{"pageNumber":"2368","pageRowStart":"59175","pageSize":"25","recordCount":68846,"records":[{"id":48157,"text":"ofr73137 - 1975 - A survey of the water resources of St. Croix, Virgin Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:10:06","indexId":"ofr73137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"73-137","title":"A survey of the water resources of St. Croix, Virgin Islands","docAbstract":"St. Croix consists of two mountainous volcanic rock cores separated by a graben containing clays with minor limestone and conglomerate that is overlain by about 300 feet of marl and limestone. Predominantly fine-grained alluvium mantles much of the limestone and marl area and fills overdeepened south-trending valleys to depths of as much as 100 feet. Rainfall follows an orographic pattern ranging from about 30 inches in eastern St. Croix to 55 inches in the northwestern mountains. \r\n\r\nFour streams, all heading in the Northside Range, have intermittent reaches. All other streams in St. Croix are ephemeral, flowing only for a few hours or days following major rainstorms. Flow in the intermittent streams ranges from about 1 to 9 percent of the total rainfall and usually half or more of the flow is storm runoff resulting from two or three major storms. Storm runoff from individual storms seldom exceeds 5 percent of the rainfall. Only from 2 storms, one of 5 inches and the other of 7 inches in less than 48 hours, did runoff reach 20 percent, both times on River Gut at Golden Grove. The lack of storm runoff is attributed to the capability of the soil zone to accept large volumes of water and deficient soil moisture most of the year. \r\n\r\nThe dissolved-solids content of the water of St. Croix. reflects the influence of the sea and land. Bulk precipitation is believed to be the source of the initial mineral content of the island water. Additional mineralization, particularly of ground water, results from the solution of soluble salts, mixing with residual sea water, and concentration by evapotranspiration. Water in the volcanic rocks is basically a calcium bicarbonate sodium chloride type with dissolved solids ranging from 500 to 1,000 mg/l (milligrams per liter), and chloride concentration of 100 to 300 mg/1. By contrast, water in the limestone is a sodium bicarbonate sodium chloride type with dissolved-solids content ranging from less than 1,000 to more than 20,000 mg/1 and chloride concentration from less than 100 to more than 10,000 mg/l. The mineral content of water in the limestone invariably increases with depth. Water in the alluvial deposits and in the streams usually reflects the characteristics of water from the adjacent bedrock. \r\n\r\nThe retention of large volumes of rainfall in the soil zone from which it is evaporated and transpired by plants greatly reduces the water available for recharge to the aquifers of the island. Estimates of effective recharge to the aquifers range from less than 0.5 inch in some volcanic and marl rocks to 5 inches annually in more porous limestone and alluvium. Long-term yield from the aquifers is also affected by their storage capacity which may range from less than 1 percent in volcanic rocks and marl to 10 to 15 percent in limestone and alluvium. The ground-water potential (equivalent to the quantity of recharge) of St. Croix is estimated at 3.9 mgd (million gallons per day)--0.9 mgd from the Northside Range (Area 1) ; 0.4 mgd from the East End Range (Area 2), and 2.6 mgd from the central lowlands (Area 3). Most areas where major ground-water supplies are .available, principally in Central St. Croix, have already been developed. The Castle Coakley area, with a potential yield of 400,000 gpd, is the only major ground-water area still undeveloped. \r\n\r\nThe ground-water potential could be increased by reducing the brush and forest cover thus reducing water losses from transpiration; artificial recharge of alluvial aquifer by water spreading; utilizing streamflow (including storm runoff) or treated sewage effluent; or by lowering the ground-water level adjacent to streams to induce infiltration. \r\n\r\nAdvancements in desalination have made the brackish ground water in the Kingshill Marl (estimated at 35 billion recoverable gallons by Robison, 1972) a potential source of water. Recovery of this water would partly de-water the aquifer, which would cause water of better quality in the overlying rocks to","language":"ENGLISH","doi":"10.3133/ofr73137","usgsCitation":"Jordan, D.G., 1975, A survey of the water resources of St. Croix, Virgin Islands: U.S. Geological Survey Open-File Report 73-137, 131 p. part col.ill., part col.maps ; 28 cm., https://doi.org/10.3133/ofr73137.","productDescription":"131 p. part col.ill., part col.maps ; 28 cm.","costCenters":[],"links":[{"id":162666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0137/report-thumb.jpg"},{"id":84890,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0137/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0137/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0137/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5dae","contributors":{"authors":[{"text":"Jordan, Donald George","contributorId":44127,"corporation":false,"usgs":true,"family":"Jordan","given":"Donald","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":236889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65858,"text":"i947 - 1975 - Shaded relief map of the Erythraeum region of Mars","interactions":[{"subject":{"id":41642,"text":"ofr73316 - 1973 - Atlas of Mars, Erythraeum region of Mars (controlled photomosaic)","indexId":"ofr73316","publicationYear":"1973","noYear":false,"title":"Atlas of Mars, Erythraeum region of Mars (controlled photomosaic)"},"predicate":"SUPERSEDED_BY","object":{"id":65858,"text":"i947 - 1975 - Shaded relief map of the Erythraeum region of Mars","indexId":"i947","publicationYear":"1975","noYear":false,"title":"Shaded relief map of the Erythraeum region of Mars"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i947","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"947","subseriesTitle":"NONE","title":"Shaded relief map of the Erythraeum region of Mars","language":"ENGLISH","doi":"10.3133/i947","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Shaded relief map of the Erythraeum region of Mars: U.S. Geological Survey IMAP 947, 1 map :col. ;107 x 48 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i947.","productDescription":"1 map :col. ;107 x 48 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101206,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0947/plate-1.pdf","size":"5879","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 16,20 ], [ 16,28 ], [ 35,28 ], [ 35,20 ], [ 16,20 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f468d","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":534212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2127,"text":"wsp1827G - 1975 - Effects of organic solutes on chemical reactions of aluminum","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1827G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1827","chapter":"G","title":"Effects of organic solutes on chemical reactions of aluminum","docAbstract":"Concentrations of organic matter