{"pageNumber":"5619","pageRowStart":"140450","pageSize":"25","recordCount":165626,"records":[{"id":68063,"text":"ha477 - 1973 - Selected hydrologic data in the upper Colorado River basin","interactions":[],"lastModifiedDate":"2017-02-21T10:37:02","indexId":"ha477","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"477","title":"Selected hydrologic data in the upper Colorado River basin","docAbstract":"

Most of the information in this atlas pertains to the ground-water resources of the basin. The surface-water resources, climate, and geohydrologic framework have been described in considerable detail by Iorns and others (1964, 1965).

The maps in this atlas are highly generalized, and are intended to provide the reader with only a general understanding of the geology, ground-water conditions, and chemical quality of the water in the basin as a whole. In most instances, the availability, depth to, and chemical quality of ground water at a given well site can be determined only by special investigations. Only previously collected data were used to compile the maps in this atlas. More detailed information for specific parts of the basin can be found in the reports and maps in the list of references.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha477","collaboration":"Prepared in cooperation with the states of Arizona, Colorado, New Mexico, Utah, and Wyoming","usgsCitation":"Price, D., and Waddell, K., 1973, Selected hydrologic data in the upper Colorado River basin: U.S. Geological Survey Hydrologic Atlas 477, 2 Sheets: 46.44 x 39.94 inches and 47.25 x 35.53 inches, https://doi.org/10.3133/ha477.","productDescription":"2 Sheets: 46.44 x 39.94 inches and 47.25 x 35.53 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":185539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91817,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/477/plate-2.pdf","text":"Sheet 2","size":"6.24 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Chemical quality of surface and ground water"},{"id":89329,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/477/plate-1.pdf","text":"Sheet 1","size":"9.15 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Physical setting and general availability of ground water"}],"scale":"2500000","country":"United States","state":"Arizona, Colorado, New Mexico, Utah, Wyoming","otherGeospatial":"Colorado River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.5,\n 35.5\n ],\n [\n -105.5,\n 35.5\n ],\n [\n -105.5,\n 43.5\n ],\n [\n -112.5,\n 43.5\n ],\n [\n -112.5,\n 35.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a52","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":277589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":277590,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65217,"text":"i853A - 1973 - Map showing spawning areas of anadromous fish in southern Hood Canal, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:11:02","indexId":"i853A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"853","subseriesTitle":"NONE","chapter":"A","title":"Map showing spawning areas of anadromous fish in southern Hood Canal, Washington","language":"ENGLISH","doi":"10.3133/i853A","usgsCitation":"Findlay, J., 1973, Map showing spawning areas of anadromous fish in southern Hood Canal, Washington: U.S. Geological Survey IMAP 853, 1 map :col. ;45 x 56 cm., https://doi.org/10.3133/i853A.","productDescription":"1 map :col. ;45 x 56 cm.","costCenters":[],"links":[{"id":107008,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9717.htm","linkFileType":{"id":5,"text":"html"},"description":"9717"},{"id":189198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0853a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.25,47.25 ], [ -123.25,47.5 ], [ -122.83333333333333,47.5 ], [ -122.83333333333333,47.25 ], [ -123.25,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644b11","contributors":{"authors":[{"text":"Findlay, J.D.","contributorId":99228,"corporation":false,"usgs":true,"family":"Findlay","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":272861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3110,"text":"wsp2110 - 1973 - Surface water supply of the United States, 1966-70, Part 3, Ohio River basin, v. 4, Ohio River basin below Wabash River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp2110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2110","title":"Surface water supply of the United States, 1966-70, Part 3, Ohio River basin, v. 4, Ohio River basin below Wabash River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Surface water supply of the United States, 1966-70, Part 3, Ohio River basin, v. 4, Ohio River basin below Wabash River: U.S. Geological Survey Water Supply Paper 2110, ix, 806 p. ;23 cm., https://doi.org/10.3133/wsp2110.","productDescription":"ix, 806 p. ;23 cm.","costCenters":[],"links":[{"id":139355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2110/report-thumb.jpg"},{"id":30022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db6920db","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":528087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68234,"text":"ha511 - 1973 - Flood of June 9-10, 1972, at Rapid City, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:37:08","indexId":"ha511","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"511","title":"Flood of June 9-10, 1972, at Rapid City, South Dakota","docAbstract":"

Rapid City, the second largest city in South Dakota, is located at the eastern edge of the Black Hills about 9 miles downstream from Pactola Dam.  It is bisected laterally by Rapid Creek, and longitudinally by the eastern flank of the Black Hills.  Canyon Lake, a samll recreation reservior having a surface area of 35 to 40 acres, is located near the west city limits on Rapid Creek. 

\n

The floods of June 9-10, 1972, covered a relatively small area of the eastern hills, extending from Sturgis on the north to Hermosa on the south and the west to Pactola Dam.  THe area is mountainous with very steep heavily wooded slopes.  Channels are shallow and generally are confined in narrow, winding canyons.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha511","usgsCitation":"Larimer, O.J., 1973, Flood of June 9-10, 1972, at Rapid City, South Dakota: U.S. Geological Survey Hydrologic Atlas 511, 40.50 x 38.00 inches, https://doi.org/10.3133/ha511.","productDescription":"40.50 x 38.00 inches","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":190297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha511.PNG"},{"id":89611,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/511/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"8000","country":"United States","state":"South Dakota","city":"Rapid City","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.33333333333333,44.034166666666664 ], [ -103.33333333333333,44.083333333333336 ], [ -103.11749999999999,44.083333333333336 ], [ -103.11749999999999,44.034166666666664 ], [ -103.33333333333333,44.034166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed50","contributors":{"authors":[{"text":"Larimer, Owen J.","contributorId":78412,"corporation":false,"usgs":true,"family":"Larimer","given":"Owen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277888,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66134,"text":"i767F - 1973 - Areas with abundant sinkholes in Knox County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i767F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"767","subseriesTitle":"NONE","chapter":"F","title":"Areas with abundant sinkholes in Knox County, Tennessee","language":"ENGLISH","doi":"10.3133/i767F","usgsCitation":"Harris, L.D., 1973, Areas with abundant sinkholes in Knox County, Tennessee: U.S. Geological Survey IMAP 767, 1 map :col. ;35 x 45 cm. on sheet 48 x 74 cm., https://doi.org/10.3133/i767F.","productDescription":"1 map :col. ;35 x 45 cm. on sheet 48 x 74 cm.","costCenters":[],"links":[{"id":255625,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0767f/plate-1.pdf","size":"3905","linkFileType":{"id":1,"text":"pdf"}},{"id":255626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0767f/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":255627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0767f/report-thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.25,35.75 ], [ -84.25,36.25 ], [ -83.66666666666667,36.25 ], [ -83.66666666666667,35.75 ], [ -84.25,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672fe0","contributors":{"authors":[{"text":"Harris, Larry D.","contributorId":70758,"corporation":false,"usgs":true,"family":"Harris","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":274030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64958,"text":"i845C - 1973 - Map showing distribution and estimated thickness of alluvial deposits in the Phoenix area, Arizona","interactions":[],"lastModifiedDate":"2025-08-08T19:54:21.995614","indexId":"i845C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"845","subseriesTitle":"NONE","chapter":"C","title":"Map showing distribution and estimated thickness of alluvial deposits in the Phoenix area, Arizona","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i845C","usgsCitation":"1973, Map showing distribution and estimated thickness of alluvial deposits in the Phoenix area, Arizona: U.S. Geological Survey IMAP 845, 1 Plate: 35.49 x 27.66 inches, https://doi.org/10.3133/i845C.","productDescription":"1 Plate: 35.49 x 27.66 inches","costCenters":[],"links":[{"id":493900,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9690.htm","linkFileType":{"id":5,"text":"html"}},{"id":254831,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0845c/report-thumb.jpg"},{"id":254830,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0845c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":254829,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0845c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","city":"Phoenix","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113,\n 33.921\n ],\n [\n -113,\n 32.75\n ],\n [\n -110.906,\n 32.75\n ],\n [\n -110.906,\n 33.921\n ],\n [\n -113,\n 33.921\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660e29","contributors":{"compilers":[{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":945439,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":4219,"text":"cir687 - 1973 - Report on water injectivity test, lease OCS-P 0241, Well No. B-49-1, Dos Cuadras Field, Santa Barbara Channel, off California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:47","indexId":"cir687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"687","title":"Report on water injectivity test, lease OCS-P 0241, Well No. B-49-1, Dos Cuadras Field, Santa Barbara Channel, off California","language":"ENGLISH","publisher":"U.S. Geological Survey, National Center],","doi":"10.3133/cir687","usgsCitation":"Adams, M.V., 1973, Report on water injectivity test, lease OCS-P 0241, Well No. B-49-1, Dos Cuadras Field, Santa Barbara Channel, off California: U.S. Geological Survey Circular 687, v, 28 p. :illus. ;26 cm., https://doi.org/10.3133/cir687.","productDescription":"v, 28 p. :illus. ;26 cm.","costCenters":[],"links":[{"id":118234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1973/0687/report-thumb.jpg"},{"id":31333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1973/0687/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f5db","contributors":{"authors":[{"text":"Adams, Maurice V.","contributorId":99957,"corporation":false,"usgs":true,"family":"Adams","given":"Maurice","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":148432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62501,"text":"gq1098 - 1973 - Geologic map of the Pennington Gap quadrangle, Lee County, Virginia, and Harlan County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq1098","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1098","title":"Geologic map of the Pennington Gap quadrangle, Lee County, Virginia, and Harlan County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1098","usgsCitation":"Miller, R.L., and Roen, J.B., 1973, Geologic map of the Pennington Gap quadrangle, Lee County, Virginia, and Harlan County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1098, 1 map., https://doi.org/10.3133/gq1098.","productDescription":"1 map.","costCenters":[],"links":[{"id":107538,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10642.htm","linkFileType":{"id":5,"text":"html"},"description":"10642"},{"id":248664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1098/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":253891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1098/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.11749999999999,36.75 ], [ -83.11749999999999,36.8675 ], [ -83,36.8675 ], [ -83,36.75 ], [ -83.11749999999999,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a6a","contributors":{"authors":[{"text":"Miller, Ralph L.","contributorId":74737,"corporation":false,"usgs":true,"family":"Miller","given":"Ralph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":267465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roen, John B.","contributorId":14425,"corporation":false,"usgs":true,"family":"Roen","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":267464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5836,"text":"pp775 - 1973 - Petrography of some granitic bodies in the northern White Mountains, California-Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:54","indexId":"pp775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"775","title":"Petrography of some granitic bodies in the northern White Mountains, California-Nevada","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp775","usgsCitation":"Crowder, D., and Ross, D., 1973, Petrography of some granitic bodies in the northern White Mountains, California-Nevada: U.S. Geological Survey Professional Paper 775, 28 p., https://doi.org/10.3133/pp775.","productDescription":"28 p.","costCenters":[],"links":[{"id":118145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0775/report-thumb.jpg"},{"id":32583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0775/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4fbd","contributors":{"authors":[{"text":"Crowder, D. F.","contributorId":57045,"corporation":false,"usgs":true,"family":"Crowder","given":"D. F.","affiliations":[],"preferred":false,"id":151654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Donald Clarence","contributorId":49768,"corporation":false,"usgs":true,"family":"Ross","given":"Donald Clarence","affiliations":[],"preferred":false,"id":151653,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62693,"text":"gq1075 - 1973 - Geologic map of the Laurel quadrangle, Ohio-Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq1075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1075","title":"Geologic map of the Laurel quadrangle, Ohio-Kentucky","language":"ENGLISH","doi":"10.3133/gq1075","usgsCitation":"Kohut, J.J., Weiss, M.P., and Luft, S.J., 1973, Geologic map of the Laurel quadrangle, Ohio-Kentucky: U.S. Geological Survey Geologic Quadrangle 1075, 1 map., https://doi.org/10.3133/gq1075.","productDescription":"1 map.","costCenters":[],"links":[{"id":107517,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10620.htm","linkFileType":{"id":5,"text":"html"},"description":"10620"},{"id":248849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1075/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":254242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1075/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.25,38.8675 ], [ -84.25,39 ], [ -84.11749999999999,39 ], [ -84.11749999999999,38.8675 ], [ -84.25,38.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696fbb","contributors":{"authors":[{"text":"Kohut, Joseph James","contributorId":91173,"corporation":false,"usgs":true,"family":"Kohut","given":"Joseph","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":267736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, Malcolm P.","contributorId":98378,"corporation":false,"usgs":true,"family":"Weiss","given":"Malcolm","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":267737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luft, Stanley J.","contributorId":30634,"corporation":false,"usgs":true,"family":"Luft","given":"Stanley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6115,"text":"pp824 - 1973 - Devonian carrier shells (Euomphalidae) from North America and Germany","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp824","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"824","title":"Devonian carrier shells (Euomphalidae) from North America and Germany","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp824","usgsCitation":"Linsley, R.M., and Yochelson, E.L., 1973, Devonian carrier shells (Euomphalidae) from North America and Germany: U.S. Geological Survey Professional Paper 824, 26 p., https://doi.org/10.3133/pp824.","productDescription":"26 p.","costCenters":[],"links":[{"id":117282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0824/report-thumb.jpg"},{"id":33172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0824/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd13","contributors":{"authors":[{"text":"Linsley, Robert M.","contributorId":49785,"corporation":false,"usgs":true,"family":"Linsley","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yochelson, Ellis Leon","contributorId":66678,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"Leon","affiliations":[],"preferred":false,"id":152145,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62608,"text":"gq1080 - 1973 - Geologic map of the Walton quadrangle, north-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1080","title":"Geologic map of the Walton quadrangle, north-central Kentucky","language":"ENGLISH","doi":"10.3133/gq1080","usgsCitation":"Luft, S.J., 1973, Geologic map of the Walton quadrangle, north-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1080, 1 map., https://doi.org/10.3133/gq1080.","productDescription":"1 map.","costCenters":[],"links":[{"id":107521,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10624.htm","linkFileType":{"id":5,"text":"html"},"description":"10624"},{"id":248767,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1080/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":254077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1080/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.61749999999999,38.75 ], [ -84.61749999999999,38.8675 ], [ -84.5,38.8675 ], [ -84.5,38.75 ], [ -84.61749999999999,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0d7","contributors":{"authors":[{"text":"Luft, Stanley J.","contributorId":30634,"corporation":false,"usgs":true,"family":"Luft","given":"Stanley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70112314,"text":"70112314 - 1973 - Concealed structures in Arctic Alaska identified on ERTS-1 imagery","interactions":[],"lastModifiedDate":"2018-02-19T17:25:53","indexId":"70112314","displayToPublicDate":"1990-06-12T14:30:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2941,"text":"Oil & Gas Journal","printIssn":"0030-1388","active":true,"publicationSubtype":{"id":10}},"title":"Concealed structures in Arctic Alaska identified on ERTS-1 imagery","docAbstract":"No abstract available.","language":"English","publisher":"PennWell Corporation","publisherLocation":"Tulsa, OK","usgsCitation":"Fischer, W., and Lathram, E.H., 1973, Concealed structures in Arctic Alaska identified on ERTS-1 imagery: Oil & Gas Journal, v. 71, no. 22, p. 97-102.","productDescription":"6 p.","startPage":"97","endPage":"102","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","volume":"71","issue":"22","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbece4b0e83db6d08ee1","contributors":{"authors":[{"text":"Fischer, William A.","contributorId":47787,"corporation":false,"usgs":true,"family":"Fischer","given":"William A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":494660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lathram, Ernest H.","contributorId":13900,"corporation":false,"usgs":true,"family":"Lathram","given":"Ernest","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":494659,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70120891,"text":"70120891 - 1973 - Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10","interactions":[],"lastModifiedDate":"2019-12-16T14:33:13","indexId":"70120891","displayToPublicDate":"1975-01-01T11:39:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10","docAbstract":"

