A rapid procedure suitable for the routine determination of 1–10 ng of bismuth in a silicate rock matrix is described. Results for the U.S. Geological Survey standard rocks are presented. Rocks and minerals are dissolved in hydrofluoric-perchloric acid in the presence of 207Bi tracer and the silica is removed by evaporation. The perchloric acid residue is taken up in water and bismuth iodide is extracted into methyl isobutyl ketone. After three acid-iodide washes, the bismuth is stripped into water and reacted with a substoichiometric amount of EDTA. Excess of bismuth is extracted as the iodide and the specific activity of the bismuth-EDTA complex is determined.
Chemical composition of water samples, temperature of inflow water, and theoretical calculations were compared to evaluate the water-contributing intervals to the zone to be mined--1,782.8 to 1,798.6 meters (5,849 to 5,901 feet)--in hole UA-1, Amchitka Island, Alaska. Chemical composition and temperature of inflow water indicated the contributing zones to have a mean depth of 1,670 meters {5,478 feet) and 1,726.7 meters (5,665 feet), respectively. An unrestricted inflow rate based on this data was calculated to be 380 cubic meters per day (70 gallons per minute) which compared well with the measured restricted-inflow rate of 164 cubic meters per day (30 gallons per minute) for hole UA-1 at the end of November 1970.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70156965","usgsCitation":"Ballance, W.C., and Beetem, W., 1972, Water inflow into hole UA-1, Amchitka Island, Alaska, ii, 31 p., https://doi.org/10.3133/70156965.","productDescription":"ii, 31 p.","numberOfPages":"36","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr474456.JPG"},{"id":308583,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156965/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 178.584136963,\n 51.63677159243599\n ],\n [\n 178.592376709,\n 51.61290019118336\n ],\n [\n 179.21585083,\n 51.3254629443313\n ],\n [\n 179.508361816,\n 51.37520943448463\n ],\n [\n 179.057922363,\n 51.587309751245456\n ],\n [\n 178.628082275,\n 51.67936786087718\n ],\n [\n 178.584136963,\n 51.63677159243599\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efcde4b05d6c4e4fa9a9","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beetem, W.A.","contributorId":19173,"corporation":false,"usgs":true,"family":"Beetem","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":571260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70156962,"text":"70156962 - 1972 - Hydraulic tests in hole UAe-6h, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2019-11-13T15:00:13","indexId":"70156962","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Hydraulic tests in hole UAe-6h, Amchitka Island, Alaska","docAbstract":"Inflatable straddle packers were used to isolate and test 14 intervals ranging from 39 to 258 meters (127 to 846 feet) each in hole UAe-6h. Packer seats were poor in part of the hole because of unstable wall conditions. Thus, some zones had to be tested several times. The static water levels in the intervals tested ranged from about 23 meters (71 feet) below land surface in the upper interval to an estimated 90 meters (295 feet) below land surface in the lower intervals, indicating a decreasing head with depth. The specific capacity of the hole from 85. 0 to 2,133. 6 meters (279 to 7,000 feet) was 1.94 cubic meters per day per meter (0. 11 gallon per minute per foot) of drawdown after the hole had been jetted at an average rate of 327 cubic meters per day (60 gallons per minute) for about 23 hours . Transmissivity computed from the recovery of water level after jetting stopped was 0.60 cubic meter per day per meter (48.3 gallons per day per foot). The relative specific capacities of isolated intervals ranged from 0.004 cubic meter per day per meter (less than 0.001 gallon per minute per foot) of drawdown to 0.430 cubic meter per day per meter (0.024 gallon per minute per foot) of drawdown.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70156962","usgsCitation":"Ballance, W.C., 1972, Hydraulic tests in hole UAe-6h, Amchitka Island, Alaska, iii, 31 p., https://doi.org/10.3133/70156962.","productDescription":"iii, 31 p.","numberOfPages":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156962.PNG"},{"id":308554,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156962/report.pdf","text":"Report","size":"7,712 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 178.584136963,\n 51.63677159243599\n ],\n [\n 178.592376709,\n 51.61290019118336\n ],\n [\n 179.21585083,\n 51.3254629443313\n ],\n [\n 179.508361816,\n 51.37520943448463\n ],\n [\n 179.057922363,\n 51.587309751245456\n ],\n [\n 178.628082275,\n 51.67936786087718\n ],\n [\n 178.584136963,\n 51.63677159243599\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efb9e4b05d6c4e4fa977","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571252,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000350,"text":"1000350 - 1972 - The future of salmonid communities in the Laurentian Great Lakes","interactions":[],"lastModifiedDate":"2016-03-14T13:25:25","indexId":"1000350","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"The future of salmonid communities in the Laurentian Great Lakes","docAbstract":"The effects of human population growth, industrialization, and the introduction of marine fishes have reduced the suitability of each of the Great Lakes for oligotrophic fish communities. The ultimate consequence has been a reduction of fishery productivity that has ranged from extreme in Lake Ontario to moderate in Lake Superior. If measures are not taken to alleviate the adverse effects of marine invaders and trends in environmental quality, a major reduction in fishery productivity can eventually be expected throughout the Great Lakes.Prospects for the next century will be improved if the lakes can be intensively managed. More stringent control of the sea lamprey (Petromyzon marinus), and subsequent reduction of the alewife (Alosa pseudoharengus), by the reestablishment of populations of large piscivores, should permit the recovery of some of the previous predator and prey species, or the development of populations of new species that are more compatible with a reduced number of lampreys. Even if marine species can be reduced greatly, the full restoration of the former fishery productivity remains uncertain and will require a high degree of coordination among all management and research agencies that have responsibilities on the Great Lakes.Unfavorable trends toward progressive degradation of water quality pose the greatest threat to restoration of the fishery resources of the Great Lakes. Where changes in water quality have been the greatest, oligotrophic species have become scarce or absent, and in the deepwater regions no other species have reoccupied the vacated niches.