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This report contains discharge records for 278 gaging stations; stage only records for 10 gaging stations; stage and contents for 44 lakes and reservoirs; water quality for 85 gaging stations, and water levels for 95 observation wells. Also included are 91 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and co-operating State and Federal agencies in Oregon.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrOR781","collaboration":"Prepared in cooperation with the State of Oregon and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water resources data for Oregon, water year 1978: U.S. Geological Survey Water Data Report OR-78-1, xvi, 650 p., https://doi.org/10.3133/wdrOR781.","productDescription":"xvi, 650 p.","costCenters":[],"links":[{"id":497148,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1978/or-78-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174939,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1978/or-78-1/report-thumb.jpg"}],"country":"United 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,{"id":24090,"text":"ofr79510 - 1979 - Annual peak discharges from small drainage areas in Montana for stations discontinued before 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr79510","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":"79-510","title":"Annual peak discharges from small drainage areas in Montana for stations discontinued before 1978","docAbstract":"Annual peak stage and discharge data have been tabulated for crest-stage gage sites in Montana. The crest-stage program was begun in July 1955 to investigate the magnitude and frequency of floods from samll drainage areas. The program has expanded from 45 crest-stage gaging stations initially to 172 stations maintained in 1978. From 1955 to 1978, 156 stations have been discontinued. This report is a tabulation of the stage and discharge data for the discontinued stations. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr79510","issn":"0094-9140","usgsCitation":"Omang, R.J., Hull, J.A., and Parrett, C., 1979, Annual peak discharges from small drainage areas in Montana for stations discontinued before 1978: U.S. Geological Survey Open-File Report 79-510, viii, 24 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr79510.","productDescription":"viii, 24 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67ba5a","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":191301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":191302,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":191300,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24659,"text":"ofr79432 - 1979 - Landslides and related features, Kentucky; Winchester 1 ° x 2 ° sheet","interactions":[],"lastModifiedDate":"2025-01-06T20:00:36.41397","indexId":"ofr79432","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":"79-432","title":"Landslides and related features, Kentucky; Winchester 1 ° x 2 ° sheet","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79432","issn":"0094-9140","usgsCitation":"Taylor, A.R., 1979, Landslides and related features, Kentucky; Winchester 1 ° x 2 ° sheet: U.S. Geological Survey Open-File Report 79-432, 47 Plates: 15.22 x 27.94 inches or smaller, 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,{"id":26276,"text":"wri78131 - 1979 - The Citronelle aquifers in Mississippi","interactions":[],"lastModifiedDate":"2019-02-22T14:08:06","indexId":"wri78131","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":"78-131","title":"The Citronelle aquifers in Mississippi","docAbstract":"The Citronelle aquifers consist of sand and gravel of Pliocene age that forms a discontinuous outcrop area of about 6,000 square miles in southern Mississippi. The beds dip to the south at an average rate of about 6 feet per mile. The unconfined aquifers are used mostly for domestic and farm use but also supply water to several municipalities and industries. The average saturated thickness of the aquifers is about 45 feet. 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H.","contributorId":38954,"corporation":false,"usgs":true,"family":"Boswell","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24884,"text":"ofr79683 - 1979 - Hydrologic data for a subsurface waste-injection site at Mulberry, Florida; 1972-77","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"ofr79683","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":"79-683","title":"Hydrologic data for a subsurface waste-injection site at Mulberry, Florida; 1972-77","docAbstract":"Since October 1972, industrial liquid waste has been injected into a brine aquifer of limestone and dolomite in Mulberry, FL., at a depth of more than 4,000 feet below land surface. During 1977, the injection rate was about 8.8 million gallons per month. To determine what effect the injected waste has on the ground-water body, water levels have been measured and water samples collected from two monitor wells that tap different permeable zones above the injection zone, and from a satellite monitor well that taps the injection zone. The monitor wells are in the annulus of the injection well, and the satellite monitor well is 2,291 feet from the injection well. This report updates previous data reports and includes all hydrologic data collected by the U.S. Geological Survey during 1972-77. Included is a table of well-construction data, a graph showing the volume of waste injected each month, and hydrographs of the annulus monitor wells and the satellite monitor well. