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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr274","usgsCitation":"U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Landsat image map of the Wādī Ash Shaʻbah quadrangle, sheet 26E, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 274, 21.26 x 33.46 inches, https://doi.org/10.3133/ofr274.","productDescription":"21.26 x 33.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312949,"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 26\n ],\n [\n 40.5,\n 27\n ],\n [\n 42,\n 27\n ],\n [\n 42,\n 26\n ],\n [\n 40.5,\n 26\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56826b45e4b0a04ef4925b78","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":583531,"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":583532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160663,"text":"ofr213 - 1982 - Landsat image map of the Wādī Ar Rayn quadrangle, sheet 23H, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-12-28T16:36:09","indexId":"ofr213","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1982","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":"213","title":"Landsat image map of the Wādī Ar Rayn quadrangle, sheet 23H, Kingdom of Saudi Arabia","docAbstract":"Interagency Report 326
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr213","usgsCitation":"U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Landsat image map of the Wādī Ar Rayn quadrangle, sheet 23H, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 213, 21.26 x 33.46 inches, https://doi.org/10.3133/ofr213.","productDescription":"21.26 x 33.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312945,"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 45,\n 23\n ],\n [\n 45,\n 24\n ],\n [\n 46.5,\n 24\n ],\n [\n 46.5,\n 23\n ],\n [\n 45,\n 23\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56826b44e4b0a04ef4925b72","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":583503,"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":583504,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160550,"text":"ofr273 - 1982 - Landsat image map of the Ḩarrat Ithnayn quadrangle, sheet 26D, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-12-22T17:20:59","indexId":"ofr273","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1982","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":"273","title":"Landsat image map of the Ḩarrat Ithnayn quadrangle, sheet 26D, Kingdom of Saudi Arabia","docAbstract":"Interagency Report 477
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr273","usgsCitation":"U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Landsat image map of the Ḩarrat Ithnayn quadrangle, sheet 26D, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 273, 21.26 x 33.46 inches, https://doi.org/10.3133/ofr273.","productDescription":"21.26 x 33.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312754,"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 26\n ],\n [\n 40.5,\n 27\n ],\n [\n 39,\n 27\n ],\n [\n 39,\n 26\n ],\n [\n 40.5,\n 26\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567a8244e4b0a04ef490fd0f","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":583133,"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":583134,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160662,"text":"ofr277 - 1982 - Landsat image map of the Unnamed quadrangle, sheet 27D, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-12-28T16:30:01","indexId":"ofr277","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1982","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":"277","title":"Landsat image map of the Unnamed quadrangle, sheet 27D, Kingdom of Saudi Arabia","docAbstract":"","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr277","usgsCitation":"U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Landsat image map of the Unnamed quadrangle, sheet 27D, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 277, 21.26 x 33.46 inches, https://doi.org/10.3133/ofr277.","productDescription":"21.26 x 33.46 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312944,"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 45,\n 23\n ],\n [\n 45,\n 24\n ],\n [\n 43.5,\n 24\n ],\n [\n 43.5,\n 23\n ],\n [\n 45,\n 23\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56826b44e4b0a04ef4925b70","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":583501,"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":583502,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80037,"text":"ofr811103 - 1982 - Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"ofr811103","displayToPublicDate":"2007-06-20T00:00:00","publicationYear":"1982","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":"81-1103","title":"Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","docAbstract":"INTRODUCTION\r\n\r\nThe tertiary limestone aquifer system of the southeastern United States is a sequence of carbonate rocks referred to as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina. More than 3 billion gallons of water are pumped daily from the limestone aquifer; and the system is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida.\r\n\r\nThe aquifer system includes units of Paleocene to early Miocene age that combine to form a continuous carbonate sequence that is hydraulically connected in varying degrees. In a small area near Brunswick, Ga., a thin sequence of rocks of Late Cretaceous age is part of the system. In and directly downdip from much of the outcrop area, the system consists of one continuous permeable unit. Further downdip the aquifer system generally consists of two major permeable zones separated by a less-permeable unit of highly variable hydraulic properties (very leaky to virtually nonleaky). Conditions for the system vary from unconfined to confined depending upon whether the argillaceous Miocene and younger rocks that form the upper confining unit have been removed by erosion.\r\n\r\nThis report is one of a series of preliminary products depicting the hydrogeologic framework, water chemistry, and hydrology of the aquifer system. The map shows the distribution of chloride ions in water from the upper permeable zone of the limestone aquifer system. The upper permeable zone consists of several formations, primarily the Tampa, Suwannee, Ocala, and Avon Park Limestones (Miller 1981a, b).\r\n\r\nChloride concentrations of water within the upper permeable zone vary from nearly zero in recharge areas to many thousands of milligrams per liter (mg/L) in coastal discharge areas. Where the aquifer system discharges into the sea, the upper permeable zone contains increasing amounts of seawater. In these areas, wells that fully penetrate the upper permeable zone will yield water with chloride concentrations that approach that of seawater, about 19500 mg/L.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr811103","usgsCitation":"Sprinkle, C.L., 1982, Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States (WRI/OFR 81-1103): U.S. Geological Survey Open-File Report 81-1103, Map: 35 x 44 inches, https://doi.org/10.3133/ofr811103.","productDescription":"Map: 35 x 44 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1103/report-thumb.jpg"},{"id":91219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,24 ], [ -89,34 ], [ -80,34 ], [ -80,24 ], [ -89,24 ] ] ] } } ] }","edition":"WRI/OFR 81-1103","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e253c","contributors":{"authors":[{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011693,"text":"70011693 - 1982 - Bedform climbing in theory and nature","interactions":[],"lastModifiedDate":"2025-07-25T16:52:12.285703","indexId":"70011693","displayToPublicDate":"2006-06-14T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3369,"text":"Sedimentology","active":true,"publicationSubtype":{"id":10}},"title":"Bedform climbing in theory and nature","docAbstract":"Where bedforms migrate during deposition, they move upward (climb) with respect to the generalized sediment surface. Sediment deposited on each lee slope and not eroded during the passage of a following trough is left behind as a cross-stratified bed. Because sediment is thus transferred from bedforms to underlying strata, bedforms must decrease in cross-sectional area or in number, or both, unless sediment lost from bedforms during deposition is replaced with sediment transported from outside the depositional area. Where sediment is transported solely by downcurrent migration of two-dimensional bedforms, the mean thickness of cross-stratified beds is equal to the decrease in bedform cross-sectional area divided by the migration distance over which that size decrease occurs; where bedforms migrate more than one spacing while depositing cross-strata, bed thickness is only a fraction of bedform height.
Equations that describe this depositional process explain the downcurrent decrease in size of tidal sand waves in St Andrew Bay, Florida, and the downwind decrease in size of transverse aeolian dunes on the Oregon coast. Using the same concepts, dunes that deposited the Navajo, De Chelly, and Entrada Sandstones are calculated to have had mean heights between several tens and several hundreds of metres.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-3091.1982.tb01714.x","issn":"00370746","usgsCitation":"Rubin, D.M., and Hunter, R.E., 1982, Bedform climbing in theory and nature: Sedimentology, v. 29, no. 1, p. 121-138, https://doi.org/10.1111/j.1365-3091.1982.tb01714.x.","productDescription":"18 p.","startPage":"121","endPage":"138","costCenters":[],"links":[{"id":221060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-06-14","publicationStatus":"PW","scienceBaseUri":"5059f040e4b0c8380cd4a696","contributors":{"authors":[{"text":"Rubin, D. M.","contributorId":103689,"corporation":false,"usgs":true,"family":"Rubin","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":361728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}