in the general range of 1-10 milligrams per litre organic carbon are common in natural water, and many naturally occurrin7 organic compounds form aluminum complexes. The aluminum concentrations in near-neutral pH solutions may be 10-100 times higher than the values predicted from solubility data if formation of such organic complexes is ignored. The processes of polymerization of aluminum hydroxide and precipitation of gibbsite are inhibited by the presence of the organic flavone compound quercetin in concentrations as low as 10 x -5.3 mole per litre. Quercetin forms a complex, with a probable molar ratio of 1:2 aluminum to quercetin, that has a formation constant (f12) of about 10 12. A complex with a higher aluminum-quercetin ratio also was observed, but this material tends to evolve into a compound of low solubility that removes aluminum from solution. \r\n\r\nIn the presence of both dissolved aluminum and aqueous silica, low concentrations of quercetin improved the yield of crystallized kaolinite and halloysite. Small amounts of well-shaped kaolinite and halloysite crystals were identified by electron microscopy in solutions with pH's in the range 6.5-8.5 after 155 days aging in one experimer t and 481 days aging in a repeated experiment. The bulk of the precipitated material was amorphous to X-rays, and crystalline material was too small a proportion of the total to give identifiable X-ray diffraction peaks. The precipitates had aluminum-silicon ratios near 1, and their solubility corresponded to that found by Hem, Roberson, Lind, and Polzer (1973) for similar aluminosilicate precipitated in the absence of organic solutes. The improved yield of crystalline material obtained in the presence of quercetin probably is the result of the influence of the organic compound on the aluminum hydroxide polymerization process. \r\n\r\nNatural water containing color imparted by organic material tends to be higher in aluminum than would be predicted by pH, silica concentrations, and solubility data for inorganic aluminum species.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1827G","usgsCitation":"Lind, C.J., and Hem, J.D., 1975, Effects of organic solutes on chemical reactions of aluminum: U.S. Geological Survey Water Supply Paper 1827, v, 83 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1827G.","productDescription":"v, 83 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1827g/report-thumb.jpg"},{"id":27727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1827g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686720","contributors":{"authors":[{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56529,"text":"wdrNC742 - 1975 - Water resources data for North Carolina, water year 1974; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2020-05-06T20:37:35.963271","indexId":"wdrNC742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NC-74-2","title":"Water resources data for North Carolina, water year 1974; Part 2, Water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNC742","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for North Carolina, water year 1974; Part 2, Water quality records: U.S. Geological Survey Water Data Report NC-74-2, v, 158 p. , https://doi.org/10.3133/wdrNC742.","productDescription":"v, 158 p. 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,{"id":25118,"text":"cir601K - 1975 - An introduction to the processes, problems, and management of urban lakes","interactions":[],"lastModifiedDate":"2017-07-07T08:54:01","indexId":"cir601K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"601","chapter":"K","title":"An introduction to the processes, problems, and management of urban lakes","docAbstract":"<p>Lakes are bodies of water formed in depressions on the earth's surface, and as such, act as depositories for a variety of chemical and biological materials. The study of lakes has become increasingly prevalent in recent years. Lakes are a valuable resource, and their multiple uses have made them susceptible to water-quality problems such as algal blooms, sediment deposition and fish kills. These problems are products of the eutrophication process (enrichment, aging and extinction of lakes), which is often accelerated by man. Therefore, it becomes important to understand the properties and processes of lakes which govern lake enrichment, and the measures available to control enrichment.</p>\n<p>Lakes are described in terms of their physical (light penetration, temperature, sediment, and morphology), chemical (chemical constituents, plant nutrients:, and dissolved gases) and biological (plankton, benthos, and nekton) properties. These properties are all interre]ated, and are important variables to measure to evaluate water quality. In addition, lake processes, such as photosynthesis, respiration, eutrophication, and biogeochemical cycling, are important factors in determining the sources and extent of enrichment, and managing a lake for maximum benefit. Meeting demands for water of high quality requires a general knowledge of lake properties and processes, coupled with lake-basin planning, watershed and lake management, and water-quality control. There are many lake-management and control practices, but the best tools for quality control are preventive measures. Once extensive enrichment has occurred, there are few management or control options available.</p>\n<p>As lake studies become more common, sampling techniques for data collection need increased accuracy and consistency, in order to make meaningful comparisons between different lakes. Therefore, the report discusses the main factors involved in conducting lake studies. These factors include the types and frequency of measurements useful in lake reconnaissance studies and a review of literature on sampling equipment and techniques. A glossary of selected terms begins the report, which is intended for guideline use by urban planners and managers.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir601K","usgsCitation":"Britton, L.J., Averett, R., and Ferreira, R.F., 1975, An introduction to the processes, problems, and management of urban lakes: U.S. Geological Survey Circular 601, vi, 22 p., https://doi.org/10.3133/cir601K.","productDescription":"vi, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science 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States\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843c7","contributors":{"authors":[{"text":"Britton, L. J.","contributorId":39788,"corporation":false,"usgs":true,"family":"Britton","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":193246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferreira, R. F.","contributorId":80690,"corporation":false,"usgs":true,"family":"Ferreira","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":193248,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1046,"text":"wsp2039A - 1975 - Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River","interactions":[],"lastModifiedDate":"2017-09-03T14:21:30","indexId":"wsp2039A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2039","chapter":"A","title":"Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River","docAbstract":"<p>The major tributaries to Flaming Gorge Reservoir contribute an average of about 97 percent of the total streamflow and 82 percent of the total load of dissolved solids. The Green River is the largest tributary, and for the 1957-72 water years it contributed 81 percent of the total streamflow and 70 percent of the total load of dissolved solids. The principal constituents in the tributary streamflow are calcium and sulfate during periods of lowest flow and calcium and bicarbonate during periods of highest flow.