No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf996","usgsCitation":"Schmidt, P.W., 1978, Reconnaissance map showing relative amounts of soil and bedrock in the Buckhorn Mountain quadrangle, Larimer County, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 996, 1 Plate: 26.43 × 38.25 inches, https://doi.org/10.3133/mf996.","productDescription":"1 Plate: 26.43 × 38.25 inches","costCenters":[],"links":[{"id":182270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390573,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6841.htm"},{"id":276342,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0996/plate-1.pdf"}],"scale":"0","country":"United States","state":"Colorado","county":"Larimer County","otherGeospatial":"Buckhorn Mountain quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.375,40.5 ], [ -105.375,40.6275 ], [ -105.25,40.6275 ], [ -105.25,40.5 ], [ -105.375,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e880","contributors":{"authors":[{"text":"Schmidt, P. W.","contributorId":28303,"corporation":false,"usgs":true,"family":"Schmidt","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10214,"text":"ofr78303 - 1978 - U.S. Geological Survey Oil and Gas Resource Investigations Program","interactions":[],"lastModifiedDate":"2013-08-02T07:12:12","indexId":"ofr78303","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-303","title":"U.S. Geological Survey Oil and Gas Resource Investigations Program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78303","usgsCitation":"Mast, R.F., 1978, U.S. Geological Survey Oil and Gas Resource Investigations Program: U.S. Geological Survey Open-File Report 78-303, i, 33, [46] leaves :ill., maps ;28 cm.; (81 p. - PGS), https://doi.org/10.3133/ofr78303.","productDescription":"i, 33, [46] leaves :ill., maps ;28 cm.; (81 p. - PGS)","costCenters":[],"links":[{"id":142508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0303/report-thumb.jpg"},{"id":275902,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0303/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973d2","contributors":{"authors":[{"text":"Mast, Richard F.","contributorId":60244,"corporation":false,"usgs":true,"family":"Mast","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10039,"text":"ofr78512 - 1978 - Petrology of Potomac Group sands in Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr78512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-512","title":"Petrology of Potomac Group sands in Fairfax County, Virginia","docAbstract":"The Potomac Group sands sampled in Fairfax County are dominantly microcline-rich lithic arkoses. Quartz averages 59%, microcline 25%, plagioclase less than 1% and lithic grains 16%. Most sands are texturally submature and medium grained. Microcline is somewhat more abundant in the deeper beds in the subsurface than in the shallow subsurface and outcrop sections, with quartz correspondingly more abundant at the surface. Zircon is the only abundant non-opaque heavy mineral in the outcrop section as well as in the shallow subsurface, but tourmaline, rutile and staurolite are also common. In contrast, the lower beds in the subsurface have a heavy mineral assemblage with zircon, garnet and apatite as the dominant species. \r\n\r\nSeveral alternative explanations for the vertical variation in mineral assemblages from less to more stable types in the Potomac Group sands are possible: 1) removal of primary Piedmont apatite-bearing igneous and garnet-bearing metamorphic source rock by erosion or burial by overlapping Potomac Group sediments, 2) deep weathering of primary Piedmont source areas and destruction of less stable minerals (apatite and garnet) in Cretaceous time, 3) destruction of less stable minerals (apatite and garnet) near the surface and in the shallow subsurface by post-Cretaceous deep weathering and/or intrastratal solution.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78512","usgsCitation":"Lindholm, R.C., 1978, Petrology of Potomac Group sands in Fairfax County, Virginia: U.S. Geological Survey Open-File Report 78-512, 37 leaves :ill., maps (some fold. in envelope) ;29 cm.; (38 p., 3 sheets - PGS), https://doi.org/10.3133/ofr78512.","productDescription":"37 leaves :ill., maps (some fold. in envelope) ;29 cm.; (38 p., 3 sheets - PGS)","costCenters":[],"links":[{"id":144872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0512/report-thumb.jpg"},{"id":37887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0512/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0512/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0512/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0512/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db65708a","contributors":{"authors":[{"text":"Lindholm, Roy C.","contributorId":99151,"corporation":false,"usgs":true,"family":"Lindholm","given":"Roy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20810,"text":"ofr7874 - 1978 - Preliminary catalog of earthquakes in northern Imperial Valley, California, January 1, 1977 to March 31, 