{"pageNumber":"567","pageRowStart":"14150","pageSize":"25","recordCount":16498,"records":[{"id":24953,"text":"ofr791329 - 1979 - Preliminary hydrogeologic investigation of the Maxey Flats radioactive waste burial site, Fleming County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"ofr791329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1329","title":"Preliminary hydrogeologic investigation of the Maxey Flats radioactive waste burial site, Fleming County, Kentucky","docAbstract":"Burial trenches at the Maxey Flats radioactive waste burial site , Fleming County, Ky., cover an area of about 0.03 square mile, and are located on a plateau, about 300 to 400 feet above surrounding valleys. Although surface-water characteristics are known, little information is available regarding the ground-water hydrology of the Maxey Flats area. If transport of radionuclides from the burial site were to occur, water would probably be the principal mechanism of transport by natural means. Most base flow in streams around the burial site is from valley alluvium, and from the mantle of regolith, colluvium, and soil partially covering adjacent hills. Very little base flow is due to ground-water flow from bedrock. Most water in springs is from the mantle, rather than from bedrock. Rock units underlying the Maxey Flats area are, in descending order, the Nancy and Farmers Members of the Borden Formation, Sunbury, Bedford, and Ohio Shales, and upper part of the Crab Orchard Formation. These units are mostly shales, except for the Farmers Member, which is mostly sandstone. Total thickness of the rocks is about 320 feet. All radioactive wastes are buried in the Nancy Member. Most ground-water movement in bedrock probably occurs in fractures. The ground-water system at Maxey Flats is probably unconfined, and recharge occurs by (a) infiltration of rainfall into the mantle, and (b) vertical, unsaturated flow from the saturated regolith on hilltops to saturated zones in the Farmers Member and Ohio Shale. Data are insufficient to determine if saturated zones exist in other rock units. The upper part of the Crab Orchard Formation is probably a hydrologic boundary, with little ground-water flow through the formation. (USGS)","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr791329","issn":"0094-9140","usgsCitation":"Zehner, H.H., 1979, Preliminary hydrogeologic investigation of the Maxey Flats radioactive waste burial site, Fleming County, Kentucky (WRI/OFR): U.S. Geological Survey Open-File Report 79-1329, viii, 120 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr791329.","productDescription":"viii, 120 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157320,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1329/report-thumb.jpg"},{"id":53923,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1329/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53924,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1329/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1329/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec19","contributors":{"authors":[{"text":"Zehner, Harold H.","contributorId":12888,"corporation":false,"usgs":true,"family":"Zehner","given":"Harold","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":192859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29658,"text":"wri7914 - 1979 - Ground-water quality in Bannock, Bear Lake, Caribou, and part of Power counties, southeastern Idaho","interactions":[],"lastModifiedDate":"2018-09-07T13:13:03","indexId":"wri7914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-14","title":"Ground-water quality in Bannock, Bear Lake, Caribou, and part of Power counties, southeastern Idaho","docAbstract":"<p>This report provides information about the current quality of ground waters in southeastern Idaho and discusses the natural and manmade environmental controls on that quality. This information will be useful in planning and monitoring the development and use of the ground-water resources of southeastern Idaho.</p><p>The southeastern corner of Idaho, as described in this report, encompasses an area of about 4,000 mil in Bannock, Bear Lake, Caribou, and part of Power Counties. The popu- lation of the area in 1975, based on best estimates by the Idaho Division of Budget, Policy Planning, and Coordination (1976) was 75,200. About 80 percent of the population is in and near the city of Pocatello, which is the second largest population center in the State.</p><p>Pocatello's economy depends largely on manufacturing and industrial processing, which includes chemicalfertilizer plants. The econ- omy in the rural areas depends largely on agriculture--both dry and irrigated farming are practiced. Mining is important and expected to dominate the economy in the eastcentral part of the area in the future.</p><p>Natural resources include phosphate ore, which makes up about 35 percent of the U.S. reserves (U.S. Department of Interior and U.S. Department of Agriculture, 1977); ground water, which mostly underlies&nbsp;the several intermontane valleys that dissect the area; and hot springs, which indicate that geothermal energy sources may underlie part of the area. Also, current (1978) speculation is that petroleum reserves may be present in the vicinity of Bear Lake. Development of more sprink- ler-irrigated lands, increases in population, and growth of phosphate mining are expected to place stress on the ground-water resources, both in quality and quantity.&nbsp;</p><p>The purpose of this report is to present the results of a study whose primary objectives were (1) to provide current waterquality data representative of the water in several different aquifers (water- bearing formations) in the study area, and (2) to relate these data to natural and manmade environmental controls. The wells sampled during this study establish a quasi-network, which could be resampled in the future to document and analyze changes (if any) in ground-water quality. Based on this information, planners and water managers could better understand the causeand-effect relations controlling water quality and could better manage land and water-resource development.</p><p>The report is designed for ease of reading and presentation. It uses maps, tables, and abbreviated text to describe geology, hydrology, and ground-water quality and how they are interrelated. Some practical ways for improving water quality are discussed for the benefit of individual water users. The field data collected in making the study are contained in the Data Section of this report.</p><p>The authors gratefully acknowledge the many individual well owners, municipal officials, and private industries that provided well information and allowed access to their properties and collection of water samples. Without their help, this work could not have been done. Water samples were collected at 103 well sites. Waterlevel measurements were made at 98 of these sites during July, August, and September of 1976.&nbsp;</p><p>This study was made by the U.S. Geological Survey in cooperation with the Idaho Department of Water Resources. A similar study is being made (1978) in north Idaho. Other studies are planned, specifically to obtain ground-water-quality data in areas where land and water-resource development is expected or accelerating.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7914","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources","usgsCitation":"Seitz, H.R., and Norvitch, R.F., 1979, Ground-water quality in Bannock, Bear Lake, Caribou, and part of Power counties, southeastern Idaho: U.S. Geological Survey Water-Resources Investigations Report 79-14, vii, 53 p., https://doi.org/10.3133/wri7914.","productDescription":"vii, 53 p.","costCenters":[],"links":[{"id":357118,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0014/report-thumb.jpg"}],"country":"United States","state":"Idaho","county":"Bannock County, Bear Lake County, Caribou County, Power County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.90924072265625,\n              42.004407212963585\n            ],\n            [\n              -111.04705810546874,\n              42.004407212963585\n            ],\n            [\n              -111.04705810546874,\n              43.068887774169625\n            ],\n            [\n              -112.90924072265625,\n              43.068887774169625\n            ],\n            [\n              -112.90924072265625,\n              42.004407212963585\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66726f","contributors":{"authors":[{"text":"Seitz, Harold R.","contributorId":61814,"corporation":false,"usgs":true,"family":"Seitz","given":"Harold","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norvitch, Ralph F.","contributorId":65456,"corporation":false,"usgs":true,"family":"Norvitch","given":"Ralph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":201910,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9938,"text":"ofr79203 - 1979 - Hydrologic data, 1974-77, Stovepipe Wells Hotel area, Death Valley National Monument, Inyo County, California","interactions":[],"lastModifiedDate":"2025-12-29T15:10:38.975673","indexId":"ofr79203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-203","title":"Hydrologic data, 1974-77, Stovepipe Wells Hotel area, Death Valley National Monument, Inyo County, California","docAbstract":"<p>Ground-water levels in most wells did not change significantly from 1974 to 1977 in the Stovepipe Wells Hotel area. The average water-level decline was less than 0.10 foot between August 1974 and August 1977 in 10 observation wells. Water-level contours show a depression centered on the two pumping wells, but this depression existed before the National Park Service started pumping its well.</p><p>The chemical quality of the ground water is poor. Dissolved-solids concentrations in water samples ranged from 2,730 to 6,490 milligrams per liter. Analyses of water samples from two wells showed large changes in some constituents from 1976 to 1977. Water-quality monitoring will continue at these sites to verify the changes.