</p><p>Flaming Gorge Dam was closed in November 1962, and the most significant load changes of chemical constituents due to the net effect of inflow, outflow, leaching, and chemical precipitation in the reservoir have been load changes of sulfate and bicarbonate. The average increase of dissolved load of sulfate in the reservoir for the 1969-72 water years was 110,000 tons (99,790 t) per year, which was 40,000 tons (36,287 t) per year less than for the 1963-66 water years. The average decrease of dissolved load of bicarbonate in the reservoir for 1969-72 was 40,000 tons (36,287 t) per year, which was the same as the decrease for 1963-66.</p><p>Anaerobic conditions were observed in the deep, uncirculated part of the reservoir near the dam during the 1971 and 1972 water years, and anaerobic or near-anaerobic conditions were observed near the confluence of the Blacks Fork and Green River during the summers of 1971 and 1972.</p><p>The water in Flaming Gorge Reservoir is in three distinct layers, and the upper two layers (the epilimnion and the metalimnion) mixed twice during each of the 1971-72 water years. The two circulation periods were in the spring and fall. The water in the deepest layer (the hypolimnion) did not mix with the waters of the upper zones because the density difference was too great and because the deep, narrow shape of the basin probably inhibits mixing.</p><p>The depletion of flow in the Green River downstream from Flaming Gorge Dam between closure of the dam and the end of the 1972 water year was 4,500,000 acre-feet (5,550.8 hm<sup>3</sup>). Of this total, water stored in the reservoir accounted for 3,500,000 acre-feet (4,317.2 hm<sup>3</sup>), evaporation consumed 700,000 acre-feet (863.4 hm<sup>3</sup>), and 300,000 acre-feet (370.0 hm<sup>3</sup>) went into bank storage.</p><p>The net load of dissolved solids added to the river system during the 1963-72 water years, due to leaching and chemical precipitation, was 1,730,000 tons (1,569,421 t). The leaching rate was 200,000 tons (181,436 t) per year for 1963-68,115,000 tons (104,326 t) per year for 1969-70 and 150,000 tons (136,077 t) per year for 1971-72. It appears that the leaching rates should decrease in the future since the reservoir level in 1972 was near maximum pool level.</p><p>The most significant increase in concentration of the chemical constituents in the water below the reservoir involved the sulfate ion, which increased from about 115 milligrams per litre (42 percent of the anions) in 1957 to about 200 milligrams per litre (54 percent), in 1972. But the highest concentration, about 290 milligrams per litre (58 percent), occurred in 1963, immediately after closure of the dam.</p><p>Prior to closure of the dam, the average monthly temperature of the Green River below the damsite ranged from 0<span class=\"_Tgc\">°</span>C to 19.5<span class=\"_Tgc\">°</span>C as compared to 3.5<span class=\"_Tgc\">°</span>C to 10.0<span class=\"_Tgc\">°</span>C after closure.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2039A","usgsCitation":"Bolke, E., and Waddell, K.M., 1975, Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River: U.S. Geological Survey Water Supply Paper 2039, Report: iv, 26 p.; 1 Plate: 42.70 in. x 24.66 in., https://doi.org/10.3133/wsp2039A.","productDescription":"Report: iv, 26 p.; 1 Plate: 42.70 in. x 24.66 in.","numberOfPages":"31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2039a/report-thumb.jpg"},{"id":25710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2039a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":246958,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2039a/plate-1.pdf","size":"5519","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Flaming Gorge Dam","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ce4b07f02db50b473","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":143087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8948,"text":"ofr75413 - 1975 - Land-surface subsidence at Seabrook, Texas","interactions":[],"lastModifiedDate":"2017-06-14T14:44:53","indexId":"ofr75413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-413","title":"Land-surface subsidence at Seabrook, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75413","usgsCitation":"Gabrysch, R., and Bonnet, C., 1975, Land-surface subsidence at Seabrook, Texas: U.S. Geological Survey Open-File Report 75-413, 51 leaves, https://doi.org/10.3133/ofr75413.","productDescription":"51 leaves","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Seabrook","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.04444122314453,\n              29.53791790738083\n            ],\n            [\n              -95.04444122314453,\n              29.589132141849095\n            ],\n            [\n              -94.99465942382811,\n              29.589132141849095\n            ],\n            [\n              -94.99465942382811,\n              29.53791790738083\n            ],\n            [\n              -95.04444122314453,\n              29.53791790738083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adec7","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":158607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":158606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1215,"text":"wsp2023 - 1975 - Selenium in waters in and adjacent to the Kendrick Project, Natrona County, Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:18:25","indexId":"wsp2023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2023","title":"Selenium in waters in and adjacent to the Kendrick Project, Natrona County, Wyoming","docAbstract":"Selenium in concentrations exceeding the maximum limit, 0.01 milligrams per liter or 10 micrograms per liter, recommended by the U.S. Public Health Service in 'Drinking-Water Standards, 1962,' Public Health Pub. 956, is present in waters in areas near Casper, Wyo. Some streams containing selenium flow into the North Platte River upstream from several municipalities that obtain water from the river and the alluvium along the river. \r\n\r\nThe area of this investigation includes about 725 square miles in Natrona County in central Wyoming. Study effort was most intensive within the area bounded by the North Platte River, Casper Creek, and Casper Canal, the approximate boundaries of the Kendrick irrigation project. \r\n\r\nGeologic formations in the area contain selenium that may have been derived from deposits of seleniferous material or from volcanic emanations brought down by rain. Formations older than Cretaceous age were not considered as important sources of selenium in waters of the area, because no irrigation water is applied to areas underlain by these rocks. The selenium concentration in 82 samples of Cretaceous rocks