; however, some wells intercepting fractures may yield as much as 10 gallons per minute from wells 100 to 200 feet deep. Wells drilled in Tertiary sandstones to a depth of 50 to 500 feet may supply 1 to 50 gallons per minute. Wells drilled in unconsolidated glacial and alluvial deposits of Quaternary age yield the largest supplies of ground water in the Rocky Mountain National Park. These deposits commonly can supply 5 to 100 gallons per minute to wells.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division, Colorado District,","doi":"10.3133/ofr71320","issn":"0094-9140","usgsCitation":"Welder, F., 1971, Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado: U.S. Geological Survey Open-File Report 71-320, iii, 16 p. :maps ;27 cm., https://doi.org/10.3133/ofr71320.","productDescription":"iii, 16 p. :maps ;27 cm.","costCenters":[],"links":[{"id":156916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0320/report-thumb.jpg"},{"id":53825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0320/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667186","contributors":{"authors":[{"text":"Welder, F.A.","contributorId":104878,"corporation":false,"usgs":true,"family":"Welder","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":192618,"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 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":110036,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25120.htm","linkFileType":{"id":5,"text":"html"},"description":"25120"},{"id":29441,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1899e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29442,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1899e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899e/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Brooten-Belgrade area","geographicExtents":"{ 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,{"id":925,"text":"wsp1999C - 1971 - Water resources of the upper White River basin, east-central Indiana","interactions":[],"lastModifiedDate":"2022-11-07T16:50:28.66113","indexId":"wsp1999C","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":"1999","chapter":"C","title":"Water resources of the upper White River basin, east-central Indiana","docAbstract":"<p>Ground-water discharge to the streams sustains year-round streamflow in the upper White River basin. This discharge, referred to as ground-water runoff or base runoff, is considered to be an index to the amount of g ound water available for development. A comparison of the variations of groundwater runoff and aquifer distribution in the basin shows that the areas of best development potential are areas where thick sand and gravel aquifers are adjacent to the streams. The average ground-water runoff for these areas is between 400,000 and 500,000 gallons per day per square mile.</p>\n<p>The most permeable aquifers in the basin are the sand and gravel deposits of Quaternary age. These aquifers occur mainly as relatively thick elongate bodies along bedrock valleys and as relatively thin sheetlike deposits at or near land surface. The representative hydraulic conductivity of these aquifers ranges from 1,500 to 2,500 gallons per day per square foot. The limestone and dolomite formations of the bedrock are a source of moderate quar tities of water.</p>\n<p>The long-term average streamflow in the basin is approximately 0.9 cubic feet per second per square mile. The yearly average discharge varies from about one-fourth to twice the long-term average. The 7-day 10-year low flow ranges from about 0.01 to 0.3 cubic feet per second per square mile; the main-stem flow ranges from 0.10 to 0.13 cubic feet per second per square mile.</p>\n<p>The water in the aquifers is predominately a very hard calcium bicarbonate type; it is generally high in iron and contains a moderate amount of dissolved solids. Fresh water (1,000 milligrams per liter dissolved solids or less) is present to depths of approximately 400 feet below land surface. In the tributaries and in the headwaters region of the White River, the composition of surface water is very similar to that of ground water. The quality cf the water in the White River deteriorates in the downstream direction owing to the cumulative effects of sewage effluent.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1999C","usgsCitation":"Cable, L.W., Daniel, J.F., Wolf, R.J., and Tate, C.H., 1971, Water resources of the upper White River basin, east-central Indiana: U.S. Geological Survey Water Supply Paper 1999, Report: v, 38 p.; 4 Plates: 25.00 × 20.50 inches or smaller, https://doi.org/10.3133/wsp1999C.","productDescription":"Report: v, 38 p.; 4 Plates: 25.00 × 20.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":25397,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409195,"rank":7,"type":{"id":36,"text":"NGMDB Index 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,{"id":68326,"text":"ha354 - 1971 - Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula","interactions":[],"lastModifiedDate":"2021-10-21T15:11:14.56474","indexId":"ha354","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":"354","title":"Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, trout fishing) but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resource for recreation and other demands, an analysis of the hydrologic factors related to recreational values is essential.</p><p>The Black River north of Johannesburg in Otsego County has been rated by many fisherman as the number one brook-trout stream in the north-central part of the southern peninsula of Michigan. Headwaters are a few miles north of Johannesburg, and the Black flows northward to join the Cheboygan river a few miles south of Cheyboygan. Only the part of the Black upstream from the impoundment at Tower is included in this report.</p><p>The headwaters of the Black can be reached by driving east and north from Gaylord, or east from Vanderbilt. The lower reaches included in this study can be reached from Tower or Onaway.</p><p>The recreational value of a river depends on the characteristics of streamflow, water-quality, and its bed and banks. The purpose of this atlas is to describe these characteristics and to show how they relate to recreational uses.</p><p>Some of the information presented here was derived from basic records of the U.S. Geological Survey's Water-Resources Division. Additional information was obtained in field reconnaissance surveys in 1966 and 1968. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Conservation Department.</p><p>Sheet 1 of this atlas presents information on streamflow characteristics and water quality. Sheet 2 describes the physical character of the stream channel, bed and banks, and shows how it relates to streamflow, water quality, and recreational use.