During the period October 1978 to September 1983, the U.S. Geological Survey, in cooperation with the City of Portland (Oregon) Water Bureau, conducted a study in the Bull Run River basin to define the hydrologic characteristics of the basin, and to examine relations between basin characteristics (both natural and man-made) and stream water quality and quantity within the basin. Hydrologically, the 1978-1983 period can be characterized as representative of the long-term average, with no records of extreme events. Likewise, water quality constituent concentrations affected by quantity of streamflow are representative of average values and ranges and exclude values that would be obtained during periods of extreme events. Ranges of concentration of major anions and cations for surface water collected October 1978 to September 1983 are similar to values collected historically. The ratio of constituent to chloride values determined for precipitation data collected during the period June 1980 to September 1981 indicated that other sources besides seawater contributed to its composition. In ratios of constituents in precipitation, Bull Run values are similar to those of other remote sites in Alaska, Washington, and California. Comparisons of storm-related suspended sediment load to annual suspended sediment loads indicated that 62% to 78% of the total annual loads occurred in 3 to 4 days during an average year. Multiple-linear regression analysis using discharge, suspended sediment and specific conductance indicated that most of the variation in the annual values could be explained by naturally occurring processes within the basin. A nonparametric time-trend analysis of 24 water quantity and quality constituents showed no statistically significant trends with estimated slopes large enough to be readily measurable for a particular year. Four constituents that were sampled weekly (turbidity, specific conductance, silica, and phytoplankton) had statistically significant trends with slope indicators that might be measurable after 6 years. However, trend analysis on daily mean specific conductance and suspended sediment values does not confirm the weekly constituent trend results.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1257","usgsCitation":"Robson, S.G., 1987, Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal: U.S. Geological Survey Professional Paper 1257, Report: v, 73 p.; 5 Plates: 29.00 × 39.00 inches, https://doi.org/10.3133/pp1257.","productDescription":"Report: v, 73 p.; 5 Plates: 29.00 × 39.00 inches","costCenters":[],"links":[{"id":104583,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4771.htm","linkFileType":{"id":5,"text":"html"},"description":"4771"},{"id":33712,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1257/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33711,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33710,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33709,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33708,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33707,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1257/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Denver Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.275,\n 38.6389\n ],\n [\n -103.6458,\n 38.6389\n ],\n [\n -103.5458,\n 40.4167\n ],\n [\n -105.275,\n 40.4167\n ],\n [\n -105.275,\n 38.6389\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63da79","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":152569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39662,"text":"pp1368 - 1987 - Late Mississippian gastropods of the Chainman Shale, west-central Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"pp1368","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1368","title":"Late Mississippian gastropods of the Chainman Shale, west-central Utah","docAbstract":"The Chainman Shale of Mississippian (Osagean to late Chesterian) age, well exposed in the Confusion Range of western Utah, has yielded a profusion of fossils during investigations conducted by the U.S. Geological Survey in the past 30 years. Conspicuous among these fossils are gastropods, which range in age from latest Meramecian to late Chesterian. In west-central Utah, not far from the State boundary, the Chainman outcrop belt stretches from Granite Mountain south to the northern part of the Needle Range, a distance of69 miles (110 km). The Chainman thickens from north to south; the section at Granite Mountain is 1,315 feet (401 m) thick and that at Jensen Wash in the Burbank Hills, 2,203 feet (671 m). \r\n\r\nThe rocks of the Chainman Shale record a general though irregular shallowing of the area from moderate depths of 330 feet (100 m) or so to quite shallow depths of perhaps locally little more than 3-6 feet (1-2 m). Most of the gastropods occur with ammonoids in a facies of shale or shale containing phosphatic limestone concretions, In this lutaceous facies, Glabrocingulum is predominant and Lunulazona and Retispira are common; these genera are represented by a succession of species. A thick limestone unit is present in some areas in the upper part of the formation, particularly in the vicinity of Skunk Spring, where it is 318 feet (97 m) thick. This limestone unit represents a calcareous shoal facies having an entirely different gastropod fauna, characterized by Catazona and species of Naticopsis. \r\n\r\nThe Chainman Shale could be easily zoned by gastropods, but we are not proposing such azonation. A framework of ammonoid and foraminiferal zones already is available, and we prefer to regard the gastropod assemblages as part of this framework. The assemblages are confined to the major ammonoid and foraminiferal zones, and only three of the gastropod species seem to range across major zonal boundaries. These species are Bellerophon (Bellerophon vespertinus Gordon and Yochelson and Straparollus (Euomphalus intermedius Gordon and Yochelson, both of which are present in Mamet Foraminifer Zones 17 and 18, and Bellazona polita n. sp., which locally seems to range from Mamet Foraminifer Zone 16s into the basal part of Zone 17. \r\n\r\nEight assemblages, seven of them in ascending stratigraphic order, are recognized within the gastropod fauna of the Chainman Shale; the eighth assemblage is a facies equivalent of the sixth highest. The seven mud-dwelling assemblages are characterized mainly by species of Glabrocingulum and Lunulazona, which together account for 80 percent of the gastropod specimens in our Chainman collections. The eighth assemblage, that in the shallow-water carbonate facies, is the one characterized by Catazona and species of Naticopsis. \r\n\r\nThe lowermost gastropod