{"pageNumber":"573","pageRowStart":"14300","pageSize":"25","recordCount":16498,"records":[{"id":70011710,"text":"70011710 - 1979 - Space, time, and the third dimension (model error)","interactions":[],"lastModifiedDate":"2018-02-05T12:26:24","indexId":"70011710","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Space, time, and the third dimension (model error)","docAbstract":"<p>The space-time tradeoff of hydrologic data collection (the ability to substitute spatial coverage for temporal extension of records or vice versa) is controlled jointly by the statistical properties of the phenomena that are being measured and by the model that is used to meld the information sources. The control exerted on the space-time tradeoff by the model and its accompanying errors has seldom been studied explicitly. The technique, known as Network Analyses for Regional Information (NARI), permits such a study of the regional regression model that is used to relate streamflow parameters to the physical and climatic characteristics of the drainage basin.</p><p>The NARI technique shows that model improvement is a viable and sometimes necessary means of improving regional data collection systems. Model improvement provides an immediate increase in the accuracy of regional parameter estimation and also increases the information potential of future data collection. Model improvement, which can only be measured in a statistical sense, cannot be quantitatively estimated prior to its achievement; thus an attempt to upgrade a particular model entails a certain degree of risk on the part of the hydrologist.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR015i006p01797","usgsCitation":"Moss, M.E., 1979, Space, time, and the third dimension (model error): Water Resources Research, v. 15, no. 6, p. 1797-1800, https://doi.org/10.1029/WR015i006p01797.","productDescription":"4 p.","startPage":"1797","endPage":"1800","costCenters":[],"links":[{"id":221386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"505b940ae4b08c986b31a819","contributors":{"authors":[{"text":"Moss, Marshall E.","contributorId":6830,"corporation":false,"usgs":true,"family":"Moss","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361780,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012532,"text":"70012532 - 1979 - The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin","interactions":[],"lastModifiedDate":"2025-04-10T16:22:10.414366","indexId":"70012532","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin","docAbstract":"<p><sup>14</sup>C analyses of groundwaters from the Chalk of the London Basin are re-interpreted and the age of the groundwater is revised. Radio-isotope analyses are used to examine the flow mechanism in the aquifer. The evidence supports the view that a network of micro-fissures and larger intergranular pores in the matrix provides a significant part of the water pumped from Chalk wells and the major fissures distribute the water to the wells. Most of the matrix is fine-grained and contains a very old water. This diffuses into the micro-fissures and larger pores and is carried to the wells by the major fissures.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(79)90088-X","issn":"00221694","usgsCitation":"Downing, R., Pearson, F., and Smith, D.B., 1979, The flow mechanism in the Chalk based on radio-isotope analyses of groundwater in the London Basin: Journal of Hydrology, v. 40, no. 1-2, p. 67-83, https://doi.org/10.1016/0022-1694(79)90088-X.","productDescription":"17 p.","startPage":"67","endPage":"83","costCenters":[],"links":[{"id":221830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"England","otherGeospatial":"southeast England","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -0.2450492943921745,\n              51.789943291380695\n            ],\n            [\n              -0.2450492943921745,\n              51.5027068477811\n            ],\n            [\n              1.0281677944668104,\n              51.5027068477811\n            ],\n            [\n              1.0281677944668104,\n              51.789943291380695\n            ],\n            [\n              -0.2450492943921745,\n              51.789943291380695\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"40","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac1ae4b08c986b32328c","contributors":{"authors":[{"text":"Downing, R.A.","contributorId":25293,"corporation":false,"usgs":true,"family":"Downing","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":363836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, F.J.","contributorId":58262,"corporation":false,"usgs":true,"family":"Pearson","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":363837,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":363835,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012588,"text":"70012588 - 1979 - Uranium transport in the Walker River Basin, California and Nevada","interactions":[],"lastModifiedDate":"2025-03-05T17:23:39.748459","indexId":"70012588","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uranium transport in the Walker River Basin, California and Nevada","docAbstract":"<div class=\"u-margin-s-bottom\">During the summer of 1976 waters from tributaries, rivers, springs and wells were sampled in the Walker River Basin. Snow and sediments from selected sites were also sampled. All samples were analyzed for uranium and other elements. The resulting data provide an understanding of the transport of uranium within a closed hydrologic basin as well as providing a basis for the design of geochemical reconnaissance studies for the Basin and Range Province of the Western United States.</div><div class=\"u-margin-s-bottom\">Spring and tributary data are useful in locating areas containing anomalous concentrations of uranium. However, agricultural practices obscure the presence of known uranium deposits and render impossible the detection of other known deposits.</div><div class=\"u-margin-s-bottom\">Uranium is extremely mobile in stream waters and does not appear to sorb or precipitate. Uranium has a long residence time (2500 years) in the open waters of Walker Lake; however, once it crosses the sediment-water interface, it is reduced to the U(IV) state and is lost from solution.</div><div class=\"u-margin-s-bottom\">Over the past two million years the amount of uranium transported to the terminal point of the Walker River system may have been on the order of 4 × 10<sup>8</sup><span>&nbsp;</span><i>kg</i>. This suggests that closed basin termini are sites for significant uranium accumulations and are, therefore, potential sites of uranium ore deposits.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(79)90002-5","issn":"03756742","usgsCitation":"Benson, L.V., and Leach, D.L., 1979, Uranium transport in the Walker River Basin, California and Nevada: Journal of Geochemical Exploration, v. 11, no. 3, p. 227-248, https://doi.org/10.1016/0375-6742(79)90002-5.","productDescription":"22 p.","startPage":"227","endPage":"248","numberOfPages":"22","costCenters":[],"links":[{"id":489976,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://www.escholarship.org/uc/item/6kb8n2r2","text":"External Repository"},{"id":221959,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdd6e4b08c986b329266","contributors":{"authors":[{"text":"Benson, L. V.","contributorId":50159,"corporation":false,"usgs":true,"family":"Benson","given":"L.