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr79683","issn":"0094-9140","usgsCitation":"Wilson, W.E., Parsons, D.C., and Spechler, R., 1979, Hydrologic data for a subsurface waste-injection site at Mulberry, Florida; 1972-77: U.S. Geological Survey Open-File Report 79-683, iii, 25 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr79683.","productDescription":"iii, 25 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eba3","contributors":{"authors":[{"text":"Wilson, William Edward","contributorId":82321,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":192737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parsons, David C.","contributorId":92293,"corporation":false,"usgs":true,"family":"Parsons","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spechler, R. M.","contributorId":85961,"corporation":false,"usgs":true,"family":"Spechler","given":"R. M.","affiliations":[],"preferred":false,"id":192738,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26069,"text":"wri7922 - 1979 - Water quality in the proposed Prosperity Reservoir area, Center Creek Basin, Missouri","interactions":[],"lastModifiedDate":"2019-11-14T12:57:57","indexId":"wri7922","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":"79-22","title":"Water quality in the proposed Prosperity Reservoir area, Center Creek Basin, Missouri","docAbstract":"<p>Water in Center Creek basin, Mo., upstream from the proposed Prosperity Reservoir damsite is a calcium bicarbonate type that is moderately mineralized, hard, and slightly alkaline. Ammonia and organic nitrogen, phosphorus, total organic carbon, chemical oxygen demand, and bacteria increased considerably during storm runoff, probably due to livestock wastes. Nitrogen and phosphorus concentrations are probably high enough to cause the proposed lake to be eutrophic. Minor-element concentrations were at or near normal levels in Center and Jones Creeks. The only pesticides detected were 0.01 micrograms per liter of 2, 4, 5-T in one base-flow sample and 0.02 to 0.04 micrograms per liter of 2, 4, 5-T and 2, 4-D in all storm-runoff samples. Fecal coliform and fecal streptococcus densities ranged from 2 to 650 and 2 to 550 colonies per 100 milliliters, respectively, during base flow , but were 17,000 to 45,000 and 27,000 to 70,000 colonies per 100 milliliters, respectively, during storm runoff. Water in Center Creek about 2.5 miles downstream from the proposed damsite is similar in quality to that upstream from the damsite except for higher concentrations of sodium, sulfate, chloride, fluoride, nitrogen, and phosphorus. These higher concentrations are caused by fertilizer industry wastes that enter Center Creek about 1.0 mile downstream from the proposed damsite. (Woodard-USGS).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7922","usgsCitation":"Barks, J.H., and Berkas, W.R., 1979, Water quality in the proposed Prosperity Reservoir area, Center Creek Basin, Missouri: U.S. Geological Survey Water-Resources Investigations Report 79-22, ii, 26 p., https://doi.org/10.3133/wri7922.","productDescription":"ii, 26 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":157906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0022/report-thumb.jpg"},{"id":369214,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Missouri","county":"Jasper","city":"Carl Junction","otherGeospatial":"Southwest Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.57305908203124,\n              37.18746751526529\n            ],\n            [\n              -94.57305908203124,\n              37.2062007795906\n            ],\n            [\n              -94.54726696014404,\n              37.2062007795906\n            ],\n            [\n              -94.54726696014404,\n              37.18746751526529\n            ],\n            [\n              -94.57305908203124,\n              37.18746751526529\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a21","contributors":{"authors":[{"text":"Barks, James H.","contributorId":73569,"corporation":false,"usgs":true,"family":"Barks","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":195745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25707,"text":"wri7934 - 1979 - Plan of study for the northern Great Plains regional aquifer-system analysis in parts of Montana, North Dakota, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2018-11-14T10:19:32","indexId":"wri7934","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":"79-34","title":"Plan of study for the northern Great Plains regional aquifer-system analysis in parts of Montana, North Dakota, South Dakota, and Wyoming","docAbstract":"<p>The Northern Great Plains, an area of about 250,000 square miles in parts of Montana, North Dakota, South Dakota, and Wyoming, is underlain by an accumulation of sediments eroded from the Black Hills and from mountains to the west. Principal aquifers are areally extensive beds of sandstone within these sedimentary rocks, some at great depths. Anticipated future water needs dictate that available ground-water supplies be evaluated for management of this natural resource. The U.S. Geological Survey has started (1978) a 4-year study of the Northern Great Plains aquifer system. The objective of this study is to define availability and quality of ground water and to predict the effects of using this resource. To achieve this objective, the ground-water system will be described in terms of spatial distribution, hydraulics, geology, and geochemistry. Once described, the ground-water system will be simulated by mathematical models that will be used to define responses of the system to various management alternatives and assumed development patterns.