In much of western North Dakota, minable lignite beds and associated sand beds are valuable local aquifers. Strip mining disrupts the aquifers and could significantly impact the local hydrology, imposing hardships on local residents. This comprehensive water-resources study of a 147-square-mile coal area in west-central North Dakota was done to facilitate sound management decisions regarding the suitability of the site for mining.
Two strippable lignite beds, identified as the D and E beds, in the lower 250 to 300 feet of the Sentinel Butte Member of the Fort Union Formation underlie much of two small stream basins. The lignites and two closely associated sand deposits are the only consistently occurring aquifers within several hundred feet of the land surface.
The D lignite bed underlies nearly the entire study area, but is not water bearing where it is structurally uplifted beneath upland areas. It is, for the most part, marginally confined. The E lignite bed overlies the D bed and is extensively eroded along North Creek in the southern part of the study area. The E bed is either unsaturated or unconfined in most of its area of occurrence. Direction of ground-water flow in both lignite aquifers is largely controlled by topography.
Interconnected sand beds deposited as channel fill in braided streams form aquifers between the E and D beds (E-D aquifer) and below the D bed (D-HT aquifer). Both aquifers underlie the central part of the study area and each consists of as much as 100 feet of predominantly fine to medium silty unconsolidated sand. Maximum depth to the top of the aquifers was 200 feet for the E-D aquifer and 320 feet for the D-HT aquifer. The E-D aquifer, where near land surface, is unconfined, whereas the D-HT aquifer is entirely confined. Direction of ground-water flow in the D-HT aquifer is not influenced by the local topography as in the three overlying aquifers.
Aquifers also occur at much greater depth beneath the study area in strata of Late Cretaceous and early Tertiary age. The Fox Hills and Tongue River aquifers are most commonly utilized and lie at depths of about 1,700 and 750 feet, respectively.
Water in all aquifers beneath the study area is a sodium bicarbonate or sodium sulfate type. Mean dissolved solids in the four aquifers in the Sentinel Butte Member ranged from 1,290 to 1,970 milligrams per liter- Most of the samples were soft water, had low dissolved iron concentration, and were slightly to moderately colored (tan to brown) by dissolved organics. Several samples from the four aquifers had a perceptible hydrogen sulfide odor.
North Creek and an unnamed tributary of the Green River drain most of the study area. North Creek flows intermittently during most years, while the Green River tributary flows perennially and has base flow of about 0.2 cubic foot per second. North Creek has predominately a sodium sulfate type water and the Green River tributary has a sodium bicarbonate-sulfate type water. At high flows, the dissolved solids generally are less than 1,000 milligrams per liter, and the water contains greater percentages of calcium and magnesium than at low flow.
The impacts of strip mining on the shallow ground-water flow system would be very localized due to the already low water levels and the segmented nature of the flow system. Similarly, water-quality impacts on the ground-water system would be localized. Natural geochemical processes are effective in limiting the severity and lateral spread of chemically enriched waters.
Streamflow magnitudes should not be significantly affected by mining activities. Stream quality impacts should be readily manageable by ordinary routing, impoundment, and treatment techniques.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834228","usgsCitation":"Horak, W., 1983, Water resources of the Rattlesnake Butte area, a site of potential lignite mining in west-central North Dakota: U.S. Geological Survey Water-Resources Investigations Report 83-4228, Report: vi, 53 p. 2 Plates: 23.74 x 12.80 inches and 21.90 x 14.80 inches, https://doi.org/10.3133/wri834228.","productDescription":"Report: vi, 53 p. 2 Plates: 23.74 x 12.80 inches and 21.90 x 14.80 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":56605,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4228/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56606,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4228/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4228/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03d1","contributors":{"authors":[{"text":"Horak, W.F.","contributorId":82326,"corporation":false,"usgs":true,"family":"Horak","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":198649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21376,"text":"ofr83243 - 1983 - Stratigraphic evidence for Devonian tectonism on lineaments at Allegheny Front, West Virginia; supporting material","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr83243","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":"83-243","title":"Stratigraphic evidence for Devonian tectonism on lineaments at Allegheny Front, West Virginia; supporting material","docAbstract":"At the Allegheny Front in northeastern West Virginia, five large structural lineaments trend northwesterly to westerly across the structural grain. This paper concludes that two and perhaps three of them separated structures that were active in Devonian time. \r\n\r\nAlong strike over about 200 km of the Front, J. M. Dennison and coworkers recognized and mapped numerous, mostly thin, shale, siltstone, sandstone, and limestone units in 18 measured sections between the Early Devonian Oriskany Sandstone