Surface-water data for the 1980 water year for Texas are presented in three volumes, appropriately identified as to content by river basins. Data in each volume consist of records of stage, discharge, and water quality of streams and canals; and stage, contents, and water quality of lakes and reservoirs. Also included are crest-stage and flood-hydrograph partial-record stations, reconnaissance partial-record stations, and low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. Records for a few pertinent stations in bordering States are also included. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Texas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrTX803","programNote":"Prepared in cooperation with the State of Texas and with other agencies","usgsCitation":"United States Geological Survey, 1981, Water resources data for Texas, water year 1980, Volume 3: Colorado River basin, Lavaca River basin, Guadalupe River basin, Neces River basin, Rio Grande basin, and intervening coastal basins: U.S. Geological Survey Water Data Report TX-80-3, xii, 582 p., https://doi.org/10.3133/wdrTX803.","productDescription":"xii, 582 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":184280,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/tx-80-3/report-thumb.jpg"},{"id":432451,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/tx-80-3/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc897","contributors":{"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":533074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9717,"text":"ofr81858 - 1981 - Identification of transportation route alternatives and engineering feasibility studies for Bridger-Teton National Forest, Cache Creek, and Little Granite Creek EIS data gathering and evaluation","interactions":[],"lastModifiedDate":"2025-12-08T18:09:25.527807","indexId":"ofr81858","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-858","title":"Identification of transportation route alternatives and engineering feasibility studies for Bridger-Teton National Forest, Cache Creek, and Little Granite Creek EIS data gathering and evaluation","docAbstract":"This portion of the Cache Creek-Little Granite Creek EIS Data Gathering and Evaluation Study had two central objectives.
The first was to review all land access possibilities to the NCRA Cache Creek and to the Getty-Reserve Little Granite Creek proposed drilling sites. Based on this review, the preferred access corridor to each site was selected.
The second objective was to perform a reconnaissance survey of a feasible route within the selected corridor. Soils and design data were collected for the development of cost estimates and for use in studies being performed by other disciplines.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81858","usgsCitation":"Jorgensen, P.M., 1981, Identification of transportation route alternatives and engineering feasibility studies for Bridger-Teton National Forest, Cache Creek, and Little Granite Creek EIS data gathering and evaluation: U.S. Geological Survey Open-File Report 81-858, Report: 53 p.; 2 Plates: 34.85 x 24.18 inches and 37.29 x 24.63 inches, https://doi.org/10.3133/ofr81858.","productDescription":"Report: 53 p.; 2 Plates: 34.85 x 24.18 inches and 37.29 x 24.63 inches","costCenters":[],"links":[{"id":142316,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0858/report-thumb.jpg"},{"id":495488,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0858/exhibit-C-1.pdf","text":"Exhibit C-1","linkFileType":{"id":1,"text":"pdf"}},{"id":495487,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0858/exhibit-B-1.pdf","text":"Exhibit B-1","linkFileType":{"id":1,"text":"pdf"}},{"id":495486,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0858/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Bridger-Teton National Forest, Cache Creek, Little Granite Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c76d","contributors":{"authors":[{"text":"Jorgensen, Peter M.","contributorId":67093,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160176,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7854,"text":"ofr81825 - 1981 - Quality of water and time of travel in part of Tillatoba Creek basin, Mississippi, October 1974 to September 1980","interactions":[],"lastModifiedDate":"2022-11-09T18:03:17.767903","indexId":"ofr81825","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-825","title":"Quality of water and time of travel in part of Tillatoba Creek basin, Mississippi, October 1974 to September 1980","docAbstract":"A 6-year quality of water and time-of-travel study was conducted during the construction phase of a flood-water protection and flood prevention project in a 118 square mile area of Tillatoba Creek basin in northwest Mississippi. Weekly suspended sediment, daily discharge, time of travel, nutrient, biochemical oxygen demand, bacteria and field data were collected. The study was conducted by the U.S. Geological Survey in cooperation with the U.S. Soil Conservation Service. The results of the study are presented in graphs and tables in this report without interpretation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81825","collaboration":"Prepared in cooperation with the U.S. Department of Agriculture Soil Conservation Service","usgsCitation":"Bednar, G.A., 1981, Quality of water and time of travel in part of Tillatoba Creek basin, Mississippi, October 1974 to September 1980: U.S. Geological Survey Open-File Report 81-825, vi, 87 p., https://doi.org/10.3133/ofr81825.","productDescription":"vi, 87 p.","costCenters":[],"links":[{"id":141449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0825/report-thumb.jpg"},{"id":409266,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0825/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","otherGeospatial":"Tillatoba Creek 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e0183","contributors":{"authors":[{"text":"Foose, Donald W.","contributorId":85144,"corporation":false,"usgs":true,"family":"Foose","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thagard, Martha E.","contributorId":68315,"corporation":false,"usgs":true,"family":"Thagard","given":"Martha","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":158473,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11120,"text":"ofr81946 - 1981 - Statistical data for movements on young faults of the conterminous United States; paleoseismic implications and regional earthquake forecasting","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr81946","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-946","title":"Statistical data for movements on young faults of the conterminous United States; paleoseismic implications and regional earthquake forecasting","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81946","usgsCitation":"Shaw, H.R., Gartner, A., and Lusso, F., 1981, Statistical data for movements on young faults of the conterminous United States; paleoseismic implications and regional earthquake forecasting: U.S. Geological Survey Open-File Report 81-946, iv, 377 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81946.","productDescription":"iv, 377 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0946/report-thumb.jpg"},{"id":38890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0946/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2649","contributors":{"authors":[{"text":"Shaw, H. R.","contributorId":23952,"corporation":false,"usgs":true,"family":"Shaw","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":162578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, A.E.","contributorId":48183,"corporation":false,"usgs":true,"family":"Gartner","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":162579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lusso, F.","contributorId":65853,"corporation":false,"usgs":true,"family":"Lusso","given":"F.","email":"","affiliations":[],"preferred":false,"id":162580,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7875,"text":"ofr81824 - 1981 - Rainfall-runoff hydrographs and basin characteristics data for small streams in Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr81824","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-824","title":"Rainfall-runoff hydrographs and basin characteristics data for small streams in Oklahoma","docAbstract":"Rainfall with concordant runoff events recorded at 45 gages located in drainage basins of less than 30 square miles in Oklahoma are summarized. Selected basin characteristics which relate to storm runoff are described and tabulated for each gage site summarized. A tabulation is included which identifies drainage basins that produce atypical rainfall-runoff distribution as a result of regulation by upstream flood-retention structures.