assemblage, that of Lunulazona nodomarginata (McChesney), includes 10 species and is restricted to the northern end of the study area, where it occurs in the upper part of the Goniatites americanus Ammonoid Zone, in beds equivalent to the lower part of Mamet's Foraminifer Zone 16i. We regard the entire G. americanus Zone as late Meramecian in age. All the zones higher in the Chainman are Chesterian in age. The second assemblage is that of Lunulazona costata Sadlick and Neilsen, which includes six gastropod species; it occurs in the Goniatites granos us Ammonoid Zone, equivalent to Mamet's Foraminifer Zone 16s. \r\n\r\nThree gastropod assemblages are recognized within the Paracravenoceras barnettense Ammonoid Zone, equivalent to Mamet's Foraminifer Zone 17. The earliest, that of Lunulazona sadlicki, includes five species; the intermediate, that of Glabrocingulum hosei n. sp., four species; and the highest, that of Glabrocingulum confusionense n, sp., two species (the second being G. hosei). \r\n\r\nTwo laterally equivalent facies-controlled assemblages are present within the Cravenoceras hesperium Ammonoid Zone, most of which is equivalent to Mamet's Foraminifer Zone 18","language":"ENGLISH","doi":"10.3133/pp1368","usgsCitation":"Gordon, M., and Yochelson, E.L., 1987, Late Mississippian gastropods of the Chainman Shale, west-central Utah: U.S. Geological Survey Professional Paper 1368, 112 p., https://doi.org/10.3133/pp1368.","productDescription":"112 p.","costCenters":[],"links":[{"id":119440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1368/report-thumb.jpg"},{"id":67382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1368/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bdc","contributors":{"authors":[{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":221936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":221937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25546,"text":"wri874115 - 1987 - Ground-water and soil contamination near two pesticide-burial sites in Minnesota","interactions":[],"lastModifiedDate":"2025-01-07T22:08:08.336463","indexId":"wri874115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4115","title":"Ground-water and soil contamination near two pesticide-burial sites in Minnesota","docAbstract":"Preliminary investigations of the geology, groundwater hydrology , and soil and groundwater chemistry at sites in Pine and St. Louis Counties, Minnesota, have shown that contamination associated with pesticides buried at the sites is not widespread or highly concentrated. None of the pesticides sampled for in soil and in groundwater at the sites exceeded Minnesota soil and drinking water standards. About 1,500 pounds of lead arsenate were buried at the site in St. Louis County. Nearly 10,000 pounds of lead arsenate, as well as smaller quantities of organic pesticides (such as chlorpropham, DDT, endrin, and aldrin), lime sulfur, and magnesium carbonate were buried at the Pine County site. These chemicals were buried in shallow trenches at the sites during the early 1970's.
\nThe first wells drilled at each site were located to establish the direction of horizontal groundwater flow in each area. Groundwater flows to the northeast at the St. Louis County site and to the southeast at the Pine County site. Depths to the water table are about 30 ft at the Pine County site and about 25 ft at the St. Louis County site. In addition, groundwater is perched seasonally at about 5 ft below land surface in the immediate vicinity fo the burial site in Pine County. After the direction of flow was determined, additional wells were drilled down-gradient from the disposal areas at both sites to determine whether contaminations were migrating with groundwater away from the sites.
\nIn general, concentrations of lead and arsenic in soil and groundwater were below background concentrations for the areas. Concentrations of organic pesticides generally were below analytical-detection limits. The limited solubility of the chemicals and the tendency of the contaminants to be sorbed on soil particles probably combined to restrict mobilization of the chemicals.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri874115","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"Stark, J., Strudell, J., Bloomgren, P., and Eger, P., 1987, Ground-water and soil contamination near two pesticide-burial sites in Minnesota: U.S. Geological Survey Water-Resources Investigations Report 87-4115, vii, 48 p., https://doi.org/10.3133/wri874115.","productDescription":"vii, 48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":54266,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4115/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123310,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4115/report-thumb.jpg"},{"id":465853,"rank":3,"type":{"id":36,"text":"NGMDB Index 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J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":194139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strudell, J.D.","contributorId":16869,"corporation":false,"usgs":true,"family":"Strudell","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":194136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bloomgren, P.A.","contributorId":19599,"corporation":false,"usgs":true,"family":"Bloomgren","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":194137,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eger, P.","contributorId":26330,"corporation":false,"usgs":true,"family":"Eger","given":"P.","email":"","affiliations":[],"preferred":false,"id":194138,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":3603,"text":"cir968 - 1987 - Development of sinkholes resulting from man's activities in the Eastern United States","interactions":[],"lastModifiedDate":"2016-01-25T10:39:26","indexId":"cir968","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"968","title":"Development of sinkholes resulting from man's activities in the Eastern United States","docAbstract":"Development of induced sinkholes in carbonate terranes in the Eastern United States has resulted in costly damage and water pollution. Previously, detailed investigations of sinkholes were limited to Alabama and Missouri, with the most comprehensive being in Alabama. An investigation of the remainder of the area was made in 1981 to regionalize previous findings. More than 850 sites of sinkhole development have been identified in 19 States. It is estimated that more than 6,500 sinkholes or related features have formed at these sites. Most have occurred since 1950. Based on information available, States most impacted are Alabama, Florida, Georgia, Missouri, Pennsylvania, and Tennessee.