Leg 10 interstitial water analyses provide new indications of the distribution of rock salt beneath the floor of the Gulf of Mexico, both confirming areas previously indicated to be underlain by salt bodies and extending evidence of salt distribution to seismically featureless areas in the Sigsbee Knolls trend and Isthmian Embayment. The criterion for presence of salt at depth is a consistent increase in interstitial salinity and chlorinity with depth.

Site 86, on the northern margin of the Yucatan Platform, provided no evidence of salt at depth. Thus, our data tend to rule out the suggestion of Antoine and Bryant (1969) that the Sigsbee Knolls salt was squeezed out from beneath the Yucatan Scarp. Cores from Sites 90 and 91, in the central Sigsbee Deep, were not obtained from a great enough depth to yield definite evidence for the presence of buried salt.

Site 86, on the northern margin of the Yucatan Platform, provided no evidence of salt at depth. Thus, our data tend to rule out the suggestion of Antoine and Bryant (1969) that the Sigsbee Knolls salt was squeezed out from beneath the Yucatan Scarp. Cores from Sites 90 and 91, in the central Sigsbee Deep, were not obtained from a great enough depth to yield definite evidence for the presence of buried salt.

","language":"English","publisher":"Integrated Ocean Drilling Program Management International","publisherLocation":"College Station, TX","doi":"10.2973/dsdp.proc.10.121.1973","usgsCitation":"Manheim, F., Sayles, F.L., and Waterman, L.S., 1973, Interstitial water studies on small core samples, Deep Sea Drilling Project: Leg 10: Initial reports of the Deep Sea Drilling Project, v. 10, p. 615-623, https://doi.org/10.2973/dsdp.proc.10.121.1973.","productDescription":"9 p.","startPage":"615","endPage":"623","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488226,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.10.121.1973","text":"Publisher Index Page"},{"id":292419,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Gulf Of Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.86,18.18 ], [ -97.86,30.4 ], [ -81.04,30.4 ], [ -81.04,18.18 ], [ -97.86,18.18 ] ] ] } } ] }","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53f25fe7e4b0333418718930","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":45294,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank T.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":498570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, Fred L.","contributorId":88279,"corporation":false,"usgs":true,"family":"Sayles","given":"Fred","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":498571,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waterman, Lee S.","contributorId":30151,"corporation":false,"usgs":true,"family":"Waterman","given":"Lee","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":498569,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70006470,"text":"70006470 - 1973 - Effects of temperature on embryonic development of lake herring (Coregonus artedii)","interactions":[],"lastModifiedDate":"2014-06-20T11:36:49","indexId":"70006470","displayToPublicDate":"1975-01-01T11:18:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Effects of temperature on embryonic development of lake herring (Coregonus artedii)","docAbstract":"Embryonic development of lake herring (Coregonus artedii) was observed in the laboratory at 13 constant temperatures from 0.0 to 12.1 C and in Pickerel Lake (Washtenaw County, Michigan) at natural temperature regimes. Rate of development during incubation was based on progression of the embryos through 20 identifiable stages. \n\nAn equation was derived to predict development stage at constant temperatures, on the general assumption that development stage (DS) is a function of time (days, D) and temperature (T). The equation should also be useful in interpreting estimates from future regressions that include other environmental variables that affect egg development. \n\nA second regression model, derived primarily for fluctuating temperatures, related development rate for stage j (DRj), expressed as the reciprocal of time, to temperature (x). The generalized equation for a development stage is: DRj = abx cx2 dx3. \n\nIn general, time required for embryos to reach each stage of development in Pickerel Lake agreed closely with the time predicted from this equation, derived from our laboratory observations. Hatching time was predicted within 1 day in 1969 and within 2 days in 1970. \n\nWe used the equations derived with the second model to predict the effect of the superimposition of temperature increases of 1 and 2 C on the measured temperatures in Pickerel Lake. Conceivably, hatching dates could be affected sufficiently to jeopardize the first feeding of lake herring through loss of harmony between hatching date and seasonal food availability.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the Fisheries Research Board of Canada","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"NRC Research Press","doi":"10.1139/f73-135","usgsCitation":"Colby, P.J., and Brooke, L., 1973, Effects of temperature on embryonic development of lake herring (Coregonus artedii): Journal of the Fisheries Research Board of Canada, v. 30, no. 6, p. 799-810, https://doi.org/10.1139/f73-135.","productDescription":"12 p.","startPage":"799","endPage":"810","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":288970,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288968,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1139/f73-135"}],"country":"United States","state":"Michigan","county":"Washtenaw County","otherGeospatial":"Pickerel Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.789812,45.386668 ], [ -84.789812,45.408435 ], [ -84.743084,45.408435 ], [ -84.743084,45.386668 ], [ -84.789812,45.386668 ] ] ] } } ] }","volume":"30","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae76a1e4b0abf75cf2bfc6","contributors":{"authors":[{"text":"Colby, Peter J.","contributorId":89831,"corporation":false,"usgs":true,"family":"Colby","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":354575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooke, L.T.","contributorId":60589,"corporation":false,"usgs":true,"family":"Brooke","given":"L.T.","email":"","affiliations":[],"preferred":false,"id":354574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70106983,"text":"70106983 - 1973 - Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey","interactions":[],"lastModifiedDate":"2015-10-17T19:24:16","indexId":"70106983","displayToPublicDate":"1975-01-01T10:47:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":135,"text":"Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"36","title":"Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey","docAbstract":"

The Wharton Tract is an area of 150 square miles located in the Mullica River basin in southern New Jersey's Pine Barrens region. The tract is a relatively flat, low-lying, generally sandy area containing shallowly incised streams. The larger streams are commonly bordered by swamps. The tract was purchased by the State primarily as a water-supply preserve, but also for conservation and recreational purposes.

