{"pageNumber":"529","pageRowStart":"13200","pageSize":"25","recordCount":16501,"records":[{"id":7619,"text":"ofr84609 - 1984 - Water-resources reports prepared by or in cooperation with the U.S. Geological Survey, Kansas, 1886-1983","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"ofr84609","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-609","title":"Water-resources reports prepared by or in cooperation with the U.S. Geological Survey, Kansas, 1886-1983","docAbstract":"Water-resources data and the results of hydrologic investigations in Kansas are published or released by the U.S. Geological Survey, by cooperating State or Federal agencies, or by technical or scientific journals. This report lists more than 800 water-resources reports prepared by or in cooperation with the U.S. Geological Survey in Kansas for 1886 through 1983. The reports are listed by author, publication series, year of publication, and subject. The first water-resources investigations by the U.S. Geological Survey in Kansas was completed by A.C. Peale in 1886. The first cooperative program with a State agency was initiated 9 years later in 1895 and included the first stream-gaging stations operated by the Survey in western Kansas. The U.S. Geological Survey continues to investigate the occurrence, quantity, quality, distribution, and movement of surface and ground waters within the State. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84609","usgsCitation":"Combs, L., 1984, Water-resources reports prepared by or in cooperation with the U.S. Geological Survey, Kansas, 1886-1983: U.S. Geological Survey Open-File Report 84-609, iv, 117 p. :map ;28 cm., https://doi.org/10.3133/ofr84609.","productDescription":"iv, 117 p. :map ;28 cm.","costCenters":[],"links":[{"id":140107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0609/report-thumb.jpg"},{"id":35107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0609/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e57","contributors":{"authors":[{"text":"Combs, L. J.","contributorId":25133,"corporation":false,"usgs":true,"family":"Combs","given":"L. J.","affiliations":[],"preferred":false,"id":156314,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11190,"text":"ofr84446 - 1984 - Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81","interactions":[],"lastModifiedDate":"2021-01-21T17:24:06.763454","indexId":"ofr84446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-446","title":"Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81","docAbstract":"Water at 102 sites in 59 coal-mine ponds in eastern Oklahoma was sampled at lease twice during June to November 1977-81 to determine temperature, specific conductance, dissolved oxygen, pH, and dissolved sulfate, chloride, iron, and manganese--as part of a study of the hydrology of the Oklahoma coalfield. These determinations show that during June to October water in ponds deeper than ~10 ft was stratified; ponds which had little or not change of temperature with depth generally were shallow or were sampled in early November. Temperature, dissolved oxygen, and pH usually decreased with depth, whereas specific conductance usually increased with depth. Concentrations of dissolved sulfate, chloride, iron, and manganese varied from site to site. Specific conductance, which is a measure of dissolved solids in the water, ranged from 93 to 4,800 mmho/cm at 25oC. Some physical and chemical characteristics of the mine-pond water are related to the coal bed adjacent to the pond. Mean specific-conductance values and dissolved-sulfate concentrations were greatest in ponds associated with mining of Dawson, Weir-Pittsburg, and Secor coals. Mean dissolved-iron concentrations were greatest in ponds associated with mining of the Dawson, Secor, and Hartshorne coals. Mean dissolved-manganese concentrations were greatest in ponds associated with mining of the Dawson, Weir-Pittsburg, and Secor coals, but greatly exceeded secondary drinking-water limits regardless of coal bed mined.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84446","collaboration":"This report was also published by the Oklahoma Geological Survey as Special Publication 87-2","usgsCitation":"Slack, L.J., and Blumer, S.P., 1984, Physical and chemical characteristics of water in coal-mine ponds, eastern Oklahoma, June to November 1977-81: U.S. Geological Survey Open-File Report 84-446, Report: vi, 183 p.; 1 Plate: 16.79 x 22.84 inches, https://doi.org/10.3133/ofr84446.","productDescription":"Report: vi, 183 p.; 1 Plate: 16.79 x 22.84 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,{"id":4159,"text":"cir904A - 1984 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","interactions":[{"subject":{"id":7850,"text":"ofr83759 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","indexId":"ofr83759","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines"},"predicate":"SUPERSEDED_BY","object":{"id":4159,"text":"cir904A - 1984 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","indexId":"cir904A","publicationYear":"1984","noYear":false,"chapter":"A","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines"},"id":1}],"lastModifiedDate":"2019-11-07T12:09:06","indexId":"cir904A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"904","chapter":"A","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines","docAbstract":"<p>The U.S. Geological Survey's program for geologic and hydrologic evaluation of physiographic provinces to identify areas potentially suitable for locating repository sites for disposal of high-level nuclear wastes was announced to the Governors of the eight States in the Basin and Range Province on May 5, 1981. Representatives of Arizona, California, Idaho, New Mexico, Nevada, Oregon, Texas, and Utah, were invited to cooperate with the Federal Government in the evaluation process. Each Governor was requested to nominate an Earth scientist to represent the State in a province working group composed of State and U.S. Geological Survey representatives. This report, Part I of a three-part report, provides the background, introduction and scope of the study. This part also includes a discussion of geologic and hydrologic guidelines that will be used in the evaluation process and illustrates geohydrologic environments and the effect of individual factors in providing multiple natural barriers to radionuclide migration.</p><p>Part II is a reconnaissance characterization of the geologic and hydrologic factors to be used in the initial screening of the Basin and Range Province. Part III will be the initial evaluation of the Province and will identify regions that appear suitable for further study.</p><p>The plan for study of the Province includes a stepwise screening process by which successively smaller land units are considered in increasing detail. Each step involves characterization of the geology and hydrology and selection of subunits for more intensive characterization. Selection of subunits for further study is by evaluation of geologic and hydrologic conditions following a set of guidelines. By representation on the Province Working Group, the States participate in a consultation and review role in: (1) Establishing geologic and hydrologic guidelines, and (2) characterizing and evaluating the Province. The States also participate in compilation of geologic and hydrologic data used in characterizing the Province.</p><p>The current (1983) needs for a high-level radioactive waste repository include: (1) Disposal in a mined repository; (2) retrievability of the waste for as much as 50 years; and (3) confidence of isolation of the waste from the accessible environment. Isolation of the waste needs to be assured using geologic and hydrologic conditions that: (1) Minimize risk of inadvertent future intrusions by man; (2) minimize the possibility of disturbance by processes that would expose the waste or increase its mobility; and (3) provide a system of natural barriers to the migration of waste by ground water. The guidelines adopted by the Province Working Group are designed to provide a standard with which these conditions can be compared.