{"pageNumber":"5575","pageRowStart":"139350","pageSize":"25","recordCount":184828,"records":[{"id":24624,"text":"ofr80551 - 1980 - Index of streamflow and water quality records to September 30, 1978, Southwest Alaska","interactions":[],"lastModifiedDate":"2018-10-31T13:59:29","indexId":"ofr80551","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-551","title":"Index of streamflow and water quality records to September 30, 1978, Southwest Alaska","docAbstract":"

This report, which is one of a series of reports for Alaska, lists stations in southwest Alaska (fig. 1) at which streamflow and water-quality data have been collected by the U.S. Geological Survey.

Most of the data referred to in this report have been published in reports of the Geological Survey. Water-quality data which were not included in those reports have been placed in the Survey's national computer storage system and are available through data-retrieval programs. Some of the older streamflow data have not been entered into the computer system. Geological Survey Water-Supply Paper (WSP) 1372 contains a summary of previously published records of monthly and annual discharges through September 1945, as well as records of daily and monthly discharges for the water years 1946-50 that had not yet been published. Water-Supply Paper 1372 also contains other stream chemical quality records collected between September 1948 and September 1950 and also some earlier records for the Yukon River at Anvik. Since 1950 data have been published in water-supply papers and a series of annual reports...

Data have been published in the annual series of reports, \"Water Resources Data for Alaska,\" since 1961 for streamflow records and 1964 for water-quality records.

This index lists: continuous-record streamgaging stations, crest-stage gage and low-flow partial-record stations; daily chemical, sediment, and temperature stations; and stations where some chemical, sediment, and biological data have been collected on an intermittent basis.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80551","issn":"0094-9140","usgsCitation":"Still, P.J., 1980, Index of streamflow and water quality records to September 30, 1978, Southwest Alaska: U.S. Geological Survey Open-File Report 80-551, iii, 13 p., https://doi.org/10.3133/ofr80551.","productDescription":"iii, 13 p.","costCenters":[],"links":[{"id":359036,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0551/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":111907,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11301","linkFileType":{"id":5,"text":"html"}},{"id":157864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0551/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -188.7890625,\n 51.069016659603896\n ],\n [\n -152,\n 51.069016659603896\n ],\n [\n -152,\n 64\n ],\n [\n -188.7890625,\n 64\n ],\n [\n -188.7890625,\n 51.069016659603896\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e9e4b07f02db553ad5","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24588,"text":"ofr80808 - 1980 - A possible relationship between subsidence and uranium mineralization in the Petrified Forest Member of the Chinle Formation in the Cameron and Holbrook-St. Johns area of Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr80808","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-808","title":"A possible relationship between subsidence and uranium mineralization in the Petrified Forest Member of the Chinle Formation in the Cameron and Holbrook-St. Johns area of Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80808","issn":"0094-9140","usgsCitation":"Spirakis, C.S., 1980, A possible relationship between subsidence and uranium mineralization in the Petrified Forest Member of the Chinle Formation in the Cameron and Holbrook-St. Johns area of Arizona: U.S. Geological Survey Open-File Report 80-808, 9 p. :map ;28 cm., https://doi.org/10.3133/ofr80808.","productDescription":"9 p. :map ;28 cm.","costCenters":[],"links":[{"id":155730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab729","contributors":{"authors":[{"text":"Spirakis, Charles S.","contributorId":97111,"corporation":false,"usgs":true,"family":"Spirakis","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":192209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22339,"text":"ofr801197 - 1980 - Study plan for the regional aquifer-system analysis of alluvial basins in south-central Arizona and adjacent states","interactions":[],"lastModifiedDate":"2022-04-26T22:35:43.105676","indexId":"ofr801197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1197","title":"Study plan for the regional aquifer-system analysis of alluvial basins in south-central Arizona and adjacent states","docAbstract":"

The alluvial basins in the Southwestern United States constitute a major source of ground water and are relied upon extensively for agricultural, industrial, and public water supplies. Large-scale depletion of ground water is directly related to pumping that has occurred in the past few decades and is continuing today. The U.S. Geological Survey has started a 4-year study of the alluvial basins in south-central Arizona and parts of California, Nevada, and New Mexico. The study is designed to document and describe the hydrologic setting in the basins, the ground-water resources available, and the effects of historical development on the ground-water system. To aid in the study, mathematical models of selected basins will be developed for appraising the local and regional flow systems.

