{"pageNumber":"2101","pageRowStart":"52500","pageSize":"25","recordCount":68919,"records":[{"id":9307,"text":"ofr83531 - 1983 - Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983","interactions":[],"lastModifiedDate":"2017-09-01T14:41:43","indexId":"ofr83531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-531","title":"Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983","docAbstract":"<p>This report summarizes the progress on water-resources studies in Utah by the U.S. Geological Survey during the period July 1, 1982, to June 30, 1983. Much of the work was done in cooperation with the State of Utah and local agencies. Additional supporting funds were transferred from other Federal agencies or appropriated directly to the Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr83531","usgsCitation":"1983, Water-resources studies in Utah by the U.S. Geological Survey, July 1, 1982 to June 30, 1983: U.S. Geological Survey Open-File Report 83-531, 49, https://doi.org/10.3133/ofr83531.","productDescription":"49","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":37022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0531/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0531/report-thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c8e4b07f02db5413f6","contributors":{"compilers":[{"text":"Hamblin, Linda S.","contributorId":52202,"corporation":false,"usgs":true,"family":"Hamblin","given":"Linda","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":659124,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":3840,"text":"cir850K - 1983 - Sediment deposition in the Columbia and lower Cowlitz rivers, Washington-Oregon, caused by the May 18, 1980, eruption of Mount St. Helens","interactions":[],"lastModifiedDate":"2022-10-04T18:45:45.113686","indexId":"cir850K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"850","chapter":"K","title":"Sediment deposition in the Columbia and lower Cowlitz rivers, Washington-Oregon, caused by the May 18, 1980, eruption of Mount St. Helens","docAbstract":"<p>On May 18, 1980, Mount St. Helens violently erupted, sending billions of cubic yards of mud, ash, rock fragments, and debris down the North and South Forks of the Toutle River, the Cowlitz and Columbia Rivers, and other streams. A total of 35.6 million cubic yards of mudflow material was deposited in the lower Cowlitz (downstream from the Union Pacific Railroad bridge) and Columbia Rivers. </p><p>The arrival of this material at the Columbia River, during a period of the daily tidal cycle, when the flow was at a minimum or quite probably reversed and flowing upstream resulted in its deposition in an area 7 miles upstream and 2 miles downstream from the junction of the Cowlitz and Columbia Rivers. The thickness of the deposit was at a maximum near Coffin Rock, where a hole 140 feet deep was filled with 90 feet of sediment. Incomplete filling, compaction, and (or) erosion caused a 1Q-foot depression to form in the surface of the newly deposited material at this location. </p><p>On May 23, 1980, the presence of two scour channels on each side of a tonguelike deposit (delta) of very fine sand and silt indicates that the coarse-grained sediment and water surge on the morning of May 19 initially scoured the lower 0.5 mile of the Cowlitz River bed. A minimum of 0.4 million cubic yard of material was scoured from the Cowlitz River bed and subsequently redeposited in the Columbia River before the 1.3-million-cubic-yard delta was formed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir850K","usgsCitation":"Haeni, F., 1983, Sediment deposition in the Columbia and lower Cowlitz rivers, Washington-Oregon, caused by the May 18, 1980, eruption of Mount St. Helens: U.S. Geological Survey Circular 850, v, 21 p., https://doi.org/10.3133/cir850K.","productDescription":"v, 21 p.","costCenters":[],"links":[{"id":30913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0850k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0850k/report-thumb.jpg"},{"id":407869,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23831.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River, Cowlitz River, Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.02490234375,\n              46.038922598236\n            ],\n            [\n              -122.04711914062499,\n              46.038922598236\n            ],\n            [\n              -122.04711914062499,\n              46.475699386607516\n            ],\n            [\n              -123.02490234375,\n              46.475699386607516\n            ],\n            [\n              -123.02490234375,\n              46.038922598236\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f5a6","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":147705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43736,"text":"ofr83879 - 1983 - Land use and land cover and associated maps for Fairmont, Minnesota; Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:04:57","indexId":"ofr83879","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-879","title":"Land use and land cover and associated maps for Fairmont, Minnesota; Iowa","language":"ENGLISH","doi":"10.3133/ofr83879","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Fairmont, Minnesota; Iowa: U.S. Geological Survey Open-File Report 83-879, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr83879.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":134655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b135e","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":531337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11534,"text":"ofr83252 - 1983 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","interactions":[{"subject":{"id":11534,"text":"ofr83252 - 1983 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"ofr83252","publicationYear":"1983","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2868,"text":"wsp2247 - 1985 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"wsp2247","publicationYear":"1985","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"id":1}],"supersededBy":{"id":2868,"text":"wsp2247 - 1985 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"wsp2247","publicationYear":"1985","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"lastModifiedDate":"2021-03-05T02:04:08.849089","indexId":"ofr83252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-252","title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83252","usgsCitation":"Waddell, K., Darby, D., and Theobald, S., 1983, Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah: U.S. Geological Survey Open-File Report 83-252, 74 p., https://doi.org/10.3133/ofr83252.","productDescription":"74 p.","costCenters":[],"links":[{"id":384039,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0252/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0252/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Carbon County","otherGeospatial":"Scofield Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.18713378906249,\n              