{"pageNumber":"526","pageRowStart":"13125","pageSize":"25","recordCount":16452,"records":[{"id":27841,"text":"wri834207 - 1984 - Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 2","interactions":[],"lastModifiedDate":"2022-01-18T22:40:21.549985","indexId":"wri834207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4207","title":"Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 2","docAbstract":"In response to the increasing demand on water supplies and declining water levels in eastern San Joaquin County, the U.S. Geological Survey, in cooperation with the San Joaquin County Flood Control and Water Conservation District, is evaluating the potential for artificially recharging the aquifer system in eastern San Joaquin County, Calif. Phase 1 of this study evaluated the geologic and hydrological conditions in the area and selected 20 drill sites in three areas of high potential for artificial recharge of the aquifer system. In phase 2, test holes were drilled. This report is on phase 2, and summarizes the data collected during the drilling and evaluates the suitability of the drilled areas for their potential for artificial recharge. Two areas seem to have a fair potential for artificial recharge of the aquifer system using the basin-spreading method: (1) The flood plain area along the Mokelumne River north of Lockeford, and (2) an area northeast of Linden along the Calaveras River. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834207","usgsCitation":"Ireland, R.L., 1984, Evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California — Phase 2: U.S. Geological Survey Water-Resources Investigations Report 83-4207, Report: iv, 28 p.; 2 Plates: 29.24 × 35.17 inches and 34.60 × 27.49 inches, https://doi.org/10.3133/wri834207.","productDescription":"Report: iv, 28 p.; 2 Plates: 29.24 × 35.17 inches and 34.60 × 27.49 inches","costCenters":[],"links":[{"id":56669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56668,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4207/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394484,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35850.htm"},{"id":56667,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4207/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123318,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4207/report-thumb.jpg"}],"country":"United States","state":"California","county":"San Joaquin County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.25,\n              37.8740\n            ],\n            [\n              -120.917,\n              37.8740\n            ],\n            [\n              -120.917,\n              38.25\n            ],\n            [\n              -121.25,\n              38.25\n            ],\n            [\n              -121.25,\n              37.8740\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1fc","contributors":{"authors":[{"text":"Ireland, R. L.","contributorId":89893,"corporation":false,"usgs":true,"family":"Ireland","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30416,"text":"wri844193 - 1984 - Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri844193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4193","title":"Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada","docAbstract":"Analyses were made on 19 core samples of unsaturated tuff from test well USW H-1. Moisture-characteristic curves relating saturation and moisture tension were developed from results of mercury-injection tests. Ambient moisture tension estimated from these curves generally was 1 to 2 bars. Values of relative permeability ranging from about 0.002 to 0.1 were determined by fitting an analytical expression to eight of the moisture-characteristic curves, and then integrating to solve for relative permeability. These values of relative permeability were applied to values of saturated hydraulic conductivity of core from a nearby test well to obtain effective hydraulic conductivities of about 8 x 10 to the minus twelfth power to 7 x 10 to the minus tenth power centimeter per second. If a unit hydraulic-head gradient is assumed, these values convert to a vertial matrix flux of 0.003 to 0.2 millimeter per year. The validity of this assumption was not verified due to the sparseness of data and uncertainties in their reliability. Consequently, the results of this study are preliminary and need to be used principally as a guide for future studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844193","usgsCitation":"Weeks, E., and Wilson, W., 1984, Preliminary evaluation of hydrologic properties of cores of unsaturated tuff, test well USW H-1, Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4193, iv, 30 p. :ill. ;28 cm., https://doi.org/10.3133/wri844193.","productDescription":"iv, 30 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159691,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4193/report-thumb.jpg"},{"id":59185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d06","contributors":{"authors":[{"text":"Weeks, E.P.","contributorId":38514,"corporation":false,"usgs":true,"family":"Weeks","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":203213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":203214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27817,"text":"wri844016 - 1984 - Ground-water models as a management tool in Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri844016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4016","title":"Ground-water models as a management tool in Florida","docAbstract":"Highly sophisticated computer models provide powerful tools for analyzing historic data and for simulating future water levels, water movement, and water chemistry under stressed conditions throughout the ground-water system in Florida. Models that simulate the movement of heat and subsidence of land in response to aquifer pumping also have potential for application to hydrologic problems in the State. Florida, with 20 ground-water modeling studies reported since 1972, has applied computer modeling techniques to a variety of water-resources problems. Models in Florida generally have been used to provide insight to problems of water supply, contamination, and impact on the environment. The model applications range from site-specific studies, such as estimating contamination by wastewater injection at St. Petersburg, to a regional model of the entire State that may be used to assess broad-scale environmental impact of water-resources development. Recently, groundwater models have been used as management tools by the State regulatory authority to permit or deny development of water resources. As modeling precision, knowledge, and confidence increase, the use of ground-water models will shift more and more toward regulation of development and enforcement of environmental laws. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844016","usgsCitation":"Hutchinson, C.B., 1984, Ground-water models as a management tool in Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4016, iv, 26 p. :ill. ;28 cm., https://doi.org/10.3133/wri844016.","productDescription":"iv, 26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":126884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4016/report-thumb.jpg"},{"id":56653,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660d9a","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30395,"text":"wri844025 - 1984 - Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81","interactions":[],"lastModifiedDate":"2017-01-24T09:37:21","indexId":"wri844025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4025","title":"Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81","docAbstract":"Beginning in late 1978, stream channels throughout the 60-square mile Chicod Creek basin underwent extensive modification to increase drainage efficiency and reduce flooding potential. Drainage modifications in this Coastal Plain basin, consisting primarily of channel excavation and clearing of channel blockages, were completed in December 1981. The hydrologic condition of the basin before and during modification was determined from observed data.\r\n\r\nObserved data indicate hydrologic changes occurred in selected basin characteristics. For example, water levels in the surficial aquifer within 250 feet of Juniper Branch declined as much as 0.4 feet during modifications; at distances greater than 250 feet from the stream, ground-water levels did not change. Base flows increased, and suspended-sediment concentrations for high flows were several times greater than before channel modifications. Increases in selected chemical constituent concentrations in stream water during modifications were as follows: calcium, 12 percent; sodium, 18 percent; bicarbonate, 84 percent; and phosphorous, 80 percent. Significant changes were not found in either pesticide concentrations or coliform bacteria counts.