Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas, Fort Worth, and San Antonio areas.
\nThe Geological Survey, in cooperation with the Texas Department of Water Reources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Ealcones Fault Zone.
\nThe objectives of the Austin urban hydrology study are as follows:
\nThis report presents the basic hydrologic data collected in the Austin urban area for the 1982 water year (Oct. 1, 1981 to Sept. 30, 1982).
\nAdditional explanations of terms related to streamflow, water quality, and other hydrologic data used in this report are defined in the U.S. Geological Survey annual report Water Resources Data for Texas, TX-82-3, 1982.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr8461","collaboration":"Prepared in cooperation with the City of Austin and the Texas Department of Water Resources","usgsCitation":"Slade, R., Veenhuis, J., Dorsey, M., Stewart, S., and Ruiz, L., 1984, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1982: U.S. Geological Survey Open-File Report 84-61, vi, 196 p., https://doi.org/10.3133/ofr8461.","productDescription":"vi, 196 p.","numberOfPages":"202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":149338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0061/report-thumb.jpg"},{"id":46394,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0061/report.pdf","text":"Report","size":"3.81 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.09280395507812,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 29.991812888666043\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db60816a","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":175582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Veenhuis, J.E.","contributorId":6850,"corporation":false,"usgs":true,"family":"Veenhuis","given":"J.E.","affiliations":[],"preferred":false,"id":175579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":175580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stewart, S.L.","contributorId":81117,"corporation":false,"usgs":true,"family":"Stewart","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":175581,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ruiz, L.M.","contributorId":93925,"corporation":false,"usgs":true,"family":"Ruiz","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":175583,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":26377,"text":"wri844175 - 1984 - Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T11:33:26","indexId":"wri844175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4175","title":"Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota","docAbstract":"The hydrologic effects of proposed impoundments in Sherburne National Wildlife Refuge were found to be insignificant with respect to both ground- and surface-water flow patterns and water quality. Monitoring of water levels in 23 observation wells and of discharge in the St. Francis River during 1980 and 1981 has shown that ground water in the surf icial aquifer responds quickly to areal recharge and subsequently discharges to the St. Francis River. The impoundment of surface water in the refuge was not found to affect water levels in the refuge significantly. The impoundments may affect ground-water-flow systems beneath and adjacent to the impoundments. Quality of ground and surface water was found to be similar except ground water contained higher concentrations of dissolved nitrite plus nitrate nitrogen than surface water. Phytoplankton removed dissolved nitrite plus nitrate nitrogen from surface water. The effects of impoundments on water quality are expected to be minor.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri844175","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Brown, R.G., 1984, Hydrologic effects of impoundments in Sherburne National Wildlife Refuge, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4175, iv, 20 p., https://doi.org/10.3133/wri844175.","productDescription":"iv, 20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":55169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4175/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4175/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Sherburne county","otherGeospatial":"Sherburne National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.85482788085938,\n 45.36854917415683\n ],\n [\n -93.85482788085938,\n 45.58425087527735\n ],\n [\n -93.50875854492188,\n 45.58425087527735\n ],\n [\n -93.50875854492188,\n 45.36854917415683\n ],\n [\n -93.85482788085938,\n 45.36854917415683\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ff3","contributors":{"authors":[{"text":"Brown, R. G.","contributorId":106118,"corporation":false,"usgs":true,"family":"Brown","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28015,"text":"wri834275 - 1984 - True location and orientation of fractures logged with the acoustic televiewer (including programs to correct fracture orientation)","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri834275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4275","title":"True location and orientation of fractures logged with the acoustic televiewer (including programs to correct fracture orientation)","docAbstract":"The attitude of fractures measured on acoustic-televiewer logs may be misorientated by as much as 180 degrees in a drill hole that is deviated significantly from vertical, because of the effect of the vertical component of the magnetic field on the tilted magnetometer that is used to orient the log. A method has been developed to correct for the misorientation by analyzing the orientation of the magnetometer with respect to the magnetic-field vector acting at the magnetometer 's center. Computer programs were written to correct the attitude of fractures for both magnetic effects and hole deviation. For the reorientation of a single fracture, a stereographic solution is illustrated. Test results suggest that the fracture orientation can be corrected to plus or minus five degrees of true orientation, provided there are no other magnetic effects, such as magnetite in the rocks. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834275","usgsCitation":"Kierstein, R., 1984, True location and orientation of fractures logged with the acoustic televiewer (including programs to correct fracture orientation): U.S. Geological Survey Water-Resources Investigations Report 83-4275, iv, 73 p. :ill. ;28 cm., https://doi.org/10.3133/wri834275.","productDescription":"iv, 73 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4275/report-thumb.jpg"},{"id":56842,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4275/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6242d7","contributors":{"authors":[{"text":"Kierstein, R.A.","contributorId":52222,"corporation":false,"usgs":true,"family":"Kierstein","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":199070,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18205,"text":"ofr84256 - 1984 - Statistical relations among earthquake magnitude, surface rupture length, and surface fault displacement","interactions":[],"lastModifiedDate":"2018-06-21T13:26:31","indexId":"ofr84256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-256","title":"Statistical relations among earthquake magnitude, surface rupture length, and surface fault displacement","docAbstract":"In order to refine correlations of surface-wave magnitude, fault rupture length at the ground surface, and fault displacement at the surface by including the uncertainties in these variables, the existing data were critically reviewed and a new data base was compiled. Earthquake magnitudes were redetermined as necessary to make them as consistent as possible with the Gutenberg methods and results, which necessarily make up much of the data base. Measurement errors were estimated for the three variables for 58 moderate to large shallow-focus earthquakes. Regression analyses were then made utilizing the estimated measurement errors. \r\nThe regression analysis demonstrates that the relations among the variables magnitude, length, and displacement are stochastic in nature. The stochastic variance, introduced in part by incomplete surface expression of seismogenic faulting, variation in shear modulus, and regional factors, dominates the estimated measurement errors. Thus, it is appropriate to use ordinary least squares for the regression models, rather than regression models based upon an underlying deterministic relation with the variance resulting from measurement errors. \r\n\r\nSignificant differences exist in correlations of certain combinations of length, displacement, and magnitude when events are qrouped by fault type or by region, including attenuation regions delineated by Evernden and others. Subdivision of the data results in too few data for some fault types and regions, and for these only regressions using all of the data as a group are reported. \r\n\r\nEstimates of the magnitude and the standard deviation of the magnitude of a prehistoric or future earthquake associated with a fault can be made by correlating M with the logarithms of rupture length, fault displacement, or the product of length and displacement. Fault rupture area could be reliably estimated for about 20 of the events in the data set. Regression of MS on rupture area did not result in a marked improvement over regressions that did not involve rupture area. Because no subduction-zone earthquakes are included in this study, the reported results do not apply to such zones.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84256","usgsCitation":"Bonilla, M.G., Mark, R.K., and Lienkaemper, J.J., 1984, Statistical relations among earthquake magnitude, surface rupture length, and surface fault displacement (Online Version 1.0): U.S. Geological Survey Open-File Report 84-256, 46 p., https://doi.org/10.3133/ofr84256.","productDescription":"46 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":150859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1027,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1984/of84-256/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1ed3","contributors":{"authors":[{"text":"Bonilla, M. G.","contributorId":33698,"corporation":false,"usgs":true,"family":"Bonilla","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":178702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mark, R. K.","contributorId":32159,"corporation":false,"usgs":true,"family":"Mark","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":178701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lienkaemper, J. J.","contributorId":71947,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178703,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18171,"text":"ofr84469 - 1984 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","interactions":[{"subject":{"id":18171,"text":"ofr84469 - 1984 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr84469","publicationYear":"1984","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":12700,"text":"ofr86310 - 1986 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr86310","publicationYear":"1986","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"id":1}],"supersededBy":{"id":12700,"text":"ofr86310 - 1986 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr86310","publicationYear":"1986","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"lastModifiedDate":"2017-12-06T13:03:40","indexId":"ofr84469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-469","title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)","docAbstract":"The National Water Data Exchange (NAWDEX) is a national confederation of water-oriented organizations working together to improve access to water data. It consists of member organizations from all sectors of the water-data community. This Directory provides the names, addresses, and telephone numbers of all NAWDEX member organizations and their designated NAWDEX representatives.