{"pageNumber":"6309","pageRowStart":"157700","pageSize":"25","recordCount":165969,"records":[{"id":12659,"text":"ofr5321 - 1953 - Geology of the Knife River area, North Dakota","interactions":[{"subject":{"id":43649,"text":"ofr5122 - 1951 - Geologic maps of Medicine Butte, Broncho, Golden Valley, Beulah, Stanton, and Hazen quadrangles, North Dakota","indexId":"ofr5122","publicationYear":"1951","noYear":false,"title":"Geologic maps of Medicine Butte, Broncho, Golden Valley, Beulah, Stanton, and Hazen quadrangles, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":12659,"text":"ofr5321 - 1953 - Geology of the Knife River area, North Dakota","indexId":"ofr5321","publicationYear":"1953","noYear":false,"title":"Geology of the Knife River area, North Dakota"},"id":1}],"lastModifiedDate":"2026-02-05T20:06:27.236189","indexId":"ofr5321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-21","title":"Geology of the Knife River area, North Dakota","docAbstract":"The Knife River area, consisting of six 15-minute quadrangles, includes the lower half of the Knife River valley in west-central North Dakota. The area, in the center of the Williston Basin, is underlain by the Tongue River member of the Fort Union formation (Paleocene) and the Golden Valley formation (Eocene). The Tongue River includes beds equivalent to the Sentinel Butte shale; the Golden Valley formation, which receives its first detailed description in this report, consists of two members, a lower member of gray to white sandy kaolin clay and an upper member of cross-bedded micaceous sandstone.\r\n\r\nPro-Tongue River rocks that crop out in southwestern North Dakota include the Ludlow member of the Fort Union formation, the Cannonball marine formation (Paleocene) and the Hell Creek, Fox Hills, and Pierre formations, all upper Cretaceous. Post-Golden Valley rocks include the White River formation (Oligocene) and gravels on an old planation surface that may be Miocene or Pliocent.\r\n\r\nSurficial deposits include glacial and fluvial deposits of Pleistocene age and alluvium, dune sand, residual silica, and landslide blocks of Recent age. Three ages of glacial deposits can be differentiated, largely on the basis of three fills, separated by unconformities, in the Knife River valley. All three are of Wisconsin age and probably represent the Iowan, Tazewell, and Mankato substages. Deposits of the Cary substage have not been identified either in the Knife River area or elsewhere in southern North Dakota. Iowan glacial deposits form the outermost drift border in North Dakota. Southwest of this border are a few scattered granite boulders that are residual from the erosion of either the White River formation or a pre-Wisconsin till. The Tazewell drift border cannot be followed in southern North Dakota. The Mankato drift border can be traced in a general way from the South Dakota State line northwest across the Missouri River and through the middle of the Knife River area.\r\n\r\nThe major land forms of southwestern North Dakota are: (1) high buttes that stand above (2) a gravel-capped planation surface and (3) a gently-rolling upland; below the upland surface are (4) remnants of a broad valley stage of erosion into which (5) modern valleys have been cut. The broad valley profiles of many streams continue east across the Missouri River trench and are part of a former drainage system that flowed into Hudson Bay. Crossing the divides are (6) large trenches, formed when the former northeast-flowing streams were dammed by the glacier and diverted to the southeast. The largest diversion valley is occupied by the Missouri River; another diversion system, now largely abandoned, extends from the Killdeer Mountains southwest to the mouth of Porcupine Creek in Sioux County. By analogy with South Dakota, most of the large diversion valleys are thought to have been cut in Illinoian time.\r\n\r\nNumerous diversion valleys of Illinoian to late Wisconsin age cut across the divides. Other Pleistocene land forms include ground and moraines, kames, and terraces. Land forms of Recent age include dunes, alluvial terraces, floodplains, and several types of landslide blocks. One type of landslide, called rockslide slump, has not previously been described.\r\n\r\nDrainage is well adjusted to the structure, most of the streams flowing down the axes of small synclines.\r\n\r\nThe bedrock formations have been gently folded into small domes and synclines that interrupt a gentle northward regional dip into the Williston Basin. Three episodes of deformation affected southwestern North Dakota in Tertiary time: (1) intra-Paleocene, involving warping and minor faulting; (2) post-Eocene, involving uplift and tilting; (2) Oligocene, involving uplift and gentle folding.