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844025","usgsCitation":"Watkins, S., and Simmons, C., 1984, Hydrologic conditions in the Chicod Creek basin, North Carolina, before and during channel modifications, 1975-81: U.S. Geological Survey Water-Resources Investigations Report 84-4025, vii, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844025.","productDescription":"vii, 36 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":59167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4025/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Chicod Creek basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.3382568359375,\n              35.60818490437746\n            ],\n            [\n              -77.32177734375,\n              35.60148556537354\n            ],\n            [\n              -77.31216430664061,\n              35.594785665487244\n            ],\n            [\n              -77.2998046875,\n              35.595902354416566\n            ],\n            [\n              -77.28881835937499,\n              35.58808520476323\n            ],\n            [\n              -77.27371215820312,\n              35.5936689609791\n            ],\n            [\n              -77.25997924804688,\n              35.60036895434144\n            ],\n            [\n              -77.24624633789062,\n              35.60930140634475\n            ],\n            [\n              -77.21466064453125,\n              35.610417892730524\n            ],\n            [\n              -77.2064208984375,\n              35.598135685537905\n            ],\n            [\n              -77.19680786132812,\n              35.59255224089235\n            ],\n            [\n              -77.18994140625,\n              35.586968406786475\n            ],\n            [\n              -77.18170166015625,\n              35.576916524038616\n            ],\n            [\n              -77.16659545898438,\n              35.570214567965984\n            ],\n            [\n              -77.14324951171875,\n              35.56686337967425\n            ],\n            [\n              -77.12127685546875,\n              35.563512051219696\n            ],\n            [\n              -77.11166381835938,\n              35.561277754384555\n            ],\n            [\n              -77.10479736328125,\n              35.555691739779654\n            ],\n            [\n              -77.06634521484375,\n              35.543401137387335\n            ],\n            [\n              -77.07321166992188,\n              35.48415637985317\n            ],\n            [\n              -77.07870483398436,\n              35.43605776486772\n            ],\n            [\n              -77.09312438964844,\n              35.38513141280172\n            ],\n            [\n              -77.12265014648438,\n              35.383451974194934\n            ],\n            [\n              -77.29774475097656,\n              35.38569121790089\n            ],\n            [\n              -77.3382568359375,\n              35.60818490437746\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61161b","contributors":{"authors":[{"text":"Watkins, S.A.","contributorId":83962,"corporation":false,"usgs":true,"family":"Watkins","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":203182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, C.E.","contributorId":32572,"corporation":false,"usgs":true,"family":"Simmons","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":203181,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25531,"text":"wri844054 - 1984 - Geohydrology, aqueous geochemistry, and thermal regime of the Soda Lakes and Upsal Hogback geothermal systems, Churchill County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri844054","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4054","title":"Geohydrology, aqueous geochemistry, and thermal regime of the Soda Lakes and Upsal Hogback geothermal systems, Churchill County, Nevada","docAbstract":"A flow-routing model of the upper Schoharie Creek basin, New York, was developed and used to simulate high flows at the inlet of the Blenheim-Gilboa Reservoir. The flows from Schoharie Creek at Prattsville, the primary source of flow data in the basin, and tributary flows from the six minor basins downstream, are combined and routed along the 9.7 mile reach of the Schoharie Creek between Prattsville and the reservoir inlet. Data from five historic floods were used for model calibration and four for verification. The accuracy of the model as measured by the difference between simulated and observed total flow volumes, is within 14 percent. Results indicate that inflows to the Blenheim-Gilboa Reservoir can be predicted approximately 2 hours in advance. One of the historical floods was chosen for additional model testing to assess a hypothetical real-time model application. Total flow-volume errors ranged from 30.2 percent to -9.2 percent. Alternative methods of obtaining hydrologic data for model input are presented for use in the event that standard forms of hydrologic data are unavailable. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844054","usgsCitation":"Olmsted, F.H., Welch, A., Van Denburgh, A.S., and Ingebritsen, S.E., 1984, Geohydrology, aqueous geochemistry, and thermal regime of the Soda Lakes and Upsal Hogback geothermal systems, Churchill County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4054, xiv, 166 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844054.","productDescription":"xiv, 166 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":110164,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35951.htm","linkFileType":{"id":5,"text":"html"},"description":"35951"},{"id":121804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4054/report-thumb.jpg"},{"id":54251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4054/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54252,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4054/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf2c","contributors":{"authors":[{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, A. H.","contributorId":14836,"corporation":false,"usgs":true,"family":"Welch","given":"A. H.","affiliations":[],"preferred":false,"id":194066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194067,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingebritsen, S. E.","contributorId":8078,"corporation":false,"usgs":true,"family":"Ingebritsen","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":194065,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27773,"text":"wri844051 - 1984 - Effects of urbanization on three ponds in Middleton, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-19T15:36:40","indexId":"wri844051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4051","title":"Effects of urbanization on three ponds in Middleton, Wisconsin","docAbstract":"<p>A digital hydrologic model was used to simulate the effects of future residential development on pond inflow volumes and resulting water levels of three ponds in Middleton, Wisconsin. The model computed the daily water budget and the resulting water level for each pond. The results of the model calibration are presented in the report, along with the existing watershed hydrologic conditions and runoff volumes for the 1982 study period. Data was collected during 1982 to claibrate the model; the data included pond stage, ground-water levels, precipitation and other meteorological characteristics. In addition, water-quality samples were collected at each pond to characterize the water quality. Simulation of pond levels with the 1982 rainfall and fully developed watersheds did not result in stages greater than those observed in 1982. Simulation of pond levels with rainfall having a 20-year recurrence interval (1978) and hypothetical, fully developed watersheds resulted in maximum pond stages above those observed in 1982. Peak stage of Tiedeman 's Pond would increase by 2.77 feet, Stricker 's Pond by 3.91 feet, and Esser 's Pond by 1.44 feet. Simulation of pond levels with an estimated 100-year rainfall and hyopthetical, fully developed watersheds would result in peak stage increases of 5.30, 5.32, and 1.97 feet above the peak 1982 observed stages for Tiedeman's, Stricker's, and Esser 's Ponds, respectively. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844051","usgsCitation":"House, L.B., 1984, Effects of urbanization on three ponds in Middleton, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 84-4051, Report: iv, 17 p.; 1 Plate: 34.50 x 18.25 inches, https://doi.org/10.3133/wri844051.","productDescription":"Report: iv, 17 p.; 1 Plate: 34.50 x 18.25 inches","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":56616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4051/report-thumb.jpg"},{"id":56615,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane","city":"Middleton","otherGeospatial":"Esser's Pond, Stricker's Pond, Tiedeman's Pond","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.52638626098633,\n              43.07948352439867\n            ],\n            [\n              -89.52638626098633,\n              43.098914753540164\n            ],\n            [\n              -89.49402809143066,\n              43.098914753540164\n            ],\n            [\n              -89.49402809143066,\n              43.07948352439867\n            ],\n            [\n              -89.52638626098633,\n              43.07948352439867\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6024e2","contributors":{"authors":[{"text":"House, Leo B.","contributorId":70766,"corporation":false,"usgs":true,"family":"House","given":"Leo","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198668,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30368,"text":"wri844287 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Thames River basin","interactions":[],"lastModifiedDate":"2022-01-19T19:32:10.670286","indexId":"wri844287","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4287","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Thames River basin","docAbstract":"<p>The Thames River basin includes streams draining the Quinebaug River (141 square miles), French River (99.5 square miles), and Middle River (about 6 square miles) basins in south central Massachusetts. Drainage areas, using the latest available 1:24 ,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics at seven sites, were calculated using a new data base with daily flow records through 1980. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10 year recurrence intervals. Seven-day low-flow statistics are presented for 32 partial-record sites, and the procedures used to determine the hydrologic characteristics of the basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are provided for seven gaged streams. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844287","usgsCitation":"Wandle, S.W., and LeBlanc, J.A., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Thames River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4287, iv, 31 p., https://doi.org/10.3133/wri844287.","productDescription":"iv, 31 p.","costCenters":[],"links":[{"id":394531,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36130.htm"},{"id":59154,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4287/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4287/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Thames River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.225,\n              42\n            ],\n            [\n              -71.747,\n              42\n            ],\n            [\n              -71.747,\n              42.249\n            ],\n            [\n              -72.225,\n              42.249\n            ],\n            [\n              -72.225,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11e7","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBlanc, J. A.","contributorId":51795,"corporation":false,"usgs":true,"family":"LeBlanc","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203135,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30367,"text":"wri844283 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Taunton and Ten Mile River basins and coastal river basins of Mount Hope Bay, Narragansett Bay, and Rhode Island Sound","interactions":[],"lastModifiedDate":"2022-01-19T19:28:42.483747","indexId":"wri844283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4283","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Taunton and Ten Mile River basins and coastal river basins of Mount Hope Bay, Narragansett Bay, and Rhode Island Sound","docAbstract":"<p>The study area includes streams draining the Taunton River (562 square miles), the Tenmile River (53.1 square miles), and the minor streams flowing into Mount Hope Bay, Narragansett Bay, and Rhode Island Sound in southern Massachusetts, and adjacent areas of Rhode Island. Drainage areas, using the latest available 1:24 ,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were re-computed for data-collection sites. Streamflow characteristics, at 10 gaging stations were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 44 partial-record sites and the procedures used to determine the hydrologic characteristics of a basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for selected gaged streams. This gazetteer will aid in the planning and managing of water-resources related activities, and will provide a common data base for governmental agencies and the engineering and planning communities.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844283","usgsCitation":"Wandle, S.W., and Keezer, G.R., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Taunton and Ten Mile River basins and coastal river basins of Mount Hope Bay, Narragansett Bay, and Rhode Island Sound: U.S. Geological Survey Water-Resources Investigations Report 84-4283, iv, 42 p., https://doi.org/10.3133/wri844283.","productDescription":"iv, 42 p.","costCenters":[],"links":[{"id":394530,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36126.htm"},{"id":59153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4283/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4283/report-thumb.jpg"}],"country":"United States","state":"Massachusetts, Rhode Island","otherGeospatial":"Mount Hope Bay, Narragansett Bay, Rhode Island Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.386,\n              41.5\n            ],\n            [\n              -70.739,\n              41.5\n            ],\n            [\n              -70.739,\n              42.1320\n            ],\n            [\n              -71.386,\n              42.1320\n            ],\n            [\n              -71.386,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11db","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keezer, G. R.","contributorId":13281,"corporation":false,"usgs":true,"family":"Keezer","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30366,"text":"wri844284 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Merrimack River basin","interactions":[],"lastModifiedDate":"2022-01-19T19:23:31.777762","indexId":"wri844284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4284","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Merrimack River basin","docAbstract":"<p>The Merrimack River basin in northeastern Massachusetts includes streams draining the Nashua (507 square miles), Concord (400 square miles), Shawsheen (78.0 square miles), and lower Merrimack (275 square miles) River basins. Drainage areas using the latest available 1:24,000 scale topographic maps were computed for the first time for streams draining more than 3 square miles and were recomputed for data collection sites. Streamflow characteristics at 12 gaging stations were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics , duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 79 partial-record sites and procedures used to determine the hydrologic characteristics of a basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for 12 gaged streams. This gazetteer will aid in the planning and siting of water-resources related activities, and will provide a common data base for governmental agencies and the engineering and planning communities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844284","usgsCitation":"Wandle, S.W., and Fontaine, R.A., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Merrimack River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4284, iv, 58 p., https://doi.org/10.3133/wri844284.","productDescription":"iv, 58 p.","costCenters":[],"links":[{"id":59152,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4284/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122912,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4284/report-thumb.jpg"},{"id":394529,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36127.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Merrimack River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72,\n              42.208\n            ],\n            [\n              -70.818,\n              42.208\n            ],\n            [\n              -70.818,\n              42.887\n            ],\n            [\n              -72,\n              42.887\n            ],\n            [\n              -72,\n              42.208\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11ae","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fontaine, R. A.","contributorId":78331,"corporation":false,"usgs":true,"family":"Fontaine","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":203131,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30365,"text":"wri834250 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Hudson River basin","interactions":[],"lastModifiedDate":"2022-01-24T19:29:58.062323","indexId":"wri834250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4250","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Hudson River basin","docAbstract":"<p>The Hudson River basin includes streams draining the Hoosic River (205 square miles), Kinderhook Creek (20.9 square miles), and Roeliff Jansen Kill (13.3 square miles) basins in western Massachusetts, eastern New York, and southern Vermont. Drainage areas, using the latest available 1:24,000 scale topographic maps, are re-computed for data-collection sites and computed for the first time for streams draining greater than 3 square miles. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for the five gaged streams in the Hoosic River basin. Streamflow characteristics, representing statistics computed using a new data base with records through 1979, include annual and monthly flow statistics , duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 21 partial-record sites. The procedures used to determine the hydrologic characteristics are summarized. This gazetteer of hydrologic characteristics will aid in the planning and siting of water-resources-related activities and will provide a common data base for governmental agencies and the engineering and planning communities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834250","usgsCitation":"Wandle, S.W., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Hudson River basin: U.S. Geological Survey Water-Resources Investigations Report 83-4250, iv, 24 p., https://doi.org/10.3133/wri834250.","productDescription":"iv, 24 p.","costCenters":[],"links":[{"id":394768,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35883.htm"},{"id":59151,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4250/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4250/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Hudson River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.508,\n              42.052\n            ],\n            [\n              -73.067,\n              42.052\n            ],\n            [\n              -73.067,\n              42.75\n            ],\n            [\n              -73.508,\n              42.75\n            ],\n            [\n              -73.508,\n              42.052\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b122c","contributors":{"authors":[{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":203130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30364,"text":"wri844285 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Housatonic River basin","interactions":[],"lastModifiedDate":"2022-01-19T19:19:38.094155","indexId":"wri844285","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4285","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Housatonic River basin","docAbstract":"<p>The Housatonic River basin includes streams that drain 504 square miles in western Massachusetts and 30.5 square miles in eastern New York. Drainage areas, using the latest available 1:24,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics for four gaged streams were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 52 partial-record sites, and the procedures used to determine the hydrologic characteristics of the basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are provided for selected gaging stations. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844285","usgsCitation":"Wandle, S.W., and Lippert, R.G., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Housatonic River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4285, iv, 34 p., https://doi.org/10.3133/wri844285.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":394528,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36128.htm"},{"id":124256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4285/report-thumb.jpg"},{"id":59150,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4285/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Housatonic River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              42.05\n            ],\n            [\n              -73.028,\n              42.05\n            ],\n            [\n              -73.028,\n              42.567\n            ],\n            [\n              -73.5,\n              42.567\n            ],\n            [\n              -73.5,\n              42.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1172","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lippert, R. G.","contributorId":68356,"corporation":false,"usgs":true,"family":"Lippert","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203128,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48900,"text":"ofr84717 - 1984 - Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama, fiscal year 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr84717","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-717","title":"Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama, fiscal year 1983","language":"ENGLISH","doi":"10.3133/ofr84717","usgsCitation":"Morris, F., 1984, Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama, fiscal year 1983: U.S. Geological Survey Open-File Report 84-717, iv, 174 leaves : ill., map ; 29 x 40 cm., https://doi.org/10.3133/ofr84717.","productDescription":"iv, 174 leaves : ill., map ; 29 x 40 cm.","costCenters":[],"links":[{"id":162105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60672f","contributors":{"authors":[{"text":"Morris, Fred III","contributorId":103693,"corporation":false,"usgs":true,"family":"Morris","given":"Fred","suffix":"III","email":"","affiliations":[],"preferred":false,"id":238539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30363,"text":"wri844282 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Connecticut River basin","interactions":[],"lastModifiedDate":"2022-01-19T19:16:20.225932","indexId":"wri844282","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4282","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Connecticut River basin","docAbstract":"<p>The Connecticut River basin study area includes streams draining the Ashuelot River (6.6 square miles), Millers River (389 square miles), Deerfield River (663 square miles), Chicopee River (727 square miles), Westfield River (517 square miles), Farmington River (158 square miles), and Connecticut River lowlands (656 square miles) basin in western Massachusetts, northern Connecticut, southern Vermont, and southern New Hampshire. Drainage areas, using the latest available 1:24,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were re-computed for data-collection sites. Streamflow characteristics at 45 gaging stations, representing statistics were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 118 partial-record sites, and the procedures used to determine the hydrologic characteristics of a basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for 54 sites in the Connecticut River basin. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844282","usgsCitation":"Wandle, S.W., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Connecticut River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4282, iv, 114 p., https://doi.org/10.3133/wri844282.","productDescription":"iv, 114 p.","costCenters":[],"links":[{"id":394527,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36125.htm"},{"id":59149,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4282/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4282/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Connecticut River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.167,\n              42\n            ],\n            [\n              -71.924,\n              42\n            ],\n            [\n              -71.924,\n              42.741\n            ],\n            [\n              -73.167,\n              42.741\n            ],\n            [\n              -73.167,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae74f","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48896,"text":"ofr84431 - 1984 - Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal","interactions":[{"subject":{"id":48896,"text":"ofr84431 - 1984 - Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal","indexId":"ofr84431","publicationYear":"1984","noYear":false,"title":"Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal"},"predicate":"SUPERSEDED_BY","object":{"id":6355,"text":"pp1257 - 1987 - Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal","indexId":"pp1257","publicationYear":"1987","noYear":false,"title":"Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal"},"id":1}],"supersededBy":{"id":6355,"text":"pp1257 - 1987 - Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal","indexId":"pp1257","publicationYear":"1987","noYear":false,"title":"Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal"},"lastModifiedDate":"2018-11-06T14:41:30","indexId":"ofr84431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-431","title":"Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal","docAbstract":"<p>The Denver metropolitan area is experiencing a rapid population growth that is requiring increasing supplies of potable water to be pumped from bedrock aquifers in order to meet demand. In an effort to determine the ability of the aquifers to continue to meet this demand, the Colorado Department of Natural Resources, the Denver Board of Water Commissioners, and Adams, Arapahoe, Douglas, Elbert and El Paso Counties joined with the U.S. Geological Survey in undertaking a hydrologic evaluation of the ground-water resources of the basin. This involved mapping of aquifer extent, thickness, structure, hydraulic characteristics, and water-level and water-quality conditions. This enabled ground-water modeling techniques to be used to simulate aquifer response to various pumpage estimates and ground-water development plans.