Water resources data for the 1978 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report, in three volumes, contains discharge records for 76 gaging stations; stage records for 66 of these gaging stations; stage only for 32 gaging stations; contents for 1 reservoir; stage only for 12 lakes; water quality for 147 stations; 22 of these at gaging stations;80 miscellaneous sites, 10 lakes, and 169 wells; and water levels for 686 observation wells. Also included are 199 crest-stage partial-record stations and flood-profile partial-record stations. Additional water-data were collected at various sites, not involved in the systematic data-collection program, and are published as miscellaneous measurements. Records for a few pertinent stations in bordering States are also included in this report. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4652","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60208,"text":"mf878G - 1978 - Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-05-19T20:06:04.46265","indexId":"mf878G","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":"878","chapter":"G","title":"Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska","docAbstract":"This geochemical map shows the distribution and abundance of barium (Ba), arsenic (As), boron (B), and vanadium (V) in -80 mesh (177 micrometers) stream sediment samples in the Chandalar quadrangle, Alaska. The map is a part of a series of geochemical maps that together with the background information circular (Reiser and others, 1978) comprise the folio on the Chandalar quadrangle, Alaska. The data are plotted on a subdued base map showing the generalized geology, topography, and sample localities. Map symbols showing the ranges of metal values are indicated on the accompanying histograms and all values shown are considered anomalous. An explanation of sampling, preparation, analytical procedures, and geochemical raw data for all samples are discussed by O'Leary and others (1976). The -80 mesh (177 micrometers) stream sediment medium was used in this study because of the regional setting in the north-central Brooks Range. Given the rather restrictive time and manpower constraints the -80 mesh (177 micrometers) stream sediment combined with panned concentrates was determined to be the most economical and adequate medium in this case where clastic sediments are being derived from local bedrock.
The study area is generally one of high relief with short fast-moving streams and broad glacial valleys. All samples were taken from active streams, as close to the center channel as possible. All sediments were considered to be locally derived. Care was taken, when sampling an obviously glaciated terrane, to sample above or upstream from morainal material, wherever possible. Most samples were taken in areas where bedrock was within 30 m of the sample site.
Due to the poor sensitivity by spectrographic analysis for arsenic, 200 ppm (parts per million), all arsenic analyses were done by colorimetry.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf878G","usgsCitation":"Marsh, S., Detra, D., and Smith, S., 1978, Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 878, 1 Plate: 40.94 x 34.75 inches, https://doi.org/10.3133/mf878G.","productDescription":"1 Plate: 40.94 x 34.75 inches","costCenters":[],"links":[{"id":183637,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0878-G/report-thumb.jpg"},{"id":417264,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0878-G/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chandalar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,67 ], [ -150,68 ], [ -147,68 ], [ -147,67 ], [ -150,67 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae84b","contributors":{"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":263321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":263322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":263320,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68517,"text":"ha590 - 1978 - Backwater at bridges and densely wooded flood plains, Tallahala Creek at Waldrup, Mississippi","interactions":[],"lastModifiedDate":"2018-12-10T14:27:33","indexId":"ha590","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"590","title":"Backwater at bridges and densely wooded flood plains, Tallahala Creek at Waldrup, Mississippi","docAbstract":"New techniques for predicting water-surface profiles, needed in the design of economical, structurally sound, and environmentally compatible stream crossings, are under investigation. The investigation has accelerated with the advent of digital computers capable of analyzing large quantities of data. Among the techniques is the development of two-dimensional (2-D) digital models. Field data are essential for development and evaluation of these techniques for predicting water-surface profiles. This atlas is the first of a series that will provide a wide range of field data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha590","usgsCitation":"Colson, B., Ming, C.O., and Arcement, G.J., 1978, Backwater at bridges and densely wooded flood plains, Tallahala Creek at Waldrup, Mississippi: U.S. Geological Survey Hydrologic Atlas 590, 9 Plates, https://doi.org/10.3133/ha590.","productDescription":"9 Plates","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278749,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-5a.pdf"},{"id":185532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/590/report-thumb.jpg"},{"id":278742,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-1.pdf"},{"id":278745,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-3b.pdf"},{"id":278746,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-3a.pdf"},{"id":278743,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-2a.pdf"},{"id":278748,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-4b.pdf"},{"id":278744,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-2b.pdf"},{"id":278747,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-4a.pdf"},{"id":360120,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/590/plate-5b.pdf"}],"scale":"4000","country":"United States","state":"Mississippi","city":"Waldrup","otherGeospatial":"Tallahala Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.11805555555554,31.91722222222222 ], [ -89.11805555555554,32 ], [ -89.08444444444444,32 ], [ -89.08444444444444,31.91722222222222 ], [ -89.11805555555554,31.91722222222222 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad47","contributors":{"authors":[{"text":"Colson, B.E.","contributorId":71546,"corporation":false,"usgs":true,"family":"Colson","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":278382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ming, C. O.","contributorId":9266,"corporation":false,"usgs":true,"family":"Ming","given":"C.