39.74732195489861\n            ],\n            [\n              -111.11709594726561,\n              39.74732195489861\n            ],\n            [\n              -111.11709594726561,\n              39.82013946676259\n            ],\n            [\n              -111.18713378906249,\n              39.82013946676259\n            ],\n            [\n              -111.18713378906249,\n              39.74732195489861\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e480e","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":163318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darby, D.W.","contributorId":49333,"corporation":false,"usgs":true,"family":"Darby","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":163316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Theobald, S.M.","contributorId":51270,"corporation":false,"usgs":true,"family":"Theobald","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":163317,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7442,"text":"ofr83291 - 1983 - Preliminary mineralogic, fluid inclusion, and stable isotope study of the Mahd adh Dhahab gold mine, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr83291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-291","title":"Preliminary mineralogic, fluid inclusion, and stable isotope study of the Mahd adh Dhahab gold mine, Kingdom of Saudi Arabia","docAbstract":"The Mahd adh Dhahab mine, located about 280 km northeast of Jiddah, Kingdom of Saudi Arabia, has yielded more than 2 million ounces of gold from periodic production during the past 3,000 years. A new orebody on the southern side of the ancient workings, known as the South orebody, is being developed by Gold Fields-Mahd adh Dhahab Limited. A suite of samples was collected from the newly exposed orebody for preliminary mineralogic, stable isotope, fluid inclusion, and geochemical studies. \r\n\r\nThe Mahd adh Dhahab deposit is in the carapace of a Proterozoic epizonal rhyolite stock that domed pyroclastic and metasedimentary rocks of the Proterozoic Halaban group. Ore of gold, silver, copper, zinc, tellurium, and lead is associated with north-trending, steeply dipping quartz veins in a zone 1,000 m long and 400 m wide. The veins include an assemblage of quartz-chlorite-pyrite-hematite-chalcopyrite-sphalerite-precious metals, which is similar to the mineral assemblage at the epithermal deposit at Creede, Colorado. \r\n\r\nThe primary ore contains abundant chalcopyrite, sphalerite, and pyrite in addition to a complex precious metal assemblage. Gold and silver occur principally as minute grains of telluride minerals disseminated in quartz-chlorite-hematite and as inclusions in chalcopyrite and sphalerite. Telluride minerals include petzite, hessite, and sylvanite. Free gold is present but not abundant. \r\n\r\nAll of the vein-quartz samples contained abundant, minute inclusions of both low-density, vapor-rich fluids and liquid-rich fluids. Primary fluid inclusions yielded homogenization temperatures of from 110? to 238? C. Preliminary light-stable isotope studies of the sulfide minerals and quartz showed that all of the d34S values are between 1.2 and 6.3 per mil, which is a typical range for hydrothermal sulfide minerals that derive their sulfur from an igneous source. \r\n\r\nThe data-suggest that the sulfide sulfur isotope geochemistry was controlled by exchange with la large sulfur isotope reservoir at depth.\r\n\r\nThe d18O values of all stages of vein quartz in the South orebody range between 8.5 and 11.1 per mil. This range is similar to that for quartz from the North orebody and indicates that the hydrothermal system consisted of dominantly exchanged meteoric water, which was uniform in temperature and d18O content throughout the area during the entire period of mineralization.\r\n\r\nLead isotope analyses of two galena samples indicate that the lead in the South orebody is less radiogenic than that from the North orebody and confirm that the lead was derived from oceanic crust approximately 700 Ma ago.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83291","usgsCitation":"Rye, R.O., Hall, W., Cunningham, C.G., Czamanske, G., Afifi, A., and Stacey, J.S., 1983, Preliminary mineralogic, fluid inclusion, and stable isotope study of the Mahd adh Dhahab gold mine, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-291, 26 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83291.","productDescription":"26 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0291/report-thumb.jpg"},{"id":34855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cdfb","contributors":{"authors":[{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":155633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, W. E.","contributorId":6431,"corporation":false,"usgs":true,"family":"Hall","given":"W. E.","affiliations":[],"preferred":false,"id":155634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":155638,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":155635,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Afifi, A.M.","contributorId":39375,"corporation":false,"usgs":true,"family":"Afifi","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":155636,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155637,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":11502,"text":"ofr82769 - 1983 - Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr82769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-769","title":"Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model","docAbstract":"The principal dissolved constituents in water in the Spokane aquifer are calcium and bicarbonate. These constituents (as well as dissolved solids, hardness, and magnesium) each correlate well with specific conductance, whereas chloride, sodium, and nitrate each do not. Specific conductance ranges from 73 to 820 micromhos per centimeter throughout the study area. Short-term variations in water quality in the Spokane aquifer are generally greater than long-term variations. \r\n\r\nVertical variations in concentration of chemical constituents occurred in four of 15 wells used to sample the upper 50 feet of the aquifer along several cross sections. Changes in water quality from one cross section to another could not be directly related to land-use activities. \r\n\r\nA digital model was developed and used to simulate solute transport of conservative ions in the Spokane aquifer. Specifically, the model was used to estimate the impact of the chloride ion from recharge through septic tanks and from irrigation on the water quality of the aquifer. Analysis shows that the estimated impact on the aquifer from these two source loadings was less than a 1-milligram-per-liter increase throughout approximately 80 percent of the aquifer, but increases averaging about 3 milligrams per liter occurred in some peripheral areas. Various water-quality-management schemes based on manmade or natural stresses can be tested with the model.