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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97361","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Banta, E.R., 1997, Data for water levels, water quality, lithology, and surface-water discharge in the vicinity of Lincoln Park, Colorado, 1961 through 1996: U.S. Geological Survey Open-File Report 97-361, Report: iv, 16 p.; 1 Plate: 28.65 x 36.42 inches, https://doi.org/10.3133/ofr97361.","productDescription":"Report: iv, 16 p.; 1 Plate: 28.65 x 36.42 inches","costCenters":[],"links":[{"id":411033,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18766.htm","linkFileType":{"id":5,"text":"html"}},{"id":270235,"rank":2,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1997/0361/application.zip"},{"id":51825,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51824,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0361/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155982,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0361/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Lincoln Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.243,\n 38.468\n ],\n [\n -105.243,\n 38.404\n ],\n [\n -105.189,\n 38.404\n ],\n [\n -105.189,\n 38.468\n ],\n [\n -105.243,\n 38.468\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62546c","contributors":{"authors":[{"text":"Banta, E. R.","contributorId":63038,"corporation":false,"usgs":true,"family":"Banta","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":188181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21608,"text":"ofr97272 - 1997 - The Areal Extent of Continuous Type Gas Accumulations in Lower Silurian Clinton Sands and Medina Group Sandstones of the Appalachian Basin and the Environments Affected by Their Development","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr97272","displayToPublicDate":"2000-02-01T00:00:00","publicationYear":"1997","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":"97-272","title":"The Areal Extent of Continuous Type Gas Accumulations in Lower Silurian Clinton Sands and Medina Group Sandstones of the Appalachian Basin and the Environments Affected by Their Development","docAbstract":"In order to best preserve and manage our energy and natural resources we must understand the relationships between these resources and the impacts of their development. To further this understanding the U.S. Geological Survey is studying unconventional continuous-type and, to a lesser extent, conventional oil and gas accumulations and the environmental impacts associated with their development. Continuous-type gas accumulations are generally characterized by low matrix permeabilities, large areal extents, and no distinct water contacts. This basin scale map shows the overall extent of these accumulations and the general land use types that may be impacted by their development.\r\n\r\nThe Appalachian Basin has the longest history of oil and gas exploration and production in the United States. Since Drake's Titusville discovery well was drilled in 1859, oil and gas has been continuously produced in the basin. While there is still a great deal of oil and gas production, new field discoveries are rare and relatively small. For most of the second half of the 20th century the Appalachian basin has been considered a mature petroleum province because most of the large plays have already been discovered and developed.\r\n\r\nOne exception to this trend is the Lower Silurian Clinton Sands and Medina Group Gas play which is being developed in New York, Pennsylvania, and Ohio. This continuous-type gas play has been expanding since the early 1970's (see inset maps). In the 1980's economic incentives such as large increases in wellhead prices further stimulated continuous-type gas resource development.\r\n\r\nContinuous-type gas plays can be large in areal extent and in thickness. 'Sweetspots' (areas of greater prodcution) are hard to predict and generally associated with better than average permeabilities, and enhanced by natural fracture systems. With an overall success rate often approaching 90%, drilling most of the play with closely spaced wells is often the best way to maximize gas recovery.\r\n\r\nSome positive economic characteristics associated with the development of these continuous-type accumulations are high success rates, low drilling and development costs, and low water production, which results in low water disposal costs. Large areas within the Appalachian basin with good potential for this type of gas accumulation remain to be tested. Positive environmental characteristics include, a clean energy source, low water production, and relatively low surface impact.\r\n\r\nSome negative characteristics associated with these continuous -type accumulations are low individual well production rates and small well drainage area. Negative environmental characteristics are primarily related to the dense well spacing used to develop the resource to its full potential. Often negative environmental impacts such as surface disturbance can be greatly reduced. The number of well sites can be decreased by using a single centrally located surface location and associated facilities for several directionally or horizonatally drilled wells. This also minimizes the transportation infrastructure (access roads and pipelines) required to maintain the wells and deliver the gas. Visual impacts can be reduced by selecting well locations visible only over short distances.\r\n\r\nWhile the prospective area is large, potential decreases basin- ward and toward the northeast and southwest. These areas are represented by the lower potential plays 6727, 6730, and 6731.\r\n\r\nThe U.S. Geological Survey landuse and landcover data was derived from USGS 1:250,000 and 1:100,000 scale maps. This information was collected between the mid 1970s to mid 1980s. The land use and land cover data was mapped and coded using the Anderson classification system (Anderson, 1975) which is a hierarchical system of general (level 1) to more specific (level 2) characterization. Level 1 characterization was used for this map; the land use and land cover designations are displayed below in the Explanation.\r\n\r\nT","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr97272","issn":"0566-8174","usgsCitation":"Wandrey, C., Ryder, R., Nuccio, V.F., and Aggen, K., 1997, The Areal Extent of Continuous Type Gas Accumulations in Lower Silurian Clinton Sands and Medina Group Sandstones of the Appalachian Basin and the Environments Affected by Their Development: U.S. Geological Survey Open-File Report 97-272, Available online, https://doi.org/10.3133/ofr97272.","productDescription":"Available online","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":153592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11539,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-0272/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683407","contributors":{"authors":[{"text":"Wandrey, C. J.","contributorId":99578,"corporation":false,"usgs":true,"family":"Wandrey","given":"C. J.","affiliations":[],"preferred":false,"id":184890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryder, Robert T.","contributorId":77918,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert T.","affiliations":[],"preferred":false,"id":184889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nuccio, Vito F. vnuccio@usgs.gov","contributorId":853,"corporation":false,"usgs":true,"family":"Nuccio","given":"Vito","email":"vnuccio@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":184888,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aggen, Kerry L.","contributorId":106749,"corporation":false,"usgs":true,"family":"Aggen","given":"Kerry L.","affiliations":[],"preferred":false,"id":184891,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32241,"text":"ofr97852 - 1997 - Revised preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado","interactions":[{"subject":{"id":31876,"text":"ofr9552 - 1995 - Preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado","indexId":"ofr9552","publicationYear":"1995","noYear":false,"title":"Preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":32241,"text":"ofr97852 - 1997 - Revised preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado","indexId":"ofr97852","publicationYear":"1997","noYear":false,"title":"Revised preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado"},"id":1}],"lastModifiedDate":"2017-03-09T11:50:17","indexId":"ofr97852","displayToPublicDate":"2000-02-01T00:00:00","publicationYear":"1997","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":"97-852","title":"Revised preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado","docAbstract":"The Rifle quadrangle extends from the Grand Hogback monocline into the southeastern part of the Piceance basin. In the northeastern part of the map area, the Wasatch Formation is nearly vertical, and over a distance of about 1 km, the dip decreases sharply from about 70-85o to about 15-30o toward the southwest. No evidence of a fault in this zone of sharp change in dip is observed but exposures in the Shire Member of the Wasatch Formation are poor, and few marker horizons that might demonstrate offset are distinct. In the central part of the map area, the Shire Member is essentially flat lying. In the south and southwest part of the map area, the dominant dip is slightly to the north, forming an open syncline that plunges gently to the northwest. Evidence for this fold also exists in the subsurface from drill-hole data. According to Tweto (1975), folding of the early Eocene to Paleocene Wasatch Formation along the Grand Hogback reqired an early Eocene age for the last phase of Laramide compression. We find the attitude of the Wasatch Formation to be nearly horizontal, essentially parallel to the overlying Anvil Points Member of the Eocene Green River Formation; therefore, we have no information that either confirms or disputes that early Eocene was the time of the last Laramide event. Near Rifle Gap in the northeast part of the map area, the Mesaverde Group locally dips about 10o less steeply than the overlying Wasatch Formation, indicating that not only had the formation of the Hogback monocline not begun by the time the Wasatch was deposited at this locality, but the underlying Mesaverde Group was locally tilted slightly toward the present White River uplift. Also the basal part of the Atwell Gulch Member of the Wasatch Formation consists of fine-grained mudstones and siltstones containing sparse sandstone and rare conglomerates, indicating that the source of sediment was not from erosion of the adjacent Upper Cretaceous Mesaverde Group. The most likely source of andesitic conglomerate clasts abundant in the upper part of the Atwell Gulch Member was Late Cretaceous-Early Tertiary andesitic igneous rocks, remnants of which are present southeast of the Piceance Basin (Tweto, 1979). Thinning of the Atwell Gulch and Molina Members to the northwest also suggests a southeastern source of sediments, ruling out a northeastern source related to earlier deformation of the Upper Cretaceous Mesa Verde Group.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97852","usgsCitation":"Shroba, R., and Scott, R.B., 1997, Revised preliminary geologic map of the Rifle Quadrangle, Garfield County, Colorado: U.S. Geological Survey Open-File Report 97-852, 1 over-size sheet, https://doi.org/10.3133/ofr97852.","productDescription":"1 over-size sheet","costCenters":[],"links":[{"id":163167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3219,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-0852/","linkFileType":{"id":5,"text":"html"}},{"id":109006,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18866.htm","linkFileType":{"id":5,"text":"html"},"description":"18866"}],"scale":"1","country":"United States","state":"Colorado","county":"Garfield","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ea5","contributors":{"authors":[{"text":"Shroba, R. R.","contributorId":44133,"corporation":false,"usgs":true,"family":"Shroba","given":"R. R.","affiliations":[],"preferred":false,"id":208062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, R. B.","contributorId":13638,"corporation":false,"usgs":false,"family":"Scott","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":208061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32238,"text":"ofr97289 - 1997 - Digital compilation of landslide overview map of the conterminous United States","interactions":[],"lastModifiedDate":"2022-09-21T21:49:08.862698","indexId":"ofr97289","displayToPublicDate":"2000-02-01T00:00:00","publicationYear":"1997","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":"97-289","title":"Digital compilation of landslide overview map of the conterminous United States","docAbstract":"This dataset consists of polygons enclosing areas of landslide incidence and\r\nsusceptibility for the conterminous United States.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr97289","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1997, Digital compilation of landslide overview map of the conterminous United States: U.S. Geological Survey Open-File Report 97-289, HTML Document, https://doi.org/10.3133/ofr97289.","productDescription":"HTML Document","costCenters":[],"links":[{"id":163118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407190,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18904.htm","linkFileType":{"id":5,"text":"html"}},{"id":3198,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-0289/","linkFileType":{"id":5,"text":"html"}},{"id":373254,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp1183","text":"Professional Paper 1183","linkFileType":{"id":5,"text":"html"},"linkHelpText":"Landslide overview map of the conterminous United States"},{"id":373255,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ofr97289B","text":"Open file Report 97-289-B","linkFileType":{"id":5,"text":"html"},"linkHelpText":"Digital compilation of landslide overview map of the conterminous United States"}],"country":"United States","otherGeospatial":"conterminous United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"geometry\": {\n \"type\": \"MultiPolygon\",\n \"coordinates\": [\n [\n [\n [\n -94.81758,\n 49.38905\n ],\n [\n -94.64,\n 48.84\n ],\n [\n -94.32914,\n 48.67074\n ],\n [\n -93.63087,\n 48.60926\n ],\n [\n -92.61,\n 48.45\n ],\n [\n -91.64,\n 48.14\n ],\n [\n -90.83,\n 48.27\n ],\n [\n -89.6,\n 48.01\n ],\n [\n -89.27292,\n 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J.","contributorId":104055,"corporation":false,"usgs":true,"family":"Bragg","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":187706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oman, J. K.","contributorId":97515,"corporation":false,"usgs":true,"family":"Oman","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":187705,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tewalt, S.J.","contributorId":55838,"corporation":false,"usgs":true,"family":"Tewalt","given":"S.J.","affiliations":[],"preferred":false,"id":187703,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oman, C.L.","contributorId":95893,"corporation":false,"usgs":true,"family":"Oman","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":187704,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rega, N. H.","contributorId":8469,"corporation":false,"usgs":true,"family":"Rega","given":"N.