{"pageNumber":"517","pageRowStart":"12900","pageSize":"25","recordCount":16449,"records":[{"id":16454,"text":"ofr85567 - 1985 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","interactions":[{"subject":{"id":16454,"text":"ofr85567 - 1985 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"ofr85567","publicationYear":"1985","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":2894,"text":"wsp2304 - 1989 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"wsp2304","publicationYear":"1989","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"id":1}],"supersededBy":{"id":2894,"text":"wsp2304 - 1989 - Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","indexId":"wsp2304","publicationYear":"1989","noYear":false,"title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas"},"lastModifiedDate":"2013-01-08T13:49:54","indexId":"ofr85567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-567","title":"Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas","docAbstract":"A study was conducted to evaluate the effects of potential development of the Dakota aquifer on the layered aquifer system above Permian rocks in a 5,000 sq mi area of southwestern Kansas. Transmissivity of the Dakota aquifer, determined from analyses of pumping tests, ranges from 100 to 7,100 sq ft/day. Water in the Dakota aquifer is a calcium bicarbonate type water, similar to water in the High Plains aquifer, in the subcrop area. However, in areas distant from the subcrop, water in the Dakota aquifer is a sodium bicarbonate type water with dissolved solids concentrations in excess of 500 mg/L. Gradual declines in the potentiometric surface of the Dakota aquifer have occurred since the onset of pumpage in the 1960's; however, water levels in some wells have risen during the late 1970's. A digital computer model of 3-D groundwater flow was developed to simulate hydrologic conditions of a five-layer hydrologic system for 1975-82 conditions. The major components of the simulated 1975-82 water budget were well discharge from the High Plains aquifer and loss of ground water from storage in the High Plains aquifer. Although downward leakage from the High Plains aquifer in the study area represented only 18,000 acre-ft of the 1,365 ,000 acre-ft discharged from the High Plains aquifer during 1982 , it was a major source of inflow to the Dakota aquifer. Changes in storage in the Dakota aquifer in the study area during 1982 were about 5,000 acre-ft. A base-line projection was made using 1982 simulated hydraulic heads from the calibrated model and 1982 rates of pumpage from both the High Plains and the Dakota aquifers for comparison with eight additional projection simulations in which maximum pumpage from the Dakota aquifer at the end of the projections ranged from about 78,000 to 294,000 acre-ft/yr. The results from the projections indicate that: (1) pumpage from the Dakota aquifer will have a limited effect on hydraulic heads in the High Plains aquifer, (2) drawdown in the hydraulic heads in the Dakota aquifer will result in conversion of much of the Dakota aquifer to unconfined conditions, (3) change in storage will become the major water-budget component for the Dakota aquifer, (4) continuation of 1982 rates of withdrawal from the High Plains aquifer will result in dewatering of a substantial part of the aquifer in the study area. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85567","usgsCitation":"Watts, K.R., 1985, Potential hydrologic effects of ground-water withdrawals from the Dakota Aquifer, southwestern Kansas: U.S. Geological Survey Open-File Report 85-567, x, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85567.","productDescription":"x, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0567/report-thumb.jpg"},{"id":265398,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0567/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a878b","contributors":{"authors":[{"text":"Watts, Kenneth R.","contributorId":43783,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":172878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14605,"text":"ofr85186 - 1985 - Selected hydrologic data for the Powell River basin in Wise County, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr85186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-186","title":"Selected hydrologic data for the Powell River basin in Wise County, Virginia","docAbstract":"Evaluation of selected surface-water, ground-water, and water-quality data shows that hydrologic data collected by governmental agencies comprises less than 10 percent of the total data available in the Powell River basin, Virginia. Only a small portion of the hydrologic data for the basin has been compiled and stored by Federal and state agencies in two computerized hydrologic indexing systems (National Water Data Exchange and Commonwealth Data Base). Selected ground-water, surface-water, and water-quality data collected in the Powell River Basin in Wise County, Virginia are summarized. The data are obtained from three coal-mining companies, the Virginia State Water Control Board, and the U.S. Geological Survey. Water-quality data for 61 ground-water and 86 surface-water sites indicate elevated iron and manganese concentrations are present throughout the basin. A bibliography of available hydrologic reports on the area and selected pertinent hydrologic reports from other coal-producing areas is present. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85186","usgsCitation":"Larson, J.D., 1985, Selected hydrologic data for the Powell River basin in Wise County, Virginia: U.S. Geological Survey Open-File Report 85-186, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85186.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0186/report-thumb.jpg"},{"id":43292,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0186/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8ac2","contributors":{"authors":[{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":169728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10944,"text":"ofr84611 - 1985 - Hydrology of the Floridan Aquifer system in west-central Florida","interactions":[{"subject":{"id":10944,"text":"ofr84611 - 1985 - Hydrology of the Floridan Aquifer system in west-central Florida","indexId":"ofr84611","publicationYear":"1985","noYear":false,"title":"Hydrology of the Floridan Aquifer system in west-central Florida"},"predicate":"SUPERSEDED_BY","object":{"id":39655,"text":"pp1403F - 1985 - Hydrology of the Floridan aquifer system in west-central Florida","indexId":"pp1403F","publicationYear":"1985","noYear":false,"chapter":"F","title":"Hydrology of the Floridan aquifer system in west-central Florida"},"id":1}],"supersededBy":{"id":39655,"text":"pp1403F - 1985 - Hydrology of the Floridan aquifer system in west-central Florida","indexId":"pp1403F","publicationYear":"1985","noYear":false,"title":"Hydrology of the Floridan aquifer system in west-central Florida"},"lastModifiedDate":"2020-02-03T12:27:19","indexId":"ofr84611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-611","title":"Hydrology of the Floridan Aquifer system in west-central Florida","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84611","usgsCitation":"Ryder, P., 1985, Hydrology of the Floridan Aquifer system in west-central Florida: U.S. Geological Survey Open-File Report 84-611, vii, 92 p. , https://doi.org/10.3133/ofr84611.","productDescription":"vii, 92 p. ","costCenters":[],"links":[{"id":371936,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0611/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0611/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.000000,25.000000 ], [ -84.000000,30.000000 ], [ -81.000000,30.000000 ], [ -81.000000,25.000000 ], [ -84.000000,25.000000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601e86","contributors":{"authors":[{"text":"Ryder, P.D.","contributorId":104021,"corporation":false,"usgs":true,"family":"Ryder","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":162247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4080,"text":"cir893 - 1985 - Water Resources Division in the 1980's : a summary of activities and programs of the U.S. Geological Survey's Water Resources Division","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"cir893","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"893","title":"Water Resources Division in the 1980's : a summary of activities and programs of the U.S. Geological Survey's Water Resources Division","docAbstract":"The Water Resources Division of the U.S. Geological Survey has the principal responsibility within the Federal government for providing hydrologic information and appraising the Nation's water resounds. The Geological Survey is unique among government organizations because it has neither regulatory nor developmental authority--its sole product is information that is made available equally to all interested parties. \r\n\r\nThis report describes the Water Resources Division's mission, organization, source of funds, and major programs. Three types of programs are described: long-term programs, which include the Federal-State cooperative program, coordination of Federal water-data acquisition, assistance to other Federal agencies, the national research program, the national water-data exchange, the water resources scientific information center, the national water-use information program, hydrologic-data collection, and international hydrology activities; topical programs, which include hazardous waste hydrology, coal and oil-shale hydrology, regional aquifer system analyses, acid rain, volcano hazards, and national water-resources conditions; and technical-assistance programs. Emphasis is on programs that will contribute to identifying, mitigating, or solving nationwide water-resources problems in the 1980's. A discussion of how the data and information axe disseminated and a selected list of references complete the report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir893","usgsCitation":"Chase, E.B., Moore, J.E., and Rickert, D.A., 1985, Water Resources Division in the 1980's : a summary of activities and programs of the U.S. Geological Survey's Water Resources Division (Revised edition 1985): U.S. Geological Survey Circular 893, iii, 78 p. :ill. (1 col.) ;28 cm., https://doi.org/10.3133/cir893.","productDescription":"iii, 78 p. :ill. (1 col.) ;28 cm.","costCenters":[],"links":[{"id":124477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0893/report-thumb.jpg"},{"id":31179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0893/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revised edition 1985","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4987e4b07f02db5af288","contributors":{"authors":[{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":148146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":148147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rickert, David A.","contributorId":80247,"corporation":false,"usgs":true,"family":"Rickert","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148148,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13972,"text":"ofr85160 - 1985 - Hydrologic data for Leviathan Mine and vicinity, Alpine County, California, 1981-83","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr85160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-160","title":"Hydrologic data for Leviathan Mine and vicinity, Alpine County, California, 1981-83","docAbstract":"The U.S. Geological Survey collected basic hydrologic and water-quality data during 1981-83 to facilitate the geohydrologic evaluation of the Leviathan Mine area and the design of a pollution-abatement project. Surface-water field data included one or more measurements of pH, water temperature, and specific conductance at 45 sites in and adjacent to the mine area. At nine of these sites, daily data on discharge, specific conductance, and water temperature were collected during parts of 1981-82 by using electronic monitor-recorder systems. Ground-water field data included one or more of the water-quality measurements listed above at 71 piezometers in the mine area. Borehole geophysical data included neutron-moisture, neutron-porosity, gamma-gamma density, natural gamma, and temperature logs at three sites. Mineralogic and hydrologic data were obtained for cores taken from nine test holes. One or more surface-water samples from 26 sites were analyzed for major cations, major anions, and a wide range of minor inorganic constituents. Single ground-water samples from 36 piezometers were analyzed for the same array of major and minor constituents. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85160","usgsCitation":"Hammermeister, D., and Walmsley, S., 1985, Hydrologic data for Leviathan Mine and vicinity, Alpine County, California, 1981-83: U.S. Geological Survey Open-File Report 85-160, ix, 161 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85160.","productDescription":"ix, 161 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0160/report-thumb.jpg"},{"id":42622,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed75","contributors":{"authors":[{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":168721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walmsley, S.J.","contributorId":89909,"corporation":false,"usgs":true,"family":"Walmsley","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":168722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12106,"text":"ofr85407 - 1985 - Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1982","interactions":[],"lastModifiedDate":"2017-06-14T11:19:27","indexId":"ofr85407","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-407","title":"Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1982","docAbstract":"

Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas-Fort Worth and San Antonio areas.

\n

The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:

\n
    \n
  1. To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volumes.
    2. \n
  2. To determine the effect of urban development on flood peaks and volumes.
    3. \n
  3. To ascertain the variation in water quality for different flow conditions and different seasons.
    4. \n
\n

This report, the nineteenth in a series of reports to be published annually, is primarily applicable to objective 2. The report presents hydrologic data collected in the Houston urban area for the 1982 water year (October 1, 1981 to September 30, 1982).

\n

A report by Johnson and Sayre (1973) utilized records collected from 1965 to 1969 to study the effects of urbanization on floods in the Houston area. The report also summarizes various basin parameters. A report by Waddell, Massey, and Jennings (1979) presents data on runoff from the Houston area and computed concentrations and loads of selected water-quality constituents discharged to Galveston Bay. The study utilized a variation of the \"STORM\" model developed by the Hydrologic Engineering Center of the U.S. Army Corps of Engineers. A report prepared by Li scum and Massey (1980) presents a technique for estimating the magnitude and frequency of floods in the Houston area from drainage areas, bank-full conveyance, and percentage of urban development.

\n

A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in \"U.S. Geological Survey, Water-resources data for Texas, water year 1982, volume 2.\"

\n

To facilitate the publication and distribution of this report some material has been included that does not conform to the formal publications standards of the U.S. Geological Survey.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85407","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., Bruchmiller, J., Hutchinson, J., and Paul, E., 1985, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1982: U.S. Geological Survey Open-File Report 85-407, viii, 252 p., https://doi.org/10.3133/ofr85407.","productDescription":"viii, 252 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0407/report-thumb.jpg"},{"id":40138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0407/report.pdf","text":"Report","size":"5.13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.36819458007811,\n 30.039377605001338\n ],\n [\n -95.42587280273438,\n 30.039377605001338\n ],\n [\n -95.49179077148438,\n 30.03462216002981\n ],\n [\n -95.56320190429686,\n 30.0262995822237\n ],\n [\n -95.62774658203125,\n 30.001327656702326\n ],\n [\n -95.73348999023438,\n 29.969211659636663\n ],\n [\n -95.83648681640624,\n 29.92756435779241\n ],\n [\n -95.87493896484374,\n 29.888280933159265\n ],\n [\n -95.86257934570312,\n 29.80251790576445\n ],\n [\n -95.86944580078125,\n 29.75364773335698\n ],\n [\n -95.8447265625,\n 29.69640358280457\n ],\n [\n -95.79940795898438,\n 29.672542219068987\n ],\n [\n -95.69641113281249,\n 29.630771207229\n ],\n [\n -95.63186645507812,\n 29.60092416008231\n ],\n [\n -95.51513671875,\n 29.57106827738255\n ],\n [\n -95.40252685546875,\n 29.511330027309146\n ],\n [\n -95.28030395507812,\n 29.485034019181064\n ],\n [\n -95.17730712890625,\n 29.482643134466617\n ],\n [\n -95.086669921875,\n 29.499378142743375\n ],\n [\n -94.99740600585938,\n 29.532839863453397\n ],\n [\n -94.95483398437499,\n 29.551955878093022\n ],\n [\n -94.9493408203125,\n 29.604506272365295\n ],\n [\n -94.96719360351562,\n 29.653449050468925\n ],\n [\n -94.9822998046875,\n 29.680894340704334\n ],\n [\n -95.01800537109374,\n 29.71787396585316\n ],\n [\n -95.0372314453125,\n 29.744109309616487\n ],\n [\n -95.06881713867188,\n 29.76556948666697\n ],\n [\n -95.06744384765625,\n 29.797751134173065\n ],\n [\n -95.07705688476562,\n 29.837070205715218\n ],\n [\n -95.10314941406249,\n 29.871610558533725\n ],\n [\n -95.1361083984375,\n 29.925183985247404\n ],\n [\n -95.15396118164062,\n 29.972780616663897\n ],\n [\n -95.14572143554688,\n 29.997759725578906\n ],\n [\n -95.185546875,\n 30.01916538794235\n ],\n [\n -95.2294921875,\n 30.02511058549258\n ],\n [\n -95.2789306640625,\n 30.029866486852946\n ],\n [\n -95.33660888671875,\n 30.032244351965684\n ],\n [\n -95.36819458007811,\n 30.039377605001338\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c551","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":165096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruchmiller, J.P.","contributorId":102490,"corporation":false,"usgs":true,"family":"Bruchmiller","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":165097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hutchinson, J.S.","contributorId":14827,"corporation":false,"usgs":true,"family":"Hutchinson","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":165094,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paul, E.M.","contributorId":65089,"corporation":false,"usgs":true,"family":"Paul","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":165095,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":13391,"text":"ofr85338 - 1985 - Hydrologic and geochemical data for the Big Brown lignite mine area, Freestone County, Texas","interactions":[],"lastModifiedDate":"2016-08-12T13:41:15","indexId":"ofr85338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-338","title":"Hydrologic and geochemical data for the Big Brown lignite mine area, Freestone County, Texas","docAbstract":"

Lignite mining in east and east-central Texas is increasing in response to increased energy needs throughout the State. Associated with the increase in mining activities is a greater need to know the effects of mining activities on the water quantity and quality of near-surface aquifers. The near-surface lignite beds mined at the Big Brown Lignite Mine are from the Calvert Bluff Formation of the Wilcox Group of Eocene age, which is a minor aquifer generally having water suitable for all uses, in eastern Freestone County, Texas. One of the potential hydro!ogic effects of surface-coal mining is a change in the quality of ground water associated with replacement of aquifer materials by mine spoils. The purpose of this report is to compile and categorize geologic, mineralogic, geochemical, and hydrologic data for the Big Brown Lignite Mine and surrounding area in east-central Texas. Included are results of pasteextract analyses, constituent concentrations in water from batch-mixing experiments, sulfur analyses, and minerals or mineral groups detected by X-ray diffraction in 12 spoil material samples collected from 3 locations at the mine site. Also, common-constituent and trace-constituent concentrations in water from eight selected wells, located updip and downdip from the mine, are presented. Dissolved-solids concentrations in water from batch-mixing experiments vary from 12 to 908 milligrams per liter. Water from selected wells contain dissolved-solids concentrations ranging from 75 to 510 milligrams per liter.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85338","usgsCitation":"Dorsey, M.E., 1985, Hydrologic and geochemical data for the Big Brown lignite mine area, Freestone County, Texas: U.S. Geological Survey Open-File Report 85-338, Report: iv, 17 p.; 2 Plates: 23.17 x 17.62 inches and 23.92 x 17.92 inches, https://doi.org/10.3133/ofr85338.","productDescription":"Report: iv, 17 p.; 2 Plates: 23.17 x 17.62 inches and 23.92 x 17.92 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":41818,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0338/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41819,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0338/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41820,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0338/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0338/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62757e","contributors":{"authors":[{"text":"Dorsey, Michael E.","contributorId":101739,"corporation":false,"usgs":true,"family":"Dorsey","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":167734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4160,"text":"cir904C - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","interactions":[{"subject":{"id":18097,"text":"ofr83756 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","indexId":"ofr83756","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation"},"predicate":"SUPERSEDED_BY","object":{"id":4160,"text":"cir904C - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","indexId":"cir904C","publicationYear":"1985","noYear":false,"chapter":"C","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation"},"id":1}],"lastModifiedDate":"2019-11-07T12:10:42","indexId":"cir904C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"904","chapter":"C","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation","docAbstract":"