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":363986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363985,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001664,"text":"1001664 - 1979 - Fall foods of migrant common snipe in North Dakota","interactions":[],"lastModifiedDate":"2025-02-14T16:35:27.887348","indexId":"1001664","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Fall foods of migrant common snipe in North Dakota","docAbstract":"<p>Studies of foods consumed by common snipe (<i>Capella gallinago</i>) during fall migration (Sperry 1940, Erickson 1941, Choate in Tuck 1972, Tuck 1972) have shown that diets vary among habitats. More recently, Fogarty and Arnold (1977) expressed the need for more detailed information on snipe food habits and more refined knowledge of the snipe's range and adaptability to various food situations. There is a paucity of information on snipe feeding ecology in the prairie pothole region of North America where unstable and unpredictable hydrological conditions affect abundance and availability of aquatic foods. The objectives of  study were to (1) identify foods consumed by common snipe during fall migration in south-central North Dakota, and (2) describe changes in diet during years with different water regimes.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3800667","usgsCitation":"Fritzell, E., Swanson, G., and Meyer, M., 1979, Fall foods of migrant common snipe in North Dakota: Journal of Wildlife Management, v. 43, no. 1, p. 253-257, https://doi.org/10.2307/3800667.","productDescription":"5 p.","startPage":"253","endPage":"257","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130344,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North 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Dakota\",\"nation\":\"USA  \"}}]}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f79a1","contributors":{"authors":[{"text":"Fritzell, E.K.","contributorId":35685,"corporation":false,"usgs":true,"family":"Fritzell","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":311473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, G.A.","contributorId":49299,"corporation":false,"usgs":true,"family":"Swanson","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":311474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, M.I.","contributorId":56584,"corporation":false,"usgs":true,"family":"Meyer","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":311475,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012425,"text":"70012425 - 1979 - Disequilibrium in the 238uranium series in samples from Yeelirrie, Western Australia","interactions":[],"lastModifiedDate":"2025-03-05T17:21:49.889322","indexId":"70012425","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Disequilibrium in the <sup>238</sup>uranium series in samples from Yeelirrie, Western Australia","title":"Disequilibrium in the 238uranium series in samples from Yeelirrie, Western Australia","docAbstract":"<div class=\"u-margin-s-bottom\">Uranium-series disequilibrium studies carried out on samples from the Yeelirrie uranium deposit, Western Australia, indicate that uranium and radium have been migrating within the deposit during recent times, and are actually being removed from the deposit. Samples collected for<span>&nbsp;</span><sup>230</sup>Th/<sup>234</sup>U age dating were found to be substantially out of equilibrium, with<span>&nbsp;</span><sup>230</sup>Th/<sup>234</sup>U activity ratios ranging from 0.750 to 1.345. This can be explained by a dynamic hydrologic system in which there has been, and continues to be, uranium migration caused by leaching in this arid, oxidizing environment, and a fluctuating water table.</div><div class=\"u-margin-s-bottom\">Recent, extensive<span>&nbsp;</span><sup>226</sup>Ra migration (<sup>226</sup>Ra/<sup>230</sup>Th activity ratios range from 0.53 to 1.30), and a very low emanation factor (<i>E</i>) of<span>&nbsp;</span><sup>222</sup>Rn limit the quantitative application of radon exploration techniques in this environment.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(79)90063-3","usgsCitation":"Lively, R., Harmon, R., Levinson, A.A., and Bland, C., 1979, Disequilibrium in the 238uranium series in samples from Yeelirrie, Western Australia: Journal of Geochemical Exploration, v. 12, no. C, p. 57-65, https://doi.org/10.1016/0375-6742(79)90063-3.","productDescription":"9 p.","startPage":"57","endPage":"65","numberOfPages":"9","costCenters":[],"links":[{"id":222076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0212e4b0c8380cd4fe7d","contributors":{"authors":[{"text":"Lively, R.S.","contributorId":70927,"corporation":false,"usgs":true,"family":"Lively","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":363546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harmon, R.S.","contributorId":6585,"corporation":false,"usgs":true,"family":"Harmon","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":363543,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Levinson, A. A.","contributorId":55283,"corporation":false,"usgs":true,"family":"Levinson","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bland, C.J.","contributorId":36423,"corporation":false,"usgs":true,"family":"Bland","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":363544,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012455,"text":"70012455 - 1979 - Major geochemical processes in the evolution of carbonate-Aquifer systems","interactions":[],"lastModifiedDate":"2019-12-06T07:13:19","indexId":"70012455","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Major geochemical processes in the evolution of carbonate-Aquifer systems","docAbstract":"<p>As a result of recent advances by carbonate petrologists and geochemists, hydrologists are provided with new insights into the origin and explanation of many aquifer characteristics and hydrologic phenomena. Some major advances include the recognition that: (1) most carbonate sediments are of biological origin; (2) they have a strong bimodal size-distribution; and (3) they originate in warm shallow seas. Although near-surface ocean water is oversaturated with respect to calcite, aragonite, dolomite and magnesite, the magnesium-hydration barrier effectively prevents either the organic or inorganic formation of dolomite and magnesite. Therefore, calcareous plants and animals produce only calcite and aragonite in hard parts of their bodies. Most carbonate aquifers that are composed of sand-size material have a high initial porosity; the sand grains that formed these aquifers originated primarily as small shells, broken shell fragments of larger invertebrates, or