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":187700,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Washington, P. M.","contributorId":29453,"corporation":false,"usgs":true,"family":"Washington","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187702,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Finkelman, R. B.","contributorId":20341,"corporation":false,"usgs":true,"family":"Finkelman","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":187701,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":24505,"text":"ofr96684 - 1997 - Biostratigraphic data for the Cretaceous marine sediments in the USGS-St. George no. 1 core (DOR-211), Dorchester County, South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr96684","displayToPublicDate":"1999-05-01T00:00:00","publicationYear":"1997","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":"96-684","title":"Biostratigraphic data for the Cretaceous marine sediments in the USGS-St. George no. 1 core (DOR-211), Dorchester County, South Carolina","docAbstract":"The USGS-St. George corehole was drilled for the U.S. Geological Survey (USGS) by a commercial drilling company during 1982. The corehole is located within the Coastal Plain Province in northern Dorchester County, South Carolina, about three miles southeast of the town of St. George near the village of Byrd (fig. 1). Coordinates for the corehole are 33o09'25'N latitude and 80o31'18'W longitude; ground elevation at the site is +78 feet (Reid and others, 1986). The St. George corehole is designated as USGS drill hole DOR-211. \r\n\r\nThe St. George corehole was drilled to a total depth of 2,067 ft. The hole was cored continuously with generally good recovery from 300 ft to its total depth. Spot cores were taken at selected intervals between the top of the hole and a depth of 300 ft (50-55 ft, 100-110 ft, 150-165 ft, 200-205 ft, and 250-255 ft); however, recovery was poor in most of these intervals. The St. George core currently is stored at the USGS National Center, Reston, VA (March, 1997). \r\n\r\nThe St. George corehole bottomed in basalt of probable early Mesozoic age beneath an Upper Cretaceous and Cenozoic sedi-mentary section. Reid and others (1986) placed the top of basalt saprolite at 1,962 ft in the hole. Our examination of the geophysical logs and original core descriptions suggests that the top of the saprolite is higher in the hole, at about 1,939 ft. The Cretaceous-Tertiary boundary was placed at or near 550 ft in the core by Reid and others (1986) and by Habib and Miller (1989). \r\n\r\nIn this report, we provide paleontologic data for marine sediments in the upper part of the Upper Cretaceous section in the St. George core. Biostratigraphic and paleoenvironmental data and interpretations based on the study of calcareous nannofossils and ostracodes from the Cretaceous section are discussed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96684","issn":"0094-9140","usgsCitation":"Self-Trail, J.M., and Gohn, G., 1997, Biostratigraphic data for the Cretaceous marine sediments in the USGS-St. George no. 1 core (DOR-211), Dorchester County, South Carolina: U.S. Geological Survey Open-File Report 96-684, 29 leaves :ill., map ;28 cm. + 1 computer disk ; 3 1/2 in., https://doi.org/10.3133/ofr96684.","productDescription":"29 leaves :ill., map ;28 cm. + 1 computer disk ; 3 1/2 in.","costCenters":[],"links":[{"id":1606,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://geology.usgs.gov/pdf/of96-684.html","linkFileType":{"id":5,"text":"html"}},{"id":156759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0684/report-thumb.jpg"},{"id":53564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a34e4b07f02db61971b","contributors":{"authors":[{"text":"Self-Trail, Jean M. jstrail@usgs.gov","contributorId":2205,"corporation":false,"usgs":true,"family":"Self-Trail","given":"Jean","email":"jstrail@usgs.gov","middleInitial":"M.","affiliations":[{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true}],"preferred":false,"id":192044,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gohn, Gregory S.","contributorId":50155,"corporation":false,"usgs":true,"family":"Gohn","given":"Gregory S.","affiliations":[],"preferred":false,"id":192045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3003,"text":"wsp2450 - 1997 - Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway","interactions":[{"subject":{"id":24896,"text":"ofr95428 - 1996 - Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway","indexId":"ofr95428","publicationYear":"1996","noYear":false,"title":"Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway"},"predicate":"SUPERSEDED_BY","object":{"id":3003,"text":"wsp2450 - 1997 - Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway","indexId":"wsp2450","publicationYear":"1997","noYear":false,"title":"Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway"},"id":1}],"lastModifiedDate":"2017-09-19T18:13:25","indexId":"wsp2450","displayToPublicDate":"1999-05-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2450","title":"Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway","docAbstract":"The water and salt balance of Great Salt Lake primarily depends on the amount of inflow from tributary streams and the conveyance properties of a causeway constructed during 1957-59 that divides the lake into the south and north parts. The conveyance properties of the causeway originally included two culverts, each 15 feet wide, and the permeable rock-fill material.
During 1980-86, the salt balance changed as a result of record high inflow that averaged 4,627,000 acre-feet annually and modifications made to the conveyance properties of the causeway that included opening a 300-foot-wide breach. In this study, a model developed in 1973 by Waddell and Bolke to simulate the water and salt balance of the lake was revised to accommodate the high water-surface altitude and modifications made to the causeway. This study, done by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of State Lands and Forestry, updates the model with monitoring data collected during 1980-86. This report describes the calibration of the model and presents the results of simulations for three hypothetical 10-year periods.
During January 1, 1980, to July 31, 1984, a net load of 0.5 billion tons of dissolved salt flowed from the south to the north part of the lake primarily as a result of record inflows. From August 1, 1984, when the breach was opened, to December 31,1986, a net load of 0.3 billion tons of dissolved salt flowed from the north to the south part of the lake primarily as a result of the breach.
For simulated inflow rates during a hypothetical 10-year period resulting in the water-surface altitude decreasing from about 4,200 to 4,192 feet, there was a net movement of about 1.0 billion tons of dissolved salt from the south to the north part, and about 1.7 billion tons of salt precipitated in the north part. For simulated inflow rates during a hypothetical 10-year period resulting in a rise in water-surface altitude from about 4,200 to 4,212 feet, there was a net movement of about 0.2 billion tons of dissolved salt from the south to the north part and no salt was precipitated in the north part of the lake.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wsp2450","isbn":"0-607-86822-8","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of State Lands and Forestry","usgsCitation":"Wold, S.R., Thomas, B.E., and Waddell, K.M., 1997, Water and salt balance of Great Salt Lake, Utah, and simulation of water and salt movement through the causeway: U.S. Geological Survey Water Supply Paper 2450, vi, 64 p., https://doi.org/10.3133/wsp2450.","productDescription":"vi, 64 p.","numberOfPages":"75","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2450/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2450/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4987e4b07f02db5af1b1","contributors":{"authors":[{"text":"Wold, Steven R.","contributorId":103262,"corporation":false,"usgs":true,"family":"Wold","given":"Steven","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Blakemore E.","contributorId":93871,"corporation":false,"usgs":true,"family":"Thomas","given":"Blakemore","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":146131,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24818,"text":"ofr97744 - 1997 - General distribution of geologic materials in the San Francisco Bay region, California: A digital map database","interactions":[{"subject":{"id":21355,"text":"ofr93693 - 1993 - General distribution of geologic materials in the southern San Francisco Bay Region, California: A digital map database","indexId":"ofr93693","publicationYear":"1993","noYear":false,"title":"General distribution of geologic materials in the southern San Francisco Bay Region, California: A digital map database"},"predicate":"SUPERSEDED_BY","object":{"id":24818,"text":"ofr97744 - 1997 - General distribution of geologic materials in the San Francisco Bay region, California: A digital map database","indexId":"ofr97744","publicationYear":"1997","noYear":false,"title":"General