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W.","contributorId":70369,"corporation":false,"usgs":true,"family":"Stover","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reagor, B.G.","contributorId":99121,"corporation":false,"usgs":true,"family":"Reagor","given":"B.G.","affiliations":[],"preferred":false,"id":264736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Algermissen, S. T.","contributorId":39790,"corporation":false,"usgs":true,"family":"Algermissen","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":264734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3355,"text":"cir798 - 1979 - Unstable ground in western North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"cir798","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"798","title":"Unstable ground in western North Dakota","docAbstract":"Unstable ground in western North Dakota is mainly the result of mass-wasting processes. The units most affected are mudstones, siltstones, and sandstones of the Fort Union Formation. Ground instability generally is indicated by landslides, soil slides, or subsidence. \r\n\r\nLandslides are mostly of the slump-earthflow type and are localized along the flanks of the high buttes in southwestern North Dakota, including HT (Black) Butte, Chalky Buttes, Sentinel Butte, and East and West Rainy Buttes, and along parts of the valleys of the Des Lacs, Missouri, Little Missouri, and Heart Rivers. Landslides are sparse elsewhere. \r\n\r\nSoil slides are common in the areas south and southwest of the maximum position of the Pleistocene glacial ice margin on slopes of 15 degrees or more, and have taken place on some slopes as gentle as five degrees. The weathered, exposed surface of the Fort Union Formation seems to be especially susceptible to soil slides. Soil slides constitute the major type of ground instability in southwestern North Dakota. \r\n\r\nSubsidence is of two types: (1) subsidence over old underground mine workings, and (2) subsidence over naturally ignited and burned underground coal beds. Major subsidence has taken place over old, underground workings near Beulah, Wilton, Lehigh, Haynes, and Belfield, and lesser subsidence near Scranton, and west and north of Bowman. Thickness of overburden above the coal in all these areas is believed to be less than 30 m (100 ft). Subsidence has not taken place over old underground workings along the Des Lacs and-Souris valleys northwest of Minot, where the thickness of overburden is more than 60 m (200 ft). \r\n\r\nSpectacular subsidence has occurred over a burning underground coal bed at Burning Coal Vein Park near the Little Missouri River, northwest of Amidon.","language":"ENGLISH","publisher":"Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir798","usgsCitation":"Trimble, D.E., 1979, Unstable ground in western North Dakota: U.S. Geological Survey Circular 798, iii, 19 p. :ill., map ;26 cm., https://doi.org/10.3133/cir798.","productDescription":"iii, 19 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":124597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0798/report-thumb.jpg"},{"id":30365,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0798/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d344","contributors":{"authors":[{"text":"Trimble, Donald E.","contributorId":75910,"corporation":false,"usgs":true,"family":"Trimble","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43016,"text":"ofr791564 - 1979 - Simple Bouguer gravity anomaly map and geologic interpretation, Iron River 1 degree by 2 degree Quadrangle, northern Michigan and Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr791564","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1564","title":"Simple Bouguer gravity anomaly map and geologic interpretation, Iron River 1 degree by 2 degree Quadrangle, northern Michigan and Wisconsin","language":"ENGLISH","doi":"10.3133/ofr791564","usgsCitation":"Klasner, J.S., and Jones, W.J., 1979, Simple Bouguer gravity anomaly map and geologic interpretation, Iron River 1 degree by 2 degree Quadrangle, northern Michigan and Wisconsin: U.S. Geological Survey Open-File Report 79-1564, 1 map ;47 x 64 cm. on sheet 107 x 125 cm.; 22 p., https://doi.org/10.3133/ofr791564.","productDescription":"1 map ;47 x 64 cm. on sheet 107 x 125 cm.; 22 p.","costCenters":[],"links":[{"id":168942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1564/report-thumb.jpg"},{"id":80828,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1564/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1564/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3a47","contributors":{"authors":[{"text":"Klasner, J. 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The data have been reexamined and intensities assigned where none had been assigned before, on the basis of available data. Other intensity values were updated from new and additional data sources that were not available at the time of original compilation. Some epicenters were relocated on the basis of new information. The data shown in table 1 are estimates of the most accurate epicenter, magnitude, and intensity of each earthquake, on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed but are incomplete in many instances, especially for ones that occurred before seismic instruments were in universal usage.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1391F","usgsCitation":"Simons, F.S., Armbrustmacher, T., Van Noy, R., Zilka, N.T., Federspiel, F.E., Ridenour, J., and Anderson, L.A., 1979, Mineral resources of the Beartooth Primitive Area and vicinity, Carbon, Park, Stillwater, and Sweet Grass Counties, Montana, and Park County, Wyoming, with a section on interpretation of aeromagnetic data: U.S. Geological Survey Bulletin 1391, Report; viii, 125 p.; 2 Plates: 30.00 × 22.50 inches and 25.50 × 22.50 inches, https://doi.org/10.3133/b1391F.","productDescription":"Report; viii, 125 p.; 2 Plates: 30.00 × 22.50 inches and 25.50 × 22.50 inches","costCenters":[],"links":[{"id":407070,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21504.htm","linkFileType":{"id":5,"text":"html"}},{"id":61141,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1391f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61140,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1391f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61139,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1391f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1391f/report-thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","county":"Carbon County, Park County (MT), Park County (WY), Stillwater County, Sweet Grass County","otherGeospatial":"Beartooth Primitive Area and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.25,\n 44.915\n ],\n [\n -109.333,\n 44.915\n ],\n [\n -109.333,\n 45.417\n ],\n [\n -110.25,\n 45.417\n ],\n [\n -110.25,\n 44.915\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b2dd","contributors":{"authors":[{"text":"Simons, Frank S.","contributorId":42203,"corporation":false,"usgs":true,"family":"Simons","given":"Frank","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":210467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armbrustmacher, T.J.","contributorId":92642,"corporation":false,"usgs":true,"family":"Armbrustmacher","given":"T.J.","affiliations":[],"preferred":false,"id":210470,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Noy, R. 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A digital computer model of these reservoirs and the stream reaches from the reservoirs downstream to the Green River at Calhoun, Ky., was developed to simulate mean daily streamflows. Simulations of 1941 through 1971 water year streamflows were made for both the pre-reservoir and post-reservoir basin conditions, thus supplying homogeneous data sets for low-flow analyses of eight stream sites. The 7-day, 10-year recurrence interval, minimum discharges of the simulated regulated flows exceed those of the simulated natural flows by about 30 cubic feet per second for the Barren River at Bowling Green, Ky., and about 260 cubic feet per second for the Green River at Calhous, Ky. Analyses of the pre-reservoir simulations show that, for seven of the stream sites, the model yields streamflow which have annual minimum 7-day average discharges that are not significantly different, at the 95 percent significance level, from those of the observed flows. Results of the post-reservoir simulations show that actual reservoir operation was not closely matched by the model. Therefore, the low-flow characteristics of the simulated regulated streamflows are merely estimates of those that could be expected if the basin were regulated according to the modeled reservoir operating criteria. 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