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81824","usgsCitation":"Bergman, D.L., and Huntzinger, T.L., 1981, Rainfall-runoff hydrographs and basin characteristics data for small streams in Oklahoma: U.S. Geological Survey Open-File Report 81-824, 323 p.; 1 over-size sheet, maps ;28 cm., https://doi.org/10.3133/ofr81824.","productDescription":"323 p.; 1 over-size sheet, maps ;28 cm.","costCenters":[],"links":[{"id":140383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0824/report-thumb.jpg"},{"id":35382,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0824/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0824/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633d83","contributors":{"authors":[{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huntzinger, Thomas L.","contributorId":104054,"corporation":false,"usgs":true,"family":"Huntzinger","given":"Thomas","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7927,"text":"ofr81139 - 1981 - Evaluation of ground-water monitoring network, Santa Cruz County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr81139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-139","title":"Evaluation of ground-water monitoring network, Santa Cruz County, California","docAbstract":"The Santa Cruz County Flood Control and Water Conservation District seeks to improve the existing network of observation wells to monitor water levels and ground-water quality in the Pajaro Valley subarea and the Aptos-Soquel, San Lorenzo, and Santa Cruz Coastal subbasins in California. The proposed network , consisting of 92 wells, is designed to monitor changes in storage and quality of ground water resulting from climatic changes and management-induced stresses. In the proposed network , water levels in all wells would be measured semiannually, in April and September, and monthly in a few key wells. The water-level measurements would provide data that could be used to determine changes in ground-water storage. In addition to the currently monitored characteristics--temperature, specific conductance, pH, and chloride ion concentration--inclusion of annual sampling and analysis for major ions and nutrients is proposed. The network would also include sampling and analysis for trace elements once every 4 years. More frequent analyses are proposed in areas where water-quality problems are known to exist or where potential water-quality problems are recognized. Analyses for major ions, nutrients, and trace elements are included in the proposed network to provide baseline data for monitoring long-term changes in water quality and to detect any unexpected changes in quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81139","usgsCitation":"Blankenbaker, G.G., and Farrar, C.D., 1981, Evaluation of ground-water monitoring network, Santa Cruz County, California: U.S. Geological Survey Open-File Report 81-139, iv, 24 p., 2 over-size sheets ;28 cm., https://doi.org/10.3133/ofr81139.","productDescription":"iv, 24 p., 2 over-size sheets ;28 cm.","costCenters":[],"links":[{"id":140723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0139/report-thumb.jpg"},{"id":35491,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0139/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35492,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0139/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea02","contributors":{"authors":[{"text":"Blankenbaker, G. G.","contributorId":17993,"corporation":false,"usgs":true,"family":"Blankenbaker","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, Christopher D. cdfarrar@usgs.gov","contributorId":1501,"corporation":false,"usgs":true,"family":"Farrar","given":"Christopher","email":"cdfarrar@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":156848,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28255,"text":"wri8135 - 1981 - Ground-water resources of the White River basin, Madison County, Indiana","interactions":[],"lastModifiedDate":"2020-11-04T18:03:15.372006","indexId":"wri8135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-35","title":"Ground-water resources of the White River basin, Madison County, Indiana","docAbstract":"The ground-water resources of the White River basin in and near Madison County, Indiana, were investigated by mapping the aquifers, estimating their hydraulic properties, determining the distribution of potentiometric head in the aquifers, and estimating some of the components of the ground-water budget from data collected in the field. This information was used to construct and calibrate a five-layer, digital ground-water flow model. The model, constructed and calibrated to ground-water-level and seepage data collected during the study, simulates conditions for the autumn of 1976. The model was used to provide estimates of ground-water potential in terms of yield, drawdown, and depletion in streamflow.
Glacial drift covers nearly the entire study area and ranges in thickness from 0 to approximately 300 feet. Beneath the drift lie Ordovician to Devonian limestone, dolomite, and shale. A bedrock valley trends west-northwest through the center of the study area. Relief of the bedrock surface is approximately 325 feet.
Four confined sand and gravel aquifers interbedded in the glacial drift, a bedrock aquifer, and an unconfined outwash aquifer are the three most important aquifer systems in the study area. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers have an average thickness of about 15 feet and an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying the entire study area has a thick-ness estimated to be 150 feet and an average transmissivity estimated in previous studies in the basin to be 1,340 square feet per day. The unconfined outwash aquifer, although thin and narrow, is an important aquifer because of its proximity to sources of induced recharge.
Water-level fluctuations in observation wells in the basin indicate that the ground-water system is in dynamic equilibrium. Ground-water seepage to streams at 90-percent flow duration on October 1, 1976, was estimated to be between 15.9 and 74.4 cubic feet per second. Ground-water pumpage for 1976 was estimated to be 19.7 million gallons per day (30.5 cubic feet per second). The water budget, as simulated in the model, indicates that the rate of inflow to the ground-water system in the modeled area is 92.4 cubic feet per second. Of this, 78 percent is from effective areal recharge of precipitation, and 22 percent is from ground-water flow across the boundaries into the study area. Thirty-three percent of the ground-water outflow is pumpage, 59 percent is seepage to streams, and the remaining 8 percent is ground-water flow across the boundaries out of the study area.
