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","language":"English","publisher":"Taylor & Francis","doi":"10.1111/j.0033-0124.1964.00028.x","usgsCitation":"Gerlach, A.C., 1964, Centennial celebration of the national academy of sciences: Professional Geographer, v. 16, no. 1, p. 28-28, https://doi.org/10.1111/j.0033-0124.1964.00028.x.","productDescription":"1 p.","startPage":"28","endPage":"28","costCenters":[],"links":[{"id":386210,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gerlach, Arch C.","contributorId":78249,"corporation":false,"usgs":true,"family":"Gerlach","given":"Arch","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34682,"text":"b1135 - 1964 - Oxidized zinc deposits of the United States","interactions":[{"subject":{"id":57012,"text":"b1135A - 1962 - Oxidized zinc deposits of the United States: Part 1. General geology","indexId":"b1135A","publicationYear":"1962","noYear":false,"chapter":"A","title":"Oxidized zinc deposits of the United States: Part 1. General geology"},"predicate":"IS_PART_OF","object":{"id":34682,"text":"b1135 - 1964 - Oxidized zinc deposits of the United States","indexId":"b1135","publicationYear":"1964","noYear":false,"title":"Oxidized zinc deposits of the United States"},"id":1},{"subject":{"id":57013,"text":"b1135B - 1963 - Oxidized zinc deposits of the United States: Part 2. Utah","indexId":"b1135B","publicationYear":"1963","noYear":false,"chapter":"B","title":"Oxidized zinc deposits of the United States: Part 2. Utah"},"predicate":"IS_PART_OF","object":{"id":34682,"text":"b1135 - 1964 - Oxidized zinc deposits of the United States","indexId":"b1135","publicationYear":"1964","noYear":false,"title":"Oxidized zinc deposits of the United States"},"id":2},{"subject":{"id":57014,"text":"b1135C - 1964 - Oxidized zinc deposits of the United States: Part 3. Colorado","indexId":"b1135C","publicationYear":"1964","noYear":false,"chapter":"C","title":"Oxidized zinc deposits of the United States: Part 3. Colorado"},"predicate":"IS_PART_OF","object":{"id":34682,"text":"b1135 - 1964 - Oxidized zinc deposits of the United States","indexId":"b1135","publicationYear":"1964","noYear":false,"title":"Oxidized zinc deposits of the United States"},"id":3}],"lastModifiedDate":"2017-08-08T15:47:07","indexId":"b1135","displayToPublicDate":"1964-01-01T11:27:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1135","title":"Oxidized zinc deposits of the United States","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1135","usgsCitation":"Heyl, A.V., and Bozion, C.N., 1964, Oxidized zinc deposits of the United States: U.S. Geological Survey Bulletin 1135, 247 p.; 16 Maps, https://doi.org/10.3133/b1135.","productDescription":"247 p.; 16 Maps","costCenters":[],"links":[{"id":289900,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1135/report-thumb.jpg"},{"id":344681,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc5ee4b0b58d96eeb5ed","contributors":{"authors":[{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":213394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bozion, C. N.","contributorId":19233,"corporation":false,"usgs":true,"family":"Bozion","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":213393,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70263594,"text":"wdrCA642 - 1964 - Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2025-02-14T15:32:39.182988","indexId":"wdrCA642","displayToPublicDate":"1964-01-01T10:32:13","publicationYear":"1964","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":"CA-64-2","title":"Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer, Surface Water Branch.
Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in parts 9, 10, and 11 of that series.
