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)
","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":26681,"text":"wri844248 - 1984 - Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri844248","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":"84-4248","title":"Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada","docAbstract":"Test well UE-25pNo1 was drilled in cooperation with the U.S. Department of Energy in the southwestern part of the Nevada Test Site, for investigations related to the isolation of high-level nuclear wastes. Rocks penetrated in the well are predominantly ash-flow tuffs of Tertiary age to a depth of 1,244 meters and dolomite of Paleozoic age to a total depth of 1,805 meters. Hydraulic head is 20 meters higher in the Paleozoic dolomite than in most of the Tertiary tuffs; this hydraulic-head difference indicates a major hydrologic barrier to the downward movement of fluid. Any vertical fluid movement from the Tertiary to the Paleozoic sections would be small, as would be movement from the Paleozoic rocks into the Tertiary rocks. In the Tertiary section, an interval of less than 30 meters in the upper Prow Pass Member of Crater Flat Tuff has an apparent transmissivity of 14 meters squared per day. In the Paleozoic section, an interval of less than 22 meters has an apparent transmissivity of 69 meters squared per day. Compositions of water from the Tertiary and Paleozoic sections are similar to regional waters from rocks of the same ages. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844248","usgsCitation":"Craig, R.W., and Robison, J.H., 1984, Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4248, vi, 57 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844248.","productDescription":"vi, 57 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":122883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4248/report-thumb.jpg"},{"id":55546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4248/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a79","contributors":{"authors":[{"text":"Craig, R. W.","contributorId":40984,"corporation":false,"usgs":true,"family":"Craig","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196820,"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":196821,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28728,"text":"wri844242 - 1984 - Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach","interactions":[],"lastModifiedDate":"2022-01-04T19:41:38.50013","indexId":"wri844242","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":"84-4242","title":"Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach","docAbstract":"An appraisal of Oregon ground-water quality was made using existing data accessible through the U.S. Geological Survey computer system. The data available for about 1,000 sites were separated by aquifer units and hydrologic units. Selected statistical moments were described for 19 constituents including major ions. About 96 percent of all sites in the data base were sampled only once. The sample data were classified by aquifer unit and hydrologic unit and analysis of variance was run to determine if significant differences exist between the units within each of these two classifications for the same 19 constituents on which statistical moments were determined. Results of the analysis of variance indicated both classification variables performed about the same, but aquifer unit did provide more separation for some constituents. Samples from the Rogue River basin were classified by location within the flow system and type of flow system. The samples were then analyzed using analysis of variance on 14 constituents to determine if there were significant differences between subsets classified by flow path. Results of this analysis were not definitive, but classification as to the type of flow system did indicate potential for segregating water-quality data into distinct subsets.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844242","usgsCitation":"Miller, T.L., and Gonthier, J.B., 1984, Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach: U.S. Geological Survey Water-Resources Investigations Report 84-4242, vii, 88 p., https://doi.org/10.3133/wri844242.","productDescription":"vii, 88 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":393870,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36091.htm"},{"id":57555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4242/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691139","contributors":{"authors":[{"text":"Miller, T. L.","contributorId":54557,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonthier, J. B.","contributorId":63805,"corporation":false,"usgs":true,"family":"Gonthier","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":200302,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26477,"text":"wri844181 - 1984 - Potential effects of surface coal mining on the hydrology of the Circle West coal tracts, McCone County, eastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri844181","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":"84-4181","title":"Potential effects of surface coal mining on the hydrology of the Circle West coal tracts, McCone County, eastern Montana","docAbstract":"The Circle West coal tracts in McCone County, Montana, contain about 460 million tons of recoverable coal reserves. Estimates of coal reserves for the tract are based predominantly on the S coal bed, which averages about 16 ft in thickness. About 175 million tons, or 38%, of the recoverable coal is Federally owned and has been identified for potential lease sale. A hydrologic study has been conducted in the potential lease area to describe existing hydrologic systems and to assess potential effects of surface coal mining on local water resources. Geohydrologic data collected from wells and drill holes