as chemically precipitated oolites. Carbonate rocks that originated as fine-grained muds were initially composed primarily of aragonite needles precipitated by algae and have extremely low permeability that requires fracturing and dissolution to develop into aquifers. Upon first emergence, most sand beds and reefs are good aquifers; on the other hand, the clay-sized carbonate material initially has high porosity but low permeability, a poor aquifer property. Without early fracture development in response to influences of tectonic activity these calcilutites would not begin to develop into aquifers. As a result of selective dissolution, inversion of the metastable aragonite to calcite, and recrystallization, the porosity is collected into larger void spaces, which may not change the overall porosity, but greatly increases permeability. Another major process which redistributes porosity and permeability in carbonates is dolomitization, which occurs in a variety of environments. These environments include back-reefs, where reflux dolomites may form, highly alkaline, on-shore and continental lakes, and sabkha flats; these dolomites are typically associated with evaporite minerals. However, these processes cannot account for most of the regionally extensive dolomites in the geologic record. A major environment of regional dolomitization is in the mixing zone (zone of dispersion) where profound changes in mineralogy and redistribution of porosity and permeability occur from the time of early emergence and continuing through the time when the rocks are well-developed aquifers. The reactions and processes, in response to mixing waters of differing chemical composition, include dissolution and precipitation of carbonate minerals in addition to dolomitization. An important control on permeability distribution in a mature aquifer system is the solution of dolomite with concomitant precipitation of calcite in response to gypsum dissolution (dedolomitization). Predictive models developed by mass-transfer calculations demonstrate the controlling reactions in aquifer systems through the constraints of mass balance and chemical equilibrium. An understanding of the origin, chemistry, mineralogy and environments of deposition and accumulation of carbonate minerals together with a comprehension of diagenetic processes that convert the sediments to rocks and geochemical, tectonic and hydrologic phenomena that create voids are important to hydrologists. With this knowledge, hydrologists are better able to predict porosity and permeability distribution in order to manage efficiently a carbonate-aquifer system.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0167-5648(09)70022-X","issn":"00221694","usgsCitation":"Hanshaw, B., and Back, W., 1979, Major geochemical processes in the evolution of carbonate-Aquifer systems: Journal of Hydrology, v. 43, no. 1-4, p. 287-312, https://doi.org/10.1016/S0167-5648(09)70022-X.","productDescription":"26 p. ","startPage":"287","endPage":"312","numberOfPages":"26","costCenters":[],"links":[{"id":222536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4c10e4b0c8380cd699a5","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":363617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Back, W.","contributorId":33839,"corporation":false,"usgs":true,"family":"Back","given":"W.","email":"","affiliations":[],"preferred":false,"id":363618,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012483,"text":"70012483 - 1979 - Geochemical and hydrologic considerations and the use of enthalpy-chloride diagrams in the prediction of underground conditions in hot-spring systems","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012483","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Geochemical and hydrologic considerations and the use of enthalpy-chloride diagrams in the prediction of underground conditions in hot-spring systems","docAbstract":"Thermal water ascending in a hot-spring system may cool by conduction of heat to the surrounding rock, by boiling, by mixing with cooler water, or by a combination of these processes. Complete or partial chemical reequilibration may occur as a result of this cooling. In spite of these complexities, in many places chemical compositions of hot-spring waters may be used to estimate underground conditions. A plot of enthalpy versus chloride is particularly useful for determining underground temperatures, salinities, and boiling and mixing relations. The utility of this approach is illustrated using hot-spring composition data from Cerro Prieto, Mexico, Orakeikorako, New Zealand, and Yellowstone National Park, Wyoming. ?? 1979.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Fournier, R., 1979, Geochemical and hydrologic considerations and the use of enthalpy-chloride diagrams in the prediction of underground conditions in hot-spring systems: Journal of Volcanology and Geothermal Research, v. 5, no. 1-2, p. 1-16.","startPage":"1","endPage":"16","numberOfPages":"16","costCenters":[],"links":[{"id":222142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a15d4e4b0c8380cd54f63","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":363724,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012589,"text":"70012589 - 1979 - International cooperation in water resources","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70012589","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1746,"text":"GeoJournal","active":true,"publicationSubtype":{"id":10}},"title":"International cooperation in water resources","docAbstract":"Advancements in hydrology proceeded slowly until the late 1800's when new ventures created a surge of interest and accomplishment. Progress waned again until the middle 20th century when an International Hydrological Decade was conceived, eventually receiving wide multinational support from governmental agencies and nongovernmental institutions. Organized by UNESCO, the Decade program was launched January 1, 1965. Participation included 107 nations, six United Nations agencies, and more than a dozen international scientific organizations. The initial program emphasized scientific research, and international cooperation; the second half of the Decade, emphasized technical assistance and technology transfer, largerly through education, training and demonstration. The success of the Decade led to the establishment of the International Hydrological Program, again under the aegis of UNESCO, to continue the work of the Decade indefinitely. The five major program activities, now involving about 90 countries and several international organizations, include: the scientific program, the promotion of education and training, the enhancement of information exchange, support of technical assistance, and the enlargement of regional cooperation. A significant amount of activity related to hydrological data networks and forecasting is carried on in an Operational Hydrology Programme by the WMO, chiefly through its Commission for Hydrology. Other international governmental organizations with a strong interest in water include the UN, the UN Development Programme, the FAO, the WHO, the International Atomic Energy Agency, the UN Environment Programme, the International Standardization Organization, and developmental institutions such as the World Bank. The specialized interests of researchers outside of the governmental structure, are met through association in various scientific and technical organizations which are world wide in scope and membership. Notwithstanding a sometimes bewildering variety of organizations, there certainly exists, for any nation, group, or individual, a demonstrated mechanism for almost any conceivable form of international cooperation in hydrology and water resources. ?? 