A basin filled with Triassic red beds, located on the South Carolina–Georgia line ∼32 km southeast of Augusta, Georgia, is buried beneath ∼350 m of Coastal Plain sediments. An extensive aeromagnetic survey, seismic refraction and reflection surveys, and geophysical logs and samples from three wells define the extent and character of the basin. This basin, herein named the Dunbarton Triassic basin, is ∼50 km long, 10 km wide, and trends northeast.
The northwest margin of the basin is well defined by the aeromagnetic survey, a seismic reflection traverse, and a well that passed through 485 m of Triassic fanglomerate before entering the crystalline metamorphic rocks below. Near the center of the Triassic basin, a well passed through 902 m of maroon Triassic mudstone and sandstone of fluvial origin without penetrating the bottom of the basin.
The permeability of the Triassic rock is extremely low, and water-transmitting fractures were not penetrated. Even slight water-level disturbances in the Triassic wells require many years to recover. Total dissolved solids of the water from the Triassic basin are about twice that in the crystalline metamorphic rocks that surround it.
The inferred geologic history of this basin is similar to the history of Triassic basins that crop out in North Carolina.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/5652","usgsCitation":"Baker, E., and Watson, J.A., 1974, Quantity of low flow in Barton Creek, Texas, July 6-8 and October 1-3, 1970: Open-File Report, 24 p., https://doi.org/10.3133/5652.","productDescription":"24 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":289754,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Barton Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.7129908803,30.9185620197 ], [ -96.7129908803,30.9212599803 ], [ -96.7102929197,30.9212599803 ], [ -96.7102929197,30.9185620197 ], [ -96.7129908803,30.9185620197 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bfb60ce4b06d97a6487d30","contributors":{"authors":[{"text":"Baker, Ernest T.","contributorId":99900,"corporation":false,"usgs":true,"family":"Baker","given":"Ernest T.","affiliations":[],"preferred":false,"id":151369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watson, Jerry A.","contributorId":24691,"corporation":false,"usgs":true,"family":"Watson","given":"Jerry","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":151368,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70199339,"text":"70199339 - 1974 - Lakes of Oregon, Volume 2: Benton, Lincoln, and Polk Counties","interactions":[],"lastModifiedDate":"2018-09-21T14:27:23","indexId":"70199339","displayToPublicDate":"1974-01-01T15:27:14","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Lakes of Oregon, Volume 2: Benton, Lincoln, and Polk Counties","docAbstract":"An inventory of lakes and reservoirs of Oregon is essential for a complete evaluation of the total surface-water supply of the State and to provide a basis for answering questions about Oregon's lakes. Much of the information on lakes and reservoirs previously collected by Federal and State agencies has never been published. These data were compiled and used as a basis for collecting additional information. This report provides information for use by city, county, and State planning groups as well as for sportsmen, tourists, and others interested in preserving the recreational value of Oregon's lakes.
Because of the large number of lakes and reservoirs in Oregon, a single report covering the State would be bulky. Therefore, the lake information is being published in several volumes on a county or multicounty basis. Volume .1, published in 1973, covered Clatsop, Columbia, and Tillamook Counties. Benton, Lincoln, and Polk Counties were selected for this report. (See fig. 1.)
In addition to office compilation of existing data, most lakes were also visited. Visits were made in late summer or early fall when lakes were most accessible and when water temperature and biological activity are at a maximum. Some lakes previously studied by other Federal or State agencies and included in this report were not visited during the study.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70199339","collaboration":"Prepared in cooperation with the Oregon State Engineer","usgsCitation":"Shulters, M., 1974, Lakes of Oregon, Volume 2: Benton, Lincoln, and Polk Counties: Open-File Report, iii, 71 p., https://doi.org/10.3133/70199339.","productDescription":"iii, 71 p.","costCenters":[],"links":[{"id":357627,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70199339/report-thumb.jpg"},{"id":357628,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70199339/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Benton County, Lincoln County, Polk County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.10705566406249,\n 44.25\n ],\n [\n -123,\n 44.25\n ],\n [\n -123,\n 45.15\n ],\n [\n -124.10705566406249,\n 45.15\n ],\n [\n -124.10705566406249,\n 44.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shulters, M.V.","contributorId":54583,"corporation":false,"usgs":true,"family":"Shulters","given":"M.V.","email":"","affiliations":[],"preferred":false,"id":746021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168647,"text":"70168647 - 1974 - Water resources data for Iowa, water year 1973","interactions":[],"lastModifiedDate":"2016-02-22T14:02:29","indexId":"70168647","displayToPublicDate":"1974-01-01T15:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Iowa, water year 1973","docAbstract":"No abstract available.