\nThe total cost of damage and associated protective measures resulting from induced sinkholes is unknown. Costs reported for a limited number of sites were about $170 million--expended almost entirely after 1970. About $140 million were expended at five dams in four States and to repair or protect highways in two States.
\nSinkholes are of two types, natural and induced {accelerated or caused by man}. The sudden development of both types results from the collapse of the roof of a cavity or cavern in rock, or from the downward migration of unconsolidated deposits into solutionally enlarged openings in the top of bedrock. The occurrence of sinkholes resulting from bedrock roof collapses, in comparison with the occurrence of sinkholes resulting from downward migration of unconsolidated deposits, is rare.
\nInduced sinkholes are of two types: those resulting from a decline in water level due to ground-water withdrawals and those resulting from construction. Sinkholes resulting from water-level declines are caused by loss of buoyant support, increase in velocity of water movement, water-level fluctuations, and induced recharge. Most induced sinkholes resulting from construction are caused by the diversion or impoundment of surface drainage over unconsolidated deposits resting on openings in the top of bedrock. Collapse mechanisms include loading, saturation, and piping.
\nAssessment of existing or potential sinkhole problems at a site requires recognition of features associated with sinkhole development and knowledge of triggering mechanisms that cause sinkholes. Natural sinkhole development is generally not predictable. Induced sinkhole development is predictable in some instances, but is predictable only in the sense that it will occur in a particular area. The most predictable development results from dewatering by wells, quarries, and mines.
\nAlternatives that allow avoiding or minimizing sinkhole hazards are most numerous when a problem or potential problem is recognized during site evaluation. The number of alternatives declines after the beginning of site development. Where sinkhole development is predictable, zoning of land use can minimize hazards.
","language":"English","publisher":"U.S. Government Print Office","doi":"10.3133/cir968","usgsCitation":"Newton, J.G., 1987, Development of sinkholes resulting from man's activities in the Eastern United States: U.S. Geological Survey Circular 968, iv, 54 p., https://doi.org/10.3133/cir968.","productDescription":"iv, 54 p.","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":30638,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0968/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0968/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.294921875,\n 49.009050809382046\n ],\n [\n -96.8115234375,\n 45.460130637921004\n ],\n [\n -96.6357421875,\n 42.65012181368025\n ],\n [\n -95.5810546875,\n 40.01078714046552\n ],\n [\n -94.658203125,\n 39.027718840211605\n ],\n [\n -94.41650390625,\n 33.578014746143985\n ],\n [\n -94.130859375,\n 33.52307880890422\n ],\n [\n -94.0869140625,\n 32.02670629333614\n ],\n [\n -93.55957031249999,\n 31.109388560814963\n ],\n [\n -93.91113281249999,\n 29.7453016622136\n ],\n [\n -89.09912109375,\n 29.05616970274342\n ],\n [\n -89.45068359374999,\n 30.183121842195515\n ],\n [\n -86.68212890625,\n 30.372875188118016\n ],\n [\n -85.23193359375,\n 29.554345125748267\n ],\n [\n -84.17724609375,\n 30.088107753367257\n ],\n [\n -82.7490234375,\n 28.94086176940557\n ],\n [\n -82.9248046875,\n 27.9361805667694\n ],\n [\n -81.97998046875,\n 26.352497858154\n ],\n [\n -81.18896484375,\n 25.045792240303445\n ],\n [\n -80.17822265625,\n 25.145284610685064\n ],\n [\n -79.91455078125,\n 26.941659545381516\n ],\n [\n -80.48583984375,\n 28.57487404744697\n ],\n [\n -81.38671875,\n 30.675715404167743\n ],\n [\n -80.88134765625,\n 31.89621446335144\n ],\n [\n -79.07958984375,\n 33.15594830078649\n ],\n [\n -77.9150390625,\n 33.925129700072\n ],\n [\n -76.3330078125,\n 34.75966612466248\n ],\n [\n -75.4541015625,\n 35.97800618085568\n ],\n [\n -75.8056640625,\n 37.03763967977139\n ],\n [\n -74.90478515625,\n 38.75408327579141\n ],\n [\n -73.76220703125,\n 40.463666324587685\n ],\n [\n -71.4990234375,\n 41.0130657870063\n ],\n [\n -69.5654296875,\n 41.73852846935917\n ],\n [\n -70.4443359375,\n 42.53689200787317\n ],\n [\n -70.33447265624999,\n 43.40504748787035\n ],\n [\n -66.884765625,\n 44.574817404670306\n ],\n [\n -67.7197265625,\n 45.75219336063106\n ],\n [\n -67.78564453125,\n 47.17477833929903\n ],\n [\n -68.22509765625,\n 47.428087261714275\n ],\n [\n -69.19189453125,\n 47.487513008956554\n ],\n [\n -69.98291015625,\n 46.78501604269254\n ],\n [\n -71.54296874999999,\n 45.042478050891546\n ],\n [\n -74.8388671875,\n 45.042478050891546\n ],\n [\n -76.81640625,\n 43.644025847699496\n ],\n [\n -79.07958984375,\n 43.59630591596548\n ],\n [\n -79.03564453124999,\n 42.89206418807337\n ],\n [\n -82.44140625,\n 41.672911819602085\n ],\n [\n -83.07861328125,\n 41.902277040963696\n ],\n [\n -83.03466796874999,\n 42.374778361114195\n ],\n [\n -82.46337890625,\n 42.601619944327965\n ],\n [\n -82.1337890625,\n 43.51668853502909\n ],\n [\n -82.55126953124999,\n 45.398449976304086\n ],\n [\n -84.13330078125,\n 46.51351558059737\n ],\n [\n -88.26416015625,\n 48.31242790407178\n ],\n [\n -90.966796875,\n 48.25394114463431\n ],\n [\n -93.2080078125,\n 48.66194284607008\n ],\n [\n -94.63623046875,\n 48.73445537176822\n ],\n [\n -94.81201171875,\n 49.32512199104001\n ],\n [\n -95.1416015625,\n 49.410973199695846\n ],\n [\n -95.11962890625,\n 49.023461463214126\n ],\n [\n -97.294921875,\n 