</p><p>The Laramie-Fox Hills aquifer (the deepest aquifer) underlies the 6,700-square-mile study area and is overlain by the more permeable Arapahoe aquifer, the Denver aquifer, and the Dawson aquifer, which crops out in the southern part of the study area. It is estimated that 260x10<sup>6</sup> acre-feet of recoverable ground water are in storage in these four bedrock aquifers. However, less than 0.1 percent of this volume of water is stored under confined conditions. The larger volume of water stored under unconfined conditions will be available for use only when the water levels in the confined aquifers&nbsp;decline below the top of the individual aquifer, allowing water-table conditions to develop.</p><p>Annual precipitation on the Denver basin supplies an average of 6,900 cubic feet per second of water to the area; about 55 cubic feet per second of this recharges the bedrock aquifers, principally through the Dawson Arkose. The direction of ground-water movement is generally from ground-water divides in the southern part of the area northward toward the margins of the aquifers. Pumpage has ranged from about 5 cubic feet per second in 1884 to about 41 cubic feet per second in 1978. Pumpage exceeds recharge in the metropolitan area and has caused water-level declines (1958-78) to exceed 200 feet in a 135-square-mile area of the Arapahoe aquifer southeast of Denver.</p><p>A quasi-three-dimensional finite-difference model of the aquifer system was constructed and calibrated under steady-state and transient-state conditions. Steady-state calibration indicated that lateral hydraulic conductivity within the aquifers is about 100,000 times larger than the vertical hydraulic conductivity between the aquifers. Transient-state calibration indicated that between 1958 and 1978, 374,000 acre-feet of water was pumped from the aquifers, producing a 90,000-acre-foot net decrease in the volume of water in storage in the aquifers. During this time, pumpage also changed the rates of interaquifer flow, induced additional recharge, and caused capture of natural discharge.</p><p>Three 1979-2050 pumpage estimates were made for use in simulating the effects of various ground-water development plans. Simulations using each of these pumpage estimates indicate that by the year 2050 large water-level declines could occur, particularly in the deeper aquifers. Maximum water-level declines of 410, 1,700, and 1,830 feet were produced using the small, medium, and large pumping rates.</p><p>Four plans for supplementing the Denver water supply include pumping a satellite well field, pumping a municipal well field, pumping to irrigate parks, and injecting water during periods of low demand for later use during periods of peak demand. Model simulation of these plans indicates that the satellite well field will yield twice as much water as the municipal well field, but will produce larger and more widespread water-level declines in the four aquifers. The municipal well field would not significantly affect water levels in the Dawson aquifer. Pumping the Arapahoe aquifer to supply irrigation water to selected parks was shown to produce only small water-level declines in the aquifer. Results of simulating injection-pumpage well fields at two locations indicate that simulated injection rates could range from 1.7 to 10 cubic feet per second, depending on the choice of site. The volume of water that could be stored in the bedrock aquifer is, thus, sensitive to the hydrologic characteristics of the chosen site. More study is needed to evaluate water-chemistry compatibility of native and injected water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84431","usgsCitation":"Robson, S.G., 1984, Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal: U.S. Geological Survey Open-File Report 84-431, Report: vii, 111 p.; 5 Plates: 29.87 x 40.03 inches or smaller, https://doi.org/10.3133/ofr84431.","productDescription":"Report: vii, 111 p.; 5 Plates: 29.87 x 40.03 inches or smaller","costCenters":[],"links":[{"id":162405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0431/report-thumb.jpg"},{"id":359231,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0431/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359232,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0431/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359233,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0431/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359234,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0431/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359235,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0431/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359236,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0431/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Denver basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.32318115234375,\n              38.77978137804918\n            ],\n            [\n              -103.68072509765625,\n              38.77978137804918\n            ],\n            [\n              -103.68072509765625,\n              40.46157664398329\n            ],\n            [\n              -105.32318115234375,\n              40.46157664398329\n            ],\n            [\n              -105.32318115234375,\n              38.77978137804918\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63da50","contributors":{"authors":[{"text":"Robson, S. G.","contributorId":97102,"corporation":false,"usgs":true,"family":"Robson","given":"S.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":238534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48838,"text":"ofr83852 - 1984 - Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","interactions":[],"lastModifiedDate":"2012-02-02T00:10:05","indexId":"ofr83852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-852","title":"Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","docAbstract":"A series of workshops was conducted in September, 1982, by staff of the Virginia Office, Mid-Atlantic District of the U.S.-Geological Survey for the benefit of coal operators, consultants, and resource managers in the coal-producing area of southwest Virginia. The purpose of the workshop series was to present hydrologic information and data by the U.S. Geological Survey collected during four years of study of the. coal hydrology of Virginia. The workshop series was held one day a week for three weeks at two locations within southwest Virginia in order to reduce travel time and overnight travel costs for participants. Results of an independently conducted questionnaire indicate the series was a success. The report summarizes the workshop preparation, organization, and presentation, and gives general conclusions and suggestions for those interested in conducting workshops.","language":"ENGLISH","doi":"10.3133/ofr83852","usgsCitation":"Hufschmidt, P.W., 1984, Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\": U.S. Geological Survey Open-File Report 83-852, 23 p.  ill., map ; 28 cm., https://doi.org/10.3133/ofr83852.","productDescription":"23 p.  ill., map ; 28 cm.","costCenters":[],"links":[{"id":162746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0852/report-thumb.jpg"},{"id":85671,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0852/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db44","contributors":{"authors":[{"text":"Hufschmidt, Peter W.","contributorId":85185,"corporation":false,"usgs":true,"family":"Hufschmidt","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":238394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30362,"text":"wri844288 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the South Shore and Buzzards Bay","interactions":[],"lastModifiedDate":"2022-01-18T23:00:34.339204","indexId":"wri844288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4288","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the South Shore and Buzzards Bay","docAbstract":"<p>The coastal river basins include the minor river basins draining into Massachusetts Bay along the South Shore or into Buzzards Bay. The larger of these basins are the North, South, Jones, Wareham, Weweantic, Mattapoisett, Acushnet, and Slocums River basins. Drainage areas, using the latest available 1:24,000 scale topographic maps, were computed for data collection sites. Statistics on streamflow characteristics computed with a new data base are presented for six gaged streams. Daily-flow records through 1982 were used to compute annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 49 partial-record sites and procedures used to determine the hydrologic characteristics of the basin are summarized. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844288","usgsCitation":"Wandle, S.W., and Morgan, M., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the South Shore and Buzzards Bay: U.S. Geological Survey Water-Resources Investigations Report 84-4288, iv, 30 p., https://doi.org/10.3133/wri844288.