\n

Mean streamflow at three continuous record gaging stations in the Wharton Tract is: Mullica River near Batsto (46.1-square mile drainage area), 6 mgd (million gallons per day); Batsto River at Batsto (70.5-square mile drainage area), 81 mgd; Oswego River at Harrisville (64.0-square mile drainage area), 55 mgd. Thus mean discharge from this 180.6-sq mi (square mile) area is 202 mgd or 1.12 mgd per sq mi.

\n

Principal aquifers in the Wharton Tract and Mullic River basin are in the Kirkwood Formation of middle Miocene age, Cohansey Sand of Miocene(?) and Pliocene(?) age, and in overlying hydraulically connected deposits of Quaternary age.

\n

The Kirkwood Formation is composed of sand, silt, and clay. Diverse lithologies represent deposition in different environments such as nearshore marine, barrier bar, lagoonal, estuarine, and tidal marsh. Hydraulic characteristics of the Kirkwood in the Mullica River basin are virtually unknown. Most Kirkwood aquifers in the basin are believed to be hydraulically connected with the overlying Cohansey Sand.

\n

The Cohansey Sand is dominantly a quartz sand containing minor amounts of pebbly sand, silty sand, and interbedded clay. Almost all of the Wharton Tract and most of the Mullica River basin lie within the sandier area of the Cohansey, which contains approximately 75 percent sand beds and 25 percent silt and clay beds. Data from test drilling show that the upper 100 feet of sediments in the Wharton Tract contain about 93 percent sand beds, 3.5 percent clay beds, and 3.5 percent silt beds. The Cohansey in the Tract ranges in thickness from less than 50 feet to about 180 feet; the average thickness is about 125 feet.

\n

The Cohansey Sand is believed to be, in overall aspect, a deltaic deposit. It contains materials that were deposited locally in nearshore-marine, fluvial, estuarine, lagoonal, and beach environments.

\n

The hydraulic conductivity of Cohansey aquifer material ranges from about 90 to 250 feet per day (660 to 1,885 gallons per day per square foot) in southern New Jersey. One aquifer test in the Wharton Tract gives an average value of 130 feet per day (1,000 gallons per day per square foot). The transmissivity of the Cohansey Sand aquifer through most of the Wharton Tract is typically between 10,000 and 20,000 square feet per day (75,000 and 150,000 gallons per day per foot).

\n

Deposits of Quaternary age form a discontinuous veneer lying unconformably above the Cohansey Sand. The most important hydrologic function of most of these deposits is to absorb precipitation and transmit the water to the underlying Cohansey Sand. Thicker deposits of estuarine sand and clay of the Cape May Formation fill a channel in the underlying Cohansey Sand along the lower reaches of the Mullica River. This channel deposit is 85 feet thick near Batsto.

\n

Ground water and surface water in the Mullica River basin are low in dissolved solids, generally less than 50 mg/1 (milligrams per liter). Iron concentrations are generally high, up to 49,000 micrograms per liter (49 mg/1) in ground water and up to 7,100 micrograms per liter (7.1 mg/1) in the streams. The water is acidic as indicated by typical pH values of from 4.5 to 6.5. Color of the surface water is commonly high, ranging from 3 - 150 platinum-cobalt units. After appropriate treatment these waters are acceptable for most uses.

\n

The Wharton Tract is well situated to support the growing water needs of nearby New Jersey communities. Maximum development of water can be achieved by conjunctive use of ground and surface water. During most of the year, some water would be withdrawn either directly from streams or from adjacent wells. During periods of low flow during summer or fall water would be pumped from wells farther from the stream~. From analysis of flow-duration curves it is estimated that 70 mgd of water could be developed with minimal effect upon low flows in the half of the tract above the gaging stations on the Mullica and Batsto Rivers. The quantity available in the entire tract is greater, possibly in the order of 150 mgd. With augmentation of streamflow by pumping from ground water, it is likely that considerably more water could be safely used on a perennial basis.

\n

A possibility exists for multiple use of the water resources of the Mullica River through construction of an inexpensive tide barrier at the Garden State Parkway. This would create a fresh water lake in a State forest, park, and recreational area, which would also provide a flexible and economical water supply for much of the Atlantic coastal resort development.