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Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Miller, R. Adam","contributorId":21540,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"Adam","affiliations":[],"preferred":false,"id":829281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69500,"text":"hu20 - 1974 - Hydrologic Unit Map -- 1974, states of Maryland and Delaware","interactions":[],"lastModifiedDate":"2014-07-29T10:55:52","indexId":"hu20","displayToPublicDate":"1974-01-01T10:52:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"20","subseriesTitle":"Maryland & Delaware 1974","title":"Hydrologic Unit Map -- 1974, states of Maryland and Delaware","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu20","isbn":"607767782","collaboration":"Prepared in cooperation with the U.S. Water Resources Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, states of Maryland and Delaware: U.S. Geological Survey Hydrologic Unit 20, 1 map: 17.72 x 32.28 inches, https://doi.org/10.3133/hu20.","productDescription":"1 map: 17.72 x 32.28 inches","costCenters":[],"links":[{"id":291273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"500000","country":"United States","state":"Delaware;Maryl","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.0,38.0 ], [ -79.0,39.0 ], [ -75.0,39.0 ], [ -75.0,38.0 ], [ -79.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffc248e4b0824b2d172e58","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":534596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70247401,"text":"70247401 - 1974 - Water-management studies of a stream-aquifer system, Arkansas River Valley, Colorado","interactions":[],"lastModifiedDate":"2023-08-02T15:36:25.743334","indexId":"70247401","displayToPublicDate":"1974-01-01T10:33:10","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Water-management studies of a stream-aquifer system, Arkansas River Valley, Colorado","docAbstract":"A mathematical model was developed and used to simulate the stream-aquifer system in the Arkansas River valley in southeastern Colorado, from Pueblo to the Colorado-Kansas State line. The model simulates the interrelations among ground water and surface water including reservoirs, losses, and transmountain diversions, utilizing various water-distribution rules. The model was used to analyze 24 water-management plans designed to reduce shortages in the irrigation supply. One management plan simulated salvage of water from phreatophyte evapotranspiration, different reservoir operation regulations, use of imported ground and surface water, a new reservoir, additional ground-water use, and application of excess streamflow. The resulting annual dependable supply was increased from 610,000 acre-feet to 870,000 acre-feet in relation to an annual demand of 1,100,000 acre-feet. The model can be used as a tool to analyze other water-management plans.
