{"pageNumber":"588","pageRowStart":"14675","pageSize":"25","recordCount":16498,"records":[{"id":9372,"text":"ofr76818 - 1976 - Hydrologic and geologic data for water management in Huntsville, Madison County, 1974-75","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr76818","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-818","title":"Hydrologic and geologic data for water management in Huntsville, Madison County, 1974-75","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76818","usgsCitation":"Harris, W.F., and Warren, W.M., 1976, Hydrologic and geologic data for water management in Huntsville, Madison County, 1974-75: U.S. Geological Survey Open-File Report 76-818, iv, 69 leaves :ill. (some fold.) ;31 cm.; (82 p. - PGS), https://doi.org/10.3133/ofr76818.","productDescription":"iv, 69 leaves :ill. (some fold.) ;31 cm.; (82 p. - PGS)","costCenters":[],"links":[{"id":141435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611848","contributors":{"authors":[{"text":"Harris, Wiley F.","contributorId":86767,"corporation":false,"usgs":true,"family":"Harris","given":"Wiley","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":159565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warren, William M.","contributorId":85963,"corporation":false,"usgs":true,"family":"Warren","given":"William","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159564,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9036,"text":"ofr76549 - 1976 - Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr76549","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-549","title":"Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado","docAbstract":"This report summarizes the hydrologic studies related to coal development being conducted by the U.S. Geological Survey in the State of Colorado. The objective of the hydrologic data-acquisition program is to collect surface-water quality and quantity data and ground-water level records. These data are needed to define predevelopment conditions and to monitor the effects of construction and operation of coal mines and waste-disposal areas. Data-acquisition activities related to coal development in Colorado have concentrated on the Yampa River basin. A description of the hydrologic data-acquisition activities, including parameters collected and frequency of collection, precedes the summaries of the three interpretive studies currently in progress. Each study summary consists of the project title, definition of the problem being studied, objective of the study, approach of the study, and when known, the schedule for completion of the study and proposed report products resulting from the study. (Woodard-USGS)","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr76549","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic studies of the U.S. Geological Survey related to coal development on Colorado: U.S. Geological Survey Open-File Report 76-549, iv, 22 p. :maps ;28 cm., https://doi.org/10.3133/ofr76549.","productDescription":"iv, 22 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605283","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":528883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30654,"text":"wri7622 - 1976 - Geohydrology of the lowland lakes area, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2019-07-16T12:01:01","indexId":"wri7622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-22","title":"Geohydrology of the lowland lakes area, Anchorage, Alaska","docAbstract":"Unconsolidated deposits, chiefly of glacial origin, make up the surficial geologic materials in the Anchorage lowland lakes area , the western part of the Anchorage glacial outwash plain. Postglacial accumulation of peat, commonly 5 to 10 feet thick, and the presence of ground water at or very near the surface combine to create the swamp-muskeg terrane of much of the area. Deeper, confined ground water is also present beneath thick silt and clay layers that underlie the surficial deposits. Domestic water supply for the lowland lakes area is provided largely by public-supply wells completed in the deep, confined aquifers. No large perennial streams traverse the area, thus streamflow is not a major parameter in the area 's natural water balance. The major uses of surface water are recreational, including fishing and boating at several of the larger lakes, and private and commercial aircraft operations at Hood-Spenard Lakes floatplane base. The hydrology and water balance of these lakes is complex. Water levels in some lakes appear to be closely related to adjacent ground-water levels. Other lakes are evidently perched above the local water table. The relation of lake level to adjacent ground-water level may vary along the shoreline of a single lake. The effect of residential development practices on lake basin water balance is not completely understood. At Sand Lake, the largest lake in this area of rapid urbanization, the water level has declined about 6 feet since the early 1960's. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7622","usgsCitation":"Zenone, C., 1976, Geohydrology of the lowland lakes area, Anchorage, Alaska: U.S. Geological Survey Water-Resources Investigations Report 76-22, 2 Plates: 27.49 x 28.65 inches and 27.31 x 28.52 inches, https://doi.org/10.3133/wri7622.","productDescription":"2 Plates: 27.49 x 28.65 inches and 27.31 x 28.52 inches","costCenters":[],"links":[{"id":159970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0022/report-thumb.jpg"},{"id":365608,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0022/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365609,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.93041992187497,\n              61.15383794909113\n            ],\n            [\n              -149.776611328125,\n              61.15383794909113\n            ],\n            [\n              -149.776611328125,\n              61.227957176677876\n            ],\n            [\n              -149.93041992187497,\n              61.227957176677876\n            ],\n            [\n              -149.93041992187497,\n              61.15383794909113\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a883e","contributors":{"authors":[{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":203612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9629,"text":"ofr76268 - 1976 - Hydrology of a nuclear-processing plant site, Rocky Flats, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr76268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-268","title":"Hydrology of a nuclear-processing plant site, Rocky Flats, Jefferson County, Colorado","docAbstract":"Accidental releases of contaminants resulting from the operation of the U.S. Energy Research and Development Administration's nuclear-processing and recovery plant located on Rocky Flats will move at different rates through -different parts of the hydrologic system. Rates of movement are dependent upon the magnitude of the accidental release and the hydrologic conditions at the time of the release. For example, during wet periods, a contaminant resulting from a 5,000-gallon (19,000-1itre) release on the land surface would enter the ground-water system in about 2 to 12 hours. Ground-water flow in the Rocky Flats Alluvium might move the contaminant eastward at a rate of about 3 to 11 feet (0.9 to 3.4 metres) per day, if it remains dissolved. Maximum time to a point of discharge would be about 3 years; minimum time could be a few days. A contaminant entering a stream would then move at a rate of about 60 feet (18 metres) per minute under pool-and-riffle conditions. The rate of movement might be about 420 feet (128 metres) per minute under open-channel-flow conditions following intense thunderstorms.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76268","usgsCitation":"Hurr, R.T., 1976, Hydrology of a nuclear-processing plant site, Rocky Flats, Jefferson County, Colorado: U.S. Geological Survey Open-File Report 76-268, 77 leaves :ill., maps (2 fold. in envelope) ;29 cm.; (137 p., scale 1:24,000 - PGS), https://doi.org/10.3133/ofr76268.","productDescription":"77 leaves :ill., maps (2 fold. in envelope) ;29 cm.; (137 p., scale 1:24,000 - PGS)","costCenters":[],"links":[{"id":142937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0268/report-thumb.jpg"},{"id":37357,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0268/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37358,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0268/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37359,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0268/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0268/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60435a","contributors":{"authors":[{"text":"Hurr, R. Theodore","contributorId":27023,"corporation":false,"usgs":true,"family":"Hurr","given":"R.","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":160017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2576,"text":"wsp1798N - 1976 - Hydrology and sedimentation of Bixler Run Basin, central Pennsylvania","interactions":[{"subject":{"id":15597,"text":"ofr7526 - 1975 - Hydrology and sedimentation of Bixler Run basin, central Pennsylvania","indexId":"ofr7526","publicationYear":"1975","noYear":false,"title":"Hydrology and sedimentation of Bixler Run basin, central Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":2576,"text":"wsp1798N - 1976 - Hydrology and sedimentation of Bixler Run Basin, central Pennsylvania","indexId":"wsp1798N","publicationYear":"1976","noYear":false,"chapter":"N","title":"Hydrology and sedimentation of Bixler Run Basin, central Pennsylvania"},"id":1}],"lastModifiedDate":"2017-06-19T14:06:02","indexId":"wsp1798N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1798","chapter":"N","title":"Hydrology and sedimentation of Bixler Run Basin, central Pennsylvania","docAbstract":"Rainfall, streamflow, stream chemical, and sediment discharge data were collected from Bixler Run near Loysville, Pa., during the period from February 1954 to September 1969 as part of a project to evaluate sediment discharge from an agricultural area in which soil-conservation techniques were being adopted at a moderate rate. The study was conducted by the U.S. Geological Survey in cooperation with the Pennsylvania Department of Environmental Resources, State Conservation Commission. \r\n\r\nSediment yields from the basin averaged 64 tons per square mile (22 tonnes per square kilometre) per year, approximately 25 percent less than yields from the surrounding area. The relation between water discharge and suspended-sediment discharge remained constant during the study. Suspended-sediment concentrations in the streamflow were less than 10 milligrams per litre 70 percent of the time. The concentration of chloride ions in the streamflow increased from 1959 to 1969. Ground water maintained flows at the gaging location at a rate of 1.9 cubic feet per second (0.054 cubic metres per second) during the period of data collection.