</p><p>The guidelines can be grouped into four principal categories: (1) Potential host media, (2) ground-water conditions, (3) tectonic conditions, and. (4) occurrence of natural resources. Ideally the host medium constitutes the first natural barrier to migration of radionculides. The host medium ideally should be a rock type that prevents or retards dissolution and transport of radionuclides. Rocks in both the saturated and unsaturated zones may have desirable characteristics for host media. Rocks-other than the host-in the ground-water flow path from the repository ideally should be major barriers to radionuclide migration. Confining beds of low permeability might be present to retard the rate of flow between more permeable beds. Additionally, sorption of radionuclides by materials such as clays and zeolites in the flow path can further retard the flow of radionuclides by several orders of magnitude. Tectonic conditions in an area should not present a probable cause for exhumation or increased mobility of radioactive waste. Natural resources are a factor for consideration because of the problem of future human intrusion and exposure to radioactivity in the quest for minerals, oil, gas, water, and geothermal resources.</p><p>The ultimate evaluation of the suitability of a geohydrologic environment for developing a mined repository needs to assess all geologic and hydrologic characteristics and their interaction in providing confidence that a geohydrologic environment will effectively isolate radionuclides from human access. Several hypothetical settings with typical geohydrologic conditions in the Basin and Range Province are used to illustrate the effect of multiple barriers in the isolation of radionuclides.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904A","usgsCitation":"Bedinger, M.S., Sargent, K., and Reed, J., 1984, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part I, Introduction and guidelines: U.S. Geological Survey Circular 904, viii, 16 p., https://doi.org/10.3133/cir904A.","productDescription":"viii, 16 p.","numberOfPages":"26","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335932,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904B","text":"Circular 904-B","linkHelpText":"Part II, Geologic and hydrologic characterization"},{"id":335933,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904C","text":"Circular 904-C","linkHelpText":"Part III, Geologic and hydrologic evaluation"},{"id":121301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0904a/report-thumb.jpg"},{"id":31269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0904a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Oregon, Texas","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.6640625,\n              32.65787573695528\n            ],\n            [\n              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S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":148316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":148314,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":148315,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20368,"text":"ofr84613 - 1984 - January 1984 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr84613","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-613","title":"January 1984 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly during January 1984, in about 1,450 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of 7 consecutive years of measurement (1978-84). The ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84613","usgsCitation":"Pabst, M., and Dague, B., 1984, January 1984 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 84-613, iv, 163 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84613.","productDescription":"iv, 163 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0613/report-thumb.jpg"},{"id":49901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0613/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fb2","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":182529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dague, B.J.","contributorId":45723,"corporation":false,"usgs":true,"family":"Dague","given":"B.J.","affiliations":[],"preferred":false,"id":182530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20388,"text":"ofr8462 - 1984 - A selected bibliography of water resources publications for Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr8462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-62","title":"A selected bibliography of water resources publications for Mississippi","docAbstract":"Hydrologic data were collected at 15 stream sites draining potential lignite areas in Calhoun, Montgomery, and Webster Counties during a period of low streamflow. The total dissolved solids ranged from 25 to 14.9 mg/L and most major ion concentrations were less and suspended sediment concentrations were less than 30 mg/L. The pH ranged from 6.7 to 8.1 units. Aluminum concentrations ranged from less than 100 to 500 micrograms per liter. Chromium and zinc concentrations ranged from 1 to 10 micrograms per gram and mercury concentrations ranged from 0.01 to 0.04 micrograms per gram in bottom material. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8462","usgsCitation":"Parker, G., Walker, D., and Moss, C., 1984, A selected bibliography of water resources publications for Mississippi: U.S. Geological Survey Open-File Report 84-62, iii, 80 p. :maps ;28 cm., https://doi.org/10.3133/ofr8462.","productDescription":"iii, 80 p. :maps ;28 cm.","costCenters":[],"links":[{"id":153628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0062/report-thumb.jpg"},{"id":49937,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a655e","contributors":{"authors":[{"text":"Parker, G.G.","contributorId":107723,"corporation":false,"usgs":true,"family":"Parker","given":"G.G.","email":"","affiliations":[],"preferred":false,"id":182567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walker, Debbe","contributorId":68762,"corporation":false,"usgs":true,"family":"Walker","given":"Debbe","email":"","affiliations":[],"preferred":false,"id":182566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moss, Carol","contributorId":35340,"corporation":false,"usgs":true,"family":"Moss","given":"Carol","affiliations":[],"preferred":false,"id":182565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":233,"text":"wsp2262 - 1984 - Selected papers in the hydrologic sciences 1984; July 1984","interactions":[],"lastModifiedDate":"2018-10-22T18:13:33","indexId":"wsp2262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2262","title":"Selected papers in the hydrologic sciences 1984; July 1984","docAbstract":"The rapid, accurate measurement of the oxygen content of soil gas in the unsaturated zone or dissolved oxygen in soil water in the saturated zone can be useful in wetland vegetation studies. A method has been devised and tested in the Great Dismal Swamp, a wetland with fine silt-clay and organic soils, that appears to provide good results. A 60-milliliter sample of soil gas or water is withdrawn from permanently installed chambers at various depths in the soil profile. The oxygen concentration of air samples is measured with a specially constructed analyzer cell fitted to the polarographic oxygen electrode of a portable oxygen meter. The dissolved oxygen concentration of water samples is measured directly with the oxygen electrode while stirring the sample in a 32-milliliter glass bottle with a portable magnetic stirrer. Field tests with duplicate chamber installations showed that consistent results are obtained for soil gas and water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2262","usgsCitation":"1984, Selected papers in the hydrologic sciences 1984; July 1984: U.S. Geological Survey Water Supply Paper 2262, v, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2262.","productDescription":"v, 66 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2262/report-thumb.jpg"},{"id":24843,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f83da","contributors":{"editors":[{"text":"Meyer, Eric L.","contributorId":58619,"corporation":false,"usgs":true,"family":"Meyer","given":"Eric","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":749260,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":7460,"text":"ofr84760 - 1984 - Proceedings of the Geologic and Hydrologic Hazards Training Program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr84760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-760","title":"Proceedings of the Geologic and Hydrologic Hazards Training Program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84760","usgsCitation":"Williams, M., 1984, Proceedings