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f72-138","usgsCitation":"Smith, S.H., 1972, The future of salmonid communities in the Laurentian Great Lakes: Journal of the Fisheries Research Board of Canada, v. 29, no. 6, p. 951-957, https://doi.org/10.1139/f72-138.","productDescription":"7 p.","startPage":"951","endPage":"957","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da4c","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308437,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000187,"text":"1000187 - 1972 - Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide","interactions":[],"lastModifiedDate":"2025-03-04T16:45:25.143844","indexId":"1000187","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide","docAbstract":"After the Pere Marquette River was treated with a lampricide in May 1964, the number of recently transformed sea lampreys (Petromyzon marinus) collected in the water-intake structure of a chemical plant near the mouth of the stream dropped 99.5%, from 13,913 (average for 1962-63 and 1963-64) to 76 (average for the next four migration seasons). Average length of the lampreys caught increased markedly after the treatment. In five of the six migration seasons, the catch of downstream migrants was higher in the fall than in the spring.","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f72-186","usgsCitation":"Hodges, J.W., 1972, Downstream migration of recently transformed sea lampreys before and after treatment of a Lake Michigan tributary with a lampricide: Journal of the Fisheries Research Board of Canada, v. 29, no. 8, p. 1237-1240, https://doi.org/10.1139/f72-186.","productDescription":"4 p.","startPage":"1237","endPage":"1240","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129283,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635fbf","contributors":{"authors":[{"text":"Hodges, John W.","contributorId":58593,"corporation":false,"usgs":true,"family":"Hodges","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":308206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175672,"text":"70175672 - 1972 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","interactions":[],"lastModifiedDate":"2016-08-17T16:02:33","indexId":"70175672","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"29","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1972, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971: Edwards Underground Water District Bulletin 29, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad1e4b03bcb0104bbca","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":645992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009762,"text":"70009762 - 1972 - Microcoulometric measurement of water in minerals","interactions":[],"lastModifiedDate":"2020-12-23T21:46:03.156376","indexId":"70009762","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Microcoulometric measurement of water in minerals","docAbstract":"A DuPont Moisture Analyzer is used in a microcoulometric method for determining water in minerals. Certain modifications, which include the heating of the sample outside the instrument, protect the system from acid gases and insure the conversion of all hydrogen to water vapor. Moisture analyzer data are compared to concurrent data obtained by a modified Penfield method. In general, there is a positive bias of from 0.1 to 0.2% in the moisture analyzer results and a similarity of bias in minerals of the same kind. Inhomogeneity, sample size, and moisture pick-up are invoked to explain deviations. The method is particularly applicable to small samples.
Water resources data collected in the Pacific Northwest during the 1972 water year include chemical and physical characteristics of surface water. Data included in this report were collected by the Water Resources Division of the U.S. Geological Survey under the direction of the following district chiefs: H.K. Hall, Idaho; George M. Pike, Montana; S.F. Kapustka, Oregon; and L.B. Laird, Washington.
The Geological Survey has published records of chemical quality, water temperatures, and sediment since 1941 in an annual series of water-supply papers entitled \"Quality of Surface Waters of the United States.\" Beginning with the 1964 water year, water-quality records have been published by the Geological Survey in annual reports on a State-boundary basis. These reports are available from the district offices.
This report is for limited distribution and is intended primarily for rapid release of selected data shortly after the end of the water year. Data contained herein is provisional and subject to revision before final publication in the foregoing reports. The following pages contain listings of selected constituents and their values sampled at 34 selected sites in the'Pacific Northwest. The sites are listed in downstream order by states. The constituent values recorded in the tables are the results of laboratory determinations except for water temperature, Ph, Dissolved Oxygen, Specific Conductance, Alkalinity, and Immediate Coliform count, which are the results of field determinations.