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":278381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arcement, George J. garcemen@usgs.gov","contributorId":3101,"corporation":false,"usgs":true,"family":"Arcement","given":"George","email":"garcemen@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":278380,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17569,"text":"ofr781012 - 1978 - Principal facts for a set of regional gravity data for the Las Vegas 1 degree by 2 degrees sheet, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:21","indexId":"ofr781012","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":"78-1012","title":"Principal facts for a set of regional gravity data for the Las Vegas 1 degree by 2 degrees sheet, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr781012","usgsCitation":"Reidy, D., Kane, M.F., Healey, D., Peterson, D.L., and Kaufmann, H.E., 1978, Principal facts for a set of regional gravity data for the Las Vegas 1 degree by 2 degrees sheet, Nevada: U.S. Geological Survey Open-File Report 78-1012, 40 p. ;27 cm., https://doi.org/10.3133/ofr781012.","productDescription":"40 p. ;27 cm.","costCenters":[],"links":[{"id":150138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1012/report-thumb.jpg"},{"id":46771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667e98","contributors":{"authors":[{"text":"Reidy, Denis","contributorId":14438,"corporation":false,"usgs":true,"family":"Reidy","given":"Denis","email":"","affiliations":[],"preferred":false,"id":176921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":176924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Healey, D.L.","contributorId":52964,"corporation":false,"usgs":true,"family":"Healey","given":"D.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":176925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, D. L.","contributorId":36484,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":176922,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kaufmann, H. E.","contributorId":40215,"corporation":false,"usgs":true,"family":"Kaufmann","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":176923,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":17013,"text":"ofr78987 - 1978 - Continuous tilt, strain, and magnetic field measurements near four earthquakes (ML = 3.6 to 3.8) on the San Andreas fault, California","interactions":[],"lastModifiedDate":"2024-05-22T22:25:49.184643","indexId":"ofr78987","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":"78-987","title":"Continuous tilt, strain, and magnetic field measurements near four earthquakes (ML = 3.6 to 3.8) on the San Andreas fault, California","docAbstract":"Four moderate earthquakes (M = 3.6 to 3.8) have occurred on the San Andreas fault in central California since October, 1977. These earthquakes are the first since 1974 to occur at this magnitude level within the array of tilt, strain, and magnetic instruments between Chalome (35.726N, 12.249 W) and San Francisco (37.79N, 122.23W) shown in Figure 1. They offer, therefore, one of the few opportunities to search for indications of precursive ground deformation. Furthermore, several other geophysical parameters such as resistivity, creek, radon, seismicity, geodetic strain, etc, are also monitored and allow comparisons for some of these events. This note reports comparative data and some possible implications in continuous strain, tilt, magnetic field and other measurements obtained from instruments within 10 km of the epicenters.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78987","usgsCitation":"Johnston, M., Jones, A., Mortensen, C., and Smith, B., 1978, Continuous tilt, strain, and magnetic field measurements near four earthquakes (ML = 3.6 to 3.8) on the San Andreas fault, California: U.S. Geological Survey Open-File Report 78-987, 10 p., https://doi.org/10.3133/ofr78987.","productDescription":"10 p.","costCenters":[],"links":[{"id":429181,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0987/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147552,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0987/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.04892001229514,\n 38.21407111486016\n ],\n [\n -123.04892001229514,\n 34.80815613844645\n ],\n [\n -118.92220349107271,\n 34.80815613844645\n ],\n [\n -118.92220349107271,\n 38.21407111486016\n ],\n [\n -123.04892001229514,\n 38.21407111486016\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b0e","contributors":{"authors":[{"text":"Johnston, M.J.S. 0000-0003-4326-8368","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":104889,"corporation":false,"usgs":true,"family":"Johnston","given":"M.J.S.","affiliations":[],"preferred":false,"id":174565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, A.C.","contributorId":26302,"corporation":false,"usgs":true,"family":"Jones","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":174562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mortensen, C.E.","contributorId":91503,"corporation":false,"usgs":true,"family":"Mortensen","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":174564,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, B.E.","contributorId":36495,"corporation":false,"usgs":true,"family":"Smith","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":174563,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":68275,"text":"ha612 - 1978 - Water resources of the Kodiak-Shelikof subregion, south-central Alaska","interactions":[{"subject":{"id":9712,"text":"ofr78127 - 1978 - Water resources of the Kodiak-Shelikof subregion, south-central Alaska","indexId":"ofr78127","publicationYear":"1978","noYear":false,"title":"Water resources of the Kodiak-Shelikof subregion, south-central Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":68275,"text":"ha612 - 1978 - Water resources of the Kodiak-Shelikof subregion, south-central Alaska","indexId":"ha612","publicationYear":"1978","noYear":false,"title":"Water resources of the Kodiak-Shelikof subregion, south-central Alaska"},"id":1}],"lastModifiedDate":"2023-03-17T20:49:19.59126","indexId":"ha612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"612","title":"Water resources of the Kodiak-Shelikof subregion, south-central Alaska","docAbstract":"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":26721,"text":"wri77123 - 1978 - Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","interactions":[],"lastModifiedDate":"2025-01-08T22:40:11.942634","indexId":"wri77123","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":"77-123","title":"Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","docAbstract":"Fourteen drainage basins above Fishtrap and Dewey Lakes in the Levisa Fork and Johns Creek drainage basins of eastern Kentucky and southwestern Virginia were studied to determine sedimentation rates and origin of sediment entering the two lakes. The basins ranged in size from 1.68 to 297 square miles. Sediment yields ranged from 2,890 to 21,000 tons per square mile where surface-mining techniques predominated, and from 732 to 3 ,470 tons per square mile where underground mining methods predominated. Yields, in terms of tons per acre-foot of runoff, ranged from 2.2 to 15 for surface-mined areas, and from 0.5 to 2.7 for underground-mined areas. Water and sediment discharges from direct runoff during storms were compared for selected surface-mined and underground-mined areas. Data points of two extensively surface-mined areas, one from the current project and one from a previous project in Beaver Creek basin, McCreary County, Kentucky, grouped similarly in magnitude and by season. Disturbed areas from mining activities determined from aerial photographs reached 17 percent in one study area where extensive surface mining was being practiced. For most areas where underground mining was practiced, percentage disturbed area was almost negligible. Trap efficiency of Fishtrap Lake was 89 percent, and was 62 percent for Dewey Lake. Average annual deposition rates were 464 and 146 acre-feet for Fishtrap and Dewey Lakes, respectively. The chemical quality of water in the Levisa Fork basin has been altered by man 's activities.