","language":"English","publisher":"State of New Jersey Department of Environmental Protection, Division of Water Resources","collaboration":"Prepared in cooperation with United States Department of the Interior Geological Survey","usgsCitation":"Rhodehamel, E.C., 1973, Geology and water resources of the Wharton Tract and the Mullica River basin in southern New Jersey: Special Report 36, 58 p.","productDescription":"58 p.","numberOfPages":"65","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":287918,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":287917,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106983/report.pdf"}],"country":"United States","state":"New Jersey","otherGeospatial":"Mullica River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.7768,38.8517 ], [ -75.7768,40.7423 ], [ -73.8448,40.7423 ], [ -73.8448,38.8517 ], [ -75.7768,38.8517 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b27f4e4b0929ba496ab78","contributors":{"authors":[{"text":"Rhodehamel, Edward C.","contributorId":38135,"corporation":false,"usgs":true,"family":"Rhodehamel","given":"Edward","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":493827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221235,"text":"5221235 - 1973 - Thickness of the American woodcock eggshell, 1971","interactions":[],"lastModifiedDate":"2020-03-24T10:56:14","indexId":"5221235","displayToPublicDate":"1974-06-16T12:17:55","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Thickness of the American woodcock eggshell, 1971","docAbstract":"Eggs or empty shells of the American woodcockwere collected from 10 states in 1971and shell thickness (mean of clutch means) was compared with that of eggs collected from 16 states during the years 1859-1939. The 1971 shells (n = 91) from hatched eggs or those containing fully developed embryos were about i0 percent thinner (P<0.001) than both unembryonated shells (n = 26) from the same year and the 1859-1939 shells (n = 169) from essentially unembryonated eggs. The difference is attributed to the transfer of calcium from the shells to the embryos and not to environmental pollutants.","language":"English","publisher":"Springer","doi":"10.1007/BF01684784","usgsCitation":"Kreitzer, J., 1973, Thickness of the American woodcock eggshell, 1971: Bulletin of Environmental Contamination and Toxicology, v. 9, no. 5, p. 281-286, https://doi.org/10.1007/BF01684784.","productDescription":"6 p.","startPage":"281","endPage":"286","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Georgia, Indiana, Iowa, Maine, Maryland, Massachusetts, Michigan, Minnesota, New Jersey, New York, North Carolina, Ohio, Pennsylvania, Texas, Vermont, Virginia, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.873779296875,\n 44.87144275016589\n ],\n [\n -67.763671875,\n 45.81348649679973\n ],\n [\n -67.8515625,\n 47.14489748555398\n ],\n [\n -69.2138671875,\n 47.45780853075031\n ],\n [\n -71.092529296875,\n 45.32897866218559\n ],\n [\n -70.960693359375,\n 43.37311218382002\n ],\n [\n -70.82061767578125,\n 43.22719386727831\n ],\n [\n -70.718994140625,\n 43.02673743559375\n ],\n [\n -70.4608154296875,\n 43.34914966389313\n ],\n [\n -70.20263671875,\n 43.56646172588961\n ],\n [\n -68.8458251953125,\n 43.79488907226601\n ],\n [\n -67.3736572265625,\n 44.48670891691767\n ],\n [\n -66.873779296875,\n 44.87144275016589\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.48779296875,\n 42.72683914955442\n ],\n [\n -72.3834228515625,\n 43.5326204268101\n ],\n [\n -72.037353515625,\n 44.10336537791152\n ],\n [\n -72.06207275390625,\n 44.28257044667387\n ],\n [\n -71.62811279296875,\n 44.46123053905879\n ],\n [\n -71.53472900390625,\n 44.61393394730626\n ],\n [\n -71.6033935546875,\n 44.73697895420882\n ],\n [\n -71.4935302734375,\n 44.904523389609324\n ],\n [\n -71.5155029296875,\n 45.02500920723146\n ],\n [\n -74.88006591796874,\n 45.01530198999212\n ],\n [\n -76.44561767578125,\n 44.1151978766043\n ],\n [\n -76.46759033203125,\n 44.06390660801779\n ],\n [\n -76.81640625,\n 43.61221676817573\n ],\n [\n -79.07958984375,\n 43.29320031385282\n ],\n [\n -78.92578124999999,\n 42.83569550641452\n ],\n [\n -79.727783203125,\n 42.33418438593939\n ],\n [\n -80.39794921875,\n 42.04113400940807\n ],\n [\n -80.518798828125,\n 41.983994270935625\n ],\n [\n -82.68310546875,\n 41.6154423246811\n ],\n [\n -83.177490234375,\n 42.01665183556825\n ],\n [\n -83.08959960937499,\n 42.342305278572816\n ],\n [\n -82.4853515625,\n 42.65012181368022\n ],\n [\n -82.30957031249999,\n 43.24520272203356\n ],\n [\n -82.716064453125,\n 44.12702800650004\n ],\n [\n -83.21044921875,\n 45.390735154248894\n ],\n [\n -83.583984375,\n 45.82114340079471\n ],\n [\n -83.616943359375,\n 46.08847179577592\n ],\n [\n -83.9794921875,\n 46.06560846138691\n ],\n [\n -84.17724609375,\n 46.543749602738565\n ],\n [\n -84.627685546875,\n 46.5739667965278\n ],\n [\n -84.990234375,\n 46.79253827035982\n ],\n [\n -86.81396484375,\n 46.581518465658014\n ],\n [\n -87.29736328125,\n 46.66451741754235\n ],\n [\n -88.275146484375,\n 47.03269459852135\n ],\n [\n -87.506103515625,\n 47.45780853075031\n ],\n [\n -88.41796875,\n 47.53203824675999\n ],\n [\n -90.494384765625,\n 46.717268685073954\n ],\n [\n -90.32958984375,\n 47.15984001304432\n ],\n [\n -91.966552734375,\n 46.84516443029276\n ],\n [\n -89.483642578125,\n 48.004625021133904\n ],\n [\n -90.736083984375,\n 48.158757304569235\n ],\n [\n -90.867919921875,\n 48.268569112964336\n ],\n [\n -91.5380859375,\n 48.07807894349862\n ],\n [\n -92.054443359375,\n 48.356249029540734\n ],\n [\n -93.2080078125,\n 48.65468584817256\n ],\n [\n -94.658203125,\n 48.76343113791796\n ],\n [\n -94.8779296875,\n 49.34659884833293\n ],\n [\n -95.11962890625,\n 49.38237278700955\n ],\n [\n -95.185546875,\n 48.99463598353405\n ],\n [\n -97.261962890625,\n 48.99463598353405\n ],\n [\n -96.6357421875,\n 46.118941506107056\n ],\n [\n -96.61376953125,\n 45.75985868785574\n ],\n [\n -96.85546875,\n 45.62940492064501\n ],\n [\n -96.50390625,\n 45.32897866218559\n ],\n [\n -96.43798828125,\n 43.52465500687185\n ],\n [\n -96.61376953125,\n 42.70665956351041\n ],\n [\n -95.97656249999999,\n 41.31082388091818\n ],\n [\n -95.7568359375,\n 40.57224011776902\n ],\n [\n -91.68090820312499,\n 40.622291783092706\n ],\n [\n -91.417236328125,\n 40.34654412118006\n ],\n [\n -91.065673828125,\n 40.72228267283148\n ],\n [\n -91.0546875,\n 41.18692242290296\n ],\n [\n -90.3515625,\n 41.63186741069748\n ],\n [\n -90.142822265625,\n 41.9921602333763\n ],\n [\n -90.703125,\n 42.52879629320373\n ],\n [\n -87.802734375,\n 42.52879629320373\n ],\n [\n -87.484130859375,\n 41.68932225997044\n ],\n [\n -87.60498046875,\n 39.12153746241925\n ],\n [\n -87.5115966796875,\n 38.7519413494709\n ],\n [\n -87.74711608886719,\n 38.4632670276956\n ],\n [\n -87.74711608886719,\n 38.40840605494758\n ],\n [\n -88.099365234375,\n 37.900865092570065\n ],\n [\n -87.506103515625,\n 37.90953361677018\n ],\n [\n -86.484375,\n 38.03078569382294\n ],\n [\n -86.055908203125,\n 38.229550455326134\n ],\n [\n -85.528564453125,\n 38.51378825951165\n ],\n [\n -85.39672851562499,\n 38.71980474264237\n ],\n [\n -84.91333007812499,\n 38.77978137804918\n ],\n [\n -84.473876953125,\n 39.027718840211605\n ],\n [\n -83.9794921875,\n 38.71123253895224\n ],\n [\n -83.03466796874999,\n 38.61687046392973\n ],\n [\n -82.94677734375,\n 38.71980474264237\n ],\n [\n -82.46337890625,\n 38.44498466889473\n ],\n [\n -82.001953125,\n 39.0533181067413\n ],\n [\n -81.727294921875,\n 38.976492485539396\n ],\n [\n -81.5625,\n 39.308800296002914\n ],\n [\n -80.79345703125,\n 39.825413103424786\n ],\n [\n -80.518798828125,\n 39.80009595634838\n ],\n [\n -80.52429199218749,\n 39.7240885773337\n ],\n [\n -79.4476318359375,\n 39.73253798438173\n ],\n [\n -79.486083984375,\n 39.1854331703021\n ],\n [\n -79.07135009765625,\n 39.46800484919317\n ],\n [\n -78.9697265625,\n 39.45104033807322\n ],\n [\n -78.7884521484375,\n 39.631076770083666\n ],\n [\n -78.64562988281249,\n 39.51887357127223\n ],\n [\n -78.519287109375,\n 39.535821539950376\n ],\n [\n -77.87109375,\n 39.198205348894795\n ],\n [\n -77.75299072265625,\n 39.317300373271024\n ],\n [\n -77.4700927734375,\n 39.251397769004924\n ],\n [\n -77.51678466796875,\n 39.11301365149975\n ],\n [\n -77.2833251953125,\n 39.036252959636606\n ],\n [\n -77.14324951171875,\n 38.953001345359894\n ],\n [\n -77.1240234375,\n 38.935911987561624\n ],\n [\n -77.03887939453125,\n 38.99463939467871\n ],\n [\n -76.91253662109375,\n 38.89317057287496\n ],\n [\n -77.02377319335936,\n 38.80654039080487\n ],\n [\n -77.04299926757812,\n 38.720876195817276\n ],\n [\n -77.11715698242186,\n 38.687653678261704\n ],\n [\n -77.13775634765625,\n 38.628672522795796\n ],\n [\n -77.27096557617188,\n 38.5256072620712\n ],\n [\n -77.28469848632812,\n 38.38795699631396\n ],\n [\n -77.18170166015625,\n 38.35458032659834\n ],\n [\n -77.03475952148438,\n 38.42884932888259\n ],\n [\n -76.93450927734375,\n 38.25974980039479\n ],\n [\n -76.5692138671875,\n 38.156156969924915\n ],\n [\n -76.31240844726562,\n 37.99724489645483\n ],\n [\n -75.89355468749999,\n 37.882441088286186\n ],\n [\n -75.64910888671875,\n 37.95286091815649\n ],\n [\n -75.62301635742188,\n 37.993998198369574\n ],\n [\n -75.37582397460938,\n 38.01455819225335\n ],\n [\n -75.21652221679688,\n 38.029703972192\n ],\n [\n -75.04074096679688,\n 38.35027253825765\n ],\n [\n -75.05447387695312,\n 38.45681495946778\n ],\n [\n -75.69854736328124,\n 38.46219172306828\n ],\n [\n -75.78781127929688,\n 39.72620102617506\n ],\n [\n -75.772705078125,\n 39.72620102617506\n ],\n [\n -75.70266723632812,\n 39.810645900839134\n ],\n [\n -75.56259155273438,\n 39.842286020743394\n ],\n [\n -75.4266357421875,\n 39.81170080625297\n ],\n [\n -75.41290283203125,\n 39.80009595634838\n ],\n [\n -75.5694580078125,\n 39.62896140981413\n ],\n [\n -75.52413940429688,\n 39.56864645674722\n ],\n [\n -75.55847167968749,\n 39.46906499385169\n ],\n [\n -75.33462524414062,\n 39.31623792008409\n ],\n [\n -75.1300048828125,\n 39.17478791493289\n ],\n [\n -74.92401123046875,\n 39.17478791493289\n ],\n [\n -75.00228881835938,\n 38.93163900447185\n ],\n [\n -74.84848022460936,\n 38.9070643560226\n ],\n [\n -74.48867797851562,\n 39.32155002466662\n ],\n [\n -74.30328369140625,\n 39.420281624085696\n ],\n [\n -74.06570434570312,\n 39.787433886224406\n ],\n [\n -73.95034790039062,\n 40.364334716590214\n ],\n [\n -73.99566650390625,\n 40.483515047963024\n ],\n [\n -73.22250366210938,\n 40.60456943720527\n ],\n [\n -72.34085083007812,\n 40.826280356677124\n ],\n [\n -71.8450927734375,\n 41.062786068733026\n ],\n [\n -71.7901611328125,\n 41.39741506646461\n ],\n [\n -71.8011474609375,\n 42.02889410108475\n ],\n [\n -71.378173828125,\n 42.02889410108475\n ],\n [\n -71.3397216796875,\n 41.832735062152615\n ],\n [\n -71.1474609375,\n 41.70982942509964\n ],\n [\n -71.136474609375,\n 41.52091689636249\n ],\n [\n -70.762939453125,\n 41.22824901518529\n ],\n [\n -69.8785400390625,\n 41.253032440653186\n ],\n [\n -69.8895263671875,\n 42.09007006868398\n ],\n [\n -70.125732421875,\n 42.13896840458089\n ],\n [\n -70.8233642578125,\n 42.85985981506279\n ],\n [\n -71.1419677734375,\n 42.8115217450979\n ],\n [\n -71.290283203125,\n 42.69051116998238\n ],\n [\n -72.48779296875,\n 42.72683914955442\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.92675781249999,\n 37.996162679728116\n ],\n [\n -75.95947265625,\n 37.89219554724437\n ],\n [\n -76.97021484375,\n 38.77121637244273\n ],\n [\n -77.67333984375,\n 39.36827914916014\n ],\n [\n -78.77197265625,\n 39.70718665682654\n ],\n [\n -80.00244140625,\n 37.996162679728116\n ],\n [\n -80.37597656249999,\n 37.47485808497102\n ],\n [\n -81.03515625,\n 37.3002752813443\n ],\n [\n -81.97998046875,\n 37.42252593456307\n ],\n [\n -83.51806640624999,\n 36.56260003738545\n ],\n [\n -81.5625,\n 36.61552763134925\n ],\n [\n -82.55126953124999,\n 35.29943548054545\n ],\n [\n -83.056640625,\n 35.0120020431607\n ],\n [\n -82.0458984375,\n 35.263561862152095\n ],\n [\n -81.03515625,\n 35.04798673426734\n ],\n [\n -80.68359375,\n 34.831841149828655\n ],\n [\n -79.541015625,\n 34.79576153473033\n ],\n [\n -78.486328125,\n 33.8339199536547\n ],\n [\n -77.62939453125,\n 33.8339199536547\n ],\n [\n -76.3330078125,\n 34.75966612466248\n ],\n [\n -75.25634765625,\n 35.35321610123823\n ],\n [\n -75.498046875,\n 37.19533058280065\n ],\n [\n -74.92675781249999,\n 37.996162679728116\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.5615234375,\n 35.0120020431607\n ],\n [\n -85.53955078125,\n 34.45221847282654\n ],\n [\n -85.10009765625,\n 32.47269502206151\n ],\n [\n -85.0341796875,\n 31.353636941500987\n ],\n [\n -84.83642578125,\n 30.751277776257812\n ],\n [\n -82.06787109374999,\n 30.581179257386985\n ],\n [\n -81.9140625,\n 30.80791068136646\n ],\n [\n -81.34277343749999,\n 30.675715404167743\n ],\n [\n -80.83740234375,\n 32.045332838858506\n ],\n [\n -81.82617187499999,\n 33.32134852669881\n ],\n [\n -82.79296874999999,\n 34.542762387234845\n ],\n [\n -83.07861328125,\n 35.0120020431607\n ],\n [\n -85.5615234375,\n 35.0120020431607\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -99.931640625,\n 36.4566360115962\n ],\n [\n -102.65625,\n 36.4566360115962\n ],\n [\n -103.18359375,\n 32.62087018318113\n ],\n [\n -106.435546875,\n 32.47269502206151\n ],\n [\n -106.34765625,\n 31.952162238024975\n ],\n [\n -104.32617187499999,\n 29.611670115197377\n ],\n [\n -103.095703125,\n 29.152161283318915\n ],\n [\n -102.216796875,\n 29.84064389983441\n ],\n [\n -101.6015625,\n 29.6880527498568\n ],\n [\n -99.228515625,\n 26.43122806450644\n ],\n [\n -97.294921875,\n 25.799891182088334\n ],\n [\n -93.779296875,\n 29.84064389983441\n ],\n [\n -93.515625,\n 31.353636941500987\n ],\n [\n -94.130859375,\n 33.578014746143985\n ],\n [\n -99.931640625,\n 34.45221847282654\n ],\n [\n -99.931640625,\n 36.4566360115962\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c56c","contributors":{"authors":[{"text":"Kreitzer, J.F.","contributorId":57170,"corporation":false,"usgs":true,"family":"Kreitzer","given":"J.F.","affiliations":[],"preferred":false,"id":333356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70107931,"text":"70107931 - 1973 - Sediment discharge in the Lake Tahoe basin, California, 1972 water year","interactions":[],"lastModifiedDate":"2014-06-11T09:39:44","indexId":"70107931","displayToPublicDate":"1974-01-01T11:15:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Sediment discharge in the Lake Tahoe basin, California, 1972 water year","docAbstract":"