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1798N","usgsCitation":"Reed, L.A., 1976, Hydrology and sedimentation of Bixler Run Basin, central Pennsylvania: U.S. Geological Survey Water Supply Paper 1798, v, 20 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1798N.","productDescription":"v, 20 p. :ill., maps ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":28852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798n/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605056","contributors":{"authors":[{"text":"Reed, Lloyd A.","contributorId":79861,"corporation":false,"usgs":true,"family":"Reed","given":"Lloyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16261,"text":"ofr75676 - 1976 - Ground-water hydrology of the Cocoa well-field area, Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:10","indexId":"ofr75676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-676","title":"Ground-water hydrology of the Cocoa well-field area, Orange County, Florida","docAbstract":"The city of Cocoa, Brevard County, Florida, supplies water for much of central Brevard County including Cape Kennedy and Patrick Air Force Base. The water supply is obtained from a well field in east Orange County. Many of the easternmost wells in that well field yield salty water (chloride concentration greater than 250 milligrams per liter). The interface between the fresh and salty water in the west part of the well field occurs at a depth of about 1,400 feet. An upward hydraulic gradient exists between the the lower (salty) zones and the upper, or pumped zones of the Floridan aquifer in the west part of the well field. Secondary artesian aquifers in the well-field area are relatively high-yielding but are of limited areal extent. However, they are suitable as a source of water for supplemental supply or for artificially recharging the Floridan aquifer. Fresh water was transferred by siphon from a secondary artesian aquifer to the Floridan aquifer at 90 gallons per minute. Artificial recharge and recovery experiments show that it is feasible to retrieve fresh water stored in salty zones of the Floridan aquifer. (Woodard-USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr75676","isbn":"pbk","usgsCitation":"Tibbals, C.H., and Frazee, J., 1976, Ground-water hydrology of the Cocoa well-field area, Orange County, Florida: U.S. Geological Survey Open-File Report 75-676, 67 p. :ill. ;28 cm.; (70 p. - PGS), https://doi.org/10.3133/ofr75676.","productDescription":"67 p. :ill. ;28 cm.; (70 p. - PGS)","costCenters":[],"links":[{"id":148486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667268","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":172510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frazee, J.M.","contributorId":44556,"corporation":false,"usgs":true,"family":"Frazee","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":172509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20929,"text":"ofr76214 - 1976 - Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr76214","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-214","title":"Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations","docAbstract":"The distribution functions for hydrologic statistics that may be used to assess the significance of differences between sample means, standard deviations, coefficients of skewness, and coefficients of variations are obtained by Monte Carlo experiments. The distributions are expressed as functions of sample size, cross correlation, and skewness. In general, the distributions are more sensitive to cross correlation than to skewness. As sample size increases, however, the distributions tend to become more sensitive to skewness. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76214","usgsCitation":"Slack, J.R., Matalas, N.C., and Wallis, J.R., 1976, Distribution functions for statistics derived from bivariate normal and bivariate two-parameter log-normal populations: U.S. Geological Survey Open-File Report 76-214, 22 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr76214.","productDescription":"22 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":154082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649372","contributors":{"authors":[{"text":"Slack, James Richard","contributorId":83905,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":183522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matalas, Nicholas C.","contributorId":34535,"corporation":false,"usgs":true,"family":"Matalas","given":"Nicholas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":183521,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallis, James R.","contributorId":100419,"corporation":false,"usgs":true,"family":"Wallis","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27728,"text":"wri76106 - 1976 - Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes","interactions":[],"lastModifiedDate":"2018-08-08T13:56:03","indexId":"wri76106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-106","title":"Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes","docAbstract":"<p>Land-cover information is needed to select subbasins within the New River basin, Tennessee, for the study of hydrologic processes and also is needed to transfer study results to other sites affected by coal mining. It was believed that data recorded by the first Earth Resources Technology Satellite (Landsat-1) could be processed to yield the needed land-cover information. This study demonstrates that digital computer processing of the spectral information contained in each picture element (pixel) of 1.1 acres (4,500 m2) can produce maps and tables of the areal extent of selected land-cover categories.</p><p>The distribution of water, rock, agricultural areas, evergreens, bare earth, hardwoods, and uncategorized areas, is portrayed on a map of the entire New River basin (1:62,500 scale) and on 15 quadrangles (1:24,000 scale). Although some categories are a mixture of land-cover types, they portray the predominant component named. Tables quantify the area of each category and indicate that agriculture covers 5 percent of the basin, evergreens cover 7 percent, bare earth covers 6 percent, three categories of hardwoods cover 81 percent, and water, rock, and uncategorized areas each cover less than 1 percent of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76106","usgsCitation":"Hollyday, E., and Sauer, S., 1976, Mapping and measuring land-cover characteristics of New River Basin, Tennessee, using Landsat digital tapes: U.S. Geological Survey Water-Resources Investigations Report 76-106, iv, 14 p., https://doi.org/10.3133/wri76106.","productDescription":"iv, 14 p.","numberOfPages":"20","costCenters":[],"links":[{"id":356335,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0106/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0106/report-thumb.jpg"}],"country":"United States","state":"Tennessee","otherGeospatial":"New River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.8636474609375,\n              35.27925852568387\n            ],\n            [\n              -83.9630126953125,\n              35.27925852568387\n            ],\n            [\n              -83.9630126953125,\n              36.96744946416934\n            ],\n            [\n              -85.8636474609375,\n              36.96744946416934\n            ],\n            [\n              -85.8636474609375,\n              35.27925852568387\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69de82","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":198601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, S.P.","contributorId":100869,"corporation":false,"usgs":true,"family":"Sauer","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":198602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14610,"text":"ofr75625 - 1976 - Geology and hydrology of radioactive solid-waste burial grounds at the Hanford Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr75625","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"75-625","title":"Geology and hydrology of radioactive solid-waste burial grounds at the Hanford Reservation, Washington","docAbstract":"The geology and hydrology of radioactive solid waste burial grounds at the Hanford Reservation were investigated, using existing data, by the U.S. Geological Survey as part of the waste management plan of the Richland Operations Office of the Energy Research and Development Administration. The purpose of the investigation was to assist the operations office in characterizing the burial sites as to present environmental safety and as to their suitability for long-term storage (several thousand to tens of thousands of years) of radioactive sol id wastes. \r\n\r\nThe burial ground sites fall into two classifications: (1) those on the low stream terraces adjacent to the Columbia River, mainly in the 100 Areas and 300 Area, and (2) those lying on the high terraces south of Gable Mountain in the 200 Areas. Evaluation of the suitability of the burial grounds for long-term storage was made almost entirely on hydrologic, geologic, and topographic criteria. Of greatest concern was the possibility that radionuclides might be leached from the buried wastes by infiltrating water and carried downward to the water table. The climate is semi-arid and the average annual precipitation is 6.4 inches at the Hanford Meteorological Station. However, the precipitation is seasonally distributed with about 50 percent occurring during the months of November, December, January, and February when evapotranspiration is negligible and conditions for infiltration are most favorable. None of the burial grounds are instrumented with monitoring devices that could be used to determine if radionuclides derived from them are reaching the water table. \r\n\r\nBurial grounds on the low stream terraces are mainly underlain by permeable materials and the water table lies at relatively shallow depths. Radionuclides conceivably could be leached from these burial grounds by percolating soil water, and radionuclides might reach the Columbia River in a relatively short