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The papers were presented by members of the U.S. Geological Survey at the International Seminar on Organization and Operation of Hydrologic Services, Ottawa, Canada, July 15-16, 1976, sponsored by the World Meteorological Organization. The first paper, ' Standardization of Hydrologic Measurements, ' by George F. Smoot discusses the need for standardization of the methods and instruments used in measuring hydrologic data. The second paper, ' Use of Earth Satellites for Automation of Hydrologic Data Collection, ' by Richard W. Paulson discusses the use of inexpensive battery-operated radios to transmit realtime hydrologic data to earth satellites and back to ground receiving stations for computer processing. The third paper, ' Operation Hydrometeorological Data-Collection System for the Columbia River, ' by Nicholas A. Kallio discusses the operation of a complex water-management system for a large river basin utilizing the latest automatic telemetry and processing devices. The fourth paper, ' Storage and Retrieval of Water-Resources Data, ' by Charles R. Showen discusses the U.S. Geological Survey 's National Water Data Storage and Retrieval System (WATSTORE) and its use in processing water resources data. The final paper, ' Publication of Water Resources Data, ' by S. M. Lang and C. B. Ham discusses the requirement for publication of water-resources data to meet the needs of a widespread audience and for archival purposes. (See W78-09324 thru W78-09328) (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir756","usgsCitation":"Showen, C.R., 1978, Collection, storage, retrieval, and publication of water-resources data: U.S. Geological Survey Circular 756, v, 39 p. :ill., maps ;26 cm. , https://doi.org/10.3133/cir756.","productDescription":"v, 39 p. :ill., maps ;26 cm. ","costCenters":[],"links":[{"id":124229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0756/report-thumb.jpg"},{"id":30868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0756/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae89e","contributors":{"authors":[{"text":"Showen, C. R. (compiler)","contributorId":27430,"corporation":false,"usgs":true,"family":"Showen","given":"C.","suffix":"(compiler)","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":147619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3263,"text":"cir769 - 1978 - A theoretical basis for exploration for native copper in northern Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"769","title":"A theoretical basis for exploration for native copper in northern Wisconsin","docAbstract":"Exploration for native copper in the Keweenawan lavas of northern Wisconsin has been concentrated in areas of relatively shallow overburden that have sparse to numerous outcrops. Lack of success of this exploration suggests that if large deposits, comparable to those of northern Michigan, are present, they are more likely to be found in one or more of the large tracts that have few, if any, exposures, away from the ' copper ranges. ' A hydrologic model that may explain the mineralization of the classic native-copper district of Michigan could be helpful in suggesting that certain covered tracts are more favorable than others, and in narrowing the targets for physical exploration within these tracts. This model involves updip migration of a hydrothermal fluid of metamorphic origin, formed when ground water contained in the interstices of lava flows and conglomerate beds was carried to great depth along the axis of the Lake Superior syncline. The largest reservoirs of such buried ground water would be expected in the peripheral rather than central parts of the basins in which the lavas originally accumulated because the ratio of porous fragmental flow tops and conglomerate beds to massive basalt should increase towards the margins of a basin. Thus, the areas most promising for copper deposits should be those updip from places where the trough of the later formed Lake Superior syncline crosses the marginal parts of a lava basin. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir769","usgsCitation":"White, W., 1978, A theoretical basis for exploration for native copper in northern Wisconsin: U.S. Geological Survey Circular 769, iii, 19 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir769.","productDescription":"iii, 19 p. :ill., maps ;26 cm.","numberOfPages":"21","costCenters":[],"links":[{"id":123904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0769/report-thumb.jpg"},{"id":30257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56dc","contributors":{"authors":[{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":146538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4294,"text":"cir779 - 1978 - Geologic disposal of high-level radioactive wastes; earth-science perspectives","interactions":[],"lastModifiedDate":"2017-07-07T08:35:48","indexId":"cir779","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"779","title":"Geologic disposal of high-level radioactive wastes; earth-science perspectives","docAbstract":"No abstract available
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir779","usgsCitation":"Bredehoeft, J., England, A.W., Stewart, D.B., Trask, N., and Winograd, I., 1978, Geologic disposal of high-level radioactive wastes; earth-science perspectives: U.S. Geological Survey Circular 779, v, 15 p. :ill. ;26 cm., https://doi.org/10.3133/cir779.","productDescription":"v, 15 p. :ill. ;26 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":31405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0779/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0779/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a637e","contributors":{"authors":[{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":148747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"England, A. 