This report describes the first phase in evaluating the geology and hydrology of the Basin and Range Province for potential suitability of geohydrologic environments for isolation of high-level radioactive waste. The evaluation of the Province applies the guidelines, discussed in Part I (Bedinger, Sargent, and Reed, 1983) of this report to the geologic and hydrologic information compiled for the Province in Part II (Sargent and Bedinger, 1983).

The geologic and hydrologic factors considered in the Province evaluation include distribution of potential host rocks, tectonic conditions and data on ground-water hydrology. Potential host media considered include argillaceous rocks, tuff, basaltic rocks, granitic rocks, evaporites, and the unsaturated zone. The tectonic factors considered are Quaternary faults, late Cenozoic volcanics, seismic activity, heat flow, and late Cenozoic rates of vertical uplift. Hydrologic conditions considered include length of flow path from potential host rocks to discharge areas, interbasin and geothermal flow systems and thick unsaturated sections as potential host media.

The Basin and Range Province was divided into 12 subprovinces; each subprovince is evaluated separately and prospective areas for further study are identified. About onehalf of the Province appears to have combinations of potential host rocks, tectonic conditions, and ground-water hydrology that merit consideration for further study.

The prospective areas for further study in each subprovince are summarized in a brief list of the potentially favorable factors and the issues of concern. Data compiled for the entire Province do not permit a complete evaluation of the favorability for high-level waste isolation. The evaluations here are intended to identify broad regions that contain potential geohydrologic environments containing multiple natural barriers to radionuclide migration.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904C","usgsCitation":"Bedinger, M.S., Sargent, K., and Brady, B., 1985, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part III, Geologic and hydrologic evaluation: U.S. Geological Survey Circular 904, iv, 27 p., https://doi.org/10.3133/cir904C.","productDescription":"iv, 27 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335937,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904B","text":"Circular 904-B","linkHelpText":"Part II, Geologic and hydrologic characterization"},{"id":335936,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904A","text":"Circular 904-A","linkHelpText":"Part I, Introduction and guidelines"},{"id":31270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0904c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0904c/report-thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Oregon, Texas","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 -115.6640625,\n 32.65787573695528\n ],\n [\n -114.6533203125,\n 32.80574473290688\n ],\n [\n -114.6533203125,\n 32.509761735919426\n ],\n [\n -111.09374999999999,\n 31.353636941500987\n ],\n [\n -108.5009765625,\n 31.353636941500987\n ],\n [\n -108.28125,\n 31.952162238024975\n ],\n [\n -106.3916015625,\n 31.952162238024975\n ],\n [\n -104.8974609375,\n 30.751277776257812\n ],\n [\n -104.6337890625,\n 30.600093873550072\n ],\n [\n -104.5458984375,\n 30.183121842195515\n ],\n [\n -103.3154296875,\n 29.11377539511439\n ],\n [\n -102.7880859375,\n 29.99300228455108\n ],\n [\n -105.9521484375,\n 34.52466147177172\n ],\n [\n -106.8310546875,\n 34.95799531086792\n ],\n [\n -107.6220703125,\n 34.88593094075317\n ],\n [\n -108.544921875,\n 33.76088200086917\n ],\n [\n -111.57714843749999,\n 34.88593094075317\n ],\n [\n -113.0712890625,\n 35.7286770448517\n ],\n [\n -114.01611328125,\n 35.96022296929667\n ],\n [\n -111.33544921874999,\n 40.763901280945866\n ],\n [\n -111.005859375,\n 42.69858589169842\n ],\n [\n -112.67578124999999,\n 43.16512263158296\n ],\n [\n -116.76269531249999,\n 41.64007838467894\n ],\n [\n -118.30078125,\n 42.52069952914966\n ],\n [\n -119.50927734374999,\n 43.61221676817573\n ],\n [\n -120.62988281249999,\n 43.5326204268101\n ],\n [\n -121.1572265625,\n 43.26120612479979\n ],\n [\n -121.75048828124999,\n 42.53689200787315\n ],\n [\n -121.83837890625,\n 41.902277040963696\n ],\n [\n -121.728515625,\n 41.27780646738183\n ],\n [\n -120.36621093749999,\n 40.83043687764923\n ],\n [\n -120.30029296875,\n 39.30029918615029\n ],\n [\n -120.30029296875,\n 38.75408327579141\n ],\n [\n -116.93847656250001,\n 36.29741818650811\n ],\n [\n -118.19091796875,\n 35.02999636902566\n ],\n [\n -116.08154296875001,\n 34.27083595165\n ],\n [\n -115.6640625,\n 32.65787573695528\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"This is Part III of a series of reports being prepared by the U.S. Geological Survey in consultation with States in the Basin and Range Province.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8229","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":148319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":148318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brady, Bruce T.","contributorId":8059,"corporation":false,"usgs":true,"family":"Brady","given":"Bruce T.","affiliations":[],"preferred":false,"id":148317,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13219,"text":"ofr85645 - 1985 - Annual water-resources review, White Sands Missile Range, New Mexico, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr85645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-645","title":"Annual water-resources review, White Sands Missile Range, New Mexico, 1984","docAbstract":"Hydrologic data were collected at White Sands Missile Range in 1984. The total groundwater withdrawal in 1984 was 685,275,000 gallons. The Post Headquarters well field produced 650,821,000 gallons in 1984. Six new wells were drilled at White Sands Missile Range in 1984. Nineteen water samples were collected for major chemical-constituent, trace-element, or radiochemical analysis in 1984. Depth-to-water measurements in the Post Headquarters supply wells showed seasonal fluctuations as well as continued long-term declines. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85645","usgsCitation":"Cruz, R.R., 1985, Annual water-resources review, White Sands Missile Range, New Mexico, 1984: U.S. Geological Survey Open-File Report 85-645, iv, 25 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85645.","productDescription":"iv, 25 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0645/report-thumb.jpg"},{"id":41600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b743","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":167424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14827,"text":"ofr8584 - 1985 - Texas stream-gaging program: an analysis of data uses and funding","interactions":[],"lastModifiedDate":"2016-08-12T13:11:03","indexId":"ofr8584","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-84","title":"Texas stream-gaging program: an analysis of data uses and funding","docAbstract":"

This report presents an analysis of data uses and funding for the stream-gaging program operated by the U.S. Geological Survey in Texas. Presently (1984), 391 continuous surface water stations are operated in Texas. Selected hydrologic data, data uses, and funding sources are presented for each of the 391 stations.