49.009050809382046\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65ddf4","contributors":{"authors":[{"text":"Newton, John G.","contributorId":22323,"corporation":false,"usgs":true,"family":"Newton","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14949,"text":"ofr87735 - 1987 - Missouri ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr87735","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-735","title":"Missouri ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87735","usgsCitation":"Mesko, T.O., and Berkas, W., 1987, Missouri ground-water quality: U.S. Geological Survey Open-File Report 87-735, iv, 9 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87735.","productDescription":"iv, 9 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0735/report-thumb.jpg"},{"id":43765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0735/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699acc","contributors":{"authors":[{"text":"Mesko, T. O.","contributorId":83934,"corporation":false,"usgs":true,"family":"Mesko","given":"T.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":170302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":170301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14753,"text":"ofr87571 - 1987 - Regional study of the Castle Hayne Aquifer of eastern North Carolina","interactions":[],"lastModifiedDate":"2016-12-15T13:20:46","indexId":"ofr87571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-571","title":"Regional study of the Castle Hayne Aquifer of eastern North Carolina","docAbstract":"The Castle Hayne aquifer is an eastward sloping and thickening wedge of limestone and sandstone, located in a 12,500 sq mi area in the eastern part of North Carolina. The Castle Hayne aquifer is the major source of freshwater for much of coastal North Carolina where the aquifers underlying the Castle Hayne contain saltwater. A regional study of the Castle Hayne aquifer was conducted to provide definitive information on the declines in water levels and of saltwater intrusion in the area. A series of geohydrologic maps produced from the study, show the altitude of the top of the aquifer, location of saltwater in the aquifer, aquifer thickness, aquifer transmissivity, and confining-unit thickness. The history of groundwater pumpage can be compared with historical water levels in the aquifer. These geohydrologic, pumpage, and water level data can be used to develop estimates of aquifer and confining-unit hydraulic coefficients and to develop a groundwater flow model for the Castle Hayne aquifer. The model will increase the understanding of the groundwater flow system and also can be used to assess various groundwater development scenarios for the entire Castle Hayne aquifer.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87571","usgsCitation":"Lyke, W., and Coble, R.W., 1987, Regional study of the Castle Hayne Aquifer of eastern North Carolina: U.S. Geological Survey Open-File Report 87-571, 2 p. :maps ;28 cm., https://doi.org/10.3133/ofr87571.","productDescription":"2 p. :maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":43523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0571/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Castle Hayne Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.03564453124999,\n 33.65120829920497\n ],\n [\n -79.03564453124999,\n 36.633162095586556\n ],\n [\n -74.66308593749999,\n 36.633162095586556\n ],\n [\n -74.66308593749999,\n 33.65120829920497\n ],\n [\n -79.03564453124999,\n 33.65120829920497\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c447","contributors":{"authors":[{"text":"Lyke, W.L.","contributorId":75551,"corporation":false,"usgs":true,"family":"Lyke","given":"W.L.","affiliations":[],"preferred":false,"id":169950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coble, R. W.","contributorId":49380,"corporation":false,"usgs":true,"family":"Coble","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":40036,"text":"ofr85648E - 1987 - Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada","interactions":[],"lastModifiedDate":"2022-10-17T15:26:53.171278","indexId":"ofr85648E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-648","chapter":"E","title":"Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada","docAbstract":"Water quality data for groundwater were compiled for the McDermitt 1° x 2° quadrangle which covers a portion of northern Nevada. Chemical characteristics of the water are shown on a map (at a scale of 1:250,000) and on trilinear diagrams for the major ions. The data for the area are also presented in a table.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85648E","usgsCitation":"Welch, A., and Williams, R.P., 1987, Data on ground-water quality for the McDermitt 1° x 2° quadrangle, northern Nevada: U.S. Geological Survey Open-File Report 85-648, 2 Plates: 40.17 × 24.24 inches and 33.25 × 19.82 inches, https://doi.org/10.3133/ofr85648E.","productDescription":"2 Plates: 40.17 × 24.24 inches and 33.25 × 19.82 inches","costCenters":[],"links":[{"id":165427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":67962,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67963,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0648e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392477,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16875.htm"}],"country":"United States","state":"Nevada","otherGeospatial":"McDermitt 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118,\n 41\n ],\n [\n -116,\n 41\n ],\n [\n -116,\n 42\n ],\n [\n -118,\n 42\n ],\n [\n -118,\n 