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7934","usgsCitation":"Dinwiddie, G.A., 1979, Plan of study for the northern Great Plains regional aquifer-system analysis in parts of Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 79-34, iii, 20 p., https://doi.org/10.3133/wri7934.","productDescription":"iii, 20 p.","costCenters":[],"links":[{"id":156684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0034/report-thumb.jpg"},{"id":359418,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana, North Dakota, South Dakota, Wyoming","otherGeospatial":"Northern Great Plains Regional Aquifer-System","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.02783203125,\n              41.95131994679697\n            ],\n            [\n              -96.65771484375,\n              41.95131994679697\n            ],\n            [\n              -96.65771484375,\n              48.99463598353405\n            ],\n            [\n              -111.02783203125,\n              48.99463598353405\n            ],\n            [\n              -111.02783203125,\n              41.95131994679697\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685614","contributors":{"authors":[{"text":"Dinwiddie, George A.","contributorId":21135,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24920,"text":"ofr791508 - 1979 - A preliminary assessment of the 1977 INPUT survey on the Arabian Shield, Kingdom of Saudi Arabia, with guides for interpretation and ground follow-up","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr791508","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":"79-1508","title":"A preliminary assessment of the 1977 INPUT survey on the Arabian Shield, Kingdom of Saudi Arabia, with guides for interpretation and ground follow-up","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791508","issn":"0094-9140","usgsCitation":"Wynn, J.C., and Blank, H., 1979, A preliminary assessment of the 1977 INPUT survey on the Arabian Shield, Kingdom of Saudi Arabia, with guides for interpretation and ground follow-up: U.S. Geological Survey Open-File Report 79-1508, ii, 35 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr791508.","productDescription":"ii, 35 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab0d2","contributors":{"authors":[{"text":"Wynn, Jeffrey C.","contributorId":81081,"corporation":false,"usgs":true,"family":"Wynn","given":"Jeffrey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blank, Horace Richard","contributorId":95101,"corporation":false,"usgs":true,"family":"Blank","given":"Horace Richard","affiliations":[],"preferred":false,"id":192801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":26266,"text":"wri7762 - 1979 - Comparison of selected cultural, physical, and water-quality characteristics of lakes in Washington","interactions":[],"lastModifiedDate":"2018-11-16T09:39:56","indexId":"wri7762","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":"77-62","title":"Comparison of selected cultural, physical, and water-quality characteristics of lakes in Washington","docAbstract":"<p>This report presents comparisons and a graphical overview of the relative magnitude and the regional and statewide distribution of 19 selected cultural, physical, and water-quality characteristics measured in a reconnaissance study of several hundred lakes in Washington. The selected characteristics presented for each lake include types of land use in the lake drainage basin, shoreline residential development, altitude of lake, mean lake depth, nitrogen and phosphorus concentrations in upper and bottom waters, specific conductance, temperature and dissolved-oxygen concentration cf bottom water, Secchi-disc visibility,&nbsp;emersed macrophytes covering shoreline and lake surface, and fecal-coliform bacteria.</p><p>Statewide, about two-thirds of the lake drainage basins studied have more than half their land in forest. Urban and suburban developments of the basins are highest in the more populated western Washington counties near Puget Sound, whereas most land in the drainage basins of lakes in the Columbia Plateau of eastern Washington is used for agricultural purposes. Statewide, almost one-fourth of the lakes are shallow (mean depth 2.0 meters or less) and only 7 percent of the lakes have mean depths greater than 20 meters. Dissolved-oxygen layering in summer was detected in many lakes throughout the State. The oxygen concentrations in the upper waters of these lakes were typically near saturation, but the bottom waters of many were severely depleted. Statewide, about one-third of the lakes had Secchi-disc readings of 2.0 meters or less, a value often considered characteristic of eutrophic lakes. The poorest water clarity was observed in the Columbia Plateau, where 68 percent of the lakes had Secchi-disc readings of less than 2.0 meters. Statewide, the median concentration of total phosphorus in the upper waters of lakes was 20 micrograms per liter. More than one-third of the lakes in the State had total phosphorus concentrations in their upper waters that exceeded 30 micrograms per liter, a concentration that is often considered characteristic of eutrophic lakes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7762","usgsCitation":"Bortleson, G.C., and Dion, N.P., 1979, Comparison