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,{"id":59174,"text":"mf410 - 1972 - Metallic mineral resource map of the Fairbanks quadrangle, Alaska","interactions":[{"subject":{"id":13067,"text":"ofr6756 - 1967 - Metallic mineral resources map of the Fairbanks Quadrangle, Alaska","indexId":"ofr6756","publicationYear":"1967","noYear":false,"title":"Metallic mineral resources map of the Fairbanks Quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":59174,"text":"mf410 - 1972 - Metallic mineral resource map of the Fairbanks quadrangle, Alaska","indexId":"mf410","publicationYear":"1972","noYear":false,"title":"Metallic mineral resource map of the Fairbanks quadrangle, Alaska"},"id":1}],"lastModifiedDate":"2022-08-17T20:21:00.237849","indexId":"mf410","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"410","title":"Metallic mineral resource map of the Fairbanks quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf410","usgsCitation":"Cobb, E.H., 1972, Metallic mineral resource map of the Fairbanks quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 410, 1 Plate: 35.00 × 22.50 inches, https://doi.org/10.3133/mf410.","productDescription":"1 Plate: 35.00 × 22.50 inches","costCenters":[],"links":[{"id":180510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":111294,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13194","linkFileType":{"id":5,"text":"html"}},{"id":405282,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2836.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Fairbanks quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150,\n              64\n            ],\n            [\n              -147,\n              64\n            ],\n            [\n              -147,\n              65\n            ],\n            [\n              -150,\n              65\n            ],\n            [\n              -150,\n              64\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6272df","contributors":{"authors":[{"text":"Cobb, E. H.","contributorId":71971,"corporation":false,"usgs":true,"family":"Cobb","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":261568,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":59022,"text":"mf355 - 1972 - Active faults, probable active faults, and associated fracture zones, San Mateo County, California","interactions":[],"lastModifiedDate":"2018-12-17T14:41:56","indexId":"mf355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"355","title":"Active faults, probable active faults, and associated fracture zones, San Mateo County, California","docAbstract":"<p>As used on this map, the term active fault is defined as a fracture or fracture zone several miles long along which the two sides either are moving relative to one another and parallel to the fracture or are judged likely to move in such fashion within the useful life of existing man-made structures.&nbsp; The judgment that a fault is active may be based on: 1) historic records of surface faulting and earthquake activity, 2) topographic evidence that demonstrates repeated and systematic displacements along the fault trace, 3) systematic displacement of Holocene or Pleistocene geologic units along the fault trace, 4) a linear pattern of small-earthquake activity either along the surface trace of the fault or parallel to it and within 2 miles of the surface trace, or 5) current and measurable systematic displacement across the surface trace of the fault.&nbsp; Most active faults shown on the map are recognized as active on the basis of two or more of these criteria.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf355","usgsCitation":"Brown, R.D., 1972, Active faults, probable active faults, and associated fracture zones, San Mateo County, California: U.S. Geological Survey Miscellaneous Field Studies Map 355, 35.51 x 44.68 inches, https://doi.org/10.3133/mf355.","productDescription":"35.51 x 44.68 inches","costCenters":[],"links":[{"id":360390,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0355/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0355/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Mateo County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.56666666666666,36.96666666666667 ], [ -122.56666666666666,37.583333333333336 ], [ -122.06666666666666,37.583333333333336 ], [ -122.06666666666666,36.96666666666667 ], [ -122.56666666666666,36.96666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a34cb","contributors":{"authors":[{"text":"Brown, Robert D. Jr.","contributorId":71146,"corporation":false,"usgs":true,"family":"Brown","given":"Robert","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":261281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13704,"text":"ofr72126 - 1972 - Exploration for iron in the Sakarkaya-Cavdar area, Mugla district, Turkey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr72126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-126","title":"Exploration for iron in the Sakarkaya-Cavdar