time. These sites could also be inundated by erosion during a catastrophic flood. For these reasons, they are judged to be unsuited for long-term storage. Local conditions at several of these burial grounds are particularly unfavorable from the standpoint of safety. Depressions and swales at some burial grounds, such as numbers 4 and 5 in the 300 Area in which runoff can collect, enhance the possibility of water infiltrating through the buried wastes and transporting radionuclides to the water table. Also, during a high stage of the Columbia River, the water table conceivably could rise into burial grounds l and 2 of the 100 F Area. Most of the burial grounds on the low terraces contain either (1) reactor components and related equipment bearing activation products, principally cobalt-60, or (2) less hazardous radioactive materials such as uranium. The inventory of activation products in these burial grounds will decay to a safe level in a relatively short period of time (about 100 years), according to estimates made by C. D. Corbit, Douglas United Nuclear, Inc., 1969. The inventory of radionuclides is not considered by the ERDA staff to be complete, however. At these burial grounds containing activation products or less hazardous materials, investigations should be made of the radioactivity in soil and ground water beneath selected representative sites to verify that radionuclides are not migrating from the burial grounds. If migration is detected, field investigations should be made to determine the source or sources of the radionuclides and the desirability of removing the source wastes. Other burial grounds on the low terraces contain plutonium and fission products, which require long-term storage. Both the 300 WYE and the 300 North burial grounds are reported to contain plutonium in large quantities. Burial ground no. l in the 300 Area reportedly also contains plutonium. The inventory records of any other burial grounds on the low terraces suspected of containing plutonium should be reviewed to determine if pl","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75625","usgsCitation":"LaSala, A.M., and Doty, G.C., 1976, Geology and hydrology of radioactive solid-waste burial grounds at the Hanford Reservation, Washington: U.S. Geological Survey Open-File Report 75-625, viii, 73 leaves :maps ;27 cm.; (70 p. - PGS), https://doi.org/10.3133/ofr75625.","productDescription":"viii, 73 leaves :maps ;27 cm.; (70 p. - PGS)","costCenters":[],"links":[{"id":108641,"rank":700,"type":{"id":15,"text":"Index 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Albert Mario","contributorId":74754,"corporation":false,"usgs":true,"family":"LaSala","given":"Albert","email":"","middleInitial":"Mario","affiliations":[],"preferred":false,"id":169734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doty, Gene C.","contributorId":96272,"corporation":false,"usgs":true,"family":"Doty","given":"Gene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":169735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17256,"text":"ofr76471 - 1976 - Hydrology of the solid waste burial ground as related to potential migration of radionuclides, Idaho National Engineering Laboratory","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr76471","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"76-471","title":"Hydrology of the solid waste burial ground as related to potential migration of radionuclides, Idaho National Engineering Laboratory","docAbstract":"A study was made (1970-1974) to evaluate the geohydrologic and geochemical controls on subsurface migration of radionuclides from pits and trenches in the Idaho National Engineering Laboratory (INEL) solid waste burial ground and to determine the existence and extent of radionuclide migration from the burial ground. A total of about 1,700 sediment, rock, and water samples were collected from 10 observation wells drilled in and near the burial ground of Idaho National Engineering Laboratory, formerly the National Reactor Testing Station (NRTS). Within the burial ground area, the subsurface rocks are composed principally of basalt. Wind- and water-deposited sediments occur at the surface and in beds between the thicker basalt zones. Two principal sediment beds occur at about 110 feet and 240 feet below the land surface. The average thickness of the surficial sedimentary layer is about 15 feet while that of the two principal subsurface layers is 13 and 14 feet, respectively. The water table in the aquifer beneath the burial ground is at a depth of about 580 feet. Fission, activation, and transuranic elements were detected in some of the samples from the 110- and 240-foot sedimentary layers. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nNTIS,","doi":"10.3133/ofr76471","usgsCitation":"Barraclough, J.T., Robertson, J., Janzer, V., and Saindon, L., 1976, Hydrology of the solid waste burial ground as related to potential migration of radionuclides, Idaho National Engineering Laboratory: U.S. Geological Survey Open-File Report 76-471, ix, 183, [2] p. :ill. ;28 cm.; (199 p. - PGS), https://doi.org/10.3133/ofr76471.","productDescription":"ix, 183, [2] p. :ill. ;28 cm.; (199 p. - PGS)","costCenters":[],"links":[{"id":149126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7b5","contributors":{"authors":[{"text":"Barraclough, Jack T.","contributorId":8822,"corporation":false,"usgs":true,"family":"Barraclough","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":175627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robertson, J.B.","contributorId":85173,"corporation":false,"usgs":true,"family":"Robertson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":175629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Janzer, V.J.","contributorId":31777,"corporation":false,"usgs":true,"family":"Janzer","given":"V.J.","affiliations":[],"preferred":false,"id":175628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Saindon, L.G.","contributorId":103281,"corporation":false,"usgs":false,"family":"Saindon","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":175630,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70156622,"text":"70156622 - 1976 - Fresh ground water found deep beneath Nantucket Island, Masachusetts","interactions":[],"lastModifiedDate":"2017-11-05T12:13:17","indexId":"70156622","displayToPublicDate":"1976-10-26T17:15:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Fresh ground water found deep beneath Nantucket Island, Masachusetts","docAbstract":"<p>In a deep water-resources and stratigraphic test well near the center of Nantucket Island, about 30 miles (48 kilometres) off the New England coast, freshwater has been found at greater depths than predicted by the Ghyben-Herzberg principle. An uppermost lens of freshwater, which occupies relatively permeable glacial-outwash sand and gravel to a depth of 520 feet (158 metres), is believed to be in hydrodynamic equilibrium with the present level of the sea and the height of the water table. However, two zones of freshwater at 730 to 820 ft (222-249 m) and 900 to 930 ft (274-283 m) are anomalously deep. Although several explanations are possible, the most likely is that the entire surface of the Continental Shelf was exposed to recharge by precipitation during long periods of low sea level in Pleistocene time. After the last retreat of glacial ice, seawater rapidly drowned the shelf around Nantucket Island. Since then, about 8,000 years ago, the deep freshwater zones which underlie dense clay layers have not had time to adjust to a new equilibrium. Under similar circumstances, freshwater may remain trapped under extensive areas of the Continental Shelf wherever clay confining beds have not permitted saltwater to intrude rapidly to new hydrodynamic equilibria positions. The implications are far reaching because all continental shelves worldwide were exposed to similar hydrologic influences during Pleistocene time.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Kohout, F., Walker, E., Bothner, M., and Hathaway, J., 1976, Fresh ground water found deep beneath Nantucket Island, Masachusetts: Journal of Research of the U.S. Geological Survey, v. 4, no. 5, p. 511-515.","productDescription":"5 p.","startPage":"511","endPage":"515","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307390,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue5/report.pdf#page=11","size":"29.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Nantucket Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.2,\n              41\n            ],\n            [\n              -71.2,\n              43\n            ],\n            [\n              -69.5,\n              43\n            ],\n            [\n              -69.5,\n              41\n            ],\n            [\n              -71.2,\n              41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55dd91b4e4b0518e354dd16d","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":103979,"corporation":false,"usgs":true,"family":"Kohout","given":"F. A.","affiliations":[],"preferred":false,"id":569698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, E.H.","contributorId":104088,"corporation":false,"usgs":true,"family":"Walker","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":569699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bothner, Michael H. mbothner@usgs.gov","contributorId":139855,"corporation":false,"usgs":true,"family":"Bothner","given":"Michael H.","email":"mbothner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":569700,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":569701,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010216,"text":"70010216 - 1976 - Bicarbonate content of groundwater in carbonate rock in eastern North America","interactions":[],"lastModifiedDate":"2025-04-10T15:50:17.089441","indexId":"70010216","displayToPublicDate":"1976-09-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Bicarbonate content of groundwater in carbonate rock in eastern North America","docAbstract":"<p>In carbonate-rock terrane the most effective solution occurs where soil and vegetative cover facilitate biogenic production and storage of CO<sub>2</sub> in the soil until part of it is carried downward in percolating water. Bicarbonate data for groundwater in eastern North America are examined in the light of these conditions, of the CO<sub>2</sub> content of soil gas, and of the timing of groundwater recharge relative to seasonal changes in soil temperature. There appears to be no well-marked relation between latitude and bicarbonate content