","language":"English","publisher":"National Groundwater Association","doi":"10.1111/j.1745-6584.1974.tb02997.x","usgsCitation":"Taylor, O., and Luckey, R.R., 1974, Water-management studies of a stream-aquifer system, Arkansas River Valley, Colorado: Groundwater, v. 12, no. 1, p. 22-38, https://doi.org/10.1111/j.1745-6584.1974.tb02997.x.","productDescription":"17 p.","startPage":"22","endPage":"38","costCenters":[],"links":[{"id":419506,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Arkansas River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.78393923614753,\n 39.03731677993051\n ],\n [\n -105.78393923614753,\n 36.991243523169516\n ],\n [\n -102.0502964601309,\n 36.991243523169516\n ],\n [\n -102.0502964601309,\n 39.03731677993051\n ],\n [\n -105.78393923614753,\n 39.03731677993051\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"12","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, O. James","contributorId":23958,"corporation":false,"usgs":true,"family":"Taylor","given":"O. James","affiliations":[],"preferred":false,"id":879464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luckey, Richard R.","contributorId":17980,"corporation":false,"usgs":true,"family":"Luckey","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":879465,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70247415,"text":"70247415 - 1974 - Determination of selenium in water","interactions":[],"lastModifiedDate":"2023-08-03T14:23:29.735796","indexId":"70247415","displayToPublicDate":"1974-01-01T09:15:30","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":16673,"text":"Atomic Absorption Newsletter","active":false,"publicationSubtype":{"id":10}},"title":"Determination of selenium in water","docAbstract":"The determination of selenium by hydride generation atomic absorption spectrophotometry using zinc is widely used. Very little is mentioned, however, on possible interferences. In an attempt to use this technique for the determination of selenium in natural waters, interferences were found. The most serious interference occurred when arsenic was present. As little as 5 μg of arsenic/l suppressed the formation of selenium hydride. Because arsenic may be present with selenium in natural waters, the above method was abandoned in favor of the following atomic absorption spectrophotometric method for the determination of both inorganic and organically bound selenium. Organic selenium compounds, if present, are first decomposed by digestion with potassium permanganate in hot acid solution. The solution is then made basic and the solution evaporated to dryness in the presence of calcium chloride which prevents the loss of selenate during the evaporation. Hydrochloric acid is added to the residue to reduce the selenate to selenite. Quantitative reduction is obtained without loss of selenium by controlling the temperature, time, and acid concentration. It should be emphasized that the selenium must be in the selenite form prior to its final reduction. The selenium is finally liberated from 6M hydrochloric acid solution with stannous chloride and the selenium hydride vapor subsequently removed from solution by aeration and swept by a flow of nitrogen into a hydrogen flame where it is determined by atomic absorption at 196.0 nm. The method may be used to analyze water samples containing at least 2 μg/l of selenium.
","language":"English","publisher":"Perkin-Elmer Corporation","usgsCitation":"Lansford, M., McPherson, E.M., and Fishman, M., 1974, Determination of selenium in water: Atomic Absorption Newsletter, v. 13, no. 4, p. 103-105.","productDescription":"3 p.","startPage":"103","endPage":"105","costCenters":[],"links":[{"id":419526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lansford, M.","contributorId":317859,"corporation":false,"usgs":true,"family":"Lansford","given":"M.","email":"","affiliations":[],"preferred":false,"id":879514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McPherson, E. M.","contributorId":100068,"corporation":false,"usgs":true,"family":"McPherson","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":879515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":879516,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37137,"text":"37137 - 1974 - Life history of the spottail shiner (Notropis hudsonius) in southeastern Lake Michigan, the Kalamazoo River, and western Lake Erie","interactions":[],"lastModifiedDate":"2012-02-02T00:15:50","indexId":"37137","displayToPublicDate":"1974-01-01T01:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78","title":"Life history of the spottail shiner (Notropis hudsonius) in southeastern Lake Michigan, the Kalamazoo River, and western Lake Erie","docAbstract":"In southeastern Lake Michigan spottail shiners in samples ranged from ages 0 to V, but most were in age groups I-IV. In the Kalamazoo River (a tributary of southeastern Lake Michigan) age group II was commonest in the catches, and no fish older than age IV were sampled. In western Lake Erie, most shiners were in age groups 0-II, and none were older than age IV. Mortality of males was much higher than that of females after age II in Lake Michigan and after age I in Lake Erie. Growth of spottail shiners was fastest in western Lake Erie (125 mm at the end of the third year, sexes combined) and slowest (77 mm) in the Kalamazoo River; in all three waters growth declined rapidly after the first year. Females grew faster than males.