No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6947","usgsCitation":"1969, Metallic mineral resources map of the Hagemeister Island Quadrangle, Alaska: U.S. Geological Survey Open-File Report 69-47, Report: 3 p.; 1 Plate: 25.32 x 23.08 inches, https://doi.org/10.3133/ofr6947.","productDescription":"Report: 3 p.; 1 Plate: 25.32 x 23.08 inches","costCenters":[],"links":[{"id":145897,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0047/report-thumb.jpg"},{"id":424644,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424645,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Hagemeister Island Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -162.5,\n 58\n ],\n [\n -160,\n 58\n ],\n [\n -160,\n 59\n ],\n [\n -162.5,\n 59\n ],\n [\n -162.5,\n 58\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6274c0","contributors":{"compilers":[{"text":"Cobb, Edward H.","contributorId":64689,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward H.","affiliations":[],"preferred":false,"id":892854,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":37719,"text":"wl483 - 1969 - Wildlife imported into the United States in 1968.","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"wl483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"483","title":"Wildlife imported into the United States in 1968.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Division Of Management And Enforcement, 1969, Wildlife imported into the United States in 1968. (Revises Wildlife Leaflet 480 (1968).): Wildlife Leaflet 483, 4 p.","productDescription":"4 p.","costCenters":[],"links":[{"id":162821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 480 (1968).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3ed3","contributors":{"authors":[{"text":"Division Of Management And Enforcement","contributorId":127883,"corporation":true,"usgs":false,"organization":"Division Of Management And Enforcement","id":529684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3796,"text":"cir630 - 1969 - Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","interactions":[],"lastModifiedDate":"2022-09-02T21:59:54.813067","indexId":"cir630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"630","title":"Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal","docAbstract":"The Oklahoma Panhandle and adjacent areas in Texas, Kansas, Colorado, and New Mexico have prospered because of the development of supplies of fresh water and of oil and gas. The Ogallala and, in places, Cretaceous rocks produce fresh water for irrigation, public supply, and domestic and stock use through approximately 9,000 irrigation and public supply wells and a large but undetermined number of other wells. Disposal of oil-field brine and other wastes into the Glorieta Sandstone is of concern to many local residents because of the possibility of pollution of the overlying fresh-water aquifers, particularly the Ogallala Formation. Permits for 147 disposal wells into the Glorieta have been issued in this area. This report summarizes the data on geology, hydrology, and water development currently available to the U.S. Geological Survey. Geologic information indicates that, in the report area, the Glorieta Sandstone lies at depths ranging from about 500 to 1,600 feet below the base of the Ogallala Fox, nation. The rocks between those two formations are of relatively impermeable types, but solution and removal of salt has resulted in collapse of the rocks in some places. Collapse and fracturing of the rocks could result in increased vertical permeability. This might result in movement of brine under hydrostatic head from the Glorieta Sandstone into overlying fresh-water aquifers, in places where an upward hydraulic gradient exists or is created by an increase in pressure within the Glorieta. Abandoned or inadequately sealed boreholes also are possible conduits for such fluids. The mixing of water in the fresh-water aquifers with brines injected into the Glorieta is not known to have occurred anywhere in the report area, but the information available is not adequate to show positively whether or not this may have occurred locally. Much additional information on the stratigraphy and hydrology--particularly, data on the potentiometric surface of water in the Glorieta--needs to be collected and analyzed before conclusions can be drawn regarding the possibility of vertical movement of oil-field brines from the Glorieta to fresh-water aquifers above.