\r\n\r\nMineral resources include ceramic clay, sand and gravel and lignite coal. The Knife River area is the largest lignite-producing district in the United States.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5321","usgsCitation":"Benson, W.E., 1953, Geology of the Knife River area, North Dakota: U.S. Geological Survey Open-File Report 53-21, 318 p, https://doi.org/10.3133/ofr5321.","productDescription":"318 p","costCenters":[],"links":[{"id":499594,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_39546.htm","linkFileType":{"id":5,"text":"html"}},{"id":41066,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144021,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0021/report-thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Knife River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.25,\n              47.525\n            ],\n            [\n              -102.25,\n              47\n            ],\n            [\n              -101.25,\n              47\n            ],\n            [\n              -101.25,\n              47.525\n            ],\n            [\n              -102.25,\n              47.525\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecc0","contributors":{"authors":[{"text":"Benson, William Edward","contributorId":13637,"corporation":false,"usgs":true,"family":"Benson","given":"William","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":166501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57001,"text":"b989B - 1953 - Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska","interactions":[{"subject":{"id":55593,"text":"ofr4720 - 1947 - Preliminary report on the gypsum deposits near Iyoukeen Cove, Chicagof Island, southeastern Alaska","indexId":"ofr4720","publicationYear":"1947","noYear":false,"title":"Preliminary report on the gypsum deposits near Iyoukeen Cove, Chicagof Island, southeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":57001,"text":"b989B - 1953 - Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska","indexId":"b989B","publicationYear":"1953","noYear":false,"chapter":"B","title":"Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska"},"id":1},{"subject":{"id":57001,"text":"b989B - 1953 - Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska","indexId":"b989B","publicationYear":"1953","noYear":false,"chapter":"B","title":"Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska"},"predicate":"IS_PART_OF","object":{"id":33311,"text":"b989 - 1955 - Mineral resources of Alaska, 1951-53","indexId":"b989","publicationYear":"1955","noYear":false,"title":"Mineral resources of Alaska, 1951-53"},"id":2}],"isPartOf":{"id":33311,"text":"b989 - 1955 - Mineral resources of Alaska, 1951-53","indexId":"b989","publicationYear":"1955","noYear":false,"title":"Mineral resources of Alaska, 1951-53"},"lastModifiedDate":"2017-08-08T10:34:50","indexId":"b989B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"989","chapter":"B","title":"Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska","language":"ENGLISH","doi":"10.3133/b989B","usgsCitation":"Flint, G., and Cobb, E., 1953, Gypsum deposits near Iyoukeen Cove, Chichagof Island, southeastern Alaska: U.S. Geological Survey Bulletin 989, 10 p., https://doi.org/10.3133/b989B.","productDescription":"10 p.","costCenters":[],"links":[{"id":100538,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0989b/plate-3.pdf","size":"191","linkFileType":{"id":1,"text":"pdf"}},{"id":180985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0989b/report-thumb.jpg"},{"id":100537,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0989b/report.pdf","size":"727","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a070","contributors":{"authors":[{"text":"Flint, G.M. Jr.","contributorId":79942,"corporation":false,"usgs":true,"family":"Flint","given":"G.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":256066,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cobb, E.H.","contributorId":68729,"corporation":false,"usgs":true,"family":"Cobb","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":256065,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57000,"text":"b989A - 1953 - Geology of Buldir Island, Aleutian Islands, Alaska","interactions":[{"subject":{"id":57000,"text":"b989A - 1953 - Geology of Buldir Island, Aleutian Islands, Alaska","indexId":"b989A","publicationYear":"1953","noYear":false,"chapter":"A","title":"Geology of Buldir Island, Aleutian Islands, Alaska"},"predicate":"IS_PART_OF","object":{"id":33311,"text":"b989 - 1955 - Mineral resources of Alaska, 