1977","interactions":[],"lastModifiedDate":"2021-12-20T22:24:24.271445","indexId":"ofr7874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-74","title":"Preliminary catalog of earthquakes in northern Imperial Valley, California, January 1, 1977 to March 31, 1977","docAbstract":"The northern section of the Imperial Valley region in Southern California is an area of known geothermal resources and an area of high seismicity. To study in detail the relationship between geothermal areas and earthquakes, the U.S. Geological Survey has been monitoring seismicity in the Imperial Valley with a sixteen station network since 1973. Six new stations were added to the network in November 1976. This catalog contains a description of the network and a list of preliminary data on earthquakes recorded by the network from January 1977 through March 1977.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7874","usgsCitation":"Schnapp, M., and Fuis, G.S., 1978, Preliminary catalog of earthquakes in northern Imperial Valley, California, January 1, 1977 to March 31, 1977: U.S. Geological Survey Open-File Report 78-74, 13 p., https://doi.org/10.3133/ofr7874.","productDescription":"13 p.","numberOfPages":"15","temporalStart":"1977-01-01","temporalEnd":"1977-03-31","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":287777,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393166,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74818.htm"},{"id":287776,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0074/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Imperial Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.0,32.75 ], [ -116.0,33.5 ], [ -115.25,33.5 ], [ -115.25,32.75 ], [ -116.0,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7cc","contributors":{"authors":[{"text":"Schnapp, Madeline","contributorId":26305,"corporation":false,"usgs":true,"family":"Schnapp","given":"Madeline","email":"","affiliations":[],"preferred":false,"id":183292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuis, Gary S. 0000-0002-3078-1544 fuis@usgs.gov","orcid":"https://orcid.org/0000-0002-3078-1544","contributorId":2639,"corporation":false,"usgs":true,"family":"Fuis","given":"Gary","email":"fuis@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":183291,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27842,"text":"wri7821 - 1978 - Chemical and physical quality of selected public water supplies in Florida, August-September 1976","interactions":[],"lastModifiedDate":"2019-11-13T10:34:59","indexId":"wri7821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-21","title":"Chemical and physical quality of selected public water supplies in Florida, August-September 1976","docAbstract":"Results of a 1976 water-quality reconnaissance made by the U.S. Geological Survey indicated that, with few exceptions, all public water supplies in Florida are of high quality and meet the standards set forth in the National Interim Primary Drinking Water Regulations. Occasionally the concentrations of fluoride, turbidity, cadmium, chromium, and lead approximated, equaled, or exceeded maximum contaminant levels with exceedences occurring very infrequently. The pesticides 2,4-D and silvex, were detected in some public supplies throughout the State mainly in surface water. Although pesticides were not detected in concentrations approaching the maximum levels established in the regulations, their presence does signal that the activities of man are beginning to affect some water resources. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633f2c","contributors":{"authors":[{"text":"Irwin, G. A.","contributorId":35733,"corporation":false,"usgs":true,"family":"Irwin","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, Henry G.","contributorId":89916,"corporation":false,"usgs":true,"family":"Healy","given":"Henry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198765,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10004,"text":"ofr78199 - 1978 - Water-quality investigation near the Chico and Hunters geothermal lease-application areas, Park and Sweet Grass counties, Montana","interactions":[],"lastModifiedDate":"2022-10-04T21:11:17.391781","indexId":"ofr78199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-199","title":"Water-quality investigation near the Chico and Hunters geothermal lease-application areas, Park and Sweet Grass counties, Montana","docAbstract":"Water quality in and adjacent to geothermal lease-application areas near Chico and Hunters Hot Springs was investigated during two surveys in October 1976 and April 1977. The resulting data were needed to evaluate the effects of proposed geothermal exploration and development on the Yellowstone River and its tributaries.
Waters from the two hot springs, the Yellowstone River, and its tributaries that drain the proposed lease areas are generally suitable for drinking, except for excessive concentrations of fluoride and hydrogen sulfide in waters from Hunters Hot Springs. The water from Chico Hot Springs is suitable for irrigation, but the water from Hunters Hot Springs presents a very high sodium and a medium salinity hazard and is generally unsatisfactory for irrigation.