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B.","contributorId":41809,"corporation":false,"usgs":true,"family":"Stewart","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":148749,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":148748,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winograd, I.J.","contributorId":10408,"corporation":false,"usgs":true,"family":"Winograd","given":"I.J.","affiliations":[],"preferred":false,"id":148746,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":4920,"text":"pp1081 - 1978 - Rock pushing and sampling under rocks on Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"pp1081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1081","title":"Rock pushing and sampling under rocks on Mars","docAbstract":"Viking Lander 2 acquired samples on Mars from beneath two rocks, where living organisms and organic molecules would be protected from ultraviolet radiation. Selection of rocks to be moved was based on scientific and engineering considerations, including rock size, rock shape, burial depth, and location in a sample field. Rock locations and topography were established using the computerized interactive video-stereophotogrammetric system and plotted on vertical profiles and in plan view. Sampler commands were developed and tested on Earth using a full-size lander and surface mock-up. The use of power by the sampler motor correlates with rock movements, which were by plowing, skidding, and rolling. \r\n\r\nProvenance of the samples was determined by measurements and interpretation of pictures and positions of the sampler arm. Analytical results demonstrate that the samples were, in fact, from beneath the rocks. Results from the Gas Chromatograph-Mass Spectrometer of the Molecular Analysis experiment and the Gas Exchange instrument of the Biology experiment indicate that more adsorbed(?) water occurs in samples under rocks than in samples exposed to the sun. This is consistent with terrestrial arid environments, where more moisture occurs in near-surface soil un- der rocks than in surrounding soil because the net heat flow is toward the soil beneath the rock and the rock cap inhibits evaporation. Inorganic analyses show that samples of soil from under the rocks have significantly less iron than soil exposed to the sun. \r\n\r\nThe scientific significance of analyses of samples under the rocks is only partly evaluated, but some facts are clear. Detectable quantities of martian organic molecules were not found in the sample from under a rock by the Molecular Analysis experiment. The Biology experiments did not find definitive evidence for Earth-like living organisms in their sample. Significant amounts of adsorbed water may be present in the martian regolith. The response of the soil from under a rock to the aqueous nutrient in the Gas Exchange instrument indicates that adsorbed water and hydrates play an important role in the oxidation potential of the soil. The rock surfaces are strong, because they did not scratch, chip or spall when the sampler pushed them. Fresh surfaces of soil and the undersides of rocks were exposed so that they could be imaged in color. A ledge of soil adhered to one rock that tilted, showing that a crust forms near the surface of Mars. The reason for low amounts of iron in the sampIes from under the rocks is not known at this time.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1081","usgsCitation":"Moore, H., Liebes, S., Crouch, D., and Clark, L., 1978, Rock pushing and sampling under rocks on Mars: U.S. Geological Survey Professional Paper 1081, 21 p., https://doi.org/10.3133/pp1081.","productDescription":"21 p.","costCenters":[],"links":[{"id":124996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1081/report-thumb.jpg"},{"id":31784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b436c","contributors":{"authors":[{"text":"Moore, H. J.","contributorId":71962,"corporation":false,"usgs":true,"family":"Moore","given":"H. J.","affiliations":[],"preferred":false,"id":150116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liebes, S. 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1978 - Geologic map of the Lebanon West quadrangle, Marion County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq1509","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1509","title":"Geologic map of the Lebanon West quadrangle, Marion County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1509","usgsCitation":"Moore, S.L., 1978, Geologic map of the Lebanon West quadrangle, Marion County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1509, 1 map : col. ;58 x 46 cm. on sheet 79 x 92 cm., https://doi.org/10.3133/gq1509.","productDescription":"1 map : col. ;58 x 46 cm. on sheet 79 x 92 cm.","costCenters":[],"links":[{"id":102610,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1059.htm","linkFileType":{"id":5,"text":"html"},"description":"1059"},{"id":248596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1509/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":253740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1509/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.36749999999999,37.5 ], [ -85.36749999999999,37.6175 ], [ -85.25,37.6175 ], [ -85.25,37.5 ], [ -85.36749999999999,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a47c","contributors":{"authors":[{"text":"Moore, Samuel L.","contributorId":88727,"corporation":false,"usgs":true,"family":"Moore","given":"Samuel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":267365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61810,"text":"gq1417 - 1978 - Geologic map of the La Center quadrangle, Ballard and McCracken Counties, Kentucky","interactions":[{"subject":{"id":46832,"text":"ofr78134 - 1978 - Geologic map of the La Center Quadrangle, Ballard and McCracken counties, Kentucky","indexId":"ofr78134","publicationYear":"1978","noYear":false,"title":"Geologic map of the La Center Quadrangle, Ballard and McCracken counties, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":61810,"text":"gq1417 - 1978 - Geologic map of the La Center quadrangle, Ballard and McCracken Counties, Kentucky","indexId":"gq1417","publicationYear":"1978","noYear":false,"title":"Geologic map of the La Center quadrangle, Ballard and McCracken Counties, Kentucky"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq1417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1417","title":"Geologic map of the La Center quadrangle, Ballard and McCracken Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1417","usgsCitation":"Swanson, R.W., 1978, Geologic map of the La Center quadrangle, Ballard and McCracken Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1417, 1 map : col. ;58 x 47 cm. on sheet 75 x 94 cm. --, https://doi.org/10.3133/gq1417.","productDescription":"1 map : col. ;58 x 47 cm. on sheet 75 x 94 cm. --","costCenters":[],"links":[{"id":107841,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10951.htm","linkFileType":{"id":5,"text":"html"},"description":"10951"},{"id":248101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1417/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":252761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1417/report-thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,37 ], [ -89,37.1175 ], [ -88.86749999999999,37.1175 ], [ -88.86749999999999,37 ], [ -89,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69729b","contributors":{"authors":[{"text":"Swanson, Roger Warren","contributorId":13946,"corporation":false,"usgs":true,"family":"Swanson","given":"Roger","email":"","middleInitial":"Warren","affiliations":[],"preferred":false,"id":266394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61809,"text":"gq1485 - 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