{"pageNumber":"1514","pageRowStart":"37825","pageSize":"25","recordCount":41032,"records":[{"id":5210310,"text":"5210310 - 1983 - Nutrition and disease relationships that may serve as models for feeding oiled birds","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"5210310","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Nutrition and disease relationships that may serve as models for feeding oiled birds","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Effects of Oil on Birds: A Multi-discipline Symposium","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Tri-State Bird Rescue and Research, Inc.","publisherLocation":"Wilmington, Delaware","usgsCitation":"Serafin, J.A., 1983, Nutrition and disease relationships that may serve as models for feeding oiled birds, chap. of The Effects of Oil on Birds: A Multi-discipline Symposium, p. 167-178.","productDescription":"iv, 178","startPage":"167","endPage":"178","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696690","contributors":{"editors":[{"text":"Rosie, D.","contributorId":111324,"corporation":false,"usgs":true,"family":"Rosie","given":"D.","affiliations":[],"preferred":false,"id":506261,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Barnes, S.N.","contributorId":112903,"corporation":false,"usgs":true,"family":"Barnes","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":506262,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Serafin, John A.","contributorId":11292,"corporation":false,"usgs":true,"family":"Serafin","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":328178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210332,"text":"5210332 - 1983 - Effects of oil on avian reproduction: A review and discussion","interactions":[],"lastModifiedDate":"2012-02-02T00:15:20","indexId":"5210332","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Effects of oil on avian reproduction: A review and discussion","docAbstract":"Oil pollution is a highly visible form of environmental contamination that affects avian reproduction in a variety of ways. Plumage oiling causes widespread and locally severe mortality of adult birds. Egg oiling can be a serious hazard for bird embryos but only a few field observationons of this have been reported. Oil ingestion seldom kills birds directly but it causes sublethal change~ in the bodily functions and behavior of adults and nestlings. Studies of the effects of oil on avian reproduction have produced varied and, in ingestion studies, sometimes conflicting results because of inconsistent experimental design and the use of different test species and types of oil. Field experimentation with the sublethal effects of ingested oil on avian reproduction has been limited. Simulation modelling of seabird populations has shown that (l) an occasional decrease in survival of breeding adults will have a greater impact on seabird populations than an occasional decrease in reproductive success, and (2) populations of long-lived seabirds with low reproductive potential have great difficulty recovering from high one-time mortality when experiencing even small sustained annual decreases in either natality or breeding adult survival. The impact of oil-related decreases in survival or reproduction will be more noticeable at the local or colony level than at the regional or species level. Immigration, surplus breeders, and possible compensatory changes in natality and mortality resulting from population reductions usually prevent local population reductions from lasting very long (unless the species is rare or at the edge of its range). A study of west European seabird populations indicates that the natural annual mortality of the region greatly exceeds the annual mortality due to plumage oiling; effects of oil ingestion and egg oiling were not measured but were thought to be less than the mortality from plu~age oiling. Oil-related mortality, even if in addition to expected mortality, would not have a detectable impact on regional populations if environmental conditions were favorable (increased natality, decreased mortality) for the birds.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Effects of Oil on Birds: Physiological Research, Clinical Applications and Rehabilitation. A Multi-discipline Symposium","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Tri-State Bird Rescue and Research, Inc.","publisherLocation":"Wilmington, Delaware","collaboration":"OCLC: 11500897","usgsCitation":"Albers, P., 1983, Effects of oil on avian reproduction: A review and discussion, chap. of The Effects of Oil on Birds: Physiological Research, Clinical Applications and Rehabilitation. A Multi-discipline Symposium, p. 78-96.","productDescription":"iv, 178","startPage":"78","endPage":"96","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611ae4","contributors":{"editors":[{"text":"Rosie, Don","contributorId":114014,"corporation":false,"usgs":true,"family":"Rosie","given":"Don","email":"","affiliations":[],"preferred":false,"id":506295,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Barnes, Stephen N.","contributorId":111980,"corporation":false,"usgs":true,"family":"Barnes","given":"Stephen","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":506294,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":328215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210308,"text":"5210308 - 1983 - Environmental contaminants in tissues, foods, and feces of California condors","interactions":[],"lastModifiedDate":"2012-02-02T00:15:13","indexId":"5210308","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Environmental contaminants in tissues, foods, and feces of California condors","docAbstract":"Two wild California Condors contained moderate to high levels of DDE in their tissues. The levels found could be high enough to cause reproductive problems in adult condors, if the assumption is made that condors are as susceptible to DDE as many other species of birds of prey. Other organochlorines occurred at low levels and probably were not high enough to cause deleterious effects. Metal residues in tissues of one bird were generally low except for copper in liver and lead in bone. Normal background levels of these metals in cathartids are unknown, making interpretation of the results difficult. Organochlorine residues in biopsy samples from a captive condor were low and probably would not have an adverse effect on reproduction if the bird were used for captive breeding. Organochlorines were not detected in food items used in the supplemental feeding program, and mercury and lead residues in these items were generally low. Information is needed on current contaminant levels in natural condor prey throughout the condor range.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Vulture Biology and Management","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"University of California Press","publisherLocation":"Berkeley and Los Angeles","usgsCitation":"Wiemeyer, S.N., Krynitsky, A.J., and Wilbur, S., 1983, Environmental contaminants in tissues, foods, and feces of California condors, chap. of Vulture Biology and Management, p. 427-439.","productDescription":"xxii, 550","startPage":"427","endPage":"439","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602418","contributors":{"editors":[{"text":"Wilbur, Sanford R.","contributorId":34188,"corporation":false,"usgs":true,"family":"Wilbur","given":"Sanford","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":506259,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Jackson, Jerome A.","contributorId":112944,"corporation":false,"usgs":true,"family":"Jackson","given":"Jerome","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":506260,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":328176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krynitsky, A. J.","contributorId":73954,"corporation":false,"usgs":true,"family":"Krynitsky","given":"A.","middleInitial":"J.","affiliations":[],"preferred":false,"id":328175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilbur, S.R.","contributorId":53908,"corporation":false,"usgs":true,"family":"Wilbur","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":328174,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5200140,"text":"5200140 - 1983 - Effects of the insecticide, orthene, on unconfined populations of the meadow vole (Microtus pennsylvanicus). I. Capture/recapture procedures; II. Residues and cholinesterase inhibition","interactions":[],"lastModifiedDate":"2012-02-02T00:15:18","indexId":"5200140","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1983","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Effects of the insecticide, orthene, on unconfined populations of the meadow vole (Microtus pennsylvanicus). I. Capture/recapture procedures; II. Residues and cholinesterase inhibition","docAbstract":"In 1982 and 1983. the population demography of M. pennsylvanicus was not altered significantly by single or double applications of Orthene. Although inconsistencies in population size, survival, and recruitment were not explained by differences between control and experimental grids in breeding, emigration, interspecific competition, or pesticide-induced mortality, there may have been fundamental microhabitat differences between grids in both years, and this is supported by prespray data. Slight differences between grids may also reflect the random error associated with the models used to estimate parameters. No evidence was found to indicate an effect on relative weight change or average distances moved. The level of brain AChE in 1982 during sequential days after spraying was significantly lower than control levels. However, this inhibition was not enough to cause direct mortality. Recovery of brain AChe was gradual, probably reflecting continual re-exposure through the diet. Acephate and methamidophos residues were present in the vegetation collected from sprayed areas immediately following treatment, but were reduced or absent after 8 days. AChE inhibition in 1982 and 1983 extended beyond the disappearance of residues in the vegetation. Residues were only present in the G.l. tracts of voles collected immediately following treatment due to rapid metabolism and excretion. Levels in the vegetation and G.l. tracts in 1982 and 1983 were well below the rat oral LD50 of acephate. It is concluded that Orthene applied at recommended levels, in a single or double treatment, should not affect unconfined populations of M. pennsylvanicus in Maryland old-field habitats. Furthermore, this study confirms this method as a sensitive means to determine the overall impact of insecticides on wildlife populations. However, caution must be exercised to insure that all control and experimental areas are closely scrutinized for habitat differences.","language":"English","publisher":"M.S. thesis, University of Maryland.","publisherLocation":"College Park, MD","usgsCitation":"Jett, D.A., 1983, Effects of the insecticide, orthene, on unconfined populations of the meadow vole (Microtus pennsylvanicus). I. Capture/recapture procedures; II. Residues and cholinesterase inhibition, viii, 83.","productDescription":"viii, 83","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6101e7","contributors":{"authors":[{"text":"Jett, David A.","contributorId":66366,"corporation":false,"usgs":false,"family":"Jett","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":327067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011211,"text":"70011211 - 1983 - Heavy-mineral distribution in modern and ancient bay deposits, Willapa Bay, Washington, U.S.A.","interactions":[],"lastModifiedDate":"2025-07-24T15:32:22.113321","indexId":"70011211","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"Heavy-mineral distribution in modern and ancient bay deposits, Willapa Bay, Washington, U.S.A.","docAbstract":"

Analysis of heavy-mineral distribution in modern sediments of Willapa Bay, Washington, indicates a dominance of two mineralogic assemblages, one with approximately equivalent amounts of hornblende, orthopyroxene and clinopyroxene, the other dominated by clinopyroxene. The hornblende-orthopyroxene-clinopyroxene suite is derived from the Columbia River, which discharges into the ocean a short distance south of the bay. The clinopyroxene suite is restricted in modern sediments to sands in rivers flowing into the bay from the east. The heavy-mineral distributions suggest that sand discharged from the Columbia River, borne north by longshore transport, and carried into the bay by tidal currents accounts for most of the sand within the interior of Willapa Bay.