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77123","usgsCitation":"Curtis, W.F., Flint, R.F., George, F.H., and Santos, J.F., 1978, Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia: U.S. Geological Survey Water-Resources Investigations Report 77-123, xi, 92 p., https://doi.org/10.3133/wri77123.","productDescription":"xi, 92 p.","costCenters":[],"links":[{"id":366194,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0123/report-thumb.jpg"},{"id":465926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35124.htm","text":"Dewey Lake","linkFileType":{"id":5,"text":"html"}},{"id":465927,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35125.htm","text":"Fishtrap Lake","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky, Virginia","otherGeospatial":"Dewey Lake, Fishtrap Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.7764892578125,\n 37.38979975341983\n ],\n [\n -82.29583740234375,\n 37.38979975341983\n ],\n [\n -82.29583740234375,\n 37.75334401310656\n ],\n [\n -82.7764892578125,\n 37.75334401310656\n ],\n [\n -82.7764892578125,\n 37.38979975341983\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c3e4b07f02db4a7e1d","contributors":{"authors":[{"text":"Curtis, William F.","contributorId":70433,"corporation":false,"usgs":true,"family":"Curtis","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Russell F.","contributorId":91144,"corporation":false,"usgs":true,"family":"Flint","given":"Russell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"George, Frederick H.","contributorId":16462,"corporation":false,"usgs":true,"family":"George","given":"Frederick","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196886,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":10584,"text":"ofr78409 - 1978 - January 1978 water levels, and data related to water-level changes since 1940 or 1950, western Kansas","interactions":[],"lastModifiedDate":"2017-09-29T16:01:45","indexId":"ofr78409","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":"78-409","title":"January 1978 water levels, and data related to water-level changes since 1940 or 1950, western Kansas","docAbstract":"This report contains basic data on water-level measurements in observation wells in western Kansas. The measurements were made in mid-winter, mostly in January, when pumping was minimal and water levels had recovered from the effects of pumping during the previous irrigation season. This report also provides basic hydrologic data for relating water-level changes from a \"base-reference year\" (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966), and the previous year (1977). The \"base-reference year\" for the northwestern and west-central areas is designated as 1950; for the southwestern area is designated as 1940; and for the south-central area is not yet designated.
Tables in the report show the depths to water level in 1940 or 1950 (predevelopment year), 1966, 1977, and 1978; water-level changes from 194078 or 1950-78, 1966-78 and 1977-78; and the average annual changes from 1940-78 or 1950-78, and from 1966-78. Also shown are saturated thicknesses of the deposits in 1940 or 1950 and in 1978, as well as the change in feet and percentage.
The annual water-level measurements are made by personnel of the Division of Water Resources of the Kansas State Board of Agriculture and of the U.S. Geological Survey. State-agency support for this program is provided through the Kansas Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78409","usgsCitation":"Pabst, M.E., 1978, January 1978 water levels, and data related to water-level changes since 1940 or 1950, western Kansas: U.S. Geological Survey Open-File Report 78-409, 179 p., https://doi.org/10.3133/ofr78409.","productDescription":"179 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":346273,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0409/report-thumb.jpg"}],"country":"United States","state":"Kansas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62319e","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10844,"text":"ofr78428 - 1978 - Analyses of natural gases from Gulf of Mexico Outer Continental Shelf","interactions":[],"lastModifiedDate":"2023-02-14T22:50:58.604987","indexId":"ofr78428","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":"78-428","title":"Analyses of natural gases from Gulf of Mexico Outer Continental Shelf","docAbstract":"This report contains analyses and related source data for natural gas samples from 32 fields in the Gulf of Mexico OCS (Outer Continental Shelf).
The interpretation of this data, along with analyses from other fields in Texas, is still in progress.
Water resources data for the 1977 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water-quality of ground water. This report, in two volumes, contains discharge records for 258 gaging stations; stage only records for 4 gaging stations; stage and contents for 44 lakes and reservoirs; water quality for 162 gaging stations, 7 lakes, 50 wells and 71 miscellaneous sites; and water levels for 173 observation wells. Also included are 146 crest-stage partial-record stations and 19 low-flow partial-record stations. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA772","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Washington, water year 1977, Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-77-2, xi, 419 p., https://doi.org/10.3133/wdrWA772.","productDescription":"xi, 419 p.","costCenters":[],"links":[{"id":174643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1977/wa-77-2/report-thumb.jpg"},{"id":410998,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/wa-77-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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geochemical evaluation of National Petroleum Reserve, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7870D","usgsCitation":"Theobald, P., and Barton, H.N., 1978, Basic data for the geochemical evaluation of National Petroleum Reserve, Alaska: U.S. Geological Survey Open-File Report 78-70, Report: 102 p.; 2 Plates: 21.75 × 22.33 inches and 21.62 × 22.74 inches, https://doi.org/10.3133/ofr7870D.","productDescription":"Report: 102 p.; 2 Plates: 21.75 × 22.33 inches and 21.62 × 22.74 inches","costCenters":[],"links":[{"id":85036,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0070d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85035,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0070d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0070d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0070d/report-thumb.jpg"},{"id":391776,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14846.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"National Petroleum Reserve","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -162,\n 68\n ],\n [\n -156,\n 68\n ],\n [\n -156,\n 69\n ],\n [\n -162,\n 69\n ],\n [\n -162,\n 68\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487b1","contributors":{"authors":[{"text":"Theobald, P. 