Streamflow and fluvial-sediment discharge data are being collected at selected streams and highway gutters in the Lake Tahoe basin to determine the extent of erosion from highway cuts and to evaluate the effects of various land treatment practices to reduce erosion.

\n
\n

Precipitation in the Lake Tahoe area during 1972 was 77 percent of normal; consequently, runoff was well below normal. Seventy-six percent of the total annual runoff during the 1972 water year occurred from March through June 1972.

\n
\n

Sediment samples were collected during the year at streamflow gaging stations and at gutter stations at highway cuts to define the range of transport conditions. The major part (87 percent) of the annual suspended-sediment discharge during the 1972 water year occurred during the snowmelt runoff period, March through June.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/70107931","collaboration":"Prepared in cooperation with the California Department of Transportation Division of Highways","usgsCitation":"Kroll, C.G., 1973, Sediment discharge in the Lake Tahoe basin, California, 1972 water year, iv, 33 p., https://doi.org/10.3133/70107931.","productDescription":"iv, 33 p.","numberOfPages":"38","temporalStart":"1971-10-01","temporalEnd":"1972-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":288274,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70107931/report-thumb.jpg"},{"id":288273,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70107931/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Lake Tahoe","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.2862,38.6007 ], [ -120.2862,39.3786 ], [ -119.6624,39.3786 ], [ -119.6624,38.6007 ], [ -120.2862,38.6007 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537dcb14e4b05ed6215c08b8","contributors":{"authors":[{"text":"Kroll, Carl G.","contributorId":72389,"corporation":false,"usgs":true,"family":"Kroll","given":"Carl","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":493937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038039,"text":"70038039 - 1973 - Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts","interactions":[],"lastModifiedDate":"2015-02-09T09:17:45","indexId":"70038039","displayToPublicDate":"1974-01-01T10:48:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":367,"text":"Massachusetts Hydrologic - Data Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"14","title":"Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts","docAbstract":"

The Neponset, Weymouth Fore, and Weymouth Back River basins occupy an area of 183 square miles in eastern Massachusetts south of Boston and Braintree, Brockton, Canton, Dedham, Dover, Foxborough, Hingham, Holbrook, Medfield, Milton, Norwood, Quincy, Randolph, Rockland, Sharon, Stoughton, Walpole, Westwood, and Weymouth.

\n

Hydrologic data presented in this report were collected during an investigation of the water resources in the areas of these basins that are upstream from tide effect or heavy urbanization. This investigation was conducted by the U.S. Geological Survey in cooperation with the Massachusetts Water Resources Commission. The data are released in order to make available to the public basic hydrologic and related information that will facilitate the planning of water-resources development and will complement an interpretive report, \"Hydrology and water resources of the Neoponset and Weymouth River basins, Massachusetts\" (HA-484).

\n

The well and boring data contained herein were selected from a larger group of data in order to minimize redundancy of information for intensely drilled areas. All of the data are on filed and available for inspection at the office of the U.S. Geological Survey, Water Resources Division, Boston, Massachusetts.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, Massachusetts","doi":"10.3133/70038039","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Brackley, R., Fleck, W.B., and Willey, R.E., 1973, Hydrologic Data of the Neponset and Weymouth River Basins, Massachusetts: Massachusetts Hydrologic - Data Report 14, Report: 51 p.; Plate: 47.12 x 35.64 inches, https://doi.org/10.3133/70038039.","productDescription":"Report: 51 p.; Plate: 47.12 x 35.64 inches","numberOfPages":"56","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":264632,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038039/plate-1.pdf","size":"16.2 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":264633,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038039/report.pdf","size":"4.3 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":264634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70038039/report-thumb.jpg"}],"scale":"31680","country":"United States","state":"Massachusetts","otherGeospatial":"Neponset River, Weymouth River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.29852294921875,\n 42.06968462804663\n ],\n [\n -71.29852294921875,\n 42.35245491952619\n ],\n [\n -70.8837890625,\n 42.35245491952619\n ],\n [\n -70.8837890625,\n 42.06968462804663\n ],\n [\n -71.29852294921875,\n 42.06968462804663\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3510e4b0c8380cd5fc27","contributors":{"authors":[{"text":"Brackley, R. A.","contributorId":16851,"corporation":false,"usgs":true,"family":"Brackley","given":"R. A.","affiliations":[],"preferred":false,"id":463316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleck, William B.","contributorId":17587,"corporation":false,"usgs":true,"family":"Fleck","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":463317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willey, Richard E.","contributorId":30972,"corporation":false,"usgs":true,"family":"Willey","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463318,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70174291,"text":"70174291 - 1973 - The benthic fauna of the Northern Bering Sea","interactions":[],"lastModifiedDate":"2016-07-08T09:44:40","indexId":"70174291","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"The benthic fauna of the Northern Bering Sea","docAbstract":"

The shelled benthic fauna of the northern Bering Sea has been extensively sampled and the taxonomy, distribution and functional role of 105 species of mollusks, two species of barnacles, two species of echinoids and one species of brachiopod havet4pen examined: The major benthic communities were evaluated by cluster analysis. They are:

\n
    \n
  1. the Balanus rostratus alaskensis community which inhabits cobble or gravel substrates;
    2. \n
  2. the Tellina lutea alternidentata community which is limited to areas of clean sand;
    3. \n
  3. the Clinocardium ciliatum community which is found on silty-sand substrates; and
    4. \n
  4. the Macoma balthica community which inhabits the brackish coastal lagoons.
    5. \n
\n

These associations were compared with the classic boreal benthic communities of Peterson & Thorson. Although the Bering Sea fauna is compositionally similar to the Scandinavian, the species associations differ markedly. These differences are believed to be due to substrate differences. The Bering Sea sediments are more poorly sorted and patchily distributed than those of Scandinavian waters.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70174291","usgsCitation":"Rowland, R.W., 1973, The benthic fauna of the Northern Bering Sea: Open-File Report, vi, 234 p., https://doi.org/10.3133/70174291.","productDescription":"vi, 234 p.","numberOfPages":"236","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":324811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70174291.PNG"},{"id":324883,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"577f7d33e4b0ef4d2f45facf","contributors":{"authors":[{"text":"Rowland, Robert W.","contributorId":42200,"corporation":false,"usgs":true,"family":"Rowland","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":641712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207474,"text":"70207474 - 1973 - Interstitial water studies on small core samples, leg 19","interactions":[],"lastModifiedDate":"2019-12-19T18:10:35","indexId":"70207474","displayToPublicDate":"1973-12-31T18:05:09","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg 19","docAbstract":"

The sediments cored on Leg 19 consist primarily of diatomaceous oozes with variable proportions of volcanic material and terrigenous clays and silts. With a few exceptions, deposition rates are high at these sites, usually exceeding 5cm/103y. The interstitial solutions sampled exhibit compositional changes which previously have been found to characterize rapidly deposited terrigenous sediments. Some of the largest changes in Na+, K+, Mg2+, Cl-, and HCO3 yet found in DSDP samples occur in the pore waters studied from this leg (see Table 1).

","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.19.133.1973","usgsCitation":"Sayles, F., Waterman, L., and Manheim, F.T., 1973, Interstitial water studies on small core samples, leg 19: Initial reports of the Deep Sea Drilling Project, v. 19, p. 871-874, https://doi.org/10.2973/dsdp.proc.19.133.1973.","productDescription":"4 p.","startPage":"871","endPage":"874","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488853,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.19.133.1973","text":"Publisher Index Page"},{"id":370533,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778187,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207473,"text":"70207473 - 1973 - Interstitial water studies on small core samples, legs 16, 17, and 18","interactions":[],"lastModifiedDate":"2019-12-19T18:02:56","indexId":"70207473","displayToPublicDate":"1973-12-31T17:52:08","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, legs 16, 17, and 18","docAbstract":"

Legs 16, 17, and 18 encountered three groups of sediment types: rapidly deposited biogenic deposits, showing marked changes in interstitial calcium, magnesium, and strontium; slowly deposited biogenic deposits, showing little variability in pore fluids other than elevated silica concentrations; and terrigenous deposits. The latter showed the usual loss of sulfate and combination of diagenetic reactions culminating in loss of Na+ , K+ , Mg++, with variable changes in Ca++. Very high barium concentrations (to 59 mg/kg) occurred at Site 178 (Leg 18).