Three heavy-mineral assemblages are present in the surrounding Pleistocene deposits; two of these are identical to the modern assemblages described above. These heavy-mineral assemblages reflect the relative influence of tidal and fluvial processes on the Late Pleistocene deposits; their relative influences are consistent with those inferred on the basis of sedimentary structures and stratigraphic relations in about two-thirds of the samples examined. The anomalies can be explained by recycling of sand from older deposits. The persistence of the two heavy-mineral assemblages suggests that the pattern of estuarine sedimentation in Late Pleistocene deposits closely resembled that of the modern bay.

The third heavy-mineral suite, dominated by epidote, occurs in a few older Pleistocene units. On the north side of the bay, the association of this suite with southwest-directed foresets in crossbedded gravel indicates derivation from the northeast, perhaps from an area of glacial outwash. The presence of this suite in ancient estuarine sands exposed on the east side of the bay suggests that input from this northerly source may have intermittently dominated bay deposition in the past.

","language":"English","publisher":"Elsevier","doi":"10.1016/0037-0738(83)90060-X","issn":"00370738","usgsCitation":"Luepke, G., and Clifton, H.E., 1983, Heavy-mineral distribution in modern and ancient bay deposits, Willapa Bay, Washington, U.S.A.: Sedimentary Geology, v. 35, no. 4, p. 233-247, https://doi.org/10.1016/0037-0738(83)90060-X.","productDescription":"15 p.","startPage":"233","endPage":"247","costCenters":[],"links":[{"id":220693,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Willapa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.0937343147915,\n 46.746899656305146\n ],\n [\n -124.0937343147915,\n 46.648829449792714\n ],\n [\n -123.82927626347455,\n 46.648829449792714\n ],\n [\n -123.82927626347455,\n 46.746899656305146\n ],\n [\n -124.0937343147915,\n 46.746899656305146\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"35","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3026e4b0c8380cd5d3ea","contributors":{"authors":[{"text":"Luepke, Gretchen","contributorId":91827,"corporation":false,"usgs":true,"family":"Luepke","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":360568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clifton, H. Edward","contributorId":46503,"corporation":false,"usgs":true,"family":"Clifton","given":"H.","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":360569,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3978,"text":"cir895B - 1983 - Digital elevation models","interactions":[],"lastModifiedDate":"2012-05-24T01:02:39","indexId":"cir895B","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1983","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":"895","chapter":"B","title":"Digital elevation models","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir895B","collaboration":"replaced by Data Users Guide 5","usgsCitation":"Elassal, A.A., and Caruso, V.M., 1983, Digital elevation models: U.S. Geological Survey Circular 895, vi, 40 p. :ill. ;27 cm., https://doi.org/10.3133/cir895B.","productDescription":"vi, 40 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":122901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0895b/report-thumb.jpg"},{"id":31063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0895b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d4b2","contributors":{"authors":[{"text":"Elassal, Atef A.","contributorId":105699,"corporation":false,"usgs":true,"family":"Elassal","given":"Atef","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caruso, Vincent M.","contributorId":80251,"corporation":false,"usgs":true,"family":"Caruso","given":"Vincent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":147939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10521,"text":"ofr83865 - 1983 - Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83865","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-865","title":"Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982","docAbstract":"Hydrologic data collected on the Great and Denbow Heaths, Maine, include precipitation, pan evaporation, air temperatures, streamflow, and ground water levels. These data were collected for a peat bog hydrology study conducted in cooperation with the Maine Geological Survey. The data network consisted of climate information from three rain gages, an evaporation pan and two maximum-minimum thermometers; surface water information from two continuous gaging stations and 19 partial record sites; groundwater information from an observation well equipped with a continuous recorder and 106 piezometers. Methods used for the collection and analyses of data included standard Survey techniques modified for the unique hydrologic environment of the study area. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83865","usgsCitation":"Nichols, W.J., 1983, Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982: U.S. Geological Survey Open-File Report 83-865, 34 p. :maps ;28 cm., https://doi.org/10.3133/ofr83865.","productDescription":"34 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0865/report-thumb.jpg"},{"id":38370,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c79f","contributors":{"authors":[{"text":"Nichols, Wallace J.","contributorId":81106,"corporation":false,"usgs":false,"family":"Nichols","given":"Wallace","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7494,"text":"ofr83390 - 1983 - Saudi Arabian seismic deep-refraction profiles; final project report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr83390","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-390","title":"Saudi Arabian seismic deep-refraction profiles; final project report","docAbstract":"In February 1978 a seismic deep-refraction profile was recorded by the U.S. Geological Survey along a 1000-km line across the Arabian Shield in western Saudi Arabia. The line begins in Mesozoic cover rocks near Riyadh on the Arabian Platform, leads southwesterly across three major Precambrian tectonic provinces, traverses Cenozoic rocks of the coastal plain near Jizan (Tihamat-Asir), and terminates at the outer edge of the Farasan Bank in the southern Red Sea. More than 500 surveyed recording sites were occupied, including 19 in the Farasan Islands. Six shot points were used: five on land, with most charges placed below the water table in drill holes, and one at sea, with charges placed on the sea floor and detonated from a ship. Slightly more than 61 metric tons of explosives were used in 19 discrete firings. \r\n\r\nSeismic energy was recorded by 100 newly-developed portable seismic stations deployed in approximately 200 km-long arrays for each firing. Each station consisted of a standard 2-Hz vertical component geophone coupled to a self-contained analog recording instrument equipped with a magnetic-tape cassette.\r\n\r\nIn this final report, we fully document the field and data-processing procedures and present the final seismogram data set as both a digital magnetic tape and as record sections for each shot point. Record sections include a normalized set of seismograms, reduced at 6 km/s, and a true-amplitude set, reduced at 8 km/s, which have been adjusted for amplifier gain, individual shot size, and distance from the shot point.\r\n\r\nAppendices give recorder station and shot information, digital data set descriptions, computer program listings, arrival times used in the interpretation, and a bibliography of reports published as a result of this project.\r\n\r\nWe used two-dimensional ray-tracing techniques in the data analysis, and our interpretation is based primarily on horizontally layered models. The Arabian Shield is composed, to first-order, of two layers, each about 20 km thick, with average velocities of 6.3 km/s and 7.0 km/s, respectively. At the western shield margin the crust thins to less than 20 km total thickness, beyond which the Red Sea shelf and coastal plain are interpreted to be underlain by oceanic crust.\r\n\r\nA major crustal lateral velocity inhomogeneity northeast of Sabhah in the Shammar Tectonic Province is interpreted as the suture zone of two crustal blocks of different composition. Several high-velocity anomalies in the upper crust correlate with mapped gneissic dome structures. Two intra-crustal reflectors at13 km depth are interpreted as the tops of mafic intrusives.\r\n\r\nThe Mohorovicic discontinuity beneath the shield varies from 43 km depth in the northeast with 8.2 km/s mantle velocity to 38 km depth in the southwest with 8.0 km/s mantle velocity. Two velocity discontinuities are identified in the upper mantle, at 59 and 70 km depth.\r\n\r\nWe suggest further work, including refined analyses of the data employing filtering and synthetic seismogram techniques, as well as consideration of attenuation properties. Extension of the seismic refraction profile to the Arabian Gulf and some short profiles perpendicular to the existing profile would be fruitful areas for future field work.