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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr325","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1983, Landsat image map of the Judayyidat Ar'ar quadrangle, sheet 31E, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 325, 21.26 x 33.07 inches, https://doi.org/10.3133/ofr325.","productDescription":"21.26 x 33.07 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","projection":"Transverse Mercator","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 40.5,\n 32\n ],\n [\n 40.5,\n 31\n ],\n [\n 42,\n 31\n ],\n [\n 42,\n 32\n ],\n [\n 40.5,\n 32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567a823ee4b0a04ef490fcf5","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":583141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saudi Arabia. Deputy Ministry for Mineral Resources","contributorId":147327,"corporation":true,"usgs":false,"organization":"Saudi Arabia. Deputy Ministry for Mineral Resources","id":583142,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160124,"text":"ofr320 - 1983 - Landsat image map of the Abū Hadrīyah quadrangle, sheet 27J, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-12-11T15:18:21","indexId":"ofr320","displayToPublicDate":"2008-12-28T00:00:00","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":"320","title":"Landsat image map of the Abū Hadrīyah quadrangle, sheet 27J, Kingdom of Saudi Arabia","docAbstract":"Interagency Report 517
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr320","usgsCitation":"U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1983, Landsat image map of the Abū Hadrīyah quadrangle, sheet 27J, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 320, 21.26 x 33.46 inches, https://doi.org/10.3133/ofr320.","productDescription":"21.26 x 33.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312190,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","projection":"Transverse Mercator","country":"Saudi Arabia","otherGeospatial":"Persian Gulf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 48,\n 27\n ],\n [\n 48,\n 28\n ],\n [\n 49.5,\n 28\n ],\n [\n 49.5,\n 27\n ],\n [\n 48,\n 27\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"566c01e4e4b09cfe53ca5ad9","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":581968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saudi Arabia. Deputy Ministry for Mineral Resources","contributorId":147327,"corporation":true,"usgs":false,"organization":"Saudi Arabia. Deputy Ministry for Mineral Resources","id":581969,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":17255,"text":"ofr83146 - 1983 - Hydrology of area 54, northern Great Plains, and Rocky Mountain coal provinces, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2022-08-26T19:52:02.712546","indexId":"ofr83146","displayToPublicDate":"1994-01-01T01:00:00","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":"83-146","title":"Hydrology of area 54, northern Great Plains, and Rocky Mountain coal provinces, Colorado and Wyoming","docAbstract":"A nationwide need for information characterizing hydrologic conditions in mined and potential mine areas has become paramount with the enactment of the Surface Mining Control and Reclamation Act of 1977. This report, one in a series covering the coal provinces nationwide, presents information thematically by describing single hydrologic topics through the use of brief texts and accompanying maps, graphs, or other illustrations. The summation of the topical discussions provides a description of the hydrology of the area. Area 54, in north-central Colorado and south-central Wyoming, is 1 of 20 hydrologic reporting areas of the Northern Great Plains and Rocky Mountain coal provinces. Part of the Southern Rocky Mountains and Wyoming Basin physiographic provinces, the 8,380-square-mile area is one of contrasting geology, topography, and climate. This results in contrasting hydrologic characteristics. The major streams, the North Platte, Laramie, and Medicine Bow Rivers, and their principal tributaries, all head in granitic mountains and flow into and through sedimentary basins between the mountain ranges. Relief averages 2,000 to 3,000 feet. Precipitation in the mountains may exceed 40 inches annually, much of it during the winter, which produces deep snowpacks. Snowmelt in spring and summer provides most streamflow. Precipitation in the basins averages 10 to 16 inches annually, insufficient for sustained streamflow; thus, streams originating in the basins are ephemeral. Streamflow quality is best in the mountains where dissolved-solids concentrations generally are least. These concentrations increase as streams flow through sedimentary basins. The increases are mainly natural, but some may be due to irrigation in and adjacent to the flood plains. In the North Platte River, dissolved-solids concentrations are usually less than 300 milligrams per liter; in the Laramie and the Medicine Bow Rivers, the concentrations may average 500 to 850 milligrams per