\nYoung shiners started growing earlier in the year than older ones in all three waters. Males and females of the same age resumed growth at about the same time. The growing season began as early as mid-May in the Kalamazoo River and continued as late as September or early October in the other two waters. Small spottail shiners in Lake Michigan and the Kalamazoo River weighed about the same at a given length, but at lengths greater than about 100 mm the lake fish were heavier. In all three waters, spottail shiners matured at about the same length, and males at a somewhat smaller size than females. Smallest mature fish were 65-69 mm long, and the largest immatures were 80-84 mm. In Lake Michigan about half and in Lake Erie about three-quarters of age-I fish were mature, as were all age-II fish in both lakes. In the Kalamazoo River a few fish of age II and all of age III were mature. The spawning season in Lake Michigan in 1964 was from late June or early July to late July, whereas in 1972, which had a colder spring, spawning occurred from mid-July to late August or early September. All shiners in the Kalamazoo River had spawned by the end of June if 1964. Lake Erie spottail shiners spawned during early June to early or mid-July in 1958. Spottail shiners 87-143 mm long from the different waters contained 915 to 8,898 mature eggs.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Wells, L., and House, R., 1974, Life history of the spottail shiner (Notropis hudsonius) in southeastern Lake Michigan, the Kalamazoo River, and western Lake Erie: Research Report 78, 10 p. : ill. ; 26 cm.","productDescription":"10 p. : ill. ; 26 cm.","startPage":"0","endPage":"10","numberOfPages":"10","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":94582,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009784570?urlappend=%3Bseq=3"},{"id":203849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a53e8","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":217546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"House, Robert","contributorId":58974,"corporation":false,"usgs":true,"family":"House","given":"Robert","affiliations":[],"preferred":false,"id":217545,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000494,"text":"1000494 - 1974 - Effect of acclimation temperature and heat shock on vulnerability of fry of lake whitefish (Coregonus clupeaformis) to predation","interactions":[],"lastModifiedDate":"2016-03-14T11:14:04","indexId":"1000494","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"Effect of acclimation temperature and heat shock on vulnerability of fry of lake whitefish (Coregonus clupeaformis) to predation","docAbstract":"Fry of lake whitefish (Coregonus clupeaformis) acclimated to 10, 15, and 18 C were exposed to temperatures of 24.5, 25, and 28 C for 1 min and then immediately returned to water at their acclimation temperature, in test tanks containing yearling yellow perch (Perca flavescens). The number of attacks on the fry and the number captured and eaten in 30 min were recorded in separate tests of shocked and unshocked (control) whitefish.Significantly more whitefish were captured per attack (data for shocked and unshocked fry combined) at 15 and 18 C than at 10 C; and shocked fry were significantly more vulnerable to capture by the perch than were unshocked controls.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f74-180","usgsCitation":"Yocom, T.G., and Edsall, T.A., 1974, Effect of acclimation temperature and heat shock on vulnerability of fry of lake whitefish (Coregonus clupeaformis) to predation: Journal of the Fisheries Research Board of Canada, v. 31, no. 9, p. 1503-1506, https://doi.org/10.1139/f74-180.","productDescription":"4 p.","startPage":"1503","endPage":"1506","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62578d","contributors":{"authors":[{"text":"Yocom, Thomas G.","contributorId":38095,"corporation":false,"usgs":true,"family":"Yocom","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":308623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edsall, Thomas A.","contributorId":84302,"corporation":false,"usgs":true,"family":"Edsall","given":"Thomas","email":"","middleInitial":"A.","affiliations":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"preferred":false,"id":308624,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48243,"text":"ofr741066 - 1974 - The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada","interactions":[],"lastModifiedDate":"2022-07-07T19:09:19.724679","indexId":"ofr741066","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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":"74-1066","title":"The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada","docAbstract":"Fifty-five of the principal hot springs in northern and central Nevada have been sampled for chemical analyses. Major element constituents, sodium, potassium, calcium, and silica suggest minimum thermal-aquifer temperatures of 140°C or more at 16 of the hot spring complexes. At least five of the hot springs issue mixed waters which may indicate thermal-aquifer temperatures significantly lower than the true thermal-aquifer temperature.