distribution of geologic materials in the San Francisco Bay region, California: A digital map database"},"id":1}],"lastModifiedDate":"2021-11-17T21:03:26.691453","indexId":"ofr97744","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-744","title":"General distribution of geologic materials in the San Francisco Bay region, California: A digital map database","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97744","issn":"0094-9140","usgsCitation":"Wentworth, C.M., 1997, General distribution of geologic materials in the San Francisco Bay region, California: A digital map database: U.S. Geological Survey Open-File Report 97-744, 27 p., https://doi.org/10.3133/ofr97744.","productDescription":"27 p.","costCenters":[],"links":[{"id":156917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1840,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/of97-744/","linkFileType":{"id":5,"text":"html"}},{"id":108384,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13164.htm","linkFileType":{"id":5,"text":"html"},"description":"13164"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.533,\n 36.875\n ],\n [\n -121.208,\n 36.875\n ],\n [\n -121.208,\n 38.875\n ],\n [\n -123.533,\n 38.875\n ],\n [\n -123.533,\n 36.875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0fcf","contributors":{"authors":[{"text":"Wentworth, C. M.","contributorId":55453,"corporation":false,"usgs":true,"family":"Wentworth","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24725,"text":"ofr97203 - 1997 - Hydrologic and water-quality data related to the occurrence of arsenic for areas along the Madison and Upper Missouri Rivers, southwestern and west-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"ofr97203","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-203","title":"Hydrologic and water-quality data related to the occurrence of arsenic for areas along the Madison and Upper Missouri Rivers, southwestern and west-central Montana","docAbstract":"Geothermal waters in Yellowstone National Park contribute large quantities of arsenic to the headwaters of the Madison River. Water in some Quaternary and Tertiary valley-fill deposits along the Madison and upper Missouri Rivers also is locally enriched in arsenic. Arsenic in surface and ground water in these valleys is an important public- health concern because arsenic concentrations frequently exceed the State of Montana water- quality human health standard of 18 micrograms per liter as well as the U.S. Environmental Protection Agency Maximum Contaminant Level of 50 micrograms per liter. This report presents hydrologic and water-quality data for the Madison and upper Missouri Rivers and selected tributaries, irrigation supply canals or ditches, drains, springs and seeps, for Lake Helena, and for ground water in adjacent areas. Hydrologic and water-quality data were collected and compiled to provide information to more fully understand the extent, magnitude, and source of arsenic in surface and ground water along the Madison and upper Missouri Rivers; to assess, to the extent possible, the mechanisms that control arsenic concentrations; and to assess the effect of irrigation on arsenic concentrations. Hydrologic and arsenic- concentration data were collected by the U.S. Geological Survey and other agencies for 104 surface-water sites and 273 ground-water sites during this and previous studies. The quality of analytical results for arsenic concentrations was evaluated by quality-control samples that were submitted from the field and analyzed in the laboratory with routing samples. Quality-control samples consisted of replicates, standard reference samples, interlaboratory comparison samples, and field blanks.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor,","doi":"10.3133/ofr97203","issn":"0094-9140","usgsCitation":"Tuck, L., Dutton, D., and Nimick, D., 1997, Hydrologic and water-quality data related to the occurrence of arsenic for areas along the Madison and Upper Missouri Rivers, southwestern and west-central Montana: U.S. Geological Survey Open-File Report 97-203, v, 124 p. (some folded) :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr97203.","productDescription":"v, 124 p. (some folded) :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":157778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0203/report-thumb.jpg"},{"id":53751,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6116ce","contributors":{"authors":[{"text":"Tuck, L.K.","contributorId":54247,"corporation":false,"usgs":true,"family":"Tuck","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":192444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutton, D.M.","contributorId":67923,"corporation":false,"usgs":true,"family":"Dutton","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":192445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nimick, D. A.","contributorId":70399,"corporation":false,"usgs":true,"family":"Nimick","given":"D. A.","affiliations":[],"preferred":false,"id":192446,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28237,"text":"wri974132 - 1997 - Water-quality assessment of the Trinity River Basin, Texas — Nutrients and pesticides in the watersheds of Richland and Chambers Creeks, 1993-95","interactions":[],"lastModifiedDate":"2021-12-16T20:25:18.758611","indexId":"wri974132","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-4132","title":"Water-quality assessment of the Trinity River Basin, Texas — Nutrients and pesticides in the watersheds of Richland and Chambers Creeks, 1993-95","docAbstract":"A study of nutrients and pesticides was conducted during February-August 1995 in the west-central part of the Trinity River Basin, where land commonly is used for growing crops. Water and bed-sediment samples were collected at 8 small reservoir sites in the headwaters (known as Natural Resources Conservation Service reservoirs), at 5 stream sites, and at 3 Richland-Chambers Reservoir sites. The analysis included data from the Chambers Creek near Rice site (08064100), which was sampled repeatedly during March 1993-September 1995.\r\n\r\nTotal nitrogen concentrations in the Natural Resources Conservation Service reservoirs were less than 1.0 milligram per liter, as nitrogen, except in 2 of the 8 reservoirs. For the five stream sites, total nitrogen concentrations at the beginning of the study ranged from 0.5 to 1.8 milligrams per liter. Peaks were noted in all stream sites during either March or April; the greatest peak concentration was 4.8 milligrams per liter, as nitrogen. By the end of the study, concentrations decreased to less than 1.2 milligrams per liter, as nitrogen. In the Richland-Chambers Reservoir, the February-March and June sampling showed total nitrogen concentrations of about 0.6 milligram per liter, as nitrogen.\r\n\r\nAt the beginning of the study, all five of the stream sites had total phosphorus concentrations less than 0.04 milligram per liter, as phosphorus. Peak concentrations in the streams occurred in the May sampling except at one site. Two sites had concentrations greater than 0.2 milligram per liter, as phosphorus. By the end of the study, concentrations decreased to less than 0.04 milligram per liter, as phosphorus, except at one site where the concentrations were about 0.08 milligram per liter. Concentrations in the Richland-Chambers Reservoir were less than 0.04 milligram per liter, as phosphorus.\r\n\r\nTotal nitrogen and total phosphorus concentrations generally increased with streamflow and with the percentage of cropland in the drainage area upstream from the sampling site.\r\n\r\nHerbicides were detected in the streams much more often than insecticides were. Nineteen herbicides and 9 insecticides were detected at the 08064100 Chambers Creek near Rice site. Atrazine and metolachlor, the most commonly detected herbicides, occurred in all samples at this site. Other herbicides detected in 25 percent or more of the samples were alachlor, fluometuron, prometon, simazine, trifluralin, and 2,4-D.