ranged from less than 10 to 4,200 ?g/kg (micrograms per kilogram of sample); no correlation was found between selenium concentration and the depth at which the sample was collected. Of four samples of Tertiary rocks analyzed, three contained no selenium and one had a selenium concentration of 40 ?g/kg. The selenium concentration in 93 samples of Quaternary rocks ranged from less than 10 to 52.0 ?g/kg, and the highest selenium concentration was generally found at depths less than 4 feet. No geologic formation has consistently high concentrations of selenium, but high concentrations were found at points throughout the study area. Probably the rocks in any locality could be the source of selenium in the water in the surrounding vicinity. \r\n\r\nThe selenium concentration in water from some wells fluctuates widely. It is concluded that the selenium concentrations in the ground water in these areas have not reached a state of equilibrium in the aquifer. It is possible that such nonequilibrium conditions exist in aquifers throughout much of the area. If so, statements in this report concerning- trends of selenium concentration in ground water are somewhat speculative.Poison Spring Creek, Poison Spider Creek, Oregon Trail Drain, and Casper Creek are the principal tributaries that contribute selenium to the North Platte River. The selenium load, expressed in pounds per day, in Poison Spring Creek and Poison Spider Creek decreased slightly during the first year of sampling and increased slightly during the second year of sampling. The selenium load in Oregon Trail Drain is greatest in late winter and early spring during the period of low flow; the selenium load in Casper Creek varies, but shows no correlation with season and little correlation with stream discharge. The North Platte River above and below the irrigation project had consistently low selenium concentrations, 10 ?g/l (micrograms per liter) or less, in the period April 1968 through June 1969. The total selenium load contributed to the North Platte River from tributaries in the study area is almost undetectable after mixing with the river water. \r\n\r\nFrom the fall of 1968 .to the spring of 1969, results of water sampling in areas influenced by irrigation show that the selenium concentration increased at 29 percent of the locations (average net increase of 64 ?g/l), decreased at 34 percent of the locations (average net decrease of 80 ?g/l), and had little (10 ?g/l or .less) or no change at 37 percent of the locations. \r\n\r\nAs a comparison, results of water sampling in areas not influenced by irrigation showed that the selenium concentration increased at 2 percent of the locations (average net increase of 30 ?g/l), decreased at 26 percent of the locations (average net decrease of 30?g/l), and had little or no change at 72 percent of the locations. It is not possible to","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2023","usgsCitation":"Crist, M.A., 1975, Selenium in waters in and adjacent to the Kendrick Project, Natrona County, Wyoming: U.S. Geological Survey Water Supply Paper 2023, iv, 39 p. :ill., maps (3 fold. col. in pocket) ;23 cm., https://doi.org/10.3133/wsp2023.","productDescription":"iv, 39 p. :ill., maps (3 fold. col. in pocket) ;23 cm.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":26111,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2023/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26112,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2023/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2023/report-thumb.jpg"},{"id":26110,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7c19","contributors":{"authors":[{"text":"Crist, Marvin A.","contributorId":63376,"corporation":false,"usgs":true,"family":"Crist","given":"Marvin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143382,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43989,"text":"ofr75558 - 1975 - Time-of-travel of solutes in the Trinity River basin, Texas, September 1973 and July-August 1974","interactions":[],"lastModifiedDate":"2016-08-19T10:50:49","indexId":"ofr75558","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-558","title":"Time-of-travel of solutes in the Trinity River basin, Texas, September 1973 and July-August 1974","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers and the Trinity River Authority of Texas, conducted timee-of-travel studies in the Trinity River basin during a period of low flow September 19-23, 1973, and during a period of moderate flow July 23-August 1, 1974. &nbsp;The purpose of these two studies was to provide data that could be used by the Trinity River Authority as part of the basic input to a mathematical water-quality model of the river. The model is being developed as part of a comprehensive water-quality management plan for the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75558","usgsCitation":"Ollman, R., 1975, Time-of-travel of solutes in the Trinity River basin, Texas, September 1973 and July-August 1974: U.S. Geological Survey Open-File Report 75-558, 3 Plates: 15.97 x 21.44 inches or smaller, https://doi.org/10.3133/ofr75558.","productDescription":"3 Plates: 15.97 x 21.44 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":168835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr75558.PNG"},{"id":326943,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0558/plate-2.pdf"},{"id":326942,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0558/plate-1.pdf"},{"id":326944,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0558/plate-3.pdf"}],"country":"United States","state":"Texas","otherGeospatial":"Trinity River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.20703125,\n              29.267232865200878\n            ],\n            [\n              -97.20703125,\n              33.137551192346145\n            ],\n            [\n              -94.54833984375,\n              33.137551192346145\n            ],\n            [\n              -94.54833984375,\n              29.267232865200878\n            ],\n            [\n              -97.20703125,\n              29.267232865200878\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b53f","contributors":{"authors":[{"text":"Ollman, R.H.","contributorId":88806,"corporation":false,"usgs":true,"family":"Ollman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":228944,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15558,"text":"ofr75104 - 1975 - Ground-water availability in the Belcourt area, Rolette County, North Dakota","interactions":[],"lastModifiedDate":"2018-03-12T16:01:40","indexId":"ofr75104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-104","title":"Ground-water availability in the Belcourt area, Rolette County, North Dakota","docAbstract":"<p>Test drilling and geologic data indicate that there are two potential aquifers in the Belcourt, N. Dak. area capable of supplying a sufficient quantity of ground water for the city of Belcourt. &nbsp;The Fox Hills aquifer, located about 3 miles (4.8 kilometres) west of Belcourt, could yield a sufficient quantity, as much as 500,000 gallons per day (1,900 cubic metres per day), of ground water for Belcourt, but the quality is unsuitable for a public supply. &nbsp;The Shell Valley aquifer, located about 5 miles (8 kilometres) southwest of Belcourt, appears to contain the quantity and quality of ground water required for the city of Belcourt municipal supply.