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Discharge data from 91 gaging stations were used in developing the techniques. The discharge at 50-percent duration can be estimated if the drainage-area size and mean annual precipitation are known. The \"ordinary high water\" can be estimated if the drainage-area size, mean annual precipitation, channel cross section, channel slope, and Manning's roughness value are known.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78218","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development, Office of Highways","usgsCitation":"Neely, B.L., 1978, Study to determine discharge at 50-percent flow duration and ordinary high water for streams in Louisiana: U.S. Geological Survey Open-File Report 78-218, iii, 21 p., https://doi.org/10.3133/ofr78218.","productDescription":"iii, 21 p.","costCenters":[],"links":[{"id":407752,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0218/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0218/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a80bd","contributors":{"authors":[{"text":"Neely, Braxtel L. Jr.","contributorId":46537,"corporation":false,"usgs":true,"family":"Neely","given":"Braxtel","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10508,"text":"ofr78947 - 1978 - Sediment transport by irrigation return flows on the Yakima Indian Reservation, Washington 1975 and 1976 irrigation seasons","interactions":[],"lastModifiedDate":"2018-11-19T12:31:16","indexId":"ofr78947","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":"78-947","title":"Sediment transport by irrigation return flows on the Yakima Indian Reservation, Washington 1975 and 1976 irrigation seasons","docAbstract":"As determined from data collected at 10 sites on the Yakima Indian Reservation during the 1975 and 1976 irrigation seasons (April-September), seasonal sediment discharges in irrigation return flows ranged from 11,000 tons from Marion Drain and Satus Drain 302, to 400 tons from Coulee Drain. There was little variation between the sediment discharges of the 1975 and 1976 irrigation seasons except those from Satus Drain 302. Due to the lack of natural runoff during those seasons, no distinction could be made between sediment discharges from irrigated and nonirrigated areas. No significant or usable relationships were found between suspended-sediment concentration and concurrent water turbidity or discharge.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78947","usgsCitation":"Nelson, L.M., 1978, Sediment transport by irrigation return flows on the Yakima Indian Reservation, Washington 1975 and 1976 irrigation seasons: U.S. Geological Survey Open-File Report 78-947, iv, 42 p., https://doi.org/10.3133/ofr78947.","productDescription":"iv, 42 p.","costCenters":[],"links":[{"id":359568,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0947/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0947/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Yakima Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.36346435546874,\n 46.175075887712296\n ],\n [\n -119.87869262695312,\n 46.175075887712296\n ],\n [\n -119.87869262695312,\n 46.43407119942979\n ],\n [\n -120.36346435546874,\n 46.43407119942979\n ],\n [\n -120.36346435546874,\n 46.175075887712296\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf05","contributors":{"authors":[{"text":"Nelson, Leonard M.","contributorId":96695,"corporation":false,"usgs":true,"family":"Nelson","given":"Leonard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38702,"text":"pp813Q - 1978 - Summary appraisals of the nation's ground-water resources – Missouri basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:56:38.395429","indexId":"pp813Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"Q","title":"Summary appraisals of the nation's ground-water resources – Missouri basin region","docAbstract":"The Missouri Basin Region lies in the north-central part of the United States and southern Canada. It includes parts of Alberta and Saskatchewan in Canada; parts of Montana, Wyoming, North Dakota, South Dakota, Minnesota, Iowa, Colorado, Kansas, and Missouri, and all of Nebraska in the United States. The region includes about one-sixth of the contiguous United States and requires large water supplies for irrigation, industrial, public, and rural uses. Climate ranges from semiarid to subhumid. Normal annual precipitation increases generally eastward in the downstream direction, but precipitation is not a dependable source of supply. The Missouri River and its tributaries furnish water to many users, but surface water is often inadequate to meet large demands. Numerous surface reservoirs help to regulate streamflow and provide storage, but they also allow an increase in evapotranspiration, which in some areas exceeds normal precipitation. Ground water occurs in aquifers classified as alluvial deposits of sand and gravel, glacial deposits, dune-sand deposits, basin-fill deposits of sand and gravel, sandstone, siltstone, fractured sandy clay, limestone, and dolomite. Ground water can be developed and managed in an orderly manner provided adequate geologic and hydrologic data are available to determine aquifer characteristics and response to pumping and other hydraulic stresses. These data and determinations are essential to design, testing, and implementation of water management plans.
\nUnconsolidated and semiconsolidated aquifers include valley-fill alluvium, areally extensive alluvium, glacial deposits, and basin-fill deposits. The aquifers normally consist of alluvial sand and gravel that contain unconfined ground water that lies near the land surface. Many wells completed in the alluvial aquifers have high yields of good-quality water because most alluvial aquifers are highly transmissive and hydraulically connected to streams. Aquifers in glacial deposits may be difficult to locate and in some areas contain saline water; nevertheless, these aquifers are sources of water supply for many users. Basin-fill aquifers are as much as several thousand feet thick, and many contain large ground-water supplies. Ground-water mining has occurred in semiconsolidated aquifers because of withdrawals from wells. Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.
\nSandstone aquifers lie near the land surface and in structural basins. Interbasin movement of ground water occurs in the Virgelle (Milk River aquifer), Fox Hills-basal Hell Creek, and Dakota aquifers. Sandstone aquifers are less transmissive than unconsolidated and semiconsolidated aquifers in general. Confined sandstone aquifers are common, and flowing wells are obtained in many areas. However, flowing wells may cause large declines in water levels if uncontrolled. Water quality is variable in sandstone aquifers but is adequate for most needs. Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.
\nLimestone and dolomite aquifers are extensive in the region, but in some areas they lie deep below the land surface. The occurrence of ground water in small pores, fractures, or large caverns causes yields from wells to range widely. Large flows through cavern systems in the aquifers are indicated by large springs in some areas. Water quality is extremely variable and must be considered in any water-development plan. Limestone and dolomite aquifers have potential for development of large water supplies in some areas. The development may be aided by induced recharge and interaquifer leakage.