</p><p>Streamflow in Salt Creek has been monitored since February 1974. Base flow is seasonal, being 0.10 to 0.20 cubic foot per second during the summer and as much as three times that amount during the winter. Two chemical analyses of water from Salt Creek, representing summer and winter flow conditions, show large differences for many constituents.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79203","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Lamb, C.E., and Downing, D., 1979, Hydrologic data, 1974-77, Stovepipe Wells Hotel area, Death Valley National Monument, Inyo County, California: U.S. Geological Survey Open-File Report 79-203, iv, 19 p., https://doi.org/10.3133/ofr79203.","productDescription":"iv, 19 p.","costCenters":[],"links":[{"id":498096,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0203/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143191,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0203/report-thumb.jpg"}],"country":"United States","state":"California","county":"Inyo County","otherGeospatial":"Death Valley National 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,{"id":9557,"text":"ofr791163 - 1979 - Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo sandstone","interactions":[{"subject":{"id":9557,"text":"ofr791163 - 1979 - Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo sandstone","indexId":"ofr791163","publicationYear":"1979","noYear":false,"title":"Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo sandstone"},"predicate":"SUPERSEDED_BY","object":{"id":70043754,"text":"70043754 - 1981 - Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone","indexId":"70043754","publicationYear":"1981","noYear":false,"title":"Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone"},"id":1}],"supersededBy":{"id":70043754,"text":"70043754 - 1981 - Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone","indexId":"70043754","publicationYear":"1981","noYear":false,"title":"Bedrock aquifers in the lower Dirty Devil River basin area, Utah, with special emphasis on the Navajo sandstone"},"lastModifiedDate":"2025-12-29T15:46:44.414142","indexId":"ofr791163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1163","title":"Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo sandstone","docAbstract":"<p>The lower Dirty Devil River basin area in southeastern Utah has an area of about 4,300 square miles (11,1140 square kilometers) and ranges in altitude from about 3,700 to more than 11,000 feet (1,130 to 3,350 meters) above mean sea level. Precipitation, the main source of water in the area, ranges from slightly less than 6 inches (152 millimeters) per year in the lowlands to more than 30 inches per year (762 millimeters) in the Henry Mountains and along the western boundary.</p><p>Rocks that crop out in or underlie the area range from the Precambrian to the Holocene in age. The thickness of the composite section of sedimentary rocks ranges from about 7,300 feet (2,200 meters) to about 23,000 feet (7,000 meters). The Entrada, Navajo, Wingate, and Coconino Sandstones and rocks of Mississippian age are considered major aquifers because of their large areal extent or thickness or their known locally large yields to wells. The chemical quality of the water in these aquifers ranges from fresh to briny.</p><p>The permeability of the aquifers in the area is affected by folding, faulting, and igneous intrusion. These geologic processes have locally enhanced ground-water circulation by fracturing or impeded circulation by offsetting permeable beds or sealing some zones with rocks of lower permeability.</p><p>The total hydrologic system in the lower Dirty Devil River basin has estimated long-term average annual inflow and outflow of about 1.6 million acre-feet (1,970 cubic hectometers), of which about 1.55 million acre-feet (1,910 cubic hectometers) is derived from precipitation. An estimated 96 percent of the water available to the area is consumed by evapotranspiration.</p><p>The estimated gross annual average ground-water recharge is 34,000 acre-feet (42 cubic hectometers), of which 5,000 acre-feet (6.2 cubic hectometers) recharges the Navajo Sandstone. Recoverable fresh to moderately saline water stored in the Navajo, Wingate, and Coconino Sandstones is estimated to be 210 million acre-feet (259,000 cubic hectometers), of which 89 million acre-feet (110,000 cubic hectometers) is stored in the Navajo alone.</p><p>Long-term large withdrawals from the Navajo Sandstone are feasible. Withdrawal of 12,000 gallons per minute (757 liters per second) over a period of about 36 years probably would diminish the amount of water in storage by less than 1 percent. The withdrawals, would eventually diminish the average annual discharge of the Dirty Devil River by possibly as much as 13 cubic feet per second (0.37 cubic meter per second). A change of this magnitude on the flow of the Colorado River would be too small to measure.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791163","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., and Danielson, T.W., 1979, Bedrock aquifers in the lower Dirty Devil River Basin area, Utah, with special emphasis on the Navajo sandstone: U.S. Geological Survey Open-File Report 79-1163, Report: 175 p.; 14 Figures: 25.47 x 33.30 inches or smaller; 26 Tables: 17.15 x 22.36 inches or smaller, https://doi.org/10.3133/ofr791163.","productDescription":"Report: 175 p.; 14 Figures: 25.47 x 33.30 inches or smaller; 26 Tables: 17.15 x 22.36 inches or smaller","costCenters":[],"links":[{"id":498132,"rank":32,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1979/1163/table-7-1.pdf","text":"Table 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W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":159885,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69594,"text":"i1157 - 1979 - Geologic and hydrologic aspects of tunneling in the Twin Cities area, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:39:07","indexId":"i1157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1157","title":"Geologic and hydrologic aspects of tunneling in the Twin Cities area, Minnesota","docAbstract":"<p>This report presents the results of a pilot study of geologic and hydrologic aspects of tunneling in part of the Minneapolis-St. Paul (Twin Cities) metropolitan area, Minnesota. The Minnesota Geological Survey collected, compiled and interpreted geologic and engineering-test data and the U.S. Geological Survey complies and interpreted hydrologic data. The report was prepared on behalf of the U.S. Department of Transportation and funding was provided by that agency. A similar pilot study was recently made in the Los Angeles area, California (Yerkes and others, 1977).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1157","collaboration":"Prepared in cooperation with the Minnesota Geological Survey and the United States Department of Transportation","usgsCitation":"Norvitch, R.F., and Walton, M., 1979, Geologic and hydrologic aspects of tunneling in the Twin Cities area, Minnesota: U.S. Geological Survey IMAP 1157, 7 Plates: 43.26 x 31.91 inches or smaller, https://doi.org/10.3133/i1157.","productDescription":"7 Plates: 43.26 x 31.91 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":191275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-1.pdf","size":"9190","linkFileType":{"id":1,"text":"pdf"}},{"id":101479,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-2.pdf","size":"12201","linkFileType":{"id":1,"text":"pdf"}},{"id":101480,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-3.pdf","size":"11712","linkFileType":{"id":1,"text":"pdf"}},{"id":101481,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-4.pdf","size":"7732","linkFileType":{"id":1,"text":"pdf"}},{"id":101482,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-5.pdf","size":"5700","linkFileType":{"id":1,"text":"pdf"}},{"id":101483,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-6.pdf","size":"10351","linkFileType":{"id":1,"text":"pdf"}},{"id":101484,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1157/plate-7.pdf","size":"7381","linkFileType":{"id":1,"text":"pdf"}},{"id":106624,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8998.htm","linkFileType":{"id":5,"text":"html"},"description":"8998"}],"scale":"24000","country":"United States","state":"Minnesota","city":"Minneapolis-St. Paul","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.325,\n              45.016667\n            ],\n            [\n              -93.245833,\n              45.016667\n            ],\n            [\n              -93.041667,\n              44.970833\n            ],\n            [\n              -93.041667,\n              44.925\n            ],\n            [\n              -93.325,\n              44.925\n            ],\n            [\n              -93.325,\n              45.016667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8246","contributors":{"authors":[{"text":"Norvitch, Ralph F.","contributorId":65456,"corporation":false,"usgs":true,"family":"Norvitch","given":"Ralph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":280693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walton, Matt S.","contributorId":16932,"corporation":false,"usgs":true,"family":"Walton","given":"Matt S.","affiliations":[],"preferred":false,"id":280692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":45940,"text":"ofr79521 - 1979 - Hydrologic overlay maps of the Tropic Quadrangle, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"ofr79521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-521","title":"Hydrologic overlay maps of the Tropic Quadrangle, Florida","language":"ENGLISH","doi":"10.3133/ofr79521","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1979, Hydrologic overlay maps of the Tropic Quadrangle, Florida: U.S. Geological Survey Open-File Report 79-521, 5 maps ;80 x 55 cm., https://doi.org/10.3133/ofr79521.","productDescription":"5 maps ;80 x 55 cm.","costCenters":[],"links":[{"id":167999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606533","contributors":{"authors":[{"text":"Frazee, James M. Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":232346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":232345,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","interactions":[{"subject":{"id":10049,"text":"ofr7818 - 1977 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah","indexId":"ofr7818","publicationYear":"1977","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley playa, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2129,"text":"wsp2057 - 1979 - Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","indexId":"wsp2057","publicationYear":"1979","noYear":false,"title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah"},"id":1}],"lastModifiedDate":"2017-09-03T10:07:56","indexId":"wsp2057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2057","title":"Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah","docAbstract":"<p>The Bonneville Salt Flats and Pilot Valley are in the western part of the Great Salt Lake Desert in northwest Utah. The areas are separate, though similar, hydrologic basins, and both contain a salt crust. The Bonneville salt crust covered about 40 square miles in the fall of 1976, and the salt crust in Pilot Valley covered 7 square miles. Both areas lack any noticeable surface relief (in 1976, 1.3 feet on the Bonneville salt crust and 0.3 foot on the Pilot Valley salt crust).</p><p>The salt crust on the Salt Flats has been used for many years for automobile racing, and brines from shallow lacustrine deposits have been used for the production of potash. In recent years, there has been an apparent conflict between these two major uses of the area as the salt crust has diminished in both thickness and extent. Much of the Bonneville Racetrack has become rougher, and there has also been an increase in the amount of sediment on the south end of the racetrack. The Pilot Valley salt crust and surrounding playa have been largely unused.</p><p>Evaporite minerals on the Salt Flats and the Pilot Valley playa are concentrated in three zones: (1) a carbonate zone composed mainly of authigenic clay-size carbonate minerals, (2) a sulfate zone composed mainly of authigenic gypsum, and (3) a chloride zone composed of crystalline halite (the salt crust). Five major types of salt crust were recognized on the Salt Flats, but only one type was observed in Pilot Valley. Geomorphic differences in the salt crust are caused by differences in their hydrologic environments. The salt crusts are dynamic features that are subject to change because of climatic factors and man's activities.</p><p>Ground water occurs in three distinct aquifers in much of the western Great Salt Lake Desert: (1) the basin-fill aquifer, which yields water from conglomerate in the lower part of the basin fill, (2) the alluvial-fan aquifer, which yields water from sand and gravel along the western margins of both playas, and (3) the shallow-brine aquifer, which yields water from near-surface carbonate muds and crystalline halite and gypsum. The shallow-brine aquifer is the main source of brine used for the production of potash on the Salt Flats.</p><p>Recharge to that part of the shallow-brine aquifer north of Interstate Highway 80 on the Salt Flats is mainly by infiltration of precipitation and wind-driven floods of surface brine. Discharge was mainly by evaporation at the playa surface and withdrawals from brine-collection ditches. Some water was transpired by phreatophytes, and some leaked into the alluvial fan along the western edge of the playa.</p><p>Salt-scraping studies indicate that the amount of halite on the Salt Flats is directly related to the amount of recharge through the surface (which causes re-solution of halite) and the amount of evaporation at the surface (which causes crystallization of halite). Evaporation rates through sediment-covered salt crust and the gypsum surface were estimated at between 3x10<sup>-4</sup> and 4x10<sup>-3</sup> inches per day during the summer and fall of 1976. Evaporation rates through the surface of thick perennial salt crust were much higher.</p><p>The concentration of dissolved solids in brine in the shallow-brine aquifer varies, but it generally increases from the edges of the playas toward areas of salt crust. Dissolved-solids concentration in the shallow brine ranges from less than 100,000 to more than 300,000 milligrams per liter on both playas. The increase in salinity toward areas of salt crust reflects the natural direction of brine movement through the aquifer toward the natural discharge area.</p><p>On the Salt Flats, the percentages of dissolved potassium chloride and magnesium chloride in the shallow-brine aquifer generally increase from the edge of the playa to- ward the salt crust. The relative enrichment in potassium and magnesium reflects the many years of subsurface drainage toward the main discharge area (the salt crust) prior to man's withdrawal of brine. By artificially extracting brines from the carbonate muds, the percentages of potassium and magnesium have decreased while brine salinity has been maintained by re-solution of the salt crust.</p><p>The configuration of the density-corrected potentiometric surface in the fall of 1976 indicates that brine in the shallow-brine aquifer under the Bonneville Racetrack was draining toward brine-collection ditches or a well field to the west. Ground-water divides have no effect on the movement of dissolved salt across the surface in wind-driven floods, and salt in surface brine was carried from the racetrack into the area of influence of the ditches by such surface movement. During 1976 on the Salt Flats, some brine was moving through the shallow-brine aquifer across lease and property boundaries.</p><p>An evaluation of suggested remedial measures indicates that none will completely eliminate the conflict between uses or transform the Bonneville Salt Flats to its original state prior to man's activities in the area.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2057","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lines, G.C., 1979, Hydrology and surface morphology of the Bonneville Salt Flats and Pilot Valley Playa, Utah: U.S. Geological Survey Water Supply Paper 2057, vii, 107 p., https://doi.org/10.3133/wsp2057.","productDescription":"vii, 107 p.","numberOfPages":"117","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2057/report-thumb.jpg"},{"id":27729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Bonneville Salt Flats, Pilot Valley Playa","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e898","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2181,"text":"wsp1532J - 1979 - Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado","interactions":[{"subject":{"id":10116,"text":"ofr78289 - 1978 - Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado","indexId":"ofr78289","publicationYear":"1978","noYear":false,"title":"Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":2181,"text":"wsp1532J - 1979 - Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado","indexId":"wsp1532J","publicationYear":"1979","noYear":false,"chapter":"J","title":"Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado"},"id":1}],"lastModifiedDate":"2023-01-05T22:44:43.288576","indexId":"wsp1532J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1532","chapter":"J","title":"Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado","docAbstract":"Changes in runoff and sediment yield caused by changing sagebrush cover to grass \r\ncover were studied at four small watersheds in western Colorado during a 9-year \r\nperiod, from 1965 to 1978. Measurements of runoff and sediment yield from the four \r\nwatersheds were made for 8 years, at which time two watersheds were plowed and \r\nseeded to beardless bluebunch wheatgrass. The same measurements were then continued for an additional 6 years. \r\n\r\nMeasurements indicated that conversion to grass caused a reduction in runoff from \r\nsummer rainstorms of about 75 percent. Runoff from spring snowmelt increased about \r\n12 percent, and annual runoff from treated watersheds decreased about 20 percent \r\nwhen compared to control watersheds. Sediment yield from the seeded watersheds was \r\nreduced by about 80 percent; most of this reduction is related to the decrease in runoff \r\nfrom summer rainstorms. \r\n\r\nThe size of barren interspaces between plants was reduced on the converted water- \r\nsheds to about 30 percent of those on the untreated watersheds. Linear regression \r\nanalysis indicates that a reduction of 38 percent in the amount of bare soil resulting \r\nfrom planting grass would result in a decrease of 73 percent in sediment concentration.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1532J","usgsCitation":"Lusby, G.C., 1979, Effects of converting sagebrush cover to grass on the hydrology of small watersheds at Boco Mountain, Colorado: U.S. Geological Survey Water Supply Paper 1532, Report: iv, 36 p.; 1 Plate: 19.00 x 15.80 inches, https://doi.org/10.3133/wsp1532J.","productDescription":"Report: iv, 36 p.; 1 Plate: 19.00 x 15.80 inches","costCenters":[],"links":[{"id":109969,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24713.htm","linkFileType":{"id":5,"text":"html"},"description":"24713"},{"id":27804,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27803,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138237,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532j/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Boco Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.687,\n              39.75\n            ],\n            [\n              -106.687,\n              39.739\n            ],\n            [\n              -106.667,\n              39.739\n            ],\n            [\n              -106.667,\n              39.75\n            ],\n            [\n              -106.687,\n              39.