and the Late Devonian Hampshire Formation. Many of these units terminate in intervals between measured sections. Nonparametric statistical analysis reveals that significant numbers of stratigraphic terminations occur in and between intervals in which three of the five lineaments intersect the Front. \r\n\r\nThe Petersburg and Fairmont-Rowlesburg and perhaps the Bartow lineaments were loci of structural control over topography, bathymetry, or both, and of structural influence on patterns of influx and dispersal of clastic sediment. It is not clear whether this pre-Alleghany activity reflects intermittent motion (1) on a strike-transverse basement fault, as occurred under similar lineaments in Pennsylvania and Alabama, or (2) between Paleozoic thrust masses advancing somewhat independently of each other. However, if the Petersburg lineament formed over a basement fault, it cannot still overlie it because the rocks containing the lineament have been detached and transported too far to the northwest. Of the five lineaments considered, the one most likely to have formed over and to still overlie a basement fault is the Parsons lineament, especially in its northwestern portion in the eastern Plateau province.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83243","usgsCitation":"Wheeler, R.L., 1983, Stratigraphic evidence for Devonian tectonism on lineaments at Allegheny Front, West Virginia; supporting material: U.S. Geological Survey Open-File Report 83-243, i, 25 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83243.","productDescription":"i, 25 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0243/report-thumb.jpg"},{"id":50935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0243/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae82c","contributors":{"authors":[{"text":"Wheeler, R. L.","contributorId":34916,"corporation":false,"usgs":true,"family":"Wheeler","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":184314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11229,"text":"ofr83533 - 1983 - A statistical summary of data from the U.S. Geological Survey's national water quality networks","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr83533","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":"83-533","title":"A statistical summary of data from the U.S. Geological Survey's national water quality networks","docAbstract":"The U.S. Geological Survey Operates two nationwide networks to monitor water quality, the National Hydrologic Bench-Mark Network and the National Stream Quality Accounting Network (NASQAN). The Bench-Mark network is composed of 51 stations in small drainage basins which are as close as possible to their natural state, with no human influence and little likelihood of future development. Stations in the NASQAN program are located to monitor flow from accounting units (subregional drainage basins) which collectively encompass the entire land surface of the nation. Data collected at both networks include streamflow, concentrations of major inorganic constituents, nutrients, and trace metals. The goals of the two water quality sampling programs include the determination of mean constituent concentrations and transport rates as well as the analysis of long-term trends in those variables. This report presents a station-by-station statistical summary of data from the two networks for the period 1974 through 1981. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83533","usgsCitation":"Smith, R.A., and Alexander, R.B., 1983, A statistical summary of data from the U.S. Geological Survey's national water quality networks: U.S. Geological Survey Open-File Report 83-533, 20 p. ;28 cm., https://doi.org/10.3133/ofr83533.","productDescription":"20 p. ;28 cm.","costCenters":[],"links":[{"id":145085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0533/report-thumb.jpg"},{"id":39019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0533/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62c9","contributors":{"authors":[{"text":"Smith, R. A.","contributorId":60584,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, R. B.","contributorId":108103,"corporation":false,"usgs":true,"family":"Alexander","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":59009,"text":"mf1518 - 1983 - Occurrence and distribution chart of Ostracodes from the northeastern Gulf of Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"mf1518","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1518","title":"Occurrence and distribution chart of Ostracodes from the northeastern Gulf of Alaska","language":"ENGLISH","doi":"10.3133/mf1518","usgsCitation":"Brouwers, E., 1983, Occurrence and distribution chart of Ostracodes from the northeastern Gulf of Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1518, 1 chart on 2 sheets ;88 x 124 cm., 103 x 124 cm., folded in envelope 25 x 32 cm. +1 pamphlet (13 p. : map ; 28 cm.), https://doi.org/10.3133/mf1518.","productDescription":"1 chart on 2 sheets ;88 x 124 cm., 103 x 124 cm., folded in envelope 25 x 32 cm. +1 pamphlet (13 p. : map ; 28 cm.)","costCenters":[],"links":[{"id":184977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1518/report-thumb.jpg"},{"id":88578,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1518/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88579,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1518/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1518/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0f9","contributors":{"authors":[{"text":"Brouwers, E. M.","contributorId":98319,"corporation":false,"usgs":true,"family":"Brouwers","given":"E. M.","affiliations":[],"preferred":false,"id":261264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26048,"text":"wri834056 - 1983 - Preliminary plasma spectrometric analyses for selected elements in some geothermal waters from Cerro Prieto, Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri834056","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4056","title":"Preliminary plasma spectrometric analyses for selected elements in some geothermal waters from Cerro Prieto, Mexico","docAbstract":"As part of a cooperative study with Dr. Alfred Truesdell, water samples collected from geothermal power production wells at Cerro Prieto, Mexico, were analyzed for selected elements by d.c. argon plasma emission spectroscopy. Spectral interferences due to the presence of high concentrations of Ca, Si, Na and K in these water affected the apparent concentration values obtained. These effects were evaluated and correction techniques were developed and applied to the analytical values. Precipitates present in the samples at the time of analysis adversely affected the accuracy, precision and interpretability of the data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834056","usgsCitation":"Ball, J., and Jenne, E., 1983, Preliminary plasma spectrometric analyses for selected elements in some geothermal waters from Cerro Prieto, Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4056, iii, 12 p. ;28 cm., https://doi.org/10.3133/wri834056.","productDescription":"iii, 12 p. ;28 cm.","costCenters":[],"links":[{"id":158055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4056/report-thumb.jpg"},{"id":54825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ccaf","contributors":{"authors":[{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":195712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenne, E. A.","contributorId":45716,"corporation":false,"usgs":true,"family":"Jenne","given":"E. A.","affiliations":[],"preferred":false,"id":195711,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11622,"text":"ofr83206 - 1983 - Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","interactions":[{"subject":{"id":11622,"text":"ofr83206 - 1983 - Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","indexId":"ofr83206","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":70043374,"text":"70043374 - 1983 - Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico","indexId":"70043374","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico"},"id":1}],"supersededBy":{"id":70043374,"text":"70043374 - 1983 - Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico","indexId":"70043374","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico"},"lastModifiedDate":"2013-02-12T15:12:04","indexId":"ofr83206","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":"83-206","title":"Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","language":"ENGLISH","publisher":"New Mexico State Engineer,","doi":"10.3133/ofr83206","usgsCitation":"Welder, G.E., 1983, Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico: U.S. Geological Survey Open-File Report 83-206, vi, 66 p. :ill., maps ;26 cm., https://doi.org/10.3133/ofr83206.","productDescription":"vi, 66 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":145438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Chaves County;Eddy County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,31.33 ], [ -109.0,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.0,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ea6","contributors":{"authors":[{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7943,"text":"ofr83432 - 1983 - Montana; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83432","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":"83-432","title":"Montana; basic data for thermal springs and wells as recorded in Geotherm","docAbstract":"Changes in ground-water withdrawals, water levels, and quality of water occurred in the artesian aquifers of the Sevier Desert, Utah during 1963-81. Ground-water withdrawals increased from an average of 9,500 acre-feet (11.7 cubic hectometers) per year between 1951 and 1963 to an average of 27,500 acre-feet (33.9 cubic hectometers) per year between 1964 and 1981. Most of the increased withdrawal was from the deep artesian aquifer. Water levels declined as much as 19 feet (5.8 meters) in the deep artesian aquifer and as much as 13 feet (4.0 meters) in the shallow artesian aquifer between 1963 and 1981. The declines probably are due to increased ground-water withdrawals for irrigation and municipal use. Quality of water in parts of the shallow artesian aquifer is deteriorating. The deterioration probably is the result of recharge of poor quality from the overlying water-table aquifer. A digital-computer model was constructed to predict water-level changes resulting from changes in recharge and discharge for 20 years (1981-2000) at one-half, one, and two times the 1977-79 average rate. The model computer water-level declines of more than 80 feet (24 meters) in the deep artesian aquifer with withdrawals twice the 1977-79 average, declines of more than 40 feet (12 meters) if withdrawals were equal to the 1977-79 average, and declines of more than 15 feet (4.6 meters) if withdrawals were one-half the 1977-79 average. Computer water-level declines after 20 years in the shallow artesian aquifer were more than 50 feet (15 meters) at two times the 1977-79 average rate, more than 15 feet (4.6 meters) at the 1977-79 average, and less than 4 feet (1.2 meters) at one-half the 1977-79 average. The model also was used to predict the effects of approximate changes in ground-water withdrawals related to the Intermountain Power Project. Water-level declines in the deep artesian aquifer of more than 15 feet (4.6 meters), and only small changes in water levels in the shallow artesian aquifer after 20 years. These changes are in addition to changes computed for 20 years of withdrawals at the 1977-79 rate. 