These data were collected and analyzed by the Geological Survey under cooperative programs with Environmental Protection Agency and other Federal, State, County, and municipal organizations as identified in the annual State-wide reports. Additional water-quality data may be obtained from district offices of the Geological Survey and from Environmental Protection Agency.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/70176806","usgsCitation":"U.S. Geological Survey Northwest Water Resources Data Center, 1972, Annual summary of water quality data for selected sites in the Pacific Northwest, October 1971 to September 1972, 35 p., https://doi.org/10.3133/70176806.","productDescription":"35 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":329383,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70176806.jpg"},{"id":330317,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70176806/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Montana, Oregon, Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.8486328125,\n 41.16211393939692\n ],\n [\n -124.8486328125,\n 49.009050809382046\n ],\n [\n -110.32470703125,\n 49.009050809382046\n ],\n [\n -110.32470703125,\n 41.16211393939692\n ],\n [\n -124.8486328125,\n 41.16211393939692\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57f7c08be4b0bc0bec09c7ed","contributors":{"authors":[{"text":"U.S. Geological Survey Northwest Water Resources Data Center","contributorId":175193,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey Northwest Water Resources Data Center","id":650384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48075,"text":"ofr72348 - 1972 - Water-resources reconnaissance of Anaktuvuk Pass, Alaska","interactions":[],"lastModifiedDate":"2023-08-29T20:48:49.921019","indexId":"ofr72348","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-348","title":"Water-resources reconnaissance of Anaktuvuk Pass, Alaska","docAbstract":"A hydrologic reconnaissance was made of Anaktuvuk pass in the central Brooks Range during the summer of 1971 to help develop a water supply for the village school. Winter icings and summer flow conditions in Contact Creek both indicate that ground water is present beneath the creek bed. A well-site area was selected in the channel of Contact Creek near the school where the prospects of obtaining a suitable ground-water supply seem best. In the event that wells are unsuccessful, water can be hauled from Eleanor Lake to the school. Chemical quality of water at Anaktuvuk Pass is excellent, but any source of water may be subject to bacterial contamination and would require treatment.
No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Reeves, R., Rawson, J., and Blakey, J., 1972, Chemical and bacteriological quality of water at selected sites in the San Antonio area, Texas, August 1968-April 1972, 69 p.","productDescription":"69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c6aecfe4b0f2f0cebe43f0","contributors":{"authors":[{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":646940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rawson, Jack","contributorId":18345,"corporation":false,"usgs":true,"family":"Rawson","given":"Jack","affiliations":[],"preferred":false,"id":646941,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blakey, J.F.","contributorId":23969,"corporation":false,"usgs":true,"family":"Blakey","given":"J.F.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":646942,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70048669,"text":"70048669 - 1972 - Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California","interactions":[],"lastModifiedDate":"2013-11-22T09:41:28","indexId":"70048669","displayToPublicDate":"1969-10-29T09:24:00","publicationYear":"1972","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}},"title":"Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California","docAbstract":"This study evaluates the adequacy of a 39-mile reach of the Mokelumne River in San Joaquin and Sacramento Counties, California, to carry planned flood releases between Camanche Reservoir and the Bensons Ferry Bridge near Thornton. The flood releases from Camanche Reservoir are to be restricted, insofar as possible, so that the flows in the Mokelumne River will not exceed 5,000 cfs (cubic feet per second) as measured at the gaging station below Camanche Dam.
\nAreas of inundation and computed floodwater profiles are based on channel conditions in late 1970 and on observed water-surface profiles during flood releases of about 5,000 cfs in January 1969 and January 1970. The inundated area shown on the maps (appendix A) and the water-surface elevations indicated on the cross sections (appendix G) are for the flood releases of those dates.
\nThe following conclusions are contingent on there being no levee failures during periods of high flow and no significant channel changes since the flood release of January 1970.
\n1. High tides in San Francisco Bay and, to a greater degree, flood stages on the Cosumnes River, cause backwater in the study reach. Severe backwater conditions occurring simultaneously with a flow of 5,000 cfs in the Mokelumne River can increase the flood stage 4 to 6 feet at Bensons Ferry Bridge (cross section 1). Backwater effects decrease in an upstream direction and are less than 0.5 foot at cross section 35, a river distance of 8.6 miles upstream from cross section 1, and 1.5 miles downstream from the Peltier Road bridge.
\n2. In the reach between cross sections 1 and 35, a 5,000 cfs release from Camanche Reservoir with maximum backwater effect (measured at cross section 1 at the mouth of the Cosumnes River) is confined within the natural or leveed banks except on the right bank flood plain between cross sections 12 and 19.
\n3. Upstream from cross section 35, there is overbank flooding at a flow of 5,000 cfs between cross sections 48 and 51, and 62 and 67.5. An increase in flow from 5,000 to 6,000 cfs will cause flooding between cross sections 43 and 47, 52 and 56, and 73 and 85.
\n4. A discharge of 5,000 cfs will pass through all bridge openings in the study reach except that of the Western Pacific Railroad Co. bridge at cross section 4. If large amounts of debris lodge on the railroad bridge when backwater from the Cosumnes River occurs, the debris could cause higher stages and flooding along the right bank between cross sections 5 and 12.