Major tasks necessary to accomplish the study objectives include accumulating existing data on ground-water quantity and quality, entering the data into a computer file, identifying data deficiencies, and developing a program to remedy the deficiencies by collection of additional data. The approach to the study will be to develop and calibrate models of selected basins for which sufficient data exist and then to develop interpretation-transfer techniques whereby general predevelopment and postdevelopment conceptual models of the hydrologic system in other basins may be synthesized. The results will be applied to selected basins for testing, calibration, and modification. The end result of the project will be a better definition of the hydrologic parameters and a better understanding of the workings of the hydrologic system in the alluvial basins. The results will include models that can be used to study the effects of management alternatives and water-resources development on the hydrologic system.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801197","issn":"0094-9140","usgsCitation":"Anderson, T.W., 1980, Study plan for the regional aquifer-system analysis of alluvial basins in south-central Arizona and adjacent states: U.S. Geological Survey Open-File Report 80-1197, iv, 22 p., https://doi.org/10.3133/ofr801197.","productDescription":"iv, 22 p.","costCenters":[],"links":[{"id":399715,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1197/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1197/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"south-central Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.85107421875,\n 31.259769987394286\n ],\n [\n -109.09423828125,\n 31.259769987394286\n ],\n [\n -109.09423828125,\n 36.2265501474709\n ],\n [\n -114.85107421875,\n 36.2265501474709\n ],\n [\n -114.85107421875,\n 31.259769987394286\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ca1","contributors":{"authors":[{"text":"Anderson, T. W.","contributorId":105686,"corporation":false,"usgs":true,"family":"Anderson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":188068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24622,"text":"ofr80600 - 1980 - Index of streamflow and water quality records to September 30, 1978, south-central Alaska","interactions":[],"lastModifiedDate":"2019-08-29T11:04:21","indexId":"ofr80600","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-600","title":"Index of streamflow and water quality records to September 30, 1978, south-central Alaska","docAbstract":"This report, which is one of a series of reports for Alaska, lists stations in south-central Alaska at which streamflow and water quality data have been collected by the U.S. Geological Survey. Included are a hydrologic subregion map of south-central Alaska and a table listing the types of data collected and periods of record. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80600","issn":"0094-9140","usgsCitation":"Still, P.J., 1980, Index of streamflow and water quality records to September 30, 1978, south-central Alaska: U.S. Geological Survey Open-File Report 80-600, iii, 54 p., https://doi.org/10.3133/ofr80600.","productDescription":"iii, 54 p.","costCenters":[],"links":[{"id":157761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0600/report-thumb.jpg"},{"id":111911,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/11297","linkFileType":{"id":5,"text":"html"}},{"id":367084,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0600/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -152.29248046875,\n 59.0405546167585\n ],\n [\n -141.0205078125,\n 59.0405546167585\n ],\n [\n -141.0205078125,\n 62.804978549147954\n ],\n [\n -152.29248046875,\n 62.804978549147954\n ],\n [\n -152.29248046875,\n 59.0405546167585\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624659","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3386,"text":"cir836B - 1980 - Earthquakes in the United States, April-June 1979","interactions":[],"lastModifiedDate":"2022-09-14T20:24:09.68315","indexId":"cir836B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"836","chapter":"B","title":"Earthquakes in the United States, April-June 1979","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir836B","usgsCitation":"Stover, C.W., Hubiak, P., Minsch, J.H., and Person, W., 1980, Earthquakes in the United States, April-June 1979: U.S. Geological Survey Circular 836, iv, 34 p., https://doi.org/10.3133/cir836B.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":406725,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23726.htm","linkFileType":{"id":5,"text":"html"}},{"id":30403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0836b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0836b/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n 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Measurements at bankfull stage were made at 136 sites to determine whether predictions of flood discharges using channel-geometry characteristics are as good as or better than predictions using basin characteristics. These measurements are used to determine the variables of bankfull width, area, depth, and velocity. These variables are combined with basin characteristics for the sites, and multiple-regression techniques are used to select the best combination of variables to estimate the selected floods.

Generally, discharge estimates obtained from equations using channel characteristics have smaller standard errors than those using basin characteristics, and equations using both basin and channel characteristics have even lower standard errors.

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No abstract available.

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Federal and State legislation require the trophic classification of lakes and ponds in the State of Maine as part of a lake management program. In 1974, the State of Maine Department of Environmental Protection (DEP) adopted a preliminary set of procedures for establishing an index of lake trophic status. Also in 1974, this three-year study of selected Maine lakes was initiated to evaluate and improve this trophic classification system.

Analyses of project results led to the following rec-commendations for modifications in Maine's lake-management program. Lake trophic state should be established using a mean annual value of twice monthly observations of chlorophyll a in epilimnetic waters during the open-water season. Actual Trophic State Index (TSI) values for lakes are calculated using the formula: TSI = 77.7 - 27.3 (log annual mean chlorophyll a, in mg/L). In lakes with colors less than or equal to TO platinum-cobalt units, mean annual Secchi disk transparencies may be used for calculation of lake TSI using the formula: TSI = 40.0 + 33.0 (log annual10mean Secchi disk, in meters).