The effect of the thermal waters on streamflow and chemical discharge of the Yellowstone River during the surveys was negligible and less than the accepted error of measurement. Production of higher volumes of more concentrated water can be expected to accompany testing and development of the geothermal resource.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78199","collaboration":"Prepared for the U.S. Bureau of Land Management","usgsCitation":"Leonard, R., Shields, R.R., and Midtlyng, N.A., 1978, Water-quality investigation near the Chico and Hunters geothermal lease-application areas, Park and Sweet Grass counties, Montana: U.S. Geological Survey Open-File Report 78-199, iii, 23 p., https://doi.org/10.3133/ofr78199.","productDescription":"iii, 23 p.","costCenters":[],"links":[{"id":142598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0199/report-thumb.jpg"},{"id":407895,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0199/Report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Park County, Sweet Grass County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.28416666666666,45.333333333333336 ], [ -110.28416666666666,45.516666666666666 ], [ -109.75,45.516666666666666 ], [ -109.75,45.333333333333336 ], [ -110.28416666666666,45.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e553f","contributors":{"authors":[{"text":"Leonard, Robert B.","contributorId":14407,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert B.","affiliations":[],"preferred":false,"id":160660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shields, Ronald R.","contributorId":64655,"corporation":false,"usgs":true,"family":"Shields","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Midtlyng, Norman A. nmidtlyn@usgs.gov","contributorId":4442,"corporation":false,"usgs":true,"family":"Midtlyng","given":"Norman","email":"nmidtlyn@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":160659,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10114,"text":"ofr78348 - 1978 - Supplementary hydraulic analysis of proposed bridge site on Mohawk River, Whitesboro, New York","interactions":[],"lastModifiedDate":"2023-02-17T20:54:38.588458","indexId":"ofr78348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-348","title":"Supplementary hydraulic analysis of proposed bridge site on Mohawk River, Whitesboro, New York","docAbstract":"As a supplement to a 1975 report, titled \"Floodflow Characteristics at Proposed Bridge Site on Mohawk River, Whitesboro, New York,\" by Bernard Dunn (U.S. Geological. Survey open-file report), in which the hydraulic effects of two alternative highway plans during a large-magnitude flood were evaluated, a hydraulic analysis was made for a third highway plan. The two plans evaluated in the original report had been found by the State Department of Transportation to be infeasible. A design-flood discharge of 18,200 cubic feet per second was used in the new evaluation, as in the original report. The recurrence interval of that flood is approximately 100 years. The corresponding peak flood stage at the proposed bridge site was determined by the New York State Department of Transportation to be 411.8 feet.
During the design flood, the new proposed alternative would cause a 0.1-foot increase in water-surface elevation from the bridge to the approach section; 1,300 cubic feet per second would overflow the road north of the bridge and 6,800 cubic feet per second south of it. Discharge through the bridge would be 10,100 cubic feet per second.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78348","collaboration":"Prepared in cooperation with New York State Department of Transportation","usgsCitation":"Lumia, R., 1978, Supplementary hydraulic analysis of proposed bridge site on Mohawk River, Whitesboro, New York: U.S. Geological Survey Open-File Report 78-348, ii, 4 p., https://doi.org/10.3133/ofr78348.","productDescription":"ii, 4 p.","costCenters":[],"links":[{"id":413182,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144591,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0348/report-thumb.jpg"}],"country":"United States","state":"New York","city":"Whitesboro","otherGeospatial":"Mohawk River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.30662121855386,\n 43.13256739587925\n ],\n [\n -75.30662121855386,\n 43.11202773792513\n ],\n [\n -75.24896748030349,\n 43.11202773792513\n ],\n [\n -75.24896748030349,\n 43.13256739587925\n ],\n [\n -75.30662121855386,\n 43.13256739587925\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6972c2","contributors":{"authors":[{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":160838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18203,"text":"ofr78239 - 1978 - Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978","interactions":[],"lastModifiedDate":"2017-01-09T10:18:08","indexId":"ofr78239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-239","title":"Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978","docAbstract":"This report contains lists of streamflow and reservoir stations, peak-flow partial-record stations, chemical-quality stations, sediment stations, and observation wells where water levels are measured in Wyoming. The locations of the basic-data sites are shown on maps. Thirty-two water-resources appraisal projects in Wyoming are also described, including many that are related to the development of energy resources. The general locations of the projects are shown on maps. The report serves as an annual progress report to cooperators and the public.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Cheyenne, WY","doi":"10.3133/ofr78239","usgsCitation":"Boner, F.C., 1978, Water-resources investigations of the U.S. Geological Survey in Wyoming, fiscal year 1978: U.S. Geological Survey Open-File Report 78-239, v, 106 p., https://doi.org/10.3133/ofr78239.","productDescription":"v, 106 p.","numberOfPages":"112","costCenters":[],"links":[{"id":47568,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0239/report-thumb.jpg"}],"country":"United States","state":"Wyoming","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9c1a","contributors":{"authors":[{"text":"Boner, F. C.","contributorId":32136,"corporation":false,"usgs":true,"family":"Boner","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":178698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9958,"text":"ofr78461 - 1978 - Ground-water availability in the Hayes-Red Willow, Frenchman, and Meeker-Driftwood irrigation districts, southwest Nebraska","interactions":[],"lastModifiedDate":"2023-02-13T17:22:28.07217","indexId":"ofr78461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-461","title":"Ground-water availability in the Hayes-Red Willow, Frenchman, and Meeker-Driftwood irrigation districts, southwest Nebraska","docAbstract":"Surface-water supplies are diminishing in the Hitchcock-Red Willow and Frenchman Valley Irrigation Districts in southwest Nebraska. Stream depletions due to ground-water withdrawals upstream from Enders Reservoir (northwest of the study area) have resulted in a shortage of about 8,700 acre-feet per year. The availability of ground water to supply part of this deficit was examined. Two surficial aquifers that are currently economical to develop were investigated.