1979 Akademische Verlagsgesellschaft.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GeoJournal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00455987","issn":"03432521","usgsCitation":"Jones, J., Beall, R., and Giusti, E., 1979, International cooperation in water resources: GeoJournal, v. 3, no. 5, p. 481-487, https://doi.org/10.1007/BF00455987.","startPage":"481","endPage":"487","numberOfPages":"7","costCenters":[],"links":[{"id":222025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205185,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00455987"}],"volume":"3","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3d39e4b0c8380cd633d1","contributors":{"authors":[{"text":"Jones, J.R.","contributorId":15967,"corporation":false,"usgs":true,"family":"Jones","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":363987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beall, R.M.","contributorId":88392,"corporation":false,"usgs":true,"family":"Beall","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":363989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Giusti, E.V.","contributorId":51342,"corporation":false,"usgs":true,"family":"Giusti","given":"E.V.","affiliations":[],"preferred":false,"id":363988,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012514,"text":"70012514 - 1979 - A review of numerical simulation of hydrothermal systems","interactions":[],"lastModifiedDate":"2025-01-03T16:59:39.801197","indexId":"70012514","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1926,"text":"Hydrological Sciences Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A review of numerical simulation of hydrothermal systems","docAbstract":"<p><span>Many advances in simulating single and two-phase fluid flow and heat transport in porous media have recently been made in conjunction with geothermal energy research. These numerical models reproduce system thermal and pressure behaviour and can be used for heat-transport problems other than those associated with geothermal energy development, such as high-level radioactive waste disposal and heat-storage projects. Although these models are general, additional research is necessary before they can be applied to certain site-specific problems that are concerned with additional processes, such as mass transport and flow in fractured media.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626667909491871","issn":"03036936","usgsCitation":"Mercer, J., and Faust, C., 1979, A review of numerical simulation of hydrothermal systems: Hydrological Sciences Bulletin, v. 24, no. 3, p. 335-344, https://doi.org/10.1080/02626667909491871.","productDescription":"10 p.","startPage":"335","endPage":"344","numberOfPages":"10","costCenters":[],"links":[{"id":488798,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626667909491871","text":"Publisher Index Page"},{"id":222541,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e554e4b0c8380cd46cba","contributors":{"authors":[{"text":"Mercer, J.W.","contributorId":90741,"corporation":false,"usgs":true,"family":"Mercer","given":"J.W.","affiliations":[],"preferred":false,"id":363795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faust, C.R.","contributorId":9922,"corporation":false,"usgs":true,"family":"Faust","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":363794,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043280,"text":"70043280 - 1978 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","interactions":[{"subject":{"id":11325,"text":"ofr77263 - 1977 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, west-central Utah","indexId":"ofr77263","publicationYear":"1977","noYear":false,"title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043280,"text":"70043280 - 1978 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","indexId":"70043280","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:26:49","indexId":"70043280","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"59","title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","docAbstract":"The Dugway Valley-Government Creek area covers about 890 square miles (2,300 square kilometers) in west-central Utah. Total annual precipitation on the area averages about 380,000 acre-feet (470 cubic hectometers). Most streams are ephemeral except for a few in their upper reaches--all are ephemeral below the altitude of about 6,000 feet (1,830 meters). Surface-water development and use in the area are insignificant.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Stephens, J.C., and Sumsion, C.T., 1978, Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah: Technical Publication 59, vi, 42 p.","productDescription":"vi, 42 p.","numberOfPages":"50","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331963,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-450"},{"id":267165,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009l.pdf"}],"datum":"United States","country":"United States","state":"Utah","county":"Juab County, Tooele County","otherGeospatial":"Dugway Valley-Government Creek Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.27316284179688,\n              40.226072729473884\n            ],\n            [\n              -113.31573486328124,\n              40.15683567591309\n            ],\n            [\n              -113.27041625976562,\n              40.11799004890473\n            ],\n            [\n              -113.26766967773438,\n              40.065460682065535\n            ],\n            [\n              -113.22509765625,\n              40.01078714046552\n            ],\n            [\n              -113.16055297851562,\n              39.985538414809746\n            ],\n            [\n              -113.07952880859375,\n              39.93711893299021\n            ],\n            [\n              -113.06854248046875,\n              39.839122664473194\n            ],\n            [\n              -113.148193359375,\n              39.818029898770206\n            ],\n            [\n              -113.16329956054688,\n              39.74837783143156\n            ],\n            [\n              -113.11248779296874,\n              39.688167045890395\n            ],\n            [\n              -113.06304931640625,\n              39.675484393594814\n            ],\n            [\n              -112.78701782226562,\n              39.7642140375156\n            ],\n            [\n              -112.78152465820312,\n              39.842286020743394\n            ],\n            [\n              -112.73483276367188,\n              39.883396390093075\n            ],\n            [\n              -112.59887695312499,\n              39.88128876522249\n            ],\n            [\n              -112.664794921875,\n              39.9602803542957\n            ],\n            [\n              -112.68402099609374,\n              40.03182061333687\n            ],\n            [\n              -112.70736694335936,\n              40.127441029049486\n            ],\n            [\n              -112.78701782226562,\n              40.2313150803688\n            ],\n            [\n              -112.97241210937499,\n              40.364334716590214\n            ],\n            [\n              -113.17428588867188,\n              40.286859051369504\n            ],\n            [\n              -113.27316284179688,\n              40.226072729473884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177dffe4b0893acf3fffb5","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":473278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":473277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","interactions":[{"subject":{"id":10425,"text":"ofr7815 - 1977 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"ofr7815","publicationYear":"1977","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"70043282","publicationYear":"1978","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"id":1}],"lastModifiedDate":"2016-12-12T14:46:33","indexId":"70043282","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"63","title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","docAbstract":"Beaver Valley includes 534 square miles in southwestern Utah, in the Basin and Range physiographic province. The project area consists of a valley plain underlain by unconsolidated to partly consolidated material. The valley plain is bounded by mountains that are composed of partly consolidated to consolidated rocks of Pennsylvanian through Tertiary age except for local thin unconsolidated surficial deposits of Quaternary age. The water needs of the valley are supplied mainly by four streams rising in the Tushar Mountains along the eastern side of the valley and by wells in the unconsolidated to partly consolidated materials of the valley plain. The objectives of this study were (1) to measure and analyze the discharge/recharges rates and (2) to measure and analyze the total amount of water in storage in the ground-water reservoirs.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., 1978, Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water: Technical Publication 63, vi, 90 p.","productDescription":"vi, 90 p.","numberOfPages":"100","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331971,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009p.pdf"},{"id":331970,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-530"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.9,\n              38.15\n            ],\n            [\n              -112.9,\n              38.5\n            ],\n            [\n              -112.4,\n              38.5\n            ],\n            [\n              -112.4,\n              38.15\n            ],\n            [\n              -112.9,\n              38.15\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e04e4b0893acf3fffc6","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","interactions":[{"subject":{"id":7977,"text":"ofr78312 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah","indexId":"ofr78312","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","indexId":"70043963","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:08:28","indexId":"70043963","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64","title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","docAbstract":"The Fish Springs Flat area includes about 590 square miles (1,530 square kilometers) in western Utah. Total annual precipitation on the area averages about 7 inches (180 millimeters) and totals about 232,000 acre-feet (286 cubic hectometers). Fish Springs Wash is the major drainage in the area; and, along with numerous smaller washes, it flows only in direct response to precipitation. Runoff from the area is estimated to be about 2,000 acre-feet (2.5 cubic hectometers) per year.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Bolke, E., and Sumsion, C.T., 1978, Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah: Technical Publication 64, iv, 30 p.","productDescription":"iv, 30 p.","numberOfPages":"36","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268165,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009q.pdf"},{"id":331953,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-560"}],"country":"United States","state":"Utah","county":"Juab County, Millard County, Tooele County","otherGeospatial":"Fish Springs Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.65905761718749,\n              39.41497702499074\n            ],\n            [\n              -113.65905761718749,\n              40.000267972646796\n            ],\n            [\n              -112.9779052734375,\n              40.000267972646796\n            ],\n            [\n              -112.9779052734375,\n              39.41497702499074\n            ],\n            [\n              -113.65905761718749,\n              39.41497702499074\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44a5e4b0523e997a814a","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":474556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":474555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20271,"text":"ofr78959 - 1978 - Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","interactions":[],"lastModifiedDate":"2021-12-17T22:40:18.314429","indexId":"ofr78959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-959","title":"Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","docAbstract":"The flood plain on the Chena and Tanana Rivers near Fairbanks, Alaska, has abundant water in rivers and in an unconfined alluvial aquifer. The principal source of ground water is the Tanana River, from which ground water flows northwesterly to the Chena River. Transmissivity of the aquifer commonly exceed 100 ,000 sq ft. The shallow water table (less than 15 ft below land surface), high hydraulic conductivity of the sediments and cold soil give the flood plain a high susceptibility to pollution by onsite sewerage systems. The Environmental Protection Agency recommended maximum concentrations for drinking water may be exceeded in surface water for manganese and bacteria and in ground water for iron, manganese, and bacteria. Residents of the uplands obtain water principally from a widely-distributed fractured schist aquifer. The aquifer is recharged by local infiltration of precipitation and is drained by springs on the lower slopes and by ground-water flow to alluvial aquifers of the valleys. The annual base flow from basins in the uplands ranged from 3,000 to 100,000 gallons per acre; the smallest base flows occur in basins nearest the city of Fairbanks. The thick silt cover and great depth to the water table give much of the uplands a low susceptibility to pollution by onsite sewage disposal. Ground water is locally high in nitrate, arsenic, iron , and manganese. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78959","usgsCitation":"Nelson, G.L., 1978, Hydrologic information for land-use planning, Fairbanks vicinity, Alaska: U.S. Geological Survey Open-File Report 78-959, vi, 47 p., https://doi.org/10.3133/ofr78959.","productDescription":"vi, 47 p.","costCenters":[],"links":[{"id":152287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94448,"rank":800,"type":{"id":15,"text":"Index Page"},"url":"https://dggs.alaska.gov/pubs/id/11192"},{"id":393068,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14970.htm"}],"country":"United States","state":"Alaska","city":"Fairbanks","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.326416015625,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              64.73429692356085\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a25","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3263,"text":"cir769 - 1978 - A theoretical basis for exploration for native copper in northern Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"769","title":"A theoretical basis for exploration for native copper in northern Wisconsin","docAbstract":"Exploration for native copper in the Keweenawan lavas of northern Wisconsin has been concentrated in areas of relatively shallow overburden that have sparse to numerous outcrops. Lack of success of this exploration suggests that if large deposits, comparable to those of northern Michigan, are present, they are more likely to be found in one or more of the large tracts that have few, if any, exposures, away from the ' copper ranges. ' A hydrologic model that may explain the mineralization of the classic native-copper district of Michigan could be helpful in suggesting that certain covered tracts are more favorable than others, and in narrowing the targets for physical exploration within these tracts. This model involves updip migration of a hydrothermal fluid of metamorphic origin, formed when ground water contained in the interstices of lava flows and conglomerate beds was carried to great depth along the axis of the Lake Superior syncline. The largest reservoirs of such buried ground water would be expected in the peripheral rather than central parts of the basins in which the lavas originally accumulated because the ratio of porous fragmental flow tops and conglomerate beds to massive basalt should increase towards the margins of a basin. Thus, the areas most promising for copper deposits should be those updip from places where the trough of the later formed Lake Superior syncline crosses the marginal parts of a lava basin. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir769","usgsCitation":"White, W., 1978, A theoretical basis for exploration for native copper in northern Wisconsin: U.S. Geological Survey Circular 769, iii, 19 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir769.","productDescription":"iii, 19 p. :ill., maps ;26 cm.","numberOfPages":"21","costCenters":[],"links":[{"id":123904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0769/report-thumb.jpg"},{"id":30257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56dc","contributors":{"authors":[{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":146538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20762,"text":"ofr78176 - 1978 - Recent and projected changes in Dead Sea level and effects on mineral production from the sea","interactions":[],"lastModifiedDate":"2022-09-23T20:25:47.485204","indexId":"ofr78176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-176","title":"Recent and projected changes in Dead Sea level and effects on mineral production from the sea","docAbstract":"<p>Hydrologic data for the Dead Sea area were reviewed to assess the probable magnitude and rate of change of the water level of the Dead Sea. Historical average annual Dead Sea levels range from a minimum of 399.4 meters below sea level in about 1818 to a maximum of 388.6 meters below in 1896. Present levels are rapidly approaching the historical low. There is a close correlation between Dead Sea level and accumulated departure from the mean of long-term rainfall except for the most recent period since 1964. During that period rainfall has been near the long-term average but water levels have continued to decline, in part due to abstractions for irrigation in the Jordan River basin.</p><p>The dissolved-solids concentration of Dead Sea water presently is approximately 322,000 milligrams per liter and is generally well mixed throughout. This concentration is at the saturation level, resulting in continuous precipitation of some salts. The increase in dissolved solids to the present high concentration has resulted in an evaporation rate less than that estimated in previous reports. Evaporation rate from the North Basin is estimated at 1,310 millimeters per year at present. The evaporation rate from the South Basin was not estimated due to extensive existing or planned modifications for mineral production facilities.</p><p>Water budget computations were performed at various inflow rates in order to project water-level changes for 50 years. Computations assumed closure of the South Basin by existing and proposed mineral extraction facilities. The projected 50-year changes ranged from a decline of 51 meters with no inflow from any sources to a rise of 10.2 meters when average annual inflow from the Jordan River was 750 cubic hectometers. An average annual inflow to the Sea of 900 cubic hectometers from all sources is required to stabilize the Sea at the present level. Principal impact of declining water levels on proposed potash production facilities in Jordan would be an increase in power requirements.</p><p>A cursory review of a proposed plan to divert water from the Mediterranean Sea into the Dead Sea to generate electric power and stabilize water levels indicates a very limited impact on chemical, physical, and ecological characteristics of the Dead Sea in the near future. Water-budget computations indicate that if all but 200 cubic hectometers of tributaries' waters were utilized for irrigation and other purposes, a maximum diversion of 700 cubic hectometers per year into the Dead Sea would be possible without significantly raising long-term average water levels.