area, Mugla district, Turkey","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72126","usgsCitation":"Gair, J.E., and Capan, U.Z., 1972, Exploration for iron in the Sakarkaya-Cavdar area, Mugla district, Turkey: U.S. Geological Survey Open-File Report 72-126, iii, 30 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr72126.","productDescription":"iii, 30 leaves :ill., maps ;27 cm.","costCenters":[],"links":[{"id":146840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8cf3","contributors":{"authors":[{"text":"Gair, Jacob E.","contributorId":18381,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168263,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capan, Ussal Z.","contributorId":100402,"corporation":false,"usgs":true,"family":"Capan","given":"Ussal","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":168264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56740,"text":"wdrNY712 - 1972 - Water resources data for New York, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2020-12-14T23:23:35.436375","indexId":"wdrNY712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-71-2","title":"Water resources data for New York, water year 1971; Part 2, Water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for New York, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report NY-71-2, vi, 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,{"id":46884,"text":"ofr72253 - 1972 - Geologic map of the Lone Haystack Mountain Quadrangle, Carbon County, Wyoming","interactions":[{"subject":{"id":46884,"text":"ofr72253 - 1972 - Geologic map of the Lone Haystack Mountain Quadrangle, Carbon County, Wyoming","indexId":"ofr72253","publicationYear":"1972","noYear":false,"title":"Geologic map of the Lone Haystack Mountain Quadrangle, Carbon County, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":62512,"text":"gq1064 - 1973 - Geologic map of the Lone Haystack Mountain quadrangle, Carbon County, Wyoming","indexId":"gq1064","publicationYear":"1973","noYear":false,"title":"Geologic map of the Lone Haystack Mountain quadrangle, Carbon County, Wyoming"},"id":1}],"supersededBy":{"id":62512,"text":"gq1064 - 1973 - Geologic map of the Lone Haystack Mountain quadrangle, Carbon County, Wyoming","indexId":"gq1064","publicationYear":"1973","noYear":false,"title":"Geologic map of the Lone Haystack Mountain quadrangle, Carbon County, Wyoming"},"lastModifiedDate":"2018-09-04T16:50:40","indexId":"ofr72253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-253","title":"Geologic map of the Lone Haystack Mountain Quadrangle, Carbon County, Wyoming","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72253","usgsCitation":"Merewether, E., 1972, Geologic map of the Lone Haystack Mountain Quadrangle, Carbon County, Wyoming: U.S. Geological Survey Open-File Report 72-253, 1 Plate: 38.39 x 34.93 inches, https://doi.org/10.3133/ofr72253.","productDescription":"1 Plate: 38.39 x 34.93 inches","costCenters":[],"links":[{"id":170837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0253/report-thumb.jpg"},{"id":357054,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0253/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Wyoming","county":"Carbon County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.125,\n              41.875\n            ],\n            [\n              -107,\n              41.875\n            ],\n            [\n              -107,\n              42\n            ],\n            [\n              -107.125,\n              42\n            ],\n            [\n              -107.125,\n              41.875\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696de5","contributors":{"authors":[{"text":"Merewether, E.A.","contributorId":32517,"corporation":false,"usgs":true,"family":"Merewether","given":"E.A.","affiliations":[],"preferred":false,"id":234253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17612,"text":"ofr72283 - 1972 - Reconnaissance geology of the Bi'r Al Badriyah quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:22","indexId":"ofr72283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-283","title":"Reconnaissance geology of the Bi'r Al Badriyah quadrangle, Kingdom of Saudi Arabia","docAbstract":"The Bi'r al Badriyah quadrangle covers an area of 2843 sq km in the extreme eastern part of the Precambrian Shield in central Saudi Arabia. The Precambrian rocks in the southeastern part of the area are unconformably overlain by limestone of Permian age, which occupies only a small part of the quadrangle. Three great sequences of Precambrian rocks are recognized and called, from oldest to youngest, the Halaban Group, the Bi'r Khountina Group, and the Murdama Group. From evidence within the quadrangle itself the three groups are seen to be separated by erosional unconformities, and the Halaban and Bi'r Khountina Groups are intruded by granitic and gabbroic plutonic rocks and a wide variety of dikes. Exposures north of the quadrangle show that the