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Bismarck, ND","doi":"10.3133/ofr75104","collaboration":"Prepared in cooperation with the U.S. Public Health Service","usgsCitation":"Randich, P., 1975, Ground-water availability in the Belcourt area, Rolette County, North Dakota: U.S. Geological Survey Open-File Report 75-104, Report: iv, 36 p.; 2 Plates: 31.93 x 31.27 inches and 33.24 x 17.50 inches, https://doi.org/10.3133/ofr75104.","productDescription":"Report: iv, 36 p.; 2 Plates: 31.93 x 31.27 inches and 33.24 x 17.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":148573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr75104.jpg"},{"id":310407,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0104/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310408,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0104/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":310406,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Rolette County","city":"Belcourt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.80083465576172,\n              48.805167591409095\n            ],\n            [\n              -99.80083465576172,\n              48.86460183609278\n            ],\n            [\n              -99.69938278198241,\n              48.86460183609278\n            ],\n            [\n              -99.69938278198241,\n              48.805167591409095\n            ],\n            [\n              -99.80083465576172,\n              48.805167591409095\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d362","contributors":{"authors":[{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":171330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56528,"text":"wdrMO741 - 1975 - Water resources data for Missouri, water year 1974","interactions":[],"lastModifiedDate":"2025-08-19T13:58:19.763343","indexId":"wdrMO741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-74-1","title":"Water resources data for Missouri, water year 1974","docAbstract":"<p>Water resources data for the 1974 water year for Missouri including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included for 144 gaging stations of which 137 are streamflow discharge stations, and 7 are reservoir or lake stations; also included are records for 105 crest-stage partial-record stations, and miscellaneous sites. Locations of gaging stations are shown in figure1. In Part 2, water-quality data on chemical, physical, and biological characteristics of surface water were collected from designated sampling sites at predetermined intervals such as once daily, weekly, monthly, or less frequently, and at some sites data were recorded on punched paper tape at 15-, 30-, or 60-minute intervals. Records are given for 108 sampling stations of which 53 are continuous record stations, 30 are partial-record stations, and 25 are miscellaneous sampling sites. Locations of water-quality stations are shown in figure 1. A few pertinent stations in bordering states are also included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Anthony Homyk, district chief. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Missouri.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMO741","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for Missouri, water year 1974: U.S. Geological Survey Water Data Report MO-74-1, xii, 372 p., https://doi.org/10.3133/wdrMO741.","productDescription":"xii, 372 p.","costCenters":[],"links":[{"id":181666,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1974/mo-74-1/report-thumb.jpg"},{"id":494299,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/mo-74-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":56450,"text":"wdrAR742 - 1975 - Water resources data for Arkansas, water year 1974; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrAR742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-74-2","title":"Water resources data for Arkansas, water year 1974; Part 2, Water quality records","language":"ENGLISH","doi":"10.3133/wdrAR742","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for Arkansas, water year 1974; Part 2, Water quality records: U.S. Geological Survey Water Data Report AR-74-2, 253 p., https://doi.org/10.3133/wdrAR742.","productDescription":"253 p.","costCenters":[],"links":[{"id":185116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ccc","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":532631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65007,"text":"i856B - 1975 - Lakes in the greater Denver area, Front Range urban corridor, Colorado","interactions":[],"lastModifiedDate":"2021-10-13T22:16:02.762796","indexId":"i856B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"856","chapter":"B","title":"Lakes in the greater Denver area, Front Range urban corridor, Colorado","docAbstract":"<p>The many lakes in Colorado's semiarid&nbsp;<span>Front Range Urban Corridor have an especially high value. In the past they were used primarily to store water for irrigation and domestic uses. Some were used for recreation. Today, rapid suburban development in the&nbsp;Front Range Urban Corridor is accompanied by a shift of the principal use of many lakes to recreation and to centers of real estate developments. These same lakes are threatened with a general deterioration of chemical and biological quality caused by heavy use and development of the surrounding area.&nbsp;</span></p>\n<p>The purpose of this report is to present the results of an inventory of the lakes in the central one-third of the Colorado&nbsp;Front Range Urban Corridor. This inventory provides information that might be helpful in planning the best and most beneficial use of lakes in an area of rapid population growth. The report includes data on lake size and water quality. Size data are included on most of the lakes of 2 hectares (20,000 m<sup>2</sup><span>,&nbsp;</span>or about 5 acres) or greater, and water-quality data are provided on most lakes larger than 10 hectares (about 25 acres). Bodies of water resulting form excavation of gravel (borrow pits) were generally not included in the inventory.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i856B","usgsCitation":"Danielson, T.W., 1975, Lakes in the greater Denver area, Front Range urban corridor, Colorado: U.S. Geological Survey IMAP 856, 1 Plate: 36.07 x 34.48 inches, https://doi.org/10.3133/i856B.","productDescription":"1 Plate: 36.07 x 34.