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir630","usgsCitation":"Irwin, J.H., and Morton, R.B., 1969, Hydrogeologic information on the Glorieta Sandstone and the Ogallala Formation in the Oklahoma Panhandle and adjoining areas as related to underground waste disposal: U.S. Geological Survey Circular 630, Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller, https://doi.org/10.3133/cir630.","productDescription":"Report: iii, 26 p.; 4 Plates: 41.62 x 21.27 inches or smaller","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311912,"rank":304,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":406196,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23973.htm","linkFileType":{"id":5,"text":"html"}},{"id":311911,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":30866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0630/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311910,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":124418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0630/report-thumb.jpg"},{"id":311909,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1969/0630/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma, Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.388,\n 35.242\n ],\n [\n -104.388,\n 38.25\n ],\n [\n -99.25,\n 38.25\n ],\n [\n -99.25,\n 35.242\n ],\n [\n -104.388,\n 35.242\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627989","contributors":{"authors":[{"text":"Irwin, James Haskell","contributorId":56633,"corporation":false,"usgs":true,"family":"Irwin","given":"James","email":"","middleInitial":"Haskell","affiliations":[],"preferred":false,"id":147617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert B.","contributorId":50899,"corporation":false,"usgs":true,"family":"Morton","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16143,"text":"ofr69273 - 1969 - Test of data compilation procedures for Fraunhofer line discriminator","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr69273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-273","title":"Test of data compilation procedures for Fraunhofer line discriminator","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69273","usgsCitation":"Stoertz, G.E., 1969, Test of data compilation procedures for Fraunhofer line discriminator: U.S. Geological Survey Open-File Report 69-273, 35 p. ill. ;30 cm., https://doi.org/10.3133/ofr69273.","productDescription":"35 p. ill. ;30 cm.","costCenters":[],"links":[{"id":150498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684be7","contributors":{"authors":[{"text":"Stoertz, George Eimert","contributorId":99572,"corporation":false,"usgs":true,"family":"Stoertz","given":"George","email":"","middleInitial":"Eimert","affiliations":[],"preferred":false,"id":172316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16144,"text":"ofr69274 - 1969 - Testing the Fraunhofer line discriminator by sensing fluorescent dye","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr69274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-274","title":"Testing the Fraunhofer line discriminator by sensing fluorescent dye","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69274","usgsCitation":"Stoertz, G.E., 1969, Testing the Fraunhofer line discriminator by sensing fluorescent dye: U.S. Geological Survey Open-File Report 69-274, 40 p. ill. ;30 cm., https://doi.org/10.3133/ofr69274.","productDescription":"40 p. ill. ;30 cm.","costCenters":[],"links":[{"id":150499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6847ed","contributors":{"authors":[{"text":"Stoertz, George Eimert","contributorId":99572,"corporation":false,"usgs":true,"family":"Stoertz","given":"George","email":"","middleInitial":"Eimert","affiliations":[],"preferred":false,"id":172317,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57743,"text":"ofr69276 - 1969 - Evaluation of installation methods for nuclear meter access tubes","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr69276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-276","title":"Evaluation of installation methods for nuclear meter access tubes","language":"ENGLISH","doi":"10.3133/ofr69276","usgsCitation":"Teasdale, W.E., and Johnson, A., 1969, Evaluation of installation methods for nuclear meter access tubes: U.S. Geological Survey Open-File Report 69-276, 19 leaves : ill. ; 27 cm., https://doi.org/10.3133/ofr69276.","productDescription":"19 leaves : ill. ; 27 cm.","costCenters":[],"links":[{"id":183543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad78","contributors":{"authors":[{"text":"Teasdale, Warren E.","contributorId":85164,"corporation":false,"usgs":true,"family":"Teasdale","given":"Warren","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":257679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":257678,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44915,"text":"ofr69250 - 1969 - Availability of palynological material from Naval Petroleum Reserve No.4, XVIII: Umiat Test Wells Nos. 1 and 2, East Topagoruk Test Well No. 1","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr69250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-250","title":"Availability of palynological material from Naval Petroleum Reserve No.4, XVIII: Umiat Test Wells Nos. 1 and 2, East Topagoruk Test Well No. 1","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69250","usgsCitation":"Scott, R., 1969, Availability of palynological material from Naval Petroleum Reserve No.4, XVIII: Umiat Test Wells Nos. 1 and 2, East Topagoruk Test Well No. 1: U.S. Geological Survey Open-File Report 69-250, 2 p. ;28 cm., https://doi.org/10.3133/ofr69250.","productDescription":"2 