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":59148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4288/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394489,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36131.htm"},{"id":122963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4288/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"coastal river basins of the South Shore and Buzzards Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.158447265625,\n              41.47360232634395\n            ],\n            [\n              -70.543212890625,\n              41.47360232634395\n            ],\n            [\n              -70.543212890625,\n              42.271211911185354\n            ],\n            [\n              -71.158447265625,\n              42.271211911185354\n            ],\n            [\n              -71.158447265625,\n              41.47360232634395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b11ec","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, M. A.","contributorId":32203,"corporation":false,"usgs":true,"family":"Morgan","given":"M. A.","affiliations":[],"preferred":false,"id":203125,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30361,"text":"wri844281 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the North Shore and Massachusetts Bay","interactions":[],"lastModifiedDate":"2022-01-18T22:57:47.115066","indexId":"wri844281","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4281","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the North Shore and Massachusetts Bay","docAbstract":"The coastal river basins of the North Shore and Boston Bay include streams draining the Parker River (60.4 square miles), Rowley River (9.9 square miles), Ipswich River (156 miles), Mystic River (66.0 square miles), Charles River (311 square miles), Neponset River (117 square miles), Weymouth Fore and Weymouth Back Rivers (about 63 square miles) and Weir River (about 20 square miles) basins. The study area in eastern and northeastern Massachusetts also includes the minor river basins draining into Massachusetts Bay, Ipswich Bay, or the Atlantic Ocean. Drainage areas using the latest available 1:24,000 scale topographic maps were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics at 15 gaging stations were calculated using a new data base with daily flow records through 1981. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. Seven-day low-flow statistics are presented for 95 partial-record sites and the procedures used to determine the hydrologic characteristics of a basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for 15 gaged streams. This gazetteer will aid in the planning and siting of water-resources related activities and will provide a common data base for governmental agencies and the engineering and planning communities. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844281","usgsCitation":"Wandle, S.W., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Coastal river basins of the North Shore and Massachusetts Bay: U.S. Geological Survey Water-Resources Investigations Report 84-4281, iv, 64 p., https://doi.org/10.3133/wri844281.","productDescription":"iv, 64 p.","costCenters":[],"links":[{"id":124079,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4281/report-thumb.jpg"},{"id":59147,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4281/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394488,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36124.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"coastal river basins of the North Shore and Massachusetts Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.38092041015625,\n              42.09822241118974\n            ],\n            [\n              -70.477294921875,\n              42.09822241118974\n            ],\n            [\n              -70.477294921875,\n              42.66628070564928\n            ],\n            [\n              -71.38092041015625,\n              42.66628070564928\n            ],\n            [\n              -71.38092041015625,\n              42.09822241118974\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b126f","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30360,"text":"wri844286 - 1984 - Gazetteer of hydrologic characteristics of streams in Massachusetts — Blackstone River basin","interactions":[],"lastModifiedDate":"2022-01-18T22:52:25.861482","indexId":"wri844286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4286","title":"Gazetteer of hydrologic characteristics of streams in Massachusetts — Blackstone River basin","docAbstract":"<p>The Blackstone River basin encompasses 335 square miles in south-central Massachusetts, including parts of Bristol, Middlesex, Norfolk, and Worcester Counties. Drainage areas, using the latest available 1:24,000 scale topographic maps, were computed for the first time for streams draining more than 3 square miles and were recomputed for data-collection sites. Streamflow characteristics, were calculated using a new data base with records through 1980. These characteristics include annual and monthly flow statistics, duration of daily flow values, and the annual 7-day mean low flow at the 2-year and 10-year recurrence intervals. The 7-day, 10-year low-flow values are presented for 31 partial-record sites and the procedures used to determine the hydrologic characteristics of the basin are summarized. Basin characteristics representing 14 commonly used indices to estimate various streamflows are presented for the six gaged streams in the Blackstone River basin. This gazetteer will aid in the planning and siting of water-resources-related activities and will provide a common data base for governmental agencies and the engineering and planning communities.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844286","usgsCitation":"Wandle, S.W., and Phipps, A.F., 1984, Gazetteer of hydrologic characteristics of streams in Massachusetts — Blackstone River basin: U.S. Geological Survey Water-Resources Investigations Report 84-4286, iv, 30 p., https://doi.org/10.3133/wri844286.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":59146,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4286/report-thumb.jpg"},{"id":394487,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36129.htm"}],"country":"United States","state":"Massachusetts, Rhode Island","otherGeospatial":"Blackstone River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.862,\n              41.9\n            ],\n            [\n              -71.3380,\n              41.9\n            ],\n            [\n              -71.3380,\n              42.367\n            ],\n            [\n              -71.862,\n              42.367\n            ],\n            [\n              -71.862,\n              41.9\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b124b","contributors":{"authors":[{"text":"Wandle, S. W.","contributorId":86789,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phipps, A. F.","contributorId":44196,"corporation":false,"usgs":true,"family":"Phipps","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":203122,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29285,"text":"wri834215 - 1984 - Ground-water hydrology and quality before and after strip mining of a small watershed in Jefferson County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:45","indexId":"wri834215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4215","title":"Ground-water hydrology and quality before and after strip mining of a small watershed in Jefferson County, Ohio","docAbstract":"Ground-water conditions before and after surface mining of a small watershed are described as part of a study to determine the effects of mining on hydrologic systems. The watershed was underlain by stratified sedimentary rocks containing local aquifers above shaley clay beds associated with the major coal seams. Mining involved removing the overburden rocks, including most of the top aquifer, stripping the coal, and recontouring the overburden spoils to the approximate premining shape of the watershed. Replacement of the top aquifer by spoils during regrading has caused many changes in recharge and discharge rates, saturated thickness, aquifer characteristics, and water quality. In the middle aquifer there were changes in saturated thickness and water quality. Resaturation of the top-aquifer spoils during and after reclamation has been slow. Saturated thicknesses have ranged from zero initially after mining to 4 feet after 1 1/2 years. Water levels in the middle aquifer have risen from a few feet to 40 feet. Water quality generally has been degraded: concentrations of bicarbonate, calcium, magnesium , chloride, iron, manganese, sulfate, and dissolved solids have increased. Premining water types remained about the same after mining, except for some changes from bicarbonate type to sulfate type. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834215","usgsCitation":"Razem, A., 1984, Ground-water hydrology and quality before and after strip mining of a small watershed in Jefferson County, Ohio: U.S. Geological Survey Water-Resources Investigations Report 83-4215, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834215.