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":390510,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9739.htm"},{"id":254878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0856b/report-thumb.jpg"},{"id":254877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0856b/report.pdf","linkFileType":{"id":1,"text":"pdf"},"description":"Cover sheet"},{"id":254876,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0856b/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"}],"country":"United States","state":"Colorado","county":"Denver","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.2984619140625,\n              39.51675478434244\n            ],\n            [\n              -104.6722412109375,\n              39.51675478434244\n            ],\n            [\n              -104.6722412109375,\n              40.019201307686785\n            ],\n            [\n              -105.2984619140625,\n              40.019201307686785\n            ],\n            [\n              -105.2984619140625,\n              39.51675478434244\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b425e","contributors":{"authors":[{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":272499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36963,"text":"fwsobs76_10 - 1975 - A selected annotated bibliography on fish and wildlife implications of Missouri water allocation","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"fwsobs76_10","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"76/10","title":"A selected annotated bibliography on fish and wildlife implications of Missouri water allocation","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Cochran, A., 1975, A selected annotated bibliography on fish and wildlife implications of Missouri water allocation: FWS/OBS 76/10, 71 p.","productDescription":"71 p.","costCenters":[],"links":[{"id":193064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6571","contributors":{"authors":[{"text":"Cochran, A.","contributorId":25254,"corporation":false,"usgs":true,"family":"Cochran","given":"A.","email":"","affiliations":[],"preferred":false,"id":217250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41589,"text":"ofr75184 - 1975 - Aeromagnetic map of Santa Fe and vicinity, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"ofr75184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-184","title":"Aeromagnetic map of Santa Fe and vicinity, New Mexico","language":"ENGLISH","doi":"10.3133/ofr75184","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Aeromagnetic map of Santa Fe and vicinity, New Mexico: U.S. Geological Survey Open-File Report 75-184, 1 map., https://doi.org/10.3133/ofr75184.","productDescription":"1 map.","costCenters":[],"links":[{"id":173050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79327,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0184/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69811e","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":530485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12957,"text":"ofr75484 - 1975 - Water availability in Bibb County, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr75484","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-484","title":"Water availability in Bibb County, Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75484","usgsCitation":"Causey, L.V., Willmon, J., and Ellard, J., 1975, Water availability in Bibb County, Alabama: U.S. Geological Survey Open-File Report 75-484, 21 leaves :ill., col. maps ;29 cm.; (40 p. - PGS), https://doi.org/10.3133/ofr75484.","productDescription":"21 leaves :ill., col. maps ;29 cm.; (40 p. - PGS)","costCenters":[],"links":[{"id":146961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa32a","contributors":{"authors":[{"text":"Causey, Lawson V.","contributorId":33714,"corporation":false,"usgs":true,"family":"Causey","given":"Lawson","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":167034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willmon, J.R.","contributorId":102894,"corporation":false,"usgs":true,"family":"Willmon","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":167036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellard, Jesse S.","contributorId":90315,"corporation":false,"usgs":true,"family":"Ellard","given":"Jesse S.","affiliations":[],"preferred":false,"id":167035,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66111,"text":"i856C - 1975 - Map showing availability of hydrologic data published by the U.S. Environmental Data Service and by the U.S. Geological Survey and cooperating agencies, greater Denver area, Front Range Urban Corridor, Colorado","interactions":[],"lastModifiedDate":"2021-10-27T19:22:59.797259","indexId":"i856C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"856","chapter":"C","title":"Map showing availability of hydrologic data published by the U.S. Environmental Data Service and by the U.S. Geological Survey and cooperating agencies, greater Denver area, Front Range Urban Corridor, Colorado","docAbstract":"<p>What is the rainfall of this region? What areas are prone to periodic flooding? What is the water supply? What is the chemical quality of the ground water and water in the streams? How deep is the water table? Which streams are gaged, and where? These and similar questions are being asked regularly by land and resource developers, urban planners, industrial consultants, and governmental resource managers. This map provides the first step toward answering these questions. It shows by symbols and color the hydrologic data published as of January 1974 for the Greater Denver area by the U.S. Environmental Data Service and by the U.S. Geological Survey and cooperating agencies, and the points or areas where these data have been collected. The sources of the data are given in both the following discussion and the references.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i856C","usgsCitation":"Hampton, E.R., 1975, Map showing availability of hydrologic data published by the U.S. Environmental Data Service and by the U.S. Geological Survey and cooperating agencies, greater Denver area, Front Range Urban Corridor, Colorado: U.S. Geological Survey IMAP 856, 1 Plate: 33.15 x 36.48 inches, https://doi.org/10.3133/i856C.","productDescription":"1 Plate: 33.15 x 36.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":391029,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9740.htm"},{"id":255605,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0856c/report.pdf","text":"Cover sheet","linkFileType":{"id":1,"text":"pdf"},"description":"Cover sheet"},{"id":255604,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0856c/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"},{"id":255606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0856c/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.36749999999999,39.3675 ], [ -105.36749999999999,40 ], [ -104.61749999999999,40 ], [ -104.61749999999999,39.3675 ], [ -105.36749999999999,39.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659732","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":273988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66119,"text":"i933 - 1975 - Bedrock topography of northeast Iowa","interactions":[{"subject":{"id":42247,"text":"ofr7588 - 1975 - Bedrock topography of northeast Iowa","indexId":"ofr7588","publicationYear":"1975","noYear":false,"title":"Bedrock topography of northeast Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":66119,"text":"i933 - 1975 - Bedrock topography of northeast Iowa","indexId":"i933","publicationYear":"1975","noYear":false,"title":"Bedrock topography of northeast Iowa"},"id":1}],"lastModifiedDate":"2016-08-23T09:53:35","indexId":"i933","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"933","title":"Bedrock topography of northeast Iowa","docAbstract":"<p>The bedrock in Iowa (Hershey, 1969) is generally overlain by deposits of glacial drift and alluvium, which range in thickness from less than 1 foot (0.3 m) to more than 400 ft (18 m), respectively. 