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83390","usgsCitation":"Healy, J.H., Mooney, W.D., Blank, H., Gettings, M.E., Kohler, W., Lamson, R., and Leone, L., 1983, Saudi Arabian seismic deep-refraction profiles; final project report: U.S. Geological Survey Open-File Report 83-390, 434 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83390.","productDescription":"434 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0390/report-thumb.jpg"},{"id":34937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34938,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34939,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34940,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34941,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34942,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34943,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34944,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34945,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0390/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb74","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mooney, W. D.","contributorId":72376,"corporation":false,"usgs":true,"family":"Mooney","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":155881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blank, H. R.","contributorId":50516,"corporation":false,"usgs":true,"family":"Blank","given":"H. R.","affiliations":[],"preferred":false,"id":155878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155876,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kohler, W.M.","contributorId":62999,"corporation":false,"usgs":true,"family":"Kohler","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":155879,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lamson, R.J.","contributorId":86762,"corporation":false,"usgs":true,"family":"Lamson","given":"R.J.","affiliations":[],"preferred":false,"id":155882,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leone, L.E.","contributorId":71969,"corporation":false,"usgs":true,"family":"Leone","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":155880,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":7423,"text":"ofr83486 - 1983 - Preliminary assessment of the geochemistry and mineral favorability of the postorogenic granites of the southeastern Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-16T16:03:09","indexId":"ofr83486","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-486","title":"Preliminary assessment of the geochemistry and mineral favorability of the postorogenic granites of the southeastern Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"

Chemical analyses of samples for 19 postorogenic plutons from the southeastern Arabian Shield show that these rocks have average potassium/rubidium ratios (162) and average rubidium/strontium ratios (11.8) characteristic of highly evolved granites. Most of the analyzed samples are peraluminous. Three plutons are physically similar in terms of shape and megascopic textural zonation to peralkaline complexes in the northeastern part of the Shield, but none of the samples from these plutons is peralkaline. However, these plutons do contain the least-evolved samples.

\n

Zinc, yttrium, uranium, thorium, and possibly copper, each occur in anomalously high concentrations in at least one pluton relative to contents typically cited for granite. The average regional concentrations of copper and zinc are anomalously high. These facts suggest at least a moderate potential for mineralization in the southeastern part of the Shield. Good correlations (r of 0.5 to 0.8) between uranium, thorium, yttrium, and rubidium and an excellent correlation (r=0.98) between uranium and radium-equivalent uranium suggest that secondary deposits of these elements are unlikely and that magmatic deposits, especially of a pegmatitic nature, are more likely.

\n

Concentrations of some major elements and several trace elements covary with sample location as measured by latitude and longitude. This fact is interpreted to reflect regional variations in the protolith that have been proposed on the basis of lead isotopic data. The chemical variations suggest a largely oceanic crustal component for granites in the southwestern part of the southeastern Shield and a largely continental crustal component to the northeast.

\n

Further quantitative analysis is recommended to verify and accurately delineate anomalous concentrations of trace elements. Trend surface analysis of all available data for postorogenic granites from the eastern Arabian Shield is suggested as a method for testing regional variations in the protolith that might control locations of highly favorable areas of ore deposition.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83486","usgsCitation":"Stuckless, J.S., VanTrump, G., Christiansen, E.H., Bush, C.A., Bunker, C.M., and Bartel, A., 1983, Preliminary assessment of the geochemistry and mineral favorability of the postorogenic granites of the southeastern Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-486, Report: ii, 44 p., ill.; maps: 28 cm., https://doi.org/10.3133/ofr83486.","productDescription":"Report: ii, 44 p., ill.; maps: 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":140460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0486/report-thumb.jpg"},{"id":34835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 42.5,\n 17\n ],\n [\n 42.5,\n 24\n ],\n [\n 45.5,\n 24\n ],\n [\n 45.5,\n 17\n ],\n [\n 42.5,\n 17\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6695b7","contributors":{"authors":[{"text":"Stuckless, John S. 0000-0002-7536-0444 jstuckless@usgs.gov","orcid":"https://orcid.org/0000-0002-7536-0444","contributorId":4974,"corporation":false,"usgs":true,"family":"Stuckless","given":"John","email":"jstuckless@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":155549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanTrump, G.","contributorId":95869,"corporation":false,"usgs":true,"family":"VanTrump","given":"G.","affiliations":[],"preferred":false,"id":155554,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christiansen, E. H.","contributorId":65077,"corporation":false,"usgs":true,"family":"Christiansen","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155552,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bush, C. A.","contributorId":43344,"corporation":false,"usgs":true,"family":"Bush","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155551,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bunker, C. M.","contributorId":75138,"corporation":false,"usgs":true,"family":"Bunker","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155553,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bartel, A.J.","contributorId":34508,"corporation":false,"usgs":true,"family":"Bartel","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":155550,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":7074,"text":"ofr83638 - 1983 - Crustal structure of southwestern Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr83638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-638","title":"Crustal structure of southwestern Saudi Arabia","docAbstract":"The southwestern Arabian Shield is composed of uplifted Proterozoic metamorphic and plutonic rocks. The Shield is bordered on the southwest by Cenozoic sedimentary and igneous rocks of the Red Sea paar and on the east by the Arabian Platform, an area of basin sedimentation throughout Phanerozoic time. The Shield appears to have been formed by successive episodes of island arc volcanism and sea-floor spreading, followed by several cycles of compressive tectonism and metamorphism. An interpretation and synthesis of a deep-refraction seismic profile from the Riyadh area to the Farasan Islands, and regional gravity, aeromagnetic, heat flow, and surface geologic data have yielded a self-consistent regional-scale model of the crust and upper mantle for this area. \r\n\r\nThe model consists of two 20 km-thick layers of crust with an average compressional wave velocity in the upper crust of about 6.3 km/s and an average velocity in the lower. crust of about 7.0 km/s. This crust thins abruptly to less than 20 km near the southwestern end of the profile where Precambrian outcrops abut the Cenozoic rocks and to 8 km beneath the Farasan Islands. The data over the coastal plain and Red Sea shelf areas are fit satisfactorily by an oceanic crustal model. A major lateral velocity inhomogeneity in the crust is inferred about 25 km northeast of Sabhah and is supported by surface geologic evidence. \r\n\r\nThe major velocity discontinuities occur at about the same depth across the entire Shield and are interpreted to indicate horizontal metamorphic stratification of the Precambrian crust. Several lateral inhomogenities in both the upper and lower .crust of the . Shield are interpreted, to indicate bulk compositional variations. \r\n\r\nThe subcrustal portion of the model is composed of a hot, low-density lithosphere beneath the Red Sea which is systematically cooler and denser to the northeast. This model provides a mechanism which explains the observed topographic uplift, regional gravity pattern, heat flow, and mantle compressional wave velocities. Such a lithosphere could be produced by upwelling of hot asthenosphere beneath the Red Sea which then flows laterally beneath the lithosphere of the Arabian Plate.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83638","usgsCitation":"Gettings, M.E., Blank, H., Mooney, W.D., and Healy, J.H., 1983, Crustal structure of southwestern Saudi Arabia: U.S. Geological Survey Open-File Report 83-638, ii, 55 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83638.","productDescription":"ii, 55 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0638/report-thumb.jpg"},{"id":34400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f432","contributors":{"authors":[{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":154183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blank, H. R.","contributorId":50516,"corporation":false,"usgs":true,"family":"Blank","given":"H. R.","affiliations":[],"preferred":false,"id":154185,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mooney, W. D.","contributorId":72376,"corporation":false,"usgs":true,"family":"Mooney","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":154186,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":154184,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11303,"text":"ofr8385 - 1983 - A practical, low-noise coil system for magnetotellurics","interactions":[],"lastModifiedDate":"2016-02-08T11:23:36","indexId":"ofr8385","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-85","title":"A practical, low-noise coil system for magnetotellurics","docAbstract":"