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124212,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4215/report-thumb.jpg"},{"id":58130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4215/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668195","contributors":{"authors":[{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":201281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25622,"text":"wri844073 - 1984 - Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","interactions":[],"lastModifiedDate":"2021-01-27T19:54:28.722464","indexId":"wri844073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4073","title":"Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky","docAbstract":"Oil shales in Kentucky are rocks of predominantly Devonian age. The most prominant are the Ohio, Chattanooga, and New Albany Shales. A leaching study was done on six fresh oil shale samples and one retorted oil shale sample. Leaching reagents were distilled water, 0.0005 N sulfuric acid, and 0.05 N sulfuric acid. The concentration of constituents in the leachates were highly variable. The concentration of sodium, manganese, and zinc in the retorted shale leachate was several orders of magnitude higher than those of the leachates of fresh shale samples. The major oil shale outcrop covers approximately 1,000 square miles in a horseshoe pattern from Vanceburg, Lewis County , in the east, to Louisville, Jefferson County, in the west. The Kentucky, Red, and Licking Rivers cross the outcrop belt, the Rolling Fork River flows along the strike of the shale in the southwest part of the outcrop, and the Ohio River flows past the outcrop at the ends of the horseshoe. Oil shale does not appear to significantly alter the water quality of these streams. Oil shale is not an aquifer, but seeps and springs found in the shale indicate that water moves through it. Ground water quality is highly variable. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844073","usgsCitation":"Leung, S.S., Leist, D., Davis, R.W., and Cordiviola, S., 1984, Leaching study of oil shale in Kentucky: With a section on hydrologic reconnaissance of the oil shale outcrop in Kentucky: U.S. Geological Survey Water-Resources Investigations Report 84-4073, Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 inches, https://doi.org/10.3133/wri844073.","productDescription":"Report: viii, 68 p.; 1 Plate: 26.54 x 26.30 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W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194450,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordiviola, Steven","contributorId":24814,"corporation":false,"usgs":true,"family":"Cordiviola","given":"Steven","email":"","affiliations":[],"preferred":false,"id":194448,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25635,"text":"wri834119D - 1984 - Map showing outcrops of granitic rocks, Basin and Range Province, Nevada","interactions":[],"lastModifiedDate":"2020-03-27T14:54:31","indexId":"wri834119D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4119","chapter":"D","title":"Map showing outcrops of granitic rocks, Basin and Range Province, Nevada","docAbstract":"<p>This map report is one of a series of geologic and hydrologic maps covering all or parts of States within the Basin and Range province of the western United States. The map reports contain information on subjects that characterize the geohydrology of the province, including the ground-water hydrology, ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources. This work is a part of the U.S. Geological Survey's program for geologic and hydrologic evaluation of the Basin and Range province to identify potentially suitable regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984).</p><p>Data for this report were taken largely from Spengler and others (1979), supplemented by data from individual geologic maps and reports, following the project guidelines as defined in Sargent and Bedinger (1984). As used in this report, granitic rocks include granodiorite, quartz monzonite, and granite, and locally associated mafic rocks such as diorite and gabbro. In the Snake Range and Ruby Mountains, Stewart (1980) has recognized large areas as metamorphic core complexes, and in these complexes some plutonic masses may not extend to great depth because of lateral displacement along low-angle faults subsequent to intrusion.</p><p>The Description of Map Units includes the sources of data, the geologic, and if available, the radiometric age, lithologic character, type of intrusive body and relation to rock units, where known, for the granitic rocks within outlined and numbered areas in each county of the study area. The radiometric ages of the rock units are only those which are available and do not necessarily represent the entire age range of the geologic units.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834119D","usgsCitation":"Sargent, K.A., and Roggensack, K., 1984, Map showing outcrops of granitic rocks, Basin and Range Province, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4119, Report: 36 p.; 2 Plates: 44.34 x 34.69 inches and 43.46 x 37.84 inches, https://doi.org/10.3133/wri834119D.","productDescription":"Report: 36 p.; 2 Plates: 44.34 x 34.69 inches and 43.46 x 37.84 inches","costCenters":[],"links":[{"id":118874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4119d/report-thumb.jpg"},{"id":54388,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4119d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373628,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373629,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.0146484375,\n              35.02099970111467\n            ],\n            [\n              -114.027099609375,\n              35.02099970111467\n            ],\n            [\n              -114.027099609375,\n              42.00032514831621\n            ],\n            [\n              -120.0146484375,\n              42.00032514831621\n            ],\n            [\n              -120.0146484375,\n              35.02099970111467\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a37e6","contributors":{"authors":[{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194486,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roggensack, Kurt","contributorId":35771,"corporation":false,"usgs":true,"family":"Roggensack","given":"Kurt","email":"","affiliations":[],"preferred":false,"id":194485,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29849,"text":"wri844278 - 1984 - Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area","interactions":[],"lastModifiedDate":"2022-08-22T19:22:52.092101","indexId":"wri844278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4278","title":"Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area","docAbstract":"<p>The conceptual model of the Lassen system is termed a liquid-dominated hydrothermal system with a parasitic vapor-dominated zone. The essential feature of this model is that steam and steam-heated discharge at relatively high elevations in Lassen Volcanic National Park (LVNP) and liquid discharge with high chloride concentrations at relatively low elevations outside LVNP are both fed by an upflow of high-enthalpy two-phase fluid within the Park. Liquid flows laterally away from the upflow area towards the areas of high-chloride discharge, and steam rises through a vapor-dominated zone to feed the steam and steam-heated features. Numerical simulations show that several conditions are necessary for the development of this type of system, including (1) large-scale topographic relief, (2) an initial period of convective heating within an upflow zone followed by some change in hydrologic or geologic conditions that initiates drainage of liquid from portions of the upflow zone, and (3) low permeability barriers that inhibit the movement of cold water into the vapor zone. Simulations of thermal fluid withdrawal south of LVNP, carried out in order to determine the effects of such withdrawal on portions of the hydrothermal system within the Park, showed decreases in pressure and liquid saturation beneath the vapor zone which result in a temporary increase and subsequent decrease in the rate of upflow of steam.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844278","usgsCitation":"Sorey, M., and Ingebritsen, S.E., 1984, Quantitative analysis of the hydrothermal system in Lassen Volcanic National Park and Lassen Known Geothermal Resource Area: U.S. Geological Survey Water-Resources Investigations Report 84-4278, viii, 80 p., https://doi.org/10.3133/wri844278.","productDescription":"viii, 80 p.","costCenters":[],"links":[{"id":405396,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36121.htm","linkFileType":{"id":5,"text":"html"}},{"id":58658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4278/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4278/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Lassen Volcanic Park and Lassen Known Geothermal Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.9921875,\n              40.01078714046552\n            ],\n            [\n              -120.7012939453125,\n              40.01078714046552\n            ],\n            [\n              -120.7012939453125,\n              40.91766362458114\n            ],\n            [\n              -121.9921875,\n              40.91766362458114\n            ],\n            [\n              -121.9921875,\n              40.01078714046552\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ecb","contributors":{"authors":[{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":202238,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ingebritsen, S. E.","contributorId":8078,"corporation":false,"usgs":true,"family":"Ingebritsen","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202237,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25651,"text":"wri834116C - 1984 - Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Southern California","interactions":[],"lastModifiedDate":"2021-12-21T19:34:08.397851","indexId":"wri834116C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4116","chapter":"C","title":"Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Southern California","docAbstract":"<p>This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural resources. This information is the basis for a summary report that characterizes the Basin and Range Province. The geologic and hydrologic characterization will be used to evaluate the Province for prospective regions for further study relative to isolation of high-level radioactive waste. (Bedinger, Sargent and Reed, 1984).