","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.18.app2.1973","usgsCitation":"Waterman, L., Sayles, F., and Manheim, F.T., 1973, Interstitial water studies on small core samples, legs 16, 17, and 18: Initial reports of the Deep Sea Drilling Project, v. 18, p. 1001-1012, https://doi.org/10.2973/dsdp.proc.18.app2.1973.","productDescription":"12 p.","startPage":"1001","endPage":"1012","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488844,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.18.app2.1973","text":"Publisher Index Page"},{"id":370532,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778184,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207089,"text":"70207089 - 1973 - Mantle convection and volcanic periodicity in the pacific; Evidence from Hawaii","interactions":[],"lastModifiedDate":"2019-12-06T07:14:24","indexId":"70207089","displayToPublicDate":"1973-12-31T14:27:28","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Mantle convection and volcanic periodicity in the pacific; Evidence from Hawaii","docAbstract":"

The thermal-feedback theory of mantle melting proposed by Shaw in 1969 is found to be quantitatively consistent with data pertaining to the evolution of the Hawaiian Ridge. Applicable rate factors are estimated from relations between lava volumes and position along the ridge given in this paper and the radio-metric age distributions given by Jackson and others in 1972. Rate curves derived from these data provide a new method of age extrapolation or interpolation; results indicate that previous methods used to estimate the age of the Hawaiian-Emperor Bend are in error. No definite age is established, but calculations suggest an age greater than 50 m.y. Much more extensive radiometric data are required to define kinematic relations between the Hawaiian Ridge and Emperor Seamount chain. It appears to be firmly established from the work of Jackson and others and from the present study that the evolution of the Hawaiian Ridge has been episodic, with episodes of several different time scales. Average growth rates of the entire ridge system are divided into two regimes with a discontinuity at a position roughly 1,000 km northwest of Kilauea; the estimated age of this discontinuity is about 10 m.y. Other episodes relate to the durations of eruptive sequences along individual or contiguous lines of volcanoes within the en échelon set of locus lines defined by Jackson and others. The latest of these episodes, beginning about 6 m.y. ago, is marked by accelerating volume rates of eruption and accelerating rates of ridge propagation; this episode appears to be approaching a culminating stage represented by the present activity of Kilauea Volcano. The calculated rate of eruption of Kilauea (0.11 km3 per yr) is virtually identical with a rate independently estimated by Swanson in 1972 using different data. Calculated durations for older locus lines are generally greater than 6 m.y., but major time overlaps occur that are not adequately understood. Episodic behavior of shorter durations also exists relative to growth of individual shields or to synchronous activity on neighboring shields (for example, Mauna Loa and Kilauea). Some of these shorter term effects are partly explained in terms of isostatic factors acting on the lithosphere and asthenosphere. The longer episodes are explained in terms of variations of melting rates in the asthenosphere, governed by viscous heating produced by the interaction of lithosphere translation and both vertical and horizontal shear flows in the subjacent mantle. Accelerations of eruption and propagation rates are explained by melting instabilities in the upper zones of the asthenosphere as a result of thermal feedback. During the latest melting episode, shear stresses in the asthenosphere derived from the rate data as interpreted by the thermal feedback model are in the range 100 to 200 bars; apparent viscosities range from 2 × 1021 to 4 × 1020 poise, decreasing with increasing melting rate. In general, a thermomechanical model is shown to be consistent with the idea that oceanic melting spots can be fixed relative to the deep mantle, although this invariance is not completely established. The thermal plume model of Morgan is not definitely ruled out but does not seem to be required for internally consistent interpretations of oceanic chains of volcanism. It is concluded that motion vectors of the Pacific plate cannot be inferred directly from rates of propagation of volcanic chains, because these rates reflect local, not average, relative velocities of lithosphere versus mantle flow. During growth of the Hawaiian Ridge, propagation speeds calculated on the basis of rate data for the southeastern Hawaiian Islands ranged from less than 1 cm per yr near the Hawaiian-Emperor Bend to nearly 30 cm per yr at the present ridge front. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1973)84<1505:MCAVPI>2.0.CO;2","issn":"00167606","usgsCitation":"Shaw, H.R., 1973, Mantle convection and volcanic periodicity in the pacific; Evidence from Hawaii: Geological Society of America Bulletin, v. 84, no. 5, p. 1505-1526, https://doi.org/10.1130/0016-7606(1973)84<1505:MCAVPI>2.0.CO;2.","productDescription":"22 p.","startPage":"1505","endPage":"1526","costCenters":[],"links":[{"id":370013,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Hawaii","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-155.778234,20.245743],[-155.772734,20.245409],[-155.746893,20.232325],[-155.737004,20.222773],[-155.735822,20.212417],[-155.732704,20.205392],[-155.653966,20.16736],[-155.630382,20.146916],[-155.624565,20.145911],[-155.607797,20.137987],[-155.600909,20.126573],[-155.598033,20.124539],[-155.590923,20.122497],[-155.58168,20.123617],[-155.568368,20.130545],[-155.558933,20.13157],[-155.523661,20.120028],[-155.516795,20.11523],[-155.502561,20.114155],[-155.468211,20.104296],[-155.443957,20.095318],[-155.405459,20.078772],[-155.4024,20.075541],[-155.387578,20.067119],[-155.33021,20.038517],[-155.29548,20.024438],[-155.282629,20.021969],[-155.270316,20.014525],[-155.240933,19.990173],[-155.204486,19.969438],[-155.194593,19.958368],[-155.179939,19.949372],[-155.149215,19.922872],[-155.144394,19.920523],[-155.131235,19.906801],[-155.124618,19.897288],[-155.12175,19.886099],[-155.107541,19.872467],[-155.098716,19.867811],[-155.095032,19.867882],[-155.086341,19.855399],[-155.084357,19.849736],[-155.085674,19.838584],[-155.088979,19.826656],[-155.094414,19.81491],[-155.09207,19.799409],[-155.091216,19.776368],[-155.093517,19.771832],[-155.093387,19.737751],[-155.087118,19.728013],[-155.079426,19.726193],[-155.063972,19.728917],[-155.045382,19.739824],[-155.006423,19.739286],[-154.997278,19.72858],[-154.987168,19.708524],[-154.981102,19.690687],[-154.984718,19.672161],[-154.983778,19.641647],[-154.974342,19.633201],[-154.963933,19.627605],[-154.950359,19.626461],[-154.947874,19.62425],[-154.947718,19.621947],[-154.951014,19.613614],[-154.947106,19.604856],[-154.93394,19.597505],[-154.928205,19.592702],[-154.924422,19.586553],[-154.903542,19.570622],[-154.875,19.556797],[-154.852618,19.549172],[-154.837384,19.538354],[-154.826732,19.537626],[-154.814417,19.53009],[-154.809561,19.522377],[-154.809379,19.519086],[-154.822968,19.48129],[-154.838545,19.463642],[-154.86854,19.438126],[-154.887817,19.426425],[-154.928772,19.397646],[-154.944185,19.381852],[-154.964619,19.365646],[-154.980861,19.349291],[-155.020537,19.331317],[-155.061729,19.316636],[-155.113272,19.290613],[-155.1337,19.276099],[-155.159635,19.268375],[-155.172413,19.26906],[-155.187427,19.266156],[-155.19626,19.261295],[-155.205892,19.260907],[-155.243961,19.271313],[-155.264619,19.274213],[-155.296761,19.266289],[-155.303808,19.261835],[-155.31337,19.250698],[-155.341268,19.234039],[-155.349148,19.217756],[-155.360631,19.20893],[-155.378638,19.202435],[-155.390701,19.201171],[-155.417369,19.187858],[-155.427093,19.179546],[-155.432519,19.170623],[-155.453516,19.151952],[-155.465663,19.146964],[-155.505281,19.137908],[-155.51474,19.132501],[-155.51214,19.128174],[-155.512137,19.124296],[-155.519652,19.117025],[-155.526136,19.115889],[-155.528902,19.11371],[-155.544806,19.091059],[-155.551129,19.08878],[-155.557817,19.08213],[-155.555326,19.069377],[-155.555177,19.053932],[-155.557371,19.046565],[-155.566446,19.032531],[-155.576599,19.027412],[-155.581903,19.02224],[-155.596032,18.998833],[-155.596521,18.980654],[-155.601866,18.971572],[-155.613966,18.970399],[-155.625256,18.961951],[-155.625,18.959934],[-155.638054,18.941723],[-155.658486,18.924835],[-155.672005,18.917466],[-155.681825,18.918694],[-155.687716,18.923358],[-155.690171,18.932195],[-155.693117,18.940542],[-155.726043,18.969437],[-155.763598,18.981837],[-155.806109,19.013967],[-155.853943,19.023762],[-155.88155,19.036644],[-155.884077,19.039266],[-155.886278,19.05576],[-155.903693,19.080777],[-155.908355,19.081138],[-155.921389,19.121183],[-155.917292,19.155963],[-155.903339,19.217792],[-155.90491,19.230147],[-155.902565,19.258427],[-155.895435,19.274639],[-155.890842,19.298905],[-155.887356,19.337101],[-155.888701,19.348031],[-155.898792,19.377984],[-155.913849,19.401107],[-155.909087,19.415455],[-155.921707,19.43055],[-155.924269,19.438794],[-155.925166,19.468081],[-155.922609,19.478611],[-155.924124,19.481406],[-155.930523,19.484921],[-155.935641,19.485628],[-155.936403,19.481905],[-155.939145,19.481577],[-155.95149,19.486649],[-155.952897,19.488805],[-155.953663,19.510003],[-155.960457,19.546612],[-155.962264,19.551779],[-155.965211,19.554745],[-155.96935,19.555963],[-155.970969,19.586328],[-155.978206,19.608159],[-155.997728,19.642816],[-156.028982,19.650098],[-156.032928,19.653905],[-156.034994,19.65936],[-156.033326,19.66923],[-156.027427,19.672154],[-156.029281,19.678908],[-156.036079,19.690252],[-156.04796,19.698938],[-156.051652,19.703649],[-156.052485,19.718667],[-156.064364,19.730766],[-156.05722,19.742536],[-156.052315,19.756836],[-156.049651,19.780452],[-156.021732,19.8022],[-156.006267,19.81758],[-155.982821,19.845651],[-155.976651,19.85053],[-155.964817,19.855183],[-155.949251,19.857034],[-155.945297,19.853443],[-155.940311,19.852305],[-155.925843,19.858928],[-155.926938,19.870221],[-155.92549,19.875],[-155.915662,19.887126],[-155.901987,19.912081],[-155.894099,19.923135],[-155.894474,19.926927],[-155.892533,19.932162],[-155.866919,19.954172],[-155.856588,19.968885],[-155.840708,19.976952],[-155.838692,19.975527],[-155.835312,19.976078],[-155.831948,19.982775],[-155.828965,19.995542],[-155.825473,20.025944],[-155.828182,20.035424],[-155.850385,20.062506],[-155.866931,20.078652],[-155.88419,20.10675],[-155.899149,20.145728],[-155.906035,20.205157],[-155.901452,20.235787],[-155.890663,20.25524],[-155.882631,20.263026],[-155.873921,20.267744],[-155.853293,20.271548],[-155.811459,20.26032],[-155.783242,20.246395],[-155.778234,20.245743]]],[[[-157.789581,21.438396],[-157.789734,21.437679],[-157.789276,21.435833],[-157.790543,21.434313],[-157.791718,21.434881],[-157.793045,21.43391],[-157.793167,21.43574],[-157.791565,21.43651],[-157.791779,21.437752],[-157.793289,21.437658],[-157.791779,21.438435],[-157.791092,21.438442],[-157.790741,21.43874],[-157.789581,21.438396]]],[[[-160.125,21.95909],[-160.122262,21.962881],[-160.112746,21.995245],[-160.09645,22.001489],[-160.072123,22.003334],[-160.058543,21.99638],[-160.051992,21.983681],[-160.052729,21.980321],[-160.056336,21.977939],[-160.060549,21.976729],[-160.063349,21.978354],[-160.065811,21.976562],[-160.078393,21.955153],[-160.085787,21.927295],[-160.080012,21.910808],[-160.079065,21.89608],[-160.098897,21.884711],[-160.124283,21.876789],[-160.147609,21.872814],[-160.16162,21.864746],[-160.174796,21.846923],[-160.189782,21.82245],[-160.205211,21.789053],[-160.200427,21.786479],[-160.205851,21.779518],[-160.218044,21.783755],[-160.23478,21.795418],[-160.24961,21.815145],[-160.244943,21.848943],[-160.231028,21.886263],[-160.228965,21.889117],[-160.21383,21.899193],[-160.205528,21.907507],[-160.202716,21.912422],[-160.190158,21.923592],[-160.167471,21.932863],[-160.13705,21.948632],[-160.127302,21.955508],[-160.125,21.95909]]],[[[-159.431707,22.220015],[-159.40732,22.230555],[-159.388119,22.223252],[-159.385977,22.220009],[-159.367563