Supplemental information recommended for inclusion in the lake management program should include: morphological, hydrologic, and geologic data; baseline profile water-quality surveys; and benthic invertebrate, vegetation, and cultural surveys. Another recommendation is to change DEP's method of calculating the mean annual runoff for a lake drainage basin to an empirical formula based on drainage area characteristics. This resulted in more accurate estimations of mean annual hydraulic retention times for lakes. Many of these parameters recommended for inclusion in the lake management program will allow comparisons with future surveys to determine the impacts of cultural development on Maine lakes.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae2cf","contributors":{"authors":[{"text":"Cowing, Derrill J.","contributorId":97473,"corporation":false,"usgs":true,"family":"Cowing","given":"Derrill","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Matthew","contributorId":37374,"corporation":false,"usgs":true,"family":"Scott","given":"Matthew","email":"","affiliations":[],"preferred":false,"id":196814,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24541,"text":"ofr8152 - 1980 - Behavior of weakly cemented soil slopes under static and seismic loading conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr8152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"81-52","title":"Behavior of weakly cemented soil slopes under static and seismic loading conditions","language":"ENGLISH","publisher":"The John A. Blume Earthquake Engineering Center, Dept. of Civil Engineering ;\r\nU.S. Geological Survey,","doi":"10.3133/ofr8152","issn":"0094-9140","usgsCitation":"Sitar, N., Clough, G., and Bachus, R., 1980, Behavior of weakly cemented soil slopes under static and seismic loading conditions: U.S. Geological Survey Open-File Report 81-52, 208 p.:ill. ;28 cm., https://doi.org/10.3133/ofr8152.","productDescription":"208 p.:ill. ;28 cm.","costCenters":[],"links":[{"id":156682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0052/report-thumb.jpg"},{"id":53588,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c27d","contributors":{"authors":[{"text":"Sitar, Nicholas","contributorId":42253,"corporation":false,"usgs":true,"family":"Sitar","given":"Nicholas","email":"","affiliations":[],"preferred":false,"id":192113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clough, G. Wayne","contributorId":82349,"corporation":false,"usgs":true,"family":"Clough","given":"G. Wayne","affiliations":[],"preferred":false,"id":192115,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bachus, Robert","contributorId":68349,"corporation":false,"usgs":true,"family":"Bachus","given":"Robert","email":"","affiliations":[],"preferred":false,"id":192114,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4708,"text":"twri03B3 - 1980 - Type curves for selected problems of flow to wells in confined aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri03B3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-B3","title":"Type curves for selected problems of flow to wells in confined aquifers","docAbstract":"This report presents type curves and related material for\r\n11 conditions of flow to wells m confined aquifers. These\r\nsolutions, compiled from hydrologic literature, span an\r\ninterval of time from Theis (1935) to Papadopulos, Bredehoeft,\r\nand Cooper (1973). Solutions are presented for\r\nconstant discharge, constant drawdown, and variable discharge\r\nfor pumping wells that fully penetrate leaky and\r\nnonleaky aquifers. Solutions for wells that partially penetrate\r\nleaky and nonleaky aquifers are included. Also, solutions\r\nare included for the effect of finite well radius and\r\nthe sudden injection of a volume of water for nonleaky\r\naquifers. Each problem includes the partial differential\r\nequation, boundary and initial conditions, and solutions.\r\nPrograms in FORTRAN for calculating additional function\r\nvalues are included for most of the solutions.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri03B3","issn":"0565-596X","usgsCitation":"Reed, J., 1980, Type curves for selected problems of flow to wells in confined aquifers: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B3, ix, 106 p. :ill. ;26 cm., https://doi.org/10.3133/twri03B3.","productDescription":"ix, 106 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":139146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":297,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-b3/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6237d2","contributors":{"authors":[{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":149655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23423,"text":"ofr80750 - 1980 - Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2022-08-16T21:39:59.411695","indexId":"ofr80750","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-750","title":"Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California","docAbstract":"