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78176","collaboration":"Prepared in cooperation with the U.S. Agency for International Development","usgsCitation":"Sauer, S.P., 1978, Recent and projected changes in Dead Sea level and effects on mineral production from the sea: U.S. Geological Survey Open-File Report 78-176, iv, 43 p., https://doi.org/10.3133/ofr78176.","productDescription":"iv, 43 p.","costCenters":[],"links":[{"id":407296,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0176/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0176/report-thumb.jpg"}],"country":"Israel, Jordan, West Bank","otherGeospatial":"Dead Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              35.36773681640625,\n              30.954057859276126\n            ],\n            [\n              35.6011962890625,\n              30.954057859276126\n            ],\n            [\n              35.6011962890625,\n              31.826231907142883\n            ],\n            [\n              35.36773681640625,\n              31.826231907142883\n            ],\n            [\n              35.36773681640625,\n              30.954057859276126\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485a7","contributors":{"authors":[{"text":"Sauer, Stanley P.","contributorId":38966,"corporation":false,"usgs":true,"family":"Sauer","given":"Stanley","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":183201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12239,"text":"ofr78770 - 1978 - Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic","interactions":[],"lastModifiedDate":"2018-08-21T13:24:03","indexId":"ofr78770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-770","title":"Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78770","usgsCitation":"Grolier, M.J., Ibrahim, M., Overstreet, W., Tibbitts, G., and Davidson, D., 1978, Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic: U.S. Geological Survey Open-File Report 78-770, ii, 15 p. :maps ;28 cm.; (20 p. - PGS), https://doi.org/10.3133/ofr78770.","productDescription":"ii, 15 p. :maps ;28 cm.; (20 p. - PGS)","costCenters":[],"links":[{"id":146216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0770/report-thumb.jpg"},{"id":40399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669228","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":165601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ibrahim, M.","contributorId":10797,"corporation":false,"usgs":true,"family":"Ibrahim","given":"M.","email":"","affiliations":[],"preferred":false,"id":165598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":165602,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tibbitts, G. Chase","contributorId":79453,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G. Chase","affiliations":[],"preferred":false,"id":165600,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":165599,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":11789,"text":"ofr78500 - 1978 - Selected hydrologic data, Camas Prairie, south-central Idaho","interactions":[],"lastModifiedDate":"2024-03-08T19:59:58.246624","indexId":"ofr78500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-500","title":"Selected hydrologic data, Camas Prairie, south-central Idaho","docAbstract":"<p>This report presents data collected during a 1-year study of the water resources of Camas Prairie, Idaho. Included are records of wells, discharge measurements of streams, hydrographs of water levels in wells, water-quality data, and drillers' logs of wells. The data are conveniently made available to supplement an interpretive report, which will be published separately.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78500","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources","usgsCitation":"Young, H., Backsen, R., and Kenyon, K., 1978, Selected hydrologic data, Camas Prairie, south-central Idaho: U.S. Geological Survey Open-File Report 78-500, Report: iv, 70 p.; 1 Plate: 26.41 x 17.96 inches, https://doi.org/10.3133/ofr78500.","productDescription":"Report: iv, 70 p.; 1 Plate: 26.41 x 17.96 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":426464,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1978/0500/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426463,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144776,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0500/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Camas Prairie","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -115.15207912107833,\n              43.33131287386249\n            ],\n            [\n              -115.15207912107833,\n              43.09066964193292\n            ],\n            [\n              -114.40886879477013,\n              43.09066964193292\n            ],\n            [\n              -114.40886879477013,\n              43.33131287386249\n            ],\n            [\n              -115.15207912107833,\n              43.33131287386249\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e47f6","contributors":{"authors":[{"text":"Young, H.W.","contributorId":68278,"corporation":false,"usgs":true,"family":"Young","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":163732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Backsen, R.L.","contributorId":48550,"corporation":false,"usgs":true,"family":"Backsen","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":163731,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kenyon, K.S.","contributorId":99148,"corporation":false,"usgs":true,"family":"Kenyon","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":163733,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11644,"text":"ofr78786 - 1978 - Progress toward a ground-water-quality monitoring network for Idaho","interactions":[{"subject":{"id":11644,"text":"ofr78786 - 1978 - Progress toward a ground-water-quality monitoring network for Idaho","indexId":"ofr78786","publicationYear":"1978","noYear":false,"title":"Progress toward a ground-water-quality monitoring network for Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":11645,"text":"ofr791477 - 1979 - A proposed ground water quality monitoring network for Idaho","indexId":"ofr791477","publicationYear":"1979","noYear":false,"title":"A proposed ground water quality monitoring network for Idaho"},"id":1}],"supersededBy":{"id":11645,"text":"ofr791477 - 1979 - A proposed ground water quality monitoring network for Idaho","indexId":"ofr791477","publicationYear":"1979","noYear":false,"title":"A proposed ground water quality monitoring network for Idaho"},"lastModifiedDate":"2015-10-22T11:48:14","indexId":"ofr78786","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-786","title":"Progress toward a ground-water-quality monitoring network for Idaho","docAbstract":"<p>A ground-water-quality monitoring network is being designed for Idaho. The primary objectives of the network are to (1) determine the present quality of the State's ground water, (2) provide continual monitoring of groundwater quality for water-management purposes, and (3) serve as a warning system of undesirable changes in ground-water quality.</p>\n<p>Data are compiled for geohydrologic conditions, groundwater quality, cultural elements, and pollution sources. &nbsp;A \"Hydrologic Unit Priority Index\" is calculated from these data to select priority areas for monitoring purposes.