Magnetotellurics is a geophysical technique which was developed by Cagnaird (1953) and Tikhonov (1950) and later refined by other scientists worldwide. The technique is a method of electromagnetic sounding of the Earth and is based upon the skin depth effect in conductive media. The electric and magnetic fields arising from natural sources are measured at the surface of the earth over broad frequency bands. An excellent review of the technique is provided in the paper by Vozoff (1972). The sources of the natural fields are found in two basic mechanisms. At frequencies above a few hertz, most of the energy arises from lightning in thunderstorm belts around the equatorial regions. This energy is propagated in a wave-guide formed by the earthionospheric cavity. Energy levels are higher at fundamental modes for this cavity, but sufficient energy exists over most of the audio range to be useful for sounding at these frequencies, in which case the technique is generally referred to as audio-magnetotellurics or AMT. At frequencies lower than audio, and in general below 1 Hz, the source of naturally occuring electromagnetic energy is found in ionospheric currents. Current systems flowing in the ionosphere generate EM waves which can be used in sounding of the earth. These fields generate a relatively complete spectrum of electromagnetic energy that extends from around 1 Hz to periods of one day. Figure 1 shows an amplitude spectrum characteristic of both the ionospheric and lightning sources, covering a frequency range from 0.0001 Hz to 1000 Hz. It can be seen that there is a minimum in signal levels that occurs at about 1 Hz, in the gap between the two sources, and that signal level increases with a decrease in frequency.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8385","usgsCitation":"Stanley, W., and Tinkler, R.D., 1983, A practical, low-noise coil system for magnetotellurics: U.S. Geological Survey Open-File Report 83-85, 36 p., https://doi.org/10.3133/ofr8385.","productDescription":"36 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":39103,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0085/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0085/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab5fd","contributors":{"authors":[{"text":"Stanley, William D.","contributorId":23274,"corporation":false,"usgs":true,"family":"Stanley","given":"William D.","affiliations":[],"preferred":false,"id":162900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinkler, Richard D.","contributorId":30628,"corporation":false,"usgs":true,"family":"Tinkler","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":162899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10520,"text":"ofr83866 - 1983 - Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1980 through September 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83866","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-866","title":"Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1980 through September 1981","docAbstract":"Hydrologic data collected on the Great and Denbow Heaths, Maine, include precipitation, pan evaporation, air temperatures, streamflow, groundwater levels, and water quality constituents. These data were collected for a peat bog hydrology study conducted in cooperation with the Maine Geological Survey. The data network consisted of climate information from three rain gages, an evaporation pan, and two maximum-minimum thermometers; surface water information from two continuous gaging stations and 19 partial record sites; groundwater information from an observation well equipped with a continuous recorder and 106 piezometers; and water quality information from 13 wells and seven surface water sites. Water quality constituents include: field determinations of pH, specific conductance, and temperature, and laboratory determinations of common inorganic cations and anions, trace elements, and selected organic compounds. Methods used for the collection and analyses of data included standard Survey techniques modified for the unique hydrologic environment of the study area. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83866","usgsCitation":"Nichols, W.J., Smath, J., and Adamik, J., 1983, Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1980 through September 1981: U.S. Geological Survey Open-File Report 83-866, iii, 47 p. :maps ;28 cm., https://doi.org/10.3133/ofr83866.","productDescription":"iii, 47 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0866/report-thumb.jpg"},{"id":38369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0866/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608359","contributors":{"authors":[{"text":"Nichols, Wallace J.","contributorId":81106,"corporation":false,"usgs":false,"family":"Nichols","given":"Wallace","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smath, J.A.","contributorId":15174,"corporation":false,"usgs":true,"family":"Smath","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":161533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adamik, J.T.","contributorId":55441,"corporation":false,"usgs":true,"family":"Adamik","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":161534,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3916,"text":"cir878B - 1983 - A U.S. Geological Survey Data Standard (Specifications for representation of geographic point locations for information interchange)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"cir878B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"878","chapter":"B","title":"A U.S. Geological Survey Data Standard (Specifications for representation of geographic point locations for information interchange)","docAbstract":"This standard establishes uniform formats for geographic point location data. Geographic point location refers to the use of a coordinate system to define the position of a point that may be on, above, or below the Earth's surface. It provides a means for representing these data in digital form for the purpose of interchanging information among data systems and improving clarity and accuracy of interpersonal communications. \r\n\r\nThis document is an expansion and clarification of National Bureau of Standards FIPS PUB 70, issued October 24, 1980. There are minor editorial changes, plus the following additions and modifications: \r\n\r\n(I) The representation of latitude and longitude using radian measure was added. \r\n\r\n(2) Alternate 2 for Representation of Hemispheric Information was deleted. \r\n\r\n(3) Use of the maximum precision for all numerical values was emphasized. The Alternate Representation of Precision was deleted. \r\n\r\n(4) The length of the zone representation for the State Plane Coordinate System was standardized. \r\n\r\n(5) The term altitude was substituted for elevation throughout to conform with international usage. \r\n\r\n(6) Section 3, Specifications for Altitude Data, was expanded and upgraded significantly to the same level of detail as for the \r\nhorizontal values. \r\n\r\n(7) A table delineating the coverage of Universal Transverse Mercator zones and the longitudes of the Central Meridians was added and the other tables renumbered. \r\n\r\n(8) The total length of the representation of point location data at maximum precision was standardized.","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/cir878B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, A U.S. Geological Survey Data Standard (Specifications for representation of geographic point locations for information interchange): U.S. Geological Survey Circular 878, iv, B1-B24 p. ;26 cm., https://doi.org/10.3133/cir878B.","productDescription":"iv, B1-B24 p. ;26 cm.","costCenters":[],"links":[{"id":124621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0878b/report-thumb.jpg"},{"id":31002,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0878b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd496de4b0b290850ef28a","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":528162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3513,"text":"cir899 - 1983 - Assessment of undiscovered conventionally recoverable petroleum resources of Indonesia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir899","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"899","title":"Assessment of undiscovered conventionally recoverable petroleum resources of Indonesia","docAbstract":"The estimates of undiscovered