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82769","usgsCitation":"Vaccaro, J.J., and Bolke, E., 1983, Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model: U.S. Geological Survey Open-File Report 82-769, vi, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82769.","productDescription":"vi, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0769/report-thumb.jpg"},{"id":39368,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1cce","contributors":{"authors":[{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":163260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9159,"text":"ofr83760 - 1983 - Ground-water levels in observation wells in Oklahoma, 1980-82","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-760","title":"Ground-water levels in observation wells in Oklahoma, 1980-82","docAbstract":"In the 1980-82 Climatic Years, the U. S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, collected ground-water level data in Oklahoma from 1,122 sites in 77 counties. This report presents this data.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83760","usgsCitation":"Goemaat, R.L., Mize, L.D., and Spiser, D.E., 1983, Ground-water levels in observation wells in Oklahoma, 1980-82: U.S. Geological Survey Open-File Report 83-760, viii, 612 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83760.","productDescription":"viii, 612 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0760/report-thumb.jpg"},{"id":36786,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66762b","contributors":{"authors":[{"text":"Goemaat, Robert L.","contributorId":64256,"corporation":false,"usgs":true,"family":"Goemaat","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mize, Lionel D.","contributorId":20326,"corporation":false,"usgs":true,"family":"Mize","given":"Lionel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":159199,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spiser, Dannie E.","contributorId":42214,"corporation":false,"usgs":true,"family":"Spiser","given":"Dannie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159200,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7782,"text":"ofr83677 - 1983 - Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","interactions":[],"lastModifiedDate":"2025-09-23T16:51:31.349837","indexId":"ofr83677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-677","title":"Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","docAbstract":"<p>The Jasper (Miocene) aquifer is one of several important hydrologic units in the Gulf Coastal Plain. Because the Jasper aquifer underlies shallower aquifers in many areas, regional water withdrawals from the Jasper are not significant; however, it is capable of yielding 3,000 gallons per minute (200 liters per second) or more of water to wells in certain areas. The Jasper is underlain by the Catahoula confining system (restricted) and overlain by the Burkeville confining system. The Evangeline and Chicot aquifers, in turn, overlie the Burkeville and also are prolific water-yielding aquifers.</p><p>The ground-water hydrology of the Jasper aquifer in an area of about 20,000 square miles (52,000 square kilometers) was simulated by a two-dimensional digital model using a steady-state approach. The model represents hydrologic conditions prior to development by wells, when natural recharge equaled natural discharge. The model's grid pattern of 15 x 24 nodes varies from a dimension of 5 by 10 miles (8 by 16 kilometers) in the outcrop to 10 by 10 miles (16 by 16 kilometers) in the artesian section downdip from the outcrop.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83677","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Baker, E., 1983, Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain: U.S. Geological Survey Open-File Report 83-677, Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller, https://doi.org/10.3133/ofr83677.","productDescription":"Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":27024,"text":"wri834029 - 1983 - Geology and ground-water resources of Camden County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri834029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4029","title":"Geology and ground-water resources of Camden County, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834029","usgsCitation":"Farlekas, G., Nemickas, B., and Gill, H., 1983, Geology and ground-water resources of Camden County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 83-4029, xvii, 158 p. :ill., maps ;27 cm., https://doi.org/10.3133/wri834029.","productDescription":"xvii, 158 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":110277,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49164.htm","linkFileType":{"id":5,"text":"html"},"description":"49164"},{"id":119801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4029/report-thumb.jpg"},{"id":55904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4029/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264588,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-45.pdf","size":"574","linkFileType":{"id":1,"text":"pdf"}},{"id":264589,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-table_2.pdf","size":"91","linkFileType":{"id":1,"text":"pdf"}},{"id":264581,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-02.pdf","size":"6433","linkFileType":{"id":1,"text":"pdf"}},{"id":264582,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-05.pdf","size":"871","linkFileType":{"id":1,"text":"pdf"}},{"id":264583,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-06.pdf","size":"442","linkFileType":{"id":1,"text":"pdf"}},{"id":264584,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-10.pdf","size":"79","linkFileType":{"id":1,"text":"pdf"}},{"id":264585,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-25.pdf","size":"642","linkFileType":{"id":1,"text":"pdf"}},{"id":264586,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-27.pdf","size":"2636","linkFileType":{"id":1,"text":"pdf"}},{"id":264587,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4029/plate-28.pdf","size":"2522","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c2c","contributors":{"authors":[{"text":"Farlekas, G.M.","contributorId":67129,"corporation":false,"usgs":true,"family":"Farlekas","given":"G.M.","affiliations":[],"preferred":false,"id":197428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":197429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":197427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11492,"text":"ofr83746 - 1983 - Sand-wave movement on Little Georges Bank","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr83746","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-746","title":"Sand-wave movement on Little Georges Bank","docAbstract":"A 1-x-1.5-km area on Little Georges Bank (centered at 41?08?N., 68?04?W.) was mapped three times during a ten-month period by sidescan sonar and echo-sounding techniques to assess the morphology and mobility of sand waves on Georges Bank. Sand-wave amplitudes in the survey area ranged from 1-11 m although most were 5-7 m. Wavelengths were not constant as the crests were sinuous and in places, even bifurcated. The sand waves are asymmetrical with their steepest sides facing northwest; however, gradients of their steep sides mostly are 4?