of the Geologic and Hydrologic Hazards Training Program: U.S. Geological Survey Open-File Report 84-760, iv, 1128 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84760.","productDescription":"iv, 1128 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0760/report-thumb.jpg"},{"id":34881,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34879,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0760/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34880,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0760/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6604a7","contributors":{"authors":[{"text":"Williams, M.E.","contributorId":11613,"corporation":false,"usgs":true,"family":"Williams","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":155714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":138,"text":"wsp2250 - 1984 - National water summary 1983: Hydrologic events and issues","interactions":[],"lastModifiedDate":"2018-03-16T13:06:53","indexId":"wsp2250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2250","title":"National water summary 1983: Hydrologic events and issues","docAbstract":"<p>The United States as a Nation possesses abundant water resources and has developed and used those resources extensively. The national renewable supply of water is about 1,400 billion gallons per day (for the conterminous 48 States). Approximately 380 billion gallons per day of freshwater is withdrawn for use by the Nation's homes, farms, and industries, and about 280 billion gallons per day is returned to streams. Although a large percentage of the Nation's waste is carried in this return flow, the quality of water in streams has improved in many respects as a result of the pollution-control pro- grams of recent years. However, much remains to be learned about water quality particularly the extent of contamination by synthetic organic chemicals and heavy metals, and the effects of these contaminants on human health.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2250","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, National water summary 1983: Hydrologic events and issues: U.S. Geological Survey Water Supply Paper 2250, vi, 243 p., https://doi.org/10.3133/wsp2250.","productDescription":"vi, 243 p.","numberOfPages":"254","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":136153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2250/report-thumb.jpg"},{"id":24749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2250/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698350","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":527188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20655,"text":"ofr84242 - 1984 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr84242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-242","title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3","docAbstract":"Rainfall and discharge data collected at 21 urban hydrology sites in Tennessee from July 1977 to September 1983 are summarized. These rainfall-runoff data will be used to calibrate a U.S. Geological Survey Rainfall-Runoff Model. The results of the model calibrations will then be used to develop reliable methods for determining the magnitude and frequency of floods on small streams in Tennessee where urbanization is a factor. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84242","usgsCitation":"Robbins, C.H., 1984, Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3: U.S. Geological Survey Open-File Report 84-242, iii, 32 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84242.","productDescription":"iii, 32 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":1138,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr84-242","linkFileType":{"id":5,"text":"html"}},{"id":153982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fdfe","contributors":{"authors":[{"text":"Robbins, C. H.","contributorId":54210,"corporation":false,"usgs":true,"family":"Robbins","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":183010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7252,"text":"ofr84584 - 1984 - Illinois ground-water observation network; a preliminary planning document for network design","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr84584","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-584","title":"Illinois ground-water observation network; a preliminary planning document for network design","docAbstract":"Water-level and water-quality networks in Illinois were evaluated to determine the adequacy and completeness of available data bases. Ground-water data in present data bases are inadequate to provide information on ground-water quality and water levels in large areas of Illinois and in the major geohydrologic units underlying Illinois and surrounding areas. Data-management needs indicate that a new data base is desirable and could be developed by use of carefully selected available data and new data. Types of data needed to define ground-water quality and water levels in selected geohydrologic units were tentatively identified. They include data on concentrations of organic chemicals related to activities of man, and concentrations of inorganic chemicals which relate either to man 's activities or to the chemical composition of the source aquifer. Water-level data are needed which can be used to describe short- and long-term stresses on the ground-water resources of Illinois. Establishment of priorities for data collection has been deferred until existing hydrologic data files can be stored for usable data and until input from other local, State, and Federal agencies can be solicited and compiled. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84584","usgsCitation":"Frost, L., O’Hearn, M., Gibb, J., and Sherrill, M., 1984, Illinois ground-water observation network; a preliminary planning document for network design: U.S. Geological Survey Open-File Report 84-584, v, 76 p. :ill., maps ;29 cm., https://doi.org/10.3133/ofr84584.","productDescription":"v, 76 p. :ill., maps ;29 cm.","costCenters":[],"links":[{"id":140356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0584/report-thumb.jpg"},{"id":34630,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0584/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c70e","contributors":{"authors":[{"text":"Frost, L.R.","contributorId":96675,"corporation":false,"usgs":true,"family":"Frost","given":"L.R.","affiliations":[],"preferred":false,"id":154910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Hearn, Michael","contributorId":63801,"corporation":false,"usgs":true,"family":"O’Hearn","given":"Michael","email":"","affiliations":[],"preferred":false,"id":154909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gibb, J.P.","contributorId":48969,"corporation":false,"usgs":true,"family":"Gibb","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154908,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sherrill, M.G.","contributorId":19945,"corporation":false,"usgs":true,"family":"Sherrill","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":154907,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12117,"text":"ofr83765 - 1984 - Hydrology of area 53, northern Great Plains and Rocky Mountain coal provinces, Colorado, Wyoming, and Utah","interactions":[],"lastModifiedDate":"2022-08-26T19:51:33.075067","indexId":"ofr83765","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-765","title":"Hydrology of area 53, northern Great Plains and Rocky Mountain coal provinces, Colorado, Wyoming, and Utah","docAbstract":"Hydrologic information and analysis are needed to aid in decisions to lease Federally owned coal and for the preparation of the necessary Environmental Assessments and Impact Study Reports. This need has become even more critical with the enactment of the Surface Mining Control and Reclamation Act of 1977 (Public Law 95-87). This report, one in a series of nationwide coal province reports, presents information thematically by describing single hydrologic topics through the use of brief texts and accompanying maps, graphs, or other illustrations. The report broadly characterizes the hydrology of Area 53 in northwestern Colorado, south-central Wyoming, and northeastern Utah. \r\n\r\nThe report area, located primarily in the Wyoming Basin and Colorado Plateau physiographic provinces, consists of 14,650 square miles of diverse geology, topography, and