\r\n\r\nAt the beginning of the study, the number of herbicides detected in the five stream sites was 4 or 5. The greatest number of herbicides detected in the streams occurred in May samples, ranging from 7 to 10. The number of herbicides detected in the Richland-Chambers Reservoir ranged from 6 to 8. Generally, more herbicides were detected in high-streamflow samples than in low-streamflow samples. However, a consistent relation between the number of herbicides in samples and the percentage of cropland in a drainage area was not evident.\r\n\r\nAt the beginning of the study, atrazine concentrations at the stream sites were less than 0.4 microgram per liter, except at one site. In the streams, concentrations peaked in March and April; the greatest peak concentration was 20 micrograms per liter. By the end of the study, atrazine concentrations decreased to less than 0.4 microgram per liter at all the stream sites. In the Richland-Chambers Reservoir, the concentrations were about 1 microgram per liter during February-March and about 3 micrograms per liter in June. Atrazine concentrations tended to increase with increasing streamflow. A consistent relation between atrazine concentrations and the percentage of cropland in a drainage area was not evident.\r\n\r\nThe greatest number of insecticides detected in water samples was two. Diazinon, the most frequently detected insecticide, had slightly greater concentrations in May and June - between 0.01 and 0.02 microgram per liter.\r\n\r\nThe only organochlorine insecticides detected in bed-sedime","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri974132","usgsCitation":"Land, L.F., 1997, Water-quality assessment of the Trinity River Basin, Texas — Nutrients and pesticides in the watersheds of Richland and Chambers Creeks, 1993-95: U.S. Geological Survey Water-Resources Investigations Report 97-4132, vi, 23 p., https://doi.org/10.3133/wri974132.","productDescription":"vi, 23 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":393014,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44860.htm"},{"id":57064,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4132/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Trinity River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.1667,\n 31.9\n ],\n [\n -96,\n 31.9\n ],\n [\n -96,\n 32.3917\n ],\n [\n -97.1667,\n 32.3917\n ],\n [\n -97.1667,\n 31.9\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcacb","contributors":{"authors":[{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28612,"text":"wri974115 - 1997 - Agricultural land-use classification using landsat imagery data, and estimates of irrigation water use in Gooding, Jerome, Lincoln, and Minidoka counties, 1992 water year, Upper Snake River basin, Idaho and western Wyoming","interactions":[],"lastModifiedDate":"2013-11-22T14:33:37","indexId":"wri974115","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-4115","title":"Agricultural land-use classification using landsat imagery data, and estimates of irrigation water use in Gooding, Jerome, Lincoln, and Minidoka counties, 1992 water year, Upper Snake River basin, Idaho and western Wyoming","docAbstract":"As part of the U.S. Geological Survey's \nNational Water-Quality Assessment Program in \nthe upper Snake River Basin study unit, land- and \nwater-use data were used to describe activities that \nhave potential effects on water quality, including \nbiological conditions, in the basin. Land-use maps \nand estimates of water use by irrigated agriculture \nwere needed for Gooding, Jerome, Lincoln, and \nMinidoka Counties (south-central Idaho), four of \nthe most intensively irrigated counties in the study \nunit. Land use in the four counties was mapped \nfrom Landsat Thematic Mapper imagery data for \nthe 1992 water year using the SPECTRUM computer \nprogram. Land-use data were field verified in \n108 randomly selected sections (640 acres each); \nresults compared favorably with land-use maps \nfrom other sources. Water used for irrigation during \nthe 1992 water year was estimated using land-use \nand ancillary data. In 1992, a drought year, estimated \nirrigation withdrawals in the four counties \nwere about 2.9 million acre-feet of water. Of the \n2.9 million acre-feet, an estimated 2.12 million \nacre-feet of water was withdrawn from surface \nwater, mainly the Snake River, and nearly \n776,000 acre-feet was withdrawn from ground \nwater. One-half of the 2.9 million acre-feet of water \nwithdrawn for irrigation was considered to be lost \nduring conveyance or was returned to the Snake \nRiver; the remainder was consumptively used by \ncrops during the growing season.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/wri974115","usgsCitation":"Maupin, M.A., 1997, Agricultural land-use classification using landsat imagery data, and estimates of irrigation water use in Gooding, Jerome, Lincoln, and Minidoka counties, 1992 water year, Upper Snake River basin, Idaho and western Wyoming: U.S. Geological Survey Water-Resources Investigations Report 97-4115, vi, 29 p., https://doi.org/10.3133/wri974115.","productDescription":"vi, 29 p.","numberOfPages":"35","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":119789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4115/report-thumb.jpg"},{"id":57436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4115/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Albers Equal-Area projection","country":"United States","state":"Idaho;Wyoming","city":"Gooding County;Jerome County;Lincoln County;Minidoka County","otherGeospatial":"Snake River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.25,41.5003 ], [ -115.25,44.7623 ], [ -109.7496,44.7623 ], [ -109.7496,41.5003 ], [ -115.25,41.5003 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68909a","contributors":{"authors":[{"text":"Maupin, Molly A. 0000-0002-2695-5505 mamaupin@usgs.gov","orcid":"https://orcid.org/0000-0002-2695-5505","contributorId":951,"corporation":false,"usgs":true,"family":"Maupin","given":"Molly","email":"mamaupin@usgs.gov","middleInitial":"A.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29908,"text":"wri974119 - 1997 - Potentiometric surface and specific conductance of the Sparta and Memphis aquifers in eastern Arkansas, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri974119","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-4119","title":"Potentiometric surface and specific conductance of the Sparta and Memphis aquifers in eastern Arkansas, 1995","docAbstract":"The Sparta and Memphis aquifers in eastern and south-central Arkansas are a major source of water for industrial, public supply, and agricultural uses. An estimated 240 million gallons per day was withdrawn from the Sparta and Memphis aquifers in 1995, an increase of about 17 million gallons per day from 1990. During the spring and early summer of 1995, the water level in the Sparta and Memphis aquifers was measured in 145 wells, the specific conductance of 101 ground-water samples collected from those aquifers was measured. Maps of areal distribution of potentiometric surface and specific conductance generated from these data reveal spatial trends in these parameters across the eastern and south-central Arkansas study area. The altitude of the potentiometric surface ranged from about 206 feet below sea level in Union County to about 307 feet above sea level in Saline County.\r\nThe potentiometric surface of the Sparta and Memphis aquifers contains cones of depression descending below sea level in the central and southern portions of the study area, and a potentiometric high along the western study area boundary. Major recharge areas exhibit potentiometric highs greater than 200 feet above sea level and specific conductance values less than 200 microsiemens per centimeter, and generally are located in the outcrop/subcrop areas on the southern one-third of the western boundary and the northern portion of the study area. The regional direction of ground-water flow is from the north and west to the south and east, away from the outcrop and subcrop and northern regions, except near areas affected by intense ground-water withdrawals; such areas are manifested by large cones of depression centered in Columbia, Jefferson, and Union Counties. The cones of depression in adjoining Columbia and Union Counties are coalescing at or near sea level. The lowest water level measured was about 206 feet below sea level in Union County. Increased specific conductance values were measured in the areas of the cones of depression in Columbia and Union Counties.