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84469","usgsCitation":"Blackwell, C.D., 1984, Directory of member organizations of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 84-469, viii, 66 p., https://doi.org/10.3133/ofr84469.","productDescription":"viii, 66 p.","numberOfPages":"77","costCenters":[],"links":[{"id":349787,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0469/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a989","contributors":{"authors":[{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11675,"text":"ofr84383 - 1984 - Reconnaissance geology of the Samirah Quadrangle, sheet 26/42 C, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr84383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-383","title":"Reconnaissance geology of the Samirah Quadrangle, sheet 26/42 C, Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84383","usgsCitation":"Williams, P.L., 1984, Reconnaissance geology of the Samirah Quadrangle, sheet 26/42 C, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 84-383, ii, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84383.","productDescription":"ii, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0383/report-thumb.jpg"},{"id":39543,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0383/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39544,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0383/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0383/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f25e","contributors":{"authors":[{"text":"Williams, P. L.","contributorId":79109,"corporation":false,"usgs":true,"family":"Williams","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18101,"text":"ofr84349 - 1984 - Methodology, geology and listing of analyses of helium samples in the Bisti, De-Na-Zin, and Ah-Shi-Sle-Pah Wilderness Study Areas, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr84349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-349","title":"Methodology, geology and listing of analyses of helium samples in the Bisti, De-Na-Zin, and Ah-Shi-Sle-Pah Wilderness Study Areas, San Juan County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84349","usgsCitation":"Been, J., Hassemer, J., and Murrey, D., 1984, Methodology, geology and listing of analyses of helium samples in the Bisti, De-Na-Zin, and Ah-Shi-Sle-Pah Wilderness Study Areas, San Juan County, New Mexico: U.S. Geological Survey Open-File Report 84-349, 9 p. :map ;28 cm., https://doi.org/10.3133/ofr84349.","productDescription":"9 p. :map ;28 cm.","costCenters":[],"links":[{"id":149257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0349/report-thumb.jpg"},{"id":47458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0349/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a028","contributors":{"authors":[{"text":"Been, J.M.","contributorId":26685,"corporation":false,"usgs":true,"family":"Been","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":178546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, J.R.","contributorId":18761,"corporation":false,"usgs":true,"family":"Hassemer","given":"J.R.","affiliations":[],"preferred":false,"id":178545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murrey, D.G.","contributorId":51740,"corporation":false,"usgs":true,"family":"Murrey","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":178547,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27879,"text":"wri844050 - 1984 - An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri844050","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4050","title":"An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado","docAbstract":"An investigation was made to monitor the storm runoff in McIntyre Gulch basin to determine the rainfall-runoff chracteristics. Results may now be used to evaluate the effects of future development on storm runoff from the Denver Federal Center, which is located in the McIntyre Gulch basin in Lakewood , CO. Rainfall and runoff data were collected at eight streamflow stations and three auxiliary rainfall stations in and adjacent to the Denver Federal Center. The outflow peak discharges from McIntyre Gulch in the Denver Federal Center were higher than the inflow peak discharges for eight of the storms by an average of 38 percent. Outflow peak discharges for eight of the storms were lower by an average of 12 percent. The study demonstrated that runoff varies with location of a storm--even for a relatively small basin. Peak discharges of McIntyre Gulch outflow from the Denver Federal Center were 27 percent greater than the inflow for all storms, but only 15 percent greater for evenly distributed storms. Runoff from the Denver Federal Center increased storm-runoff volumes in McIntyre Gulch by an average of 46 percent. Proper management of storm runoff in the Denver Federal Center requires that proposed improvements to the existing storm-runoff system maintain peak flows at their present levels. 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W.","contributorId":89885,"corporation":false,"usgs":true,"family":"Leinz","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160645,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimes, D. 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The area is in the northwest quarter of the Last Chance Range 15-minute quadrangle and occupies the area between 117 39 and 117 45 longitude and 37 10 and 37 15 latitudP.. The area studied lies between 5000 ( 1525 m) and 6000 ( 1830 m) feet above sea level. Relief isgenerally moderate but can be extreme in some places, as at Hanging Rock Canyon (plate 1). The climate is arid, and there are no active streams in the area. The range fronts east and west of the area are precipitous and incised by many steep canyons, whereas the range crest has relatively low relief. The old abandoned town and mine site of Crater 1 ie in this area of low relief. Access to the Crater area is by paved and dirt roads from Big Pine to the west or from the north end of the Death Valley National Monument to the southeast.
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Multiple-regression analyses revealed a relationship between flood volume, peak discharge, channel slope , and storm duration for basins smaller than 1,503 square miles. The equation VOL=0.536 PEAK1.71 SLOPE-0.85 DUR0.24, had a correlation coefficient of R=0.94 and a standard error of 0.33 log units (-53 and +113 percent). A better relationship for basins smaller than 228 square miles resulted in the equation VOL=0.483 PEAK0.98 SLOPE-0.74 AREA0.30, which had a correlation coefficient of R=0.90 and a standard error of 0.23 log units (-41 and +70 percent). 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Potential well yields range from 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 100 feet. The aquifer lies in an area containing only small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and in geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. The maps are designed to help planners evaluate developments that may affect the aquifer, particularly potential contamination sources. This set is one in a series of four that depict selected aquifers in western New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, file data in several State agencies, and field notes. 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