The Ogallala aquifer of late Tertiary age which underlies all the area except the major stream valleys has a hydraulic conductivity averaging less than 200 gallons per day per square foot. Hydraulic conductivities and saturated thicknesses are greater north of and parallel to the Republican River from McCook to Culbertson. The most productive aquifer comprises alluvial deposits of Pleistocene and Holocene age which occupy the valleys of the Republican River and Frenchman Creek. Saturated thickness of this aquifer averages 5O feet, and hydraulic conductivity averages 1,000 gallons per day per square foot. The two aquifers are hydraulically connected except where the bedrock surface on both sides of the Republican River valley is higher than the water levels in the aquifers.
Canal seepage and deep percolation have caused water levels to rise as much as 20 feet in the Hitchcock-Red Willow and Frenchman Valley Irrigation Districts north of the Republican River and as much as 40 feet in the Meeker-Driftwood Irrigation District south of the River. Streamflow accretions from ground water have not increased significantly on Frenchman, Blackwood, or Driftwood Creeks. Ground-water inflow to the Republican River has increased about 6 cubic feet per second between Trenton and McCook.
A digital model of the stream aquifer system was used to simulate the pre-1976 hydrology and assess future conditions for two supply-well configurations as well as for existing private irrigation wells. The first supply-well configuration could sustain less than 37 percent of the well-field capacity of 5,970 acre-feet per year. Projected maximum stream depletions were 12 cubic feet per second on Frenchman Creek and 4 cubic feet per second on Blackwood Creek. The second supply-well configuration could sustain 79 percent of the well-field capacity of 2,780 acre-feet per year. Simulated stream depletions were less than 5 percent of mean annual flow at the end of 19 years. Model simulation indicated that existing wells could supply consumptive-irrigation requirements to district lands for at least 19 years, with well failures limited to areas in the Meeker-Driftwood District where the aquifer is thin.
Hydrologic data for the Kodiak-Shelikof subregion of south-central Alaska are summarized to provide a basis for planning water resources development, identifying water problems and evaluating existing water quality and availability. Average annual precipitation, measured at a few coastal locations in this maritime climatic zone, ranges from 23 to 127 inches. Mean annual runoff for the Kodiak Island group ranges from 4 to 8 cfs/sq mi. A maximum instantaneous runoff of 457 cfs/sq mi has been determined from a small basin on Kodiak Island. Lowest measured stream discharges range from no flow to 0.91 cfs/sq mi. Surface water is the primary source of water supplies for the city of Kodiak and other communities. The geology of the subregion is characterized by metamorphosed sedimentary and volcanic rocks with only a thin mantle of unconsolidated material. A few small, alluvium-filled coastal valleys offer the most favorable conditions for ground-water development, but moderate yields (50-100 gal/min) have been obtained from wells in fractured bedrock. Water in streams and lakes generally has a dissolved-solids concentration less than 60 mg/L, and the water varies from a calcium-bicarbonate type to a sodium-chloride type. The chemical composition of ground waters has a dilute calcium-bicarbonate type in unconsolidated materials and a sodium-bicarbonate type in bedrock. The dissolved solids in the groundwater ranges from 170 to 250 mg/L.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha612","usgsCitation":"Jones, S.H., Madison, R.J., and Zenone, C., 1978, Water resources of the Kodiak-Shelikof subregion, south-central Alaska: U.S. Geological Survey Hydrologic Atlas 612, 2 Plates: 45.59 x 35.20 inches and 45.81 x 35.39 inches, https://doi.org/10.3133/ha612.","productDescription":"2 Plates: 45.59 x 35.20 inches and 45.81 x 35.39 inches","costCenters":[],"links":[{"id":188558,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414363,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16008.htm","linkFileType":{"id":5,"text":"html"}},{"id":89681,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/612/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89680,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/612/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Kodiak-Shelikof subregion","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -159.667,\n 59\n ],\n [\n -159.667,\n 55.5\n ],\n [\n -152,\n 55.5\n ],\n [\n -152,\n 59\n ],\n [\n -159.667,\n 59\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697300","contributors":{"authors":[{"text":"Jones, Stanley H.","contributorId":98729,"corporation":false,"usgs":true,"family":"Jones","given":"Stanley","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Madison, R. J.","contributorId":84734,"corporation":false,"usgs":true,"family":"Madison","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":277951,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10198,"text":"ofr78929 - 1978 - Regional and local networks of horizontal control, Cerro Prieto geothermal area, Mexico","interactions":[],"lastModifiedDate":"2023-11-24T20:23:08.42883","indexId":"ofr78929","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-929","title":"Regional and local networks of horizontal control, Cerro Prieto geothermal area, Mexico","docAbstract":"The Cerro Prieto geothermal area in the Mexicali Valley 30 km southeast of Mexicali, Baja California, is probably deforming due to (1) the extraction of large volumes of steam and hot water, and (2) active tectonism. Two networks of precise horizontal control were established in Mexicali Valley by the U.S. Geological Survey in 1977-78 to measure both types of movement as they occur. These networks consisted of (1) a regional trilateration net brought into the mountain ranges west of the geothermal area from survey stations on an existing U.S. Geological Survey crustal-strain network north of the international border, and (2) a local net tied to stations in the regional net and encompassing the area of present and planned geothermal production. Survey lines in this net were selected to span areas of probable ground-surface movements in and around the geothermal area.
Electronic distance measuring (EDM) instruments, operating with a modulated laser beam, were used to measure the distances between stations in both networks. The regional net was run using a highly precise long-range EDM instrument, helicopters for transportation of men and equipment to inaccessible stations on mountain peaks, and a fixed wing airplane flying along the line of sight. Precision of measurements with this complex long-range system approached 0.2 parts per million of line length. The local net was measured with medium range EDM instrument requiring minimal ancillary equipment. Precision of measurements with this less complex system approached 3 parts per million for the shorter line lengths.
The detection and analysis of ground-surface movements resulting from tectonic strains or induced by geothermal fluid withdrawal is dependent on subsequent resurveys of these networks.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78929","usgsCitation":"Massey, B.L., 1978, Regional and local networks of horizontal control, Cerro Prieto geothermal area, Mexico: U.S. Geological Survey Open-File Report 78-929, 6 p., https://doi.org/10.3133/ofr78929.","productDescription":"6 p.","costCenters":[],"links":[{"id":142560,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0929/report-thumb.jpg"},{"id":422940,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0929/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Mexico","state":"Baja California","otherGeospatial":"Cerro Prieto geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.31764533858325,\n 32.42712278149227\n ],\n [\n -115.31764533858325,\n 32.403936612481544\n ],\n [\n -115.29361274580982,\n 32.403936612481544\n ],\n [\n -115.29361274580982,\n 32.42712278149227\n ],\n [\n -115.31764533858325,\n 32.42712278149227\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5e7","contributors":{"authors":[{"text":"Massey, Bruce L.","contributorId":74001,"corporation":false,"usgs":true,"family":"Massey","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10113,"text":"ofr7885 - 1978 - Floodflow analysis of Ninemile Creek, Onondaga County, New York","interactions":[],"lastModifiedDate":"2014-05-29T08:49:04","indexId":"ofr7885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-85","title":"Floodflow analysis of Ninemile Creek, Onondaga County, New York","docAbstract":"A flood-stage and discharge analysis was made for a 3.61 mile reach of Ninemile Creek between Amboy and Camillus. Water-surface profiles were developed for 50-year, 100-year, and September 26, 1975 flood discharges at Camillus for four different channel conditions: (1) with four culverts at Camillus bypass and a bridge at County Road 36 (present conditions); (2) with only the culverts removed; (3) with only County Road 36 bridge removed; and (4) with the culverts and County Road 36 bridge removed (preconstruction conditions) The 50- and 100-year flood discharges at the Camillus gaging station were determined to be 4,700 and 5,500 cubic feet per second, respectively, and the September 1975 flood discharge was measured to be 2,120 cubic feet per second. If the four culverts are removed, peak water-surface elevations at the gaging station in Camillus during the 50- and 100-year flood would be decreased by 0.7 and 0.3 foot, respectively, relative to those calculated for present conditions. If only County Road 36 bridge is removed, water-surface elevations during the 50- and 100-year flood would be decreased by 0.2 and 0.3 foot, respectively. If both structures are removed, water-surface elevations during the 50- and 10--year floods would be decreased y 0.8 and 0.6 foot, respectively. None of the channel variations would have altered the water-surface elevation at the gage using the September 1975 flood discharge.