","language":"English","publisher":"U.S. Geological Survey Water Resources Division","publisherLocation":"Menlo Park, CA","doi":"10.3133/70048669","collaboration":"Prepared in cooperation with The Reclamation Board, State of California","usgsCitation":"Simpson, R., 1972, Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California: U.S. Geological Survey Open-File Report, iv, 64 p., https://doi.org/10.3133/70048669.","productDescription":"iv, 64 p.","numberOfPages":"68","costCenters":[],"links":[{"id":278502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70048669.jpg"},{"id":279571,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70048669/report.pdf"}],"scale":"500000","country":"United States","state":"California","county":"Sacramento County;San Joaquin County","otherGeospatial":"Camanche Reservoir;Mokelumne River","geographicExtents":"{ \"type\": 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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":210377,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":808226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180008,"text":"70180008 - 1971 - Developing a state water plan: Ground-water conditions in Utah, spring of 1971","interactions":[],"lastModifiedDate":"2017-01-23T11:34:17","indexId":"70180008","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1971","docAbstract":"This report is the eighth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.
This report, like the others (see references, p. 21), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table configuration is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1970. Water-level fluctuations, however, are described for the period spring 1970 to spring 1971. Many of the data used in the report were collected by the Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Cordova, R., Bjorklund, L., McGreevy, L.J., Bolke, E., Sumison, C., Herbert, L.R., Butler, R., Mower, R.W., Sandberg, G.W., and Adams, D.B., 1971, Developing a state water plan: Ground-water conditions in Utah, spring of 1971: Cooperative Investigations Report 9, viii, 72 p.","productDescription":"viii, 72 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333680,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333679,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-194"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a13e4b0cad700058b63","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":659725,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659726,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659727,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659728,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659729,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659730,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659731,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Adams, D. B.","contributorId":59030,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":659732,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70179729,"text":"70179729 - 1971 - Nonthermal springs of Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:22:18","indexId":"70179729","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"16","title":"Nonthermal springs of Utah","docAbstract":"Data are presented for about 4,500 nonthermal springs that discharge in the State of Utah. Most major springs having discharge of several cubic feet per second or more are in or near mountain ranges or plateaus where precipitation is much greater than in other parts of the State. The largest instantaneous discharge observed at any spring was 314 cfs at Mammoth Spring in southwestern Utah. Discharges exceeding 200 cfs have been observed at Swan Creek Spring in extreme northern Utah, and discharges of 200 cfs have been reported for Big Brush Creek Spring in northeastern Utah. Maximum discharges generally are during or within a few weeks after the main period of snowmelt, which is usually from late April to the middle of June.
The largest springs generally discharge form or very near carbonate rocks in which solution channels and fractures are numerous or from areas of porous or fractured volcanic rocks. Most nonthermal springs in Utah probably are variable springs – that is, their variability of discharge exceeds 100 percent.
Most of the major springs discharge water that contains less than 500 ppm (parts per million) of dissolved solids, and most of the water is of the calcium bicarbonate type. Water from springs is used for domestic, municipal, irrigation, livestock, mining, and industrial purposes.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah Geological and Mineralogical Survey","usgsCitation":"Mundorff, J.C., 1971, Nonthermal springs of Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 16, iv, 70 p.","productDescription":"iv, 70 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333216,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333214,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-16.pdf"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ace4b0847d353f44c8","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178877,"text":"70178877 - 1971 - Hydrologic reconnaissance of Hansel Valley and northern Rozel Flat, Box Elder County, Utah","interactions":[],"lastModifiedDate":"2016-12-09T16:41:18","indexId":"70178877","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"33","title":"Hydrologic reconnaissance of Hansel Valley and northern Rozel Flat, Box Elder County, Utah","docAbstract":"This report is the ninth in a series by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, which describes the water resources of the western basins of Utah (see fig. 1). Its purpose is to present available hydrologic data for Hansel Valley, to provide an evaluation of the potential water-resource development of the valley, and to identify needed studies that would improve understanding of the valley's water supply. Hydrologic data from the northern part of adjacent Rozel Flat were collected to aid in evaluation of southern Hansel Valley, and these data also are included in this report.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Hood, J.W., 1971, Hydrologic reconnaissance of Hansel Valley and northern Rozel Flat, Box Elder County, Utah: Technical Publication 33, ii, 41 p.","productDescription":"ii, 41 p.","numberOfPages":"46","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331829,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-710"},{"id":331830,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008v.pdf"}],"country":"United States","state":"Utah","county":"Box Elder County","otherGeospatial":"Hansel Valley, Northern Rozel Flat","geographicExtents":" {\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.0438232421875,\n 41.42625319507269\n ],\n [\n -113.0438232421875,\n 41.99624282178583\n ],\n [\n -112.4945068359375,\n 41.99624282178583\n ],\n [\n -112.4945068359375,\n 41.42625319507269\n ],\n [\n -113.0438232421875,\n 41.42625319507269\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584bd0e2e4b077fc20250e2e","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178859,"text":"70178859 - 1971 - Water resources of Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2016-12-09T13:13:45","indexId":"70178859","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"31","title":"Water resources of Salt Lake County, Utah","docAbstract":"This report is the eighth in a series prepared by the U. S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, that describes the water resources of the western basins of Utah. (See fig. 1.) Its purpose is to present available hydrologic data on the Park Valley area, to provide an evaluation of the potential water-resource development of the area, and to identify needed studies that would improve understanding of the area's water supply.