of selected cultural, physical, and water-quality characteristics of lakes in Washington: U.S. Geological Survey Water-Resources Investigations Report 77-62, vii, 54 p., https://doi.org/10.3133/wri7762.","productDescription":"vii, 54 p.","costCenters":[],"links":[{"id":157805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0062/report-thumb.jpg"},{"id":359485,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":25864,"text":"wri78126 - 1979 - The Yampa River basin, Colorado and Wyoming : a preview to expanded coal-resource development and its impacts on regional water resources","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri78126","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":"78-126","title":"The Yampa River basin, Colorado and Wyoming : a preview to expanded coal-resource development and its impacts on regional water resources","docAbstract":"Expanded coal production and conversion in the Yampa River basin , Colorado and Wyoming, may have substantial impacts on water resources, environmental amenities, and socioeconomic conditions. Preliminary results of a 3-year basin assessment by the U.S. Geological Survey are given for evaluation of surface- and ground-water resources using available data, modeling analysis of waste-load capacity of a Yampa River reach affected by municipal wastewater-treatment plant effluents, and semiquantitative descriptions of ambient air- and water-quality conditions. Aspects discussed are possible constraints on proposed development due to basin compacts and laws regulating water resources, possible changes in environmental-control regulations, and policies on energy-resource leasing and land use that will influence regional economic development. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri78126","usgsCitation":"Steele, T.D., Bauer, D.P., Wentz, D., and Warner, J.W., 1979, The Yampa River basin, Colorado and Wyoming : a preview to expanded coal-resource development and its impacts on regional water resources: U.S. Geological Survey Water-Resources Investigations Report 78-126, x, 133 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri78126.","productDescription":"x, 133 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":158161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0126/report-thumb.jpg"},{"id":54615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0126/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd78","contributors":{"authors":[{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":195393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, D. P.","contributorId":32542,"corporation":false,"usgs":true,"family":"Bauer","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wentz, D.A.","contributorId":85206,"corporation":false,"usgs":true,"family":"Wentz","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":195392,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, J. W.","contributorId":42996,"corporation":false,"usgs":true,"family":"Warner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9465,"text":"ofr78852 - 1979 - Hydrologic data for the southwest subsurface-injection test site, St. Petersburg, Florida","interactions":[],"lastModifiedDate":"2026-02-19T15:04:10.230027","indexId":"ofr78852","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":"78-852","title":"Hydrologic data for the southwest subsurface-injection test site, St. Petersburg, Florida","docAbstract":"<p>Three injection wells, A1, A2, and A3, and nine observation wells, B1 through B9, were constructed at the Southwest St. Petersburg site to determine the feasibility of injecting wastewater treatment plant effluent into permeable zones containing saline water. Two withdrawal tests and one injection test were performed. Both withdrawal tests ran for about 3 days, one discharging 650 gallons per minute from well B8; the other discharging 6,490 gallons per minute from test well A3. The injection test was run in A3 for 91.1 days at an average rate of 2,830 gallons per minute. Injection well pressure reached a maximum of 48.1 pounds per square inch near the end of the test. Rhodamine WT was used as a tracer during the injection test and was identified in wells B3, B6, and B7.&nbsp;</p><p>Before the injection test, chloride concentration in well B6, 35 feet distant from the injection well, and in well B3, 733 feet distant, ranged from 19,000 to 21,000 milligrams per liter. At the end of the test, chloride concentration in B6 was 1,800 milligrams per liter and in B3 was 5,400 milligrams per liter. Eleven wells near the site were sampled before the test for water-quality analyses and chlorides ranged from 18 to 1,400 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78852","collaboration":"Prepared in cooperation with the City of St. Petersburg, Florida","usgsCitation":"Hickey, J.J., and Spechler, R., 1979, Hydrologic data for the southwest subsurface-injection test site, St. Petersburg, Florida: U.S. Geological Survey Open-File Report 78-852, iv, 104 p., https://doi.org/10.3133/ofr78852.","productDescription":"iv, 104 p.","costCenters":[],"links":[{"id":500180,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0852/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142909,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0852/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"St. Petersburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.2199306173198,\n              28.3250638673004\n            ],\n            [\n              -83.2199306173198,\n              27.33328590951686\n            ],\n            [\n              -81.93548183780042,\n              27.33328590951686\n            ],\n            [\n              -81.93548183780042,\n              28.3250638673004\n            ],\n            [\n              -83.2199306173198,\n              28.3250638673004\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6081c7","contributors":{"authors":[{"text":"Hickey, John J.","contributorId":39763,"corporation":false,"usgs":true,"family":"Hickey","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spechler, R. M.","contributorId":85961,"corporation":false,"usgs":true,"family":"Spechler","given":"R. M.","affiliations":[],"preferred":false,"id":159734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26021,"text":"wri7992 - 1979 - Evaluation of methods for estimating ground-water withdrawals in western Kansas","interactions":[],"lastModifiedDate":"2018-11-19T12:17:44","indexId":"wri7992","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":"79-92","title":"Evaluation of methods for estimating ground-water withdrawals in western Kansas","docAbstract":"<p>During 1978, methods of estimating ground-water withdrawals in western Kansas were examined and evaluated, using both existing data from the files of the U.S. Geological Survey and newly collected data.</p><p>Values for annual ground-water withdrawals reported to the Division of Water Resources, Kansas State Board of Agriculture, by water users probably contain substantial errors because most individual users do not possess the means to measure or accurately estimate the discharge rates of their wells. Such reported values are estimated to average 10 to 15 percent higher than the actual discharge rate. Values obtained from discharge-totaling meters are reasonably accurate, but few wells are equipped with these meters, and the cost of equipping all wells with meters may be prohibitive. Measured rates of power consumption can give good estimates of total withdrawal from wells where the power consumption is measured. However, power-consumption values cannot be extrapolated reliably from one well to another.</p><p>Three techniques are regarded as promising for estimating areal ground-water withdrawals from readily collected data:</p><ol><li>Examination of a small sample of withdrawal values from metered wells indicates that the statistical approach used by Luckey (1972) may be applied to western Kansas to estimate total withdrawal with acceptable accuracy in a large area from a statistical sample of measured values.<br></li><li>Measured values of irrigation application at a small number of selected wells might be used to compute total withdrawal for irrigation by crop type and precipitation zone. Evaluation of reported values of irrigation-water application for selected crops in zones of generally similar precipitation showed that, although the reported values are judged to be erroneously high, the reported values were consistent with each other and with average precipitation.<br></li><li>Power-consumption coefficients may be used to calculate an average coefficient for an area. The method described by Luckey (1972) was used to calculate the number of power-consumption coefficients that would have to be determined to estimate the mean power consumption of wells pumped by electric or natural-gas engines. The results indicate that as few as 100 values would produce results accurate to within 10 percent of the true average at the 95-percent confidence level. Thus, power coefficients for a particular type of irrigation system in any given area can be used even though values of power coefficients have little transfer value from well to well.<br></li></ol><p>Efforts by the Instrument Development Laboratofy of the U.S. Geological Survey to design improved instruments for measuring ground-water withdrawals have produced two promising results:</p><ol><li>An electronic running-time meter (Running-time Sentry) that was tested during 1978 in western Kansas and Florida appears to give accurate values of total pumping time. Large-scale testing of this prototype running-time meter is planned for 1979.<br></li><li>A low-cost discharge-totaling meter (REELTOT), based on the concept of sensing the velocity head in a pipe with differential-pressure transducers permanently installed in the pipe, is nearly complete. Early prototypes of this instrument may be tested in western Kansas during 1979.<br></li></ol><p>For the remainder of this study, the three techniques for estimating areal ground-water withdrawals described above will be tested on a larger scale in Groundwater Management District No. 1, an area of about 1,800 square miles in west-central Kansas. About 150 randomly selected wells will be equipped with Running-time Sentry units and monitored for total withdrawal, instantaneous discharge, and power consumption. A few wells will be equipped with prototype discharge-totaling meters. The performance of the Sentry units and discharge-totaling meters will be evaluated. Areal estimates of withdrawal from measured withdrawal values, from average power-consumption coefficients, and from irrigation application by crop will be calculated and compared with each other and with reported values of withdrawal.