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2fe4b07f02db615f56","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144785,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2182,"text":"wsp1532I - 1979 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","interactions":[{"subject":{"id":10117,"text":"ofr78165 - 1978 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","indexId":"ofr78165","publicationYear":"1978","noYear":false,"title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73"},"predicate":"SUPERSEDED_BY","object":{"id":2182,"text":"wsp1532I - 1979 - Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","indexId":"wsp1532I","publicationYear":"1979","noYear":false,"chapter":"I","title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73"},"id":1}],"lastModifiedDate":"2022-01-07T19:50:06.11252","indexId":"wsp1532I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1532","chapter":"I","title":"Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrologic effects of land use","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1532I","usgsCitation":"Lusby, G.C., 1979, Effects of grazing on runoff and sediment yield from desert rangeland at Badger Wash in western Colorado, 1953-73: U.S. Geological Survey Water Supply Paper 1532, Report: iv, I34 p.; Plate, 19.00 x 12.00 inches, https://doi.org/10.3133/wsp1532I.","productDescription":"Report: iv, I34 p.; Plate, 19.00 x 12.00 inches","costCenters":[],"links":[{"id":394049,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24712.htm"},{"id":138238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532i/report-thumb.jpg"},{"id":27805,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27806,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Badger Wash","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.948,\n              39.292\n            ],\n            [\n              -108.91,\n              39.292\n            ],\n            [\n              -108.91,\n              39.356\n            ],\n            [\n              -108.948,\n              39.356\n            ],\n            [\n              -108.948,\n              39.292\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62564f","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3789,"text":"cir809 - 1979 - Status of surface-water modeling in the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir809","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"809","title":"Status of surface-water modeling in the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey is active in the development and use of models for the analysis of various types of surface-water problems. Types of problems for which models have been, or are being developed, include categories such as the following: (1)specialized hydraulics, (2)flow routing in streams, estuaries, lakes, and reservoirs, (3) sedimentation, (4) transport of physical, chemical, and biological constituents, (5) surface exchange of heat and mass, (6) coupled stream-aquifer flow systems, (7) physical hydrology for rainfall-runoff relations, stream-system simulations, channel geometry, and water quality, (8) statistical hydrology for synthetic streamflows, floods, droughts, storage, and water quality, (9) management and operation problems, and (10) miscellaneous hydrologic problems. Following a brief review of activities prior to 1970, the current status of surface-water modeling is given as being in a developmental, verification, operational, or continued improvement phase. A list of recently published selected references, provides useful details on the characteristics of models.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir809","usgsCitation":"Jennings, M.E., and Yotsukura, N., 1979, Status of surface-water modeling in the U.S. Geological Survey: U.S. Geological Survey Circular 809, iii, 17 p. ; 26 cm., https://doi.org/10.3133/cir809.","productDescription":"iii, 17 p. ; 26 cm.","costCenters":[],"links":[{"id":124686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0809/report-thumb.jpg"},{"id":30861,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0809/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a10b","contributors":{"authors":[{"text":"Jennings, Marshall E.","contributorId":55813,"corporation":false,"usgs":true,"family":"Jennings","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yotsukura, Nobuhiro","contributorId":81884,"corporation":false,"usgs":true,"family":"Yotsukura","given":"Nobuhiro","email":"","affiliations":[],"preferred":false,"id":147605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4839,"text":"pp1044E - 1979 - Hydrology and geochemistry of thermal springs of the Appalachians","interactions":[],"lastModifiedDate":"2025-04-17T16:40:09.657827","indexId":"pp1044E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"E","title":"Hydrology and geochemistry of thermal springs of the Appalachians","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044E","usgsCitation":"Hobba, W., Fisher, D., Pearson, F.J., and Chemerys, J., 1979, Hydrology and geochemistry of thermal springs of the Appalachians: U.S. Geological Survey Professional Paper 1044, 36 p., https://doi.org/10.3133/pp1044E.","productDescription":"36 p.","costCenters":[],"links":[{"id":31776,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117266,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605067","contributors":{"authors":[{"text":"Hobba, W.A. Jr.","contributorId":77518,"corporation":false,"usgs":true,"family":"Hobba","given":"W.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":149895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, D.W.","contributorId":77519,"corporation":false,"usgs":true,"family":"Fisher","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":149896,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pearson, F. J. Jr.","contributorId":7696,"corporation":false,"usgs":true,"family":"Pearson","given":"F.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chemerys, J.C.","contributorId":94293,"corporation":false,"usgs":true,"family":"Chemerys","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":149897,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6162,"text":"pp1130 - 1979 - Hydrologic and human aspects of the 1976-77 drought","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1130","title":"Hydrologic and human aspects of the 1976-77 drought","docAbstract":"The drought of 1976-77 was the most severe in at least 50 years in many parts of the United States. Record low amounts of rainfall, snowfall, and runoff, and increased withdrawals of ground water were prevalent. The use of carry-over storage in reservoirs during 1976 maintained streamflow at near normal levels, but some reservoirs went dry or dropped below the outlet works in 1977. Carry-over storage in the fall of 1977 was very low. Ground-water levels were at or near record low levels in many aquifers, hundreds of wells went dry, and thousands of wells were drilled. Yet no wide-spread deterioration of ground-water quality was reported. Water-quality problems arose in some streams and lakes, but most were localized and of short duration. Water rationing became a way of life in numerous areas , and water was hauled in many rural areas and to a few towns. Water use was affected by legal agreements or decisions, some of which were modified for the duration of the drought, and by the inability of water managers to efficiently manage surface and ground waters as one resource under existing law. There are still many drought related problems to solve and many challenges to be met before the next drought occurs. The advancement of techniques in many fields of endeavor in recent years plus ongoing, planned, and proposed research on drought and the risks involved are promising thrusts that should make it easier to cope with the next drought. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1130","usgsCitation":"Matthai, H.F., 1979, Hydrologic and human aspects of the 1976-77 drought: U.S. Geological Survey Professional Paper 1130, 84 p., https://doi.org/10.3133/pp1130.","productDescription":"84 p.","costCenters":[],"links":[{"id":126668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1130/report-thumb.jpg"},{"id":33266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687f83","contributors":{"authors":[{"text":"Matthai, Howard F.","contributorId":106491,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":152222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6187,"text":"pp1087 - 1979 - Maine coastal storm and flood of February 2, 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp1087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1087","title":"Maine coastal storm and flood of February 2, 1976","docAbstract":"A business section of Bangor, Maine, was flooded with 12 feet (3.7 m) of water on February 2, 1976. The water surface elevation reached 17.46 feet (5.32 m) above national geodetic vertical datum of 1929 (NGVD), approximately 10.5 feet (3.2 m) above the predicted astronomical tide at Bangor. The unusually high water resulted from a tidal storm surge caused by prolonged strong, south-southeasterly winds which occurred near the time of astronomical high tide. Winds exceeded 64 knots off the New England coast. The resulting flood was the third highest since 1846 and is the first documented tidal flood at Bangor. This report documents the meteorological and hydrologic conditions associated with the flooding and also contains a brief description of storm damage from Eastport to Brunswick, Maine. Included are flood elevations in the city of Bangor and along the coast of Maine east of the Kennebec River. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1087","usgsCitation":"Morrill, R.A., Chin, E.H., and Richardson, W., 1979, Maine coastal storm and flood of February 2, 1976: U.S. Geological Survey Professional Paper 1087, 20 p., https://doi.org/10.3133/pp1087.","productDescription":"20 p.","costCenters":[],"links":[{"id":104548,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4716.htm","linkFileType":{"id":5,"text":"html"},"description":"4716"},{"id":117292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1087/report-thumb.jpg"},{"id":33319,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33320,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1087/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496b0","contributors":{"authors":[{"text":"Morrill, Richard Arthur","contributorId":73200,"corporation":false,"usgs":true,"family":"Morrill","given":"Richard","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":152256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chin, Edwin H.","contributorId":87921,"corporation":false,"usgs":true,"family":"Chin","given":"Edwin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richardson, W.S.","contributorId":50150,"corporation":false,"usgs":true,"family":"Richardson","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":152255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7106,"text":"ofr791185 - 1979 - Dynamics of the Continental Crust: suggestions for U.S. Geological Survey research in the 1980's","interactions":[],"lastModifiedDate":"2023-08-28T16:32:57.219712","indexId":"ofr791185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1185","title":"Dynamics of the Continental Crust: suggestions for U.S. Geological Survey research in the 1980's","docAbstract":"<p>Crustal dynamics--the study of the movement of mass and energy within, into, and out of the Earth's crust--encompasses most efforts of earth science, either directly or as background and support. A new international program is being formulated to promote cooperative development of the concepts required to solve proliferating problems created by intensifying human use and misuse of the land and its resources. A tentative title suggested by the U.S. Geodynamics Committee for this program for the decade of the 1980's is \"Crustal Dynamics: A Framework for Resources.\" The needs are pressing at both the national and international levels. Many reasons cited for undertaking this international program are akin to the justifications for forming, maintaining, or enlarging governmental geological surveys. Thus, the U.S. Geological Survey has an obligation to participate in the Crustal Dynamics Program to meet its expanding responsibilities to serve the nation effectively.</p><p>A U.S. Geological Survey workshop was convened near Denver on September 20-23, 1978, to consider appropriate roles that might be played in the Crustal Dynamics decade. Some 60 Survey geologists, geophysicists, geochemists, and hydrologists participated. Principal questions addressed were: 1) What are the major earth-science problems that should be investigated during the next decade? 2) What are their implications to society? 3) What competence can be brought to bear on these problems and what further competence and tools need to be developed? 4) What roles are appropriate for the USGS within the broader national and international earth-science communities?</p><p>This report presents some responses to these questions. Readers may recognize some defects. The report was prepared by several committees and its sections remain uneven despite editing. Insufficient time was available for either lengthy consideration or discussions, and no opportunity was provided for communication with colleagues in other organizations. The report is not a finished proposal for USGS participation in the Crustal Dynamics program, but rather is intended as a basis for further discussion and consideration both within the organization and with colleagues in other institutions and organizations, toward formulation of a viable program.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791185","usgsCitation":"Lipman, P.W., Eaton, G.P., Hamilton, W., Oriel, S.S., and Pakiser, L., 1979, Dynamics of the Continental Crust: suggestions for U.S. Geological Survey research in the 1980's: U.S. Geological Survey Open-File Report 79-1185, vi, 92 p., https://doi.org/10.3133/ofr791185.","productDescription":"vi, 92 p.","costCenters":[],"links":[{"id":420186,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1185/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140446,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1185/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697dad","contributors":{"authors":[{"text":"Lipman, Peter W. 0000-0001-9175-6118 plipman@usgs.gov","orcid":"https://orcid.org/0000-0001-9175-6118","contributorId":3486,"corporation":false,"usgs":true,"family":"Lipman","given":"Peter","email":"plipman@usgs.gov","middleInitial":"W.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":154318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, Gordon P.","contributorId":67077,"corporation":false,"usgs":true,"family":"Eaton","given":"Gordon","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":154322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamilton, Warren","contributorId":14819,"corporation":false,"usgs":true,"family":"Hamilton","given":"Warren","affiliations":[],"preferred":false,"id":154319,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154320,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pakiser, Louis C.","contributorId":44789,"corporation":false,"usgs":true,"family":"Pakiser","given":"Louis C.","affiliations":[],"preferred":false,"id":154321,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7224,"text":"ofr791493 - 1979 - Hydrologic and climatologic data, southeastern Uinta Basin, Utah and Colorado, water year 1977","interactions":[],"lastModifiedDate":"2017-09-02T14:13:37","indexId":"ofr791493","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1493","title":"Hydrologic and climatologic data, southeastern Uinta Basin, Utah and Colorado, water year 1977","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr791493","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, the U.S. Bureau of Land Management, and the U.S. Environmental Protection Agency","usgsCitation":"Conroy, L.S., 1979, Hydrologic and climatologic data, southeastern Uinta Basin, Utah and Colorado, water year 1977: U.S. Geological Survey Open-File Report 79-1493, iv, 193 p., https://doi.org/10.3133/ofr791493.","productDescription":"iv, 193 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":140681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94478,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015010182643?urlappend=%3Bseq=5"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611880","contributors":{"authors":[{"text":"Conroy, Loretta S.","contributorId":178482,"corporation":false,"usgs":true,"family":"Conroy","given":"Loretta","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":154824,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7231,"text":"ofr791676 - 1979 - Hydrologic data from selected wells in the Helena Valley, Lewis and Clark County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr791676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1676","title":"Hydrologic data from selected wells in the Helena Valley, Lewis and Clark County, Montana","docAbstract":"Hydrologic data were collected during 1978-79 to aid in evaluating the hydrologic conditions in shallow aquifers beneath the Helena Valley, Montana. The locations of 52 shallow test wells augered during the study are shown on a map at a scale of 1:48,000. Periodic water-level measurements and water-quality analyses for the test holes are listed in tables. Water temperature, specific conductance, and nitrate concentration are given for water samples collected from 98 domestic wells, and chemical analyses are included for 11 domestic and irrigation wells. In addition, water-level drawdown and recovery data are plotted on graphs for five pumped wells and three observation wells. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791676","usgsCitation":"Moreland, J.A., Leonard, R.B., Reed, T., Clausen, R., and Wood, W., 1979, Hydrologic data from selected wells in the Helena Valley, Lewis and Clark County, Montana: U.S. Geological Survey Open-File Report 79-1676, iii, 57 p., 1 over-size sheet ;27 cm., https://doi.org/10.3133/ofr791676.","productDescription":"iii, 57 p., 1 over-size sheet ;27 cm.","costCenters":[],"links":[{"id":139940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1676/report-thumb.jpg"},{"id":34624,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1676/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1676/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607771","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":154845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, R. B.","contributorId":32917,"corporation":false,"usgs":true,"family":"Leonard","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":154844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, T.E.","contributorId":86329,"corporation":false,"usgs":true,"family":"Reed","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":154846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clausen, R.O.","contributorId":89519,"corporation":false,"usgs":true,"family":"Clausen","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":154847,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, W.A.","contributorId":6048,"corporation":false,"usgs":true,"family":"Wood","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":154843,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7233,"text":"ofr79988 - 1979 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","interactions":[{"subject":{"id":7233,"text":"ofr79988 - 1979 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"ofr79988","publicationYear":"1979","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"wsp2068","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"id":1}],"supersededBy":{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"wsp2068","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"lastModifiedDate":"2025-04-17T18:42:02.595363","indexId":"ofr79988","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-988","title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","docAbstract":"<p>Data obtained during a hydrologic reconnaissance in 1975-77 in the Wasatch Plateau-Book Cliffs coal area of Utah were correlated with existing long-term data. Maps were prepared showing average precipitation, average streamflow, stream temperature, ground- and surface-water quality, sediment yield, and geology. Recommendations were made for additional study and suggested approaches for continued monitoring in the coal areas.