\r\nThe cones of depression centered in Jefferson County coincides with an elongate area where ground water in the aquifer has low specific conductance. This area extends eastward from the outcrop/subcrop region of recharge. This extension of ground water with low specific conductance possibly indicates increased ground-water movement to the east-southeast from the outcrop/subcrop area induced by ground- water withdrawals in Jefferson County. Specific conductance increases markedly to the northeast and gradually to the south of this area.\r\nLong-term hydrographs of eight wells in the study areas, during the period 1970-1995, reveal water-level declines ranging from less than 0.5 foot per year in Phillips County to more than 2.0 feet per year in Union County. Water-level declines of greater than 1.5 feet per year generally are associated with the cones of depression centered in Columbia, Jefferson, and Union Counties.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974119","usgsCitation":"Stanton, G.P., 1997, Potentiometric surface and specific conductance of the Sparta and Memphis aquifers in eastern Arkansas, 1995: U.S. Geological Survey Water-Resources Investigations Report 97-4119, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974119.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4119/report-thumb.jpg"},{"id":58725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58726,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4119/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a4b3","contributors":{"authors":[{"text":"Stanton, Gregory P. 0000-0001-8622-0933 gstanton@usgs.gov","orcid":"https://orcid.org/0000-0001-8622-0933","contributorId":1583,"corporation":false,"usgs":true,"family":"Stanton","given":"Gregory","email":"gstanton@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":202334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28570,"text":"wri974087 - 1997 - Characteristics of fish assemblages and related environmental variables for streams of the upper Snake River basin, Idaho and western Wyoming, 1993-95","interactions":[],"lastModifiedDate":"2013-11-22T14:24:50","indexId":"wri974087","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-4087","title":"Characteristics of fish assemblages and related environmental variables for streams of the upper Snake River basin, Idaho and western Wyoming, 1993-95","docAbstract":"Fish assemblages and environmental variables \nwere evaluated for 30 first- through seventh-order \nstreams in the upper Snake River Basin, \nIdaho and western Wyoming. Data were collected \nas part of the National Water-Quality Assessment \nProgram to characterize aquatic biota and associated \nhabitats in surface water. Sampling sites represented \nmajor stream types in the basin large \nriver, agricultural, and least-disturbed reference \nstreams and springs in forested and (or) rangeland \nwatersheds.
\nTwenty-four environmental variables representing \nvarious spatial scales, from watershed \ncharacteristics to instream habitat and physicochemical \nmeasures, were used to examine relations \nwith fish assemblages. Twenty-six fish species in \nthe families Catostomidae, Centrarchidae, Cottidae, \nCyprinidae, Ictaluridae, Percidae, and Salmonidae \nwere collected. Detrended correspondence \nanalysis and canonical correspondence analysis \ndifferentiated fish assemblages on the basis of site \ntype and showed that fish assemblages were most \nstrongly correlated with percent agricultural and \nforest land uses, stream width, watershed size, and \nelevation. Fish assemblages did not correspond to \nthe four major ecoregions in the basin. Comparisons \nbetween multiple-year and multiple-reach \ncollections using Jaccard's coefficient of community \nsimilarity index generally indicated little difference \nin fish assemblages. Percent substrate fines, \npercent embeddedness, and specific conductance \ntypically were higher for streams influenced by \nagricultural land use than for reference streams in \nforested and (or) rangeland watersheds. The number \nof native species, percent introduced species, \npercent omnivores, percent common carp, percent \nsalmonids, and percent coldwater-adapted species \nvaried according to site type. Percent omnivores \nand percent common carp were higher for large \nriver and agricultural sites than for reference \nstream and spring sites. The introduction of intolerant \nsalmonid species throughout the basin confounds \nthe use of introduced species as a measure \nof environmental disturbance.
\nAnalysis offish metrics identified some large \nriver and agricultural sites in the lower part of the \nbasin that did not support viable coldwater fish \nassemblages. These sites characteristically were \ndominated by tolerant, warmwater-adapted species. \nThe findings of this study support the waterquality-\nlimited designation for the middle reach of \nthe Snake River between Milner Dam and King \nHill and provide a framework for developing indices \nof biotic integrity by using fish assemblages to \nevaluate water quality of streams in the upper \nSnake River Basin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/wri974087","usgsCitation":"Maret, T.R., 1997, Characteristics of fish assemblages and related environmental variables for streams of the upper Snake River basin, Idaho and western Wyoming, 1993-95: U.S. Geological Survey Water-Resources Investigations Report 97-4087, vii, 50 p., https://doi.org/10.3133/wri974087.","productDescription":"vii, 50 p.","numberOfPages":"58","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":126343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4087/report-thumb.jpg"},{"id":57398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Albers Equal-Area projection","country":"United States","state":"Idaho;Wyoming","otherGeospatial":"King Hill;Milner Dam;Snake River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.25,41.5003 ], [ -115.25,44.7623 ], [ -109.7496,44.7623 ], [ -109.7496,41.5003 ], [ -115.25,41.5003 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e501c","contributors":{"authors":[{"text":"Maret, Terry R. trmaret@usgs.gov","contributorId":953,"corporation":false,"usgs":true,"family":"Maret","given":"Terry","email":"trmaret@usgs.gov","middleInitial":"R.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":200044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32082,"text":"ofr97172 - 1997 - Map showing outcrop of the coal-bearing units and land use in the Gulf Coast region","interactions":[],"lastModifiedDate":"2024-01-11T22:41:58.327273","indexId":"ofr97172","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-172","title":"Map showing outcrop of the coal-bearing units and land use in the Gulf Coast region","docAbstract":"This map is a preliminary compilation of the outcrop geology of the known coal-bearing units in the Gulf Coast Coal region. The map has been compiled for use in the National Coal Resource Assessment Project currently being conducted by the U.S. Geological Survey, and will be updated as the assessment progresses. The purpose of the map is to show the distribution of coal-bearing rocks in the Gulf Coastal Plain Region and to show stratigraphic correlations, transportation network, fossil-fuel burning power plants, and federally managed lands in the region. It is hoped that this map may aid coal exploration and development in the region. Geologic contacts were digitized from paper copies of the maps listed in the reference section below. The primary source of information was the 1:500,000-scale state geology map series, but larger scale maps were use to better define certain areas, notably the Jackson-Claiborne contact in western Kentucky and Tennessee for example (Olive, 1980). Contacts along state boundaries were modified to best-fit information available from the border areas. Note that coal distribution in the mapped units is not uniform. For example, the Jackson Group contains coal in Texas, but in Mississippi is not presently known to contain significant coal deposits. The unit is widespread and in part non-marine and thus of potential future interest. In contrast, the Jackson Group is not shown in Georgia where it is mostly marine and residuum (weathered material) at the surface. Tertiary age coal has also been noted in the Vicksburg Group (Oligocene) of Louisiana and Mississippi, but is not shown on this map. Contacts with mapped surficial units are not always shown. The locations of coal mine permit boundaries are based on information available at the time of publication and were obtained from the Division of Surface Mining and Reclamation, Railroad Commission of Texas, Austin, and the Injection and Mining Division, Department of Natural Resources, Baton Rouge, Louisiana. The correlation of map units and formation names generally follow Galloway and others (1991). We have placed the Paleocene-Eocene boundary in the middle of the Calvert Bluff Formation in Texas based on unpublished pollen biostratigraphy reports (N.O. Fredericksen, unpublished data, 1993; D.J. Nichols, unpublished data, 1996).