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7992","usgsCitation":"Baker, C.H., 1979, Evaluation of methods for estimating ground-water withdrawals in western Kansas: U.S. Geological Survey Water-Resources Investigations Report 79-92, iv, 70 p., https://doi.org/10.3133/wri7992.","productDescription":"iv, 70 p.","costCenters":[],"links":[{"id":359560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0092/report-thumb.jpg"}],"country":"United 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,{"id":26082,"text":"wri78130 - 1979 - Flood elevations for the Sooes River at proposed fish hatchery, Clallam County, Washington; a surface-water site study","interactions":[],"lastModifiedDate":"2019-08-05T10:24:10","indexId":"wri78130","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":"78-130","title":"Flood elevations for the Sooes River at proposed fish hatchery, Clallam County, Washington; a surface-water site study","docAbstract":"Water-surface elevations were derived for various combinations of selected river discharges and tide elevations along a reach of the Sooes River 3 miles upstream from the mouth at the site of a proposed fish hatchery in Clallam County, Washington. Flood-frequency analyses determined river discharges having exceedence probabilities of 1, 2, 4, 10 and 20 percent (100-, 50-, 25-, 10-, and 5-year recurrence intervals) and tide elevations having exceedence probabilities of 1 and 50 percent (100- and 2-year recurrence intervals). A relationship was developed for determining river water-surface elevation for different combinations of river discharge and tide elevations. Seven different combinations of river flood-plain conditions that may be expected to occur during and after construction were simulated and water-surface elevations determined by use of the step-backwater computer program.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri78130","usgsCitation":"Bartells, J., 1979, Flood elevations for the Sooes River at proposed fish hatchery, Clallam County, Washington; a surface-water site study: U.S. Geological Survey Water-Resources Investigations Report 78-130, iii, 28 p., https://doi.org/10.3133/wri78130.","productDescription":"iii, 28 p.","costCenters":[],"links":[{"id":158030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0130/report-thumb.jpg"},{"id":366197,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"Clallam County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.66529846191406,\n              48.23565029755308\n            ],\n            [\n              -124.59938049316406,\n              48.23565029755308\n            ],\n            [\n              -124.59938049316406,\n              48.32429984442754\n            ],\n            [\n              -124.66529846191406,\n              48.32429984442754\n            ],\n            [\n              -124.66529846191406,\n              48.23565029755308\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef1d4","contributors":{"authors":[{"text":"Bartells, J.H.","contributorId":31434,"corporation":false,"usgs":true,"family":"Bartells","given":"J.H.","affiliations":[],"preferred":false,"id":195769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24065,"text":"ofr791637 - 1979 - Graphic and tabular summaries of changes in stream-channel cross sections between 1976 and 1978 for Redwood Creek and selected tributaries, Humboldt County, and Mill Creek, Del Norte County, California","interactions":[],"lastModifiedDate":"2024-06-28T21:53:55.265636","indexId":"ofr791637","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":"79-1637","title":"Graphic and tabular summaries of changes in stream-channel cross sections between 1976 and 1978 for Redwood Creek and selected tributaries, Humboldt County, and Mill Creek, Del Norte County, California","docAbstract":"<p>Forty-eight surveyed stream-channel cross sections were established along Redwood Creek, Humboldt County, California between 1973 and 1974. Eighty-three cross sections were established at selected sites along tributaries to Redwood Creek between 1974 and 1976. Eleven surveyed stream channel cross sections were established in the Mill Creek drainage basin, Del Norte County, California in the summer of 1974. All cross-sections have been resurveyed at least annually since they were established. All work was done in cooperation with the National Park Service.</p><p>Data tabulated in this report summarize changes at cross sections since release of previous reports. Data from the Redwood Creek cross sections are tabulated for the following periods: initiation of observation to summer 1978, summer 1975 to summer 1976, and summer 1977 to summer 1978. Data from the Redwood Creek tributary cross sections are tabulated for various periods between 1974 and 1978. Data from the Mill Creek cross sections are presented for the period of summer of 1975 to summer 1978. Thirteen figures are included to aid in understanding the tabulated data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791637","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Nolan, K.M., 1979, Graphic and tabular summaries of changes in stream-channel cross sections between 1976 and 1978 for Redwood Creek and selected tributaries, Humboldt County, and Mill Creek, Del Norte County, California: U.S. Geological Survey Open-File Report 79-1637, iii, 38 p., https://doi.org/10.3133/ofr791637.","productDescription":"iii, 38 p.","costCenters":[],"links":[{"id":430641,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1637/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157173,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1637/report-thumb.jpg"}],"country":"United States","state":"California","county":"Del Norte County, Humboldt County","otherGeospatial":"Mill Creek, Redwood Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.03131459692543,\n              41.95968735441147\n            ],\n            [\n              -125.03131459692543,\n              40.049452070509375\n            ],\n            [\n              -123.40458267600727,\n              40.049452070509375\n            ],\n            [\n              -123.40458267600727,\n              41.95968735441147\n            ],\n            [\n              -125.03131459692543,\n              41.95968735441147\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2f9e","contributors":{"authors":[{"text":"Nolan, K. Michael","contributorId":71943,"corporation":false,"usgs":true,"family":"Nolan","given":"K.