Sodium is the principal cation in almost all the spring waters. Four springs in northern Nye County and adjacent Eureka County have approximately equal amounts of sodium and calcium. Bicarbonate is the principal anion in most of the spring waters. However, the sampled hot springs on the western edge of the State have chloride as the principal anion. A diffuse zone of bicarbonate chloride waters with or without sulfate separates the chloride and bicarbonate regions.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741066","usgsCitation":"Mariner, R.H., Rapp, J.B., Willey, L., and Presser, T.S., 1974, The chemical composition and estimated minimum thermal reservoir temperatures of the principal hot springs of northern and central Nevada: U.S. Geological Survey Open-File Report 74-1066, 32 p., https://doi.org/10.3133/ofr741066.","productDescription":"32 p.","costCenters":[],"links":[{"id":403210,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1066/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1066/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.003662109375,\n 42.00032514831621\n ],\n [\n -120.0146484375,\n 39.01918369029134\n ],\n [\n -118.421630859375,\n 37.88352498087131\n ],\n [\n -114.04907226562499,\n 38.004819966413194\n ],\n [\n -114.0380859375,\n 42.00848901572399\n ],\n [\n -120.003662109375,\n 42.00032514831621\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db66939c","contributors":{"authors":[{"text":"Mariner, Robert H.","contributorId":81075,"corporation":false,"usgs":true,"family":"Mariner","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":237027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rapp, J. B.","contributorId":28987,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":237025,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willey, L.M.","contributorId":44607,"corporation":false,"usgs":true,"family":"Willey","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":237026,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Presser, T. 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Data on prevalence, host specificity, age of host, and geographic distribution are given. Infections were more intense in sick birds and birds in poor physical condition. Accidental or abnormal infection was more likely in sick than in normal birds. From 1 to 13 species of nematodes are reported from each host species, including 118 new host records, 3 nematodes new for North America, and 1 new species. Multiple infections were present in 76.5% of birds parasitized; eight species of nematodes were found in one whistling swan (Olor columbianus).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Disease","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McDonald, M., 1974, Nematode parasites of waterfowl (Anseriformes) from western United States: Wildlife Disease, no. 64, p. 19-19.","productDescription":"1 p.","startPage":"19","endPage":"19","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":129103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"64","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e1b","contributors":{"authors":[{"text":"McDonald, M.E.","contributorId":33661,"corporation":false,"usgs":true,"family":"McDonald","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":310700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175498,"text":"70175498 - 1974 - Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1972","interactions":[],"lastModifiedDate":"2016-08-15T14:42:38","indexId":"70175498","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1972","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175498","usgsCitation":"Buckner, H., 1974, Hydrologic data for Mountain Creek, Trinity River Basin, Texas, 1972: Open-File Report, 13 p., https://doi.org/10.3133/70175498.","productDescription":"13 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326494,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bbe4b03bcb0102e8c0","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":645502,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014366,"text":"1014366 - 1974 - Yield of channel catfish and composition of effluents from shallow-water raceways","interactions":[],"lastModifiedDate":"2025-08-05T16:26:17.960045","indexId":"1014366","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Yield of channel catfish and composition of effluents from shallow-water raceways","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1974)36[46:YOCCAC]2.0.CO;2","usgsCitation":"Tackett, D.L., 1974, Yield of channel catfish and composition of effluents from shallow-water raceways: Progressive Fish-Culturist, v. 36, no. 1, p. 46-48, https://doi.org/10.1577/1548-8659(1974)36[46:YOCCAC]2.0.CO;2.","productDescription":"3 p.","startPage":"46","endPage":"48","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129615,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de42c","contributors":{"authors":[{"text":"Tackett, Dewey L.","contributorId":8024,"corporation":false,"usgs":true,"family":"Tackett","given":"Dewey","middleInitial":"L.","affiliations":[],"preferred":false,"id":320258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175494,"text":"70175494 - 1974 - Hydrologic data for Little Pond Creek and North Elm Creek, Brazos