-10? which is well below the angle of repose for sand in water. Sand waves tended to have greater relief and a sharper asymmetry during the survey in September than during those in June or April. \r\n\r\nDuring the survey period the sand waves moved but the direction and rate of motion was variable. Even along an individual sand wave some parts moved as much as 60 m between surveys while other parts apparently remained stationary. The sand waves were asymmetrical, but movement was not consistently in the direction that the steep sides faced. Along the same sand wave, parts moved to the northwest while other parts moved to the southeast. Despite the complex pattern of sand motion, the mean displacement of the sand waves was below the resolution of the survey technique; to resolve it, a longer survey is needed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83746","usgsCitation":"Twichell, D.C., 1983, Sand-wave movement on Little Georges Bank: U.S. Geological Survey Open-File Report 83-746, ii, 22 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83746.","productDescription":"ii, 22 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0746/report-thumb.jpg"},{"id":39361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0746/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdae2","contributors":{"authors":[{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":163234,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11294,"text":"ofr83263 - 1983 - Statistical summaries of selected chemical constituents in Kansas ground-water supplies, 1976-81","interactions":[],"lastModifiedDate":"2022-01-06T20:12:29.220578","indexId":"ofr83263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-263","title":"Statistical summaries of selected chemical constituents in Kansas ground-water supplies, 1976-81","docAbstract":"Data on 24 chemical constituents or properties obtained from 766 wells in the Kansas ground-water quality monitoring network between 1976 and 1981 are statistically summarized in this report prepared in cooperation with the Kansas Department of Health and Environment. Minimum, median, and maximum concentrations and percentage of samples above the ' maximum contaminant levels ' established by the U.S. Environmental Protection Agency are presented for all wells in the statewide network. More detailed areal statistical summaries are presented for all wells in the statewide network. More detailed areal statistical summaries are presented for nine chemical constituents for which more than 3% of the observed concentrations exceeded the ' maximum contaminate level ' for that constituent. The State was divided into 14 ground-water regions based on water-use and physiographic characteristics. Summaries for these nine constituents include quartile values and percentage of samples with concentrations above the ' maximum contaminant level ' for each ground-water region. Accompanying figures show median concentrations and percentages of concentrations exceeding the ' maximum contaminant levels ' established by the U.S. Environmental Protection Agency for each ground-water region. 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,{"id":29516,"text":"wri834091 - 1983 - Hydrology of the Newberry Volcano caldera, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri834091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4091","title":"Hydrology of the Newberry Volcano caldera, Oregon","docAbstract":"Precipitation in the Newberry Caldera is very nearly in balance with evaporation, evapotranspiration, and streamflow. Calcium, magnesium, and bicarbonate ions predominate in the more dilute ground and surface water. Thermal waters from springs and wells have concentrations of 900 milligrams per liter or more and are characterized by high concentrations of sodium and sulfate. Attempts to account for the origin of the hot springs on the basis of mixing relations and isotopic analyses were inconclusive; the springs may represent mixtures of thermal and nonthermal water which are altered by gases rising from sources beneath the caldera floor. Annual recharge to deep aquifers beneath the caldera is probably in the range 2,500 to 6,500 acre-feet. Observations in a Geological Survey drill hole suggest that part of the water may flow to aquifers at depths as much as 1,900 feet beneath the caldera floor. Potential recharge to a postulated geothermal reservoir probably is extremely small. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834091","usgsCitation":"Sammel, E., and Craig, R.W., 1983, Hydrology of the Newberry Volcano caldera, Oregon: U.S. Geological Survey Water-Resources Investigations Report 83-4091, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834091.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4091/report-thumb.jpg"},{"id":58356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601a2f","contributors":{"authors":[{"text":"Sammel, E.A.","contributorId":59480,"corporation":false,"usgs":true,"family":"Sammel","given":"E.A.","affiliations":[],"preferred":false,"id":201648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Craig, R. W.","contributorId":40984,"corporation":false,"usgs":true,"family":"Craig","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201647,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10642,"text":"ofr8335 - 1983 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","interactions":[],"lastModifiedDate":"2017-03-29T14:22:44","indexId":"ofr8335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-35","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981","docAbstract":"<p>Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin and Houston. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year. The study in the San Antonio area was completed at the end of the 1981 water year.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data. The Texas Department of Water Resources ended its participation in the project in 1979, and the city of San Antonio funded the program through the 1981 water year.</p><p>The operation and maintenance of stations 08178000, San Antonio River at San Antonio; 08178700, Salado Creek (upper station) at San Antonio; and 08178800, Salado Creek (lower station) at San Antonio are funded by the city of San Antonio and the U.S Geological Survey.