A nearly threefold increase in demand for water in the 154-square-mile San Antonio Creek valley in California during the period 1958-77 has increased the potential for overdraft on the ground-water basin. The hydrologic budget for this period showed a perennial yield of about 9,800 acre-feet per year and an annual ground-water discharge of about 11,400 acre-feet per year, comprising net pumpage of 7,100 acre-feet, phreatophyte evapotranspiration of 3,000 acre-feet, and base streamflow of 1 ,300 acre-feet. The base flow in San Antonio Creek could diminish to zero when net pumpage reaches 13,500 acre-feet per year. The environmentally sensitive marshland area of Barka Slough may then become stressed as water normally lost through evapotranspiration is captured by pumpage. The aquifer consists of alluvial valley fill that ranges in thickness from 0 to 3,500 feet. Ground water moves seaward from recharge areas along mountain fronts to a consolidated rock barrier about 5 miles east of the Pacific coast. Upwelling of ground water just east of the barrier has resulted in the 550-acre Barka Slough. Transmissivity of the aquifer ranges from 2,600 to 34,000 feet squared per day, with the lowest values occurring in the central part of the valley where the aquifer is thickest but probably finer grained. The salinity problems are increasing in the agricultural parts of the valley, which is east of the barrier. West of the barrier, stream and ground-water quality is poor, owing to seepage of saline water from the marine shale that underlies the area at shallow depths. A proposed basinwide monitoring program includes 17 water-level sites, 12 water-quality sampling sites, 3 streamflow measuring sites, and periodic infrared aerial photography of Barka Slough. A computer model of the ground-water flow system could be developed to assess the impact of various water-management alternatives. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80750","usgsCitation":"Hutchinson, C.B., 1980, Appraisal of ground-water resources in the San Antonio Creek Valley, Santa Barbara County, California (WRI/OFR): U.S. Geological Survey Open-File Report 80-750, iv, 48 p., https://doi.org/10.3133/ofr80750.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":52752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0750/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0750/report-thumb.jpg"},{"id":405235,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11757.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"San Antonio Creek Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.646,\n 34.678\n ],\n [\n -120.112,\n 34.678\n ],\n [\n -120.112,\n 34.853\n ],\n [\n -120.646,\n 34.853\n ],\n [\n -120.646,\n 34.678\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a394","contributors":{"authors":[{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24510,"text":"ofr80914 - 1980 - The microzonation of the Memphis, Tennessee area","interactions":[],"lastModifiedDate":"2022-07-18T16:31:47.09312","indexId":"ofr80914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-914","title":"The microzonation of the Memphis, Tennessee area","docAbstract":"

Although the probability of a major earthquake in the central U.S. is only one-tenth of the Californian events, any such event is expected to result in damage ten times greater than that anticipated in California. The city of Memphis, which is situated very close to the inferred epicenter of one of the three major 1811-1812 earthquakes, is in a potentially hazardous zone which will be susceptible to the usual seismic hazards. By recognizing the high level of seismicity in the New Madrid area, this study attempts to microzone the potential hazards in the city of Memphis.

This study examines the pertinent criteria necessary for any microzonation study. The subjects considered include:
(i) The seismicity of the central United States,
(ii) Design earthquakes,
(iii) Response analysis which allows us to construct the necessary microzonation maps.

The seismicity of the region is evaluated according to the state-of-the-art literature available as there is no recorded strong motion data available for the central U.S. The maximum credible earthquakes which are likely to affect Memphis are evaluated as the one in a thousand year occurrence. However, earthquakes of a lower intensity (and lower recurrence rates) are selected as design earthquakes to permit a more realistic microzonation to be performed.

For the response analysis, these earthquakes are simulated using synthetically generated accelerograms which exhibit the relevant parameters. These accelerograms displaying the significant characteristics of amplitude, predominant frequency and duration were selected to display, as accurately as possible, the anticipated nature of the horizontal bedrock-motions at Memphis. The horizontal motions (SH-waves) were applied at a depth of 45m below ground surface at numerous sites in the city of Memphis, where the soil stratigraphy had been conceptualized from borehole data.

The soils data made available by local sources was the only information used for this study as any laboratory testing was outside the scope of this study. The dynamic soil properties were thus established from the available Standard Penetration Resistances and soil classifications.

The results of the response analysis were transformed into microzonation maps depicting
(i) zones showing qualitative estimates of ground response,
(ii) zones showing the natural frequency of the soils,
(iii) zones showing the peak spectral acceleration for 2% damping ratio,
(iv) zones of liquefaction potential.