<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834116C","collaboration":"Prepared in cooperation with the California Division of Mines and Geology","usgsCitation":"Thompson, T., Nuter, J., Moyle, W.R., and Woolfenden, L.R., 1984, Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Southern California: U.S. Geological Survey Water-Resources Investigations Report 83-4116, Report: 7 p.; 2 Plates: 39.92 x 55.04 inches and 40.11 x 55.03 inches, https://doi.org/10.3133/wri834116C.","productDescription":"Report: 7 p.; 2 Plates: 39.92 x 55.04 inches and 40.11 x 55.03 inches","costCenters":[],"links":[{"id":393231,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54420,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4116c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393232,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4116c/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.697265625,\n              32.879587173066305\n            ],\n            [\n              -113.99414062499999,\n              34.52466147177172\n            ],\n            [\n              -119.970703125,\n              39.027718840211605\n            ],\n            [\n              -119.88281249999999,\n              36.27970720524017\n            ],\n            [\n              -117.94921874999999,\n              33.211116472416855\n            ],\n            [\n              -117.20214843749999,\n              32.69486597787505\n            ],\n            [\n              -114.697265625,\n              32.879587173066305\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605755","contributors":{"authors":[{"text":"Thompson, Thomas H.","contributorId":20748,"corporation":false,"usgs":true,"family":"Thompson","given":"Thomas H.","affiliations":[],"preferred":false,"id":194513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nuter, Janet","contributorId":89003,"corporation":false,"usgs":true,"family":"Nuter","given":"Janet","email":"","affiliations":[],"preferred":false,"id":194516,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194514,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Woolfenden, Linda R. 0000-0003-3500-4709 lrwoolfe@usgs.gov","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":1476,"corporation":false,"usgs":true,"family":"Woolfenden","given":"Linda","email":"lrwoolfe@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":194515,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25653,"text":"wri834120B - 1984 - Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon","interactions":[],"lastModifiedDate":"2022-02-04T21:00:44.583569","indexId":"wri834120B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4120","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon","docAbstract":"<p>This report on ground-water levels, springs and depth to ground water in the Basin and Range province of Oregon (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834120B","usgsCitation":"Reed, J., Bedinger, M.S., Gonthier, J.B., Langer, W.H., McFarland, W.D., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon: U.S. Geological Survey Water-Resources Investigations Report 83-4120, Report: 4 p.; 1 Plate: 37.78 x 43.53 inches, https://doi.org/10.3133/wri834120B.","productDescription":"Report: 4 p.; 1 Plate: 37.78 x 43.53 inches","costCenters":[],"links":[{"id":395493,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35771.htm"},{"id":123216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4120b/report-thumb.jpg"},{"id":54424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4120b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393235,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4120b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.49755859375,\n              42.049292638686836\n            ],\n            [\n              -117.00439453125,\n              42.049292638686836\n            ],\n            [\n              -117.00439453125,\n              44.33956524809713\n            ],\n            [\n              -122.49755859375,\n              44.33956524809713\n            ],\n            [\n              -122.49755859375,\n              42.049292638686836\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a56","contributors":{"authors":[{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":194521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194523,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gonthier, J. B.","contributorId":63805,"corporation":false,"usgs":true,"family":"Gonthier","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":194522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":828883,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McFarland, W. D.","contributorId":57099,"corporation":false,"usgs":true,"family":"McFarland","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":828884,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":828885,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":30317,"text":"wri844267 - 1984 - Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","interactions":[],"lastModifiedDate":"2022-01-10T20:59:45.500688","indexId":"wri844267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4267","title":"Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","docAbstract":"<p>Yucca Mountain, Nevada, is one of several sites under consideration for construction of the first repository for high-level nuclear waste. The climate is arid; few perennial streams are present in the region. Flash floods occasionally occur. The site is underlain by at least 1,800 meters of volcanic tuffs of Tertiary age; limestones and dolomites of Paleozoic age underlie much of the surrounding region, and, together with alluvial deposits, comprise the major aquifers. Yucca Mountain is in the Alkali Flat-Furnace Creek Ranch ground-water subbasin, which is part of the Death Valley ground-water basin. Discharge occurs at Alkali Flat almost entirely by evapotranspiration, and at Furnace Creek Ranch from small springs and seeps. Beneath Yucca Mountain, depth to water ranges from about 460 to 700 meters; the rock under consideration for construction of the repository is in the unsaturated zone. Rate of recharge at Yucca Mountain is small, perhaps much less than 5 millimeters per year. Within the saturated zone, water movement is principally along fractures. The hydraulic gradient is small east (downgradient) of Yucca Mountain, and increases to the north and west. Lack of effective-porosity data presently precludes accurate calculation of flow velocity and travel times.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844267","usgsCitation":"Waddell, R.K., Robison, J.H., and Blankennagel, R., 1984, Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983: U.S. Geological Survey Water-Resources Investigations Report 84-4267, vi, 72 p., https://doi.org/10.3133/wri844267.","productDescription":"vi, 72 p.","costCenters":[],"links":[{"id":394133,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36112.htm"},{"id":59109,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4267/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4267/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118,\n              35.833\n            ],\n            [\n              -114.5670,\n              35.833\n            ],\n            [\n              -114.5670,\n              38.466\n            ],\n            [\n              -118,\n              38.466\n            ],\n            [\n              -118,\n              35.833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604816","contributors":{"authors":[{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":203046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blankennagel, R. K.","contributorId":65078,"corporation":false,"usgs":true,"family":"Blankennagel","given":"R. K.","affiliations":[],"preferred":false,"id":203047,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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