\nSaline ground water occurs throughout the Missouri Basin Region. Dissolved-solids concentration as much as 30,000 milligrams per liter has been measured in aquifers in glacial deposits in Montana. Saline water is common in sandstone aquifers in Wyoming, North Dakota, and South Dakota; maximum reported concentration is 280,000 milligrams per liter in water from the Tensleep Sandstone in Wyoming. Limestone contains saline water in many areas; maximum dissolved-solids concentration is about 350,000 milligrams per liter for the Madison Group in the Williston Basin in North Dakota.
\nComprehensive water-management planning in the Missouri Basin Region will require periodic or continuing inventory of precipitation, streamflow, surface-water storage, and ground water. Water demands for irrigation, industrial, public supply, and rural use are increasing rapidly. Reliance on ground-water supplies is increasing even though in many areas the ground water is still mostly undeveloped. Optimal use of water supplies will require the establishment of realistic goals and carefully conceived water-management plans, each of which will necessarily be based on an adequate baseline of hydrologic data and knowledge of the highly variable hydrologic systems in the region.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813Q","usgsCitation":"Taylor, O., 1978, Summary appraisals of the nation's ground-water resources – Missouri basin region: U.S. Geological Survey Professional Paper 813, Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller, https://doi.org/10.3133/pp813Q.","productDescription":"Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":392897,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5071.htm"},{"id":123063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813q/report-thumb.jpg"},{"id":65559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813q/report.pdf","text":"Report","size":"15.58 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":65558,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-3.pdf","text":"Plate 3","size":"7.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":65557,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-2.pdf","text":"Plate 2","size":"7.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":65556,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-1.pdf","text":"Plate 1","size":"7.64 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"country":"United States","state":"Colorado, Iowa, Kansas, Minnesota, Missouri, Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.99414062499999,\n 49.49667452747045\n ],\n [\n -111.4453125,\n 50.45750402042058\n ],\n [\n -108.896484375,\n 50.3454604086048\n ],\n [\n -104.853515625,\n 50.12057809796008\n ],\n [\n -102.041015625,\n 49.15296965617042\n ],\n [\n -98.96484375,\n 47.635783590864854\n ],\n [\n -97.822265625,\n 46.92025531537451\n ],\n [\n -97.55859375,\n 46.31658418182218\n ],\n [\n -97.3828125,\n 45.583289756006316\n ],\n [\n -96.328125,\n 44.77793589631623\n ],\n [\n -95.537109375,\n 44.02442151965934\n ],\n [\n -94.921875,\n 43.51668853502909\n ],\n [\n -93.603515625,\n 42.42345651793833\n ],\n [\n -92.021484375,\n 40.91351257612758\n ],\n [\n -91.49414062499999,\n 39.027718840211605\n ],\n [\n -91.40625,\n 37.50972584293751\n ],\n [\n -92.63671875,\n 36.87962060502676\n ],\n [\n -94.5703125,\n 37.43997405227057\n ],\n [\n -96.85546875,\n 37.92686760148135\n ],\n [\n -98.7890625,\n 37.92686760148135\n ],\n [\n -103.88671875,\n 38.20365531807149\n ],\n [\n -105.46875,\n 38.134556577054134\n ],\n [\n -107.05078125,\n 39.16414104768742\n ],\n [\n -108.45703125,\n 41.31082388091818\n ],\n [\n -110.21484375,\n 42.87596410238254\n ],\n [\n -111.09374999999999,\n 44.213709909702054\n ],\n [\n -111.4453125,\n 44.653024159812\n ],\n [\n -112.939453125,\n 44.96479793033104\n ],\n [\n -112.939453125,\n 45.460130637921004\n ],\n [\n -113.90625,\n 46.37725420510028\n ],\n [\n -114.169921875,\n 47.69497434186282\n ],\n [\n -113.99414062499999,\n 49.49667452747045\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69969c","contributors":{"authors":[{"text":"Taylor, O. James","contributorId":23958,"corporation":false,"usgs":true,"family":"Taylor","given":"O. James","affiliations":[],"preferred":false,"id":220313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10117,"text":"ofr78165 - 1978 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","interactions":[{"subject":{"id":10117,"text":"ofr78165 - 1978 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","indexId":"ofr78165","publicationYear":"1978","noYear":false,"title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73"},"predicate":"SUPERSEDED_BY","object":{"id":2182,"text":"wsp1532I - 1979 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","indexId":"wsp1532I","publicationYear":"1979","noYear":false,"chapter":"I","title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73"},"id":1}],"supersededBy":{"id":2182,"text":"wsp1532I - 1979 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","indexId":"wsp1532I","publicationYear":"1979","noYear":false,"title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73"},"lastModifiedDate":"2022-10-04T21:09:43.399883","indexId":"ofr78165","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":"78-165","title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","docAbstract":"Four different systems of livestock management were compared hydrologically during a 20-year study (November 1953-November 1973) in western Colorado. These systems were grazing by cattle and sheep from November 15 to May 15 each year, complete elimination of grazing, grazing by sheep from November 15 to February 15 each year, and grazing by sheep from November 15 to February 15 every other year. Grazing by both cattle and sheep from November 15 to May 15 each year was the standard grazing practice in the area at the beginning of the study.
Complete grazing exclusion resulted in a reduction in runoff of about 25 percent during the period 1953-65 and an additional 25 percent during 1966-73. During the same periods sediment yield was reduced by 35 and 28 percent, respectively, for a total of 63 percent.