These maps are essentially useful for preliminary investigation and we do not expect them to be used on a quantitative basis. However, further investigation is necessary in determining the stratigraphy and soil properties to a more accurate level if an earthquake hazard is anticipated.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80914","usgsCitation":"Sharma, S., and Kovacs, W.D., 1980, The microzonation of the Memphis, Tennessee area: U.S. Geological Survey Open-File Report 80-914, vi, 129 p., https://doi.org/10.3133/ofr80914.","productDescription":"vi, 129 p.","costCenters":[],"links":[{"id":403923,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0914/report.pdf"},{"id":156554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0914/report-thumb.jpg"}],"country":"United States","state":"Tennessee","city":"Memphis area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.076904296875,\n 35.074964853989556\n ],\n [\n -89.85992431640625,\n 35.074964853989556\n ],\n [\n -89.85992431640625,\n 35.22318504970181\n ],\n [\n -90.076904296875,\n 35.22318504970181\n ],\n [\n -90.076904296875,\n 35.074964853989556\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a28f","contributors":{"authors":[{"text":"Sharma, Sunil","contributorId":81522,"corporation":false,"usgs":true,"family":"Sharma","given":"Sunil","email":"","affiliations":[],"preferred":false,"id":192053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kovacs, William D.","contributorId":95096,"corporation":false,"usgs":true,"family":"Kovacs","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":192054,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24585,"text":"ofr80595 - 1980 - A preliminary report of the geohydrology of the Mississippi salt-dome basin","interactions":[],"lastModifiedDate":"2022-07-13T00:25:28.334002","indexId":"ofr80595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-595","title":"A preliminary report of the geohydrology of the Mississippi salt-dome basin","docAbstract":"The U.S. Department of Energy is investigating the suitability of salt domes in the Mississippi salt-dome basin as repositories for storing radioactive wastes. The Department of Energy has requested that the U.S. Geological Survey describe the groundwater hydrology of the Mississippi salt-dome basin, giving special attention to direction and rate of movement of water. In this first part of a continuing investigation the data obtained from one year of extensive literature search and data compilation are summarized. The regional groundwater hydrology in the salt-dome basin is defined with respect to (1) groundwater flow, (2) facies changes, (3) geological structure, (4) recharge and discharge, (5) freshwater-saltwater relations, and (6) identification of localities where additional data are needed. From the 50 piercement-type salt domes in the Mississippi salt-dome basin three domes (Richton, Cypress Creek, and Lampton) were selected for more intensive study. To further evaluate the geohydrology of Richton, Lampton, and Cypress Creek domes as possible sites for storage of radioactive waste, an intensive geohydrologic study based on a comprehensive test drilling program near the domes is planned. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80595","usgsCitation":"Spiers, C.A., and Gandl, L.A., 1980, A preliminary report of the geohydrology of the Mississippi salt-dome basin: U.S. Geological Survey Open-File Report 80-595, Report: v, 45 p.; 8 Plates: 10.60 × 16.40 inches or smaller, https://doi.org/10.3133/ofr80595.","productDescription":"Report: v, 45 p.; 8 Plates: 10.60 × 16.40 inches or smaller","costCenters":[],"links":[{"id":403577,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11701.htm","linkFileType":{"id":5,"text":"html"}},{"id":53634,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0595/report-thumb.jpg"},{"id":53635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0595/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53627,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53628,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53629,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53630,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53631,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53632,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53633,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0595/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.625,\n 30.908\n ],\n [\n -88.427,\n 30.908\n ],\n [\n -88.427,\n 32.85\n ],\n [\n -91.625,\n 32.85\n ],\n [\n -91.625,\n 30.908\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8733","contributors":{"authors":[{"text":"Spiers, C. A.","contributorId":69187,"corporation":false,"usgs":true,"family":"Spiers","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gandl, L. A.","contributorId":91856,"corporation":false,"usgs":true,"family":"Gandl","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4053,"text":"cir841 - 1980 - Four reference soil and rock samples for measuring element availability in the Western Energy Regions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"cir841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"841","title":"Four reference soil and rock samples for measuring element availability in the Western Energy Regions","docAbstract":"Attaining acceptable precision in extractable element determinations is more difficult than in total element determinations. In total element determinations, dissolution of the sample is qualitatively checked by the clarity of the solution and the absence of residues. These criteria cannot be used for extracts. Possibilities for error are introduced in virtually every step in soil extractions. Therefore, the use of reference materials whose homogeneity and element content are reasonably well known is essential for determination of extractable elements. In this report, estimates of homogeneity and element content are presented for four reference samples. Bulk samples of about 100 kilograms of each sample were ground to pass an 80-mesh sieve. The samples were homogenized and split using a Jones-type splitter. Fourteen splits of each reference sample were analyzed for total content of Ca, Co, Cu, Fe, K, Mg, Mn, Na, and Zn; DTPA-extractable Cd, Co, Cu, Fe, Mn, Ni, Pb, and Zn; exchangeable Ca, Mg, K, and Na; cation exchange capacity water-saturation-extractable Ca, Mg, K, Na, C1, and SO4; soil pH; and hot-water-extractable boron. Error measured between splits was small, indicating that the samples were homogenized adequately and that the laboratory procedure provided reproducible results.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFree on application to the Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir841","usgsCitation":"Crock, J., and Severson, R.C., 1980, Four reference soil and rock samples for measuring element availability in the Western Energy Regions: U.S. Geological Survey Circular 841, iii, 16 p. :ill. ;26 cm., https://doi.org/10.3133/cir841.","productDescription":"iii, 16 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":125130,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0841/report-thumb.jpg"},{"id":31146,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0841/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a517f","contributors":{"authors":[{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":148077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Severson, R. C.","contributorId":46498,"corporation":false,"usgs":true,"family":"Severson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":148076,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24623,"text":"ofr80698 - 1980 - Index of streamflow and water quality records to September 30, 1978, Southeast Alaska","interactions":[],"lastModifiedDate":"2018-11-19T12:20:14","indexId":"ofr80698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-698","title":"Index of streamflow and water quality records to September 30, 1978, Southeast Alaska","docAbstract":"