Model simulations of eight pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems and indicate that as much as 2.5 million gallons per day can be obtained from well fields about half a square mile in area. Model results also indicate that, for as much as 2.5-million gallons per day pumping, flow in the large streams will not be significantly affected, whereas flow in the small streams may be significantly affected. In addition, simulations indicate that adding more wells to the well field northwest of Anderson, Ind., would probably be no more advantageous than increasing the pumpage in the existing wells. How-ever, well interference, well hydraulics, and pumping-level constraints were not considered in the investigation of alternative methods of expanding the well field. In developing the ground-water system in the area, use of many small, scattered well fields that produce less than about 3 million gallons per day may be more favorable hydrologically than a few, heavily pumped well fields.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8135","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Lapham, W.W., 1981, Ground-water resources of the White River basin, Madison County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-35, vii, 112 p., https://doi.org/10.3133/wri8135.","productDescription":"vii, 112 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0035/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Madison","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.5784,40.3794],[-85.5763,40.0769],[-85.5774,39.9459],[-85.8624,39.9436],[-85.863,40.139],[-85.8617,40.2201],[-85.8621,40.3784],[-85.5784,40.3794]]]},\"properties\":{\"name\":\"Madison\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64931a","contributors":{"authors":[{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61504,"text":"mf1302 - 1981 - Map showing paleontological control of Paleozoic stratigraphy in New England","interactions":[],"lastModifiedDate":"2018-10-22T12:59:33","indexId":"mf1302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1302","title":"Map showing paleontological control of Paleozoic stratigraphy in New England","docAbstract":"Assignment of Phanerozoic stratigraphic units to their proper place in the geologica time scale is based primarily on paleontology. Radiometric methods are becoming increasingly important (Naylor, 1976), particularly where paleontological data are lacking. This map and text are concerned only with the paleontological data bearing on the Paleozoic stratigraphy of New England.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1302","usgsCitation":"Billings, M.P., and Lyttle, P.T., 1981, Map showing paleontological control of Paleozoic stratigraphy in New England: U.S. Geological Survey Miscellaneous Field Studies Map 1302, 39.35 x 47.23 inches, https://doi.org/10.3133/mf1302.","productDescription":"39.35 x 47.23 inches","costCenters":[],"links":[{"id":180285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1302/report-thumb.jpg"},{"id":358615,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1302/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"754000","country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74,\n 41\n ],\n [\n -66,\n 41\n ],\n [\n -66,\n 47.5\n ],\n [\n -74,\n 47.5\n ],\n [\n -74,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a377a","contributors":{"authors":[{"text":"Billings, Marland P.","contributorId":206889,"corporation":false,"usgs":false,"family":"Billings","given":"Marland","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":265833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyttle, Peter T. plyttle@usgs.gov","contributorId":293,"corporation":false,"usgs":true,"family":"Lyttle","given":"Peter","email":"plyttle@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":265834,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27976,"text":"wri8050 - 1981 - Kriging analysis of mean annual precipitation, Powder River Basin, Montana and Wyoming","interactions":[],"lastModifiedDate":"2019-07-09T12:33:49","indexId":"wri8050","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-50","title":"Kriging analysis of mean annual precipitation, Powder River Basin, Montana and Wyoming","docAbstract":"Kriging is a statistical estimation technique for regionalized variables which exhibit an autocorrelation structure. Such structure can be described by a semi-variogram of the observed data. The kriging estimate at any point is a weighted average of the data, where the weights are determined using the semi-variogram and an assumed drift, or lack of drift, in the data. Block, or areal, estimates can also be calculated. The kriging algorithm, based on unbiased and minimum-variance estimates, involves a linear system of equations to calculate the weights. Kriging variances can then be used to give confidence intervals of the resulting estimates. Mean annual precipitation in the Powder River basin, Montana and Wyoming, is an important variable when considering restoration of coal-strip-mining lands of the region. Two kriging analyses involving data at 60 stations were made--one assuming no drift in precipitation, and one a partial quadratic drift simulating orographic effects. Contour maps of estimates of mean annual precipitation were similar for both analyses, as were the corresponding contours of kriging variances. Block estimates of mean annual precipitation were made for two subbasins. Runoff estimates were 1-2 percent of the kriged block estimates. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8050","usgsCitation":"Karlinger, M., and Skrivan, J.A., 1981, Kriging analysis of mean annual precipitation, Powder River Basin, Montana and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 80-50, iv, 25 p. , https://doi.org/10.3133/wri8050.","productDescription":"iv, 25 p. ","costCenters":[],"links":[{"id":365382,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0050/report-thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"Powder River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.75390625,\n 43.8186748554532\n ],\n [\n -105.22705078125,\n 43.8186748554532\n ],\n [\n -105.22705078125,\n 46.027481852486645\n ],\n [\n -107.75390625,\n 46.027481852486645\n ],\n [\n -107.75390625,\n 43.8186748554532\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b450a","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":198996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skrivan, James A.","contributorId":106869,"corporation":false,"usgs":true,"family":"Skrivan","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198997,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28193,"text":"wri8141 - 1981 - Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T12:41:41","indexId":"wri8141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-41","title":"Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota","docAbstract":"A limnological and geochemical survey of Williams Lake, Minnesota, was made in 1979 to provide an initial interpretive description of the lake and the contiguous ground-water system. This survey was made as part of a continuing research program related to the investigation of the interaction of lakes and their contiguous ground-water systems at Williams Lake, Minnesota, as well as other sites within the continental United States.
\nDuring 1979, Williams Lake was dimictic, and the lake had high optical transparency; light penetrated to the lakebed throughout most of the lake. Aquatic macrophytes were present along the western shore and in the southern bay of the lake. Although the lake had clinograde-oxygen distributions during part of this survey, anaerobic conditions were not observed. The lake is moderately fertile with respect to its total phosphorus content. Nutrient data indicate phosphorus limits phytoplankton biomass levels in Williams Lake. Blue-green algae were the dominant group of the phytoplankton community and copepods were the dominant group of the zooplankton community when the lake was thermally stratified during the open-water season. Diatoms and rotifers were dominant when the lake was isothermal in the autumn.