A change in grazing use from cattle and sheep, November 15-May 15 each year, to sheep only at approximately the same utilization rate, November 15-February 15 each year, was accompanied by a reduction in runoff and sediment yield of about 29 percent. The same change in use, except that grazing was allowed every other year during the sheep grazing period, resulted in a reduction in runoff and sediment yield of about 20 percent.
Recurrence intervals of annual runoff occurring on three soil types at Badger Wash are provided. These data may be applied to similar soils in areas of like climate and physiography shown on accompanying maps.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78165","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lusby, G.C., 1978, Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73: U.S. Geological Survey Open-File Report 78-165, Report: 72 p.; 1 Plate: 10.76 x 18.12 inches, https://doi.org/10.3133/ofr78165.","productDescription":"Report: 72 p.; 1 Plate: 10.76 x 18.12 inches","costCenters":[],"links":[{"id":407894,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0165/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407893,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0165/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0165/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Badger Wash","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.97682189941406,\n 39.24288969082635\n ],\n [\n -108.89511108398436,\n 39.24288969082635\n ],\n [\n -108.89511108398436,\n 39.30454987014581\n ],\n [\n -108.97682189941406,\n 39.30454987014581\n ],\n [\n -108.97682189941406,\n 39.24288969082635\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6152c8","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10338,"text":"ofr78799 - 1978 - Geologic and geophysical data from Osceola National Forest, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr78799","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":"78-799","title":"Geologic and geophysical data from Osceola National Forest, Florida","docAbstract":"Ten core holes were drilled as part of a hydrologic study of Osceola National Forest. This report describes the detailed lithology of the cores taken from test drilling, illustrates gamma-ray logs obtained from the test holes and from wells near the forest, and lists the microfauna obtained and identified from the cores. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78799","usgsCitation":"Miller, J.A., 1978, Geologic and geophysical data from Osceola National Forest, Florida: U.S. Geological Survey Open-File Report 78-799, iii, 101 p. :logs, map ;26 cm.; (155 p. - PGS), https://doi.org/10.3133/ofr78799.","productDescription":"iii, 101 p. :logs, map ;26 cm.; (155 p. - PGS)","costCenters":[],"links":[{"id":143660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a827a","contributors":{"authors":[{"text":"Miller, James Andrew","contributorId":14824,"corporation":false,"usgs":true,"family":"Miller","given":"James","email":"","middleInitial":"Andrew","affiliations":[],"preferred":false,"id":161217,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60214,"text":"mf878D - 1978 - Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-05-19T20:05:06.877696","indexId":"mf878D","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":"878","chapter":"D","title":"Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska","docAbstract":"This geochemical map shows the distribution and abundance of molybdenum (Mo), copper (Cu), and lead (Pb) of -80 mesh (177 micrometers) stream sediment samples in the Chandalar quadrangle, Alaska. The map is a part of a series of geochemical maps that together with the background information circular (Reiser and others, 1978) comprise the folio on the Chandalar quadrangle, Alaska. The data are plotted on a subdued base map showing the generalized geology, topography, and sample localities. Map symbols showing the ranges of metal values are indicated on the accompanying histograms and all values shown are considered anomalous. An explanation of sampling, preparation, analytical procedures and geochemical raw data for all samples are discussed by O'Leary and others (1976). The -80 mesh (177 micrometers) stream sediment medium was used in this study because of the regional setting in the north-central Brooks Range. Given the rather restrictive time and manpower constraints the -80 mesh (177 micrometers) stream sediment combined with panned concentrates was determined to be the most economical and adequate medium in this case where clastic sediments are being derived from local bedrock.
The study area is generally one of high relief with short fast-moving streams and broad glacial valleys. All samples were taken from active streams, as close to the center channel as possible. All sediments were considered to be locally derived. Care was taken, when sampling an obviously glaciated terrane, to sample above or upstream from morainal material, wherever possible. Most samples were taken in areas where bedrock was within 30 m of the sample site.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf878D","usgsCitation":"Marsh, S., Detra, D., and Smith, S., 1978, Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 878, 1 Plate: 43.96 x 35.95 inches, https://doi.org/10.3133/mf878D.","productDescription":"1 Plate: 43.96 x 35.95 inches","costCenters":[],"links":[{"id":417262,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0878-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182658,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0878-D/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chandalar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,67 ], [ -150,68 ], [ -147,68 ], [ -147,67 ], [ -150,67 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae83d","contributors":{"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":263329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":263330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":263328,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20035,"text":"ofr78971 - 1978 - Summary of the water resources of Puerto Rico","interactions":[],"lastModifiedDate":"2018-09-27T13:03:54","indexId":"ofr78971","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":"78-971","title":"Summary of the water resources of Puerto Rico","docAbstract":"The U.S. Department of Commerce (DOC) is the lead agency in the Federal Interagency Study of the Economy of Puerto Rico. At the request of DOC the U.S. Geological Survey is providing a discussion of the water resources of the island for inclusion in the study's section on macroeconomic assessment.
Two of the most important aspects of a water appraisal of an area are how much water is available for use and how good is the water. \"How much\" is often difficult even to estimate because a considerable amount of data is necessary in order to define the quantity. However, the quality of water is much easier to assess in that variability in the quality of water is not as great as in the quantity of water, and less data are required for equal assessment.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78971","usgsCitation":"McCoy, H., 1978, Summary of the water resources of Puerto Rico: U.S. Geological Survey Open-File Report 78-971, iii, 17 p., https://doi.org/10.3133/ofr78971.","productDescription":"iii, 17 p.","costCenters":[],"links":[{"id":154510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0971/report-thumb.jpg"},{"id":357835,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0971/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Puerto 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Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-801","title":"A statistical summary and listing of the spectrographic analyses of heavy mineral concentrate and conventional, sieved stream-sediment samples, Silver City area, New Mexico","docAbstract":"Geochemical sampling of a tier of eight 7 1/2-minute quadrangles bordered by latitudes 32° 45'and 33° 00' N. and longitudes 108° 00' and 108° 30' W. was begun in the fall of 1974 and continued seasonally until completion in the fall of 1976. These quadrangles are in southwest New Mexico and include the well-known mineral deposits of the Silver City area. The sampling was designed to gain semidetailed information on the metal-anomaly characteristics of the strongly mineralized area surrounding Silver City, New Mexico, and to seek geochemical clues for the continuation of these mineral deposits beneath overlying Tertiary volcanic rocks to the north.