Murdama Group is also intruded by granitic rocks. \r\n\r\nThe Halaban Group, consists of three formations called, from oldest to youngest, the Umm Mushraha Formation, the Jebal al Egfool Formation, and the Wadi al Jifr Formation. These rocks are variably metamorphosed, but characteristically they are at the epidote-albite amphibolite facies of regional metamorphism, are polymetamorphic, and rest unconformably on ancient granite gneiss. The Umm Mushraha Formation consists of amphibolite, schistose andesite, and greenstone associated with minor meta-agglomerate, meta-graywacke, and marble. The Jebal al Egfool Formation consists of sheared and metamorphosed volcanic rocks of intermediate composition, and the Wadi al Jifr Formation is made up of metamorphosed felsic volcanic rocks. \r\n\r\nRocks of the Bi'r Khountina Group are rather similar to the Halaban Group in original composition, but they are separated from the Halaban by an angular unconformity and have distinctive formations of conglomerate (the Idsas Formation), marble (the Fawara Formation), and graywacke (the Abu Sawarir Formation) at the base. Most of the Bi'r Khountina Group consists of andesitic volcanic rocks in the Badriyah Formation. Mostly, the Bi'r Khountina Group is unmetamorphosed or feebly metamorphosed to the greenschist facies. Locally, as in the aureole of intrusive rocks, the Bi'r Khountina Group reaches higher metamorphic grades.\r\n\r\nThe rocks of the Murdama Group unconformably overlie the Bi'r Khountina Group, and basal conglomerates of the Murdama contain fragments of distinctive rocks intrusive into the Bi'r Khountina. The Murdama Group is composed of the Z'relba Formation, Consisting of conglomerate and schistose conglomerate and the Abt Formation, a thick sequence of laminated, mainly fine-grained, sedimentary rocks. Metamorphism in .the Murdama increases toward the north, and along the north edge of the area the Murdama Group is represented by chlorite-sericite schists. \r\n\r\nThree major episodes of folding are recorded in the Precambrian rocks. The earliest episode folded the rocks of the Halaban Group along north-trending axes which are now truncated by the unconformity at the base of the Bi'r Khountina Group. After the rocks of the Bi'r Khountina and Murdama Groups were deposited, the three groups were folded along northwest-trending axes of regional scale. Later, possibly at a time of major faulting along a northwesterly direction, the rocks were again folded on north-trending axes. \r\n\r\nSamples of rock materials collected at 105 localities in the quadrangle were analyzed for 27 elements. Only one anomalous value was found: a low positive anomaly for lead at the Umm Mushraha gold mine. Threshold amounts of Ag, B, Cr, Cu, La, Mn, Mo, NI, Sc, Sn, Ti, V, and Zr were detected. The distribution of copper and molybdenum suggests that two plutons of biotite-hornblende granite in the central part of the quadrangle, and the rocks between them, should be examined for possible disseminated copper and molybdenum of the porphyry type. The distribution of scandium and detrital scheelite suggests that a zone adjacent to phyllonite in the northeastern quarter of the quadrangle be examined for tungsten associated with amphibolite.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr72283","usgsCitation":"Overstreet, W.C., Whitlow, J.W., Kahr, V., and Ankary, A., 1972, Reconnaissance geology of the Bi'r Al Badriyah quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 72-283, ii, 47 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr72283.","productDescription":"ii, 47 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":151078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0283/report-thumb.jpg"},{"id":46808,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0283/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0283/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a86","contributors":{"authors":[{"text":"Overstreet, William C.","contributorId":73586,"corporation":false,"usgs":true,"family":"Overstreet","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":177099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitlow, J. W.","contributorId":63810,"corporation":false,"usgs":true,"family":"Whitlow","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kahr, V.P.","contributorId":88757,"corporation":false,"usgs":true,"family":"Kahr","given":"V.P.","affiliations":[],"preferred":false,"id":177101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ankary, A.O.","contributorId":74016,"corporation":false,"usgs":true,"family":"Ankary","given":"A.O.","affiliations":[],"preferred":false,"id":177100,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":34890,"text":"b1358 - 1972 - Geology of the Istaru Quadrangle, Costa Rica","interactions":[],"lastModifiedDate":"2012-02-02T00:09:21","indexId":"b1358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1358","title":"Geology of the Istaru Quadrangle, Costa