\nCalcium and bicarbonate represent more than 90 percent of the dissolved constituents in Williams Lake and the contiguous ground-water system. Major mineralogical constituents of the lake sediments are quartz, dolomite, and calcite. Marl is present only in the littoral zone of the lake. Organic sediments in the lake consist of loose organic floe and gyttja.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wri8141","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"LaBaugh, J.W., Groschen, G., and Winter, T.C., 1981, Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 81-41, v, 38 p., https://doi.org/10.3133/wri8141.","productDescription":"v, 38 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":119026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0041/report-thumb.jpg"},{"id":57031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Williams Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5226","contributors":{"authors":[{"text":"LaBaugh, J. W.","contributorId":23484,"corporation":false,"usgs":true,"family":"LaBaugh","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Groschen, G.E.","contributorId":17260,"corporation":false,"usgs":true,"family":"Groschen","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":199370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":199372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7559,"text":"ofr81749 - 1981 - Summary report on the regional geology, environmental considerations for development, petroleum potential, and estimates of undiscovered recoverable oil and gas resources of the United States southeastern Atlantic continental margin in the area of proposed oil and gas lease sale No. 78","interactions":[],"lastModifiedDate":"2018-03-13T16:56:36","indexId":"ofr81749","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-749","title":"Summary report on the regional geology, environmental considerations for development, petroleum potential, and estimates of undiscovered recoverable oil and gas resources of the United States southeastern Atlantic continental margin in the area of proposed oil and gas lease sale No. 78","docAbstract":"This report summarizes our general knowledge of the geology and petroleum potential, as well as potential problems and hazards associated with development of petroleum resources, of the area proposed for nominations for lease sale number 78. This area includes the U.S. eastern continental margin from the mouth of Chesapeake Bay to approximately Cape Canaveral, Florida, including the upper Continental Slope and inner Blake Plateau. The area for possible sales and the previous areas leased are shown in figure 1; physiographic features of the region are shown in figure 2.
Six exploration wells have been drilled within the proposed lease area (figs. 3 and 4) but no commercial discoveries have been made. All six wells were drilled on the Continental Shelf in the Southeast Georgia Embayment. No commercial production has been obtained onshore in the region. The areas already drilled have thin sedimentary sections, and the deeper rocks are dominantly continental facies. Petroleum formation may have been hindered by a lack of organic material and sufficient burial for thermal maturation. Analysis of drill and seismic profiling data presented here, however, indicates that a much thicker sedimentary rock section containing a much higher proportion of marine deposits exists seaward of the exploratory wells on the Continental Shelf. These geologic conditions imply that the offshore basins may be more favorable environments for generating petroleum.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81749","usgsCitation":"Dillon, W.P., 1981, Summary report on the regional geology, environmental considerations for development, petroleum potential, and estimates of undiscovered recoverable oil and gas resources of the United States southeastern Atlantic continental margin in the area of proposed oil and gas lease sale No. 78: U.S. Geological Survey Open-File Report 81-749, ii, 115 p., https://doi.org/10.3133/ofr81749.","productDescription":"ii, 115 p.","costCenters":[],"links":[{"id":140790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0749/report-thumb.jpg"},{"id":35019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0749/report.pdf","text":"Report","size":"20.09 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698744","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":156119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8280,"text":"ofr81662 - 1981 - Handling, storage, and retrieval of petroleum data in CCOP countries (revised)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr81662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-662","title":"Handling, storage, and retrieval of petroleum data in CCOP countries (revised)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81662","usgsCitation":"Clark, A.L., Cook, J.L., and Sinding-Larsen, R., 1981, Handling, storage, and retrieval of petroleum data in CCOP countries (revised): U.S. Geological Survey Open-File Report 81-662, iii, 210 p. ill. ;28 cm., https://doi.org/10.3133/ofr81662.","productDescription":"iii, 210 p. ill. ;28 cm.","costCenters":[],"links":[{"id":140746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0662/report-thumb.jpg"},{"id":35892,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64852a","contributors":{"authors":[{"text":"Clark, Allen L.","contributorId":96258,"corporation":false,"usgs":true,"family":"Clark","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, Jennifer L.","contributorId":66255,"corporation":false,"usgs":true,"family":"Cook","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157485,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sinding-Larsen, Richard","contributorId":77927,"corporation":false,"usgs":true,"family":"Sinding-Larsen","given":"Richard","email":"","affiliations":[],"preferred":false,"id":157486,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4055,"text":"cir801 - 1981 - Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","interactions":[],"lastModifiedDate":"2020-09-27T17:48:12.680465","indexId":"cir801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"801","title":"Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","docAbstract":"In 1960, the U.S. Geological Survey and the Kentucky Geological Survey began a program to map the State geologically at a scale of 1:24,000 and to publish the maps as 707 U.S. Geological Survey Geologic Quadrangle Maps. Fieldwork was completed by the spring of 1977, and all maps were published by December 1978. \r\n\r\nGeologic mapping of the State was proposed by the Kentucky Society of Professional Engineers in 1959. Wallace W. Hagan, Director and State Geologist of the Kentucky Geological Survey, and Preston McGrain, Assistant State Geologist, promoted support for the proposal among organizations such as Chambers of Commerce, industrial associations, professional societies, and among members of the State government. It was also arranged for the U.S. Geological Survey to supply mapping personnel and to publish the maps; the cost would be shared equally by the two organizations. \r\n\r\nMembers of the U.S. Geological Survey assigned to the program were organized as the Branch of Kentucky Geology. Branch headquarters, including an editorial staff, was at Lexington, Ky., but actual mapping