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97172","usgsCitation":"1997, Map showing outcrop of the coal-bearing units and land use in the Gulf Coast region: U.S. Geological Survey Open-File Report 97-172, 1 Plate: 13.00 x 9.00 inches, https://doi.org/10.3133/ofr97172.","productDescription":"1 Plate: 13.00 x 9.00 inches","costCenters":[],"links":[{"id":424357,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18742.htm","linkFileType":{"id":5,"text":"html"}},{"id":3372,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/of97-172/","linkFileType":{"id":5,"text":"html"}},{"id":166261,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2000000","country":"United States","state":"Alabama, Arkansas, Georgia, Florida, Kansas, Kentucky, Louisiana, Mississippi, Missouri, North Carolina, Oklahoma, Tennessee, Texas, South Carolina, Virginia","otherGeospatial":"Gulf Coast region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101,\n 26\n ],\n [\n -73,\n 26\n ],\n [\n -73,\n 37\n ],\n [\n -101,\n 37\n ],\n [\n -101,\n 26\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6553ef","contributors":{"compilers":[{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":726358,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"SanFilipo, John R. 0000-0002-8739-5628 jsan@usgs.gov","orcid":"https://orcid.org/0000-0002-8739-5628","contributorId":2385,"corporation":false,"usgs":true,"family":"SanFilipo","given":"John R.","email":"jsan@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":726359,"contributorType":{"id":3,"text":"Compilers"},"rank":2},{"text":"Crowley, Sharon S.","contributorId":78325,"corporation":false,"usgs":true,"family":"Crowley","given":"Sharon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":726360,"contributorType":{"id":3,"text":"Compilers"},"rank":3},{"text":"Thomas, Roger E.","contributorId":87899,"corporation":false,"usgs":true,"family":"Thomas","given":"Roger","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":726361,"contributorType":{"id":3,"text":"Compilers"},"rank":4},{"text":"Freid, John","contributorId":25220,"corporation":false,"usgs":true,"family":"Freid","given":"John","email":"","affiliations":[],"preferred":false,"id":726362,"contributorType":{"id":3,"text":"Compilers"},"rank":5},{"text":"Tully, John K.","contributorId":72038,"corporation":false,"usgs":true,"family":"Tully","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":726363,"contributorType":{"id":3,"text":"Compilers"},"rank":6}]}} ,{"id":38101,"text":"ofr97693 - 1997 - Preliminary geologic map of the Little Piute Mountains, California: A digital database","interactions":[],"lastModifiedDate":"2023-05-02T20:51:30.742868","indexId":"ofr97693","displayToPublicDate":"1999-04-01T00:00:00","publicationYear":"1997","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":"97-693","title":"Preliminary geologic map of the Little Piute Mountains, California: A digital database","docAbstract":"The Little Piute Mountains Digital database contains digital geologic and geographic information for the study area. The geology was mapped at a scale of 1:8,000, and the topographic information was input from the Little Piute Mountains, CA 1:24,000 quadrangle. The accuracy of the spatial information is limited to the input scale.
Postscript files, originally published in paper format as Open-file map 95-598, have been included for those who do not have access to a geographic information system. The files are equivalent to those which produced the hard-copy open file. They can be printed on any device equipped to print postscript files of the appropriate file size.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97693","usgsCitation":"Howard, K.A., Dennis, M.L., Karlstrom, K., and Phelps, G., 1997, Preliminary geologic map of the Little Piute Mountains, California: A digital database: U.S. Geological Survey Open-File Report 97-693, Report 13 p.; 2 Plates: 35.20 x 31.99 inches and 14.18 x 25.22 inches; Database Package; Postscript Files, https://doi.org/10.3133/ofr97693.","productDescription":"Report 13 p.; 2 Plates: 35.20 x 31.99 inches and 14.18 x 25.22 inches; Database Package; Postscript Files","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":9437,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/of97-693/","linkFileType":{"id":5,"text":"html"}},{"id":161545,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0693/report-thumb.jpg"},{"id":64356,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0693/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":416631,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19434.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Little Piute Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115,\n 34.625\n ],\n [\n -115,\n 34.688\n ],\n [\n -115.083,\n 34.688\n ],\n [\n -115.083,\n 34.625\n ],\n [\n -115,\n 34.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e6f9","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":218902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dennis, Michael L.","contributorId":42265,"corporation":false,"usgs":true,"family":"Dennis","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":218904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karlstrom, Karl","contributorId":89944,"corporation":false,"usgs":true,"family":"Karlstrom","given":"Karl","affiliations":[],"preferred":false,"id":218905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":218903,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32111,"text":"ofr97678 - 1997 - Sub-crop geologic map of pre-Tertiary rocks in the Yucca Flat and northern Frenchman Flat areas, Nevada Test Site, southern Nevada","interactions":[],"lastModifiedDate":"2024-02-22T21:54:13.215318","indexId":"ofr97678","displayToPublicDate":"1999-02-01T00:00:00","publicationYear":"1997","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":"97-678","title":"Sub-crop geologic map of pre-Tertiary rocks in the Yucca Flat and northern Frenchman Flat areas, Nevada Test Site, southern Nevada","docAbstract":"This map displays interpreted structural and stratigraphic relations among the Paleozoic and older rocks of the Nevada Test Site region beneath the Miocene volcanic rocks and younger alluvium in the Yucca Flat and northern Frenchman Flat basins. These interpretations are based on a comprehensive examination and review of data for more than 77 drillholes that penetrated part of the pre-Tertiary basement beneath these post-middle Miocene structural basins. Biostratigraphic data from conodont fossils were newly obtained for 31 of these holes, and a thorough review of all prior microfossil paleontologic data is incorporated in the analysis. Subsurface relationships are interpreted in light of a revised regional geologic framework synthesized from detailed geologic mapping in the ranges surrounding Yucca Flat, from comprehensive stratigraphic studies in the region, and from additional detailed field studies on and around the Nevada Test Site.