The data obtained within areas of known mineral deposits provide information on the metallogenic processes and metal suites that both relate and distinguish metal systems. Evaluation of this information relative to the regional geologic framework and the distribution of known mineral deposits will result in the identification of additional target areas for exploration, as well as further our understanding of the geochemical characteristics of mineralized areas. Extrapolation of models developed from the study of areas of known, exposed mineralization to areas covered by Tertiary volcanic rocks, such as the northern part of this tier of quadrangles, is a promising procedure for continuing research into geochemical-anomaly characteristics of covered mineral deposits.
Preliminary interpretation of the data indicates that the southern part of the area in which Paleozoic-Mesozoic rocks and mineral deposits are exposed, should be reassessed to the classification and genesis of some of the deposits and to the types of mineral commodities that may be present. Some wholly new exploration targets within these areas are also indicated by some of the data. In addition, geochemical clues to buried mineral deposits, possibly representing continuation northward of some features of the Silver City mining district, have been observed in data from the northern, Tertiary volcanic areas. The meanings of these clues are still speculative.
For this study, 917 stream-sediment and 921 stream-sediment concentrate samples were collected. The stream-sediment-concentrate samples, which consist of heavy minerals, were split into magnetic and nonmagnetic fractions, each of which was analyzed. This resulted in the analysis of 1,842 heavy-mineral and 917 sieved stream-sediment samples.
Analytical results for all of the sample types are summarized statistically on table 1 and tabulated in their entirety on table 2.
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C.","contributorId":49344,"corporation":false,"usgs":true,"family":"Watts","given":"K.","middleInitial":"C.","affiliations":[],"preferred":false,"id":156004,"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":156003,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siems, D. F.","contributorId":101239,"corporation":false,"usgs":true,"family":"Siems","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":156006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nishi, J. M.","contributorId":89886,"corporation":false,"usgs":true,"family":"Nishi","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156005,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9005,"text":"ofr78288 - 1978 - A computer-oriented system for logging, annotating, tabulating, and plotting marine geophysical and geological data collected by the Pacific-Arctic Branch of the Office of Marine Geology, U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr78288","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":"78-288","title":"A computer-oriented system for logging, annotating, tabulating, and plotting marine geophysical and geological data collected by the Pacific-Arctic Branch of the Office of Marine Geology, U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78288","usgsCitation":"Larsen, B.R., Cooper, A.K., McHendrie, G., and Gardner, J., 1978, A computer-oriented system for logging, annotating, tabulating, and plotting marine geophysical and geological data collected by the Pacific-Arctic Branch of the Office of Marine Geology, U.S. Geological Survey: U.S. Geological Survey Open-File Report 78-288, 208 leaves :ill. (1 col.), maps ;28 cm., https://doi.org/10.3133/ofr78288.","productDescription":"208 leaves :ill. (1 col.), maps ;28 cm.","costCenters":[],"links":[{"id":140791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0288/report-thumb.jpg"},{"id":36644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0288/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b0278","contributors":{"authors":[{"text":"Larsen, Bradley R.","contributorId":104898,"corporation":false,"usgs":true,"family":"Larsen","given":"Bradley","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":158731,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":158729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHendrie, G.A.","contributorId":40599,"corporation":false,"usgs":true,"family":"McHendrie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":158728,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gardner, J.V.","contributorId":76705,"corporation":false,"usgs":true,"family":"Gardner","given":"J.V.","affiliations":[],"preferred":false,"id":158730,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20211,"text":"ofr78856 - 1978 - Analyses and description of geochemical samples, Craggy Mountain Wilderness Study area, Buncombe County, North Carolina","interactions":[],"lastModifiedDate":"2024-01-31T20:45:11.435689","indexId":"ofr78856","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":"78-856","title":"Analyses and description of geochemical samples, Craggy Mountain Wilderness Study area, Buncombe County, North Carolina","docAbstract":"Semiquantitative spectrographic analyses for 30 elements and atomic absorption analyses for gold and zinc on 24 bulk stream sediments, 22 panned concentrates, and 50 rock samples from the Craggy Mountain Wilderness Study area and vicinity, Buncombe County, North Carolina, are reported here in detail. Locations for all samples are given in Universal Transverse Mercator (UTM) coordinates. Brief descriptions of rock samples are also included. Rocks analyzed include mica-garnet-kyanite schist, mica-quartz gneiss, vein quartz, pegmatite, trondhjemite and amphibolite. The data contain no obviously anomalous values that might be related to mineralized rock.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78856","usgsCitation":"Motooka, J.M., Sharkey, J.D., and Lesure, F.G., 1978, Analyses and description of geochemical samples, Craggy Mountain Wilderness Study area, Buncombe County, North Carolina: U.S. Geological Survey Open-File Report 78-856, 9 p., https://doi.org/10.3133/ofr78856.","productDescription":"9 p.","costCenters":[],"links":[{"id":152205,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0856/report-thumb.jpg"},{"id":425171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0856/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","county":"Buncombe County","otherGeospatial":"Craggy Mountain Wilderness Study area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.416667,35.683333 ], [ -82.416667,35.75 ], [ -82.35,35.75 ], [ -82.35,35.683333 ], [ -82.416667,35.683333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6839df","contributors":{"authors":[{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sharkey, John D.","contributorId":6868,"corporation":false,"usgs":true,"family":"Sharkey","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":182256,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lesure, Frank