was conducted from 18 field offices distributed throughout the State. The Publications Division of the U.S. Geological Survey established a cartographic office at Lexington to prepare the maps for publication. \r\n\r\nAbout 260 people, including more than 200 professionals, were assigned to the Branch of Kentucky Geology by the U.S. Geological Survey at one time or another. The most geologists assigned any one year was 61. To complete the mapping and ancillary studies, 661 professional man-years were required, compared with an original estimate of 600 man-years. \r\n\r\nA wide variety of field methods were used, but most geologists relied on the surveying altimeter to obtain elevations. Surface data were supplemented by drill-hole records, and several dozen shallow diamond-drill holes were drilled to aid the mapping. Geologists generally scribed their own maps, with a consequent saving of publication costs. \r\n\r\nPaleontologists and stratigraphers of the U.S. Geological Survey cooperated closely with the program. Paleontologic studies were concentrated in the Ordovician of central Kentucky, the Pennsylvanian of eastern and western Kentucky, and the Mesozoic and Cenozoic of westernmost Kentucky. \r\n\r\nIn addition to financial support, the Kentucky Geological Survey provided economic data, stratigraphic support, and drillhole records to the field offices. Geologists of the State Survey made subsurface structural interpretations, constructed bedrock topography maps, and mapped several quadrangles. \r\n\r\nSome of the problems encountered were the inadequacy of much of the existing stratigraphic nomenclature, the uneven quality of some of the mapping, and the effects of relative isolation on the professional development of some of the geologists. \r\n\r\nThe program cost a total of $20,927,500. In terms of 1960 dollars, it cost $16,035,000; this compares with an original estimate of $12,000,000. Although it is difficult to place a monetary value on the geologic mapping, the program has contributed to newly discovered mineral wealth, jobs, and money saved by government and industry. The maps are used widely in the exploration for coal, oil and gas, fluorspar, limestone, and clay. The maps are also used in planning highways and locations of dams, in evaluating foundation and excavation conditions, in preparing environmental impact statements, and in land-use planning.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir801","usgsCitation":"Cressman, E.R., and Noger, M.C., 1981, Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978: U.S. Geological Survey Circular 801, iii, 22 p., https://doi.org/10.3133/cir801.","productDescription":"iii, 22 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688648","contributors":{"authors":[{"text":"Cressman, Earle Rupert","contributorId":43324,"corporation":false,"usgs":true,"family":"Cressman","given":"Earle","email":"","middleInitial":"Rupert","affiliations":[],"preferred":false,"id":148081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noger, Martin C.","contributorId":38970,"corporation":false,"usgs":true,"family":"Noger","given":"Martin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":148080,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61500,"text":"mf1214B - 1981 - Mineral resource potential of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning (RARE II) Areas, Modoc, Shasta, and Siskiyou Counties, California","interactions":[],"lastModifiedDate":"2018-12-06T15:26:34","indexId":"mf1214B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1214","chapter":"B","title":"Mineral resource potential of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning (RARE II) Areas, Modoc, Shasta, and Siskiyou Counties, California","docAbstract":"In accordance with the provisions of the Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976), the Geological Survey and the Bureau of Mines have conducted mineral surveys on certain areas, which formally had been identified as \"natural\" and \"primitive\" areas prior to November 1, 1975.
The Wilderness Act (Public Law 88-577, September 3, 1964) and related Acts, r equire the Geological Survey and the Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and be submitted to the Administration and the Congress. These maps and reports present the results of a geological and mineral survey of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning (RARE II) areas.
The study areas have no potential for metallic commodities as determined from spectrographic analyses of rocks (Peterson, 1980). Several localities within the study areas, however, contain stone that can be used for decorative purposes in building construction . The study areas may also have geothermal potential, but at this time quantitative data are unavailable.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1214B","usgsCitation":"Peterson, J.A., Martin, L., Esparza, L.E., and Cwick, G.J., 1981, Mineral resource potential of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning (RARE II) Areas, Modoc, Shasta, and Siskiyou Counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1214, 24.73 x 28.50 inches, https://doi.org/10.3133/mf1214B.","productDescription":"24.73 x 28.50 inches","costCenters":[],"links":[{"id":180222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1214-B/report-thumb.jpg"},{"id":360000,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1214-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","county":"Modoc County, Shasta County, Siskiyou County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.5,41.083333333333336 ], [ -121.5,41.25 ], [ -121.33333333333333,41.25 ], [ -121.33333333333333,41.083333333333336 ], [ -121.5,41.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6275ae","contributors":{"authors":[{"text":"Peterson, Jocelyn A.","contributorId":13954,"corporation":false,"usgs":true,"family":"Peterson","given":"Jocelyn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":265826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, L.M.","contributorId":19224,"corporation":false,"usgs":true,"family":"Martin","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":265824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Esparza, L. E.","contributorId":72848,"corporation":false,"usgs":true,"family":"Esparza","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":265825,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cwick, Gary J.","contributorId":86022,"corporation":false,"usgs":true,"family":"Cwick","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265827,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7964,"text":"ofr81842 - 1981 - Chemical analyses of selected agricultural soils of Missouri","interactions":[],"lastModifiedDate":"2025-09-15T18:00:43.340655","indexId":"ofr81842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-842","title":"Chemical analyses of selected agricultural soils of Missouri","docAbstract":"This report contains a compilation of chemical data for samples of the plow zone of agricultural soils that were collected in 1970 from each of the 114 counties of the State of Missouri. Most of the principal taxonomic soil types that occur in each county are represented by the 10 samples per county that were collected. There are numerous examples of soils that were developed from each of the several parent-material types in the State.