p. ;28 cm.","costCenters":[],"links":[{"id":161515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d783","contributors":{"authors":[{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":230671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57748,"text":"ofr69335 - 1969 - Ground-water levels in observation wells in Oklahoma, 1967-68","interactions":[],"lastModifiedDate":"2012-02-02T00:12:33","indexId":"ofr69335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-335","title":"Ground-water levels in observation wells in Oklahoma, 1967-68","docAbstract":"The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; (5) provide long-time continuous records of fluctuations of water levels in representative wells; and (6) serve as a framework to which other types of hydrologic data my be related.\r\nPrior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U.S. Geological Survey. Beginning with the 1956 calendar year, however, Geological Survey water-level reports will contain only records of a selected network of observation wells, and will be published at 5-year intervals. The first of this series, for the 1956-59 period was published in 1962.\r\n\r\nThis report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in water-supply papers since 1955. This report, which contains water-level records for the 2-year period (1967-68), is the fifth in a series presenting water-level records for all permanent observations wells in Oklahoma. The first report, published in 1963, contains water-level records for the 2-year period of (1961-62); the second report, published in 1964, contains water-level records for the 2-year period (1961-62); the third report, published in 1965, contains water-level records for the 2-year period (1963-64); and the fourth report contains water-level records for the 2-year period (1965-66).","language":"ENGLISH","doi":"10.3133/ofr69335","usgsCitation":"Bingham, R., 1969, Ground-water levels in observation wells in Oklahoma, 1967-68: U.S. Geological Survey Open-File Report 69-335, 92 p., https://doi.org/10.3133/ofr69335.","productDescription":"92 p.","costCenters":[],"links":[{"id":182463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69818a","contributors":{"authors":[{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":257684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62260,"text":"gq818 - 1969 - Geologic map of the Superior quadrangle, Pinal County, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq818","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"818","title":"Geologic map of the Superior quadrangle, Pinal County, Arizona","language":"ENGLISH","doi":"10.3133/gq818","usgsCitation":"Peterson, D.W., 1969, Geologic map of the Superior quadrangle, Pinal County, Arizona: U.S. Geological Survey Geologic Quadrangle 818, 1 map., https://doi.org/10.3133/gq818.","productDescription":"1 map.","costCenters":[],"links":[{"id":103534,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2120.htm","linkFileType":{"id":5,"text":"html"},"description":"2120"},{"id":248444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0818/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":253422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0818/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.11749999999999,33.25 ], [ -111.11749999999999,33.3675 ], [ -111,33.3675 ], [ -111,33.25 ], [ -111.11749999999999,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a682","contributors":{"authors":[{"text":"Peterson, Donald W.","contributorId":11209,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":267150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53420,"text":"ofr69327 - 1969 - Water resources of the Marine Corps Supply Center area, Barstow, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr69327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-327","title":"Water resources of the Marine Corps Supply Center area, Barstow, California","language":"ENGLISH","doi":"10.3133/ofr69327","usgsCitation":"Miller, G., 1969, Water resources of the Marine Corps Supply Center area, Barstow, California: U.S. Geological Survey Open-File Report 69-327, iv, 51 p. : ill., maps ; 27 cm., https://doi.org/10.3133/ofr69327.","productDescription":"iv, 51 p. : ill., maps ; 27 cm.","costCenters":[],"links":[{"id":181212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0327/report-thumb.jpg"},{"id":87388,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0327/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87389,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0327/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d18","contributors":{"authors":[{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":247557,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15192,"text":"ofr70242 - 1969 - Geology of the Mackay 30-minute quadrangle, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:07:06","indexId":"ofr70242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"70-242","title":"Geology of the Mackay 30-minute quadrangle, Idaho","docAbstract":"The