conventionally recoverable petroleum in Indonesia at probability levels of 95 percent, 5 percent, and statistical mean are for oil (in billions of barrels): 5, 35, and 16; and for gas (in trillions of cubic feet): 13, 94, and 42. \r\n\r\nIn Indonesia, petroleum occurs in five types of basins: forearc, back-arc (foreland), median, inner-arc, and downwarp into-small-ocean basins. The back-arc, median, and downwarp basins have significantly greater petroleum potential than do the fore-arc and inner-are basins. The latter two types are expected to yield only small discoveries; also, significant portions of such basins lie in water depths in excess of 1,000 m. The back-arc basins have been the most petroleum productive, but they also have been the most extensively explored. The greatest undiscovered petroleum potential is estimated to lie in the downwarp and median basins. \r\n\r\nIn Indonesia, six general types of geological settings or plays have been identified as being favorable for petroleum accumulation. They are transgressive clastic sequences, regressive clastic sequences, deltas, carbonate platforms, pinnacle reefs, and fractured igneous and volcanic rocks. The multiple-pay transgressive clastic reservoirs in the back-arc basins have produced most of Indonesia's crude oil. In several basins, carbonate platform porosity has become a primary exploration target, but each reservoir (reef, bank, or bioclastic zone) tends to be restricted in size. \r\n\r\nTypically, Indonesian oil is of medium gravity with a paraffin base and has a moderate to high pour point, a low sulfur content, and a relatively low gas to oil ratio.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir899","usgsCitation":"Riva, J.P., 1983, Assessment of undiscovered conventionally recoverable petroleum resources of Indonesia: U.S. Geological Survey Circular 899, vi, 17 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir899.","productDescription":"vi, 17 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0899/report-thumb.jpg"},{"id":30527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0899/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671ce5","contributors":{"authors":[{"text":"Riva, Joseph P.","contributorId":70747,"corporation":false,"usgs":true,"family":"Riva","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":147065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10518,"text":"ofr83217 - 1983 - Drift-mine reclamation in Big Four Hollow near Lake Hope, Ohio; a preliminary data report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-217","title":"Drift-mine reclamation in Big Four Hollow near Lake Hope, Ohio; a preliminary data report","docAbstract":"A subsurface clay dike and hydraulic seals were constructed in 1979 by the Ohio Department of Natural Resources, Division of Reclamation, to reduce acid mine drainage from an abandoned drift mine into Big Four Hollow Creek; Big Four Hollow Creek flow into Sandy Run, the major tributary to Lake Hope. A monitoring program was established in 1979 by the U.S. Geological Survey, Water Resources Division to evaluate sealing effects on surface-water and ground-water systems fo the Big Four Hollow Creek and Sandy Run area just below the mine.\r\n\r\nData were collected by private consultants in 1970-71 near the mouth of Big Four Hollow Creek (U.S. Geological Survey station (03201700). Results showed an average pH of 3.1 (calculated from mean hydrogen-ion concentration in moles per liter) and a pH range of 2.7 to 4.8. The estimated sulfate load was 1,000 pounds per day, and the estimated iron load wsa 100 pounds per day.\r\n\r\nData collected in 1979, before dike construction at this site, showed a daily mean pH range of 3.4 to 5.4 with an average of 3.7, and a daily mean specific-conductance range of 160 to 600 micromhos per centimeter at 25 degrees Celsius (?mho/cm), averaging 400. Again, the estimated sulfate load was 1,000 pounds per day, but the estimated iron load had decreased to 50 pounds per day.\r\n\r\nThe first 6 months of postconstruction data from the site in 1980 showd a daily mean pH range of 4.5 to 6.8 with an average of 4.9, and a daily mean conductance range of 175 to 405 ?mho/cm with an average of 300. The estimated sulfate load had decreased to 570 pounds per day and the iron load to 8.5 pounds per day.\r\n\r\nData collected during the first 6 months after construction indicate moderate improvement in water quality. However, acidic water is still being impounded behind the dike and seals and has not yet been flushed ou by infiltrating rain and ground water. Because the system has not yet stabilized, no interpretation or conclusive statement can be made at this time.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83217","usgsCitation":"Nichols, V.E., 1983, Drift-mine reclamation in Big Four Hollow near Lake Hope, Ohio; a preliminary data report: U.S. Geological Survey Open-File Report 83-217, v, 120 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83217.","productDescription":"v, 120 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0217/report-thumb.jpg"},{"id":38366,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d81","contributors":{"authors":[{"text":"Nichols, Vance E. vnichols@usgs.gov","contributorId":5456,"corporation":false,"usgs":true,"family":"Nichols","given":"Vance","email":"vnichols@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":161530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4226,"text":"cir759 - 1983 - The Alaska Mineral Resource Assessment Program: Guide to information contained in folio of geologic and mineral resource maps of the Philip Smith Mountains quadrangle, Alaska","interactions":[],"lastModifiedDate":"2022-10-03T21:28:54.240275","indexId":"cir759","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"759","title":"The Alaska Mineral Resource Assessment Program: Guide to information contained in folio of geologic and mineral resource maps of the Philip Smith Mountains quadrangle, Alaska","docAbstract":"The geology and mineral resources of the Philip Smith Mountains quadrangle were virtually unexplored until the investigations for oil began in northern Alaska. Construction of the Trans-Alaskan Pipeline System has now made the quadrangle accessible by road. In 1975 and 1976 a team of geologists, geochemists, and geophysicists investigated the quadrangle in order to assess its mineral resource potential. This report is a guide to the resulting folio of twelve maps that \r\ndescribe the geology, stream sediment geochemistry, aeromagnetic features, Landsat imagery, and mineral resources of the area. \r\n\r\nThe bedrock geology and aeromagnetic surveys show that mineral deposits associated with intrusive rocks are probably absent. However, the geology and geochemical anomalies do indicate the possibility of vein and strata-bound deposits of copper, lead, and zinc in the Paleozoic shale and carbonate rocks in the southern part of the quadrangle and of stratabound deposits of zinc and copper in the Permian and Mesozoic shales along the mountain front. The northwestern part of the quadrangle has a low to moderate potential for oil or gas; Mississippian carbonate rocks are the most likely reservoir. The only minerals produced to date have been construction materials.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir759","usgsCitation":"Reiser, H.N., Brosge, W., Hamilton, T.D., Singer, D., Menzie, W., Bird, K.J., Cady, J.W., Le Compte, J., and Cathrall, J.B., 1983, The Alaska Mineral Resource Assessment Program: Guide to information contained in folio of geologic and mineral resource maps of the Philip Smith Mountains quadrangle, Alaska: U.S. Geological Survey Circular 759, iii, 22 p., https://doi.org/10.3133/cir759.","productDescription":"iii, 22 p.","costCenters":[],"links":[{"id":407826,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23988.htm","linkFileType":{"id":5,"text":"html"}},{"id":31340,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0759/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0759/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Philip Smith Mountains 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 68\n ],\n [\n -147,\n 68\n ],\n [\n -147,\n 69\n ],\n [\n -150,\n 69\n ],\n [\n -150,\n 68\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683538","contributors":{"authors":[{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":148456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brosge, W. P.","contributorId":58248,"corporation":false,"usgs":true,"family":"Brosge","given":"W. P.","affiliations":[],"preferred":false,"id":148461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":148458,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Singer, D.A.","contributorId":69128,"corporation":false,"usgs":true,"family":"Singer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":148462,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Menzie, W. D. II","contributorId":76295,"corporation":false,"usgs":true,"family":"Menzie","given":"W. D.","suffix":"II","affiliations":[],"preferred":false,"id":148463,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bird, K. J.","contributorId":57824,"corporation":false,"usgs":false,"family":"Bird","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":148460,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cady, J. W.","contributorId":81892,"corporation":false,"usgs":true,"family":"Cady","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148464,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Le