Beginning with the 1961 water year, streamflow records and related data are being released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic data reports is limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCA642","collaboration":"Prepared in cooperation with the State of California and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of California, 1964; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-64-2, xiv, 499-991 p., https://doi.org/10.3133/wdrCA642.","productDescription":"xiv, 499-991 p.","costCenters":[],"links":[{"id":482103,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":482102,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/ca-64-2/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley, Northern Great 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L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":295325,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":81404,"text":"81404 - 1964 - Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"81404","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"575","title":"Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"703/FH","usgsCitation":"Putz, R., and Bowen, J., 1964, Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species: Fishery Leaflet 575, 4 p.","productDescription":"4 p.","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":199058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689237","contributors":{"authors":[{"text":"Putz, R.E.","contributorId":42543,"corporation":false,"usgs":true,"family":"Putz","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":295330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, J.T.","contributorId":67946,"corporation":false,"usgs":true,"family":"Bowen","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":295331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013660,"text":"1013660 - 1964 - Comparison of various methods of hemoglobin determination on catfish blood","interactions":[],"lastModifiedDate":"2025-08-01T16:13:04.312016","indexId":"1013660","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"Comparison of various methods of hemoglobin determination on catfish blood","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2","usgsCitation":"Larsen, H., 1964, Comparison of various methods of hemoglobin determination on catfish blood: Progressive Fish-Culturist, v. 26, no. 1, p. 11-15, https://doi.org/10.1577/1548-8659(1964)26[11:COVMOH]2.0.CO;2.","productDescription":"5 p.","startPage":"11","endPage":"15","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130248,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa765","contributors":{"authors":[{"text":"Larsen, H.N.","contributorId":101601,"corporation":false,"usgs":true,"family":"Larsen","given":"H.N.","email":"","affiliations":[],"preferred":false,"id":318990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009991,"text":"70009991 - 1964 - Spectrophotometric determination of fluorine in silicate rocks","interactions":[],"lastModifiedDate":"2020-11-24T00:58:14.618203","indexId":"70009991","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric determination of fluorine in silicate rocks","docAbstract":"The rock powder is sintered with a sodium carbonate flux containing zinc oxide and magnesium carbonate, the sinter-cake leached with water and the resulting solution filtered. Fluorine is separated from the acidified filtrate by steam distillation and determined spectrophotometrically by means of a zirconium-SPADNS reagent. If a multiple-unit distillation apparatus is used, 12 determinations can be completed per man-day.
A new method for the determination of the fugacity of sulfur in laboratory systems consists of visual observation of the development and decomposition of a sulfide tarnish phase on silver-gold alloy (electrum) of precisely known composition. The alloy system is calibrated against pure sulfur. The method has the following advantages: simple apparatus; ability to cover a large range of fugacity of S2; ability to cover a large temperature range by permitting runs of long duration; ability to tolerate other components in the gas phase; and ease of recovery of the quenched charges for determinations of phases and compositions. Results obtained by the electrum-tarnish method are in satisfactory agreement with those obtained by other workers for the fs2 vs. T curves for the assemblage Ni(1–x)S + NiS2. The electrum-tarnish method shows promise for investigating many other reactions.
Univariant reactions studied by this method can be represented as lines forming a genetic grid in terms of the environmental parameters fs2 and T, The slopes of such lines can yield valuable thermodynamic data for the phases involved, but activity coefficients must be known for phases of variable composition.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90082-1","issn":"00167037","usgsCitation":"Barton, P.B., and Toulmin, P., 1964, The electrum-tarnish method for the determination of the fugacity of sulfur in laboratory sulfide systems: Geochimica et Cosmochimica Acta, v. 28, no. 5, p. 619-640, https://doi.org/10.1016/0016-7037(64)90082-1.","productDescription":"22 p.","startPage":"619","endPage":"640","numberOfPages":"22","costCenters":[],"links":[{"id":218902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505babc5e4b08c986b323069","contributors":{"authors":[{"text":"Barton, P. B. Jr.","contributorId":23683,"corporation":false,"usgs":true,"family":"Barton","given":"P.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toulmin, P. III","contributorId":81244,"corporation":false,"usgs":true,"family":"Toulmin","given":"P.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":359154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010816,"text":"70010816 - 1964 - Ground water in North America","interactions":[],"lastModifiedDate":"2017-03-27T12:47:37","indexId":"70010816","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in North America","docAbstract":"The fast-growing demands on this natural resource expose a need to resolve many hydrologic unknowns.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3610.1001","issn":"00368075","usgsCitation":"Thomas, H.E., and Leopold, L.B., 1964, Ground water in North America: Science, v. 143, no. 3610, p. 1001-1006, https://doi.org/10.1126/science.143.3610.1001.","productDescription":"6 p.","startPage":"1001","endPage":"1006","costCenters":[],"links":[{"id":218743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"North America","volume":"143","issue":"3610","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ad0e4b0c8380cd5b4a7","contributors":{"authors":[{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":359715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009992,"text":"70009992 - 1964 - Cenomanian (Cretaceons) Foraminifera from the Puerto Rico Trench","interactions":[],"lastModifiedDate":"2020-11-24T00:59:09.924534","indexId":"70009992","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1372,"text":"Deep-Sea Research and Oceanographic Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Cenomanian (Cretaceons) Foraminifera from the Puerto Rico Trench","docAbstract":"An assemblage of predominantly planktonic Foraminifera is discussed from rocks of Cenomanian age dredged from between 3,200 and 3,500 fm on the north slope of the Puerto Rico Trench. Thirty-three planktonic and benthonic species are described. Planomalina pulchella is new; nine species are specifically unidentifiable. Deposition is interpreted as having been at a depth of over 1,000 fm, possibly as deep as where found.