<br></p><p>During the 1931-75 water years, the minimum discharges for the five major streams that head in the area ranged from about 12,000 to 26,000 acre-feet per year, and the maximum discharges ranged from about 59,000 to 315,000 acre-feet per year. Correlations indicate that 3 years of low-flow records at stream sites in the Wasatch Plateau would allow the development of relationships with long-term sites that can be used to estimate future low-flow records within a standard error of about 20 percent.<br></p><p>Most water-quality degradation in streams occurs along the flanks of the Wasatch Plateau and Book Cliffs. In the uplands, dissolved-solids concentrations generally ranged from less than 100 to about 250 milligrams per liter, and in the lowlands the concentrations ranged from about 250 to more than 6,000 milligrams per liter.<br></p><p>In the lowland areas, the Ferron Sandstone Member of the Mancos Shale appears to have the most potential for subsurface development of water of suitable chemical quality for human consumption. Three wells in the Ferron yielded water with dissolved-solids concentrations ranging from about 650 to 1,230 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79988","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management and the U.S. Environmental Protection Agency","usgsCitation":"Waddell, K., Contratto, P., Sumsion, C.T., and Butler, J.R., 1979, Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah: U.S. Geological Survey Open-File Report 79-988, Report: 85 p. ; 15 Figures: 40.36 x 26.85 inches or smaller; 8 Tables, https://doi.org/10.3133/ofr79988.","productDescription":"Report: 85 p. ; 15 Figures: 40.36 x 26.85 inches or smaller; 8 Tables","costCenters":[],"links":[{"id":484732,"rank":25,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-20.pdf","text":"Figure 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16","linkFileType":{"id":1,"text":"pdf"}},{"id":484726,"rank":19,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-15.pdf","text":"Figure 15","linkFileType":{"id":1,"text":"pdf"}},{"id":484725,"rank":18,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-13-2.pdf","text":"Figure 13-2","linkFileType":{"id":1,"text":"pdf"}},{"id":484724,"rank":17,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-13-1.pdf","text":"Figure 13-1","linkFileType":{"id":1,"text":"pdf"}},{"id":484723,"rank":16,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-11.pdf","text":"Figure 11","linkFileType":{"id":1,"text":"pdf"}},{"id":484722,"rank":15,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1979/0988/figure-8.pdf","text":"Figure 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T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":154853,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, John R.","contributorId":36540,"corporation":false,"usgs":true,"family":"Butler","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":154854,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7365,"text":"ofr791062 - 1979 - A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","interactions":[],"lastModifiedDate":"2023-11-24T19:31:09.75019","indexId":"ofr791062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1062","title":"A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana","docAbstract":"<p>The Indiana State Board of Health is developing a State water-quality management plan that includes the establishing of limits for wastewater effluents discharged into Indiana streams. A digital model calibrated to conditions in Cedar Creek was used to develop alternatives for future waste loadings that would be compatible with Indiana stream water-quality standards defined for two critical hydrologic conditions, summer and winter low flows. All point-source waste loads affecting Cedar Creek are in the four incorporated municipalities of Auburn, Garrett, Huntertown, and Waterloo, in a primarily agricultural area. Avilla, because of its distance from Cedar Creek, does not significantly affect the water quality of the modeled segment.</p><p>The model indicates that the dissolved-oxygen concentration of the Auburn wastewater effluent and nitrification are the most significant factors affecting the dissolved-oxygen concentration in Cedar Creek during summer low flows. The observed dissolved-oxygen concentration of the Auburn wastewater effluent was low, and averaged 30 percent of saturation. Whether the effluent is aerated before discharge will ultimately define the waste-load assimilative capacity of Cedar Creek. Projected nitrogenous biochemical-oxygen demand loads, from the Indiana State Board of Health, for the Auburn and Waterloo wastewater-treatment facilities will result in violations of the current instream dissolved-oxygen standard (5 milligrams per liter), even with an effluent dissolved-oxygen concentration of 80 percent saturation.</p><p>Natural streamflow for Cedar Creek upstream from the confluence of Willow and Little Cedar Creeks is small compared with the waste discharge, so benefits of dilution for Waterloo and Auburn are minimal. Stream reaeration capacity is not sufficient to maintain an average dissolved-oxygen concentration of at least 5 milligrams per liter, the State's water-quality standard for streams.</p><p>The model also indicates that, during winter low flows, ammonia toxicity, rather than dissolved oxygen, is the limiting water-quality criterion in the reach of Cedar Creek downstream from the wastewater-treatment facility at Auburn and the confluence of Garrett ditch. Ammonia-nitrogen concentrations predicted for 2978 through 2000 downstream from the Waterloo wastewater-treatment facility do not exceed Indiana water-quality standards for streams.</p><p>Calculations of the stream's assimilative capacity indicate that future waste discharge in the Cedar Creek basin will be limited to the reaches between the Auburn wastewater-treatment facility and County Road 68.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791062","collaboration":"Prepared in cooperation with the Indiana State Board of Health","usgsCitation":"Wilber, W.G., Peters, J.G., Ayers, M.A., and Crawford, C.G., 1979, A one-dimensional, steady-state dissolved-oxygen model and waste-load assimilation study for Cedar Creek, Dekalb and Allen counties, Indiana: U.S. Geological Survey Open-File Report 79-1062, viii, 79 p., https://doi.org/10.3133/ofr791062.","productDescription":"viii, 79 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":422925,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1062/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Allen County, Dekalb County","otherGeospatial":"Cedar Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85.38216090798966,\n              41.60787742256892\n            ],\n            [\n              -85.38216090798966,\n              41.14208690200232\n            ],\n            [\n              -84.81087184548976,\n              41.14208690200232\n            ],\n            [\n              -84.81087184548976,\n              41.60787742256892\n            ],\n            [\n              -85.38216090798966,\n              41.60787742256892\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb2c","contributors":{"authors":[{"text":"Wilber, William G. wgwilber@usgs.gov","contributorId":297,"corporation":false,"usgs":true,"family":"Wilber","given":"William","email":"wgwilber@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":155417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, James G.","contributorId":69137,"corporation":false,"usgs":true,"family":"Peters","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ayers, Mark A.","contributorId":84730,"corporation":false,"usgs":true,"family":"Ayers","given":"Mark","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155419,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":155418,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7429,"text":"ofr79745 - 1979 - Preliminary data for Madison Limestone test well 3, NW 1/4 Sec. 35. T. 2 N., R. 27 E., Yellowstone County, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr79745","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-745","title":"Preliminary data for Madison Limestone test well 3, NW 1/4 Sec. 35. T. 2 N., R. 27 E., Yellowstone County, Montana","docAbstract":"This report provides preliminary data for Madison Limestone test well 3 in Yellowstone County, Mont., including test-well history , geology of the test well, hydrologic testing, and geochemistry. It also discusses the preliminary results and future testing. The test well was drilled as part of the study to determine the water-resource potential of the Madison Limestone and associated rocks to meet future water needs in a 188,000-square-mile region that includes the coal-rich area of the Northern Great Plains. Drilling and testing were designed to yield a maximum of stratigraphic, structural, geophysical, and hydrologic information. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79745","usgsCitation":"Blankennagel, R.K., Howells, L., Miller, W.R., and Hansen, C.V., 1979, Preliminary data for Madison Limestone test well 3, NW 1/4 Sec. 35. T. 2 N., R. 27 E., Yellowstone County, Montana: U.S. Geological Survey Open-File Report 79-745, v, 201 p., 3 leaves of plates :ill., graphs, maps ;27 cm., https://doi.org/10.3133/ofr79745.","productDescription":"v, 201 p., 3 leaves of plates :ill., graphs, maps ;27 cm.","costCenters":[],"links":[{"id":140665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94447,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015048185089?urlappend=%3Bseq=3"},{"id":34839,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0745/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34840,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0745/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34841,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0745/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6d1","contributors":{"authors":[{"text":"Blankennagel, Richard K.","contributorId":55423,"corporation":false,"usgs":true,"family":"Blankennagel","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":155572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howells, L.W.","contributorId":89887,"corporation":false,"usgs":true,"family":"Howells","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":155574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155575,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hansen, C. V.","contributorId":74749,"corporation":false,"usgs":true,"family":"Hansen","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":155573,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7605,"text":"ofr79924 - 1979 - Water-resources appraisal of the south-Arkansas lignite area","interactions":[],"lastModifiedDate":"2022-07-18T15:51:26.201051","indexId":"ofr79924","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-924","title":"Water-resources appraisal of the south-Arkansas lignite area","docAbstract":"<p>The feasibility of developing lignite resources in south-central Arkansas is an important question at the present time (1978). Part of the concern is related to the possible impacts that mining and processing of lignite will have on water resources. Not only will the disturbance caused by excavating affect the quantity and quality of surface and ground water but, the mining, processing, and conversion processes will require the use and consumption of significant quantities of water.