\n

This study is a part of a larger project to determine the cost-effectiveness of the stream gaging program in Texas. All stations have sufficient uses to justify their continued operation.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa353","contributors":{"authors":[{"text":"Massey, Bernard C.","contributorId":173558,"corporation":false,"usgs":false,"family":"Massey","given":"Bernard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":170084,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10026,"text":"ofr85170 - 1985 - Hydrogeologic data related to the potential for stock-water development on federally owned rangeland near Dillon, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr85170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-170","title":"Hydrogeologic data related to the potential for stock-water development on federally owned rangeland near Dillon, Montana","docAbstract":"Existing hydrogeologic data and information were synthesized for 20 sites on federally owned rangeland near Dillon, Montana. The purpose was to assist the U.S. Bureau of Land Management in evaluating the potential for developing additional stock-water supplies. Hydrologic and geologic conditions at most of the sites were verified by onsite inspection during the summer of 1984. Each site is described in terms of location, altitude of land surface, inferred aquifer(s), estimated depth to water, estimated drilling depth, estimated yield, estimated dissolved-solids concentration, hydrogeologic setting, and development. A plate shows the location of wells and springs, dissolved-solids concentrations and chemical-constituent diagrams for water samples, ownership status for selected rangeland areas near Dillon. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85170","usgsCitation":"Levings, J.F., 1985, Hydrogeologic data related to the potential for stock-water development on federally owned rangeland near Dillon, Montana: U.S. Geological Survey Open-File Report 85-170, iii, 25 p. :map ;28 cm., https://doi.org/10.3133/ofr85170.","productDescription":"iii, 25 p. :map ;28 cm.","costCenters":[],"links":[{"id":143880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0170/report-thumb.jpg"},{"id":37866,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0170/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0170/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628764","contributors":{"authors":[{"text":"Levings, J. F.","contributorId":94675,"corporation":false,"usgs":true,"family":"Levings","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16080,"text":"ofr85189 - 1985 - Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T14:09:09","indexId":"ofr85189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-189","title":"Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina","docAbstract":"This study presents data collected during a study of the effects on the water table aquifer from wastewater application at rates of up to 5 inches per week on a wastewater spray disposal site on Hilton Head Island, South Carolina. The study was conducted from April 1982 through December 1983. The disposal site covers approximately 14 acres. Water level and water quality data from organic, inorganic, and nutrient analyses from the water table aquifer to a depth of 30 ft and similar water quality data from the wastewater treatment plant are included. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85189","usgsCitation":"Speiran, G., and Belval, D., 1985, Selected hydrologic data from a wastewater spray disposal site on Hilton Head Island, South Carolina: U.S. Geological Survey Open-File Report 85-189, v, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85189.","productDescription":"v, 34 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":150331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0189/report-thumb.jpg"},{"id":45012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0189/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","otherGeospatial":"Hilton Head Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.94932556152344,\n 32.01273389791075\n ],\n [\n -80.94932556152344,\n 32.34574191355548\n ],\n [\n -80.57441711425781,\n 32.34574191355548\n ],\n [\n -80.57441711425781,\n 32.01273389791075\n ],\n [\n -80.94932556152344,\n 32.01273389791075\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8977","contributors":{"authors":[{"text":"Speiran, G. K.","contributorId":83534,"corporation":false,"usgs":true,"family":"Speiran","given":"G. K.","affiliations":[],"preferred":false,"id":172204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belval, D.L.","contributorId":52186,"corporation":false,"usgs":true,"family":"Belval","given":"D.L.","affiliations":[],"preferred":false,"id":172203,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8098,"text":"ofr84618 - 1985 - Hydrologic reconnaissance of the Chilkat River basin, southeast Alaska, with special reference to the bald eagle critical habitat at the Tsirku River alluvial fan","interactions":[],"lastModifiedDate":"2023-07-25T20:37:41.810256","indexId":"ofr84618","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-618","title":"Hydrologic reconnaissance of the Chilkat River basin, southeast Alaska, with special reference to the bald eagle critical habitat at the Tsirku River alluvial fan","docAbstract":"

The Chilkat River basin in southeast Alaska is characterized by rugged, highly dissected mountains with steep-gradient streams, braided rivers in broad alluvium-filled valleys, and numerous glaciers. A wide seasonal range in temperature and strong orographic effects cause variations in the amount and distribution of precipitation, and thus in the resulting runoff and streamflow. Streamflow is lowest in winter, when precipitation at higher altitudes is stored as snow, and greatest in summer, when melting snow and glacier ice augment flow. Ground-water seeps and springs flowing from alluvial fans contribute to streamflow year round.

A ground-water discharge zone of particular interest is that along the toe of the Tsirku River alluvial fan, 20 miles north of Haines. During winter, the relatively warm (4 to 6 degrees Celsius) ground water maintains open leads in a reach of the Chilkat River downstream from the fan. This ice-free reach provides favorable spawning habitat for a late run of chum and coho (silver) salmon, which in turn attracts the world's largest concentration of bald eagles (more than 3,000 birds). The principal source of recharge to the ground-water system in the fan is loss of water through the beds of the many distributary channels across the fan surface.

Calculation of a water budget for the system for the period October 1982 through May 1983 indicates that ground-water discharge at the toe of the fan averages 640 cubic feet per second.

Surface and ground waters are chemically similar, calcium bicarbonate types. All stream samples had dissolved-solids concentrations of less than 115 milligrams per liter; values for ground water were slightly greater. During high summer flows, the suspended-sediment concentrations of the glacially fed Chilkat, Tsirku, and Klehini Rivers ranged from 361 to 1,530 milligrams per liter (6,360 to 22,300 tons per day).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84618","collaboration":"Prepared in cooperation with the Alaska Department of Natural Resources Division of Geological and Geophysical Surveys","usgsCitation":"Bugliosi, E.F., 1985, Hydrologic reconnaissance of the Chilkat River basin, southeast Alaska, with special reference to the bald eagle critical habitat at the Tsirku River alluvial fan: U.S. Geological Survey Open-File Report 84-618, v, 46 p., https://doi.org/10.3133/ofr84618.","productDescription":"v, 46 p.","costCenters":[],"links":[{"id":419321,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0618/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141343,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0618/report-thumb.jpg"},{"id":388912,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13474.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Chilkat River basin, Tsirku River alluvial fan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -136.5,\n 59.8610\n ],\n [\n -137.85,\n 59.8610\n ],\n [\n -137.85,\n 59.1420\n ],\n [\n -136.5,\n 59.1420\n ],\n [\n -136.5,\n 59.8610\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606450","contributors":{"authors":[{"text":"Bugliosi, Edward F. ebuglios@usgs.gov","contributorId":1083,"corporation":false,"usgs":true,"family":"Bugliosi","given":"Edward","email":"ebuglios@usgs.gov","middleInitial":"F.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3488,"text":"cir904B - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","interactions":[{"subject":{"id":10982,"text":"ofr83699 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","indexId":"ofr83699","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization"},"predicate":"SUPERSEDED_BY","object":{"id":3488,"text":"cir904B - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","indexId":"cir904B","publicationYear":"1985","noYear":false,"chapter":"B","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization"},"id":1}],"lastModifiedDate":"2019-11-07T12:09:52","indexId":"cir904B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"904","chapter":"B","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","docAbstract":"

The geology and hydrology of the Basin and Range Province of the western conterminous United States are characterized in a series of data sets depicted in maps compiled for evaluation of prospective areas for further study of geohydrologic environments for isolation of high-level radioactive waste. The data sets include: (1) Average precipitation and evaporation; (2) surface distribution of selected rock types; (3) tectonic conditions; and (4) surface- and ground -water hydrology and Pleistocene lakes and marshes.

Rocks mapped for consideration as potential host media for the isolation of high-level radioactive waste are widespread and include argillaceous rocks, granitic rocks, tuffaceous rocks, mafic extrusive rocks, evaporites, and laharic breccias. The unsaturated zone, where probably as thick as 150 meters (500 feet), was mapped for consideration as an environment for isolation of high-level waste. Unsaturated rocks of various lithologic types are widespread in the Province.

Tectonic stability in the Quaternary Period is considered the key to assessing the probability of future tectonism with regard to high-level radioactive waste disposal. Tectonic conditions are characterized on the basis of the seismic record, heat-flow measurements, the occurrence of Quaternary faults, vertical crustal movement, and volcanic features. Tectonic activity, as indicated by seismicity, is greatest in areas bordering the western margin of the Province in Nevada and southern California, the eastern margin of the Province bordering the Wasatch Mountains in Utah and in parts of the Rio Grande valley. Late Cenozoic volcanic activity is widespread, being greatest bordering the Sierra Nevada in California and Oregon, and bordering the Wasatch Mountains in southern Utah and Idaho.

he arid to semiarid climate of the Province results in few perennial streams and lakes. A large part of the surface drainage is interior and the many closed basins commonly are occupied by playas or dry lake beds. The Province is divided into ground-water flow units defined on the basis of ground-water divides, ground-water flow lines, and surface streams that receive ground-water discharge.