41\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae409","contributors":{"authors":[{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":222898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Rhea P.","contributorId":87114,"corporation":false,"usgs":true,"family":"Williams","given":"Rhea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222899,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57338,"text":"wdrWI861 - 1987 - Water Resources Data for Wisconsin, Water Year 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"wdrWI861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-86-1","title":"Water Resources Data for Wisconsin, Water Year 1986","language":"ENGLISH","doi":"10.3133/wdrWI861","usgsCitation":"Holmstrom, B.K., Kammerer, P., and Erickson, R., 1987, Water Resources Data for Wisconsin, Water Year 1986: U.S. Geological Survey Water Data Report WI-86-1, 402 p., https://doi.org/10.3133/wdrWI861.","productDescription":"402 p.","numberOfPages":"402","costCenters":[],"links":[{"id":185145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1986/wi-86-1/report-thumb.jpg"},{"id":88260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1986/wi-86-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7d7","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":256750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammerer, P.A.","contributorId":21943,"corporation":false,"usgs":true,"family":"Kammerer","given":"P.A.","affiliations":[],"preferred":false,"id":256749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erickson, R.M.","contributorId":105789,"corporation":false,"usgs":true,"family":"Erickson","given":"R.M.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":256751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":14479,"text":"ofr87713 - 1987 - Arizona ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr87713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-713","title":"Arizona ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87713","usgsCitation":"Kister, L., Radtke, D.B., and Graf, C., 1987, Arizona ground-water quality: U.S. Geological Survey Open-File Report 87-713, iv, 8 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr87713.","productDescription":"iv, 8 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0713/report-thumb.jpg"},{"id":43173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672ebb","contributors":{"authors":[{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":169523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, D. B.","contributorId":72821,"corporation":false,"usgs":true,"family":"Radtke","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graf, Charles","contributorId":6711,"corporation":false,"usgs":true,"family":"Graf","given":"Charles","email":"","affiliations":[],"preferred":false,"id":169522,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","interactions":[{"subject":{"id":14775,"text":"ofr86532 - 1987 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"ofr86532","publicationYear":"1987","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"predicate":"SUPERSEDED_BY","object":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"chapter":"A","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"id":1}],"supersededBy":{"id":2191,"text":"wsp2336A - 1988 - Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","indexId":"wsp2336A","publicationYear":"1988","noYear":false,"title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts"},"lastModifiedDate":"2020-05-13T16:47:03.039489","indexId":"ofr86532","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-532","title":"Simulation of flow in the Edwards Aquifer, San Antonio region, Texas, and refinement of storage and flow concepts","docAbstract":"The Edwards aquifer is a complexly faulted, carbonate aquifer lying within the Balcones fault zone of south-central Texas. The aquifer is recharged mainly by streamflow losses in the outcrop area of the Edwards aquifer and is discharged by major springs located at considerable distances, as much as 150 mi, from the areas of recharge, and by wells. Groundwater flow within the Edwards aquifer of the San Antonio region was simulated to investigate concepts relating to the storage and flow characteristics. A general purpose, finite difference model, modified to provide the capability of representing barrier faults, was used to simulate groundwater flow and storage in the aquifer. The simulations investigated the effects of complex geologic structures and significant changes in transmissivity, anisotropy, and storage coefficient, with initial values based on concepts developed in previous studies. Results of the simulations confirmed the original estimates of transmissivity values (> 100 sq ft/sec) in the confined zone of the aquifer between San Antonio and Comal Springs. A storage coefficient of 0.05 in the unconfined zone of the aquifer produced the best simulation of water levels and springflow. A major interpretation resulting from the simulations is that two essentially independent areas of regional flow were identified in the west and central part of the study area. Flow from the two areas converges at Comal Springs. The directions of computed flux vectors reflected the presence of major barrier faults which locally deflect patterns of groundwater movement. The most noticeable deflection is the convergence of flow through the geologic structural opening, the Knippa gap, in eastern Uvalde County. A second significant interpretation is that groundwater flow in northeastern Bexar, Comal, and Hays Counties is diverted by barrier faults toward San Marcos Springs, a regional discharge point. (Lantz-PTT)