Rica","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1358","usgsCitation":"Krushensky, R., 1972, Geology of the Istaru Quadrangle, Costa Rica: U.S. Geological Survey Bulletin 1358, iv, 46 p. :2 fold. maps in pocket, (some col.) ;24 cm., https://doi.org/10.3133/b1358.","productDescription":"iv, 46 p. :2 fold. maps in pocket, (some col.) ;24 cm.","costCenters":[],"links":[{"id":163292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1358/report-thumb.jpg"},{"id":62848,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1358/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62849,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1358/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fe70","contributors":{"authors":[{"text":"Krushensky, R.D.","contributorId":94648,"corporation":false,"usgs":true,"family":"Krushensky","given":"R.D.","affiliations":[],"preferred":false,"id":213766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56750,"text":"wdrWA711 - 1972 - Water resources data for Washington, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2022-12-27T17:57:48.379983","indexId":"wdrWA711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-71-1","title":"Water resources data for Washington, water year 1971; Part 1, Surface water records","docAbstract":"<p>Surface-water records for the 1971 water year for Washington, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. B. Laird, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA711","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Washington, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report WA-71-1, xiv, 427 p., https://doi.org/10.3133/wdrWA711.","productDescription":"xiv, 427 p.","costCenters":[],"links":[{"id":411073,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175193,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f17ab","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":532866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2638,"text":"wsp1873C - 1972 - Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1873C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1873","chapter":"C","title":"Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67","docAbstract":"This report describes the significant results to 1967 of a comprehensive study that began in 1963 to evaluate what changes take place in an estuary as the loads .of raw and partially treated industrial and municipal wastes are replaced by effluent from a secondary treatment plant. The study area is the Duwamish River estuary, about 18.3 river kilometers long. At mean sea level the estuary has a water-surface area of about 1 square mile and a mean width of 440 feet. At the lowest and highest recorded tides, the volume of the estuary is about 205 and 592 million cubic feet, respectively. The estuary is well stratified (salt-wedge type) at fresh-water inflows greater than 1,000 cfs \r\n(cubic feet per second), but when inflow rates are less than 1,000 cfs the lower 5.6 kilometers of the estuary grades into the partly mixed type. The crosschannel salinity distribution is uniform for a given location and depth. Salinity migration is controlled by tides and fresh-water inflow. At fresh-water inflow rates greater than 1,000 cfs, water in the upper 8.4 kilometers of the estuary is always fresh regardless of tide. At inflow rates less than 600 cfs and tide heights greater than 10 feet; some salinity has been detected 16.1 kilometers above the mouth of the estuary. Studies using a fluorescent dye show that virtually no downward mixing into the salt wedge occurs; soluble pollutants introduced at the upper end of the estuary stay in the surface layer (5-15 ft thick). On the basis of dye studies when fresh-water inflow is less than 400 cfs, it is estimated that less than 10 percent of a pollutant will remain in the estuary a minimum of 7 days. Longitudinal dispersion coefficients for the surface layer have been determined to be on the order of 100-400 square feet per second. \r\n\r\nFour water-quality stations automatically monitor DO (dissolved oxygen), water temperature, pH, and specific conductance; at one station solar radiation also is measured. DO concentration in the surface layer decreases almost linearly in a downstream direction. Minimum DO concentration in the surface layer is usually greater than 4 rag/1 (milligrams per liter). The smallest DO values are consistently recorded in the bottom layer at the station 7.7 kilometers above the mouth; monthly means of less than 3 mg/1 of DO have occurred at this point. Manual sampling shows that the DO sag in the bottom layer oscillates between 7.7 and 10.4 kilometers above the mouth of the estuary. Multiple-regression analysis shows that the surface DO content can be estimated from the fresh-water inflow and water temperature. Tidal exchange and fresh-water inflow indirectly control the bottom DO content. Information available from previous studies failed to indicate