liter. However, water-quality stations on the Laramie and the Medicine Bow Rivers are farther removed from the mountain sources than the stations in the North Platte drainage. Because of the semiarid climate of the basins, soils are not adequately leached. Consequently, flow in ephemeral streams usually has a larger concentration of dissolved solids than that in perennial streams, averaging 1,000 to 1,600 milligrams per liter. Aquifers containing usable ground water are combined into three groups: (1) consolidated and unconsolidated non-coal-bearing Quaternary and Upper Tertiary deposits, (2) Mesozoic and Paleozoic sedimentary rocks, and (3) Lower Tertiary and Upper Cretaceous sedimentary rocks containing coal. These aquifers are used for municipal, domestic, irrigation, and stock supplies. Well yields range from about 5 to 1,000 gallons per minute, and depend on type of aquifer, saturated thickness, and degree of fracturing. The best quality ground water usually comes from the non-coal-bearing Quaternary and Upper Tertiary rocks or the Mesozoic and Paleozoic rocks; often it is dominated by calcium and bicarbonate ions. The coal-bearing formations have a large variability in water chemistry; dominant ions may be bicarbonate or sulfate and sodium, calcium, or magnesium. Dissolved-solids concentrations are generally larger than in the former two groups. The U.S. Geological Survey operates a network of hydrologic stations to observe the streamflow and groundwater conditions. This network currently includes 31 surface-water stations and 35 observation wells; information is available for many other sites observed in the past. Data available include rate of flow, water levels, and water quality; much of the data are available in published reports or from computer storage through the National Water Data Exchange (NAWDEX) or the National Water Data Storage and Retrieval System (WATSTORE). Five formations of Late Cretaceous and early Tertiary age contain coal.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83146","usgsCitation":"Kuhn, G., Daddow, P.D., and Craig, G.S., 1983, Hydrology of area 54, northern Great Plains, and Rocky Mountain coal provinces, Colorado and Wyoming: U.S. Geological Survey Open-File Report 83-146, vi, 96 p., https://doi.org/10.3133/ofr83146.","productDescription":"vi, 96 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":46401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0146/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405717,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13909.htm","linkFileType":{"id":5,"text":"html"}},{"id":149125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0146/report-thumb.jpg"}],"country":"United States","state":"Colorado, Wyoming","otherGeospatial":"Area 54","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.433,\n 40.32\n ],\n [\n -105.459,\n 40.32\n ],\n [\n -105.459,\n 42.224\n ],\n [\n -107.433,\n 42.224\n ],\n [\n -107.433,\n 40.32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ff3","contributors":{"authors":[{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":175626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daddow, P. D.","contributorId":54613,"corporation":false,"usgs":true,"family":"Daddow","given":"P.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":175624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Craig, G. S.","contributorId":91515,"corporation":false,"usgs":true,"family":"Craig","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":175625,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":48833,"text":"ofr83671 - 1983 - Tens of successive, colossal Missoula floods at north and east margins of channeled scabland","interactions":[],"lastModifiedDate":"2022-12-28T22:56:03.490071","indexId":"ofr83671","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":"83-671","title":"Tens of successive, colossal Missoula floods at north and east margins of channeled scabland","docAbstract":"In deposits of Pleistocene glacial lakes in northern Idaho and Washington, beds comprising 20 to 55 varves (average = 35-40) separate each successive graded gravel or sand bed that was swiftly emplaced by a catastrophic flood from glacial Lake Missoula. The floodlaid beds are similar to rhythmic successions of 40 or more graded beds in backflooded tributaries of the lower Columbia River. This new field evidence corroborates a controversial hypothesis that the great Pleistocene floods from glacial Lake Missoula were 40 or more colossal, separate joekulhlaups, and refutes the conventional notion that any two successive graded beds were deposited by one flood. \r\n\r\nThe only outlet of the 2000-km3 glacial Lake Missoula was through its great ice dam. Calculations show that each time the lake rose to about 600 m deep, it made the glacier buoyant and engendered a catastrophic discharge along the glacier bed (a joekulhlaup). A reconstructed water budget suggests that after a complete draining, the lake refilled in 3 to 6 decades; thus the hydrostatic prerequisites for a joekulhlaup were reestablished dozens of times during the late-Wisconsin episode of lake damming. \r\n\r\nVarious intercalated tephra layers, radiocarbon dates, varve successions, and the Bonneville flood deposits in the region suggest that late-Wisconsin glacial Lake Missoula existed for about 2 millennia within the period 15,000 to 12,700(?) yr ago. Varve beds indicate that the mean period between Missoula floods was about 4 decades, but became shorter during the last several floods. Between 20 and 30 of the Missoula joekulhlaups occurred after the single great flood from Lake Bonneville, which according to 14C dating in the Bonneville basin by W. E. Scott and associates and by D. R. Currey occurred some time between 15,000 and 14,000 yr ago.