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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri739","usgsCitation":"Pearson, H.E., 1973, Test-observation well near Paterson, Washington : description and preliminary results: U.S. Geological Survey Water-Resources Investigations Report 73-9, iii, 23 p. , https://doi.org/10.3133/wri739.","productDescription":"iii, 23 p. 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The investigation is part of the Commission's feasibility study on storing high-level radioactive waste in chambers mined in basaltic rocks at a. depth of about 3,000 feet or more below the surface. Ground-water flow., on a regional scale, occurs principally in the basalt and-in interbedded sediments of the Columbia River Group, and is controlled by topography, the structure of the basalt, and the large streams--the Columbia, Snake, and Yakima Rivers. The ground water beneath the main part of the Hanford Reservation, south and west of the Columbia River, inures southeastward from recharge areas in the uplands, including Cold Creek and Dry Creek valleys, and ultimately discharges to the Columbia River south of the reservation: East and southeast of the Columbia River, ground water flows generally southwestward and discharges to the River. The Yakima River valley contains a distinct flow system in which movement is toward the Yakima River from the topographic divides. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i811","usgsCitation":"West, M., 1973, Geologic map of the Censorinus region of the Moon: U.S. Geological Survey IMAP 811, 1 Plate: 58.67 × 29.33 inches, https://doi.org/10.3133/i811.","productDescription":"1 Plate: 58.67 × 29.33 inches","costCenters":[],"links":[{"id":439036,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9INFKAG","text":"USGS data release","linkHelpText":"Geologic map of the Censorinus region of the Moon"},{"id":439035,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9M9I8PP","text":"USGS data release","linkHelpText":"Interactive Map: USGS IMAP 811 Geologic Map of the Censorinus Region of the Moon"},{"id":187663,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414193,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://doi.org/10.5066/P9M9I8PP","text":"Interactive map","linkHelpText":"- Geologic Map of the Censorinus Region of the Moon, 1:250K. 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27 cm., https://doi.org/10.3133/ofr7259.","productDescription":"44 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":161660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdef7","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":236678,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15666,"text":"ofr73240 - 1973 - Geologic map of the Thoreau quadrangle, McKinley County, New Mexico","interactions":[{"subject":{"id":15666,"text":"ofr73240 - 1973 - Geologic map of the Thoreau quadrangle, McKinley County, New Mexico","indexId":"ofr73240","publicationYear":"1973","noYear":false,"title":"Geologic map of the Thoreau quadrangle, McKinley County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":61570,"text":"gq1675 - 1990 - Geologic map of the Thoreau quadrangle, McKinley County, New Mexico","indexId":"gq1675","publicationYear":"1990","noYear":false,"title":"Geologic map of the Thoreau quadrangle, McKinley County, New Mexico"},"id":1}],"supersededBy":{"id":61570,"text":"gq1675 - 1990 - Geologic map of the Thoreau quadrangle, McKinley County, New Mexico","indexId":"gq1675","publicationYear":"1990","noYear":false,"title":"Geologic map of the Thoreau quadrangle, McKinley County, New Mexico"},"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr73240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-240","title":"Geologic map of the Thoreau quadrangle, McKinley County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr73240","usgsCitation":"Robertson, J., 1973, Geologic map of the Thoreau quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 73-240, 20 p. :folded map ;27 cm.; 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Records for a few pertinent gaging stations in bordering States and Provinces are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of G. S. Hayes, 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 Maine.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME721","collaboration":"Prepared in cooperation with the Maine Public Utilities Commission and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Maine, water year 1972: U.S. Geological Survey Water Data Report ME-72-1, vi, 120 p., https://doi.org/10.3133/wdrME721.","productDescription":"vi, 120 p.","costCenters":[],"links":[{"id":181430,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1972/me-72-1/report-thumb.jpg"},{"id":494294,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/me-72-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f236e","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":532714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23217,"text":"ofr7391 - 1973 - Proposed water resources and land-capability investigation, Arusha