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Hely, A., Mower, R.W., Harr, C.A., and Arnow, T., 1971, Water resources of Salt Lake County, Utah: Technical Publication 31, xii, 240 p.","productDescription":"xii, 240 p.","numberOfPages":"258","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331795,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-670"},{"id":331796,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008t.pdf"}],"country":"United States","state":"Utah","county":"Salt Lake 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G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":655325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harr, C. Albert","contributorId":28978,"corporation":false,"usgs":true,"family":"Harr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":655327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":655328,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70178857,"text":"70178857 - 1971 - Hydrologic reconnaissance of the Park Valley area, Box Elder County, Utah","interactions":[],"lastModifiedDate":"2016-12-09T13:09:26","indexId":"70178857","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"30","title":"Hydrologic reconnaissance of the Park Valley area, Box Elder County, Utah","docAbstract":"This report is the eighth in a series prepared by the U. S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights, that describes the water resources of the western basins of Utah. (See fig. 1.) Its purpose is to present available hydrologic data on the Park Valley area, to provide an evaluation of the potential water-resource development of the area, and to identify needed studies that would improve understanding of the area's water supply.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Hood, J.W., 1971, Hydrologic reconnaissance of the Park Valley area, Box Elder County, Utah: Technical Publication 30, v, 51 p.","productDescription":"v, 51 p.","numberOfPages":"60","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331792,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-650"},{"id":331793,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008s.pdf"}],"country":"United States","state":"Utah","county":"Box Elder County","geographicExtents":" {\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.851318359375,\n 41.24064190269475\n ],\n [\n -113.851318359375,\n 41.902277040963696\n ],\n [\n -112.9669189453125,\n 41.902277040963696\n ],\n [\n -112.9669189453125,\n 41.24064190269475\n ],\n [\n -113.851318359375,\n 41.24064190269475\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584bd0e3e4b077fc20250e32","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178880,"text":"70178880 - 1971 - Ground-water resources of Cache Valley, Utah and Idaho","interactions":[],"lastModifiedDate":"2016-12-09T16:46:22","indexId":"70178880","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"36","title":"Ground-water resources of Cache Valley, Utah and Idaho","docAbstract":"This report is based on a study that was designed to provide information to enable the water managers and users in Cache Valley to develop, conserve, and administer their water resources. The report is primarily about the ground water in the valley, but it also includes a discussion of the relation of ground water to surface water and presents a general water-budget analysis for the valley. The report discusses the effects of climate, geology, and development on the source, occurrence, availability, quantity, movement, and chemical quality of the ground water. Most of the discussion pertains to ground water in the Quaternary valley fill, the principal water-bearing unit in the area, but it also includes some information about ground water in other rocks within the Cache Valley drainage basin.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Bjorklund, L., and McGreevy, L.J., 1971, Ground-water resources of Cache Valley, Utah and Idaho: Technical Publication 36, iv, 72 p.","productDescription":"iv, 72 p.","numberOfPages":"85","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331838,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-770"},{"id":331839,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008y.pdf"},{"id":331840,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Cache Valley","geographicExtents":" {\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.74468994140625,\n 41.875696393231\n ],\n [\n -111.67327880859375,\n 42.0227732629691\n ],\n [\n -111.741943359375,\n 42.165439250064345\n ],\n [\n -111.7584228515625,\n 42.25088477477567\n ],\n [\n -111.895751953125,\n 42.28340504748081\n ],\n [\n -111.98089599609375,\n 42.34636533160187\n ],\n [\n -112.06329345703125,\n 42.370720143531976\n ],\n [\n -112.08251953125,\n 42.238685347536496\n ],\n [\n -112.05780029296875,\n 42.15322331239858\n ],\n [\n -112.1044921875,\n 42.08803181932636\n ],\n [\n -112.12921142578125,\n 42.00032514831621\n ],\n [\n -112.12371826171875,\n 41.920672548686824\n ],\n [\n -112.027587890625,\n 41.79384042311992\n ],\n [\n -112.027587890625,\n 41.71187978193456\n ],\n [\n -111.91497802734375,\n 41.53325414281322\n ],\n [\n -111.76391601562499,\n 41.422134246213616\n ],\n [\n -111.71722412109374,\n 41.6010669423553\n ],\n [\n -111.74468994140625,\n 41.69957665997156\n ],\n [\n -111.7144775390625,\n 41.78360106648078\n ],\n [\n -111.74468994140625,\n 41.875696393231\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584bd0e2e4b077fc20250e2c","contributors":{"authors":[{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":655419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":655420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047885,"text":"70047885 - 1971 - Ground-water resources: Cumberland County, New Jersey","interactions":[{"subject":{"id":56051,"text":"ofr70279 - 1970 - Ground-water resources, Cumberland County, New Jersey","indexId":"ofr70279","publicationYear":"1970","noYear":false,"title":"Ground-water resources, Cumberland County, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":70047885,"text":"70047885 - 1971 - Ground-water resources: Cumberland County, New Jersey","indexId":"70047885","publicationYear":"1971","noYear":false,"title":"Ground-water resources: Cumberland County, New Jersey"},"id":1}],"lastModifiedDate":"2022-12-05T23:34:59.353431","indexId":"70047885","displayToPublicDate":"2013-01-01T16:10:16","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":135,"text":"Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"34","title":"Ground-water resources: Cumberland County, New Jersey","docAbstract":"Cumberland County is located in the Atlantic Coastal Plain physiographic province along the northeastern shore of Delaware Bay in Southwestern New Jersey. An average annual hydrologic budget was computed for Cumberland County. Water gains are: precipitation, 1,050 mgd (million gallons per day); surface-water inflow, 142 mgd; ground-water inflow negligible. Water losses are: evapotranspiration, 685 mgd; surface-water outflow, 370 mgd; ground-water outflow, 137 mgd.