indicate that shallow aquifers exist in sandstone and coal beds of the Tongue River Member of the Fort Union Formation (Paleocene age). These shallow aquifers generally have small values of hydraulic conductivity (0.1 to 380 ft/day) and typically yield from 2 to 20 gal/min to stock and domestic wells. Where coal is extremely fractured or the thickness of saturated sandstone is large, some wells can yield in excess of 70 gal/min. Chemical analyses indicate that most shallow aquifers contain a sodium sulfate bicarbonate type water. Surface water resources of the area consist of intermittent streamflow in parts of the Nelson and Timber Creek basins plus a large network of reservoirs. The reservoirs provide a large part of the water supply for area livestock and irrigation. Water quality data for Nelson and Timber Creeks indicate that the water generally is a sodium sulfate type and has a large concentration (181 to 6,960 mg/L) of dissolved solids. Mining of the S coal bed in the Circle West coal tracts would permanently remove shallow coal and sandstone aquifers, resulting in the loss of shallow stock wells. Mining would destroy livestock reservoirs, alter runoff characteristics of Nelson Creek, and temporarily lower water levels in shallow aquifers near the mine. Leaching of soluble constituents from mine spoils may cause a long-term degradation of the quality of water in shallow aquifers in and near the coal tracts. Some of the effects on local water supplies could be mitigated by development of alternative water resources in deeper aquifers such as the Tullock aquifer of Paleocene age and the Fox Hills-lower Hell Creek aquifer of Late Cretaceous age. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844181","usgsCitation":"Cannon, M.R., 1984, Potential effects of surface coal mining on the hydrology of the Circle West coal tracts, McCone County, eastern Montana: U.S. Geological Survey Water-Resources Investigations Report 84-4181, iv, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844181.","productDescription":"iv, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4181/report-thumb.jpg"},{"id":55298,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4181/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55299,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a60cd","contributors":{"authors":[{"text":"Cannon, M. R.","contributorId":99140,"corporation":false,"usgs":true,"family":"Cannon","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11086,"text":"ofr84708 - 1984 - State hydrologic unit maps","interactions":[{"subject":{"id":11086,"text":"ofr84708 - 1984 - State hydrologic unit maps","indexId":"ofr84708","publicationYear":"1984","noYear":false,"title":"State hydrologic unit maps"},"predicate":"SUPERSEDED_BY","object":{"id":2672,"text":"wsp2294 - 1987 - Hydrologic unit maps","indexId":"wsp2294","publicationYear":"1987","noYear":false,"title":"Hydrologic unit maps"},"id":1}],"supersededBy":{"id":2672,"text":"wsp2294 - 1987 - Hydrologic unit maps","indexId":"wsp2294","publicationYear":"1987","noYear":false,"title":"Hydrologic unit maps"},"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr84708","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":"84-708","title":"State hydrologic unit maps","docAbstract":"A set of maps depicting approved boundaries of, and numerical codes for, river-basin units of the United States has been developed by the U.S. Geological Survey. These ' State Hydrologic Unit Maps ' are four-color maps that present information on drainage, culture, hydrography, and hydrologic boundaries and codes: (1) the 21 major water-resources regions and the 222 subregions designated by the U.S. Water Resources Council; (2) the 352 accounting units of the U.S. Geological Survey 's National Water Data Network; and (3) the 2,149 cataloging units of the U.S. Geological Survey 's Catalog of Information on Water Data. The maps are plotted on the Geological Survey State base-map series at a scale of 1:500,000 and, except for Alaska, depict hydrologic unit boundaries for all drainage basins greater than 700 mi squared (1,813 km squared). A complete list of all the hydrologic units, along with their drainage areas, their names, and the names of the States or outlying areas in which they reside, is contained in the report. These maps and associated codes provide a standardized base for use by water-resources organizations in locating, storing, retrieving, and exchanging hydrologic data. The Hydrologic Unit Codes shown on the maps have been approved as a Federal Information Processing Standard for use by the Federal establishment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84708","usgsCitation":"Seaber, P., Kapinos, F., and Knapp, G., 1984, State hydrologic unit maps: U.S. Geological Survey Open-File Report 84-708, 175 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr84708.","productDescription":"175 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":143264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0708/report-thumb.jpg"},{"id":38845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0708/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489d17","contributors":{"authors":[{"text":"Seaber, P. R.","contributorId":53802,"corporation":false,"usgs":true,"family":"Seaber","given":"P. R.","affiliations":[],"preferred":false,"id":162508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapinos, F.P.","contributorId":73591,"corporation":false,"usgs":true,"family":"Kapinos","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":162509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knapp, G.L.","contributorId":108116,"corporation":false,"usgs":true,"family":"Knapp","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":162510,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":"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).