1951-53","indexId":"b989","publicationYear":"1955","noYear":false,"title":"Mineral resources of Alaska, 1951-53"},"id":1}],"isPartOf":{"id":33311,"text":"b989 - 1955 - Mineral resources of Alaska, 1951-53","indexId":"b989","publicationYear":"1955","noYear":false,"title":"Mineral resources of Alaska, 1951-53"},"lastModifiedDate":"2017-08-08T10:35:05","indexId":"b989A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"989","chapter":"A","title":"Geology of Buldir Island, Aleutian Islands, Alaska","language":"ENGLISH","doi":"10.3133/b989A","usgsCitation":"Coats, R., 1953, Geology of Buldir Island, Aleutian Islands, Alaska: U.S. Geological Survey Bulletin 989, 26 p., https://doi.org/10.3133/b989A.","productDescription":"26 p.","costCenters":[],"links":[{"id":180984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0989a/report-thumb.jpg"},{"id":100536,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0989a/report.pdf","size":"2379","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683fa0","contributors":{"authors":[{"text":"Coats, R.R.","contributorId":78339,"corporation":false,"usgs":true,"family":"Coats","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":256064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57707,"text":"ofr53289 - 1953 - Changes in chemical quality of the Arkansas River in Oklahoma and Arkansas (1946-52)","interactions":[],"lastModifiedDate":"2012-02-02T00:12:29","indexId":"ofr53289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-289","title":"Changes in chemical quality of the Arkansas River in Oklahoma and Arkansas (1946-52)","docAbstract":"Systematic chemical quality-of-water investigations have been carried on in both Oklahoma and Arkansas by the Geological Survey in cooperation with State and Federal agencies during the past several years. Results of the Survey's quality-of-water investigations are usually published in the annual Water-Supply Papers. However, as the Geological Survey has made no sediment investigations in the Arkansas River Basin in Oklahoma and Arkansas, the published data do not include information on sediment concentrations or loads.\r\nThis report attempts to summarize information collected to date in the Arkansas River Basin of the two States, and to show as clearly as possible from present information how the chemical quality of water in the Arkansas River changes downstream from the Oklahoma-Kansas State line to its confluence with the Mississippi River, and how it is affected by tributary inflows. Additional information is being collected and further studies are planned. Hence, the conclusions reached herein may be modified by more adequate information at a later date.\r\n\r\nThe Arkansas River enters Oklahoma near Newkirk on the northern boundary just east of the 97th meridian, crosses the State in a general southeasterly direction flowing past Tulsa, enters Arkansas at its western boundary north of the 35th parallel near Fort Smith, still flowing in a general southeasterly direction past Little Rock near the center of the State, and empties into the Mississippi River east of Dumas.\r\n\r\nThe Arkansas River is subject to many types of pollution downstream from the Oklahoma-Kansas State line, and its inferior quality along with an erratic flow pattern has caused it to be largely abandoned as a source of municipal and industrial water supply. At the present time, the Arkansas River is not directly used as a source of public supply in any part of the basin in either Oklahoma or Arkansas. In general, the river water increases in chemical concentration downstream from the Oklahoma-Kansas State line to Tulsa, due mainly to tributary inflow from the Salt Fork Arkansas River and the Cimarron River, both streams being sources of large amounts of both natural and artificial pollution. A decrease in chemical concentration is noted downstream from Tulsa due to tributary inflow from the Verdigris, Neosho, and Illinois rivers with an increase in chemical concentration then noted due to tributary inflow from the Canadian River which is largely artificial pollution. A steady decrease in concentration is then noted as the river progresses through Arkansas to the Mississippi River, as all major tributaries below the Canadian River have a dilution effect upon the chemical concentration of the Arkansas River water.\r\n\r\nProposals for storage and regulating reservoirs on the Arkansas River in both Oklahoma and Arkansas have been made by the Corps of Engineers and others. Additional proposals are being considered in the present Arkansas-White-Red River Basin Inter-Agency Committee studies. If constructed, these reservoirs will provide an opportunity for control of flow and beneficial use of Arkansas River water, both at and downstream from these sites. Impoundment alone will greatly reduce the extremes in water quality, and by reasonable control of municipal and industrial wastes, the water would be comparable in quality to many existing basin municipal and industrial supplies.