</p><p>In order to assess the magnitude of the effects of strip mining upon both surface and ground water, baseline conditions (hydrologic conditions in the area prior to mining) must be well defined. A thorough data file and literature search was made so that baseline conditions in the area could be defined. In addition, data-collection networks have been established for the collection of quantitative and qualitative information on streamflow and water levels in the aquifers. Data collected to date at these sites are included in the report. Collection of data at these sites will continue through at least September 1979.<br></p><p>Information presented in this report can be used to estimate the quantities of water available for use and the possible effects of mining and associated dewatering on water resources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79924","collaboration":"Prepared in cooperation with the Arkansas Geological Commission","usgsCitation":"Terry, J.E., Bryant, C.T., Ludwig, A.H., and Reed, J., 1979, Water-resources appraisal of the south-Arkansas lignite area: U.S. Geological Survey Open-File Report 79-924, Report: xi, 162 p.; 1 Plate: 21.68 x 20.18 inches, https://doi.org/10.3133/ofr79924.","productDescription":"Report: xi, 162 p.; 1 Plate: 21.68 x 20.18 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,{"id":7879,"text":"ofr791518 - 1979 - Bibliographic supplement to USGS Bulletin 1426; 1975 to June 1979","interactions":[],"lastModifiedDate":"2024-06-07T18:32:17.420274","indexId":"ofr791518","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1518","title":"Bibliographic supplement to USGS Bulletin 1426; 1975 to June 1979","docAbstract":"<p>This bibliography is a supplement to U.S. Geological Survey Bulletins 1426 (Bergquist, 1976) and 1263 (Heath and Tabacchi, 1968). The titles listed result from work undertaken in cooperation with national agencies partly through technical assistance projects under the auspices of the Agency for International Development, U.S. Department of State; partly under reimbursable assistance projects with other governments on behalf of the Department of State; partly under assistance projects sponsored by international organizations; and partly under scientific exchange projects supported by U.S. agencies such as the National Science Foundation.</p><p>This report includes titles published during the period 1975 through June 1979, but is not necessarily complete, as an exhaustive search was not made; however, it is being released in open file in order to make the data available to the public on an interim basis. Seven geographic regions and 71 countries are represented. A few titles published prior to 1975 have been found that are not included in Bulletins 1263 or 1426. Only reports authored solely or in part by USGS members, or jointly by USGS and counterpart staff members, are listed.</p><p>The reports are listed alphabetically by author, under the appropriate country; reports of wider scope are given under the continent or geographic region, for example, Africa, Central and South America, or CENTO region. Reports not classifiable by geographic location are listed separately under the heading \"General.\" All references to reports on water resources and hydrology were provided by J. R. Jones or R. M. Beall, USGS.</p><p>The reports and maps are available only through the listed source. Copies of articles published in scientific journals or by other governments or agencies cannot be ordered from the USGS. Instructions for ordering publications of the USGS follow.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791518","usgsCitation":"Bergquist, W., Tinsley, E., and Upton, V.S., 1979, Bibliographic supplement to USGS Bulletin 1426; 1975 to June 1979: U.S. Geological Survey Open-File Report 79-1518, iv, 66 p., https://doi.org/10.3133/ofr791518.","productDescription":"iv, 66 p.","costCenters":[],"links":[{"id":429666,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1518/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141288,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1518/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62ad08","contributors":{"authors":[{"text":"Bergquist, Wenonah E.","contributorId":96676,"corporation":false,"usgs":true,"family":"Bergquist","given":"Wenonah E.","affiliations":[],"preferred":false,"id":156774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinsley, Elizabeth J.","contributorId":29413,"corporation":false,"usgs":true,"family":"Tinsley","given":"Elizabeth J.","affiliations":[],"preferred":false,"id":156772,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Upton, Valerie S.","contributorId":82697,"corporation":false,"usgs":true,"family":"Upton","given":"Valerie","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":156773,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7887,"text":"ofr791480 - 1979 - A plan to study the aquifer system of the Central Valley of California","interactions":[],"lastModifiedDate":"2019-08-29T10:41:07","indexId":"ofr791480","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1480","title":"A plan to study the aquifer system of the Central Valley of California","docAbstract":"Unconsolidated Quaternary alluvial deposits comprise a large complex aquifer system in the Central Valley of California. Millions of acre-feet of water is pumped from the system annually to support a large and expanding agribusiness industry. Since the 1950's, water levels have been steadily declining in many areas of the valley and concern has been expressed about the ability of the entire ground-water system to support agribusiness at current levels, not to mention its ability to function at projected expansion levels. At current levels of ground-water use, an estimated 1.5 to 2 million acre-feet is withdrawn from storage each year; that is, 1.5 to 2 million acre-feet of water is pumped annually in excess of annual replenishment. The U.S. Geological Survey has initiated a 4-year study to develop geologic, hydrologic, and hydraulic information and to establish a valleywide ground-water data base that will be used to build computer models of the ground-water flow system. Subsequently, these models may be used to evaluate the system response to various ground-water management alternatives. This report describes current problems, objectives of the study, and outlines the general work to be accomplished in the study area. A bibliography of about 600 references is included. (Kosco-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr791480","usgsCitation":"Bertoldi, G.L., 1979, A plan to study the aquifer system of the Central Valley of California: U.S. Geological Survey Open-File Report 79-1480, iii, 48 p. , https://doi.org/10.3133/ofr791480.","productDescription":"iii, 48 p. ","costCenters":[],"links":[{"id":140023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1480/report-thumb.jpg"},{"id":367081,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Central Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab746","contributors":{"authors":[{"text":"Bertoldi, Gilbert L.","contributorId":60208,"corporation":false,"usgs":true,"family":"Bertoldi","given":"Gilbert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8109,"text":"ofr79748 - 1979 - An appraisal of pumping effects on the Edgeley Aquifer, La Moure County, North Dakota, as determined by a digital model","interactions":[],"lastModifiedDate":"2018-02-14T16:20:55","indexId":"ofr79748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-748","title":"An appraisal of pumping effects on the Edgeley Aquifer, La Moure County, North Dakota, as determined by a digital model","docAbstract":"<p>A finite-difference digital model simulated hydrologic conditions in the Edgeley aquifer, which is an unconfined glacial-drift aquifer. The calibrated model supported the hypothesis that under natural steady-state conditions, recharge is from precipitation and discharge is through evapotranspiration. This hypothesis was further supported by comparing simulated water levels to observed water levels collected during a 3-year period of irrigation withdrawal.</p>\n<p>Predictions of the effects of continued withdrawal of currently allocated water were made. One prediction using recharge equal to 25 percent of the average annual precipitati on showed that an equilibrium between pumping and recharge would be established within 10 years and water levels would be 2 to 4 feet below 1977 levels . A second prediction included a 2-year drought of one -half the average recharge from precipitation. This prediction also showed equilibrium within 10 years, but water level s would be 3 to 5 feet below 1977 levels . Predictions using additional withdrawals based on allocation requests were inde terminate.