River Basin, Texas, 1972","interactions":[],"lastModifiedDate":"2016-08-15T14:31:38","indexId":"70175494","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Little Pond Creek and North Elm Creek, Brazos River Basin, Texas, 1972","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175494","usgsCitation":"Mitchell, R., 1974, Hydrologic data for Little Pond Creek and North Elm Creek, Brazos River Basin, Texas, 1972: Open-File Report, 37 p., https://doi.org/10.3133/70175494.","productDescription":"37 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bbe4b03bcb0102e8be","contributors":{"authors":[{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":645498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010918,"text":"70010918 - 1974 - Oxygen isotope activities and concentrations in aqueous salt solutions at elevated temperatures: Consequences for isotope geochemistry","interactions":[],"lastModifiedDate":"2021-01-19T14:22:50.051957","indexId":"70010918","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen isotope activities and concentrations in aqueous salt solutions at elevated temperatures: Consequences for isotope geochemistry","docAbstract":"Studies of the effect of dissolved salts on the oxygen isotope activity ratio of water have been extended to 275°C. Dehydrated salts were added to water of known isotope composition and the solutions were equilibrated with CO2 which was sampled for analysis. For comparison similar studies were made using pure water. Results on water nearly coincide with earlier calculations. Salt effects diminish with increasing temperature only for solutions of MgCl2 and LiCl. Other salt solutions show complex behavior due to the temperature-dependent formation of ion pairs of changing character. Equilibrium fractionations (103 ln α) between 1 molal solutions and pure water at 25, 100, and 275°C are: NaCl 0.0, −1.5, +1.0; KCl 0.0, −1.0, +2.0; LiCl −1.0, −0.6, −0.5; CaCl2 −0.4, −1.8, +0.8; MgCl2 −1.1, −0.7, −0.3; MgSO4 −1.1, +0.1, −; NaF (0.8 m) 0.0, −1.5, −0.3; and NH4Cl (0.55 m) 0.0, −1.2, −1.3. These effects are significant in the isotope study of hot saline fluids responsible for ore deposition and of fluids found in certain geothermal systems. Minor modification of published isotope geothermometers may be required.
Water potential in Sonoran Desert shrubs was recorded from September 1968 through September 1969. Special attention was paid to recording maximum and minimum potentials on a seasonal basis and diurnal fluctuations during the wettest and driest periods of the year. Franseria deltoidea developed the lowest potential (—85 bar) of the shrubs recorded and also showed the greatest degree of response to changes in soil moisture on a seasonal basis and evaporative power of the air on a diurnal basis. Of the species tested, Eriogonum fasciculatum showed a high degree of response to changing conditions; Larrea tridentata, Krameria gravi, and Simmondsia chinesis showed a moderate response; and Cercidium microphyllum showed only a slight response to diurnal or seasonal changes.
","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1934632","usgsCitation":"Halvorson, W., and Patten, D.T., 1974, Seasonal water potential changes in Sonoran Desert shrubs in relation to topography: Ecology, v. 55, p. 173-177, https://doi.org/10.2307/1934632.","productDescription":"5 p.","startPage":"173","endPage":"177","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130406,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","noUsgsAuthors":false,"publicationDate":"1974-01-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2e3","contributors":{"authors":[{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":315853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patten, Duncan T.","contributorId":124573,"corporation":false,"usgs":false,"family":"Patten","given":"Duncan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":315852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175503,"text":"70175503 - 1974 - Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972","interactions":[],"lastModifiedDate":"2021-11-09T20:27:51.682147","indexId":"70175503","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972","docAbstract":"The U.S. Soil Conservation Service is actively engaged in the installation of flood- and soil-erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of approximately 3,500 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1972, 1,551 of these structures had been built.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175503","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Hampton, B., 1974, Hydrologic data for Pin Oak Creek, Trinity River Basin, Texas, 1972: Open-File Report, 26 p., https://doi.org/10.3133/70175503.","productDescription":"26 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":391527,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70175503/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":326500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70175503/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Pin Oak Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7bde4b03bcb0102e8ef","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":645512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}