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9739","contributors":{"compilers":[{"text":"Mitchell, Alicia A.","contributorId":97897,"corporation":false,"usgs":true,"family":"Mitchell","given":"Alicia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645314,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":18670,"text":"ofr87220 - 1987 - Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California","interactions":[{"subject":{"id":18670,"text":"ofr87220 - 1987 - Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California","indexId":"ofr87220","publicationYear":"1987","noYear":false,"title":"Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":70014717,"text":"70014717 - 1988 - Processes affecting the distribution of selenium in shallow groundwater of agricultural areas, western San Joaquin Valley, California","indexId":"70014717","publicationYear":"1988","noYear":false,"title":"Processes affecting the distribution of selenium in shallow groundwater of agricultural areas, western San Joaquin Valley, California"},"id":1}],"supersededBy":{"id":70014717,"text":"70014717 - 1988 - Processes affecting the distribution of selenium in shallow groundwater of agricultural areas, western San Joaquin Valley, California","indexId":"70014717","publicationYear":"1988","noYear":false,"title":"Processes affecting the distribution of selenium in shallow groundwater of agricultural areas, western San Joaquin Valley, California"},"lastModifiedDate":"2018-11-19T12:22:18","indexId":"ofr87220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-220","title":"Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California","docAbstract":"A study was undertaken to evaluate the processes affecting the chemistry of shallow ground water associated with agricultural drainage systems in the western San Joaquin Valley, California. The study was prompted by a need for an understanding of selenium mobility in areas having high selenium concentrations in shallow ground water. Groundwater samples were collected along transects in three artificially drained fields where the age of the drainage system varied (15, 6, and 1.5 years). Selenium concentrations in the drainage water also varied (0F30, 58, and 3700 micrograms per liter, respectively). Isotopic enrichment and chemical composition of the ground-water samples indicate that saline- and selenium-enriched water has evolved as a result of evaporation of ground water. This evaporated, isotopically enriched water is being displaced by more recent, less saline irrigation water percolating through the root zone. This displace-ment seems to be a process whereby sodium chloride and sodium sulfate water is being replaced by more dilute calcium sulfate and calcium bicarbonate water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87220","usgsCitation":"Deverel, S.J., and Fujii, R., 1987, Processes affecting the distribution of selenium in shallow ground water of agricultural areas, western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 87-220, iv, 14 p., https://doi.org/10.3133/ofr87220.","productDescription":"iv, 14 p.","costCenters":[],"links":[{"id":151901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0220/report-thumb.jpg"},{"id":359563,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db654980","contributors":{"authors":[{"text":"Deverel, S. J.","contributorId":65478,"corporation":false,"usgs":true,"family":"Deverel","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fujii, Roger rfujii@usgs.gov","contributorId":553,"corporation":false,"usgs":true,"family":"Fujii","given":"Roger","email":"rfujii@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":179533,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12109,"text":"ofr8741 - 1987 - Hydrologic hazards along Squaw Creek from a hypothetical failure of the glacial moraine impounding Carver Lake near Sisters, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T09:33:17","indexId":"ofr8741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-41","title":"Hydrologic hazards along Squaw Creek from a hypothetical failure of the glacial moraine impounding Carver Lake near Sisters, Oregon","docAbstract":"A hydrologic hazard exists that could create a large-magnitude, but short-duration, flood in the Squaw Creek drainage and inundate areas in and around the community of Sisters, Oregon. There is a 1 to 5% probability that Carver Lake, located at elevation 7,800 ft above sea level on the east slope of South Sister mountain, Oregon, could catastrophically empty. At the U.S. Geological Survey gage (14075000) on Squaw Creek between Carver Lake and Sisters, the magnitude of the breakout flood would be 10 times that of a 1% probability meteorological flood. In Sisters, the magnitude of the breakout flood would be about five times that of a 1% probability meteorological flood. Several conditions at Carver Lake indicate the potential hazard: (1) The lake is very deep for its size; the lake contains 740 acre-ft of water and is more than 100 ft deep; (2) There is a probability that a large magnitude avalanche and consequent overtopping of the lake could occur. There are steep slopes of unstable volcanic rock and an extensively cravassed glacier located above the lake; (3) The moraine dam confining the lake is steep-faced, rendering the dam unstable, and unvegetated making it highly erodible; (4) Large amounts of readily erodible material available for transport would increase the magnitude of a large flood and keep the flood from attenuating in the steep reaches of the Squaw Creek channel; (5) and, Geologically, there is a greater than normal possibility for the area to become seismically active. Earthquakes could cause rock and ice to fall into the lake. A one-dimensional unsteady-state streamflow model was used to route a hypothetical flood down the Squaw Creek drainage. This scenario creates a starting hydrograph with a peak of 180,000 cu ft/sec. The ensuing hypothetical flood would incorporate readily erodible debris and sediments in the steep canyons, increasing the total volume of the flood by a factor of two. As the peak emerges from the steeper slopes into a more gently sloping valley 8 miles from the lake, the peak would attenuate to 47,000 cu ft/sec. At the Geological Survey gage at river mile 26.6, the peak would attenuate to 21,000 cu ft/sec. In Sisters on the alluvial fan, at about 20 miles downstream from the lake, the peak would continue to attenuate to 9,800 cu ft/sec. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8741","usgsCitation":"Laenen, A., Scott, K.M., Costa, J.E., and Orzol, L., 1987, Hydrologic hazards along Squaw Creek from a hypothetical failure of the glacial moraine impounding Carver Lake near Sisters, Oregon: U.S. Geological Survey Open-File Report 87-41, viii, 48 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8741.","productDescription":"viii, 48 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":40141,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0041/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60566b","contributors":{"authors":[{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":165109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, K. M.","contributorId":8119,"corporation":false,"usgs":true,"family":"Scott","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":165106,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Costa, J. E.","contributorId":28977,"corporation":false,"usgs":true,"family":"Costa","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":165107,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Orzol, L.L.","contributorId":63419,"corporation":false,"usgs":true,"family":"Orzol","given":"L.L.","affiliations":[],"preferred":false,"id":165108,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":14542,"text":"ofr87471 - 1987 - Prediction of the effects of mine dewatering on four lakes near Crandon, Wisconsin, by use of a water-budget model","interactions":[],"lastModifiedDate":"2022-08-04T21:35:07.28172","indexId":"ofr87471","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-471","title":"Prediction of the effects of mine dewatering on four lakes near Crandon, Wisconsin, by use of a water-budget model","docAbstract":"The effects of dewatering a proposed zinc and copper mine on water levels of four lakes near Crandon, Wisconsin, were predicted by use of a digital water-budget model of the lakes.
\nThe average lake-stage reduction predicted by the model for expected ground-water levels after mine dewatering ranged from 0.21 feet for Duck Lake to 6.9 feet for Little Sand Lake. These stage reductions assume that no water is pumped into the lakes and that no changes are made to the outlet structures. The predicted flow augmentation to the lakes to offset lowering of ground-water levels by mine dewatering range from 8 gallons per minute for Duck Lake to 580 gallons per minute for Little Sand Lake.
\nBecause of uncertainty in variables used in the model and in the data used to calibrate the model, the predictions of the model are subject to an undetermined degree of uncertainty.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87471","collaboration":"Prepared in cooperation with Wisconsin Department of Natural Resources","usgsCitation":"Krug, W.R., Ostenso, N.A., and Krohelski, J.T., 1987, Prediction of the effects of mine dewatering on four lakes near Crandon, Wisconsin, by use of a water-budget model: U.S. Geological Survey Open-File Report 87-471, v, 63 p., https://doi.org/10.3133/ofr87471.","productDescription":"v, 63 p.","numberOfPages":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":404857,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17274.htm","linkFileType":{"id":5,"text":"html"}},{"id":146593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0471/report-thumb.jpg"},{"id":43220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0471/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","city":"Crandon","otherGeospatial":"Deephole Lake, Duck Lake, Little Sand Lake, Skunk Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.5001220703125,\n 45.27488643704891\n ],\n [\n -88.37127685546875,\n 45.27488643704891\n ],\n [\n -88.37127685546875,\n 45.744526980468436\n ],\n [\n -89.5001220703125,\n 45.744526980468436\n ],\n [\n -89.5001220703125,\n 45.27488643704891\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8b4","contributors":{"authors":[{"text":"Krug, William R.","contributorId":53381,"corporation":false,"usgs":true,"family":"Krug","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":169617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ostenso, Nile A.","contributorId":59811,"corporation":false,"usgs":true,"family":"Ostenso","given":"Nile","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krohelski, J. T.","contributorId":59046,"corporation":false,"usgs":true,"family":"Krohelski","given":"J.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":169618,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":18440,"text":"ofr88185 - 1987 - Water resources activities, Georgia district, 1987","interactions":[],"lastModifiedDate":"2019-11-27T10:04:05","indexId":"ofr88185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"88-185","title":"Water resources activities, Georgia district, 1987","docAbstract":"No abstract available.