</p><p>The operation and maintenance and collection of water-quality data at station 08178720, Lorence Creek at Thousand Oaks Blvd., San Antonio, station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio, are funded by the Edwards Underground Water District in cooperation with the Texas Department of Hater Resources and the U.S. Geological Survey. Station 08178640, West Elm Creek at San Antonio, and station 08178645, East Elm Creek at San Antonio will provide hydrologic data on similar and adjacent watersheds. The West Elm watershed is still predominately rural but is undergoing extensive urbanization in some areas. The East Elm watershed is relatively stable and undeveloped.</p><p>The objectives of the San Antonio urban hydrology study are:</p><ol><li>To provide data showing the effects of various stages of urbanization on flood discharge and runoff.</li><li>To provide water-quality data on surface-water runoff from floods of various magnitudes, during all seasons of the year from areas with different types of urban development.</li></ol><p>Annual publication of the San Antonio urban studies was initiated in 1969.</p><p>A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in the U.S. Geological Survey's 1979 and 1980 \"Water resources data for Texas\" reports.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8335","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1983, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1981: U.S. Geological Survey Open-File Report 83-35, v, 58 p., https://doi.org/10.3133/ofr8335.","productDescription":"v, 58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0035/report.pdf","text":"Report","size":"1.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":144085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0035/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6078df","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11425,"text":"ofr83311 - 1983 - Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-311","title":"Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","docAbstract":"Most thermal waters issuing in Lassen Volcanic National Park (LVNP) are acidic (pH =3.5), low-Cl (concentrations =30 mg/L) hot springs which are characteristic of vapor-dominated hydrothermal systems and, as such, are not useful for liquid chemical geothermometry. Thermal waters at Drakesbad and in Little Hot Springs Valley, hot spring localities characterized by neutral pH and low Cl containing water, may have equilibrated in shallow aquifers so that temperatures estimated by both the Na-K-Ca and Na-Li geothermometers approach the measured spring temperatures of 65? to 95?C. Waters rich in chloride (>2000 mg/L), such as those at Growler Hot Spring and Morgan Hot Springs, situated south of LVNP, are the most appropriate springs for liquid chemical geothermometry and indicate subsurface temperatures between 220? and 230?C. The chemical and thermal characteristics of these springs may result either from boiling at depth and subsequent mixing with meteoric water or from conductive cooling during lateral flow. In either case ~220? to 230?C thermal water probably originates inside LVNP and flows south to Morgan Hot Springs.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83311","usgsCitation":"Thompson, J., 1983, Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California: U.S. Geological Survey Open-File Report 83-311, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83311.","productDescription":"27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0311/report-thumb.jpg"},{"id":39277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0311/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e496d","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":163118,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11689,"text":"ofr8393 - 1983 - Geophysical and geologic studies in southern Mecklenburg County and vicinity, North Carolina and South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T13:30:08","indexId":"ofr8393","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-93","title":"Geophysical and geologic studies in southern Mecklenburg County and vicinity, North Carolina and South Carolina","docAbstract":"Geophysical methods consisting of gravity, aeromagnetics and aeroradioactivity have been applied to part of the Charlotte and Carolina slate belts in southern Mecklenburg County and vicinity to help interpret geology, lithology and structure. High aeroradioactivity is associated with potassium-rich granitic plutons, muscovite-rich gneisses, schists, and metavolcanic rocks; positive gravity and magnetic anomalies are associated with gabbro plutons; and negative gravity anomalies are associated with granitic plutons. \r\n\r\nAt the west side of the slate belt, the Tillery phyllite is interpreted as having undergone progressive metamorphism. The underlying Uwharrie Formation extends into the Charlotte belt where it is mapped as metavolcanic rocks. Gravity models of the Carolina slate belt indicate that it is a synform containing a wedge of metasedimentary and volcanoclastic rock on plutonic basement. The basement is exposed in the adjacent Charlotte belt antiform. \r\n\r\nThe northern Charlotte belt contains mainly plutonic rocks which have been divided into 3 supergroups of plutons based upon chemistry, mineralogy, texture, and age. They are: \r\n\r\n1. Old Plutonic supergroup - plutons 545-490 m.y. that are medium to coarse-grained tonalite, quartz diorite, and granodiorites. \r\n\r\n2. Concord-Salisbury supergroup -- plutons 426-350 m.y. which form sheet-like intrusions of differentiated gabbro; local volcanic centers with ring complexes 13 km in diameter that suggest magma chambers 0 - 8 km deep; smaller bodies of diorite, monzonite, and syenite; and small Salisbury type granodiorites. \r\n\r\n3. Landis supergroup -- plutons 350-280 m.y. that are usually very coarse-grained, porphyritic, 'big feldspar,' potassium-rich granites. \r\n\r\nThe Mecklenburg-Weddington gabbro complex of the Concord-Salisbury supergroup, the largest feature in the study area, contains three large gabbro plutons. The gabbro intruded old Plutonic complex rocks and could-have produced the metamorphic reaction K-feldspar + sillimanite quartz + muscovite reflected in the mineral assemblage of adjacent felsic metavolcanic rocks. Gravity models indicate a lopolith 3.5- to 4.5-km thick with a 2 km sill extending to the northeast. Positive magnetic and gravity anomalies suggest the lopolith is. connected with the Concord gabbro complex to the northeast. \r\n\r\nThe sheet-like intrusions of Concord-Salisbury group gabbros, forming the core of the composite 5atholith, have medium-grained Salisbury type granodiorite above, and coarser-grained Landis granite below. The position of the supergroups as presently exposed may be a function of level of erosion versus level of emplacement. The plutons in the composite batholith span 200 m.y. according to current age data and are arranged with the oldest at the top and the youngest at the bottom. However, Rb-Sr and K-At ages in the Piedmont are more likely to reflect age of crustal uplift than the age of metamorphism or intrusion. The Charlotte belt composite batholith, therefore, may very well be the result of a shorter single tectonic event or process.