All available data indicate the subsurface geology of Yucca Flat is considerably more complicated than previous interpretations have suggested. The western part of the basin, in particular, is underlain by relics of the eastward-vergent Belted Range thrust system that are folded back toward the west and thrust by local, west-vergent contractional structures of the CP thrust system. Field evidence from the ranges surrounding the north end of Yucca Flat indicate that two significant strike-slip faults track southward beneath the post-middle Miocene basin fill, but their subsurface traces cannot be closely defined from the available evidence. In contrast, the eastern part of the Yucca Flat basin is interpreted to be underlain by a fairly simple north-trending, broad syncline in the pre-Tertiary units. Far fewer data are available for the northern Frenchman Flat basin, but regional analysis indicates the pre- Tertiary structure there should also be relatively simple and not affected by thrusting.
This new interpretation has implications for ground water flow through pre-Tertiary rocks beneath the Yucca Flat and northern Frenchman Flat areas, and has consequences for ground water modeling and model validation. Our data indicate that the Mississippian Chainman Shale is not a laterally extensive confining unit in the western part of the basin because it is folded back onto itself by the convergent structures of the Belted Range and CP thrust systems. Early and Middle Paleozoic limestone and dolomite are present beneath most of both basins and, regardless of structural complications, are interpreted to form a laterally continuous and extensive carbonate aquifer. Structural culmination that marks the French Peak accommodation zone along the topographic divide between the two basins provides a lateral pathway through highly fractured rock between the volcanic aquifers of Yucca Flat and the regional carbonate aquifer. This pathway may accelerate the migration of ground-water contaminants introduced by underground nuclear testing toward discharge areas beyond the Nevada Test Site boundaries. Predictive three-dimensional models of hydrostratigraphic units and ground-water flow in the pre-Tertiary rocks of subsurface Yucca Flat are likely to be unrealistic due to the extreme structural complexities. The interpretation of hydrologic and geochemical data obtained from monitoring wells will be difficult to extrapolate through the flow system until more is known about the continuity of hydrostratigraphic units.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97678","collaboration":"Prepared in cooperation with the Nevada Operations Office U.S. Department of Energy (Interagency Agreement DE-AI08-96NV11967)","usgsCitation":"Cole, J., Harris, A.G., and Wahl, R., 1997, Sub-crop geologic map of pre-Tertiary rocks in the Yucca Flat and northern Frenchman Flat areas, Nevada Test Site, southern Nevada: U.S. Geological Survey Open-File Report 97-678, Report: ii, 24 p.; 1 Plate: 32.55 x 41.15 inches, https://doi.org/10.3133/ofr97678.","productDescription":"Report: ii, 24 p.; 1 Plate: 32.55 x 41.15 inches","costCenters":[],"links":[{"id":425886,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18824.htm","linkFileType":{"id":5,"text":"html"}},{"id":60238,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0678/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":163317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0678/report-thumb.jpg"},{"id":335274,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0678/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United States","state":"Nevada","otherGeospatial":"Yucca Flat and northern Frenchman Flat areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.25,\n 36.892\n ],\n [\n -115.85,\n 36.892\n ],\n [\n -115.85,\n 37.283\n ],\n [\n -116.25,\n 37.283\n ],\n [\n -116.25,\n 36.892\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c80","contributors":{"authors":[{"text":"Cole, J. C.","contributorId":21539,"corporation":false,"usgs":true,"family":"Cole","given":"J. C.","affiliations":[],"preferred":false,"id":207718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":207717,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wahl, Ronald R.","contributorId":7332,"corporation":false,"usgs":true,"family":"Wahl","given":"Ronald R.","affiliations":[],"preferred":false,"id":207716,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28449,"text":"wri974249 - 1997 - Techniques for estimating peak flow on small streams in Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T09:51:25","indexId":"wri974249","displayToPublicDate":"1998-12-01T00:00:00","publicationYear":"1997","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":"97-4249","title":"Techniques for estimating peak flow on small streams in Minnesota","docAbstract":"Two statistically-derived techniques, regional regression equation and region of influence regression, that estimate peak flow on small, ungaged streams in Minnesota were developed. Both techniques relate physical and climatic characteristics to peak flow for 2-, 5-, 10-, 25-, 50-, and 100-year recurrence intervals.
\nRegional regression equations were developed for each recurrence interval in each of six regions in Minnesota. The region of influence regression technique dynamically selects stations with characteristics similar to a site of interest. Thus, the region of influence regression technique allows use of a potentially unique set of stations for estimating peak flow at each site of interest. Two methods of selecting streamflow gaging stations, similarity and proximity, are recommended for use in the region of influence regression technique.
\nThe regional regression equation technique is recommended as a first estimate of peak flow in regions C, E, and F. The similarity method of the region of influence regression technique should be used as a first estimate in regions A and D. The proximity method should be used as a first estimate in region B.
\nTables showing the peak-flow-frequency data and basin characteristics for streamflow gaging stations, and regional peak-flow prediction equations, are documented.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri974249","collaboration":"Prepared in cooperation with the Minnesota Department of Transportation","usgsCitation":"Lorenz, D., Carlson, G., and Sanocki, C., 1997, Techniques for estimating peak flow on small streams in Minnesota: U.S. Geological Survey Water-Resources Investigations Report 97-4249, Document: ii, 41 p.; Downloadable zip files, https://doi.org/10.3133/wri974249.","productDescription":"Document: ii, 41 p.; Downloadable zip files","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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