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,{"id":64568,"text":"i921A - 1975 - Photomosaic base map of the Willamette River basin, Oregon: A tool for land and water-resource planning","interactions":[],"lastModifiedDate":"2025-08-13T20:15:34.212611","indexId":"i921A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"921","chapter":"A","title":"Photomosaic base map of the Willamette River basin, Oregon: A tool for land and water-resource planning","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i921A","usgsCitation":"Vickers, S.D., Brown, W., Jurado, A., and Rickert, D.A., 1975, Photomosaic base map of the Willamette River basin, Oregon: A tool for land and water-resource planning: U.S. Geological Survey IMAP 921, 4 Plates: 56.26 × 23.36 inches or smaller, https://doi.org/10.3133/i921A.","productDescription":"4 Plates: 56.26 × 23.36 inches or smaller","costCenters":[],"links":[{"id":255027,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0921a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255028,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0921a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255029,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0921a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255030,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0921a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0921a/report-thumb.jpg"},{"id":393148,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9819.htm"},{"id":255031,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0921a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"130000","country":"United States","state":"Oregon","otherGeospatial":"Willamette River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.789,\n              46\n            ],\n            [\n              -123.789,\n              43.25\n            ],\n            [\n              -121.546,\n              43.25\n            ],\n            [\n              -121.546,\n              46\n            ],\n            [\n              -123.789,\n              46\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685dd2","contributors":{"authors":[{"text":"Vickers, S. D.","contributorId":90391,"corporation":false,"usgs":true,"family":"Vickers","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":271452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, W. M.","contributorId":106138,"corporation":false,"usgs":true,"family":"Brown","given":"W. M.","affiliations":[],"preferred":false,"id":271453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jurado, Antonio","contributorId":73264,"corporation":false,"usgs":true,"family":"Jurado","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":271451,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rickert, D. A.","contributorId":53773,"corporation":false,"usgs":true,"family":"Rickert","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":271450,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":69549,"text":"hu49 - 1975 - Hydrologic Unit Map-1974, State of Wisconsin","interactions":[],"lastModifiedDate":"2023-12-19T22:33:36.894261","indexId":"hu49","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"49","subseriesTitle":"Wisconsin 1974","title":"Hydrologic Unit Map-1974, State of Wisconsin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu49","isbn":"607768053","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Hydrologic Unit Map-1974, State of Wisconsin: U.S. Geological Survey Hydrologic Unit 49, 1 Plate: 43.70 x 45.88 inches, https://doi.org/10.3133/hu49.","productDescription":"1 Plate: 43.70 x 45.88 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,{"id":12495,"text":"ofr75325 - 1975 - A water-quality assessment of the Anderson River watershed, Crawford, Dubois, Perry, and Spencer counties, Indiana","interactions":[],"lastModifiedDate":"2016-04-29T12:35:32","indexId":"ofr75325","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-325","title":"A water-quality assessment of the Anderson River watershed, Crawford, Dubois, Perry, and Spencer counties, Indiana","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75325","usgsCitation":"Ayers, M.A., and Shampine, W.J., 1975, A water-quality assessment of the Anderson River watershed, Crawford, Dubois, Perry, and Spencer counties, Indiana: U.S. Geological 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M. A.","contributorId":41417,"corporation":false,"usgs":true,"family":"Ayers","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":166229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shampine, William J.","contributorId":89891,"corporation":false,"usgs":true,"family":"Shampine","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":166230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6073,"text":"pp878 - 1975 - Evaluation of ground-water degradation resulting from waste disposal to alluvium near Barstow, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:54","indexId":"pp878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"878","title":"Evaluation of ground-water degradation resulting from waste disposal to alluvium near Barstow, California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp878","usgsCitation":"Hughes, J.L., 1975, Evaluation of ground-water degradation resulting from waste disposal to alluvium near Barstow, California: U.S. Geological Survey Professional Paper 878, 33 p., https://doi.org/10.3133/pp878.","productDescription":"33 p.","costCenters":[],"links":[{"id":118185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0878/report-thumb.jpg"},{"id":33104,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0878/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fadd6","contributors":{"authors":[{"text":"Hughes, Jerry L.","contributorId":19944,"corporation":false,"usgs":true,"family":"Hughes","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65855,"text":"i940 - 1975 - Shaded relief map of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:12","indexId":"i940","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"940","subseriesTitle":"NONE","title":"Shaded relief map of Mars","language":"ENGLISH","doi":"10.3133/i940","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Shaded relief map of Mars: U.S. Geological Survey IMAP 940, 1 map :col. ;41 x 85 cm. on sheet 104 x 99 cm. fold. in envelope 30 x 24 cm.; Reprinted 1977., https://doi.org/10.3133/i940.","productDescription":"1 map :col. ;41 x 85 cm. on sheet 104 x 99 cm. fold. in envelope 30 x 24 cm.; Reprinted 1977.","costCenters":[],"links":[{"id":189031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260809,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0940/plate-1.pdf"}],"scale":"2549000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a53fc","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":534210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15874,"text":"ofr75478 - 1975 - Water availability of Monroe County, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr75478","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-478","title":"Water