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Albany, NY","doi":"10.3133/ofr7885","collaboration":"Prepared in cooperation with New York State Department of Transportation","usgsCitation":"Lumia, R., and Dunn, B., 1978, Floodflow analysis of Ninemile Creek, Onondaga County, New York: U.S. Geological Survey Open-File Report 78-85, iii, 10 p., https://doi.org/10.3133/ofr7885.","productDescription":"iii, 10 p.","numberOfPages":"12","costCenters":[],"links":[{"id":287785,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287784,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0085/report.pdf"}],"scale":"24000","country":"United States","state":"New York","county":"Onondaga County","otherGeospatial":"Ninemile Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 76.3,43.0 ], [ 76.3,43.1 ], [ 76.2,43.1 ], [ 76.2,43.0 ], [ 76.3,43.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7292","contributors":{"authors":[{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":160836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":160837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10017,"text":"ofr78235 - 1978 - Anomalous occurrence of uranium in alpine peats, Summit County, Colorado, and results of a simple sample fractionation procedure","interactions":[],"lastModifiedDate":"2022-09-02T19:35:18.879404","indexId":"ofr78235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-235","title":"Anomalous occurrence of uranium in alpine peats, Summit County, Colorado, and results of a simple sample fractionation procedure","docAbstract":"Samples from Summit County, Colo., were fractionated for analyses of organic content and uranium. The uranium is related to organic content but not to type of organic matter. In one area uranium values are around 100 ppm in bulk samples and as much as 200 ppm in certain separated fractions of the samples; this is much higher than the 1-10 ppm normal uranium values for peat.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78235","usgsCitation":"Leventhal, J.S., Jennings, J.K., and Lemke, A.J., 1978, Anomalous occurrence of uranium in alpine peats, Summit County, Colorado, and results of a simple sample fractionation procedure: U.S. Geological Survey Open-File Report 78-235, 17 p., https://doi.org/10.3133/ofr78235.","productDescription":"17 p.","costCenters":[],"links":[{"id":406173,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74851.htm","linkFileType":{"id":5,"text":"html"}},{"id":37855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0235/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0235/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Summit County","otherGeospatial":"Alpine Peaks","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.8778,\n 39.585\n ],\n [\n -105.8069,\n 39.585\n ],\n [\n -105.8069,\n 39.5219\n ],\n [\n -105.8778,\n 39.5219\n ],\n [\n -105.8778,\n 39.585\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b69b","contributors":{"authors":[{"text":"Leventhal, Joel S.","contributorId":36529,"corporation":false,"usgs":true,"family":"Leventhal","given":"Joel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jennings, Joan K.","contributorId":53378,"corporation":false,"usgs":true,"family":"Jennings","given":"Joan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lemke, Alan J.","contributorId":96265,"corporation":false,"usgs":true,"family":"Lemke","given":"Alan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160680,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10209,"text":"ofr78188 - 1978 - Natural gas: A perspective on resource availability","interactions":[],"lastModifiedDate":"2022-09-23T20:34:57.35835","indexId":"ofr78188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-188","title":"Natural gas: A perspective on resource availability","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78188","usgsCitation":"Masters, C.D., 1978, Natural gas: A perspective on resource availability: U.S. Geological Survey Open-File Report 78-188, 8 p., https://doi.org/10.3133/ofr78188.","productDescription":"8 p.","costCenters":[],"links":[{"id":407305,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0188/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0188/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981f6","contributors":{"authors":[{"text":"Masters, Charles D.","contributorId":38969,"corporation":false,"usgs":true,"family":"Masters","given":"Charles","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161008,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61445,"text":"mf930 - 1978 - Sources of data for geologic map of Nevada","interactions":[],"lastModifiedDate":"2022-05-10T20:05:20.394895","indexId":"mf930","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"930","title":"Sources of data for geologic map of Nevada","docAbstract":"No abstract available.
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