Ground water contains less than 500 milligrams per liter of dissolved solids throughout most of the Province. Ground water is more mineralized in areas underlain by evaporitic rocks, overlain by playas, and near saline lakes. Ground water is of the calcium, magnesium, or sodium bicarbonate type in the areas where dissolved-solids concentrations are less than 500 milligrams per liter, and of the calcium, magnesium, or sodium sulfate or chloride type where dissolved-solids concentrations are greater than 500 milligrams per liter.

Geologic and hydrologic evidence is found for about 100 lakes and marshes that existed during the Pleistocene Epoch. The possibility of a recurrence of pluvial conditions, such as existed in the Pleistocene, is of concern in repository siting because of possible changes in hydrologic conditions. The Pleistocene lakes and marshes provide clues to the hydrology during pluvial climates.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904B","usgsCitation":"Sargent, K., and Bedinger, M.S., 1985, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization: U.S. Geological Survey Circular 904, iv, 30 p., https://doi.org/10.3133/cir904B.","productDescription":"iv, 30 p.","numberOfPages":"38","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335935,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904C","text":"Circular 904-C","linkHelpText":"Part III, Geologic and hydrologic evaluation"},{"id":335934,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904A","text":"Circular 904-A","linkHelpText":"Part I, Introduction and guidelines"},{"id":30497,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0904b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0904b/report-thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Oregon, Texas","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 -115.6640625,\n 32.65787573695528\n ],\n [\n -114.6533203125,\n 32.80574473290688\n ],\n [\n -114.6533203125,\n 32.509761735919426\n ],\n [\n -111.09374999999999,\n 31.353636941500987\n ],\n [\n -108.5009765625,\n 31.353636941500987\n ],\n [\n -108.28125,\n 31.952162238024975\n ],\n [\n -106.3916015625,\n 31.952162238024975\n ],\n [\n -104.8974609375,\n 30.751277776257812\n ],\n [\n -104.6337890625,\n 30.600093873550072\n ],\n [\n -104.5458984375,\n 30.183121842195515\n ],\n [\n -103.3154296875,\n 29.11377539511439\n ],\n [\n -102.7880859375,\n 29.99300228455108\n ],\n [\n -105.9521484375,\n 34.52466147177172\n ],\n [\n -106.8310546875,\n 34.95799531086792\n ],\n [\n -107.6220703125,\n 34.88593094075317\n ],\n [\n -108.544921875,\n 33.76088200086917\n ],\n [\n -111.57714843749999,\n 34.88593094075317\n ],\n [\n -113.0712890625,\n 35.7286770448517\n ],\n [\n -114.01611328125,\n 35.96022296929667\n ],\n [\n -111.33544921874999,\n 40.763901280945866\n ],\n [\n -111.005859375,\n 42.69858589169842\n ],\n [\n -112.67578124999999,\n 43.16512263158296\n ],\n [\n -116.76269531249999,\n 41.64007838467894\n ],\n [\n -118.30078125,\n 42.52069952914966\n ],\n [\n -119.50927734374999,\n 43.61221676817573\n ],\n [\n -120.62988281249999,\n 43.5326204268101\n ],\n [\n -121.1572265625,\n 43.26120612479979\n ],\n [\n -121.75048828124999,\n 42.53689200787315\n ],\n [\n -121.83837890625,\n 41.902277040963696\n ],\n [\n -121.728515625,\n 41.27780646738183\n ],\n [\n -120.36621093749999,\n 40.83043687764923\n ],\n [\n -120.30029296875,\n 39.30029918615029\n ],\n [\n -120.30029296875,\n 38.75408327579141\n ],\n [\n -116.93847656250001,\n 36.29741818650811\n ],\n [\n -118.19091796875,\n 35.02999636902566\n ],\n [\n -116.08154296875001,\n 34.27083595165\n ],\n [\n -115.6640625,\n 32.65787573695528\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"This is Part II of a series of reports being prepared by the U.S. Geological Survey in consultation with States in the Basin and Range Province.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a821e","contributors":{"authors":[{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":147018,"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":147019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12374,"text":"ofr85346 - 1985 - Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84","interactions":[],"lastModifiedDate":"2016-08-12T13:45:36","indexId":"ofr85346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-346","title":"Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84","docAbstract":"

The U.S. Geological Survey (USGS) was established by an act of Congress on March 3, 1879, to provide a permanent Federal agency to conduct the systematic and scientific classification of the public lands, and examination of the geological structure, mineral resources, and products of national domain. An integral part of that original mission includes publishing and disseminating the earth-science information needed to understand, to plan the use of, and to manage the Nation's energy, land, mineral, and water resources.

\n

Since 1879, the research and fact-finding role of the USGS has grown and been modified to meet the changing needs of the Nation it serves. As part of that evolution, the USGS has become the Federal Government's largest earth-science research agency, the Nation's largest civilian mapmaking agency, the primary source of data on the Nation's surface- and ground-water resources, and the employer of the largest number of professional earth scientists. Today's programs serve a diversity of needs and users. Programs include:

\n\n

Along with its continuing commitment to meet the growing and changing earthscience information needs of the Nation, the USGS remains dedicated to its original mission to collect, analyze, interpret, publish, and disseminate information about the natural resources of the Nation providing \"earth science in the public service.\"

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85346","usgsCitation":"Grozier, R., and Land, L.F., 1985, Water-resources activities of the U.S. Geological Survey in Texas; fiscal years 1982-84: U.S. Geological Survey Open-File Report 85-346, iv, 60 p., https://doi.org/10.3133/ofr85346.","productDescription":"iv, 60 p.","numberOfPages":"64","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":145861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0346/report-thumb.jpg"},{"id":40611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a1e","contributors":{"authors":[{"text":"Grozier, R.U.","contributorId":105704,"corporation":false,"usgs":true,"family":"Grozier","given":"R.U.","affiliations":[],"preferred":false,"id":166024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166023,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12372,"text":"ofr85422 - 1985 - Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr85422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-422","title":"Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984","docAbstract":"Project descriptions, water-resources summaries, and lists of hydrologic-data stations are presented to show the status of the U.S. Geological survey water-resources studies in South Dakota. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85422","usgsCitation":"LeRoux, E.F., and Decker, E., 1985, Water-resources activities of the U.S. Geological Survey in South Dakota; fiscal year 1984: U.S. Geological Survey Open-File Report 85-422, iii, 62 p. :ill. ;28 cm., https://doi.org/10.3133/ofr85422.","productDescription":"iii, 62 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":145859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0422/report-thumb.jpg"},{"id":40608,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0422/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f8d","contributors":{"authors":[{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":166020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Decker, E.M.","contributorId":43345,"corporation":false,"usgs":true,"family":"Decker","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":166021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13855,"text":"ofr85172 - 1985 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1983","interactions":[],"lastModifiedDate":"2017-06-14T10:54:41","indexId":"ofr85172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-172","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1983","docAbstract":"

Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas, Fort Worth, and San Antonio areas.

\n

The Geological Survey, in cooperation with the Texas Department of Water Reources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Balcones Fault Zone.

\n

The objectives of the Austin urban hydrology study are as follows:

\n
    \n
  1. To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volume.
    2. \n
  2. To determine the effect of urban development on flood peaks and volume.
    3. \n
  3. To determine the variations in water quality during different seasons and flow conditions in representative watersheds under various types of urban development.
    4. \n
  4. To quantitatively appraise the ground-water resources along the Balcones Fault Zone, the effect of urbanization on the quality and quantity of recharge and discharge, and the extent of contamination in the Edwards aquifer that is in hydrologic circulation with Barton Springs.
    5. \n
\n

This report presents the basic hydrologic data collected in the Austin urban area for the 1983 water year (Oct. 1, 1982 to Sept. 30, 1983).