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Although pes","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83148","usgsCitation":"Gaydos, M., 1983, Results of pesticide sampling in Tennessee: U.S. Geological Survey Open-File Report 83-148, 24 p. map ;29 cm., https://doi.org/10.3133/ofr83148.","productDescription":"24 p. map ;29 cm.","costCenters":[],"links":[{"id":142429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0148/report-thumb.jpg"},{"id":36628,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0148/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36629,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0148/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613bfb","contributors":{"authors":[{"text":"Gaydos, M.W.","contributorId":35714,"corporation":false,"usgs":true,"family":"Gaydos","given":"M.W.","email":"","affiliations":[],"preferred":false,"id":158662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8990,"text":"ofr83318 - 1983 - Ordovician-Silurian volcanogenic massive sulfide deposits on southern Prince of Wales Island and the Barrier Islands, southeastern Alaska","interactions":[],"lastModifiedDate":"2021-09-30T21:51:11.074258","indexId":"ofr83318","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":"83-318","title":"Ordovician-Silurian volcanogenic massive sulfide deposits on southern Prince of Wales Island and the Barrier Islands, southeastern Alaska","docAbstract":"No abstract available.
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Locations, magnitudes, and selected focal mechanisms for these events and events from prior years of network operations are presented and discussed in relation to the geologic framework of the region. These data are being collected to aid in the evaluation of the seismic hazard to a potential repository site at Yucca Mountain in the southwestern Nevada Test Site. The regional stress field orientation, as inferred from focal mechanisms, is characterized by a northwest-directed least compressive stress and a northeast-directed greatest compressive stress. We infer from this stress orientation that faults of north to northeast trend are most susceptible to slip. Faults of this orientation exist within the Yucca Muntain block, but they probably have not moved significantly in the last 500,000 years. Yucca Mountain lies within a fairly large area of relatively low level seismicity extending west to the Funeral Mountains, south to the Black Mountains and Nopah Range, and southeast to the Spring Mountains. One M 1.7 earthquake has been located in the Yucca Mountain block in about I year of intense monitoring. At present somewhat conflicting geologic, seismologic, and stress evidence hinder definitive conclusions about the seismic hazard at the proposed repository site.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83669","usgsCitation":"Rogers, A.M., Harmsen, S.C., Carr, W.J., and Spence, W., 1983, Southern Great Basin seismological data report for 1981 and preliminary data analysis: U.S. Geological Survey Open-File Report 83-669, ii, 244 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83669.","productDescription":"ii, 244 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0669/report-thumb.jpg"},{"id":46922,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0669/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0669/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e71d0","contributors":{"authors":[{"text":"Rogers, A. 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J.","contributorId":9245,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":177493,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Spence, W.","contributorId":7721,"corporation":false,"usgs":true,"family":"Spence","given":"W.","email":"","affiliations":[],"preferred":false,"id":177492,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47316,"text":"ofr83282 - 1983 - Geologic map of the Red Mountain quadrangle, Harney County, Oregon","interactions":[],"lastModifiedDate":"2021-09-27T21:46:02.613777","indexId":"ofr83282","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":"83-282","title":"Geologic map of the Red Mountain quadrangle, Harney County, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83282","usgsCitation":"Rytuba, J.J., Minor, S., Miller, R.J., and Vander Meulen, D., 1983, Geologic map of the Red Mountain quadrangle, Harney County, Oregon: U.S. Geological Survey Open-File Report 83-282, 1 Plate: 26.78 × 31.15 inches, https://doi.org/10.3133/ofr83282.","productDescription":"1 Plate: 26.78 × 31.15 inches","costCenters":[],"links":[{"id":84261,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0282/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108449,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13962.htm","linkFileType":{"id":5,"text":"html"},"description":"13962"}],"scale":"24000","country":"United States","state":"Oregon","county":"Harney County","otherGeospatial":"Red Mountain quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.25,\n 42.25\n ],\n [\n -118.375,\n 42.25\n ],\n [\n -118.375,\n 42.375\n ],\n [\n -118.25,\n 42.375\n ],\n [\n -118.25,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6913fa","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":235040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":235043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R. 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