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79748","usgsCitation":"Burkart, M.R., 1979, An appraisal of pumping effects on the Edgeley Aquifer, La Moure County, North Dakota, as determined by a digital model: U.S. Geological Survey Open-File Report 79-748, Report: iii, 22 p.; 2 Plates: 27.03 x 28.76 inches and 17.04 x 28.28 inches, https://doi.org/10.3133/ofr79748.","productDescription":"Report: iii, 22 p.; 2 Plates: 27.03 x 28.76 inches and 17.04 x 28.28 inches","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":140625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr79748.jpg"},{"id":310501,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0748/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310502,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0748/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310503,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0748/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Lamoure County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.4396,46.6296],[-98.3152,46.63],[-98.2868,46.63],[-98.1889,46.6297],[-98.0349,46.6293],[-98.0366,46.2809],[-98.1314,46.2813],[-98.1616,46.2818],[-98.2524,46.2815],[-98.2859,46.2816],[-98.5024,46.2808],[-98.5359,46.2817],[-98.6622,46.2812],[-98.755,46.281],[-98.7878,46.2805],[-98.9154,46.2821],[-99.0049,46.2822],[-99.0397,46.2821],[-99.0379,46.6309],[-98.7894,46.6294],[-98.4396,46.6296]]]},\"properties\":{\"name\":\"Lamoure\",\"state\":\"ND\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6856f2","contributors":{"authors":[{"text":"Burkart, M. R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8246,"text":"ofr791297 - 1979 - Summary of hydrologic data for Tampa Bypass Canal System, July 1974 to September 1976","interactions":[],"lastModifiedDate":"2024-03-11T18:22:11.183644","indexId":"ofr791297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1297","title":"Summary of hydrologic data for Tampa Bypass Canal System, July 1974 to September 1976","docAbstract":"<p>The Tampa Bypass Canal is part of a flood-control project east of the city of Tampa under construction by the U.S. Army Corps of Engineers. It will divert floodwater from the Hillsborough River at points upstream from Tampa through a canal system to McKay Bay. The U.S. Geological Survey began a hydrologic data program in 1974 to provide data needed to identify existing hydrologic conditions and to evaluate the effects of canal construction. A network of surface-water and ground-water sites was designed to monitor changes in nutrients, trace metals, major inorganic constituents, pesticides, and benthic invertebrates along the canal system; to monitor changes in trace elements, common constituents, nitrates, specific conductance, and chlorides in the Floridan aquifer; and to monitor changes in the potentiometric surface of the Floridan aquifer.</p><p>In 1974-75, the monitoring program consisted of drilling 12 monitor wells and initiation of the surface-water sampling program. In 1976, the program consisted of drilling five additional wells, continuation of the surface-water sampling, initiation of ground-water sampling program, and monitoring of discharge from springs.</p><p>Water-quality data for nine surface-water sites in the basin were collected at each of the control structure sites, in the tidal portion of the canal, and at each of the major tributaries to the canal system.</p><p>Fifteen ground-water sites were sampled annually to provide information on ground-water quality. Ten wells were sampled semiannually for dissolved chloride concentrations to provide information on the freshwater-saltwater interface. Ground-water levels were collected at 34 wells in the areas adjacent to the canal to monitor changes in the potentiometric surface in the Floridan aquifer.</p><p>Discharge measurements from springs along the canal system were made in 1969-73 and 1976 to provide data on the quantity of ground water entering the canal. A daily discharge station was operated at structure S-160 to determine quantity of water flowing from the canal system into the bay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791297","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Causseaux, K.W., and Rollins, H., 1979, Summary of hydrologic data for Tampa Bypass Canal System, July 1974 to September 1976: U.S. Geological Survey Open-File Report 79-1297, iv, 74 p., https://doi.org/10.3133/ofr791297.","productDescription":"iv, 74 p.","costCenters":[],"links":[{"id":426506,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1297/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142058,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1297/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Tampa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.60182943316552,\n              28.08882190162491\n            ],\n            [\n              -82.60182943316552,\n              27.846197307615455\n            ],\n            [\n              -82.36560217558342,\n              27.846197307615455\n            ],\n            [\n              -82.36560217558342,\n              28.08882190162491\n            ],\n            [\n              -82.60182943316552,\n              28.08882190162491\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699069","contributors":{"authors":[{"text":"Causseaux, Kennedy W.","contributorId":60644,"corporation":false,"usgs":true,"family":"Causseaux","given":"Kennedy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rollins, H.C.","contributorId":102885,"corporation":false,"usgs":true,"family":"Rollins","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":157415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8263,"text":"ofr79699 - 1979 - Hydrologic reconnaissance of western Arctic Alaska, 1976 and 1977","interactions":[],"lastModifiedDate":"2019-03-08T12:27:04","indexId":"ofr79699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-699","title":"Hydrologic reconnaissance of western Arctic Alaska, 1976 and 1977","docAbstract":"<p>A reconnaissance of the water resources of the western Arctic was conducted during April 1976 and August 1977. Data were collected at 9 springs, 9 lakes and 22 stream sites.</p><p>Using slope-conveyance methods based on field evidence, estimates of bankfull and maximum evident flood-peak discharges were made for 20 selected streams. Maximum evident flood peak discharges ranged from 7.0 to 80.8 (ft3/s )/mi2 and averaged 30.1 (ft<sup>3</sup>/s)/mi<sup>2</sup>. These estimates bore no obvious relation to either drainage basin physiography or climatalogical characteristics. Both the bankfull and maximum evident flood-peak discharges were generally less than the 50-year flood and greater than the 2-year flood estimates made using regression relations developed from Alaska stream gaging records and drainage basin characteristics.</p><p>Springs were found only in the foothills of the Brooks Range. Their discharge ranged from 1.42 ft<sup>3</sup>/s at the Eli River spring to 13.0 ft<sup>3</sup>/s at North Fork Squirrel River spring. Water temperatures of springs sampled ranged from 0.00C at the Omikviorok spring to 3.50C at the Kavrorak Springs near Kivalina. The nine springs were found by noting the locations of the associated icings on Landsat imagery of the previous year.</p><p>Eleven stream sites were sampled under winter conditions; all were on the Arctic Slope. No winter streamflow was found at any of the streams. It appears that the streamflow on the Arctic Slope ceases in late winter except for limited local zones of ground-water discharge that form icings.</p><p>Ice thickness on most lakes was 6 ft except at Teshekpuk Lake where the ice was 8 ft thick. Three of the nine lakes examined were frozen to the bottom.</p><p>Winter water quality of the lakes and of standing water at stream sites was characterized by higher specific conductivity values than in summer. At three of the five lakes where specific conductance was measured, it was equal to or greater than 700 micromhos per centimeter at 25<strong>°</strong>C; at four of the five rivers where standing water was found, it&nbsp;was more than 400 micromhos per centimeter at 25<strong>°</strong>C.</p><p>Biological sampling was done to identify the widest range of benthic invertebrates likely to be present in a representative reach of a stream. A total of nine spring sites was sampled using drift nets in April 1976. Twenty-one stream sites and one spring were sampled in August 1977 by dip nets. Total numbers of organisms collected using drift net sampling in April 1976 ranged from 0 to 480. Total numbers of organisms collected by dip net sampling in August 1977 ranged from 0 to 776.</p><p>A hydrologic reconnaissance of the eastern Alaskan Arctic Slope was completed in 1975. The work covered in this report and in the 1975 companion report represents a preliminary hydrologic reconnaissance for the entire Alaskan Arctic Slope and western foothills regions of the Brooks Range.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79699","usgsCitation":"Childers, J.M., Kernodle, D.R., and Loeffler, R.M., 1979, Hydrologic reconnaissance of western Arctic Alaska, 1976 and 1977: U.S. Geological Survey Open-File Report 79-699, v, 70 p., https://doi.org/10.3133/ofr79699.","productDescription":"v, 70 p.","costCenters":[],"links":[{"id":361897,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0699/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0699/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -167,\n              66\n            ],\n            [\n              -150,\n              66\n            ],\n            [\n              -150,\n              71.5\n            ],\n            [\n              -167,\n              71.5\n            ],\n            [\n              -167,\n              66\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9bf","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kernodle, Donald R.","contributorId":63003,"corporation":false,"usgs":true,"family":"Kernodle","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157447,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loeffler, Robert M.","contributorId":80672,"corporation":false,"usgs":true,"family":"Loeffler","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":157448,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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