Compte, J. R.","contributorId":41816,"corporation":false,"usgs":true,"family":"Le Compte","given":"J. R.","affiliations":[],"preferred":false,"id":148459,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cathrall, J. B.","contributorId":29400,"corporation":false,"usgs":true,"family":"Cathrall","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":148457,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":1348,"text":"wsp2216 - 1983 - Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp2216","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"2216","title":"Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","docAbstract":"Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the Eastern United States. Logarithmic transformation and first-order differencing of the data sets were necessary to produce second-order, stationary time series and remove seasonal trends. \r\n\r\nCyclic models accounted for less than 42 percent of the variance in the water series and 31 percent in the sediment series. Analysis of the apparent oscillations of given frequencies occurring in the data indicates that frequently occurring storms can account for as much as 50 percent of the variation in sediment discharge. \r\n\r\nComponents of the frequency analysis indicate that a linear representation is reasonable for the water-sediment system. Models that incorporate lagged water discharge as input prove superior to univariate techniques in modeling and prediction of sediment discharges. The random component of the models includes errors in measurement and model hypothesis and indicates no serial correlation. An index of sediment production within or between drain-gage basins can be calculated from model parameters.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2216","usgsCitation":"Fitzgerald, M.G., and Karlinger, M.R., 1983, Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach: U.S. Geological Survey Water Supply Paper 2216, vi, 24 p. :ill., 1 map ;27 cm., https://doi.org/10.3133/wsp2216.","productDescription":"vi, 24 p. :ill., 1 map ;27 cm.","costCenters":[],"links":[{"id":137526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2216/report-thumb.jpg"},{"id":26423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2216/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65acb2","contributors":{"authors":[{"text":"Fitzgerald, Michael G.","contributorId":42942,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlinger, Michael R.","contributorId":10777,"corporation":false,"usgs":true,"family":"Karlinger","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18437,"text":"ofr83696 - 1983 - Long-range plans for hydrologic investigations in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr83696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-696","title":"Long-range plans for hydrologic investigations in New Mexico","docAbstract":"Objectives of the hydrologic-data-collection projects presented in this report include continuing to identify future data needs; conducting an analysis of the water-quality, ground-water, and surface-water observation networks; and entering all available current and historical hydrologic data into the U.S. Geological Survey Water Data Storage and Retrieval System (WATSTORE). Objectives of areal-appraisal studies include evaluating the water resources in the Gallup-Grants-Zuni-Acoma Sag area and on the eastern flank of the Sandi and Manzano Mountains in Bernalillo County. Potential projects for basin assessments include quantifying the ground-water/surface-water relationships on rivers with flows governed by compacts and an investigation of the water resources of the Estancia Basin. Projects that will assist in the evaluation of energy-related activities include describing the effects of resaturation of coal mines and of milling operations on the quality and quantity of ground and surface water. Activities that need to be undertaken to assist in addressing waste-disposal problems include the evaluation of the hydrologic factors influencing the feasibility of cleanup at the Albuquerque South Valley ' superfund ' site and the establishment of a monitoring network at the Waste Isolation Pilot Plant project near Carlsbad. Scientific methods that need to be developed include (1) the testing of analytical techniques for estimating site-specific conditions with the results of digital hydrologic models, and (2) the determination of the influence of recharge from ephemeral streams on alluvial aquifers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83696","usgsCitation":"Case, H.L., and Welder, G.E., 1983, Long-range plans for hydrologic investigations in New Mexico: U.S. Geological Survey Open-File Report 83-696, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83696.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0696/report-thumb.jpg"},{"id":47788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6352fb","contributors":{"authors":[{"text":"Case, H. L. III","contributorId":70435,"corporation":false,"usgs":true,"family":"Case","given":"H.","suffix":"III","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":179118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1329,"text":"wsp2201 - 1983 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","interactions":[{"subject":{"id":8772,"text":"ofr81911 - 1981 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","indexId":"ofr81911","publicationYear":"1981","noYear":false,"title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":1329,"text":"wsp2201 - 1983 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","indexId":"wsp2201","publicationYear":"1983","noYear":false,"title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp2201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"2201","title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","docAbstract":"The N aquifer is the main source of water in the 5,400-square-mile Black Mesa area in the Navajo and Hopi Indian Reservations in northeastern Arizona. The N aquifer consists of the Navajo Sandstone and parts of the underlying Kayenta Formation and Wingate Sandstone of Jurassic and Triassic age. Maximum saturated thickness of the aquifer is about 1,050 feet in the northwestern part of the area, and the aquifer thins to extinction to the southeast. Water is under confined conditions in the central 3,300 square miles of the area. To the east, north, and west of Black Mesa, the aquifer is exposed at the surface, and water is unconfined. The aquifer was in equilibrium before about 1965. Recharge of about 13,000 acre-feet per year was balanced primarily by discharge near Moenkopi Wash and Laguna Creek and by evapotranspiration. At least 180 million acre-feet of water was in storage. The estimated average hydraulic conductivity of the aquifer is 0.65 foot per day. The confined storage coefficient is estimated to be about 0.0004 where the aquifer is thickest, and the estimated unconfined storage coefficient ranges from 0.10 to 0.15. \r\n\r\nGround-water withdrawals that averaged 5,300 acre-feet per year from 1976 to 1979 have caused water levels to decline in wells in the confined part of the aquifer. Withdrawals include an average of 3,700 acre-feet per year to supply a coal-slurry pipeline from a coal mine on Black Mesa. Six observation wells equipped with water-level recorders have been used to monitor aquifer response. The water level in one well 32 miles south of the mine declined 17 feet from 1972 through 1979 and 3.5 feet during 1979. \r\n\r\nA mathematical model of the N aquifer was developed and calibrated for equilibrium and nonequilibrium conditions. The model was used in part to improve estimates of aquifer characteristics and the water budget, and it successfully reproduced the observed response of the aquifer through 1979. The model results indicate that about 95 percent of the 44,000 acre-feet of water pumped from 1965 to 1979 was withdrawn from storage, but the reduction amounted to less than 0.03 percent of total storage. Water-level declines through 1979 were estimated to be more than 100 feet in an area of 200 square miles. Four projections of future water-level changes were made using the model. The most probable projection indicates that water-level declines would exceed 100 feet in an area of 440 square miles by 2001. Most of the decline would be recovered within a few years if withdrawals at the mine ceased. By 1990, however, municipal-supply pumpage is expected to exceed pumpage at the mine, and this pumpage would continue to have significant impacts on water levels in the Black Mesa area.