This report, which is one of a series of reports for Alaska, lists stations in southeast Alaska (fig. 1) at which streamflow and water-quality data have been collected by the U.S. Geological Survey.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80698","issn":"0094-9140","usgsCitation":"Still, P.J., 1980, Index of streamflow and water quality records to September 30, 1978, Southeast Alaska: U.S. Geological Survey Open-File Report 80-698, iii, 26 p., https://doi.org/10.3133/ofr80698.","productDescription":"iii, 26 p.","costCenters":[],"links":[{"id":157863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0698/report-thumb.jpg"},{"id":359562,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -141.0205078125,\n 54.62297813269033\n ],\n [\n -130.01220703125,\n 54.62297813269033\n ],\n [\n -130.01220703125,\n 60.4788788301667\n ],\n [\n -141.0205078125,\n 60.4788788301667\n ],\n [\n -141.0205078125,\n 54.62297813269033\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a4a5","contributors":{"authors":[{"text":"Still, Patsy J.","contributorId":27077,"corporation":false,"usgs":true,"family":"Still","given":"Patsy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":192274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10191,"text":"ofr801238 - 1980 - Heat flow from the western arm of the Black Rock Desert, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr801238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1238","title":"Heat flow from the western arm of the Black Rock Desert, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801238","usgsCitation":"Mase, C., and Sass, J., 1980, Heat flow from the western arm of the Black Rock Desert, Nevada: U.S. Geological Survey Open-File Report 80-1238, 38 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801238.","productDescription":"38 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1238/report-thumb.jpg"},{"id":38053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1238/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63cfb8","contributors":{"authors":[{"text":"Mase, C. W.","contributorId":106893,"corporation":false,"usgs":true,"family":"Mase","given":"C. W.","affiliations":[],"preferred":false,"id":160975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":160974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28282,"text":"wri79112 - 1980 - Estimated water use in Florida, 1977","interactions":[],"lastModifiedDate":"2019-12-05T08:37:54","indexId":"wri79112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-112","title":"Estimated water use in Florida, 1977","docAbstract":"During 1977, an average of 21,466 million gallons of water was withdrawn daily for use in Florida--an increase of 6,153 million gallons per day since 1970. The 1977 daily use was 14,812 million gallons of saline water and 6,654 million gallons of freshwater. Most of the saline water, largely surface water, was pumped from tidal estuaries. Only 107.6 million gallons per day of saline water--less than 1 percent--was obtained from wells. Thermoelectric power generation used virtually all the saline water, 14,738 million gallons per day, whereas all other industrial uses were only 73 million gallons of saline water per day. The freshwater supply was almost equally divided between ground water (53 percent) and surface water (47 percent). Of the total freshwater used, 43 percent was for irrigation--an average of 2,873 million gallons of freshwater daily on the average. The remaining daily use of freshwater was 21 percent for thermoelectric power generation, 19 percent for public supply; 14 percent for industrial use other than thermoelectric power generation; and 3 percent for domestic and rural use. Irrigation was also responsible for the greatest consumption during 1977, with 1,255 million gallons consumed daily which also includes 192 million gallons per day conveyance loss. (Kosco-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri79112","usgsCitation":"Leach, S.D., and Healy, H.G., 1980, Estimated water use in Florida, 1977: U.S. Geological Survey Water-Resources Investigations Report 79-112, iv, 76 p. , https://doi.org/10.3133/wri79112.","productDescription":"iv, 76 p. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc61","contributors":{"authors":[{"text":"Leach, Stanley D.","contributorId":101670,"corporation":false,"usgs":true,"family":"Leach","given":"Stanley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":199526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, Henry G.","contributorId":89916,"corporation":false,"usgs":true,"family":"Healy","given":"Henry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":199525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28481,"text":"wri79114 - 1980 - Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana","interactions":[],"lastModifiedDate":"2019-11-06T15:26:07","indexId":"wri79114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-114","title":"Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana","docAbstract":"The Red River Waterways Project provides for the construction of five locks and dams on the Red River from the Mississippi River to Shreveport, La. The methodology used by the U.S. Geological Survey in studying the effects of the navigation pools on the ground-water-flow regime involved digital modeling of steady- and nonsteady-state conditions. The steady-state model, GWFLOW, computes the head response in an aquifer due to various boundary conditions. The nonsteady-state model, SUPERMOCK, was designed to simulate transient stress and response in an alluvial-flow system. In addition to the simulation models several computer programs were developed during the study to aid in the preparation of field data for input to the models and in the calibration of the models. Calibration techniques unique to each of the models were developed for the investigation. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri79114","usgsCitation":"Ludwig, A.H., and Terry, J.E., 1980, Methods and applications of digital-model simulation of the Red River alluvial aquifer: Shreveport to the mouth of the Black River, Louisiana: U.S. Geological Survey Water-Resources Investigations Report 79-114, vi, 103 p. , https://doi.org/10.3133/wri79114.","productDescription":"vi, 103 p. ","costCenters":[],"links":[{"id":159194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0114/report-thumb.jpg"},{"id":369020,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","city":"Shreveport","otherGeospatial":"Black River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.8507080078125,\n 31.6042705179912\n ],\n [\n -91.77703857421875,\n 31.6042705179912\n ],\n [\n -91.77703857421875,\n 32.55144352864431\n ],\n [\n -93.8507080078125,\n 32.55144352864431\n ],\n [\n -93.8507080078125,\n 31.6042705179912\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a091","contributors":{"authors":[{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199881,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terry, J. E.","contributorId":87930,"corporation":false,"usgs":true,"family":"Terry","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199882,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24511,"text":"ofr801057 - 1980 - Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","interactions":[{"subject":{"id":24511,"text":"ofr801057 - 1980 - Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","indexId":"ofr801057","publicationYear":"1980","noYear":false,"title":"Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":60855,"text":"mf1483A - 1983 - Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado","indexId":"mf1483A","publicationYear":"1983","noYear":false,"chapter":"A","title":"Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado"},"id":1}],"supersededBy":{"id":60855,"text":"mf1483A - 1983 - Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado","indexId":"mf1483A","publicationYear":"1983","noYear":false,"title":"Mineral resource potential and geologic map of the Powderhorn Wilderness study area and Cannibal Plateau Roadless Area, Gunnison and Hinsdale counties, Colorado"},"lastModifiedDate":"2023-06-05T19:52:40.220456","indexId":"ofr801057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1057","title":"Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado","docAbstract":"