climate. This diversity results in contrasting hydrologic characteristics. \r\n\r\nThe two major rivers, the Yampa and the White Rivers, originate in humid granitic and basaltic mountains, then flow over sedimentary rocks underlying semiarid basins to their respective confluences with the Green River. Altitudes range from 4,800 to greater than 12,000 feet above sea level. Annual precipitation in the mountains, as much as 60 inches, is generally in the form of snow. Snowmelt produces most streamflow. Precipitation in the lower altitude sedimentary basins, ranging from 8 to 16 inches, is generally insufficient to sustain streamflow; therefore, most streams originating in the basins (where most of the streams in coal-mining areas originate) are ephemeral. \r\n\r\nStreamflow quality is best in the mountains where dissolved-solids concentrations generally are small. As streams flow across the sedimentary basins, mineral dissolution from the sedimentary rocks and irrigation water with high mineral content increase the dissolved-solids concentrations in a downstream direction. Due to the semiarid climate of the basins, soils are not adequately leached; consequently, flows in the ephemeral streams usually have larger concentrations of dissolved solids than those in perennial streams. \r\n\r\nGround-water supplies are restricted by the low yields of wells due to small permeability. Most ground-water use is for domestic and stock-watering purposes; it is limited by the amount and type of dissolved material. \r\n\r\nThe ground-water ionic composition is highly variable. Dissolved-solids concentrations for aquifers sampled in Area 53 range from a minimum of 46 milligrams per liter to a maximum of 109,000 milligrams per liter. Trace element concentrations generally are not a problem. \r\n\r\nAn estimated 82 billion tons of coal exist above a depth of 6,000 feet in the Colorado parts of the area. The coal beds of greatest economic interest occur in the sedimentary deposits of the Upper Cretaceous Iles and Williams Fork Formations of the Mesaverde Group and the Upper Cretaceous Lance Formation and the Fort Union and Wasatch Formations of Tertiary age. The coal characteristically has a low sulfur content. \r\n\r\nHydrologic problems related to surface mining are erosion, sedimentation, decline in water levels, disruption of aquifers, and degradation of water quality. Because the semiarid mine areas have very little runoff and the major streams have large buffer and dilution capacities, the effects of mining on surface water are minimal. However, effects on ground water may be much more severe and long lasting.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83765","usgsCitation":"Driver, N.E., Norris, J.M., and Kuhn, G., 1984, Hydrology of area 53, northern Great Plains and Rocky Mountain coal provinces, Colorado, Wyoming, and Utah: U.S. Geological Survey Open-File Report 83-765, vi, 93 p., https://doi.org/10.3133/ofr83765.","productDescription":"vi, 93 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":405716,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14213.htm","linkFileType":{"id":5,"text":"html"}},{"id":144806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0765/report-thumb.jpg"},{"id":40144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0765/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Wyoming and Utah","otherGeospatial":"Area 53","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.678,\n              39.454\n            ],\n            [\n              -106.619,\n              39.454\n            ],\n            [\n              -106.619,\n              41.6360\n            ],\n            [\n              -109.678,\n              41.6360\n            ],\n            [\n              -109.678,\n              39.454\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fd7","contributors":{"authors":[{"text":"Driver, N. E.","contributorId":63398,"corporation":false,"usgs":true,"family":"Driver","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":165138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, J. M.","contributorId":87953,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":165139,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":165140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17245,"text":"ofr8461 - 1984 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1982","interactions":[],"lastModifiedDate":"2017-06-14T10:54:20","indexId":"ofr8461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-61","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1982","docAbstract":"<p>Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas, Fort Worth, and San Antonio areas.</p>\n<p>The Geological Survey, in cooperation with the Texas Department of Water Reources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Ealcones Fault Zone.</p>\n<p>The objectives of the Austin urban hydrology study are as follows:</p>\n<ol>\n<li>To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volume.</li>\n<li>To determine the effect of urban development on flood peaks and volume.</li>\n<li>To determine the variations in water quality during different seasons and flow conditions in representative watersheds under various types of urban development.</li>\n<li>To quantitatively appraise the grouna-water resources along the Balcones Fault Zone, the effect of urbanization on the quality and quantity of recharge and discharge, and the extent of contamination in the Edwards aquifer that is in hydrologic circulation with Barton Springs.</li>\n</ol>\n<p>This report presents the basic hydrologic data collected in the Austin urban area for the 1982 water year (Oct. 1, 1981 to Sept. 30, 1982).</p>\n<p>Additional explanations of terms related to streamflow, water quality, and other hydrologic data used in this report are defined in the U.S. Geological Survey annual report Water Resources Data for Texas, TX-82-3, 1982.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr8461","collaboration":"Prepared in cooperation with the City of Austin and the Texas Department of Water Resources","usgsCitation":"Slade, R., Veenhuis, J., Dorsey, M., Stewart, S., and Ruiz, L., 1984, Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1982: U.S. Geological Survey Open-File Report 84-61, vi, 196 p., https://doi.org/10.3133/ofr8461.","productDescription":"vi, 196 p.","numberOfPages":"202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":149338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0061/report-thumb.jpg"},{"id":46394,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0061/report.pdf","text":"Report","size":"3.81 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db60816a","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":175582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Veenhuis, J.E.","contributorId":6850,"corporation":false,"usgs":true,"family":"Veenhuis","given":"J.E.","affiliations":[],"preferred":false,"id":175579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dorsey, M.E.","contributorId":73997,"corporation":false,"usgs":true,"family":"Dorsey","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":175580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stewart, S.L.","contributorId":81117,"corporation":false,"usgs":true,"family":"Stewart","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":175581,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ruiz, L.M.","contributorId":93925,"corporation":false,"usgs":true,"family":"Ruiz","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":175583,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":11505,"text":"ofr82357 - 1984 - Water resources of the Yap Islands","interactions":[],"lastModifiedDate":"2014-10-10T09:08:54","indexId":"ofr82357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-357","title":"Water resources of the Yap Islands","docAbstract":"The Yap Islands consist of four major islands, Yap, Gagil-Tamil, Maap, and Rumung. Of these, Yap Island has more than half the total land area, most of the population, and almost all of the economic development. The islands of Maap and Rumung together compose only 15 percent of the land area and population. Average annual rainfall over the Yap Islands amounts to 122 inches. Rainfall-runoff comparisons indicate that about half of the annual rainfall runs off to the ocean on Yap Island and Gagil-Tamil. Streams on Gagil-Tamil are perennial but streams on Yap Island are dry an average of 3 months per year due to geologic differences. \n\nAnalyses of water samples from 23 sources show the good quality and the chemical similarity of surface and ground water. This report summarizes the hydrologic data collected and provides interpretations that can be used by the planning and public works officials of Yap to make decisions concerning development and management of their water resources.