Each soil sample is a composite of several channel samples collected throughout a field from a depth 0-15cm. Soil material that passed a 2mm sieve was ground in a ceramic mill to -100 mesh and then analyzed for total concentrations of 70 elements. The methods of analysis and the lower limits of determination for each element are given in table 1. Most methods were described by Miesch (1976); delayed neutron counting for uranium and thorium was described by Millard (1976). The limits of determination for the methods did not always encompass the natural range of element concentrations in some samples, thus the elements may be classed into three groups: never detected, rarely detected, and frequently detected.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81842","usgsCitation":"Boerngen, J.G., and Tidball, R.R., 1981, Chemical analyses of selected agricultural soils of Missouri: U.S. Geological Survey Open-File Report 81-842, i, 125 p., https://doi.org/10.3133/ofr81842.","productDescription":"i, 125 p.","costCenters":[],"links":[{"id":140251,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0842/report-thumb.jpg"},{"id":495527,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0842/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.545006,36.336809],[-89.605668,36.342234],[-89.615841,36.336085],[-89.620255,36.323006],[-89.611819,36.309088],[-89.578492,36.288317],[-89.554289,36.277751],[-89.539487,36.277368],[-89.534507,36.261802],[-89.539229,36.248821],[-89.562206,36.250909],[-89.577544,36.242262],[-89.602374,36.238106],[-89.642182,36.249486],[-89.678046,36.248284],[-89.695235,36.252766],[-89.705328,36.239898],[-89.69263,36.224959],[-89.607004,36.171179],[-89.591605,36.144096],[-89.59307,36.129699],[-89.601936,36.11947],[-89.666598,36.095802],[-89.678821,36.084636],[-89.688577,36.029238],[-89.706932,36.000981],[-90.37789,35.995683],[-90.351732,36.025347],[-90.34909,36.040131],[-90.339343,36.047112],[-90.333261,36.067504],[-90.320746,36.071326],[-90.320662,36.087138],[-90.29991,36.098236],[-90.294492,36.112949],[-90.266256,36.120559],[-90.235585,36.139474],[-90.231386,36.147348],[-90.23537,36.159153],[-90.220425,36.184764],[-90.21128,36.183392],[-90.188189,36.20536],[-90.152497,36.215582],[-90.14224,36.227522],[-90.126366,36.229367],[-90.130114,36.240307],[-90.118219,36.253491],[-90.114922,36.265595],[-90.086471,36.271531],[-90.06398,36.303038],[-90.081961,36.322097],[-90.074074,36.342895],[-90.077695,36.348478],[-90.066297,36.3593],[-90.064514,36.382085],[-90.078671,36.399116],[-90.138512,36.413952],[-90.134231,36.422827],[-90.143743,36.424433],[-90.143798,36.428483],[-90.134136,36.436602],[-90.137323,36.455411],[-90.141101,36.461791],[-90.155804,36.463555],[-90.152888,36.47093],[-90.142222,36.470554],[-90.143683,36.476029],[-90.158838,36.479558],[-90.159305,36.492446],[-90.152481,36.497952],[-94.617919,36.499414],[-94.617975,37.722176],[-94.607354,39.113444],[-94.589933,39.140403],[-94.591933,39.155003],[-94.608834,39.160503],[-94.640035,39.153103],[-94.662435,39.157603],[-94.663835,39.179103],[-94.680336,39.184303],[-94.714137,39.170403],[-94.741938,39.170203],[-94.763138,39.179903],[-94.781518,39.206146],[-94.811663,39.206594],[-94.831679,39.215938],[-94.835056,39.220658],[-94.825663,39.241729],[-94.831471,39.256273],[-94.84632,39.268481],[-94.887056,39.28648],[-94.905329,39.311952],[-94.910017,39.352543],[-94.88136,39.370383],[-94.879281,39.37978],[-94.885026,39.389801],[-94.901823,39.392798],[-94.92311,39.384492],[-94.942039,39.389499],[-94.946293,39.405646],[-94.972952,39.421705],[-94.982144,39.440552],[-95.0375,39.463689],[-95.045716,39.472459],[-95.052177,39.499996],[-95.082714,39.516712],[-95.109304,39.542285],[-95.113077,39.559133],[-95.103228,39.577783],[-95.089515,39.581028],[-95.064519,39.577115],[-95.049277,39.589583],[-95.046361,39.599557],[-95.055152,39.621657],[-95.053367,39.630347],[-95.027644,39.665454],[-95.018318,39.672869],[-94.984149,39.67785],[-94.971317,39.68641],[-94.971206,39.729305],[-94.965318,39.739065],[-94.948726,39.745593],[-94.902612,39.724202],[-94.875643,39.730494],[-94.862943,39.742994],[-94.860743,39.763094],[-94.869644,39.772894],[-94.912293,39.759338],[-94.934262,39.773642],[-94.935206,39.78313],[-94.929654,39.788282],[-94.884084,39.794234],[-94.875944,39.813294],[-94.878677,39.826522],[-94.886933,39.833098],[-94.916918,39.836138],[-94.942567,39.856602],[-94.928466,39.876344],[-94.929574,39.888754],[-94.95154,39.900533],[-94.986975,39.89667],[-95.00844,39.900596],[-95.024389,39.891202],[-95.027931,39.871522],[-95.037767,39.865542],[-95.085003,39.861883],[-95.128166,39.874165],[-95.140601,39.881688],[-95.143802,39.901918],[-95.149657,39.905948],[-95.179453,39.900062],[-95.199347,39.902709],[-95.206326,39.912121],[-95.20069,39.928155],[-95.204428,39.938949],[-95.250254,39.948644],[-95.269886,39.969396],[-95.302507,39.984357],[-95.315271,40.01207],[-95.356876,40.031522],[-95.387195,40.02677],[-95.40726,40.033112],[-95.416824,40.043235],[-95.42164,40.058952],[-95.409856,40.07432],[-95.407591,40.09803],[-95.394216,40.108263],[-95.39284,40.115887],[-95.398667,40.126419],[-95.428749,40.135577],[-95.436348,40.15872],[-95.460746,40.169173],[-95.479193,40.185652],[-95.482757,40.197346],[-95.469718,40.227908],[-95.477501,40.24272],[-95.490333,40.248966],[-95.521925,40.24947],[-95.552473,40.261904],[-95.556325,40.267714],[-95.550966,40.285947],[-95.562157,40.297359],[-95.581787,40.29958],[-95.610439,40.31397],[-95.642262,40.306025],[-95.657328,40.310856],[-95.653729,40.322582],[-95.625204,40.334288],[-95.623728,40.346567],[-95.641027,40.366399],[-95.643934,40.386849],[-95.659134,40.40869],[-95.65819,40.44188],[-95.693133,40.469396],[-95.699969,40.505275],[-95.661687,40.517309],[-95.652262,40.538114],[-95.655848,40.546609],[-95.671754,40.562626],[-95.678718,40.56256],[-95.694147,40.556942],[-95.69505,40.533124],[-95.708591,40.521551],[-95.722444,40.528118],[-95.75711,40.52599],[-95.769281,40.536656],[-95.763366,40.550797],[-95.773549,40.578205],[-95.765645,40.585208],[-94.632035,40.571186],[-94.080463,40.572899],[-92.689854,40.589884],[-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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a28","contributors":{"authors":[{"text":"Boerngen, Josephine G.","contributorId":31750,"corporation":false,"usgs":true,"family":"Boerngen","given":"Josephine","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tidball, Ronald R.","contributorId":12032,"corporation":false,"usgs":true,"family":"Tidball","given":"Ronald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7564,"text":"ofr811111 - 1981 - Surface-water and climatological data, Salt Lake County, Utah, water year 1980","interactions":[],"lastModifiedDate":"2022-04-12T17:17:10.855478","indexId":"ofr811111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1111","title":"Surface-water and climatological data, Salt Lake County, Utah, water year 1980","docAbstract":"This report presents streamflow, water-quality, precipitation, and storm-runoff data collected in Salt Lake County, Utah, during the 1980 water year and certain water-quality data for the 1979 water year which were included for comparative purposes. Surface-water data consist of daily mean values of flow at 33 sites on natural streams, canals, and conduits. Water-quality data consist of chemical, biologic, and sediment analyses at 30 sites. Precipitation data consist of daily and monthly total at nine sites. Storm-runoff data consist of 5 and 15-minute interval discharge data for storms of July 1-2, August 19, and August 25, 1980, for most surface-water sites.