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).
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).
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.
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.
","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":67407,"text":"i1522D - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States; Pleistocene lakes and marshes","interactions":[{"subject":{"id":21415,"text":"ofr83751 - 1983 - Selected geologic and hydrologic characteristics of the Basin and Range Province, Western United States-- Pleistocene lakes and marshes","indexId":"ofr83751","publicationYear":"1983","noYear":false,"title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, Western United States-- Pleistocene lakes and marshes"},"predicate":"SUPERSEDED_BY","object":{"id":67407,"text":"i1522D - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States; Pleistocene lakes and marshes","indexId":"i1522D","publicationYear":"1984","noYear":false,"chapter":"D","title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States; Pleistocene lakes and marshes"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i1522D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1522","subseriesTitle":"NONE","chapter":"D","title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States; Pleistocene lakes and marshes","language":"ENGLISH","doi":"10.3133/i1522D","usgsCitation":"Williams, T., and Bedinger, M.S., 1984, Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States; Pleistocene lakes and marshes: U.S. Geological Survey IMAP 1522, 1 map :col. ;76 x 103 cm. on sheet 86 x 106 cm. folded in envelope 31 x 24 cm., https://doi.org/10.3133/i1522D.","productDescription":"1 map :col. ;76 x 103 cm. on sheet 86 x 106 cm. folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":106786,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9289.htm","linkFileType":{"id":5,"text":"html"},"description":"9289"},{"id":188679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,29 ], [ -123,44 ], [ -102,44 ], [ -102,29 ], [ -123,29 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa703","contributors":{"authors":[{"text":"Williams, T.R.","contributorId":6885,"corporation":false,"usgs":true,"family":"Williams","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":276139,"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":276140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25654,"text":"wri834116B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","interactions":[],"lastModifiedDate":"2020-03-27T14:22:19","indexId":"wri834116B","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":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","docAbstract":"This report on ground-water levels, springs and depth to ground water in the Basin and Range province of southern California (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.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834116B","usgsCitation":"Langer, W.H., Moyle, W., Woolfenden, L.R., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California: U.S. Geological Survey Water-Resources Investigations Report 83-4116, Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches, https://doi.org/10.3133/wri834116B.","productDescription":"Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches","costCenters":[],"links":[{"id":373616,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report-thumb.jpg"},{"id":373615,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.87158203125,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 32.509761735919426\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a5d","contributors":{"authors":[{"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":194526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moyle, W. R.","contributorId":27421,"corporation":false,"usgs":true,"family":"Moyle","given":"W. R.","affiliations":[],"preferred":false,"id":194524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woolfenden, L. R. 0000-0003-3500-4709","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":36945,"corporation":false,"usgs":true,"family":"Woolfenden","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194527,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47681,"text":"wri844357 - 1984 - Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1982-84","interactions":[],"lastModifiedDate":"2018-11-08T09:38:52","indexId":"wri844357","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":"84-4357","title":"Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1982-84","docAbstract":"Continuing studies are being made in west-central Kansas to provide up-to-date information to aid in the management of ground water for irrigation. This report, prepared in cooperation with the Western Kansas Groundwater Management District No. 1, presents the fourth in a series of studies that uses a statistical technique, called kriging, to produce hydrologic maps that are used as management tools.