,22.214906],[-159.359842,22.214831],[-159.357227,22.217744],[-159.353795,22.217669],[-159.339964,22.208519],[-159.315613,22.186817],[-159.308855,22.155555],[-159.297808,22.149748],[-159.295875,22.144547],[-159.295271,22.13039],[-159.297143,22.113815],[-159.317451,22.080944],[-159.321667,22.063411],[-159.324775,22.05867],[-159.333267,22.054639],[-159.337996,22.046575],[-159.341401,22.028978],[-159.333224,21.973005],[-159.333109,21.964176],[-159.334714,21.961099],[-159.350828,21.950817],[-159.356613,21.939546],[-159.382349,21.924479],[-159.408284,21.897781],[-159.425862,21.884527],[-159.446599,21.871647],[-159.471962,21.88292],[-159.490914,21.888898],[-159.517973,21.890996],[-159.555415,21.891355],[-159.574991,21.896585],[-159.577784,21.900486],[-159.584272,21.899038],[-159.610241,21.898356],[-159.637849,21.917166],[-159.648132,21.93297],[-159.671872,21.957038],[-159.681493,21.960054],[-159.705255,21.963427],[-159.72014,21.970789],[-159.758218,21.980694],[-159.765735,21.986593],[-159.788139,22.018411],[-159.790932,22.031177],[-159.786543,22.06369],[-159.780096,22.072567],[-159.748159,22.100388],[-159.741223,22.115666],[-159.733457,22.142756],[-159.726043,22.152171],[-159.699978,22.165252],[-159.66984,22.170782],[-159.608794,22.207878],[-159.591596,22.219456],[-159.583965,22.22668],[-159.559643,22.229185],[-159.554166,22.228212],[-159.548594,22.226263],[-159.54115,22.216764],[-159.534594,22.219403],[-159.523769,22.217602],[-159.51941,22.215646],[-159.518348,22.211182],[-159.515574,22.208008],[-159.507811,22.205987],[-159.501055,22.211064],[-159.500821,22.225538],[-159.488558,22.23317],[-159.480158,22.232715],[-159.467007,22.226529],[-159.45619,22.228811],[-159.441809,22.226321],[-159.431707,22.220015]]],[[[-157.014553,21.185503],[-156.999108,21.182221],[-156.991318,21.18551],[-156.987768,21.18935],[-156.982343,21.207798],[-156.984464,21.210063],[-156.984032,21.212198],[-156.974002,21.218503],[-156.969064,21.217018],[-156.962847,21.212131],[-156.951654,21.191662],[-156.950808,21.182636],[-156.946159,21.175963],[-156.918248,21.168279],[-156.903466,21.16421],[-156.898174,21.16594],[-156.89613,21.169561],[-156.896537,21.172208],[-156.867944,21.16452],[-156.841592,21.167926],[-156.821944,21.174693],[-156.771495,21.180053],[-156.742231,21.176214],[-156.738341,21.17202],[-156.736648,21.16188],[-156.719386,21.163911],[-156.712696,21.161547],[-156.714158,21.152238],[-156.726033,21.13236],[-156.748932,21.1086],[-156.775995,21.089751],[-156.790815,21.081686],[-156.794136,21.075796],[-156.835351,21.06336],[-156.865795,21.057801],[-156.877137,21.0493],[-156.891946,21.051831],[-156.89517,21.055771],[-156.953719,21.067761],[-157.00295,21.083282],[-157.02617,21.089015],[-157.032045,21.091094],[-157.037667,21.097864],[-157.079696,21.105835],[-157.095373,21.10636],[-157.125,21.1026],[-157.143483,21.096632],[-157.254061,21.090601],[-157.298054,21.096917],[-157.313343,21.105755],[-157.299187,21.132488],[-157.299471,21.135972],[-157.293774,21.146127],[-157.284346,21.157755],[-157.276474,21.163175],[-157.274504,21.162762],[-157.259911,21.174875],[-157.254709,21.181376],[-157.251007,21.190952],[-157.25026,21.207739],[-157.256935,21.215665],[-157.261457,21.217661],[-157.263163,21.220873],[-157.26069,21.225684],[-157.257085,21.227268],[-157.241534,21.220969],[-157.226445,21.220185],[-157.212082,21.221848],[-157.202125,21.219298],[-157.192439,21.207644],[-157.185553,21.205602],[-157.157103,21.200706],[-157.148125,21.200745],[-157.144627,21.202555],[-157.128207,21.201488],[-157.113438,21.197375],[-157.097971,21.198012],[-157.064264,21.189076],[-157.053053,21.188754],[-157.047757,21.190739],[-157.039987,21.190909],[-157.014553,21.185503]]],[[[-156.544169,20.522802],[-156.550016,20.520273],[-156.559994,20.521892],[-156.586238,20.511711],[-156.603844,20.524372],[-156.631143,20.514943],[-156.642347,20.508285],[-156.647464,20.512017],[-156.668809,20.504738],[-156.682939,20.506775],[-156.703673,20.527237],[-156.702265,20.532451],[-156.696662,20.541646],[-156.6801,20.557021],[-156.651567,20.565574],[-156.614598,20.587109],[-156.610734,20.59377],[-156.576871,20.60657],[-156.56714,20.604895],[-156.553604,20.594729],[-156.543034,20.580115],[-156.542808,20.573674],[-156.548909,20.56859],[-156.556021,20.542657],[-156.553018,20.539382],[-156.540189,20.534741],[-156.539643,20.527644],[-156.544169,20.522802]]],[[[-156.612012,21.02477],[-156.612065,21.027273],[-156.606238,21.034371],[-156.592256,21.03288],[-156.580448,21.020172],[-156.562773,21.016167],[-156.549813,21.004939],[-156.546291,21.005082],[-156.528246,20.967757],[-156.518707,20.954662],[-156.512226,20.95128],[-156.510391,20.940358],[-156.507913,20.937886],[-156.49948,20.934577],[-156.495883,20.928005],[-156.493263,20.916011],[-156.481055,20.898199],[-156.474796,20.894546],[-156.422668,20.911631],[-156.386045,20.919563],[-156.374297,20.927616],[-156.370729,20.932669],[-156.352649,20.941414],[-156.345655,20.941596],[-156.342365,20.938737],[-156.332817,20.94645],[-156.324578,20.950184],[-156.307198,20.942739],[-156.286332,20.947701],[-156.275116,20.937361],[-156.263107,20.940888],[-156.242555,20.937838],[-156.230159,20.931936],[-156.230089,20.917864],[-156.226757,20.916677],[-156.222062,20.918309],[-156.217953,20.916573],[-156.216341,20.907035],[-156.173103,20.876926],[-156.170458,20.874605],[-156.166746,20.865646],[-156.132669,20.861369],[-156.129381,20.847513],[-156.115735,20.827301],[-156.100123,20.828502],[-156.090291,20.831872],[-156.059788,20.81054],[-156.033287,20.808246],[-156.003532,20.795545],[-156.002947,20.789418],[-155.987944,20.776552],[-155.984587,20.767496],[-155.986851,20.758577],[-155.985413,20.744245],[-155.987216,20.722717],[-155.991534,20.713654],[-156.00187,20.698064],[-156.01415,20.685681],[-156.020044,20.686857],[-156.030702,20.682452],[-156.040341,20.672719],[-156.043786,20.664902],[-156.053385,20.65432],[-156.059753,20.652044],[-156.081472,20.654387],[-156.089365,20.648519],[-156.120985,20.633685],[-156.129898,20.627523],[-156.142665,20.623605],[-156.144588,20.624032],[-156.148085,20.629067],[-156.156772,20.629639],[-156.169732,20.627358],[-156.173393,20.6241],[-156.184556,20.629719],[-156.192938,20.631769],[-156.210258,20.628518],[-156.225338,20.62294],[-156.236145,20.61595],[-156.265921,20.601629],[-156.284391,20.596488],[-156.288037,20.59203],[-156.293454,20.588783],[-156.302692,20.586199],[-156.322944,20.588273],[-156.351716,20.58697],[-156.359634,20.581977],[-156.370725,20.57876],[-156.377633,20.578427],[-156.415313,20.586099],[-156.417523,20.589728],[-156.415746,20.594044],[-156.417799,20.598682],[-156.423141,20.602079],[-156.427708,20.598873],[-156.431872,20.598143],[-156.438385,20.601337],[-156.444242,20.607941],[-156.442884,20.613842],[-156.450651,20.642212],[-156.445894,20.64927],[-156.443673,20.656018],[-156.448656,20.704739],[-156.451038,20.725469],[-156.452895,20.731287],[-156.458438,20.736676],[-156.462242,20.753952],[-156.462058,20.772571],[-156.464043,20.781667],[-156.473562,20.790756],[-156.489496,20.798339],[-156.501688,20.799933],[-156.506026,20.799463],[-156.515994,20.794234],[-156.525215,20.780821],[-156.537752,20.778408],[-156.631794,20.82124],[-156.678634,20.870541],[-156.688969,20.888673],[-156.687804,20.89072],[-156.688132,20.906325],[-156.691334,20.91244],[-156.697418,20.916368],[-156.69989,20.920629],[-156.69411,20.952708],[-156.680905,20.980262],[-156.665514,21.007054],[-156.652419,21.008994],[-156.645966,21.014416],[-156.642592,21.019936],[-156.644167,21.022312],[-156.642809,21.027583],[-156.619581,21.027793],[-156.612012,21.02477]]],[[[-157.010001,20.929757],[-156.989813,20.932127],[-156.971604,20.926254],[-156.937529,20.925274],[-156.91845,20.922546],[-156.897169,20.915395],[-156.837047,20.863575],[-156.825237,20.850731],[-156.809576,20.826036],[-156.808469,20.820396],[-156.809463,20.809169],[-156.817427,20.794606],[-156.838321,20.764575],[-156.846413,20.760201],[-156.851481,20.760069],[-156.869753,20.754701],[-156.890295,20.744855],[-156.909081,20.739533],[-156.949009,20.738997],[-156.96789,20.73508],[-156.984747,20.756677],[-156.994001,20.786671],[-156.988933,20.815496],[-156.991834,20.826603],[-157.006243,20.849603],[-157.010911,20.854476],[-157.054552,20.877219],[-157.059663,20.884634],[-157.061128,20.890635],[-157.062511,20.904385],[-157.05913,20.913407],[-157.035789,20.927078],[-157.025626,20.929528],[-157.010001,20.929757]]],[[[-158.044485,21.306011],[-158.0883,21.2988],[-158.1033,21.2979],[-158.1127,21.3019],[-158.1211,21.3169],[-158.1225,21.3224],[-158.111949,21.326622],[-158.114196,21.331123],[-158.119427,21.334594],[-158.125459,21.330264],[-158.13324,21.359207],[-158.1403,21.3738],[-158.149719,21.385208],[-158.161743,21.396282],[-158.1792,21.4043],[-158.181274,21.409626],[-158.181,21.420868],[-158.182648,21.430073],[-158.192352,21.44804],[-158.205383,21.459793],[-158.219446,21.46978],[-158.233,21.4876],[-158.231171,21.523857],[-158.23175,21.533035],[-158.234314,21.540058],[-158.250671,21.557373],[-158.27951,21.575794],[-158.277679,21.578789],[-158.254425,21.582684],[-158.190704,21.585892],[-158.17,21.5823],[-158.12561,21.586739],[-158.10672,21.596577],[-158.106689,21.603024],[-158.1095,21.6057],[-158.108185,21.607487],[-158.079895,21.628101],[-158.0668,21.6437],[-158.066711,21.65234],[-158.0639,21.6584],[-158.0372,21.6843],[-158.018127,21.699955],[-157.9923,21.708],[-157.98703,21.712494],[-157.968628,21.712704],[-157.947174,21.689568],[-157.939,21.669],[-157.9301,21.6552],[-157.924591,21.651183],[-157.9228,21.6361],[-157.9238,21.6293],[-157.910797,21.611183],[-157.900574,21.605885],[-157.87735,21.575277],[-157.878601,21.560181],[-157.872528,21.557568],[-157.8669,21.5637],[-157.85614,21.560661],[-157.85257,21.557514],[-157.836945,21.529945],[-157.837372,21.512085],[-157.849579,21.509598],[-157.852625,21.499971],[-157.84549,21.466747],[-157.84099,21.459483],[-157.82489,21.455379],[-157.8163,21.4502],[-157.8139,21.4403],[-157.8059,21.4301],[-157.786513,21.415633],[-157.779846,21.417309],[-157.774455,21.421352],[-157.772209,21.431236],[-157.774905,21.453698],[-157.772209,21.457741],[-157.764572,21.461335],[-157.754239,21.461335],[-157.737617,21.459089],[-157.731777,21.455944],[-157.731328,21.444713],[-157.73582,21.438424],[-157.740762,21.424048],[-157.741211,21.414614],[-157.7386,21.4043],[-157.730191,21.401871],[-157.728221,21.402104],[-157.726421,21.402845],[-157.724324,21.403311],[-157.723794,21.40329],[-157.723286,21.403227],[-157.722735,21.403121],[-157.722544,21.403036],[-157.721845,21.401596],[-157.721083,21.399541],[-157.7189,21.3961],[-157.7089,21.3833],[-157.7087,21.3793],[-157.7126,21.3689],[-157.7106,21.3585],[-157.7088,21.3534],[-157.6971,21.3364],[-157.6938,21.3329],[-157.6619,21.3131],[-157.6518,21.3139],[-157.652629,21.308709],[-157.6537,21.302],[-157.6946,21.2739],[-157.6944,21.2665],[-157.7001,21.264],[-157.7097,21.2621],[-157.7139,21.2638],[-157.7142,21.2665],[-157.7114,21.272],[-157.7122,21.2814],[-157.7143,21.2845],[-157.7213,21.2869],[-157.7572,21.278],[-157.765,21.2789],[-157.7782,21.2735],[-157.7931,21.2604],[-157.8096,21.2577],[-157.8211,21.2606],[-157.8241,21.2646],[-157.8253,21.2714],[-157.8319,21.2795],[-157.8457,21.29],[-157.89,21.3065],[-157.894518,21.319632],[-157.898969,21.327391],[-157.90482,21.329172],[-157.918939,21.318615],[-157.917921,21.313781],[-157.913469,21.310983],[-157.910925,21.305768],[-157.952263,21.306531],[-157.950736,21.312509],[-157.951881,21.318742],[-157.967971,21.327986],[-157.973334,21.327426],[-157.989424,21.317984],[-158.0245,21.3093],[-158.044485,21.306011]]]]},\"properties\":{\"name\":\"Hawaii\",\"nation\":\"USA \"}}]}","volume":"84","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shaw, H. R.","contributorId":23952,"corporation":false,"usgs":true,"family":"Shaw","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":776790,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207386,"text":"70207386 - 1973 - Igneous activity, metamorphism, and heart mountain faulting at White Mountain, Northwestern Wyoming: Reply","interactions":[],"lastModifiedDate":"2019-12-20T07:09:22","indexId":"70207386","displayToPublicDate":"1973-12-31T14:01:13","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Igneous activity, metamorphism, and heart mountain faulting at White Mountain, Northwestern Wyoming: Reply","docAbstract":"