The Powderhorn Instant Study Area covers approximately 51,000 acres of land under BLM administration located about 80 km (50 mi) southwest of Gunnison, Colorado. A mineral resource survey, made in 1979 by the U.S. Geological Survey and the U.S. Bureau of Mines, indicates that both the mineral potential and the energy potential for the Powderhorn Instant Study Area are low. This report is based on geologic and geochemical investigations, examination of prospects, and an aeromagnetic survey. Spectrographic analyses were made of approximately 120 stream-sediment and rock samples. No mining districts are located within the study area.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801057","issn":"0094-9140","usgsCitation":"Sharp, W.N., Martin, R., and Lane, M., 1980, Preliminary report on the mineral resources of the Powderhorn Instant study area, Gunnison and Hinsdale counties, Colorado: U.S. Geological Survey Open-File Report 80-1057, Report: ii, 4 p.; 3 Plates: 35.83 x 51.26 inches or smaller, https://doi.org/10.3133/ofr801057.","productDescription":"Report: ii, 4 p.; 3 Plates: 35.83 x 51.26 inches or smaller","costCenters":[],"links":[{"id":417771,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417770,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417769,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1057/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417768,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156570,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1057/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Gunnison County, Hinsdale County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.3,37.916666666666664 ], [ -107.3,38.333333333333336 ], [ -107,38.333333333333336 ], [ -107,37.916666666666664 ], [ -107.3,37.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c7ef","contributors":{"authors":[{"text":"Sharp, William N.","contributorId":18751,"corporation":false,"usgs":true,"family":"Sharp","given":"William","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":192055,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, R.A.","contributorId":53379,"corporation":false,"usgs":true,"family":"Martin","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":874635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":192056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24547,"text":"ofr80836 - 1980 - Mineral resources of the Humbug Spires Instant Study Area, (primitive area and adjacent roadless areas), Silver Bow County, Montana","interactions":[],"lastModifiedDate":"2021-08-27T19:18:17.719053","indexId":"ofr80836","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-836","title":"Mineral resources of the Humbug Spires Instant Study Area, (primitive area and adjacent roadless areas), Silver Bow County, Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80836","issn":"0094-9140","usgsCitation":"Smedes, H.W., Hanna, W.F., and Hamilton, M., 1980, Mineral resources of the Humbug Spires Instant Study Area, (primitive area and adjacent roadless areas), Silver Bow County, Montana: U.S. Geological Survey Open-File Report 80-836, Report: ii, 25 p.; 3 Plates: 38.04 × 33.49 inches or smaller, https://doi.org/10.3133/ofr80836.","productDescription":"Report: ii, 25 p.; 3 Plates: 38.04 × 33.49 inches or smaller","costCenters":[],"links":[{"id":388611,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11794.htm"},{"id":53596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0836/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53595,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0836/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53594,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0836/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53593,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0836/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0836/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Silver Bow County","otherGeospatial":"Humbug Spires Instant Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.567,\n 45.8440\n ],\n [\n -112.75,\n 45.8440\n ],\n [\n -112.75,\n 45.7000\n ],\n [\n -112.567,\n 45.7000\n ],\n [\n -112.567,\n 45.8440\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685092","contributors":{"authors":[{"text":"Smedes, Harry Wynn","contributorId":41416,"corporation":false,"usgs":true,"family":"Smedes","given":"Harry","email":"","middleInitial":"Wynn","affiliations":[],"preferred":false,"id":192129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanna, William F.","contributorId":104045,"corporation":false,"usgs":true,"family":"Hanna","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":192130,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamilton, Michael","contributorId":23972,"corporation":false,"usgs":true,"family":"Hamilton","given":"Michael","affiliations":[],"preferred":false,"id":192128,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24525,"text":"ofr80403 - 1980 - Hydrologic setting of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2022-09-15T18:12:26.459915","indexId":"ofr80403","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-403","title":"Hydrologic setting of Williams Lake, Hubbard County, Minnesota","docAbstract":"