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":191251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26114,"text":"wri78122 - 1979 - Traveltime, unit-concentration, longitudinal-dispersion, and reaeration characteristics of upstream reaches of the Yampa and Little Snake Rivers, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri78122","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":"78-122","title":"Traveltime, unit-concentration, longitudinal-dispersion, and reaeration characteristics of upstream reaches of the Yampa and Little Snake Rivers, Colorado and Wyoming","docAbstract":"Measurements were made along a 58-mile reach of the Yampa River in Colorado and a 77-mile reach of the Little Snake River in Colorado and Wyoming to determine traveltime, unit-concentration , and longitudinal-dispersion characteristics. Two traveltime, unit-concentration, and dispersion analyses were made along the Yampa River when its average streamflow was approximately 100 and 3,400 cu ft/s; three traveltime, unit-concentration, and dispersion analyses were made along the Little Snake River when its average streamfow was approximately 200, 600, and 1,600 cu ft/s. Reaeration coefficients were determined only for the Yampa River, when its average streamflow was approximately 100 cu ft/s. Traveltime and unit-concentration simulations were made using a mathematical model. Data collected for the Little Snake River when the average streamflow was approximately 600 cu ft/s were used as a check of model-simulation accuracy. Traveltime simulations compared to within 5%, and unit-concentration simulations were within 30 to 40% of the measured flow data. Longitudinal-dispersion coefficients ranged from 400 to 6,050 sq ft/s for the two streams. Reaeration coefficients for the Yampa River, adjusted to 20 degrees celsius, ranged from 6.04 to 33.4 per day. Two semi-empirical equations gave reaeration coefficients in best agreement with measured reaeration coefficients. Absolute errors of estimate for these equations were 11.8 and 17.3%. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri78122","usgsCitation":"Bauer, D.P., Rathbun, R.E., and Lowham, H., 1979, Traveltime, unit-concentration, longitudinal-dispersion, and reaeration characteristics of upstream reaches of the Yampa and Little Snake Rivers, Colorado and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 78-122, vi, 66 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri78122.","productDescription":"vi, 66 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":158102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0122/report-thumb.jpg"},{"id":54913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626a69","contributors":{"authors":[{"text":"Bauer, Daniel P.","contributorId":24337,"corporation":false,"usgs":true,"family":"Bauer","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":195836,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":195834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24171,"text":"ofr79681 - 1979 - Streamflow statistical summaries for Colorado streams through September 30, 1975: Volume 1: Missouri River, Arkansas River, and Rio Grande Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr79681","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":"79-681","title":"Streamflow statistical summaries for Colorado streams through September 30, 1975: Volume 1: Missouri River, Arkansas River, and Rio Grande Basins","docAbstract":"Statistical summaries of daily streamflow data for 246 stations east of the Continental Divide in Colorado and adjacent States are presented in this report. Duration tables, high-flow sequence tables, and low-flow sequence tables provide information about daily mean discharge. The mean, variance, standard deviation, skewness, and coefficient of variation are provided for monthly and annual flows. Percentages of average flow are provided for monthly flows and first-order serial-correlation coefficients are provided for annual flows. The text explains the nature and derivation of the data and illustrates applications of the tabulated information by examples. The data may be used by agencies and individuals engaged in water studies. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr79681","issn":"0094-9140","usgsCitation":"Petsch, H.E., 1979, Streamflow statistical summaries for Colorado streams through September 30, 1975: Volume 1: Missouri River, Arkansas River, and Rio Grande Basins: U.S. Geological Survey Open-File Report 79-681, 3 v. :ill. ;28 cm.; (519 p. - PGS), https://doi.org/10.3133/ofr79681.","productDescription":"3 v. :ill. ;28 cm.; (519 p. - PGS)","costCenters":[],"links":[{"id":113017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0681/report.pdf","size":"35054","linkFileType":{"id":1,"text":"pdf"}},{"id":155465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0681/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d48","contributors":{"authors":[{"text":"Petsch, Harold E.","contributorId":25594,"corporation":false,"usgs":true,"family":"Petsch","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24983,"text":"pp1150 - 1979 - Geological Survey research 1979","interactions":[],"lastModifiedDate":"2025-01-07T19:25:39.417039","indexId":"pp1150","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":"1150","title":"Geological Survey research 1979","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1150","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Geological Survey research 1979: U.S. Geological Survey Professional Paper 1150, ix, 447 p., https://doi.org/10.3133/pp1150.","productDescription":"ix, 447 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":403859,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92990.htm","text":"Geologic setting for uranium deposits in the Date Creek basin, west-central Arizona","linkFileType":{"id":5,"text":"html"}},{"id":53968,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1150/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118862,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1150/report-thumb.jpg"},{"id":465795,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92995.htm","text":"Melones Fault north of Downieville","linkFileType":{"id":5,"text":"html"}},{"id":465796,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92997.htm","text":"Age and strontium isotopic composition of the Honolulu Volcanics","linkFileType":{"id":5,"text":"html"}},{"id":465797,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93002.htm","text":"A more complex Sebago batholith","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876c2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25039,"text":"pp1056 - 1979 - Chronological narrative of the 1969-71 Mauna Ulu eruption of Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"pp1056","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":"1056","title":"Chronological narrative of the 1969-71 Mauna Ulu eruption of Kilauea Volcano, Hawaii","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1056","usgsCitation":"Swanson, D., Duffield, W.A., Jackson, D.B., and Peterson, D.W., 1979, Chronological narrative of the 1969-71 Mauna Ulu eruption of Kilauea Volcano, Hawaii: U.S. Geological Survey Professional Paper 1056, 55 p., https://doi.org/10.3133/pp1056.","productDescription":"55 p.","costCenters":[],"links":[{"id":121790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1056/report-thumb.jpg"},{"id":54041,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1056/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54042,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1056/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54043,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1056/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54044,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1056/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54045,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f4a","contributors":{"authors":[{"text":"Swanson, Donald A. 0000-0002-1680-3591","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":22303,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","affiliations":[],"preferred":false,"id":193116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jackson, D. B.","contributorId":27057,"corporation":false,"usgs":true,"family":"Jackson","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":193117,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, D. W.","contributorId":84326,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193119,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24151,"text":"ofr79556 - 1979 - Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota","interactions":[],"lastModifiedDate":"2016-05-17T14:37:33","indexId":"ofr79556","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":"79-556","title":"Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota","docAbstract":"<p>Water samples were collected from three lakes in Voyageurs National Park to assess chemical and biological water quality in March and August 1977. Bottom material samples were also collected and analyzed for chemical quality. Results of the analyses show that the water system was dilute; specific conductance ranged from 32 to 111 micromhos. Blue-green algae, particularly <i>Oscillatoria</i>, were the most common phytoplankton in the samples. Differences in water quality, shown particularly by concentrations of nutrients and dissolved solids, were detected between samples collected in different areas of the park. The collected data were used to design a monitoring program to assess eutrophication that may occur during the development of the park.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr79556","issn":"0094-9140","collaboration":"Prepared in cooperation with National Park Service, Department of the Interior","usgsCitation":"Payne, G.A., 1979, Water-quality reconnaissance of lakes in Voyageurs National Park, Minnesota: U.S. Geological Survey Open-File Report 79-556, 40 p., https://doi.org/10.3133/ofr79556.","productDescription":"40 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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