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83671","usgsCitation":"Waitt, R.B., 1983, Tens of successive, colossal Missoula floods at north and east margins of channeled scabland: U.S. Geological Survey Open-File Report 83-671, 29 p., https://doi.org/10.3133/ofr83671.","productDescription":"29 p.","costCenters":[],"links":[{"id":411160,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75698.htm","linkFileType":{"id":5,"text":"html"}},{"id":85666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0671/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162658,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0671/report-thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Oregon, Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124,\n 49\n ],\n [\n -124,\n 45\n ],\n [\n -113.5,\n 45\n ],\n [\n -113.5,\n 49\n ],\n [\n -124,\n 49\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685155","contributors":{"authors":[{"text":"Waitt, Richard B. 0000-0002-6392-5604 waitt@usgs.gov","orcid":"https://orcid.org/0000-0002-6392-5604","contributorId":2343,"corporation":false,"usgs":true,"family":"Waitt","given":"Richard","email":"waitt@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":238384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18163,"text":"ofr83825 - 1983 - Schlumberger soundings near Newberry Caldera, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:22","indexId":"ofr83825","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":"83-825","title":"Schlumberger soundings near Newberry Caldera, Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83825","usgsCitation":"Bisdorf, R.J., 1983, Schlumberger soundings near Newberry Caldera, Oregon: U.S. Geological Survey Open-File Report 83-825, 52 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83825.","productDescription":"52 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":151008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0825/report-thumb.jpg"},{"id":47530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0825/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3d2","contributors":{"authors":[{"text":"Bisdorf, Robert J.","contributorId":107277,"corporation":false,"usgs":true,"family":"Bisdorf","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16954,"text":"ofr83360 - 1983 - Chemical analyses and statistical summary for samples of minus-200-mesh stream-sediment, magnetic, and nonmagnetic heavy-mineral concentrates from the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness study area, Taos County, New Mexico","interactions":[],"lastModifiedDate":"2022-08-08T20:55:38.463174","indexId":"ofr83360","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":"83-360","title":"Chemical analyses and statistical summary for samples of minus-200-mesh stream-sediment, magnetic, and nonmagnetic heavy-mineral concentrates from the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness study area, Taos County, New Mexico","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83360","usgsCitation":"Sutley, S.J., Ludington, S., Billings, P., and Jones, D., 1983, Chemical analyses and statistical summary for samples of minus-200-mesh stream-sediment, magnetic, and nonmagnetic heavy-mineral concentrates from the Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness study area, Taos County, New Mexico: U.S. Geological Survey Open-File Report 83-360, Report: i, 36 p.; 1 Plate: 30.19 × 40.50 inches, https://doi.org/10.3133/ofr83360.","productDescription":"Report: i, 36 p.; 1 Plate: 30.19 × 40.50 inches","costCenters":[],"links":[{"id":46061,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404951,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13997.htm","linkFileType":{"id":5,"text":"html"}},{"id":150382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0360/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Taos County","otherGeospatial":"Latir Peak and Wheeler Peak Wildernesses and the Columbine-Hondo Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.625,\n 36.5\n ],\n [\n -105.333,\n 36.5\n ],\n [\n -105.333,\n 36.833\n ],\n [\n -105.625,\n 36.833\n ],\n [\n -105.625,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bbb","contributors":{"authors":[{"text":"Sutley, S. 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