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82357","usgsCitation":"Van der Brug, O., 1984, Water resources of the Yap Islands: U.S. Geological Survey Open-File Report 82-357, xv, 233p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82357.","productDescription":"xv, 233p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0357/report-thumb.jpg"},{"id":39370,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c376","contributors":{"authors":[{"text":"Van der Brug, Otto","contributorId":37347,"corporation":false,"usgs":true,"family":"Van der Brug","given":"Otto","email":"","affiliations":[],"preferred":false,"id":163266,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7243,"text":"ofr83527 - 1984 - Hydrology of area 45, northern Great Plains and Rocky Mountain coal provinces, Montana and North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr83527","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-527","title":"Hydrology of area 45, northern Great Plains and Rocky Mountain coal provinces, Montana and North Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83527","usgsCitation":"Slagle, S.E., and and others, 1984, Hydrology of area 45, northern Great Plains and Rocky Mountain coal provinces, Montana and North Dakota: U.S. Geological Survey Open-File Report 83-527, v, 90 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr83527.","productDescription":"v, 90 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":139845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0527/report-thumb.jpg"},{"id":34626,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0527/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fed","contributors":{"authors":[{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":154883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528821,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11536,"text":"ofr84227 - 1984 - The Hydrologic Instrumentation Facility of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr84227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-227","title":"The Hydrologic Instrumentation Facility of the U.S. Geological Survey","docAbstract":"The U.S. Geological Survey Water Resources Division has improved support to the agencies field offices by the consolidation of all instrumentation support services in a single facility. This facility known as the Hydrologic Instrumentation Facility (HIF) is located at the National Space Technology Laboratory, Mississippi, about 50 miles east of New Orleans, Louisiana. The HIF is responsible for design and development, testing, evaluation, procurement, warehousing, distribution and repair of a variety of specialized hydrologic instrumentation. The centralization has resulted in more efficient and effective support of the Survey 's hydrologic programs. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84227","usgsCitation":"Wagner, C.R., and Jeffers, S., 1984, The Hydrologic Instrumentation Facility of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 84-227, i, 34 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84227.","productDescription":"i, 34 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":144573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0227/report-thumb.jpg"},{"id":39398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0227/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c34f","contributors":{"authors":[{"text":"Wagner, C. R.","contributorId":102881,"corporation":false,"usgs":true,"family":"Wagner","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jeffers, Sharon","contributorId":12862,"corporation":false,"usgs":true,"family":"Jeffers","given":"Sharon","email":"","affiliations":[],"preferred":false,"id":163321,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","interactions":[{"subject":{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","indexId":"ofr8278","publicationYear":"1982","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium"},"predicate":"SUPERSEDED_BY","object":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"id":1}],"lastModifiedDate":"2022-02-04T19:13:10.348121","indexId":"wsp2226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2226","title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","docAbstract":"A low-level radioactive-waste burial site is located in Palos Forest Preserve, about 22 kilometers southwest of Chicago, Illinois. Between 1943 and 1949 the site, named Plot M, was filled with radioactive waste from the first Argonne National Laboratory and from the University of Chicago Metallurgical Laboratory. Since 1973, tritium concentration levels up to 14 nanocuries per liter have been measured in water samples collected from a well 360 meters from the burial site. \r\n\r\nThe U.S. Geological Survey is studying the geologic, hydrologic, and geochemical properties of the glacial drift and underlying bedrock at the Plot M site to determine the factors that control the movement of radionuclides. Test wells were drilled into the drift to collect water and core samples for laboratory analysis, to gather geologic and hydrologic data, and to conduct geophysical surveys. Plot M is located in drift that ranges in thickness from 25 to 45 meters. The drift is a stratified sequence of clay- and silt-rich sediments that contain thin, interstratified sand layers. The silt content of the drift increases with depth. The permeability of the drift, as indicated by field and laboratory hydraulic conductivity tests, ranges from 1.0 x 10 -6 to 1.0 ? 10 -8 centimeters per second. \r\n\r\nA tritium plume, the contaminated zone in the drift in which tritium concentration levels exceed 10 nanocuries per liter of water, extends horizontally northward from Plot M at least 50 meters and vertically downward to bedrock. The center of the plume, where tritium concentration levels are as high as 50,000 nanocuries per liter, is approximately 15 meters beneath the burial site. The size, shape, and 'bull's-eye' concentration pattern indicate that the plume is a single slug and that the site no longer releases tritium into the drift. The leading edge, or front, of the plume (the 10 nanocuries per liter boundary) left the burial site in either the late 1940's or the early 1950's and intersected the underlying bedrock surface before 1973. The calculated movement rate of the front is 6.3 x 10 -6 centimeters per second. \r\n\r\nSeveral key factors that control both the concentration level and the extent of migration of tritium in the drift at Plot M are 1. The limited amount of tritiated waste buried at Plot M. 2. The long period of time that has elapsed since the waste was buried (30-35 years) relative to the radioactive half-life of tritium (12.3 years). 3. The great thickness and low permeability of the glacial drift at the site.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2226","usgsCitation":"Olimpio, J.C., 1984, Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium: U.S. Geological Survey Water Supply Paper 2226, iv, 34 p., https://doi.org/10.3133/wsp2226.