\nUnconsolidated and semiconsolidated Coastal Plain sediments, 2,500 to 4,500 feet thick, and ranging in age from Cretaceous to Holocene, consist of layers of clay, silt, sand and gravel. Aquifers composed mainly of sand and gravel occur in the Potomac Group and Raritan and Magothy Formations, the Wenonah Formation and Mount Laurel Sand, the Piney Point Formation, and the Kirkwood Formation and Cohansey Sand.
\nAquifers in the Potomac-Raritan-Magothy sequence contain saline water and are not currently utilized in Cumberland County. However, they may be utilized in the future for underground storage of fresh water, or possibly other uses when more is known about this aquifer system.
\nThe aquifer in the Wenonah Formation and Mount Laurel Sand is not presently utilized in Cumberland County. It is probably suitable for future development, however of wells yielding as much as 300 gpm (gallons per minute) of good quality water in the northern part of the county.
\nThe Piney Point Formation is tapped in Cumberland County by only a few wells; each of these generally yield less than 100 gpm. Additional small supplies can be developed from this aquifer. Water from this aquifer requires little or no treatment for domestic use.
\nTwo principal aquifers occur in the Kirkwood Formation and Cohansey Sand: (1) the lower Kirkwood aquifer and (2) the Cohansey-Kirkwood aquifer. Most wells tapping the lower Kirkwood aquifer yield less than 50 gpm but are capable of yielding as much as 400 gpm. Wells in the lower Kirkwood range in depth from 200 to 370 feet. The Cohansey-Kirkwood aquifer is the shallowest and most important source of ground-water in the county but is highly susceptible to surface contamination. This aquifer is highly permeable; analysis of data from two pumping tests indicates permeabilities of 1,200 and 2,700 gpm per square foot. It generally yields large supplies of water (300 to 1,200 gpm) to wells from depths of less than 180 feet. Water in the Cohansey-Kirkwood aquifer is characterized by 1mv dissolved-solids content (63 mg/l, median), low hardness (21 mg/l, median), and low pH values (5.5 pH units, median).
\nWater use in Cumberland County varies and is highly seasonal, mainly because of increasing requirements for irrigation and the food processing industries in the county. In 1964 seasonal use ranged from 27 mgd in March to 145 mgd in August. This is much higher than withdrawals in neighboring Salem and Cape May Counties. In 1964 withdrawals in Cumberland County averaged about 51 mgd; almost all of this, 49.4 mgd, was from ground-water supplies. The total annual water use in 1964 according to type of use was: for public supply, 10.6 mgd; for industrial uses, 19.0 mgd; irrigation, 15.4 mgd; suburban, rural, residential, institutional, farm, and commercial, 5.9 mgd.