of groundwater in this region. Interplay of all the factors listed above, and of lithology and soil types, is evidently such that under optimum conditions the amount of solution of carbonate rock is roughly comparable, per unit of groundwater recharge, over the region from Ohio to Florida (and, perhaps, to Puerto Rico and Yucatan). Relatively low HCO<sub>3</sub> concentrations observed in much of the southern United States are attributed to low production and storage of CO<sub>2</sub> in sandy soil that is poor in organic matter. On the other hand, concentrations observed in Ontario, New York and Michigan are markedly higher than is to be expected from interrelations of the factors considered. These high values, apparently anomalous, are attributed in part to solution of granular glacial drift derived largely from carbonate rock.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(76)90019-6","issn":"00221694","usgsCitation":"Trainer, F., and Heath, R., 1976, Bicarbonate content of groundwater in carbonate rock in eastern North America: Journal of Hydrology, v. 31, no. 1-2, p. 37-55, https://doi.org/10.1016/0022-1694(76)90019-6.","productDescription":"19 p.","startPage":"37","endPage":"55","costCenters":[],"links":[{"id":219132,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"eastern North 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,{"id":70232914,"text":"70232914 - 1976 - Simulation of forest changes related to hydrologic variables in the Atchafalaya River basin, Louisiana","interactions":[],"lastModifiedDate":"2022-07-13T13:52:03.251549","indexId":"70232914","displayToPublicDate":"1976-07-01T08:22:31","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Simulation of forest changes related to hydrologic variables in the Atchafalaya River basin, Louisiana","docAbstract":"<p>Results of forest-trend modeling from one data set in the Atchafalaya River basin show that predicted forest acreage totals for 16 forest types agree within 30 percent of actual values in two-thirds of the comparisons. 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,{"id":70010234,"text":"70010234 - 1976 - Application of multi-regional planning models to the scheduling of large-scale water resource systems development","interactions":[],"lastModifiedDate":"2025-04-10T15:32:02.76064","indexId":"70010234","displayToPublicDate":"1976-02-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Application of multi-regional planning models to the scheduling of large-scale water resource systems development","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(76)90062-7","issn":"00221694","usgsCitation":"Moody, D., 1976, Application of multi-regional planning models to the scheduling of large-scale water resource systems development: Journal of Hydrology, v. 28, no. 2-4, p. 101-125, 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,{"id":70260853,"text":"70260853 - 1976 - Limnological data report for the Maine Department of Environmental Protection: U.S. Geological Survey cooperative lake studies project","interactions":[],"lastModifiedDate":"2025-04-24T18:06:44.64493","indexId":"70260853","displayToPublicDate":"1976-01-01T11:36:19","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Limnological data report for the Maine Department of Environmental Protection: U.S. Geological Survey cooperative lake studies project","docAbstract":"<p>The report contains physical, chemical, and biological information collected on 43 Maine lakes during the 1975 calendar year. Methods for the collection and analysis of the hydrologic data are outlined.</p><p>Physical characteristics listed include drainage area, surface area, surface elevation, volume, maximum depth, mean depth, epilimnion depth, epilimnion volume, and length of shoreline. Water-quality analysis are listed or up to 27 parameters of the lake-sample sites and 5 parameters on flowing tributaries. Biological analyses include phyto-plankton data for 4 of the study lakes, zooplankton data for 4 of the study lakes, benthic macroinvertebrate data for 25 of the study lakes, and bacterial data for lake tributaries.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70260853","collaboration":"Prepared in cooperation with the Main Department of Environmental Protection","usgsCitation":"Cowing, D.J., and Scott, M., 1976, Limnological data report for the Maine Department of Environmental Protection: U.S. Geological Survey cooperative lake studies project: Open-File Report, 168 p., https://doi.org/10.3133/70260853.","productDescription":"168 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,{"id":69509,"text":"hu26 - 1976 - Hydrologic Unit Map - 1974, state of Montana","interactions":[],"lastModifiedDate":"2016-08-23T09:06:16","indexId":"hu26","displayToPublicDate":"1976-01-01T11:05:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"26","subseriesTitle":"Montana 1974","title":"Hydrologic Unit Map - 1974, state of Montana","docAbstract":"<p>This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. &nbsp;The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Informaiton on Water Data (1966-72). &nbsp;The previous U.S. Geological Survey Catalog-Indexing System was by map number and letter, such as 49M. &nbsp;The boundaries as shown have been adapted from \"The Catalog of Information on Water Data\" (1972), \"Water Resources Regions and Subregions for the National Assessment of Water and Related Land Resources\" by the U.S. Water Reseources Council (1970), \"River Basins of the United States\" by the U.S. Soil Conservation Service ((1963, 1970), \"River Basin Maps Showing Hydrologic Stations\" by the Inter-Agency Committee on Water Resources, Subcommittee on Hydrology (1961), and State planning maps.