No abstract available. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1973)84<3111:IAMAHM>2.0.CO;2","issn":"00167606","usgsCitation":"Nelson, W.H., Pierce, W.G., and Brophy, G., 1973, Igneous activity, metamorphism, and heart mountain faulting at White Mountain, Northwestern Wyoming: Reply: Geological Society of America Bulletin, v. 84, no. 9, p. 3111-3112, https://doi.org/10.1130/0016-7606(1973)84<3111:IAMAHM>2.0.CO;2.","productDescription":"2 p. ","startPage":"3111","endPage":"3112","costCenters":[],"links":[{"id":370426,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.181640625,\n 42.13082130188811\n ],\n [\n -106.2158203125,\n 42.13082130188811\n ],\n [\n -106.2158203125,\n 45.058001435398275\n ],\n [\n -111.181640625,\n 45.058001435398275\n ],\n [\n -111.181640625,\n 42.13082130188811\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"84","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nelson, W. H.","contributorId":100336,"corporation":false,"usgs":true,"family":"Nelson","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, W. G.","contributorId":11267,"corporation":false,"usgs":true,"family":"Pierce","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":777880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brophy, G.P.","contributorId":221335,"corporation":false,"usgs":false,"family":"Brophy","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":777881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207385,"text":"70207385 - 1973 - Crandall conglomerate, an unusual stream deposit, and its relation to heart mountain faulting","interactions":[],"lastModifiedDate":"2019-12-18T13:59:16","indexId":"70207385","displayToPublicDate":"1973-12-31T13:50:27","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":" Crandall conglomerate, an unusual stream deposit, and its relation to heart mountain faulting","docAbstract":"

The Crandall Conglomerate (Eocene) is a channel deposit, more than 350 ft (100 m) thick, believed to have formed as a result of preliminary movement of the Heart Mountain detachment fault in northwestern Wyoming. Initial movement of the Heart Mountain fault opened a deep rift in which the conglomerate was deposited. The rift was less than a mile (1.6 km) wide and was bordered by 2,000-ft (600 m) cliffs, mostly of Paleozoic limestone. Before the gravel was deposited, unconfined Cambrian shale below the rift was deformed into the Blacktail fold, a sharp anticline without apparent roots, while streams carried away the upwelling shale and cut a channel several hundred feet deep. The debris that accumulated in this channel is the Crandall Conglomerate. Deposition of the conglomerate was followed by Cathedral Cliffs volcanism, by movement on the Reef Creek detachment fault, and by the main movement on the Heart Mountain detachment fault. The main movement on this fault left the lower part of the conglomerate in place but carried the upper part with deposits of the upper plate roughly 15 mi (24 km) southeastward. Most of the deposits of the lower plate rest directly on the Blacktail fold. Of the 15 known deposits of Crandall Conglomerate, five are in place but have been overridden by the upper plate of the Heart Mountain fault, and ten have been transported as part of the upper plate. After this movement, volcanic rocks of the Wapiti Formation blanketed the region. © 1973 Geological Society of America.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1973)84<2631:CCAUSD>2.0.CO;2","issn":"00167606","usgsCitation":"Pierce, W.G., and Nelson, W.H., 1973, Crandall conglomerate, an unusual stream deposit, and its relation to heart mountain faulting: Geological Society of America Bulletin, v. 84, no. 8, p. 2631-2644, https://doi.org/10.1130/0016-7606(1973)84<2631:CCAUSD>2.0.CO;2.","productDescription":"14 p.","startPage":"2631","endPage":"2644","costCenters":[],"links":[{"id":370425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"84","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pierce, W. G.","contributorId":11267,"corporation":false,"usgs":true,"family":"Pierce","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":777877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, W. H.","contributorId":100336,"corporation":false,"usgs":true,"family":"Nelson","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}