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1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr87692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-692","title":"Preliminary water-use estimates in the United States in 1985","docAbstract":"Preliminary 1985 water use estimates are tabulated by State for the Und States, Puerto Rico, the Virgin Islands, and the District of Columbia. Preliminary estimates of water withdrawn from surface water and groundwater sources for offstream water use categories are presented prior to publication of the final estimates in a U.S. Geological Survey Circular to allow for the timely release of the estimates to the general public. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87692","usgsCitation":"Solley, W., Pierce, R., and Merk, C., 1987, Preliminary water-use estimates in the United States in 1985: U.S. Geological Survey Open-File Report 87-692, 5 p. ;28 cm., https://doi.org/10.3133/ofr87692.","productDescription":"5 p. ;28 cm.","costCenters":[],"links":[{"id":150347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0692/report-thumb.jpg"},{"id":44999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e66e","contributors":{"authors":[{"text":"Solley, W.B.","contributorId":25960,"corporation":false,"usgs":true,"family":"Solley","given":"W.B.","affiliations":[],"preferred":false,"id":172179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, R.R.","contributorId":52201,"corporation":false,"usgs":true,"family":"Pierce","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":172180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Merk, C.F.","contributorId":67517,"corporation":false,"usgs":true,"family":"Merk","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":172181,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19115,"text":"ofr87224 - 1987 - Hydrologic data for urban studies in the Austin metropolitan area, Texas, 1985","interactions":[],"lastModifiedDate":"2017-06-14T10:55:22","indexId":"ofr87224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-224","title":"Hydrologic data for urban studies in the Austin metropolitan area, Texas, 1985","docAbstract":"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.
\nThe 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 Balcones Fault Zone.
\nThe objectives of the Austin urban hydrology study are as follows:
\nThis report presents the basic hydrologic data collected in the Austin urban area for the 1985 water year (Oct. 1, 1984 to Sept. 30, 1985). 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-85-3, 1985.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr87224","collaboration":"Prepared in cooperation with the City of Austin","usgsCitation":"Gordon, J., Pate, D., and Dorsey, M., 1987, Hydrologic data for urban studies in the Austin metropolitan area, Texas, 1985: U.S. Geological Survey Open-File Report 87-224, vi, 170 p., https://doi.org/10.3133/ofr87224.","productDescription":"vi, 170 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":150696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0224/report-thumb.jpg"},{"id":48578,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0224/report.pdf","text":"Report","size":"2.50 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","county":"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":"4f4e4a1ce4b07f02db6080d5","contributors":{"authors":[{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":180329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pate, D.L.","contributorId":87145,"corporation":false,"usgs":true,"family":"Pate","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":180331,"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":180330,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19117,"text":"ofr87393 - 1987 - Statistical, graphical, and trend summaries of selected water-quality and streamflow data from the Trinity River near Crockett, Texas, 1964-85","interactions":[],"lastModifiedDate":"2016-08-12T15:04:44","indexId":"ofr87393","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-393","title":"Statistical, graphical, and trend summaries of selected water-quality and streamflow data from the Trinity River near Crockett, Texas, 1964-85","docAbstract":"Statistical and graphical -.summaries of selected water-quality and'\" streamflow data collected between 1964 and 1985 at the Trinity River near\" Crockett are presented to document the baseline water quality of the Trinity River at this location. Dissolved oxygen exceeded 7.0 milligrams per liter in more than 50 percent- of the samples analyzed. The mean value of pH'was 7.4 units; the mean values of specific conductance and temperature were 619 microseimens per centimeter at 25 degrees Celsius and 20.5 degrees Celsius, respectively.
\nAs part of the statistical summaries, trend tests were conducted. Several small uptrends were detected for total nitrogen, total organic nitrogen, total ammonia nitrogen, total nitrite nitrogen, total nitrate nitrogen, total organic plus ammonia nitrogen, total nitrite plus nitrate nitrogen, and total phosphorus. Small downtrends were detected for biochemical oxygen demand and dissolved magnesium.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87393","usgsCitation":"Goss, R.L., 1987, Statistical, graphical, and trend summaries of selected water-quality and streamflow data from the Trinity River near Crockett, Texas, 1964-85: U.S. Geological Survey Open-File Report 87-393, vi, 21 p., https://doi.org/10.3133/ofr87393.","productDescription":"vi, 21 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":48580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0393/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0393/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1e69","contributors":{"authors":[{"text":"Goss, Richard L.","contributorId":50178,"corporation":false,"usgs":true,"family":"Goss","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":180333,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}