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York\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f248e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532445,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29976,"text":"wri8133 - 1981 - Water type and suitability of Oklahoma surface waters for public supply and irrigation; Part I, Arkansas river mainstem and Verdigris, Neosho, and Illinois river basins through 1978","interactions":[],"lastModifiedDate":"2018-11-08T15:54:31","indexId":"wri8133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-33","title":"Water type and suitability of Oklahoma surface waters for public supply and irrigation; Part I, Arkansas river mainstem and Verdigris, Neosho, and Illinois river basins through 1978","docAbstract":"Water-quality data in the Arkansas River mainstem and the Verdigris, Neosho, and Illnois River basins are examined for water type and suitability for public water supply and for irrigation use. The classification of water type is based on the relation of the major ions -- calcium, magnesium, sodium, bicarbonate/carbonate, sulfate, and chloride -- to each other within the range of measured specific conductance. The evaluation of suitability for use as a public supply is based on the concentration levels and distribution of selected constituents. The Wilcox irrigation classification scheme is used to relate sodium concentrations and the salinity distribution to the use of the water for irrigation. The possibility of boron phytotoxic effects is discussed where data are available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8133","usgsCitation":"Stoner, J.D., 1981, Water type and suitability of Oklahoma surface waters for public supply and irrigation; Part I, Arkansas river mainstem and Verdigris, Neosho, and Illinois river basins through 1978: U.S. Geological Survey Water-Resources Investigations Report 81-33, v, 297 p., https://doi.org/10.3133/wri8133.","productDescription":"v, 297 p.","numberOfPages":"309","costCenters":[],"links":[{"id":359353,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160164,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0033/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98,\n 34.5\n ],\n [\n -94.4384765625,\n 34.5\n ],\n [\n -94.4384765625,\n 37\n ],\n [\n -98,\n 37\n ],\n [\n -98,\n 34.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d1e4b07f02db547639","contributors":{"authors":[{"text":"Stoner, Jerry D.","contributorId":38611,"corporation":false,"usgs":true,"family":"Stoner","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":202468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10872,"text":"ofr811328 - 1981 - Description of mid-range sidescan-sonar data from the continental slope, offshore New Jersey, collected by R. V. Gyer, cruise 80-G-8A","interactions":[],"lastModifiedDate":"2025-07-29T18:16:15.985482","indexId":"ofr811328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1328","title":"Description of mid-range sidescan-sonar data from the continental slope, offshore New Jersey, collected by R. V. Gyer, cruise 80-G-8A","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811328","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Robb, J.M., Ryan, W.B., and Hampson, J.C., 1981, Description of mid-range sidescan-sonar data from the continental slope, offshore New Jersey, collected by R. V. 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,{"id":7810,"text":"ofr81634 - 1981 - Hydrogeologic data from test drilling near Verna, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T07:16:24","indexId":"ofr81634","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-634","title":"Hydrogeologic data from test drilling near Verna, Florida, 1978","docAbstract":"Four test wells were drilled in the vicinity of the city of Sarasota well field near Verna, Fla., to provide hydrologic and geologic information. An expedient and economical method of air lifting water samples from isolated water-producing zones while drilling was utilized. Lithologic logs of drill cuttings and geophysical logs, including point resistance and spontaneous potential electric logs, gamma-ray logs, and caliper logs, were made. Chemical quality of water was determined for principal producing zones at each well. Dissolved solids from composite water samples ranged from 313 milligrams per liter in test well 0-1 north of the well field to 728 milligrams per liter in test well 0-3 within the well field. Each test well was pumped to determine maximum discharge, water-level drawdown, and recovery time. A leaking pump column on test well 0-1 prevented accurate measurement of drawdown on the well. Test well 0-2, located east of the well field, had a pumping rate of 376 gallons per minute and 13.11 feet of drawdown after 3 hours and 50 minutes; test well 0-3 had a maximum yield of 320 gallons per minute, a drawdown of 31.91 feet after 2 hours and 35 minutes of pumping, had a recovery time of 20 minutes; and test well 0-4, south of the well field, had a pumping rate of 200 gallons per minute with 63.34 feet of drawdown after 2 hours and 35 minutes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81634","usgsCitation":"Barker, M., Bowman, G., and Sutcliffe, H., 1981, Hydrogeologic data from test drilling near Verna, Florida, 1978: U.S. Geological Survey Open-File Report 81-634, iii, 29 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81634.","productDescription":"iii, 29 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0634/report-thumb.jpg"},{"id":275908,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0634/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628b35","contributors":{"authors":[{"text":"Barker, Michael","contributorId":34917,"corporation":false,"usgs":true,"family":"Barker","given":"Michael","email":"","affiliations":[],"preferred":false,"id":156647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowman, Geronia","contributorId":50890,"corporation":false,"usgs":true,"family":"Bowman","given":"Geronia","email":"","affiliations":[],"preferred":false,"id":156648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":156646,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7621,"text":"ofr81664 - 1981 - Western hemisphere strong-motion accelerograph station list, 1980","interactions":[],"lastModifiedDate":"2025-09-16T13:35:52.142375","indexId":"ofr81664","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-664","title":"Western hemisphere strong-motion accelerograph station list, 1980","docAbstract":"This list contains information on western hemisphere strong-motion stations that have been installed and are maintained by many different organizations. It contains information on all of those stations for which there is some data in the files of the USGS, but the list is incomplete even for stations in the United States. Since the stations being maintained are continuously changing, it is impossible to have complete information about all of the stations at any one time. The objective is to provide the community of persons who have an interest in strong-motion programs an indication of the current status of the networks in this part of the world. The USGS also maintains a computerized Strong Motion Information Retrieval System (SMIRS) which permits searching for various types of information about the strong motion stations, records, and events (Converse, 1978). In general, the information in SMIRS is more current than the information in this list.