availability of Monroe County, Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75478","usgsCitation":"Scott, J.C., Davis, M.E., McCain, J.F., and Whitman, H.M., 1975, Water availability of Monroe County, Alabama: U.S. Geological Survey Open-File Report 75-478, 30 leaves :folded ill. (some col.), folded col. maps ;30 cm.; (65 p. - PGS), https://doi.org/10.3133/ofr75478.","productDescription":"30 leaves :folded ill. (some col.), folded col. maps ;30 cm.; (65 p. - PGS)","costCenters":[],"links":[{"id":148378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa2dd","contributors":{"authors":[{"text":"Scott, John C.","contributorId":21963,"corporation":false,"usgs":true,"family":"Scott","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":171868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Marvin E.","contributorId":36553,"corporation":false,"usgs":true,"family":"Davis","given":"Marvin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171869,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCain, Jerald F.","contributorId":104039,"corporation":false,"usgs":true,"family":"McCain","given":"Jerald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":171871,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitman, Harry M.","contributorId":66703,"corporation":false,"usgs":true,"family":"Whitman","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":171870,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":15254,"text":"ofr7556 - 1975 - Preliminary hydrogeologic appraisal of selected hydrothermal systems in northern and central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr7556","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-56","title":"Preliminary hydrogeologic appraisal of selected hydrothermal systems in northern and central Nevada","docAbstract":"Several hydrothermal systems in northern and central Nevada were explored in a hydrogeologic reconnaissance. The systems studied comprise those at Stillwater and Soda Lakes-Upsal Hogback in the Carson Desert, Gerlach, Fly Ranch-Granite Range, and Double Hot Springs in the Black Rock Desert, Brady's Hot Springs, Leach Hot Springs in Grass Valley, Buffalo Valley Hot Springs, and Sulphur Hot Springs in Ruby Valley. \r\n\r\nThe investigation focused on (1) delineating of areas of high heat flow associated with rising thermal ground water, (2) determining the nature of the discharge parts of the hydrothermal systems, (3) estimating heat discharge from the systems, (4) estimating water discharge from the systems, (5) obtaining rough estimates of, conductive heat flow outside areas of hydrothermal discharge, and (6) evaluating several investigative techniques that would yield the required information quickly and at relatively low cost. The most useful techniques were shallow test drilling to obtain geologic, hydraulic, and thermal data and hydrogeologic mapping of the discharge areas. \r\n\r\nThe systems studied are in the north-central part of the Basin and Range province. Exposed volcanic rocks of latest Tertiary and Quaternary age are chiefly basaltic. Basaltic terranes are generally regarded as less favorable for geothermal resources than terranes that contain large volumes of young volcanic mocks of felsic to intermediate composition. Most of the known hydrothermal systems are associated with Basin and Range faults which are caused by crustal extension across the province. An area of high heat flow centered at Battle Mountain and possibly other areas of high heat flow may be related to crustal heat sources. However, some of the hydrothermal systems studied appear to be related to deep circulation of meteoric water in areas of 'normal' regional heat flow rather than to shallow-crustal heat sources. \r\n\r\nDischarge temperatures of thermal springs in the region range from slightly above mean annual air temperature (8?-12?C at most places) to boiling or slightly hotter. Geochemical data indicate that, in the major systems, subsurface temperatures at which thermal waters equilibrate with reservoir rocks range from 150? to more than 200?C. These data also indicate that the major systems are of the hot-water type rather than the vapor-dominated type. Depths of thermal-water circulation probably range from 2 to 6 kilometres in areas of 'normal' regional heat flow (~2 heatflow units) and from 1 to 3 kilometres in areas of high heat flow (~3-4 heat-flow units) such as near Battle Mountain. \r\n\r\nMost of the heat is discharged from the hydrothermal systems studied by (1) conduction through near-surface materials heated as a consequence of thermal-water convection, (2) convection as springflow, and (3) convection as steam discharge from spring pools, vents, fumaroles, and cracks. The mate of heat discharge by radiation from warm ground and by convection as lateral ground-water outflow is believed to be small in most systems and is not estimated. \r\n\r\nEstimates of net heat discharge from the systems studied range from about 0.8 x 106 calories per second at Buffalo Valley Hot Springs to about 14 x 106 calories per second at Stillwater. These estimates represent the approximate magnitude of the excess heat discharge from the thermal areas that results from the upward convection of hot water from deep sources. Water discharges from the hydrothermal systems by springflow, evapotranspiration, steam discharge, and lateral ground-water outflow. Estimated discharges range from about 0.2 x 106cubic metres per year from the Buffalo Valley Hot Springs system to about 3 x 106 cubic metres per year from the Stillwater system. \r\n\r\nIn most of the hydrothermal systems studied and, by inference, in other similar systems in northern and central Nevada, the scale for potential .commercial development for production of electricity or for other uses may be constrained by the","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr7556","usgsCitation":"Olmsted, F.H., Glancy, P., Harrill, J., Rush, F., and Van Denburgh, A.S., 1975, Preliminary hydrogeologic appraisal of selected hydrothermal systems in northern and central Nevada: U.S. Geological Survey Open-File Report 75-56, xi, 267 p. :ill. ;27 cm.; (360 p. - PGS), https://doi.org/10.3133/ofr7556.","productDescription":"xi, 267 p. :ill. ;27 cm.; (360 p. - PGS)","costCenters":[],"links":[{"id":147396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0056/report-thumb.jpg"},{"id":44190,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672aee","contributors":{"authors":[{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glancy, P.A.","contributorId":32160,"corporation":false,"usgs":true,"family":"Glancy","given":"P.A.","affiliations":[],"preferred":false,"id":170827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harrill, J. R.","contributorId":10417,"corporation":false,"usgs":true,"family":"Harrill","given":"J. R.","affiliations":[],"preferred":false,"id":170824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rush, F. E.","contributorId":56234,"corporation":false,"usgs":true,"family":"Rush","given":"F. E.","affiliations":[],"preferred":false,"id":170828,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Denburgh, A. 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