\n

Additional explanations of terms related to streamflow, water quality, and other hydrologic data used in this report are defined in the U.S. Geological Survey annual report Water Resources Data for Texas, TX-83-3, 1983.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85172","collaboration":"Prepared in cooperation with the City of Austin and the Texas Department of Water Resources","usgsCitation":"Gordon, J., Pate, D., and Dorsey, M., 1985, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1983: U.S. Geological Survey Open-File Report 85-172, 154 p., https://doi.org/10.3133/ofr85172.","productDescription":"154 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":144386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0172/report-thumb.jpg"},{"id":42460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0172/report.pdf","text":"Report","size":"2.70 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.09280395507812,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 29.991812888666043\n ],\n [\n -97.38006591796874,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 30.615459280672667\n ],\n [\n -98.09280395507812,\n 29.991812888666043\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608199","contributors":{"authors":[{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":168510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pate, D.L.","contributorId":87145,"corporation":false,"usgs":true,"family":"Pate","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":168512,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":168511,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":15898,"text":"ofr85177 - 1985 - Index of ground-water quality data for Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:11","indexId":"ofr85177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-177","title":"Index of ground-water quality data for Florida","docAbstract":"The Master Water Data Index of the U.S. Geological Survey contains records and information for 13,925 ground-water quality collection sites in Florida as follows: 2,180 active and 11,559 inactive well sites, and 39 active and 147 inactive spring sites. Ground-water quality data have been and are being collected at more sites in Florida than are other types of ground- and surface-water hydrologic data. Information available from the Master Water Data Index includes location (county, hydrologic unit, and latitude-longitude); reporting agency; agency identifying number; period and frequency of record; types of data (parameter sampled); and for wells, the principal aquifer sampled and well depth. This information may be retrieved, upon request, in a variety of formats. This report contains an index of the information available, not the actual water-quality data itself. The actual data may be obtained from the reporting agency that collected and stored the data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85177","usgsCitation":"Seaber, P., and Williams, O., 1985, Index of ground-water quality data for Florida: U.S. Geological Survey Open-File Report 85-177, iv, 476 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85177.","productDescription":"iv, 476 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0177/report-thumb.jpg"},{"id":44878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4286","contributors":{"authors":[{"text":"Seaber, P. R.","contributorId":53802,"corporation":false,"usgs":true,"family":"Seaber","given":"P. R.","affiliations":[],"preferred":false,"id":171900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, O.O.","contributorId":46095,"corporation":false,"usgs":true,"family":"Williams","given":"O.O.","email":"","affiliations":[],"preferred":false,"id":171899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10052,"text":"ofr85163 - 1985 - Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1981","interactions":[],"lastModifiedDate":"2017-06-14T11:17:49","indexId":"ofr85163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-163","title":"Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1981","docAbstract":"

Hydro! oqic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas-Fort Worth and San Antonio areas.

\n

The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:

\n
    \n
  1. To determine, on the basis of historical data and hydro!ogic analyses, the magnitude and frequency of flood peaks and flood volumes.
    2. \n
  2. To determine the effect of urban development on flood peaks and volumes.
    3. \n
  3. To ascertain the variation in water quality for different flow conditions and different seasons.
    4. \n
\n

This report, the eighteenth in a series of reports to be published annually, is primarily applicable to objective 2. The report presents hydro!ogic data collected in the Houston urban area for the 1981 water year (October 1, 1980 to September 30, 1981).

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr85163","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., 1985, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1981: U.S. Geological Survey Open-File Report 85-163, viii, 296 p., https://doi.org/10.3133/ofr85163.","productDescription":"viii, 296 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":37901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0163/report.pdf","text":"Report","size":"5.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":145610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0163/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.36819458007811,\n 30.039377605001338\n ],\n [\n -95.42587280273438,\n 30.039377605001338\n ],\n [\n -95.49179077148438,\n 30.03462216002981\n ],\n [\n -95.56320190429686,\n 30.0262995822237\n ],\n [\n -95.62774658203125,\n 30.001327656702326\n ],\n [\n -95.73348999023438,\n 29.969211659636663\n ],\n [\n -95.83648681640624,\n 29.92756435779241\n ],\n [\n -95.87493896484374,\n 29.888280933159265\n ],\n [\n -95.86257934570312,\n 29.80251790576445\n ],\n [\n -95.86944580078125,\n 29.75364773335698\n ],\n [\n -95.8447265625,\n 29.69640358280457\n ],\n [\n -95.79940795898438,\n 29.672542219068987\n ],\n [\n -95.69641113281249,\n 29.630771207229\n ],\n [\n -95.63186645507812,\n 29.60092416008231\n ],\n [\n -95.51513671875,\n 29.57106827738255\n ],\n [\n -95.40252685546875,\n 29.511330027309146\n ],\n [\n -95.28030395507812,\n 29.485034019181064\n ],\n [\n -95.17730712890625,\n 29.482643134466617\n ],\n [\n -95.086669921875,\n 29.499378142743375\n ],\n [\n -94.99740600585938,\n 29.532839863453397\n ],\n [\n -94.95483398437499,\n 29.551955878093022\n ],\n [\n -94.9493408203125,\n 29.604506272365295\n ],\n [\n -94.96719360351562,\n 29.653449050468925\n ],\n [\n -94.9822998046875,\n 29.680894340704334\n ],\n [\n -95.01800537109374,\n 29.71787396585316\n ],\n [\n -95.0372314453125,\n 29.744109309616487\n ],\n [\n -95.06881713867188,\n 29.76556948666697\n ],\n [\n -95.06744384765625,\n 29.797751134173065\n ],\n [\n -95.07705688476562,\n 29.837070205715218\n ],\n [\n -95.10314941406249,\n 29.871610558533725\n ],\n [\n -95.1361083984375,\n 29.925183985247404\n ],\n [\n -95.15396118164062,\n 29.972780616663897\n ],\n [\n -95.14572143554688,\n 29.997759725578906\n ],\n [\n -95.185546875,\n 30.01916538794235\n ],\n [\n -95.2294921875,\n 30.02511058549258\n ],\n [\n -95.2789306640625,\n 30.029866486852946\n ],\n [\n -95.33660888671875,\n 30.032244351965684\n ],\n [\n -95.36819458007811,\n 30.039377605001338\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4783e4b07f02db483919","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":160735,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13301,"text":"ofr85476 - 1985 - Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T14:15:13","indexId":"ofr85476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-476","title":"Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina","docAbstract":"Two years of selected hydrologic and micrometeorologic data collected at a low-level radioactive waste burial site near Barnwell, South Carolina are available on magnetic tape in card-image format. Hydrologic data include daily measurements of soil-moisture tension, soil-moisture specific conductance, and soil temperature at four monitoring site locations. Micrometeorlogic data include hourly measurements for the following parameters: dry- and wet-bulb temperatures, soil temperatures, soil heat flux, wind speeds and direction, incoming and reflected short-wave solar radiation, incoming and emitted long-wave radiation, net radiation and precipitation. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85476","usgsCitation":"Dennehy, K., and McMahon, P., 1985, Hydrologic and micrometeorologic data from an unsaturated zone study at a low-level radioactive waste burial site near Barnwell, South Carolina: U.S. Geological Survey Open-File Report 85-476, iv, 32 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85476.","productDescription":"iv, 32 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":147370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0476/report-thumb.jpg"},{"id":41720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0476/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"Barnwell","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.2198,33.4393],[-81.2148,33.3902],[-81.2215,33.2295],[-81.2176,33.2209],[-81.224,33.1581],[-81.2119,33.1476],[-81.2069,33.1344],[-81.1943,33.1231],[-81.2304,33.1176],[-81.2442,33.1189],[-81.2589,33.1134],[-81.2836,33.1083],[-81.3652,33.1081],[-81.4354,33.1297],[-81.4519,33.1346],[-81.5123,33.1503],[-81.5419,33.1579],[-81.5708,33.1332],[-81.6142,33.0953],[-81.6187,33.0952],[-81.6241,33.0946],[-81.6268,33.0941],[-81.6323,33.0928],[-81.6362,33.0924],[-81.6395,33.0923],[-81.6428,33.0928],[-81.6466,33.0937],[-81.6494,33.0949],[-81.6532,33.0973],[-81.6536,33.0977],[-81.6569,33.1009],[-81.6611,33.1041],[-81.6621,33.1046],[-81.667,33.1072],[-81.6752,33.1099],[-81.6851,33.1135],[-81.6961,33.1161],[-81.6993,33.1166],[-81.7016,33.117],[-81.7025,33.1172],[-81.7053,33.1183],[-81.7076,33.1188],[-81.7098,33.1207],[-81.7126,33.1224],[-81.7162,33.1243],[-81.7189,33.1252],[-81.7211,33.1257],[-81.7236,33.1278],[-81.7263,33.13],[-81.7297,33.1332],[-81.7352,33.1368],[-81.7407,33.1409],[-81.7428,33.1424],[-81.7479,33.1463],[-81.7545,33.1517],[-81.759,33.1557],[-81.7622,33.1599],[-81.7648,33.1649],[-81.767,33.1708],[-81.7673,33.1716],[-81.7691,33.1758],[-81.7701,33.1777],[-81.7701,33.1795],[-81.7689,33.1808],[-81.7674,33.1817],[-81.7669,33.183],[-81.7669,33.1839],[-81.7673,33.1864],[-81.7662,33.1877],[-81.7655,33.1881],[-81.7636,33.1894],[-81.762,33.1903],[-81.7615,33.1907],[-81.7609,33.1913],[-81.7588,33.1931],[-81.7577,33.1949],[-81.7573,33.1972],[-81.7575,33.1982],[-81.5165,33.3824],[-81.373,33.4907],[-81.3399,33.4831],[-81.3251,33.485],[-81.3047,33.48],[-81.2738,33.4637],[-81.2463,33.4442],[-81.2198,33.4393]]]},\"properties\":{\"name\":\"Barnwell\",\"state\":\"SC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117f3","contributors":{"authors":[{"text":"Dennehy, K.F.","contributorId":41841,"corporation":false,"usgs":true,"family":"Dennehy","given":"K.F.","affiliations":[],"preferred":false,"id":167568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMahon, P.B. 0000-0001-7452-2379","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":10762,"corporation":false,"usgs":true,"family":"McMahon","given":"P.B.","affiliations":[],"preferred":false,"id":167567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9106,"text":"ofr84748 - 1985 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","interactions":[{"subject":{"id":9106,"text":"ofr84748 - 1985 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","indexId":"ofr84748","publicationYear":"1985","noYear":false,"title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland"},"predicate":"SUPERSEDED_BY","object":{"id":1663,"text":"wsp2284 - 1988 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","indexId":"wsp2284","publicationYear":"1988","noYear":false,"title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland"},"id":1}],"supersededBy":{"id":1663,"text":"wsp2284 - 1988 - Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","indexId":"wsp2284","publicationYear":"1988","noYear":false,"title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland"},"lastModifiedDate":"2022-08-23T20:08:54.206848","indexId":"ofr84748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-748","title":"Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland","docAbstract":"