","language":"English","publisher":"New Jersey Department of Environmental Protection","collaboration":"Prepared in cooperation with New Jersey Department of Environmental Protection Division of Water Resources","usgsCitation":"Rooney, J.G., 1971, Ground-water resources: Cumberland County, New Jersey: Special Report 34, vi, 65 p.","productDescription":"vi, 65 p.","numberOfPages":"112","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":277134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047885.jpg"},{"id":311352,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047885/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New Jersey","county":"Cumberland County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.9322509765625,\n 39.191819549771694\n ],\n [\n -74.937744140625,\n 39.296048244024085\n ],\n [\n -74.90203857421875,\n 39.37677199661635\n ],\n [\n -74.893798828125,\n 39.50827899034111\n ],\n [\n -74.96520996093749,\n 39.57182223734374\n ],\n [\n -75.07507324218749,\n 39.605688178320804\n ],\n [\n -75.20690917968749,\n 39.63530729658598\n ],\n [\n -75.30029296875,\n 39.6437675734185\n ],\n [\n -75.3607177734375,\n 39.63530729658598\n ],\n [\n -75.399169921875,\n 39.63530729658598\n ],\n [\n -75.47607421875,\n 39.55911824217184\n ],\n [\n -75.5364990234375,\n 39.48284540453334\n ],\n [\n -75.5419921875,\n 39.46164364205549\n ],\n [\n -75.487060546875,\n 39.431950321168635\n ],\n [\n -75.44860839843749,\n 39.38526381099774\n ],\n [\n -75.38818359375,\n 39.34704251121735\n ],\n [\n -75.333251953125,\n 39.32579941789298\n ],\n [\n -75.25634765625,\n 39.26203141523749\n ],\n [\n -75.1959228515625,\n 39.20246222588235\n ],\n [\n -75.146484375,\n 39.16414104768742\n ],\n [\n -75.07507324218749,\n 39.198205348894795\n ],\n [\n -74.9322509765625,\n 39.191819549771694\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521f1be7e4b0f8bf2b07611a","contributors":{"authors":[{"text":"Rooney, James G.","contributorId":105628,"corporation":false,"usgs":true,"family":"Rooney","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":483221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047418,"text":"70047418 - 1971 - Floods in Arkansas, magnitude and frequency characteristics through 1968","interactions":[{"subject":{"id":52265,"text":"ofr6299 - 1961 - Floods in Arkansas, magnitude and frequency","indexId":"ofr6299","publicationYear":"1961","noYear":false,"title":"Floods in Arkansas, magnitude and frequency"},"predicate":"SUPERSEDED_BY","object":{"id":70047418,"text":"70047418 - 1971 - Floods in Arkansas, magnitude and frequency characteristics through 1968","indexId":"70047418","publicationYear":"1971","noYear":false,"title":"Floods in Arkansas, magnitude and frequency characteristics through 1968"},"id":1}],"lastModifiedDate":"2018-01-08T19:03:33","indexId":"70047418","displayToPublicDate":"2013-01-01T13:31:52","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":145,"text":"Arkansas Geological Commission Water Resources Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Floods in Arkansas, magnitude and frequency characteristics through 1968","docAbstract":"Techniques are presented for estimating the magnitude and frequency of floods on Arkansas streams. Modern topographic maps now available and computer techniques facilitate in making a comprehensive analysis in which physical and climactic characteristics of river basins are related to flood characteristics at gaging stations. Equations derived from the analysis make it possible to estimate the magnitude of future floods with recurrence intervals of as much as 50 years on gaged and ungaged streams that have drainage areas of 0.1-3,000 square miles. An estimate of the future flood potential can be used to locate and design flood-control structures, establish flood-insurance rates, and devise flood-zoning plans.
Appendixes in the report contain data on flood characteristics of gaged drainage basins, a summary of climatic and topographic characteristics of drainage basins, peak stages and discharges for gaging stations that have 5 or more years of record, and peak-flow data for outstanding floods at miscellaneous sites.
","language":"English","publisher":"Arkansas Geological Commission","publisherLocation":"Little Rock, Arkansas","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Arkansas Geological Commission and Arkansas State Highway Commission","usgsCitation":"Patterson, J.L., 1971, Floods in Arkansas, magnitude and frequency characteristics through 1968: Arkansas Geological Commission Water Resources Circular 11, viii, 21, A-26, B-199 p.","productDescription":"viii, 21, A-26, B-199 p.","numberOfPages":"258","costCenters":[],"links":[{"id":276047,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047418.PNG"},{"id":276042,"type":{"id":11,"text":"Document"},"url":"https://www.geology.ar.gov/pdf/Water%20Resources%20Circular%2011_v.pdf"}],"country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6448,36.4997 ], [ -89.6448,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5200c961e4b009d47a4c2377","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":481995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047605,"text":"70047605 - 1971 - Ground-water resources of Cass and Marion Counties, Texas","interactions":[{"subject":{"id":22575,"text":"ofr70376 - 1971 - Ground-water resources of Cass and Marion Counties, Texas","indexId":"ofr70376","publicationYear":"1971","noYear":false,"title":"Ground-water resources of Cass and Marion Counties, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047605,"text":"70047605 - 1971 - Ground-water resources of Cass and Marion Counties, Texas","indexId":"70047605","publicationYear":"1971","noYear":false,"title":"Ground-water resources of Cass and Marion Counties, Texas"},"id":1}],"lastModifiedDate":"2013-08-14T11:58:37","indexId":"70047605","displayToPublicDate":"2013-01-01T11:40:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"135","title":"Ground-water resources of Cass and Marion Counties, Texas","docAbstract":"Cass and Marion Counties, an area of 1,325 square miles in northeast Texas, are underlain by the Cypress aquifer which is composed of the Wilcox Group, Carrizo Sand, Reklaw Formation, and Queen City Sand, all of Eocene age. These geologic units are for the most part hydraulically interconnected and generally function as a single aquifer.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Texas Water Development Board","usgsCitation":"Broom, M.E., 1971, Ground-water resources of Cass and Marion Counties, Texas: Report 135, v, 66 p.