The composition of nonmarine shales of Cretaceous age that contain less than 1 per cent organic carbon is assumed to represent the inherited minor-element composition of clayey sediments delivered to the Cretaceous sea that occupied the western interior region of North America. Differences in minor-element content between these samples and samples of
(a) nonmarine carbonaceous shales (1 to 17 per cent organic carbon),
(b) nearshore marine shales (less than 1 per cent organic carbon), and
(c) offshore marine shales (as much as 8 per cent organic carbon), all of the same age, reveal certain aspects of the role played by clay minerals and organic materials in affecting the minor-element composition of the rocks.
The organic carbon in the nonmarine rocks occurs in disseminated coaly plant remains. The organic carbon in the marine rocks occurs predominantly in humic material derived from terrestrial plants. The close similarity in composition between the organic isolates from the marine samples and low-rank coal suggests that the amount of marine organic material in these rocks is small.
The minor-element content of the two kinds of nonmarine shales is the same despite the relatively large amount of organic carbon in the carbonaceous shales. The nearshore marine shales, however, contain larger median amounts of arsenic, boron, chromium, vanadium and zinc than do the nonmarine rocks; and the offshore marine shales contain even larger amounts of these elements. Cobalt, molybdenum, lead and zirconium show insignificant differences in median content between the nonmarine and marine rocks, although as much as 25 ppm molybdenum is present in some offshore marine samples. The gallium content is lower in the marine than in the nonmarine samples. Copper and selenium contents of the two kinds of nonmarine rocks and the nearshore marine samples are the same, but those of the offshore samples are larger.
In general, arsenic, chromium, copper, molybdenum, selenium, vanadium and zinc are concentrated in those offshore marine samples having the largest amounts of organic carbon, but samples with equal amounts of vanadium, for instance, may differ by a factor of 3 in their amount of organic carbon. Arsenic and molybdenum occur in some samples chiefly in syngenetic pyrite but also are present in relatively large amounts in samples that contain little pyrite.
The data on nonmarine carbonaceous shales indicate that organic matter of terrestrial origin in marine shales contributes little to the minor-element content of such rocks. It is possible that marine organic matter, even though seemingly small in amount in marine shales, contributes to the minor-element composition of the shales. In addition to any such contribution, however, the great effectiveness in sorption processes of humic materials in conjunction with clay minerals suggests that such processes must have played an important role as these materials moved from the relatively dilute solutions of the nonmarine environment to the relatively concentrated solution of sea water. The volumes of sea water sufficient to supply for sorption the amounts of most minor elements in the offshore marine samples are insignificant compared to the volumes of water with which the clay and organic matter were in contact during their transportation and sedimentation. Consequently, the chemical characteristics of the environment in which the clay minerals and organic matter accumulated and underwent diagenesis probably were the most important factors in controlling the degree to which sorption processes and the formation of syngenetic minerals affected the final composition of the rocks.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(64)90008-0","issn":"00167037","usgsCitation":"Tourtelot, H.A., 1964, Minor-element composition and organic carbon content of marine and nonmarine shales of Late Cretaceous age in the western interior of the United States: Geochimica et Cosmochimica Acta, v. 28, no. 10-11, p. 1579-1604, https://doi.org/10.1016/0016-7037(64)90008-0.","productDescription":"26 p.","startPage":"1579","endPage":"1604","numberOfPages":"26","costCenters":[],"links":[{"id":219008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"10-11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5b29e4b0c8380cd6f38b","contributors":{"authors":[{"text":"Tourtelot, H. A.","contributorId":79140,"corporation":false,"usgs":true,"family":"Tourtelot","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":358984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2354,"text":"wsp1654 - 1964 - Ground water for irrigation in the Snake River Basin in Idaho","interactions":[],"lastModifiedDate":"2023-03-24T18:32:01.922661","indexId":"wsp1654","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1654","title":"Ground water for irrigation in the Snake River Basin in Idaho","docAbstract":"The Snake