For convenience, the list has been arranged by country, north to south, alphabetically by states in the section for the United States, and then alphabetically by station name. Subsequent sections include a list by stations numbers, a cross-reference of obsolete station names, a cross-reference of station numbers as assigned by other agencies, and a cross-reference of three character designations for those that find that form of station designation useful. A list of the stations that were installed as required by a local building code or that are maintained by the owner of the facility appears in the Appendix. That list has not been updated since 1976 at which time the USGS stopped receiving information about new installations required by building codes.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81664","usgsCitation":"Switzer, J., Johnson, D., Maley, R., and Matthiesen, R., 1981, Western hemisphere strong-motion accelerograph station list, 1980: U.S. Geological Survey Open-File Report 81-664, 171 p., https://doi.org/10.3133/ofr81664.","productDescription":"171 p.","costCenters":[],"links":[{"id":495584,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0664/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0664/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f078b","contributors":{"authors":[{"text":"Switzer, J.","contributorId":15194,"corporation":false,"usgs":true,"family":"Switzer","given":"J.","affiliations":[],"preferred":false,"id":156317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, D.","contributorId":85955,"corporation":false,"usgs":true,"family":"Johnson","given":"D.","email":"","affiliations":[],"preferred":false,"id":156319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maley, R.","contributorId":87929,"corporation":false,"usgs":true,"family":"Maley","given":"R.","email":"","affiliations":[],"preferred":false,"id":156320,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Matthiesen, R.","contributorId":27855,"corporation":false,"usgs":true,"family":"Matthiesen","given":"R.","affiliations":[],"preferred":false,"id":156318,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11659,"text":"ofr81367 - 1981 - Ground-water level and precipitation data for slopes near La Honda, California","interactions":[],"lastModifiedDate":"2022-05-04T17:13:22.038335","indexId":"ofr81367","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-367","title":"Ground-water level and precipitation data for slopes near La Honda, California","docAbstract":"Ground water levels and precipitation were measured on a regular basis over a five-year period between October 1975 and October 1980 on two slopes near La Honda, California.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81367","usgsCitation":"Wieczorek, G.F., 1981, Ground-water level and precipitation data for slopes near La Honda, California: U.S. Geological Survey Open-File Report 81-367, 25 p., https://doi.org/10.3133/ofr81367.","productDescription":"25 p.","costCenters":[],"links":[{"id":400177,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0367/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143819,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0367/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"La Honda","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.44949340820312,\n 37.243448378654115\n ],\n [\n -122.09655761718749,\n 37.243448378654115\n ],\n [\n -122.09655761718749,\n 37.47812762872122\n ],\n [\n -122.44949340820312,\n 37.47812762872122\n ],\n [\n -122.44949340820312,\n 37.243448378654115\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6687f4","contributors":{"authors":[{"text":"Wieczorek, Gerald F.","contributorId":81889,"corporation":false,"usgs":true,"family":"Wieczorek","given":"Gerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":163527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9275,"text":"ofr8067 - 1981 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","interactions":[{"subject":{"id":9275,"text":"ofr8067 - 1981 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"ofr8067","publicationYear":"1981","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":1756,"text":"wsp2209 - 1985 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"wsp2209","publicationYear":"1985","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"id":1}],"supersededBy":{"id":1756,"text":"wsp2209 - 1985 - Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","indexId":"wsp2209","publicationYear":"1985","noYear":false,"title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts"},"lastModifiedDate":"2022-10-11T21:12:13.733432","indexId":"ofr8067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-67","title":"Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts","docAbstract":"The Cape Cod aquifer system was simulated with three-dimensional finite-difference ground-water-flow models. Five areas were modeled to provide tools that can be used to evaluate the hydrologic impacts of regional water development and waste disposal.
The model boundaries were selected to represent the natural hydrologic boundaries of the aquifer. The boundary between fresh and saline ground water is treated as an interface along which there is no dispersion. The saline-water zone is treated as static (nonflowing).
Comparisons of calculated and observed values of head, position of the boundary between fresh and saline water, and ground-water discharge at locations where data are available indicate that the simulated ground-water reservoirs generally agree with field conditions.
Model analyses indicate that the total steady-state freshwater-flow rate through the five modeled areas is approximately 412 cubic feet per second.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8067","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission Barnstable County, and the National Park Service","usgsCitation":"Guswa, J.H., and LeBlanc, D.R., 1981, Digital models of ground-water flow in the Cape Cod aquifer system, Massachusetts: U.S. Geological Survey Open-File Report 80-67, vi, 128 p., https://doi.org/10.3133/ofr8067.","productDescription":"vi, 128 p.","costCenters":[],"links":[{"id":408184,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0067/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.53497314453125,\n 41.549700145132725\n ],\n [\n -69.91973876953125,\n 41.549700145132725\n ],\n [\n -69.91973876953125,\n 42.11248648904184\n ],\n [\n -70.53497314453125,\n 42.11248648904184\n ],\n [\n -70.53497314453125,\n 41.549700145132725\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656d6c","contributors":{"authors":[{"text":"Guswa, John H.","contributorId":97881,"corporation":false,"usgs":true,"family":"Guswa","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":159402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}