Gardner","contributorId":70752,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"Gardner","affiliations":[],"preferred":false,"id":182258,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26740,"text":"wri78134 - 1978 - Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974","interactions":[],"lastModifiedDate":"2025-07-21T17:19:29.617438","indexId":"wri78134","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":"78-134","title":"Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974","docAbstract":"A land use, land cover, and drainage map of the 2,000-square-mile Albermarle-Pamlico peninsula of eastern North Carolina has been prepared, at a scale of 1:125,000, as part of a larger study of the effects of large-scale land clearing on regional hydrology. The peninsula includes the most extensive area of wetland in North Carolina and one of the largest in the country. In recent years the pace of land clearing on the peninsula has accelerated as land is being converted from forest, swamp, and brushland to agricultural use. Conversion of swamps to intensive farming operations requires profound changes in the landscape. Vegetation is uprooted and burned and ditches and canals are dug to remove excess water. What is the impact of these changes on ground-water supplies and on the streams and surrounding coastal waters which receive the runoff This map will aid in answering these and similar questions that have arisen about the patterns of land use and the artificial drainage system that removes excess water from the land. By showing both land use and drainage, this map can be used to identify those areas where water-related problems may occur and help assess the nature and causes of these problems. The map covers the entire area east of the Suffolk Scarp, an area of about 2,000 square miles, for the year 1974 using data from 1974-76. Land use and land cover were compiled and modified from the U.S. Geological Survey 's Rocky Mount and Manteo LUDA maps. Additional information came from U.S. Geological Survey orthophotoquads, Landsat imagery, and field checking. Drainage was mapped from orthophotoquads, some field inspection, and 7-1/2 minute topographic quadrangle maps.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri78134","collaboration":"Prepared in cooperation with the North Carolina Department of Natural Resources and Community Development","usgsCitation":"Daniel, C., 1978, Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974: U.S. Geological Survey Water-Resources Investigations Report 78-134, 2 Plates: 47.94 x 30.89 inches and 47.90 x 31.02 inches, https://doi.org/10.3133/wri78134.","productDescription":"2 Plates: 47.94 x 30.89 inches and 47.90 x 31.02 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158490,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0134/report-thumb.jpg"},{"id":492647,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492646,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492648,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0134/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Albemarle-Pamplico Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.046875,\n 34.44315867450577\n ],\n [\n -78.046875,\n 36.57142382346277\n ],\n [\n -74.99267578125,\n 36.57142382346277\n ],\n [\n -74.99267578125,\n 34.44315867450577\n ],\n [\n -78.046875,\n 34.44315867450577\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf98","contributors":{"authors":[{"text":"Daniel, C.C.","contributorId":53427,"corporation":false,"usgs":true,"family":"Daniel","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":196918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11104,"text":"ofr78105A - 1978 - Audio-magnetotelluric station location map and data log for Double Hot Springs Known Geothermal Resource Area, Nevada","interactions":[],"lastModifiedDate":"2014-05-29T08:59:45","indexId":"ofr78105A","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":"78-105","chapter":"A","title":"Audio-magnetotelluric station location map and data log for Double Hot Springs Known Geothermal Resource Area, Nevada","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78105A","usgsCitation":"Senterfit, R.M., and Hoover, D.B., 1978, Audio-magnetotelluric station location map and data log for Double Hot Springs Known Geothermal Resource Area, Nevada: U.S. Geological Survey Open-File Report 78-105, 5 p., https://doi.org/10.3133/ofr78105A.","productDescription":"5 p.","numberOfPages":"6","costCenters":[],"links":[{"id":287791,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287790,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0105-A/report.pdf"}],"country":"United States","state":"Nevada","otherGeospatial":"Double Hot Springs","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.083333,41.0 ], [ -117.083333,41.083333 ], [ -117.0,41.083333 ], [ -117.0,41.0 ], [ -117.083333,41.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668831","contributors":{"authors":[{"text":"Senterfit, R. Michael","contributorId":10791,"corporation":false,"usgs":true,"family":"Senterfit","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":162549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162550,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9569,"text":"ofr78106C - 1978 - Telluric profile location map and telluric data for the Glamis Known Geothermal Resource Area, California","interactions":[],"lastModifiedDate":"2024-08-09T17:01:03.893502","indexId":"ofr78106C","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":"78-106","chapter":"C","title":"Telluric profile location map and telluric data for the Glamis Known Geothermal Resource Area, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78106C","usgsCitation":"Hoover, D.B., Radtke, B., and Moeller, D., 1978, Telluric profile location map and telluric data for the Glamis Known Geothermal Resource Area, California: U.S. Geological Survey Open-File Report 78-106, 4 p., https://doi.org/10.3133/ofr78106C.","productDescription":"4 p.","costCenters":[],"links":[{"id":432453,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0106-c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141811,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0106-c/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Glamis Known Geothermal Resource Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.0479183502755,\n 33.13456891885758\n ],\n [\n -115.0479183502755,\n 33.00259827531859\n ],\n [\n -114.8976078018295,\n 33.00259827531859\n ],\n [\n -114.8976078018295,\n 33.13456891885758\n ],\n [\n -115.0479183502755,\n 33.13456891885758\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685874","contributors":{"authors":[{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":159917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, Bruce","contributorId":77149,"corporation":false,"usgs":true,"family":"Radtke","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":159916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moeller, D.D.","contributorId":30229,"corporation":false,"usgs":true,"family":"Moeller","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":159915,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}