region, Tanzania","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr7391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-91","title":"Proposed water resources and land-capability investigation, Arusha region, Tanzania","language":"ENGLISH","publisher":"Geological Survey, United States Dept. of the Interior :\r\nForest Service, United States Dept. of Agriculture ;\r\nGovernment of the United Republic of Tanzania,","doi":"10.3133/ofr7391","issn":"0094-9140","usgsCitation":"Gordon, E., and O’Rourke, J.F., 1973, Proposed water resources and land-capability investigation, Arusha region, Tanzania: U.S. Geological Survey Open-File Report 73-91, 113 p. :ill., col. map ;27 cm., https://doi.org/10.3133/ofr7391.","productDescription":"113 p. :ill., col. map ;27 cm.","costCenters":[],"links":[{"id":154501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d671","contributors":{"authors":[{"text":"Gordon, E.D.","contributorId":76345,"corporation":false,"usgs":true,"family":"Gordon","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":189651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Rourke, J. F.","contributorId":50554,"corporation":false,"usgs":true,"family":"O’Rourke","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":189650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48208,"text":"ofr73359 - 1973 - Base flow in the Acme-Artesia reach of the Pecos River, New Mexico, 1957-71","interactions":[],"lastModifiedDate":"2012-02-02T00:10:43","indexId":"ofr73359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-359","title":"Base flow in the Acme-Artesia reach of the Pecos River, New Mexico, 1957-71","language":"ENGLISH","doi":"10.3133/ofr73359","usgsCitation":"Welder, G.E., 1973, Base flow in the Acme-Artesia reach of the Pecos River, New Mexico, 1957-71: U.S. Geological Survey Open-File Report 73-359, 50 p. (some folded) : ill., maps ; 27 cm., https://doi.org/10.3133/ofr73359.","productDescription":"50 p. (some folded) : ill., maps ; 27 cm.","costCenters":[],"links":[{"id":100094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0359/report.pdf","size":"21962","linkFileType":{"id":1,"text":"pdf"}},{"id":100095,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0359/plate-2.pdf","size":"2883","linkFileType":{"id":1,"text":"pdf"}},{"id":172014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0359/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6492a1","contributors":{"authors":[{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":236968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39113,"text":"pp306E - 1973 - Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae)","interactions":[],"lastModifiedDate":"2017-11-29T09:21:36","indexId":"pp306E","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":"306","chapter":"E","title":"Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae)","docAbstract":"Chapter E adds 112 described species and subspecies (a few briefly described) to the some 440 covered in preceding chapters : 27 additional gastropods, 18 scaphopods, and 67 pelecypods in 10 families. It is estimated that about 125 species are to be added in chapter F, the final chapter.
The Arcidae is by far the largest family in the pelecypods so far studied : 30 species in six genera. The genus Anadara is the largest in that family : 25 species, representing the subgenera Hawaiarca?, Rasia, Tosarca, Grandiarca, Potiarca, and Cunearca. Potiarca, based on a living western Pacific species, is adopted for many American species heretofore assigned to Cunearca.
Eighteen of the 27 additional gastropods were found at a new locality in the late Eocene part of the Gatuncillo formation. They 'are assigned to 16 genera, 14 of which are not represented at other Gatuncillo localities. The genera include Faunus, Turnpanotonos, and Bezaneonia, which are rare in America, and the rare endemic American genus Harrisianella.
The marine member of the Bohio (?) formation is now assigned to the late Eocene, instead of late Eocene or early Oligocene—the only change in age assignment. Eocene affinities are especially strengthened by the presence of Samanoetia samanensis and Volvariella?, if indeed the unnamed species represents that genus, as seems likely. Both the marine member of the Bohio( ?) and the late Oligocene part of the Bohio contain early small species of Anadara, subgenus Rasia.
The fossils from the moderately deep-water facies of the late Oligocene Caimito formation include the earliest hexagonal Dentalium of the subgenus Dentalium s.s., from the American mainland, and a widespread and abundant species of the essentially deep-water subgenus Fissidentalium.
Anadara chiriquiensis chiriquiensis, a relatively small form of the subgenus Grandiarca that is widely distributed in the Miocene Caribbean province, occurs in the Culebra formation. For the most part it indicates brackish water.
Among the fossils from the La Boca formation proper, Cyphoma aff. C. intermedia is the earliest representative of an endemic American genus, and Isognomon mimeticus, a remarkable, narrowly mytiliform species is the type of the new subgenus Mimonion. Both the Culebra and La Boca, both of early Miocene age, contain predecessors of Gatun species.