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8393","usgsCitation":"Wilson, F., 1983, Geophysical and geologic studies in southern Mecklenburg County and vicinity, North Carolina and South Carolina: U.S. Geological Survey Open-File Report 83-93, 199 p.  ill., maps ;28 cm., https://doi.org/10.3133/ofr8393.","productDescription":"199 p.  ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":39562,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0093/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39561,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39563,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0093/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0093/report-thumb.jpg"}],"country":"United States","state":"North Carolina, South Carolina","county":"Mecklenburg County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.19308471679688,\n              34.84762101276787\n            ],\n            [\n              -81.19308471679688,\n              35.74316846139925\n            ],\n            [\n              -80.4144287109375,\n              35.74316846139925\n            ],\n            [\n              -80.4144287109375,\n              34.84762101276787\n            ],\n            [\n              -81.19308471679688,\n              34.84762101276787\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c208","contributors":{"authors":[{"text":"Wilson, Frederick A.","contributorId":100352,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederick A.","affiliations":[],"preferred":false,"id":163574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29987,"text":"wri834106 - 1983 - Base flow of streams in the outcrop area of southeastern sand aquifer: South Carolina, Georgia, Alabama, and Mississippi","interactions":[],"lastModifiedDate":"2022-01-28T12:33:49.391345","indexId":"wri834106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4106","title":"Base flow of streams in the outcrop area of southeastern sand aquifer: South Carolina, Georgia, Alabama, and Mississippi","docAbstract":"<p>The base flow component of streamflow was separated from hydrographs for unregulated streams in the Cretaceous and Tertiary clastic outcrop area of South Carolina, Georgia, Alabama, and Mississippi. The base flow values are used in estimating recharge to the sand aquifer. Relations developed between mean annual base flow and stream discharge at the 60- and 65-percent streamflow duration point can be used to approximate mean annual base flow in lieu of hydrograph separation methods for base flows above 10 cu ft/s. Base flow recession curves were used to derive estimates of hydraulic diffusivity of the aquifer which was converted to transmissivity using estimated specific yield. These base-flow-derived transmissivities are in general agreement with transmissivities derived from well data. The shape of flow duration curves of streams is affected by the lithology of the Coastal Plain sediments. Steep flow duration curves appear to be associated with basins underlain by clay or chalk where a low percentage of the discharge is base flow while flatter curves appear to be associated with basins underlain by sand and gravel where a high percentage of the discharge is base flow.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834106","usgsCitation":"Stricker, V., 1983, Base flow of streams in the outcrop area of southeastern sand aquifer: South Carolina, Georgia, Alabama, and Mississippi: U.S. Geological Survey Water-Resources Investigations Report 83-4106, iv, 17 p., https://doi.org/10.3133/wri834106.","productDescription":"iv, 17 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":58795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4106/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395018,"rank":4,"type":{"id":36,"text":"NGMDB Index 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,{"id":8694,"text":"ofr83268 - 1983 - Ground-water levels in Arkansas, spring 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr83268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-268","title":"Ground-water levels in Arkansas, spring 1983","docAbstract":"About 640 ground-water level measurements were made in observation wells in Arkansas in the spring of 1981. In addition , the report contains potentiometric-surface maps and well hydrographs relating to the alluvial aquifer and the Sparta Sand , the most important aquifers with respect to ground-water availability and use in Arkansas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83268","usgsCitation":"Edds, J., 1983, Ground-water levels in Arkansas, spring 1983: U.S. Geological Survey Open-File Report 83-268, v, 54 p. ill. ;28 cm., https://doi.org/10.3133/ofr83268.","productDescription":"v, 54 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141773,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0268/report-thumb.jpg"},{"id":36281,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0268/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4995e4b07f02db5b6bd5","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":158169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28683,"text":"wri834028 - 1983 - Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri834028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4028","title":"Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834028","usgsCitation":"Meisler, H., 1983, Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 83-4028, 76 p. :maps ;28 cm., https://doi.org/10.3133/wri834028.","productDescription":"76 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4028/report-thumb.jpg"},{"id":57523,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7662","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":200226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11345,"text":"ofr83127 - 1983 - Literature assessment of the Charlotte Harbor estuarine system and surrounding area, Southwest Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-127","title":"Literature assessment of the Charlotte Harbor estuarine system and surrounding area, Southwest Florida","docAbstract":"The Governor of Florida established the Charlotte Harbor Resource Planning and Management committee to recommend the course of action Florida should take in planning for potential growth in the rapidly growing area surrounding Charlotte Harbor. In May 1981, the U.S. Geological Survey began a planning study to determine detailed hydrologic study needs of the Charlotte Harbor area. A literature search of available data and reports pertaining to the Charlotte Harbor estuarine system and surrounding area resulted in almost 1,300 references. This report contains all references collected during this search. Some of the major reference topics are altered freshwater flow, water quality of the harbor and drainage systems, circulation