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha354","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1971, Reconnaissance of the Black River, a cold-water river in the northcentral part of Michigan's southern peninsula: U.S. Geological Survey Hydrologic Atlas 354, 2 Plates: 34.0 x 33.8 inches and 34.5 x 34.0 inches, https://doi.org/10.3133/ha354.","productDescription":"2 Plates: 34.0 x 33.8 inches and 34.5 x 34.0 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha354.JPG"},{"id":390725,"rank":4,"type":{"id":36,"text":"NGMDB Index 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,{"id":68321,"text":"ha353 - 1971 - Reconnaissance of the Sturgeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","interactions":[],"lastModifiedDate":"2021-10-21T15:14:18.467869","indexId":"ha353","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":"353","title":"Reconnaissance of the Sturgeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, trout fishing), but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resources for recreation and other demands, analysis of the hydrologic factors related to recreational values is essential.</p><p>The Sturgeon River north of Gaylord, one of the best brown trout streams in Michigan, is located in the north-central part of the southern peninsula of Michigan with headwaters just north of Gaylord. The Sturgeon flows northward, generally paralleling Interstate Highway 75. The West Branch of the Sturgeon, which joins the main stem at Wolverine, was not included in this study. Exits from Interstate 75 at Gaylord, Vanderbilt, Wolverine, and Indian River provide easy access to the Sturgeon. </p><p>The recreational value of a river depends on the hydrologic characteristics of the river-the streamflow, water quality, and character of bed and banks. The purpose of this atlas is to describe these characteristics and to show how they relate to recreational uses. </p><p>Much of the information presented here was derived from basic records of the U.S. Geological Survey's Water Resources Division. Additional information was obtained in a reconnaissance survey in May and June, 1966. The area of field study is limited to the channel, bed, and banks of the main stem from source to mouth. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Conservation Department. </p><p>Sheet 1 of this atlas presents information on streamflow characteristics and water quality. Sheet 2 describes the physical characteristics of the stream channel and bed and banks, and shows how these physical characteristics relate to streamflow, water quality, and recreational use.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha353","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1971, Reconnaissance of the Sturgeon River, a cold-water river in the northcentral part of Michigan's southern peninsula: U.S. Geological Survey Hydrologic Atlas 353, 2 Plates: 34 x 34 inches and 29 x 38 inches, https://doi.org/10.3133/ha353.","productDescription":"2 Plates: 34 x 34 inches and 29 x 38 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha353.JPG"},{"id":390727,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15730.htm"},{"id":89783,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/353/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89782,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/353/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Michigan","otherGeospatial":"Sturgeon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.66666666666667,45.083333333333336 ], [ -84.66666666666667,45.416666666666664 ], [ -84.58333333333333,45.416666666666664 ], [ -84.58333333333333,45.083333333333336 ], [ -84.66666666666667,45.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afa9","contributors":{"authors":[{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68328,"text":"ha384 - 1971 - Reconnaissance of the Pere Marquette River, a cold water river in the central part of Michigan's Southern Peninsula","interactions":[],"lastModifiedDate":"2022-08-16T18:39:10.219085","indexId":"ha384","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":"384","title":"Reconnaissance of the Pere Marquette River, a cold water river in the central part of Michigan's Southern Peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, and trout fishing) but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resource for recreation and other demands, an analysis of the hydrologic factors related to recreational values is essential.</p><p>The Pere Marquette, an outstanding river for brown and steelhead trout fishing, is also a popular canoe trail. Larger boats, some equipped with motors, are common in the lower reaches where the river is wide and deep. Cabins are abundant on the river near Baldwin but are relatively sparse elsewhere. The broad swampy floodplain that borders most of the river between Walhalla and Ludington apparently offers few favorable cabin sites.</p><p>The Pere Marquette is located in the west-central part of the Southern Peninsula of Michigan, and flows westward from the headwaters near Chase in Lake County to the mouth at Ludington, in Mason County. The river is south of, and roughly parallel to, U.S. Highway 10 from Chase to Ludington. Access to the river is by roads leading south from U.S. 10 at Nirvana, Idlewild, Baldwin, Branch, Walhalla, Scottville, and many intermediate points.</p><p>The recreational value of the river depends on the streamflow characteristics, quality of water, and character of stream channel and bed and banks. The purpose of this report is to describe these characteristics and show how they relate to recreational USGS.</p><p>Most of the information presented here was obtained from a field reconnaissance in July and August, 1966, and from basic records of the U.S. Geological Survey's Water Resources Division. The area of field study is limited to the channel, bed, and banks of the Middle Branch and main stem of the Pere Marquette from source to mouth. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Department of Natural Resources.</p><p>Sheet 1 of this atlas presents information on streamflow and quality of water. Sheet 2 describes the physical characteristics of the stream channel, and bed and banks, and shows how these characteristics relate to streamflow, water quality, and recreational use.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha384","collaboration":"Prepared in cooperation with the Michigan Geological Survey","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1971, Reconnaissance of the Pere Marquette River, a cold water river in the central part of Michigan's Southern Peninsula: U.S. Geological Survey Hydrologic Atlas 384, 2 Plates: 33.5 x 34.0 inches and 53.5 x 36.0 inches, https://doi.org/10.3133/ha384.","productDescription":"2 Plates: 33.5 x 34.0 inches and 53.5 x 36.0 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha384.JPG"},{"id":89792,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/384/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89791,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/384/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405207,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15764.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"Michigan","otherGeospatial":"Pere Marquette River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.433,\n              43.85\n            ],\n            [\n              -85.583,\n              43.85\n            ],\n            [\n              -85.583,\n              43.95\n            ],\n            [\n              -86.433,\n              43.95\n            ],\n            [\n              -86.433,\n              43.85\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afc4","contributors":{"authors":[{"text":"Hendrickson, G. 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