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844357","usgsCitation":"Pabst, M.E., and Dague, B.J., 1984, Percentage change in saturated thickness of the High Plains Aquifer, west-central Kansas, 1950 to average 1982-84: U.S. Geological Survey Water-Resources Investigations Report 84-4357, 54.74 x 32.53 inches, https://doi.org/10.3133/wri844357.","productDescription":"54.74 x 32.53 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":359298,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4357/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102,\n 38.3\n ],\n [\n -100.245,\n 38.3\n ],\n [\n -100.25,\n 38.55\n ],\n [\n -102,\n 38.55\n ],\n [\n -102,\n 38.3\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688732","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":235997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dague, Barbara J.","contributorId":84811,"corporation":false,"usgs":true,"family":"Dague","given":"Barbara","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":725478,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15729,"text":"ofr84233 - 1984 - Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia","interactions":[],"lastModifiedDate":"2024-12-04T21:00:35.905241","indexId":"ofr84233","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":"84-233","title":"Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84233","usgsCitation":"Roth, D., and Cooper, S., 1984, Hydrology of area 11, Eastern Coal Province, Ohio, Kentucky, and West Virginia: U.S. Geological Survey Open-File Report 84-233, v, 66 p., https://doi.org/10.3133/ofr84233.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":464766,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13321.htm","linkFileType":{"id":5,"text":"html"}},{"id":146462,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0233/report-thumb.jpg"},{"id":95324,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0233/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucky, Ohio, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83.86623180747648,\n 36.731743994525004\n ],\n [\n -81.43264711571662,\n 37.927674336656665\n ],\n [\n -81.0549105792823,\n 40.470417310879355\n ],\n [\n -81.04739335783368,\n 41.3198369033787\n ],\n [\n -82.26961292288702,\n 41.177583641541645\n ],\n [\n -84.09257837635606,\n 39.6683312010673\n ],\n [\n -84.68344347599752,\n 37.24430123159996\n ],\n [\n -83.86623180747648,\n 36.731743994525004\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604706","contributors":{"authors":[{"text":"Roth, D.K.","contributorId":60275,"corporation":false,"usgs":true,"family":"Roth","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":171607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, S.C.","contributorId":75284,"corporation":false,"usgs":true,"family":"Cooper","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":171608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47683,"text":"wri844270 - 1984 - Geohydrologic conditions in the Vekol Valley, Pinal and Maricopa Counties, Arizona-1983","interactions":[],"lastModifiedDate":"2024-06-17T21:30:19.710164","indexId":"wri844270","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":"84-4270","title":"Geohydrologic conditions in the Vekol Valley, Pinal and Maricopa Counties, Arizona-1983","docAbstract":"Vekol Valley is a north-trending valley in south-central Arizona. The valley includes 270 mi2 and is bounded by the Table Top and Vekol Mountains on the east, the Sand Tank and Maricopa Mountains and the White Hills on the west, and the Both and Haley Hills on the north. The climate is semiarid and precipitation occurs as local summer thunderstorms and regional winter storms. The average annual precipitation is 7 to 8 in., and the potential evaporation rate is about 10 times that of the average annual rainfall (Sells and Hill, 1974, p. 7, 44). Storm runoff occurs mainly as sheetflow and floods of short duration. Although some runoff is diverted into catchment tanks for use by livestock, runoff is not used for irrigation or public supply.