and tides, coastal and marine resources, fisheries, geology and hydrology of the area, impact studies, water resources, flora and fauna of the area, and water supply. Sixty-eight key words or subject identifiers are used to the index report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83127","usgsCitation":"Stoker, Y.E., and Karavitis, G.A., 1983, Literature assessment of the Charlotte Harbor estuarine system and surrounding area, Southwest Florida: U.S. Geological Survey Open-File Report 83-127, 143 p. map ;28 cm., https://doi.org/10.3133/ofr83127.","productDescription":"143 p. map ;28 cm.","costCenters":[],"links":[{"id":143667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0127/report-thumb.jpg"},{"id":39171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0127/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a481d","contributors":{"authors":[{"text":"Stoker, Yvonne E. ystoker@usgs.gov","contributorId":5101,"corporation":false,"usgs":true,"family":"Stoker","given":"Yvonne","email":"ystoker@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":162969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karavitis, George A. gkaravitis@usgs.gov","contributorId":5712,"corporation":false,"usgs":true,"family":"Karavitis","given":"George","email":"gkaravitis@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":162970,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56650,"text":"fwsobs82_10_50 - 1983 - Habitat Suitability Index Models: Roseate spoonbill","interactions":[],"lastModifiedDate":"2022-02-09T15:26:11.161465","indexId":"fwsobs82_10_50","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.50","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Roseate spoonbill","docAbstract":"<p>The roseate spoonbill is a long-legged wading bird with a height of approximately 80 cm (31.5 inches), a wingspan of 1.3 m (4.3 ft), and a weight of 1.6 kg (3.5 Ib }. The bill is narrower near the base (2-3 em, 0.8-1.2 inches) than at the flattened tip (5 cm, 2 inches) and is 15-18 cm (5.9-7.1 inches) in length.</p><p>Roseate spoonbills occur and nest in peninsular Florida, coastal Louisiana, and Texas, south through the West Indies, Mexico, Central and South America to Argentina and Chile. Marine, brackish, and freshwater habitats are utilized, but brackish areas are favored (Blacklock et al. 1978). In the late 1970·s there were 2,500 pairs nesting along the Texas coast (Texas Colonial Waterbird Society 1982), 1,300 pairs in southwestern Louisiana (Portnoy 1977), and 1,400 pairs in Florida (Robertson et al. 1983). These birds are resident year round in Florida, Louisiana, and Texas, but fewer bi rds are present duri ng the nonbreedi ng season than in the breeding season. Some individuals move northward after nesting and have been reported in Georgia, Nebraska, Pennsylvania, Utah, and Wisconsin, but most spoonbills move south when they leave the breeding area.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lewis, J., 1983, Habitat Suitability Index Models: Roseate spoonbill: FWS/OBS 82/10.50, vi, 16 p.","productDescription":"vi, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":181765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64977c","contributors":{"authors":[{"text":"Lewis, James C.","contributorId":88799,"corporation":false,"usgs":true,"family":"Lewis","given":"James C.","affiliations":[],"preferred":false,"id":255599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9976,"text":"ofr83338 - 1983 - Oxygen and strontium isotopic studies of basaltic lavas from the Snake River plain, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr83338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-338","title":"Oxygen and strontium isotopic studies of basaltic lavas from the Snake River plain, Idaho","docAbstract":"The Snake Creek-Williams Canyon pluton of the southern Snake Range crops out over an area of about 30 km2, about 60 km southeast of Ely, Nev. This Jurassic intrusion displays large and systematic chemical and mineralogical zonation over a horizontal distance of 5 km. Major-element variations compare closely with Dalyls average andesite-dacite-rhyolite over an SiO2 range of 63 to 76 percent. \r\n\r\nFor various reasons it was originally thought that assimilation played a dominant role in development of the Snake Creek-Williams Canyon pluton. However, based on modeling of more recently obtained trace element and isotopic data, we have concluded that the zonation is the result of in-situ fractional crystallization, with little assimilation at the level of crystallization. \r\n\r\nThis report summarizes data available for each of the mineral species present in the zoned intrusion. Special attention has been paid to trends We present oxygen and strontium isotopic data for olivine tholeiites, evolved (that is, differentiated and (or) contaminated) lavas, rhyolites, and crustal- derived xenoliths from the Snake River Plain. These data show that the olivine tholeiites are fairly uniform in d80 (5.1 to 6.2) and 87Sr/86Sr (0.7056 to 0.7076) and reveal no correlation between these ratios. The tholeiites are considered representative of mantle-derived magmas that have not interacted significantly with crustal material or meteoric water. The evolved lavas display a wider range in d 80 (5.6 to 7.6) and 87Sr/86Sr (0.708 to 0.717) with positive correlations between these ratios in some suites but not in others. Crustal xenoliths have high and variable 8?Sr/86Sr (0.715 to 0.830) and d80 values that vary widely (6.7 to 9.2) and are a few permil greater than d80 values of the Snake River basalts. Thus, isotopic data for the evolved lavas are permissive of small degrees of contamination by crustal rocks similar to the most d80-depleted xenoliths. The d80 enrichments in some evolved lavas also are consistent with crystal fractionation processes and do not necessarily require bulk interaction with crustal rocks. Enrichment in d80 but not in 87Sr/86Sr in one suite of evolved lavas suggests that crustal contamination may not be essential to the petrogenesis of those lavas. Other suites of evolved lavas display large variations in 87Sr/86Sr that reflect at least some selective contamination with 87St. \r\n\r\nBulk solid/liquid oxygen-isotope fractionation factors (a's) calculated for the evolved lavas from Craters of the Moon National Monument are comparatively large. These a's are dependent upon the nature and proportions of phases removed by crystal fractionation; basaltic lava a's differ from latitic lava a?s in accordance with different phenocryst assemblages in these rocks. \r\n\r\nSnake River Plain rhyolites are isotopically distinct from both the analyzed crustal xenoliths and olivine tholeiites. Their origin remains poorly understood, but crustal or sub-crustal sources may be viable. In the first case, they must be derived by anatexis of material distinct from the analyzed crustal xenoliths. In the second case, they must be derived from material unlike the source for tholeiites. No cogenetic relation with the tholeiites seems likely on the basis of available data. that might relate to the variation in the chemical petrology of the pluton.