Jefferson Dolomite, Grand View Dolomite, and Three Forks Limestone, all of Devonian age, are the oldest rocks exposed in the quadrangle. Rocks that range from Mississippian to Permian in age are widespread; they are represented by the White Knob Limestone in the eastern part of the quadrangle and the Copper Basin Formation in the western part. The Copper Basin Formation, which is composed of non-carbonate detrital rocks, is interlayered with the White Knob Limestone near the middle of the quadrangle. This interlayering is herein interpreted to be the result of depositional interbedding, but it could be in part due to juxtaposition by faulting. The Challis Volcanics, of Tertiary age, cover much of the quadrangle, and except for a conspicuous basal conglomerate, lack distinctive subdivisions similar to those in neighboring areas. Alluvial deposits which may be in part as old as Pliocene are scattered through the quadrangle. Glaciation affected all higher parts of the quadrangle, and locally glacial deposits of at least three ages can be distinguished The latest two of these are probably of late Wisconsin Bull Lake and Pinedale ages. Basalt flows of probable Recent age extend into the southernmost part of the quadrangle and originate in part from vents there. \r\n\r\nIntrusive rocks, including plutons and related dikes of Tertiary age, are scattered throughout the quadrangle. They range from granite to quartz diorite in composition. The intrusive rocks seem to be related to the Challis Volcanics. \r\n\r\nThe rocks of the quadrangle were strongly deformed and eroded prior to the deposition of the Challis Volcanics. No thrust faults have been recognized although such faults are plentiful in the adjacent region. Deformation has continued until recent times. \r\n\r\nAll or parts of five mining districts are included in the quadrangle, and the total production probably exceeded $10,000,000. Mining has been quiet since World War II but activity has been renewed at times in the past and possibilities for the discovery of substantial new deposits seem promising. The mineral deposits formed largely by replacement, partly in areas of contact metamorphism. The metals present are varied but copper has been the main product. All of the deposits are believed to be related to the intrusions of Tertiary age.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr70242","usgsCitation":"Nelson, W.H., and Ross, C.P., 1969, Geology of the Mackay 30-minute quadrangle, Idaho: U.S. Geological Survey Open-File Report 70-242, 165 p. ;27 cm., https://doi.org/10.3133/ofr70242.","productDescription":"165 p. ;27 cm.","costCenters":[],"links":[{"id":148998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0242/report-thumb.jpg"},{"id":44106,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0242/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44107,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0242/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea74","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, Clyde Polhemus","contributorId":71954,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"Polhemus","affiliations":[],"preferred":false,"id":170718,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55954,"text":"ofr69282 - 1969 - Memorandum on the ground-water resources of Rocky Springs Park, Claiborne County, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:12:19","indexId":"ofr69282","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-282","title":"Memorandum on the ground-water resources of Rocky Springs Park, Claiborne County, Mississippi","language":"ENGLISH","doi":"10.3133/ofr69282","usgsCitation":"Thomson, F., 1969, Memorandum on the ground-water resources of Rocky Springs Park, Claiborne County, Mississippi: U.S. Geological Survey Open-File Report 69-282, 11 p., 3 figs., https://doi.org/10.3133/ofr69282.","productDescription":"11 p., 3 figs.","costCenters":[],"links":[{"id":184385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613f6a","contributors":{"authors":[{"text":"Thomson, F.H.","contributorId":8132,"corporation":false,"usgs":true,"family":"Thomson","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":254551,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16528,"text":"ofr69318 - 1969 - Sedimentary rocks of the coast of Liberia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr69318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-318","title":"Sedimentary rocks of the coast of Liberia","docAbstract":"Two basins containing sedimentary rocks o# probable Cretaceous age have been recognized near the coast of Liberia in the area between Monrovia and Buchanan; geophysical evidence suggests that similar though larger basins exist on the adjacent continental shelf. \r\n\r\nThe oldest sedimentary unit recognized, the Paynesville Sandstone of possible early to middle Paleozoic age, is intruded by dikes and sills of diabase of early Jurassic age and lies unconformably on crystalline rocks of late Precambrian age. Dips in the Paynesville Sandstone define a structural basin centered south of Roberts International Airport (formerly called Roberts Field) about 25 miles east of Monrovla. Wackes and conglomerates of Cretaceous age, herein named the Farmington River Formation, unconformably overlie the Paynesville Sandstone and constitute the sedimentary fill in the Roberts basin.