River basin, in southern Idaho, upstream from the mouth of the Powder River in Oregon, includes more than 50 percent of the land area and 65 percent of the total population of the State. More than 2.5 million acres of land is irrigated ; irrigation agriculture and industry allied with agriculture are the basis of the economy of the basin. Most of the easily developed sources of surface water are fully utilized, and few storage sites remain where water could be made available to irrigate lands under present economic conditions. Because surface-water supplies have be come more difficult to obtain, use of ground water has increased greatly. At the present time (1959), about 600,000 acres of land is irrigated with ground water. Ground-water development has been concentrated in areas where large amounts of water are available beneath or adjacent to tracts of arable land and where the depth to water is not excessive under the current economy. Under these criteria, many of the most favorable areas already have been developed; however, tremendous volumes of water are still available for development. In some places, water occurs at depths considered near or beyond the limit for economic recovery, whereas in some other places, water is reasonably close to the surface but no arable land is available in the vicinity. In other parts of the basin large tracts of arable land are without available water supply. Thus the chief tasks in development of the ground-water resources include not only locating and evaluating ground-water supplies but also the planning necessary to bring the water to the land. Irrigation began in the 1860's ; at the present time more than 10 million acre feet of surface water, some of which is recirculated water, is diverted annually for irrigation of more than 2.5 million acres. Diversion of this large quantity of water has had a marked effect on the ground-water regimen. In some areas, the water table has risen more than 100 feet and the discharge of some springs has more than doubled. Large-scale development of ground water began after World War II, and it is estimated that in 1959 about 1,500,000 acre-feet of ground water was pumped for irrigation of the 600,000 acres irrigated wholly with ground water in addition to a substantial amount of ground water pumped to supplement surface-water supplies. Ground water is also the principal source of supply for municipal, industrial, and domestic use. The water regimen in the Snake River basin is greatly influenced by the geology. The rocks forming the mountains are largely consolidated rocks of low permeability; however, a fairly deep and porous subsoil has formed on them by decay and disintegration of the parent rock. Broad intermontane valleys and basins are partly filled with alluvial sand and gravel. The subsoil and alluvial materials are utilized very little as a source of water supply but are important as seasonal ground-water reservoirs because they store water during periods of high rainfall and snowmelt. Discharge from these reservoirs maintains stream flow during periods of surface runoff. Because these aquifers are fairly thin, they drain rapidly and are considerably depleted at the end of each dry cycle. The plain and plateau areas and tributary valleys, on the other hand, are underlain chiefly by rocks of high permeability and porosity. These rocks, mostly basaltic lava flows and alluvial materials, constitute a reservoir which fluctuates only slightly from season to season. Large amounts' of water are withdrawn from them for irrigation and other uses, and discharge from the Snake Plain aquifer is an important part of the total flow of the Snake River downstream from Hagerman Valley. The ultimate source of ground water in the basin is precipitation on the basin. In the mountainous areas, aquifers mostly are recharged directly by precipitation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1654","usgsCitation":"Mundorff, M.J., Crosthwaite, E., and Kilburn, C., 1964, Ground water for irrigation in the Snake River Basin in Idaho: U.S. Geological Survey Water Supply Paper 1654, vii, 224 p., https://doi.org/10.3133/wsp1654.","productDescription":"vii, 224 p.","costCenters":[],"links":[{"id":414716,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24846.htm","linkFileType":{"id":5,"text":"html"}},{"id":28283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1654/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1654/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.048,\n 45.217\n ],\n [\n -117.213,\n 45.217\n ],\n [\n -117.213,\n 42\n ],\n [\n -111.048,\n 42\n ],\n [\n -111.048,\n 45.217\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dc28","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":145068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":145069,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}