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2201","usgsCitation":"Eychaner, J.H., 1983, Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona: U.S. Geological Survey Water Supply Paper 2201, vi, 26 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2201.","productDescription":"vi, 26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":138019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2201/report-thumb.jpg"},{"id":26384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a731","contributors":{"authors":[{"text":"Eychaner, James H.","contributorId":102050,"corporation":false,"usgs":true,"family":"Eychaner","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1674,"text":"wsp2240 - 1983 - Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","interactions":[{"subject":{"id":9135,"text":"ofr82161 - 1983 - Estimation of nonpoint sources of phosphorus for lakes in the Puget Sound region, Washington","indexId":"ofr82161","publicationYear":"1983","noYear":false,"title":"Estimation of nonpoint sources of phosphorus for lakes in the Puget Sound region, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":1674,"text":"wsp2240 - 1983 - Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","indexId":"wsp2240","publicationYear":"1983","noYear":false,"title":"Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"2240","title":"Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington","docAbstract":"Control of eutrophication of lakes in watersheds undergoing development is facilitated by estimates of the amounts of phosphorus (P) that reach the lakes from areas under various types of land use. Using a mass-balance model, the author calculated P loadings from present-day P concentrations measured in lake water and from other easily measured physical characteristics in a total of 28 lakes in drainage basins that contain only forest and residential land. The loadings from background sources (forest-land drainage and bulk precipitation) to each of the lakes were estimated by methods developed in a previous study. Differences between estimated present-day P loadings and loadings from background sources were attributed to changes in land use. The mean increase in annual P yield resulting from conversion of forest to residential land use was 7 kilograms per square kilometer, not including septic tank system contributions. Calculated loadings from septic systems were found to correlate best with the number of near-shore dwellings around each lake in 1940. The regression equation expressing this relationship explained 36 percent of the sample variance. There was no significant correlation between estimated septic tank system P loadings and number of dwellings present in 1960 or 1970. The evidence indicates that older systems might contribute more phosphorus to lakes than newer systems, and that there may be substantial time lags between septic system installation and significant impacts on lake-water P concentrations. For lakes in basins that contain agricultural land, the P loading attributable to agriculture can be calculated as the difference between the estimated total loading and the sum of estimated loadings from nonagricultural sources. A comprehensive system for evaluating errors in all loading estimates is presented. The empirical relationships developed allow preliminary approximations of the cumulative impact development has had on P loading and the amounts of P loading from generalized land-use categories for Puget Sound lowland lakes. In addition, the sensitivity of a lake to increased loading can be evaluated using the mass-balance model. The data required are presently available for most lakes. Estimates of P loading are useful in developing water-quality goals, setting priorities for lake studies, and designing studies of individual lakes. The suitability of a method for management of individual lakes will often be limited by relatively high levels of uncertainty, especially if the method is used to evaluate relatively small increases in P loading.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2240","usgsCitation":"Gilliom, R.J., 1983, Estimation of nonpoint source loadings of phosphorus for lakes in the Puget Sound region, Washington: U.S. Geological Survey Water Supply Paper 2240, iv, 24 p. :ill., 1 map ;28 cm., https://doi.org/10.3133/wsp2240.","productDescription":"iv, 24 p. :ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":138235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2240/report-thumb.jpg"},{"id":26749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2240/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb25d","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":143954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7943,"text":"ofr83432 - 1983 - Montana; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83432","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-432","title":"Montana; basic data for thermal springs and wells as recorded in Geotherm","docAbstract":"Changes in ground-water withdrawals, water levels, and quality of water occurred in the artesian aquifers of the Sevier Desert, Utah during 1963-81. Ground-water withdrawals increased from an average of 9,500 acre-feet (11.7 cubic hectometers) per year between 1951 and 1963 to an average of 27,500 acre-feet (33.9 cubic hectometers) per year between 1964 and 1981. Most of the increased withdrawal was from the deep artesian aquifer. Water levels declined as much as 19 feet (5.8 meters) in the deep artesian aquifer and as much as 13 feet (4.0 meters) in the shallow artesian aquifer between 1963 and 1981. The declines probably are due to increased ground-water withdrawals for irrigation and municipal use. Quality of water in parts of the shallow artesian aquifer is deteriorating. The deterioration probably is the result of recharge of poor quality from the overlying water-table aquifer. A digital-computer model was constructed to predict water-level changes resulting from changes in recharge and discharge for 20 years (1981-2000) at one-half, one, and two times the 1977-79 average rate. The model computer water-level declines of more than 80 feet (24 meters) in the deep artesian aquifer with withdrawals twice the 1977-79 average, declines of more than 40 feet (12 meters) if withdrawals were equal to the 1977-79 average, and declines of more than 15 feet (4.6 meters) if withdrawals were one-half the 1977-79 average. Computer water-level declines after 20 years in the shallow artesian aquifer were more than 50 feet (15 meters) at two times the 1977-79 average rate, more than 15 feet (4.6 meters) at the 1977-79 average, and less than 4 feet (1.2 meters) at one-half the 1977-79 average. The model also was used to predict the effects of approximate changes in ground-water withdrawals related to the Intermountain Power Project. Water-level declines in the deep artesian aquifer of more than 15 feet (4.6 meters), and only small changes in water levels in the shallow artesian aquifer after 20 years. These changes are in addition to changes computed for 20 years of withdrawals at the 1977-79 rate. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83432","usgsCitation":"Bliss, J.D., 1983, Montana; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-432, 166 p. ;28 cm., https://doi.org/10.3133/ofr83432.","productDescription":"166 p. ;28 cm.","costCenters":[],"links":[{"id":140868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0432/report-thumb.jpg"},{"id":35514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0432/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4dab3d","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156871,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7181,"text":"ofr83672 - 1983 - Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr83672","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-672","title":"Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","docAbstract":"Geological and geochemical followup studies of airborne electromagnetic anomalies in the Wadi Bidah district, southwestern Saudi Arabia, did not reveal metals of economic grade. \r\n\r\nInvestigation of an anomaly enclosing the Rabathan ancient mine disclosed tightly folded and sheared Proterozoic tuffaceous rocks interlayered mostly with chert, dolomite, carbonaceous rocks, and volcanic wacke including cherty iron-manganese formations slightly anomalous in copper and zinc. Three drill holes placed to test anomalies within these formations yielded negative results. \r\n\r\nStudies of a long, narrow anomaly north of the Rabathan area indicated a similar geological environment. This northern area also contains limited zones that are highly anomalous in copper and zinc and extensive zones that are slightly anomalous in those metals. Drilling was not undertaken in this area. \r\n\r\nThe Bilajimah airborne electromagnetic anomaly west of Wadi Bidah coincides with a broad synclinorium of layered felsic turfs and gossans. Geochemical studies indicated slightly anomalous copper, zinc, and silver values in gossans within the anomaly area. Two drill holes intersected carbonaceous rock that contained approximately 15 percent pyrrhotite and traces of sphalerite and chalcopyrite. \r\n\r\nTwo geophysically anomalous areas west of Wadi Bidah surround ancient mines at Mahawiyah and Khayal al Masna'ah. Results of geochemical sampling at these workings were positive. An airborne electromagnetic anomaly located in the Assifar area in the southwestern corner of the Wadi Bidah district is underlain principally by metasedimentary rocks that include large linear zones of cherty iron-manganese formation and a few gossans .containing secondary base metal minerals.\r\n\r\nDetailed mapping and sampling of the Mulhal ancient mine, located west of Wadi Bidah, revealed two types of polymetallic gossans : (1) stratiform deposits interlayered with ignimbrites and mafic volcanic rocks and (2) barite-bearing gossanous material in shear zones that grade into hydrothermally altered shear zones and extend beyond the mine area. The gossans and gossanous shear zones contain anomalous amounts of gold, silver, lead, copper, zinc, barium, and selenium. \r\n\r\nTwo gossans west of Wadi Bidah were mapped and sampled in detail; both gossans are interlayered, with siliceous volcanic rocks. Although the gossan at Jabal Mohr covers a large area, it contains low amounts of precious and base metals. The gossan at Mulhal No. 2 contains moderate to high amounts of gold, silver, copper, lead, and zinc.