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83338","usgsCitation":"Leeman, W.P., and Whelan, J.F., 1983, Oxygen and strontium isotopic studies of basaltic lavas from the Snake River plain, Idaho: U.S. Geological Survey Open-File Report 83-338, 35 p. ill. ;28 cm., https://doi.org/10.3133/ofr83338.","productDescription":"35 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0338/report-thumb.jpg"},{"id":37775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0338/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0dd","contributors":{"authors":[{"text":"Leeman, William P.","contributorId":87142,"corporation":false,"usgs":true,"family":"Leeman","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whelan, Joseph F.","contributorId":29792,"corporation":false,"usgs":true,"family":"Whelan","given":"Joseph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160599,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11229,"text":"ofr83533 - 1983 - A statistical summary of data from the U.S. Geological Survey's national water quality networks","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr83533","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-533","title":"A statistical summary of data from the U.S. Geological Survey's national water quality networks","docAbstract":"The U.S. Geological Survey Operates two nationwide networks to monitor water quality, the National Hydrologic Bench-Mark Network and the National Stream Quality Accounting Network (NASQAN). The Bench-Mark network is composed of 51 stations in small drainage basins which are as close as possible to their natural state, with no human influence and little likelihood of future development. Stations in the NASQAN program are located to monitor flow from accounting units (subregional drainage basins) which collectively encompass the entire land surface of the nation. Data collected at both networks include streamflow, concentrations of major inorganic constituents, nutrients, and trace metals. The goals of the two water quality sampling programs include the determination of mean constituent concentrations and transport rates as well as the analysis of long-term trends in those variables. This report presents a station-by-station statistical summary of data from the two networks for the period 1974 through 1981. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83533","usgsCitation":"Smith, R.A., and Alexander, R.B., 1983, A statistical summary of data from the U.S. Geological Survey's national water quality networks: U.S. Geological Survey Open-File Report 83-533, 20 p. ;28 cm., https://doi.org/10.3133/ofr83533.","productDescription":"20 p. ;28 cm.","costCenters":[],"links":[{"id":145085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0533/report-thumb.jpg"},{"id":39019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0533/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62c9","contributors":{"authors":[{"text":"Smith, R. A.","contributorId":60584,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, R. B.","contributorId":108103,"corporation":false,"usgs":true,"family":"Alexander","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":162769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65430,"text":"i1525 - 1983 - Controlled photomosaic of the Casius Southwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1525","subseriesTitle":"NONE","title":"Controlled photomosaic of the Casius Southwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1525","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Controlled photomosaic of the Casius Southwest Quadrangle of Mars: U.S. Geological Survey IMAP 1525, 1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1525.","productDescription":"1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251313,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1525/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":251314,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1525/plate-1.pdf","size":"10482","linkFileType":{"id":1,"text":"pdf"}},{"id":252211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1525/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c21","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":533817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28741,"text":"wri824071 - 1983 - Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4071","title":"Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824071","usgsCitation":"Minges, D., 1983, Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4071, iv, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824071.","productDescription":"iv, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4071/report-thumb.jpg"},{"id":57593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c07","contributors":{"authors":[{"text":"Minges, D.R.","contributorId":31387,"corporation":false,"usgs":true,"family":"Minges","given":"D.R.","affiliations":[],"preferred":false,"id":200321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11622,"text":"ofr83206 - 1983 - Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","interactions":[{"subject":{"id":11622,"text":"ofr83206 - 1983 - Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","indexId":"ofr83206","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":70043374,"text":"70043374 - 1983 - Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico","indexId":"70043374","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico"},"id":1}],"supersededBy":{"id":70043374,"text":"70043374 - 1983 - Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico","indexId":"70043374","publicationYear":"1983","noYear":false,"title":"Geohydrologic framework of the Roswell ground-water basin, Chaves and Eddy Counties, New Mexico"},"lastModifiedDate":"2013-02-12T15:12:04","indexId":"ofr83206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-206","title":"Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico","language":"ENGLISH","publisher":"New Mexico State Engineer,","doi":"10.3133/ofr83206","usgsCitation":"Welder, G.E., 1983, Geohydrologic framework of the Roswell ground-water Basin, Chaves and Eddy counties, New Mexico: U.S. Geological Survey Open-File Report 83-206, vi, 66 p. :ill., maps ;26 cm., https://doi.org/10.3133/ofr83206.","productDescription":"vi, 66 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":145438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Chaves County;Eddy County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,31.33 ], [ -109.0,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.0,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ea6","contributors":{"authors":[{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":163461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}