As in other chapters, the largest number of species is from the middle Miocene Gatun formation: 50 species. Bailya crossata is the first Tertiary species of the genus from the Caribbean region, and the earliest now known. A bizarre, incomplete gastropod is described as xancid?, genus?. The Gatun contains 13 of the 24 species of Anadara and half of the 12 species of the subgenus Rasia of that genus. In consideration of two battered and worn specimens of a large form of the subgenus Grandiarca, identified as Anadara grandis patricia?, the similar Tertiary forms in the Caribbean region are reviewed and divided into a brackish-water group and a marine group. The Gatun fauna now totals some 330 species.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp306E","usgsCitation":"Woodring, W., 1973, Geology and paleontology of Canal Zone and adjoining parts of Panama: Description of Tertiary mollusks (additions to gastropods, scaphopods, pelecypods Nuculidae to Malleidae): U.S. Geological Survey Professional Paper 306, iii, 86 p., https://doi.org/10.3133/pp306E.","productDescription":"iii, 86 p.","startPage":"453","endPage":"539","numberOfPages":"128","costCenters":[],"links":[{"id":120014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0306e/report-thumb.jpg"},{"id":66572,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0306e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Panama","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843e6","contributors":{"authors":[{"text":"Woodring, W. P.","contributorId":48230,"corporation":false,"usgs":true,"family":"Woodring","given":"W. P.","affiliations":[],"preferred":false,"id":220980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38802,"text":"pp562K - 1973 - An experimental study of heavy-mineral segregation under alluvial-flow conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp562K","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":"562","chapter":"K","title":"An experimental study of heavy-mineral segregation under alluvial-flow conditions","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sediment transport in alluvial channels","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp562K","usgsCitation":"Brady, L.L., and Jobson, H., 1973, An experimental study of heavy-mineral segregation under alluvial-flow conditions: U.S. Geological Survey Professional Paper 562, 37 p., https://doi.org/10.3133/pp562K.","productDescription":"37 p.","costCenters":[],"links":[{"id":120536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0562k/report-thumb.jpg"},{"id":65678,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0562k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6847c0","contributors":{"authors":[{"text":"Brady, L. L.","contributorId":33711,"corporation":false,"usgs":true,"family":"Brady","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jobson, H.E.","contributorId":44952,"corporation":false,"usgs":true,"family":"Jobson","given":"H.E.","affiliations":[],"preferred":false,"id":220469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23031,"text":"ofr7371 - 1973 - Selected hydrologic data from the Piceance Basin, Colorado","interactions":[{"subject":{"id":23031,"text":"ofr7371 - 1973 - Selected hydrologic data from the Piceance Basin, Colorado","indexId":"ofr7371","publicationYear":"1973","noYear":false,"title":"Selected hydrologic data from the Piceance Basin, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70043691,"text":"70043691 - 1974 - Hydrologic Data from the Piceance Basin, Colorado","indexId":"70043691","publicationYear":"1974","noYear":false,"title":"Hydrologic Data from the Piceance Basin, Colorado"},"id":1}],"supersededBy":{"id":70043691,"text":"70043691 - 1974 - Hydrologic Data from the Piceance Basin, Colorado","indexId":"70043691","publicationYear":"1974","noYear":false,"title":"Hydrologic Data from the Piceance Basin, Colorado"},"lastModifiedDate":"2013-02-18T20:20:45","indexId":"ofr7371","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-71","title":"Selected hydrologic data from the Piceance Basin, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey, Colorado District,","doi":"10.3133/ofr7371","issn":"0094-9140","usgsCitation":"Ficke, J.F., Weeks, J., and Welder, F., 1973, Selected hydrologic data from the Piceance Basin, Colorado: U.S. Geological Survey Open-File Report 73-71, xiv, 193 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr7371.","productDescription":"xiv, 193 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":155141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f89a8","contributors":{"authors":[{"text":"Ficke, J. F.","contributorId":106524,"corporation":false,"usgs":true,"family":"Ficke","given":"J.","middleInitial":"F.","affiliations":[],"preferred":false,"id":189319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, J.B.","contributorId":61426,"corporation":false,"usgs":true,"family":"Weeks","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":189317,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welder, F.A.","contributorId":104878,"corporation":false,"usgs":true,"family":"Welder","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":189318,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2406,"text":"wsp2006 - 1973 - The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin","interactions":[],"lastModifiedDate":"2022-12-01T19:23:30.261504","indexId":"wsp2006","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":"2006","title":"The Pine-Popple River basin — Hydrology of a wild river area, northeastern Wisconsin","docAbstract":"The Pine and Popple Rivers, virtually unaltered by man, flow through a semiprimitive area of forests, lakes, and glacial hills. White-water streams, natural lakes, fish and animal life, and abundant vegetation contribute to the unique recreational and aesthetic characteristics of the area. Resource planning or development should recognize the interrelationships within the hydrologic system and the possible effects of water and land-use changes upon the wild nature of the area. The basin covers about 563 square miles in northeastern Wisconsin. Swamps and wetlands cover nearly 110 square miles, and the 70 lakes cover about 11 square miles. The undulating topography is formed by glacial deposits overlying an irregular, resistant surface of bedrock. An annual average of 30 inches of precipitation, highest from late spring to early autumn, falls on the basin. Of this amount, evapotranspiration, highest in mid summer and late summer, averages 19 inches; the remaining 11 inches is runoff, which is highest in spring and early summer. Ground water from the glacial drift is the source of water for the minor withdrawal use in the basin. Ground-water movement is to streams and lakes and regionally follows the slope of topography and the bedrock surface, which is generally west to east. Ground water is of good quality, although locally high in iron. The major uses of water are for recreation and power generation. Domestic use is slight. No water is withdrawn from lakes or streams, and no sewage or industrial wastes are added to lakes or streams. Most of the flow of the Pine River is used for power generation. The main stems of the Pine and Popple Rivers contain 114 canoeable miles, of which 95 percent is without such major obstructions as falls or large rapids. In general streams support cold-water fish, and lakes support warm-water fish. Trout is the principal stream and game fish in the basin. The basin has no significant water problems. Future development between the Pine River power plant and the mouth of the Pine River should have little effect on the western two-thirds of the basin, already largely protected by public ownership or development planning agreements.
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