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":395461,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25214.htm"},{"id":28419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2226/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2226/report-thumb.jpg"}],"country":"United States","state":"Illinios","otherGeospatial":"Palos Forest Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.906,\n              41.694\n            ],\n            [\n              -87.917,\n              41.694\n            ],\n            [\n              -87.917,\n              41.704\n            ],\n            [\n              -87.906,\n              41.704\n            ],\n            [\n              -87.906,\n              41.694\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648815","contributors":{"authors":[{"text":"Olimpio, Julio C.","contributorId":93877,"corporation":false,"usgs":true,"family":"Olimpio","given":"Julio","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7056,"text":"ofr84247 - 1984 - Climatic data for Williams Lake, Hubbard County, Minnesota, 1983","interactions":[],"lastModifiedDate":"2018-04-02T11:33:30","indexId":"ofr84247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-247","title":"Climatic data for Williams Lake, Hubbard County, Minnesota, 1983","docAbstract":"<p>Research on the hydrology of Williams Lake, north-central Minnesota includes study of evaporation. Presented here are those climatic data needed for energy-budget and mass-transfer studies,including: water-surface temperature, dry-bulb and wet-bulb air temperatures, wind speed, precipitation, and solar radiation. Data are collected at raft and land stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr84247","usgsCitation":"Sturrock, A., Rosenberry, D., Engelbrecht, L., Gothard, W., and Winter, T.C., 1984, Climatic data for Williams Lake, Hubbard County, Minnesota, 1983: U.S. Geological Survey Open-File Report 84-247, 41 p., https://doi.org/10.3133/ofr84247.","productDescription":"41 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":140587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0247/report-thumb.jpg"},{"id":34352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Hubbard County","otherGeospatial":"Williams Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de191","contributors":{"authors":[{"text":"Sturrock, A.M.","contributorId":25947,"corporation":false,"usgs":true,"family":"Sturrock","given":"A.M.","affiliations":[],"preferred":false,"id":154108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenberry, D.O. 0000-0003-0681-5641","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":38500,"corporation":false,"usgs":true,"family":"Rosenberry","given":"D.O.","affiliations":[],"preferred":true,"id":154110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engelbrecht, L.G.","contributorId":53227,"corporation":false,"usgs":true,"family":"Engelbrecht","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":154111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gothard, W.A.","contributorId":29690,"corporation":false,"usgs":true,"family":"Gothard","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":154109,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":154107,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":12121,"text":"ofr83698 - 1984 - Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr83698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-698","title":"Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","docAbstract":"This report summarizes available hydrologic data for Area 62 and will aid leasing decisions, and the preparation and appraisal of environmental impact studies and mine-permit applications. Area 62 is located at the southern end of the Rocky Mountain Coal Province in parts of New Mexico and Arizona and includes approximately 9,500 square miles. Surface mining alters, at least temporarily, the environment; if the areas are unreclaimed, there can be long-term environmental consequences.\r\n\r\nThe land-ownership pattern in Area 62 is complicated. The checkerboard pattern created by several types of ownership makes effective management of these lands difficult.\r\n\r\nThe climate generally is semiarid with average annual precipitation ranging from 10 to 20 inches. Pinons, junipers, and grasslands cover most of the area, and much of it is used for grazing by livestock. Soils vary with landscape, differing from flood plains and hillslopes to mountain slopes.\r\n\r\nThe major structural features of this area were largely developed during middle Tertiary time. The main structural features are the southern San Juan Basin and the Mogollon slope. Coal-bearing rocks are present in four Cretaceous rock units of the Mesaverde Group: the Gallup Sandstone, the Dileo Coal Member, and the Gibson Coal Member of the Crevasse Canyon Formation, and the Cleary Coal Member of the Menefee Formation.\r\n\r\nArea 62 is drained by Black Creek, the Puerco River, the Zuni River, Carrizo Wash-Largo Creek, and the Rio San Jose. Only at the headwaters of the Zuni River is the flow perennial. The streamflow-gaging station network consists of 25 stations operated for a variety of needs. Streamflow changes throughout the year with variation related directly to rainfall and snowmelt. Base flow in Area 62 is zero indicating no significant ground-water discharge. Mountainous areas contribute the highest mean annual runoff of 1.0 inch. Very few water-quality data are available for the surface-water stations. Of the nine surface-water stations that have water-quality data, only one has chemical analyses from more than 10 samples. Therefore, sufficient data to characterize the area in detail are not available. Suspended sediment data are available only for a few surface-\r\nwater stations in the area. Erosion rates generally are less than 1 acre-foot per square mile per year. Greater erosion rates are found within the badland areas.\r\n\r\nWater levels are periodically measured at 21 selected wells in Area 62. These observation wells are located mostly along the Rio San Jose and northeast of Gallup, New Mexico. The recharge to ground-water aquifers generally coincide with areas of greater precipitation in the mountainous areas. Depth to water below land surface is generally less than 200 feet. Well yields of 100 gallons per minute are common in most of the area.\r\n\r\nGround-water quality is variable both within each aquifer and between aquifers. Water quality generally is best near recharge areas.\r\n\r\nHistorical and current data related to stream discharge, water quality, and suspended sediment are available from computer files in the U.S. Geological Survey's National Water Data Storage and Retrieval System (WATSTORE) and through the National Water Data Exchange (NAWDEX).","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83698","usgsCitation":"Roybal, F., Wells, J., Gold, R., and Flager, J., 1984, Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona (WRI/OFR 83-698): U.S. Geological Survey Open-File Report 83-698, v, 66 p., https://doi.org/10.3133/ofr83698.","productDescription":"v, 66 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":146287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0698/report-thumb.jpg"},{"id":40145,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,34 ], [ -110,36 ], [ -107.5,36 ], [ -107.5,34 ], [ -110,34 ] ] ] } } ] }","edition":"WRI/OFR 83-698","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604be4","contributors":{"authors":[{"text":"Roybal, F.E.","contributorId":62998,"corporation":false,"usgs":true,"family":"Roybal","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":165151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J.G.","contributorId":85198,"corporation":false,"usgs":true,"family":"Wells","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":165153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":165154,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flager, J.V.","contributorId":72799,"corporation":false,"usgs":true,"family":"Flager","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":165152,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12316,"text":"ofr84739 - 1984 - Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste; characterization of the Trans-Pecos region, Texas","interactions":[{"subject":{"id":12316,"text":"ofr84739 - 1984 - Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste; characterization of the Trans-Pecos region, Texas","indexId":"ofr84739","publicationYear":"1984","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste; characterization of the Trans-Pecos region, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":38491,"text":"pp1370B - 1989 - Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Trans-Pecos region, Texas","indexId":"pp1370B","publicationYear":"1989","noYear":false,"chapter":"B","title":"Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Trans-Pecos region, Texas"},"id":1}],"supersededBy":{"id":38491,"text":"pp1370B - 1989 - Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Trans-Pecos region, Texas","indexId":"pp1370B","publicationYear":"1989","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Trans-Pecos region, Texas"},"lastModifiedDate":"2021-02-22T21:46:21.868305","indexId":"ofr84739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-739","title":"Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste; characterization