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83672","usgsCitation":"Smith, C.W., Waters, B., Naqvi, M., Worl, R.G., Helaby, A., Flanigan, V.J., Sadek, H., and Samater, R., 1983, Geological and geochemical studies in the Wadi Bidah District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-672, v, 101 p., 6 over-size sheets, ill., maps ;1983., https://doi.org/10.3133/ofr83672.","productDescription":"v, 101 p., 6 over-size sheets, ill., maps ;1983.","costCenters":[],"links":[{"id":142103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0672/report-thumb.jpg"},{"id":34537,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34538,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34532,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34533,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34534,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34535,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34536,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0672/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876b4","contributors":{"authors":[{"text":"Smith, C. W.","contributorId":57457,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waters, B.C.","contributorId":87412,"corporation":false,"usgs":true,"family":"Waters","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":154653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naqvi, M.","contributorId":84210,"corporation":false,"usgs":true,"family":"Naqvi","given":"M.","email":"","affiliations":[],"preferred":false,"id":154652,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Worl, R. G.","contributorId":13984,"corporation":false,"usgs":true,"family":"Worl","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":154647,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Helaby, A. M.","contributorId":64241,"corporation":false,"usgs":true,"family":"Helaby","given":"A. M.","affiliations":[],"preferred":false,"id":154649,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154650,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sadek, H.S.","contributorId":93915,"corporation":false,"usgs":true,"family":"Sadek","given":"H.S.","affiliations":[],"preferred":false,"id":154654,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Samater, R.M.","contributorId":82694,"corporation":false,"usgs":true,"family":"Samater","given":"R.M.","affiliations":[],"preferred":false,"id":154651,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":11004,"text":"ofr82111 - 1983 - Gravity survey of Dixie Valley, west-central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr82111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-111","title":"Gravity survey of Dixie Valley, west-central Nevada","docAbstract":"Dixie Valley, a northeast-trending structural trough typical of valleys in the Basin and Range Province, is filled with a maximum of about 10,000 feet of alluvial and lacustrine deposits , as estimated from residual-gravity measurements obtained in this study. On the basis of gravity measurements at 300 stations on nine east-west profiles, the gravity residuals reach a maximum of 30 milligals near the south-central part of the valley. Results from a three-dimensional inversion model indicate that the central depression of the valley is offset to the west of the geographic axis. This offset is probably due to major faulting along the west side of the valley adjacent to the Stillwater Range. Comparison of depths to bedrock obtained during this study and depths obtained from a previous seismic-refraction study indicates a reasonably good correlation. A heterogeneous distribution of densities within the valley-fill deposits would account for differing depths determined by the two methods. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82111","usgsCitation":"Schaefer, D.H., 1983, Gravity survey of Dixie Valley, west-central Nevada: U.S. Geological Survey Open-File Report 82-111, v, 22 p. :maps ;28 cm., https://doi.org/10.3133/ofr82111.","productDescription":"v, 22 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0111/report-thumb.jpg"},{"id":38772,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0111/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38773,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0111/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38774,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0111/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2855","contributors":{"authors":[{"text":"Schaefer, Donald H.","contributorId":77507,"corporation":false,"usgs":true,"family":"Schaefer","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25470,"text":"wri824045 - 1983 - Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York, part 1: Geohydrology, modeling strategy, and regional evaluation","interactions":[],"lastModifiedDate":"2023-09-29T21:16:58.847871","indexId":"wri824045","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4045","title":"Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York, part 1: Geohydrology, modeling strategy, and regional evaluation","docAbstract":"

A computer simulation of Long Island 's regional groundwater system has been used to evaluate the effects that new-installed sewers will have on ground-water levels. Results indicate maximum water-table decliners of as much as up to 18 feet in central Nassau County and about 9 feet in Suffolk County. Total stream base flows and freshwater outflow to the south shore bay system will decrease by 22%. The regional scale of the model does not permit detailed predictions for individual streams. To quantify the effects of lowered ground-water levels on individual streams, two fine-scale sub-regional models have been designed. This report, the first in a three-part series describing the simulated effects of sewers in southern Nassau and southwestern Suffolk Counties, presents the hydrogeologic setting, pertinent literature, modeling strategy, subregional model design, and the results obtained to date from the regional ground-water model. The regional model results described will be used in the later reports to generate flux boundary conditions for the subregional models. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824045","usgsCitation":"Reilly, T.E., Buxton, H., Franke, O., and Wait, R.L., 1983, Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York, part 1: Geohydrology, modeling strategy, and regional evaluation: U.S. Geological Survey Water-Resources Investigations Report 82-4045, v, 45 p., https://doi.org/10.3133/wri824045.","productDescription":"v, 45 p.","costCenters":[],"links":[{"id":421430,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35569.htm","linkFileType":{"id":5,"text":"html"}},{"id":54196,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4045/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118885,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4045/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau 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T. E.","contributorId":79460,"corporation":false,"usgs":true,"family":"Reilly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":193820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Franke, O.L.","contributorId":57082,"corporation":false,"usgs":true,"family":"Franke","given":"O.L.","affiliations":[],"preferred":false,"id":193819,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193818,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9882,"text":"ofr83492 - 1983 - Modifications of the IBM personal computer synchronous communications support programs for use with the Multics","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83492","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-492","title":"Modifications of the IBM personal computer synchronous communications support programs for use with the Multics","docAbstract":"Version 1.00 of the Asynchronous Communications Support supplied with the IBM Personal Computer must be modified to be used for communications with Multics. Version 2.00 can be used as supplied, but error checking and screen printing capabilities can be added by using modifications very similar to those required for Version 1.00. This paper describes and lists required programs on Multics and appropriate modifications to both Versions 1.00 and 2.00 of the programs supplied by IBM.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83492","usgsCitation":"Kork, J.O., 1983, Modifications of the IBM personal computer synchronous communications support programs for use with the Multics: U.S. Geological Survey Open-File Report 83-492, 26 p. ;28 cm., https://doi.org/10.3133/ofr83492.","productDescription":"26 p. ;28 cm.","costCenters":[],"links":[{"id":140948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0492/report-thumb.jpg"},{"id":37670,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0492/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62862a","contributors":{"authors":[{"text":"Kork, John O.","contributorId":20323,"corporation":false,"usgs":true,"family":"Kork","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":160451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}