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":276601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047605.png"},{"id":276600,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.texas.gov/publications/reports/numbered_reports/doc/R135/Report135.asp"}],"country":"United States","state":"Texas","county":"Cass County;Marion County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.708244,32.687893 ], [ -94.708244,33.3108 ], [ -94.042963,33.3108 ], [ -94.042963,32.687893 ], [ -94.708244,32.687893 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e6e4b081fa6136d3f8","contributors":{"authors":[{"text":"Broom, Mathew E.","contributorId":105633,"corporation":false,"usgs":true,"family":"Broom","given":"Mathew","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046223,"text":"70046223 - 1971 - Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah","interactions":[{"subject":{"id":57138,"text":"ofr70375 - 1970 - Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah","indexId":"ofr70375","publicationYear":"1970","noYear":false,"title":"Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70046223,"text":"70046223 - 1971 - Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah","indexId":"70046223","publicationYear":"1971","noYear":false,"title":"Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah"},"id":1}],"lastModifiedDate":"2017-05-24T10:40:37","indexId":"70046223","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"32","title":"Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah","docAbstract":"This water-resources investigation was initiated in order to provide an estimate of the average annual water yield of the Mill Creek-Pack Creek drainage basin, the parts of that total yield available as surface water and ground water, the amount of ground water that might be recovered for beneficial use, and the effect of this use on the usable ground-water storage within the valley fill in Spanish and Moab Valleys. Detailed information has been sought which is basic to the establishment of sound policies for the development and management of water resources. The investigation was carried out as part of water-resources investigations in Utah with the Utah Division of Water Rights, Department of Natural Resources. Fieldwork was done during the period July 1967-November 1969.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Sumsion, C.T., 1971, Geology and water resources of the Spanish Valley area, Grand and San Juan Counties, Utah: Technical Publication 32, Report: iv, 45 p.; 3 Plates.","productDescription":"Report: iv, 45 p.; 3 Plates","numberOfPages":"52","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":273078,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341623,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://waterrights.utah.gov/docImport/0588/05884275.jpg","text":"Plate 1","size":"23.0 MB JPEG","linkHelpText":"Map of the Spanish Valley Area, Grand and San Juan Counties, Utah, showing generalized geology and locations of selected wells and springs"},{"id":341624,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://waterrights.utah.gov/docImport/0588/05884276.jpg","text":"Plate 2","size":"21.9 MB JPEG","linkHelpText":"Hydrologic map of the Spanish Valley Area, Grand and San Juan Counties, Utah"},{"id":341625,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://waterrights.utah.gov/docImport/0588/05884277.jpg","text":"Plate 3","size":"15.4 MB JPEG","linkHelpText":"Map of Spanish Valley Area, Grand and San Juan Counties, Utah, showing simulated water-level changes"},{"id":331798,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-690"},{"id":331799,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008u.pdf"}],"country":"United States","state":"Utah","county":"Grand County, San Juan County","otherGeospatial":"Spanish Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.4,37.0 ], [ -111.4,39.5 ], [ -109.04,39.5 ], [ -109.04,37.0 ], [ -111.4,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51ac6962e4b0cc85b6ed6b40","contributors":{"authors":[{"text":"Sumsion, C. 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The series is prepared by the U. S. Geological Survey and published by the California Department of Water Resources. Each bulletin locates water wells and springs in a part of the southern California desert regions; describes well depth and yield, water use and level on dates observed; names the well owner; provides pumping data, including depths, rates, static water levels, drawdowns, and specific capacities; and lithologic data from drillers' well logs.","language":"English","publisher":"California Department of Water Resources","publisherLocation":"Sacramento, CA","collaboration":"Prepared by United States Department of Interior, Geological Survey","usgsCitation":"Moyle, W., 1971, Water wells in the Harper, Superior, and Cuddeback Valley areas, San Bernardino County, California: Bulletin 91-19, 99 p.","productDescription":"99 p.","costCenters":[],"links":[{"id":274385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046751.jpg"},{"id":274383,"type":{"id":11,"text":"Document"},"url":"https://www.water.ca.gov/waterdatalibrary/docs/historic/Bulletins/Bulletin_91/Bulletin_91-19__1971.pdf"}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Harper Valley;Superior Valley;Cuddeback Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.7829,33.6472 ], [ -114.7829,34.9272 ], [ -113.5029,34.9272 ], [ -113.5029,33.6472 ], [ -114.7829,33.6472 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51d2a4f0e4b0ca1848338aaf","contributors":{"authors":[{"text":"Moyle, W. 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These data for the 1970 water year for the quality of surface water in California are presented in this report. Data for a few water-quality stations in bordering States are also included. The data were collected by the Water Resources Division of the Geological Survey under the direction of R. Stanley Lord, district chief, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA702","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Water resources data for California, 1970; Part 2: Water quality reports: U.S. Geological Survey Water Data Report CA-70-2, xi, 450 p., https://doi.org/10.3133/wdrCA702.","productDescription":"xi, 450 p.","costCenters":[],"links":[{"id":257489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1970/ca-70/WDR-1970-wq.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_70_2.jpg"}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc952e4b08c986b32ccd7","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":535192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}