of the Trans-Pecos region, Texas","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84739","usgsCitation":"1984, Studies of geology and hydrology in the Basin and Range Province, southwestern United States, for isolation of high-level radioactive waste; characterization of the Trans-Pecos region, Texas: U.S. Geological Survey Open-File Report 84-739, Report: xiv, 122 p.; 9 Plates: 30.70 x 23.08 inches or smaller, https://doi.org/10.3133/ofr84739.","productDescription":"Report: xiv, 122 p.; 9 Plates: 30.70 x 23.08 inches or smaller","costCenters":[],"links":[{"id":383513,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383512,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383511,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383510,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383506,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-7-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383505,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-7-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383504,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0739/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383509,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383508,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383507,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0739/plate-7-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0739/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Trans-Pecos region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.8148193359375,\n              30.278044377800153\n            ],\n            [\n              -102.2662353515625,\n              30.278044377800153\n            ],\n            [\n              -102.2662353515625,\n              31.704803074739214\n            ],\n            [\n              -105.8148193359375,\n              31.704803074739214\n            ],\n            [\n              -105.8148193359375,\n              30.278044377800153\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fef","contributors":{"editors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":503990,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503989,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":503988,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}}
,{"id":12315,"text":"ofr84742 - 1984 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Sonoran region, California","interactions":[{"subject":{"id":12315,"text":"ofr84742 - 1984 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Sonoran region, California","indexId":"ofr84742","publicationYear":"1984","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Sonoran region, California"},"predicate":"SUPERSEDED_BY","object":{"id":38493,"text":"pp1370E - 1989 - Studies of geology and hydrology in the Basin and Range province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Sonoran region, California","indexId":"pp1370E","publicationYear":"1989","noYear":false,"chapter":"E","title":"Studies of geology and hydrology in the Basin and Range province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Sonoran region, California"},"id":1}],"supersededBy":{"id":38493,"text":"pp1370E - 1989 - Studies of geology and hydrology in the Basin and Range province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Sonoran region, California","indexId":"pp1370E","publicationYear":"1989","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range province, southwestern United States, for isolation of high-level radioactive waste: Characterization of the Sonoran region, California"},"lastModifiedDate":"2020-02-03T12:24:47","indexId":"ofr84742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-742","title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Sonoran region, California","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84742","usgsCitation":"1984, Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Sonoran region, California: U.S. Geological Survey Open-File Report 84-742, Report: xiv 103 p.; 6 Plates: 33.07 x 38.77 inches or smaller, https://doi.org/10.3133/ofr84742.","productDescription":"Report: xiv 103 p.; 6 Plates: 33.07 x 38.77 inches or smaller","costCenters":[],"links":[{"id":145532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0742/report-thumb.jpg"},{"id":371929,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0742/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371930,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371931,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371932,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371933,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371934,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":371935,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0742/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Basin and Range Province, Southwestern United States, Sonoran region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.21289062499999,\n              31.541089879585808\n            ],\n            [\n              -106.3037109375,\n              31.541089879585808\n            ],\n            [\n              -106.3037109375,\n              40.88029480552824\n            ],\n            [\n              -118.21289062499999,\n              40.88029480552824\n            ],\n            [\n              -118.21289062499999,\n              31.541089879585808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a0f6","contributors":{"editors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":503987,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":503986,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":503985,"contributorType":{"id":2,"text":"Editors"},"rank":3}]}}
,{"id":9834,"text":"ofr84608 - 1984 - Availability of hydrologic data in San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr84608","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-608","title":"Availability of hydrologic data in San Juan County, New Mexico","docAbstract":"San Juan County, in the northwestern corner of New Mexico, uses surface water from the San Juan, Animas, and La Plata Rivers as a principal source of water for the county, but the water in these streams is fully appropriated. Ground water is present in San Juan County in several bedrock formations and in the alluvium of the river valleys. This report describes the hydrologic data that have been collected in San Juan County, presents examples of the data, shows the locations of the data-collection sites, and indicates where more complete records may be obtained. This data base should be helpful in assessing the quantity, quality, and availability of the county 's water resources. Information collected at 1,877 water wells, 39 streamflow-gaging stations, and 172 springs is presented. The collection sites and geology are shown on a base map with a scale of 1 inch = 2 miles. (USGS).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84608","usgsCitation":"Klausing, R., and Welder, G.E., 1984, Availability of hydrologic data in San Juan County, New Mexico: U.S. Geological Survey Open-File Report 84-608, iv, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84608.","productDescription":"iv, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0608/report-thumb.jpg"},{"id":37618,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0608/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0608/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d561","contributors":{"authors":[{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":160381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15611,"text":"ofr84459 - 1984 - The principle of superposition and its application in ground-water hydraulics","interactions":[{"subject":{"id":15611,"text":"ofr84459 - 1984 - The principle of superposition and its application in ground-water hydraulics","indexId":"ofr84459","publicationYear":"1984","noYear":false,"title":"The principle of superposition and its application in ground-water hydraulics"},"predicate":"SUPERSEDED_BY","object":{"id":4709,"text":"twri03B6 - 1987 - The principle of superposition and its application in ground-water hydraulics","indexId":"twri03B6","publicationYear":"1987","noYear":false,"title":"The principle of superposition and its application in ground-water hydraulics"},"id":1}],"supersededBy":{"id":4709,"text":"twri03B6 - 1987 - The principle of superposition and its application in ground-water hydraulics","indexId":"twri03B6","publicationYear":"1987","noYear":false,"title":"The principle of superposition and its application in ground-water hydraulics"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr84459","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-459","title":"The principle of superposition and its application in ground-water hydraulics","docAbstract":"The principle of superposition, a powerful methematical technique for analyzing certain types of complex problems in many areas of science and technology, has important application in ground-water hydraulics and modeling of ground-water systems. The principle of superposition states that solutions to individual problems can be added together to obtain solutions to complex problems. This principle applies to linear systems governed by linear differential equations. This report introduces the principle of superposition as it applies to groundwater hydrology and provides background information, discussion, illustrative problems with solutions, and problems to be solved by the reader. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84459","usgsCitation":"Reilly, T.E., Franke, O., and Bennett, G., 1984, The principle of superposition and its application in ground-water hydraulics: U.S. Geological Survey Open-File Report 84-459, vi, 36 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84459.","productDescription":"vi, 36 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":112992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0459/report.pdf","size":"3087","linkFileType":{"id":1,"text":"pdf"}},{"id":147427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0459/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db641cb8","contributors":{"authors":[{"text":"Reilly, T. E.","contributorId":79460,"corporation":false,"usgs":true,"family":"Reilly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franke, O.L.","contributorId":57082,"corporation":false,"usgs":true,"family":"Franke","given":"O.L.","affiliations":[],"preferred":false,"id":171428,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, G.D.","contributorId":81073,"corporation":false,"usgs":true,"family":"Bennett","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":171430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15627,"text":"ofr84713 - 1984 - Ground-water resources of Limestone County, Texas","interactions":[],"lastModifiedDate":"2016-08-11T16:35:01","indexId":"ofr84713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-713","title":"Ground-water resources of Limestone County, Texas","docAbstract":"<p>Limestone County, located in east-central Texas, has small to plentiful ground-water supplies available, depending upon the location within the county. The Wilcox Group in the eastern part of the county has adequate supplies to meet the expected water demands in the foreseeable future. The thicker zones of the Wilcox Group can supply yields in excess of 500 gallons per minute. The Midway Group can supply yields in excess of 100 gallons per minute from the Tehuacana Member of the Kincaid Formation. This represents the largest well yields from the Midway Group in Texas. The Midway Group elsewhere in the State is mostly a poor water producer and is not considered an aquifer. The Taylor Marl and Navarro Group furnish only small quantities of ground water to wells in the western part of the county where these units crop out. The Hosston and Travis Peak Formations are present at depths in excess of 2,000 feet. These formations, which contain slightly saline water in the western part of the county, could be expected to produce water with a temperature of about 150&deg;F that might be used for heating purposes.</p>\n<p>About 0.9 million gallons per day of ground water was used for all purposes in 1980. This use has declined since 1955 but is expected to increase as additional public-supply and industrial wells are being developed. The Wilcox Group is capable of annually yielding at least 14,000 acre-feet or 11.6 million gallons per day of water to wells on a long-term basis.</p>\n<p>Generally, the ground water is of acceptable quality for most uses. Relatively high dissolved-solids and iron concentrations are the major water-quality problems. Water-quality problems that may be the result of man's activities are limited to a small oilfield area near Mexia.</p>\n<p>Lignite mining from the Wilcox Group is expected to take place in the foreseeable future. The collection of additional hydrologic data on the Wilcox would be desirable before, during, and after mining.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Ausitn, TX","doi":"10.3133/ofr84713","usgsCitation":"Rettman, P., 1984, Ground-water resources of Limestone County, Texas: U.S. Geological Survey Open-File Report 84-713, vi, 92 p., https://doi.org/10.3133/ofr84713.","productDescription":"vi, 92 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":147309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0713/report-thumb.jpg"},{"id":44590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","county":"Limestone County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.4998,31.8005],[-96.4298,31.7011],[-96.2333,31.4115],[-96.3228,31.3661],[-96.3236,31.3593],[-96.5948,31.2235],[-96.8,31.5192],[-96.9329,31.7114],[-96.7184,31.8195],[-96.4998,31.8005]]]},\"properties\":{\"name\":\"Limestone\",\"state\":\"TX\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d38","contributors":{"authors":[{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":171457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9729,"text":"ofr84462 - 1984 - Background hydrologic information in potential lignite mining areas in northeastern Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr84462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-462","title":"Background hydrologic information in potential lignite mining areas in northeastern Mississippi","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84462","usgsCitation":"Kalkhoff, S., 1984, Background hydrologic information in potential lignite mining areas in northeastern Mississippi: U.S. Geological Survey Open-File Report 84-462, iv, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84462.","productDescription":"iv, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0462/report-thumb.jpg"},{"id":37474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0462/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adbf","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":160199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","interactions":[{"subject":{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"ofr84612","publicationYear":"1984","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"id":1}],"supersededBy":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"lastModifiedDate":"2020-06-12T20:58:33.037696","indexId":"ofr84612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-612","title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","docAbstract":"On July 15, 1982, Lawn Lake Dam, a 26-foot-high earthfill irrigation dam built in 1903 in Rocky Mountain National Park, Colorado, failed, due to piping, releasing 674 acre-feet of water with a peak discharge of 18,000 cubic feet per second down the Roaring River. Three people were killed, and damages were estimated at $31 million. Cascade Lake Dam, downstream from Lawn Lake Dam, subsequently failed as a result of the flood, increasing the peak flow at this point from 7,210 cubic feet per second to 16,000 cubic feet per second. The flood wave took 3.28 hours to travel 12.5 miles to Lake Estes, where all the floodwater was stored. The channel of the Roaring River was scoured as much as 50 feet and widened 300 feet. An alluvial fan of 42.3 acres, containing 10 million cubic feet of material, was deposited at the mouth of the Roaring River, damming the Fall River and forming a 17-acre lake. Various methods were used to indirectly compute peak discharge, attenuation of flow, and flood traveltime. A version of the National Weather Service dam-break flood model was used to evaluate its performance on high-gradient streams, to provide supplemental hydrologic information, and to evaluate various scenarios of dam-break development. 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