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr53289","usgsCitation":"Dover, T., and Geurin, J., 1953, Changes in chemical quality of the Arkansas River in Oklahoma and Arkansas (1946-52): U.S. Geological Survey Open-File Report 53-289, 33 p., https://doi.org/10.3133/ofr53289.","productDescription":"33 p.","costCenters":[],"links":[{"id":182938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5455ef","contributors":{"authors":[{"text":"Dover, T.B.","contributorId":90293,"corporation":false,"usgs":true,"family":"Dover","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":257624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geurin, J.W.","contributorId":59784,"corporation":false,"usgs":true,"family":"Geurin","given":"J.W.","affiliations":[],"preferred":false,"id":257623,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57706,"text":"ofr53288 - 1953 - Summary of annual records of chemical quality of water of the Arkansas River in Oklahoma and Arkansas, 1945-1952","interactions":[],"lastModifiedDate":"2012-02-02T00:12:29","indexId":"ofr53288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-288","title":"Summary of annual records of chemical quality of water of the Arkansas River in Oklahoma and Arkansas, 1945-1952","docAbstract":"This report summarizes information collected to date in the Arkansas River Basin in Oklahoma and Arkansas, and shows, within the limitations of present information, the chemical quality of water in the Arkansas River downstream from the Oklahoma-Kansas State line to its junction with the Mississippi River, and the influence of tributary in-flows. Additional data are being collected and further studies are planned. Hence, conclusions reached herein may be modified by more complete information at a later date.\r\nThe Arkansas River is subject to many types of pollution downstream from the Oklahoma-Kansas State line, and its inferior quality along with an erratic flow pattern has caused it to be largely abandoned as a source of municipal and industrial water supply. Currently, the Arkansas River is not directly used as a source of public supply in any part of the basin in either Oklahoma or Arkansas. In general, the river water increases in chemical concentration downstream from the Oklahoma-Kansas State line to Tulsa due mainly to tributary inflow from the Salt Fork Arkansas River and the Cimarron River, both streams being sources of large amounts of both natural salts and industrial wastes. A decrease in chemical concentration is noted downstream from Tulsa due to tributary inflow from the Verdigris, Neosho, and Illinois rivers, with an increase in chemical concentration then noted due to tributary inflow from the Canadian River which is largely oil field wastes. A steady decrease in concentrations is then noted as the river progresses through Arkansas to the Mississippi River, as all major tributaries below the Canadian River have a dilution effect upon the chemical concentration of the Arkansas River water.\r\n\r\nProposals for storage and regulating reservoirs on the Arkansas River in both Oklahoma and Arkansas have been made by the Corps of Engineers and others. Additional proposals are bing considered in the present Arkansas-White-Red River Basin Inter-Agency Sub-Committee studies. If constructed, these reservoirs will provide an opportunity for control of flow and beneficial use of Arkansas River water both at and downstream from these sites. Impoundment alone will greatly reduce the extremes in water-quality, and by reasonable control of municipal and industrial wastes, the water at some points on the river would be comparable in quality to many existing municipal and industrial supplies in the basin.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr53288","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Summary of annual records of chemical quality of water of the Arkansas River in Oklahoma and Arkansas, 1945-1952: U.S. Geological Survey Open-File Report 53-288, 38 leaves ; 28 cm., https://doi.org/10.3133/ofr53288.","productDescription":"38 leaves ; 28 cm.","costCenters":[],"links":[{"id":182937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6982f7","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":533178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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