Ground water in the 3,458-square-mile lower Susquehanna River basin occupies secondary openings in bedrock. The distribution of openings is a function of lithology, depth, and topography. Local flow systems account for most of the total ground-water flow. Average annual recharge for the lower basin is 1,857 million gallons per day, most of which discharges to streams. The water table is a subdued replica of land surface; its depth varies with topography, but is generally 20 to 70 feet below land surface. Ground water circulates to depths of 500 to 600 feet below the water table.

A digital model of regional, unconfined ground-water flow was developed and used to evaluate the ground-water resources of the lower basin. On the basis of lithologic and hydrologic differences, the area was subdivided into 21 hydrogeologic units, each with different hydrologic characteristics. Each unit was divided into two layers to handle decreasing secondary permeability with depth. A finite-difference grid with square blocks approximately one mile on a side was used. The model was calibrated under steady-state and transient conditions. The model-generated results were compared to estimated water-table altitudes and estimated base flows in the steady-state calibration. In the transient calibration, the model-generated results were compared to observed changes in water-table altitude from November 1, 1980 through April 22, 1981.

Hydraulic conductivity increases from hilltops to valley bottoms. The average hydraulic conductivity for carbonate units is about 21 feet per day, which is an order of magnitude greater than the corresponding averages for Paleozoic sedimentary, Triassic sedimentary, and crystalline units. The Cumberland Valley carbonate rocks have the greatest average hydraulic conductivity--about 174 feet per day in valley bottoms. The average gaining-stream leakage coefficient for all carbonate units is about 16 feet per day, which is two orders of magnitude greater than the corresponding averages for the other lithologies. The Cumberland Valley carbonate rocks have the greatest gaining-stream leakage coefficient--about 43 feet per day. The specific yields are 0.035, 0.020, 0.020 and 0.007 for the carbonate, Paleozoic sedimentary, crystalline, and Triassic sedimentary units, respectively.

The calibrated model was used to simulate the effects of a ground-water withdrawal of 1 inch per year on water-table altitudes and average annual base flows in the modeled area. The overall effect is least for the carbonate units and greatest for the Triassic sedimentary units. The model also was used to simulate a standardized potential yield for each unit by assuming that the maximum acceptable consequence of a hypothetical withdrawal scheme is an ultimate 50-percent reduction in average annual base flow. Based on this, the potential yield for the modeled area is 891 million gallons per day. The Cumberland Valley carbonate rocks have the greatest potential yield--0.47 million gallons per day per square mile. The carbonate units have the greatest average potential yield, followed by the Paleozoic sedimentary, crystalline, and Triassic sedimentary units. About 90 percent of the eventual decline in water-table altitudes and the eventual reduction in average annual base flows occurs within five years of the implementation of the hypothetical withdrawal scheme. Nearly all of the ground water withdrawn is derived from reduced discharge to streams.