The hydrology and geology of Williams Lake watershed was studied to evaluate the accuracy of various methods used to determine precipitation and evaporation in lake water-balance studies and to define a lake and ground-water system according to approaches suggested by theoretical modeling studies. Regression analysis between estimated and measured precipitation at the lake showed that the accuracy of regionalization techniques is dependent on the closeness of the data network to the lake. For individual storms, the average-value method was found to be better than either the weighted average or isohyetal methods of determining precipitation, but it was least accurate in estimating 14-day average precipitation. The amount of evaporation calculated by the mass-transfer method ranged from 2 to 7 inches per month from July to October 1978, depending on the method used to determine the mass-transfer coefficient. Test drilling indicated that 30 to 150 feet of sand and gravel overlies till in the Williams Lake watershed. A sand lens about 50 feet thick occurs within the till.

\n

The configuration of the water table and vertical-head gradients measured from July to December 1978 indicate that ground water moves into the lake from the south and east and moves from the lake into the ground-water reservoir to the west. Preliminary numerical models indicate that the sand lens within the till is effectively isolated from the flow system interacting with the lake and that both inseepage and outseepage were about 1.4 inches from mid-July to mid-October 1978. When estimated as a residual in a water balance, ground water showed a net outseepage only of 1.47 inches.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr80403","collaboration":"Prepared in cooperation with Minnesota Department of Natural* Resources Division of Waters","usgsCitation":"Siegel, D., and Winter, T.C., 1980, Hydrologic setting of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Open-File Report 80-403, vii, 56 p., https://doi.org/10.3133/ofr80403.","productDescription":"vii, 56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":53576,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0403/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406774,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25793.htm"},{"id":156479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0403/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Hubbard County","otherGeospatial":"Williams Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.67845916748047,\n 46.948152929705195\n ],\n [\n -94.66163635253906,\n 46.948152929705195\n ],\n [\n -94.66163635253906,\n 46.959870280492964\n ],\n [\n -94.67845916748047,\n 46.959870280492964\n ],\n [\n -94.67845916748047,\n 46.948152929705195\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60547b","contributors":{"authors":[{"text":"Siegel, Donald I.","contributorId":97499,"corporation":false,"usgs":true,"family":"Siegel","given":"Donald I.","affiliations":[],"preferred":false,"id":192082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24606,"text":"ofr80512 - 1980 - Quaternary stream terraces in the northwestern Sacramento Valley, Glenn, Tehama, and Shasta counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"ofr80512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-512","title":"Quaternary stream terraces in the northwestern Sacramento Valley, Glenn, Tehama, and Shasta counties, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80512","issn":"0094-9140","usgsCitation":"Steele, W., 1980, Quaternary stream terraces in the northwestern Sacramento Valley, Glenn, Tehama, and Shasta counties, California: U.S. Geological Survey Open-File Report 80-512, xi, 167 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr80512.","productDescription":"xi, 167 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":108048,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11672.htm","linkFileType":{"id":5,"text":"html"},"description":"11672"},{"id":157682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0512/report-thumb.jpg"},{"id":53657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0512/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53653,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0512/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53654,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0512/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53655,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0512/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53656,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0512/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a140","contributors":{"authors":[{"text":"Steele, William Clinton","contributorId":34890,"corporation":false,"usgs":true,"family":"Steele","given":"William Clinton","affiliations":[],"preferred":false,"id":192241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60602,"text":"mf1192B - 1980 - Interpretation of an aerial radiometric and magnetic survey of the Salmo-Priest study area (RARE E6-981 A1-981), Pend Oreille County, Washington and Boundary County, Idaho","interactions":[],"lastModifiedDate":"2018-10-03T12:05:13","indexId":"mf1192B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1192","chapter":"B","title":"Interpretation of an aerial radiometric and magnetic survey of the Salmo-Priest study area (RARE E6-981 A1-981), Pend Oreille County, Washington and Boundary County, Idaho","docAbstract":"

An aerial radiometric and magnetic survey of the Salmo-Priest study area (RARE E6-981) (index map) was made by the U.S. Geological Survey during October, 1978.  Geophysical data from the survey will be used in the assessment of the mineral-resource potential of the study area.  The Salmo-Priest area is located in northeastern Washington and northern Idaho and the north edge is the United States-Canadian boundary.  This report presents the data obtained by the survey and an interpretation of the data.

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