a progressive decrease in DO content during the period 1949-56, but data from the present study suggest a slight general decrease in the annual minimum DO concentrations in both the upper and lower layers. Average nitrate concentration in fresh water at station 16.2 has increased progressively since 1964, by amounts greater than those which can be attributed to the Renton Treatment Plant, 4.3 kilometers upstream from station 16.2. \r\n\r\nThe BOD (biochemical oxygen demand) in both surface and bottom layers is generally less than 4 rag/1 of oxygen, but values greater than 6 rag/1 have been measured during a period of phytoplankton bloom. Phytoplankton blooms can occur during periods of minimum tidal exchange and fresh-water inflows of less than 300 cfs if solar radiation and water temperature are optimum. Nutrients (nitrogen and phosphorus compounds) do not control the occurrence of a bloom, because sufficient quantities of these nutrients are always present. Nutrients in the treated effluent may increase the biomass of the bloom. Trace-element studies have not defined any role that these elements may play in algal growth. \r\nThe inflowing fresh water contains principally calcium and bicarbonate and \r\nhas a dissolved-solids content ra","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1873C","usgsCitation":"Santos, J.F., and Stoner, J., 1972, Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67: U.S. Geological Survey Water Supply Paper 1873, vi, 74 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1873C.","productDescription":"vi, 74 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873c/report-thumb.jpg"},{"id":28957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ac0","contributors":{"authors":[{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":145542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34754,"text":"b1363 - 1972 - Underclay deposits of Somerset and eastern Fayette Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:09:42","indexId":"b1363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1363","title":"Underclay deposits of Somerset and eastern Fayette Counties, Pennsylvania","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1363","usgsCitation":"Hosterman, J.W., 1972, Underclay deposits of Somerset and eastern Fayette Counties, Pennsylvania: U.S. Geological Survey Bulletin 1363, iii, 17 p. ;23 cm., https://doi.org/10.3133/b1363.","productDescription":"iii, 17 p. ;23 cm.","costCenters":[],"links":[{"id":167206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1363/report-thumb.jpg"},{"id":62627,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1363/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62628,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1363/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62629,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1363/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f7a1","contributors":{"authors":[{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":213525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56755,"text":"wdrMS711 - 1972 - Water resources data for Mississippi, water year 1971","interactions":[],"lastModifiedDate":"2025-08-28T14:25:18.228863","indexId":"wdrMS711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MS-71-1","title":"Water resources data for Mississippi, water year 1971","docAbstract":"<p>Water resources data for the 1971 water year for Mississippi including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included for 71 gaging stations of which 67 are streamflow discharge stations, and 4 are reservoir or lake stations; also are included records for 27 low-flow partial-record stations, 143 crest-stage partial-record stations, and 91 miscellaneous sites. Locations of gaging stations are shown in Figure 1. In Part 2, data on the quality of surface water (chemical and temperature) were collected from designated sampling sites at pre-determined intervals such as monthly, or less frequently, and at one site data were recorded on punched paper tape at 60-minute intervals. Records are given for 55 sampling stations of which 5 are continuous record stations, 26 are partial-record stations, and 3 are miscellaneous sites. Locations of water-quality stations are shown in Figure 1. A few pertinent stations (not included above) in bordering States are also included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. E. Carroon, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Mississippi, water year 1971: U.S. Geological Survey Water Data Report MS-71-1, vii, 180 p., https://doi.org/10.3133/wdrMS711.","productDescription":"vii, 180 p.","costCenters":[],"links":[{"id":494996,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/ms-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175273,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/ms-71-1/report-thumb.jpg"}],"country":"United 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