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/hu26","isbn":"607767847","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map - 1974, state of Montana: U.S. Geological Survey Hydrologic Unit 26, 2 Plates: 38.71 x 46.02 inches and 40.26 x 46.08 inches, https://doi.org/10.3133/hu26.","productDescription":"2 Plates: 38.71 x 46.02 inches and 40.26 x 46.08 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5790a181e4b030378fb47434","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":534604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70273194,"text":"70273194 - 1976 - Selected hydrologic data, Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2025-12-18T17:09:12.50325","indexId":"70273194","displayToPublicDate":"1976-01-01T10:40:38","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Selected hydrologic data, Chester County, Pennsylvania","docAbstract":"<p>This report presents selected hydrologic data collected during a study of the ground-water resources of Chester County, Pennsylvania. The study was made during 1973-76 by the U. S. Geological Survey in cooperation with the Chester County Water Resources Authority. This report is intended to make the data conveniently available and to supplement an interpretive report that will be published separately.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70273194","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority","usgsCitation":"McGreevy, L., and Sloto, R.A., 1976, Selected hydrologic data, Chester County, Pennsylvania, Report: iii, 138 p.; 1 Plate: 44.85 x 40.84 inches, https://doi.org/10.3133/70273194.","productDescription":"Report: iii, 138 p.; 1 Plate: 44.85 x 40.84 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,{"id":70175535,"text":"70175535 - 1976 - Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974","interactions":[],"lastModifiedDate":"2016-08-16T10:56:11","indexId":"70175535","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175535","usgsCitation":"Buckner, H., 1976, Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1974: Open-File Report, 13 p., https://doi.org/10.3133/70175535.","productDescription":"13 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326560,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b43950e4b03bcb01039fe4","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":645576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171417,"text":"70171417 - 1976 - Hydrology of the North Cascades region, Washington: 1. Runoff, precipitation, and storage characteristics","interactions":[],"lastModifiedDate":"2018-02-04T14:30:25","indexId":"70171417","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of the North Cascades region, Washington: 1. Runoff, precipitation, and storage characteristics","docAbstract":"<p>The time and space distributions of measured precipitation and measured runoff and of spring storage, which is approximately equal to the subsequent summer runoff of snowmelt and stored groundwater, have been analyzed for the North Cascades region of Washington. Neither precipitation nor runoff shows a consistent relationship with altitude, chiefly because of precipitation-shadowing effects in this region of high relief. The relationship between mean annual precipitation and altitude is improved considerably when a topographic mean altitude is used instead of the actual altitude of the weather station. However, the improvement is not sufficient to explain a number of discrepancies that still occur. Some of the scatter in a precipitation-altitude plot appears to be due to a deficient precipitation catch by high-altitude gages. When the dependence of runoff on precipitation was examined on an annual, seasonal, and monthly basis, it was found that only a few low-altitude gages correlated well with basin runoff. In several instances, annual (water year) runoff could be better predicted from winter precipitation than from annual precipitation. Precipitation and runoff were tested for changes with time and both appeared to have been increasing slightly but not at a statistically significant level. When the summer (May–September) fraction of the total annual runoff is plotted against mean basin altitude, a consistent, physically reasonable, mildly curvilinear relationship is revealed. On the basis of this relationship, by using several drainages with diverse area-altitude profiles the spring storage versus altitude distribution can be estimated for each basin. The area-altitude distribution is used instead of the mean altitude in this calculation because of the apparent nonlinear relationship between runoff and altitude.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR012i002p00187","usgsCitation":"Rasmussen, L.A., and Tangborn, W.V., 1976, Hydrology of the North Cascades region, Washington: 1. 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