Vekol Valley is underlain by a thick sequence of basin sediments, sedimentary rocks, and volcanic rocks. The surrounding mountains are composed of crystalline and volcanic rocks, which also underlie the basin sediments to form the sides and bottom of the basin. The valley is divided into a northern part and a southern part by a bedrock outcrop of crystalline rocks between the White Hills on the west and the Table Top Mountains on the east (R. P. Wilson, 1979, p. 8). The northern part is about 90 mi2 (J. R. Marie and K. J. Hollett, U.S. Geological Survey, written commun., 1984) and the southern part is about 180 mi2.
The hydrologic data on which this map is based are available, for the most part, in computer-printout form and may be consulted at the Arizona Department of Water Resources, 99 East Virginia, Phoenix, and the U.S. Geological Survey offices in: Federal Building, 301 West Congress Street, Tucson , and 3788 North 16th Street, Suite E, Phoenix. Material from which copies can be made at private expense is available at the Tuscon and Phoenix offices of the U.S. Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844270","collaboration":"Prepared in cooperation with the U.S. Bureau of Indian Affairs","usgsCitation":"Cuff, M.K., 1984, Geohydrologic conditions in the Vekol Valley, Pinal and Maricopa Counties, Arizona-1983: U.S. Geological Survey Water-Resources Investigations Report 84-4270, 1 Plate: 40.12 x 34.31 inches, https://doi.org/10.3133/wri844270.","productDescription":"1 Plate: 40.12 x 34.31 inches","costCenters":[],"links":[{"id":161672,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4270/report-thumb.jpg"},{"id":84592,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4270/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":430341,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36114.htm","linkFileType":{"id":5,"text":"html"}}],"datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Arizona","county":"Maricopa County, Pinal County","otherGeospatial":"Vekol Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.5,\n 32.5\n ],\n [\n -112,\n 32.5\n ],\n [\n -112,\n 33\n ],\n [\n -112.5,\n 33\n ],\n [\n -112.5,\n 32.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eac","contributors":{"authors":[{"text":"Cuff, Melinda K.","contributorId":37786,"corporation":false,"usgs":true,"family":"Cuff","given":"Melinda","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":236000,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12618,"text":"ofr84745 - 1984 - Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Evaluation of the regions","interactions":[],"lastModifiedDate":"2022-06-16T21:10:44.904521","indexId":"ofr84745","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":"84-745","title":"Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Evaluation of the regions","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84745","usgsCitation":"1984, Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Evaluation of the regions: U.S. Geological Survey Open-File Report 84-745, Report: xii, 195 p.; 2 Plates: 29.08 × 40.51 inches and 35.24 × 29.92 inches, https://doi.org/10.3133/ofr84745.","productDescription":"Report: xii, 195 p.; 2 Plates: 29.08 × 40.51 inches and 35.24 × 29.92 inches","costCenters":[],"links":[{"id":41022,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0745/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0745/report-thumb.jpg"},{"id":41024,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0745/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41023,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0745/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402309,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27511.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, California, Idaho, Nevada, Oregon, Utah","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 -115.400390625,\n 32.76880048488168\n ],\n [\n -110.74218749999999,\n 31.80289258670676\n ],\n [\n -107.666015625,\n 32.02670629333614\n ],\n [\n -109.072265625,\n 39.842286020743394\n ],\n [\n -114.2578125,\n 44.33956524809713\n ],\n [\n -117.68554687499999,\n 44.715513732021336\n ],\n [\n -120.234375,\n 43.389081939117496\n ],\n [\n -120.84960937499999,\n 40.17887331434696\n ],\n [\n -119.61914062499999,\n 37.23032838760387\n ],\n [\n -115.400390625,\n 32.76880048488168\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fd8","contributors":{"editors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":503993,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503992,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":503991,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}} ,{"id":43479,"text":"ofr84430 - 1984 - Index of hydrologic data for selected sites in Dade County, Florida, 1923-80","interactions":[],"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr84430","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":"84-430","title":"Index of hydrologic data for selected sites in Dade County, Florida, 1923-80","docAbstract":"A comprehensive assessment of the surficial aquifers of southeast Florida, including the Biscayne aquifer, was begun in 1979 by the U.S. Geological Survey, in cooperation with the South Florida Water Management District. In the initial phase of the study, an inventory was made of existing data available in the files of the U.S. Geological Survey and other public agencies of Dade, Broward, and Palm Beach Counties. This report indexes, through tables and maps, the ground-water quality, ground-water level, surface-water stage, and geologic data bases for Dade County. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84430","usgsCitation":"Sonenshein, R., Causaras, C., and Fish, J.E., 1984, Index of hydrologic data for selected sites in Dade County, Florida, 1923-80: U.S. Geological Survey Open-File Report 84-430, 10 maps on 3 sheets :photocopy ;52 x 43 cm. and smaller on sheets 60 x 112 cm., folded in envelope 32 x 23 cm., https://doi.org/10.3133/ofr84430.","productDescription":"10 maps on 3 sheets :photocopy ;52 x 43 cm. and smaller on sheets 60 x 112 cm., folded in envelope 32 x 23 cm.","costCenters":[],"links":[{"id":173448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81142,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0430/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81143,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0430/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81144,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0430/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4293","contributors":{"authors":[{"text":"Sonenshein, R.S.","contributorId":10415,"corporation":false,"usgs":true,"family":"Sonenshein","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":228264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Causaras, C. R.","contributorId":66679,"corporation":false,"usgs":true,"family":"Causaras","given":"C. R.","affiliations":[],"preferred":false,"id":228265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fish, John E.","contributorId":85184,"corporation":false,"usgs":true,"family":"Fish","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":228266,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38497,"text":"pp1375 - 1984 - Geological Survey research, fiscal year 1981","interactions":[{"subject":{"id":70180414,"text":"70180414 - 1984 - Offset of Tertiary arcs on the Alaska Peninsula: A section in Geological Survey research, fiscal year 1981","indexId":"70180414","publicationYear":"1984","noYear":false,"title":"Offset of Tertiary arcs on the Alaska Peninsula: A section in Geological Survey research, fiscal year 1981"},"predicate":"IS_PART_OF","object":{"id":38497,"text":"pp1375 - 1984 - Geological Survey research, fiscal year 1981","indexId":"pp1375","publicationYear":"1984","noYear":false,"title":"Geological Survey research, fiscal year 1981"},"id":1}],"lastModifiedDate":"2018-06-12T12:51:59","indexId":"pp1375","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1375","title":"Geological Survey research, fiscal year 1981","docAbstract":"A summary of recent significant scientific and economic results accompanied by a list of geologic, hydrologic, and cartographic investigations in progress.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1375","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Geological Survey research, fiscal year 1981: U.S. Geological Survey Professional Paper 1375, vii, 424 p., https://doi.org/10.3133/pp1375.","productDescription":"vii, 424 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":65211,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1375/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1375/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673b2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20388,"text":"ofr8462 - 1984 - A selected bibliography of water resources publications for Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr8462","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":"84-62","title":"A selected bibliography of water resources publications for Mississippi","docAbstract":"Hydrologic data were collected at 15 stream sites draining potential lignite areas in Calhoun, Montgomery, and Webster Counties during a period of low streamflow. The total dissolved solids ranged from 25 to 14.9 mg/L and most major ion concentrations were less and suspended sediment concentrations were less than 30 mg/L. The pH ranged from 6.7 to 8.1 units. Aluminum concentrations ranged from less than 100 to 500 micrograms per liter. Chromium and zinc concentrations ranged from 1 to 10 micrograms per gram and mercury concentrations ranged from 0.01 to 0.04 micrograms per gram in bottom material. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8462","usgsCitation":"Parker, G., Walker, D., and Moss, C., 1984, A selected bibliography of water resources publications for Mississippi: U.S. Geological Survey Open-File Report 84-62, iii, 80 p. :maps ;28 cm., https://doi.org/10.3133/ofr8462.","productDescription":"iii, 80 p. :maps ;28 cm.","costCenters":[],"links":[{"id":153628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0062/report-thumb.jpg"},{"id":49937,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a655e","contributors":{"authors":[{"text":"Parker, G.G.","contributorId":107723,"corporation":false,"usgs":true,"family":"Parker","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":182567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, Debbe","contributorId":68762,"corporation":false,"usgs":true,"family":"Walker","given":"Debbe","email":"","affiliations":[],"preferred":false,"id":182566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moss, Carol","contributorId":35340,"corporation":false,"usgs":true,"family":"Moss","given":"Carol","affiliations":[],"preferred":false,"id":182565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28579,"text":"wri834128 - 1984 - Channel changes of Powder River between Moorhead and Broadus, Montana, 1939-1978","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri834128","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":"83-4128","title":"Channel changes of Powder River between Moorhead and Broadus, Montana, 1939-1978","docAbstract":"Bank erosion and changes in channel width, length, and pattern were determined for the Powder River between Moorhead and Broadus, Montana using maps of the bankfull channel made from aerial photographs taken during 1939, 1954, 1967, 1973, and 1978. Contemporaneous daily mean and peak discharge records from Moorhead provide the hydrologic data used to interpret the measurements. Magnitudes and frequency of flows were determined for each interval of time delimited by photographs. Bank erosion is related to the number of days that mean discharge was equal to or greater than bankfull (1.5-year flood). Mean channel width ranged between 264 ft (1973) and 415 ft (1967). The channel was wider after periods of higher annual peak flows. The channel lengthened between 1939 and 1978, although at least 12 meanders cut off between Moorhead and Broadus. Variable rates of lengthening in the reach reflect the degree of bedrock control in the valley and local variations in valley slope. Data from the Powder River verify the concept of thresholds of channel pattern stability that were demonstrated experimentally. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834128","usgsCitation":"Martinson, H.A., 1984, Channel changes of Powder River between Moorhead and Broadus, Montana, 1939-1978: U.S. Geological Survey Water-Resources Investigations Report 83-4128, vi, 62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834128.","productDescription":"vi, 62 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4128/report-thumb.jpg"},{"id":57402,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6378","contributors":{"authors":[{"text":"Martinson, H. A.","contributorId":16834,"corporation":false,"usgs":true,"family":"Martinson","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200057,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":"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.
","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":28744,"text":"wri834246 - 1984 - Ground water in the Fresno area, California; preliminary report","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834246","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":"83-4246","title":"Ground water in the Fresno area, California; preliminary report","docAbstract":"The U.S. Geological Survey, in cooperation with Fresno County, is developing a computer model of the unconfined aquifer system in the Fresno area. In the area, consolidated rocks are overlain by unconsolidated deposits. The unconsolidated deposits are divided into a lower fine-grained unit and an overlying coarse-grained unit. The system is assumed to be a single unconfined unit. The top of the system is the water table and the bottom is the base of the coarse-grained deposits. The northeastern boundary is the only natural lateral hydrologic boundary. The other lateral boundaries are placed so that errors along them will not affect heads in the area of interest. Initial heads for 1943, hydraulic conductivity, and bottom elevations were used in a steady-state model that generated net flux values. It is anticipated that most of the remaining effort will center on model calibration. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834246","usgsCitation":"Mitten, H., 1984, Ground water in the Fresno area, California; preliminary report: U.S. Geological Survey Water-Resources Investigations Report 83-4246, iv, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834246.","productDescription":"iv, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4246/report-thumb.jpg"},{"id":57594,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4246/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6744c4","contributors":{"authors":[{"text":"Mitten, H. T.","contributorId":88735,"corporation":false,"usgs":true,"family":"Mitten","given":"H. T.","affiliations":[],"preferred":false,"id":200326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":"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.
","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":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":"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.
","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":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}]}} ]}