\r\n\r\nThe Bassa basin lies to the southeast of the Roberts basin and is separated from it by an upwarp of crystalline rocks. The basin is occupied by wackes and conglomerates of the Farmington River Formation, which apparently lie directly on the crystalline basement. Both basins are bounded on the northeast by northwest-trending dip-slip faults. \r\n\r\nThe best potential for petroleum deposits that exists in Liberia is beneath the adjacent continental shelf and slope. Geophysical exploration and drilling will be required to evaluate this potential.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69318","usgsCitation":"White, R.W., 1969, Sedimentary rocks of the coast of Liberia: U.S. Geological Survey Open-File Report 69-318, 28 p. maps ;27 cm., https://doi.org/10.3133/ofr69318.","productDescription":"28 p. maps ;27 cm.","costCenters":[],"links":[{"id":150246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0318/report-thumb.jpg"},{"id":45511,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0318/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7cf9","contributors":{"authors":[{"text":"White, Richard William","contributorId":8871,"corporation":false,"usgs":true,"family":"White","given":"Richard","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":172996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68306,"text":"ha350 - 1969 - Floods on Susquehanna River at Oneonta, New York","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha350","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"350","title":"Floods on Susquehanna River at Oneonta, New York","language":"ENGLISH","doi":"10.3133/ha350","usgsCitation":"Hladio, S., 1969, Floods on Susquehanna River at Oneonta, New York: U.S. Geological Survey Hydrologic Atlas 350, 1 map., https://doi.org/10.3133/ha350.","productDescription":"1 map.","costCenters":[],"links":[{"id":186691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/350/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -42.483333333333334,75 ], [ -42.483333333333334,75.11749999999999 ], [ -42.4175,75.11749999999999 ], [ -42.4175,75 ], [ -42.483333333333334,75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df817","contributors":{"authors":[{"text":"Hladio, Stephen","contributorId":67952,"corporation":false,"usgs":true,"family":"Hladio","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":277998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68051,"text":"ha341 - 1969 - Hydrogeology of the Berea and Cussewago Sandstones in northeastern Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha341","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"341","title":"Hydrogeology of the Berea and Cussewago Sandstones in northeastern Ohio","language":"ENGLISH","doi":"10.3133/ha341","usgsCitation":"Rau, J.L., 1969, Hydrogeology of the Berea and Cussewago Sandstones in northeastern Ohio: U.S. Geological Survey Hydrologic Atlas 341, 4 maps on 2 sheets :col. ;33 x 61 cm. and 25 x 20 cm., sheets 84 x 112 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha341.","productDescription":"4 maps on 2 sheets :col. ;33 x 61 cm. and 25 x 20 cm., sheets 84 x 112 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186029,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89313,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/341/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89314,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/341/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.25,41 ], [ -82.25,41.75 ], [ -80.75,41.75 ], [ -80.75,41 ], [ -82.25,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6152d3","contributors":{"authors":[{"text":"Rau, Jon L.","contributorId":97989,"corporation":false,"usgs":true,"family":"Rau","given":"Jon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33130,"text":"b1235 - 1969 - Bibliography of North American geology, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"b1235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1235","title":"Bibliography of North American geology, 1965","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1235","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Bibliography of North American geology, 1965: U.S. Geological Survey Bulletin 1235, 1144 p., https://doi.org/10.3133/b1235.","productDescription":"1144 p.","costCenters":[],"links":[{"id":247375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1235/report.pdf","size":"55408","linkFileType":{"id":1,"text":"pdf"}},{"id":251822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1235/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629489","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":529456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67911,"text":"ha397 - 1969 - Hurricane Camille tidal floods of August 1969 along the Gulf Coast, Kiln quadrangle, Mississippi","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"397","title":"Hurricane Camille tidal floods of August 1969 along the Gulf Coast, Kiln quadrangle, Mississippi","language":"ENGLISH","doi":"10.3133/ha397","usgsCitation":"Wilson, K., and Hudson, J.W., 1969, Hurricane Camille tidal floods of August 1969 along the Gulf Coast, Kiln quadrangle, Mississippi: U.S. Geological Survey Hydrologic Atlas 397, 1 map :col. ;on sheet 76 x 84 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha397.","productDescription":"1 map :col. ;on sheet 76 x 84 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89105,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/397/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.5,30.3675 ], [ -89.5,30.5 ], [ -89.36749999999999,30.5 ], [ -89.36749999999999,30.3675 ], [ -89.5,30.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a4d9","contributors":{"authors":[{"text":"Wilson, K. V.","contributorId":51715,"corporation":false,"usgs":true,"family":"Wilson","given":"K. V.","affiliations":[],"preferred":false,"id":277306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, James W.","contributorId":36183,"corporation":false,"usgs":true,"family":"Hudson","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15393,"text":"ofr69202 - 1969 - Cretaceous sedimentation and tectonism in the southeastern Kaiparowits region, Utah","interactions":[],"lastModifiedDate":"2025-07-28T17:44:06.445282","indexId":"ofr69202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-202","title":"Cretaceous sedimentation and tectonism in the southeastern Kaiparowits region, Utah","docAbstract":"Upper Cretaceous strata in the southeastern Kaiparowits region of south-central Utah consist of approximately 3,500 feet of interfingering sandstone, mudstone, shale, and coal in the Dakota Formation (oldest), Tropic Shale, Straight Cliffs Formation, and Wahweap Formation (youngest). The formations consist of several depositional facies that can be recognized by characteristic lithologies bedding structures, and fossils; these are the alluvial plain, deltaic plain, lagoonal-paludal, barrier sandstone, and offshore marine facies. The distribution of facies clearly defines the paleogeography of the region during several cycles of marine transgression and regression. The nonmarine beds were deposited on a broad alluvial coastal plain that was bordered on the west and southwest by highlands and on the east and northeast by the Western Interior seaway. The marine beds were deposited whenever the seaway advanced into or across the region. \r\n\r\nThe Dakota Formation and the lower part of the Tropic Shale were deposited in nonmarine and marine environments, while the shoreline advanced generally westward across the region. The middle and upper part of the Tropic Shale and the Tibbet Canyon and Smoky Hollow Members of the Straight Cliffs Formation were deposited in marine and nonmarine environments when the seaway had reached its greatest areal extent and began a gradual northeastward withdrawal. An unconformity at the top of the Smoky Hollow represents a period of erosion and possibly nondeposition before deposition of the John Henry Member of the Straight Cliffs. \r\n\r\nThe John Henry Member grades from nonmarine in the southwest to predominantly marine in the northeast, and was deposited during two relatively minor cycles of transgression and regression. The Drip Tank Member at the top of the Straight Cliffs Formation is a widespread sandstone unit deposited mainly in fluvial environments. Some of the beds in the northeastern part of the region were probably deposited in marine waters during the final incursion of the seaway into the Kaiparowits region. The overlying Wahweap Formation was deposited in nonmarine environments. Slight but continued tectonism during Late Cretaceous time is indicated by lateral changes of facies and thickness variations that coincide at least partly with present structures. These criteria indicate that Laramide tectonism consisted of two phases. An early phase that lasted from about late Albian to late Campanian time included regional subsidence, basin downwarping, and movement on local folds and faults. A later phase that lasted from late Campanian to about late Paleocene time included regional uplift, monoclinal flexing, and probable new faulting, as well as continued basin downwarping and movement on local folds and probably on the older faults. \r\n\r\nThe principal economic resource in the Kaiparowits region is bituminous or subbituminous coal in the john Henry Member. Because basin downwarping and movement on local folds occurred during deposition, the thicker and more continuous coal beds are in the ancestral synclines and tile deeper part of the structural basin. Presently indicated resources total 7.3 billion tons, but considerably larger quantities are probably present in the unexplored parts of the region. 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