The calibrated model can be used to provide estimates of the impacts of ground-water development schemes on regional ground-water levels and base flows of streams. It can not be used to simulate local cones of depression or local base-flow changes. The reliability of the model is a function of its approximation of the physical characteristics of the ground-water flow system, the two calibrations, various simplifying assumptions, and the lack of calibration under ground-water withdrawal conditions. It can be used in steady-state or transient mode to assess the effects of both natural and artificial stresses.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84748","collaboration":"Prepared in cooperation with the Susquehanna River Basin Commission","usgsCitation":"Gerhart, J.M., and Lazorchick, G.J., 1985, Evaluation of the ground-water resources of the lower Susquehanna River basin, Pennsylvania and Maryland: U.S. Geological Survey Open-File Report 84-748, Report: ix, 183 p.; 2 Plates: 30.03 x 23.75 inches and 29.77 x 23.98 inches, https://doi.org/10.3133/ofr84748.","productDescription":"Report: ix, 183 p.; 2 Plates: 30.03 x 23.75 inches and 29.77 x 23.98 inches","costCenters":[],"links":[{"id":141903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0748/report-thumb.jpg"},{"id":405493,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0748/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405492,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0748/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405491,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maryland, Pennsylvania","otherGeospatial":"Susquehanna River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.761474609375,\n 39.5633531658293\n ],\n [\n -75.948486328125,\n 39.5633531658293\n ],\n [\n -75.948486328125,\n 40.14109012528468\n ],\n [\n -76.761474609375,\n 40.14109012528468\n ],\n [\n -76.761474609375,\n 39.5633531658293\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4ab","contributors":{"authors":[{"text":"Gerhart, James M.","contributorId":35717,"corporation":false,"usgs":true,"family":"Gerhart","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lazorchick, George J.","contributorId":18743,"corporation":false,"usgs":true,"family":"Lazorchick","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159110,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8082,"text":"ofr84802 - 1985 - Hydrogeologic data from a test well in east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr84802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-802","title":"Hydrogeologic data from a test well in east-central Duval County, Florida","docAbstract":"A 2,112-foot test well was drilled in east-central Duval County, Florida, to obtain geologic, hydrologic, and water chemistry data. Drill cuttings and water samples were collected, and water-level measurements and lithologic and geophysical logs were made. Deposits to a depth of 575 feet consist of sand, clayey sand, phosphatic sandy clay, coquina, sandy limestone, and dolostone. Below 575 feet, the deposits consist of fragmented and granular limestone, dolomitic limestone, and massive to finely crystalline dolostone, which comprise the Floridan aquifer system in the area. Water levels were measured near or at the bottom of the drill hole through the drill stem and in the annular space between the drilled hole and drill stem at the well head as drilling progressed from 770 to 2,112 feet in depth. Water levels measured through the drill stem ranged from 1.17 feet above land surface at a depth of 2,107 feet to 15.0 feet above land surface at a depth of 1,574 feet. Water levels measured in the annular space ranged from 7.5 feet above land surface at a depth of 770 feet to 14.9 feet at various depths from 1,574 to 1,721 feet. Chloride concentrations of water sampled through the drill stem from a depth of 711 to 1 ,616 feet ranged from 22 to 150 milligrams per liter at 1,648 feet. Chloride concentrations then ranged from 345 to about 800 milligrams per liter to a depth of 2,071 feet and then increased to a maximum of 5,450 milligrams per liter at 2,107 feet. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84802","usgsCitation":"Brown, D., Johnson, R., and Broxton, R., 1985, Hydrogeologic data from a test well in east-central Duval County, Florida: U.S. Geological Survey Open-File Report 84-802, iv, 67 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84802.","productDescription":"iv, 67 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0802/report-thumb.jpg"},{"id":35686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0802/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6273e5","contributors":{"authors":[{"text":"Brown, D.P.","contributorId":95881,"corporation":false,"usgs":true,"family":"Brown","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":157113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R.A.","contributorId":93864,"corporation":false,"usgs":true,"family":"Johnson","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157112,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broxton, R.A.","contributorId":36934,"corporation":false,"usgs":true,"family":"Broxton","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":157111,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2788,"text":"wsp2217 - 1985 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","interactions":[{"subject":{"id":11397,"text":"ofr811119 - 1981 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu, with a section on flow hydraulics in dike tunnels in Hawaii","indexId":"ofr811119","publicationYear":"1981","noYear":false,"title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu, with a section on flow hydraulics in dike tunnels in Hawaii"},"predicate":"SUPERSEDED_BY","object":{"id":2788,"text":"wsp2217 - 1985 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","indexId":"wsp2217","publicationYear":"1985","noYear":false,"title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu"},"id":1}],"lastModifiedDate":"2022-09-14T18:34:00.298716","indexId":"wsp2217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2217","title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","docAbstract":"Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the island of Oahu because they generally underlie the rainiest areas. These reservoirs accumulate the infiltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water.\r\n\r\nThe most important and productive of the dike-impounded reservoirs are in an area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Water is impounded and stored both above and below sea level. The water stored above sea level in the 135 square mile area has been roughly estimated at 560 billion gallons. In comparison, the water stored above sea level in reservoirs underlying a dike-intruded area of about 53 square miles in the Waianae Range has been roughly estimated at 100 billion gallons. Storage below sea level is indeterminable, owing to uncertainties about the ability of the rock to store water as dike density increases and porosity decreases.\r\n\r\nTunnels, by breaching dike controls, have reduced the water stored above sea level by at least 50 billion gallons in the Koolau Range and by 5 1/2 billion gallons in the Waianae Range, only a small part of the total water stored.\r\n\r\nTotal leakage from storage in the Koolau Range has been estimated at about 280 Mgal/d (million gallons per day). This estimated leakage from the dike-impounded reservoirs makes up a significant part of the ground-water yield of the Koolau Range, which has been estimated to range from 450 to 580 Mgal/d. The largest unused surface leakage is in the Kaneohe, Kahana, and Punaluu areas, and the largest unused underflow occurs in the Waialee, Hauula-Laie, Punaluu, and Kahana areas. The unused underflow leakage is small in areas near and east of Waialae, but it is an important supply because of the great need for augmenting water supplies there.\r\n\r\nTotal leakage from storage in the Waianae Range has not been estimated because underflow is difficult to determine. Much of the surface leakage, about 4 Mgal/d in the upper parts of Waianae, Makaha, and Lualualei Valleys, has been diverted by tunnels. Hence, supplies available, other than surface leakage, cannot be estimated from the discharge end of the hydrologic cycle. Infiltration in the Waianae Range to dike-intruded reservoirs in the upper part of the valleys on the west (leeward) side has been estimated at about 20 Mgal/d, and on the east (windward) side, at about 10 Mgal/d. The available supply has been estimated at about 15 Mgal/d from the infiltration on the leeward side, of which about 4 Mgal/d is now being developed. No estimate has been made for the available supply on the windward side. Dike-intruded reservoirs at shallow depths west (lee side) of the crest are in upper Makaha, Waianae, and Lualualei Valleys. They are at moderate depths in upper Haleanu and in lower Kaukonahua Gulches on the east (windward) side.\r\n\r\nFlow hydraulics in dike tunnels is also discussed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2217","usgsCitation":"Takasaki, K.J., and Mink, J.F., 1985, Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu: U.S. Geological Survey Water Supply Paper 2217, vi, 77 p., https://doi.org/10.3133/wsp2217.","productDescription":"vi, 77 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":406706,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25463.htm","linkFileType":{"id":5,"text":"html"}},{"id":29268,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2217/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2217/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -158.31298828125,\n 21.21257979063059\n ],\n [\n -157.60986328125,\n 21.21257979063059\n ],\n [\n -157.60986328125,\n 21.70847301324597\n ],\n [\n -158.31298828125,\n 21.70847301324597\n ],\n [\n -158.31298828125,\n 21.21257979063059\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7274","contributors":{"authors":[{"text":"Takasaki, Kiyoshi J.","contributorId":105700,"corporation":false,"usgs":true,"family":"Takasaki","given":"Kiyoshi","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mink, John Francis","contributorId":48164,"corporation":false,"usgs":true,"family":"Mink","given":"John","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":145789,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15660,"text":"ofr85498 - 1985 - May 1984-April 1985 water budget of Reelfoot Lake with estimates of sediment inflow and concentrations of pesticides in bottom material in tributary streams: Basic data report","interactions":[],"lastModifiedDate":"2022-12-05T20:47:14.137948","indexId":"ofr85498","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-498","title":"May 1984-April 1985 water budget of Reelfoot Lake with estimates of sediment inflow and concentrations of pesticides in bottom material in tributary streams: Basic data report","docAbstract":"

This report contains hydrologic data collected at Reelfoot Lake, Tennessee from May 1, 1984, through April 30, 1985. Continuous streamflow data were collected at four sites on the three major tributaries to Reelfoot Lake and at one site on the lake outflow channel. Daily rainfall and lake-stage were each collected at two sites on the lake shore. Additionally, suspended-sediment samples were collected by automatic samplers and also manually during equipment maintenance visits at three of the four tributary inflow sites. At these three inflow sites, samples of stream-bottom material were collected at low flow once during the study period and were analyzed to determine the concentration of various pesticides. Periodic observations of ground-water levels were made at 30 wells in the Reelfoot Lake basin. Monitoring sites and types of data collected at each site are listed.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85498","usgsCitation":"Robbins, C.H., Garrett, J., and Mulderink, D., 1985, May 1984-April 1985 water budget of Reelfoot Lake with estimates of sediment inflow and concentrations of pesticides in bottom material in tributary streams: Basic data report: U.S. Geological Survey Open-File Report 85-498, iv, 37 p., https://doi.org/10.3133/ofr85498.","productDescription":"iv, 37 p.","costCenters":[],"links":[{"id":146514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410061,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75814.htm","linkFileType":{"id":5,"text":"html"}},{"id":993,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr85-498","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","otherGeospatial":"Reelfoot Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.2875914893548,\n 36.50756978562153\n ],\n [\n -89.51549075172562,\n 36.50756978562153\n ],\n [\n -89.51549075172562,\n 36.25029316922085\n ],\n [\n -89.2875914893548,\n 36.25029316922085\n ],\n [\n -89.2875914893548,\n 36.50756978562153\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6101ec","contributors":{"authors":[{"text":"Robbins, C. H.","contributorId":54210,"corporation":false,"usgs":true,"family":"Robbins","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":171510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, J.W.","contributorId":87958,"corporation":false,"usgs":true,"family":"Garrett","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":171511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulderink, D. M.","contributorId":98736,"corporation":false,"usgs":true,"family":"Mulderink","given":"D. M.","affiliations":[],"preferred":false,"id":171512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13843,"text":"ofr85572 - 1985 - Use and availability of continuous streamflow records in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr85572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-572","title":"Use and availability of continuous streamflow records in New Mexico","docAbstract":"The use and availability of data collected at streamflow gaging stations in New Mexico is documented as the first phase of a three phase study of the cost-effectiveness of the stream gaging program. Presently, 143 continuous gaging stations are operated. Data collected at most gaging stations have multiple uses. Many stations are operated under the terms of eight legal compacts and two court decrees. These data provide the basis for distribution of irrigation water and operation of dams. Data from six stations are used for forecasting flood conditions. Water quality data are collected at many of the stations, ten of which have been designated as part of a national network of water quality data monitoring and two under the benchmark program. Data useful in the defining regional hydrology have been collected at a majority of the stations. All stations presently (1984) have sufficient justification for continued operations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85572","usgsCitation":"Gold, R., and Denis, L., 1985, Use and availability of continuous streamflow records in New Mexico: U.S. Geological Survey Open-File Report 85-572, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85572.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0572/report-thumb.jpg"},{"id":42443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0572/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60520c","contributors":{"authors":[{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":168491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denis, L.P.","contributorId":38417,"corporation":false,"usgs":true,"family":"Denis","given":"L.P.","email":"","affiliations":[],"preferred":false,"id":168490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}