</p>\n<p>New ground-water-quality data were collected where existing data were lacking and at some sites that were previously sampled. Old and new data at common sites correlated well, indicating that the water quality has not changed significantly. Most ground water in Idaho is of good quality for common uses; however, water quality may pose problems in local areas. The problems result from both natural and human causes.</p>\n<p>The potential for pollution of the aquifers is expected to be greatest in areas of greatest development. In Idaho, population centers and industries tend to be in areas of privately owned irrigated and arable &middot; land. Therefore, these areas are of primary concern for monitoring ground-water quality. Other areas requiring monitoring include those with second-home development, mining and its related processes, and radioactive-waste disposal.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78786","usgsCitation":"Whitehead, R., 1978, Progress toward a ground-water-quality monitoring network for Idaho: U.S. Geological Survey Open-File Report 78-786, Report: 42 p.; 4 Plates: 23.17 x 35.69 inches or smaller, https://doi.org/10.3133/ofr78786.","productDescription":"Report: 42 p.; 4 Plates: 23.17 x 35.69 inches or 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da49","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":163494,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11640,"text":"ofr78256 - 1978 - Nuclear power reactor sites in the southeastern United States","interactions":[],"lastModifiedDate":"2022-09-28T14:59:25.569756","indexId":"ofr78256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-256","title":"Nuclear power reactor sites in the southeastern United States","docAbstract":"<p>This report describes nuclear power reactor sites in the southeastern United States. The map indicates the location of all sites as of July 1976 in the conterminous United States, and a later published report will include all sites. The project is one of several in the National Environmental Overview Program of the U.S. Geological Survey which will identify and summarize geologic, hydrologic, and topographic topics associated with future energy, mineral resource, and land use development in the United States.</p><p>The increasing use of atomic energy creates a need for the dissemination of information about nuclear reactors. Because power plant safety is related, in part, to the geology and seismology of the plant area and surroundings, this study is focused primarily on that relationship.</p><p>Information about the geology and seismology is summarized from reports prepared by consultants to utility companies and submitted by the companies to the U.S. Nuclear Regulatory Commission (formerly the U.S. Atomic Energy Commission) in support of the application for a construction permit.</p><p>Coordinates for site locations were established by the author from descriptive information in the reports. The U.S. Geological Survey 7-1/2 minute topographic maps were used in confirming the geographic location of the sites. The coordinates may in some cases represent the planned location rather than the exact actual location.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78256","usgsCitation":"West, M., 1978, Nuclear power reactor sites in the southeastern United States: U.S. Geological Survey Open-File Report 78-256, Report: 20 p.; 1 Plate: 26.89 x 18.28 inches, https://doi.org/10.3133/ofr78256.","productDescription":"Report: 20 p.; 1 Plate: 26.89 x 18.28 inches","costCenters":[],"links":[{"id":407413,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0256/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407412,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0256/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407510,"rank":4,"type":{"id":36,"text":"NGMDB Index 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69686e","contributors":{"authors":[{"text":"West, Mareta","contributorId":64221,"corporation":false,"usgs":true,"family":"West","given":"Mareta","affiliations":[],"preferred":false,"id":163489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11435,"text":"ofr78413 - 1978 - Hydrologic data for the Copper Basin area, a potential mining area in Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2023-02-15T21:42:15.73389","indexId":"ofr78413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-413","title":"Hydrologic data for the Copper Basin area, a potential mining area in Yavapai County, Arizona","docAbstract":"<p>Large low-grade ore bodies have been discovered in Copper Basin, and a large copper-mining operation is anticipated in the near future. Hydrologic data are being collected to provide the data base necessary to determine the effects of a potential mining operation on the water resources of the area. The area of potential depletion or contamination of water supplies is the 50-square-mile alluvial slope downgradient from Copper Basin. In the Copper Basin area the streams generally are dry, except for the perennial flow in a 3-mile-long reach of Kirkland Creek, where the base flow ranges from about 1 to 3 cubic feet per second.</p><p>The water in the alluvium, which is more than 1,000 feet thick in places, generally is under unconfined conditions. The direction of ground-water movement is generally southwesterly toward Skull Valley Wash and Kirkland Creek. The depth to water in wells ranges from less than 10 to 675 feet below the land surface. Near the center of the area, test wells penetrate a clay confining bed at the base of the alluvium and an underlying sequence of volcanic rocks, which is more than 1,000 feet thick and contains water under confined conditions.</p><p>Pump tests indicate that the confining bed forms a barrier between the water in the alluvium and the water in the volcanic rocks and that, initially, pumping from the volcanic rocks would not affect the water level in the alluvium. The areal extent of the volcanic sequence is not known.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78413","collaboration":"Prepared in cooperation with the Arizona Water Commission","usgsCitation":"Thomsen, B.W., and Stulik, R., 1978, Hydrologic data for the Copper Basin area, a potential mining area in Yavapai County, Arizona: U.S. Geological Survey Open-File Report 78-413, Report: vi, 51 p.; 1 Plate: 34.88 x 45.93 inches, https://doi.org/10.3133/ofr78413.","productDescription":"Report: vi, 51 p.; 1 Plate: 34.88 x 45.93 inches","costCenters":[],"links":[{"id":413108,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0413/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144159,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0413/report-thumb.jpg"},{"id":413107,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0413/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Copper Basin 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B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":163136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stulik, R.S.","contributorId":51749,"corporation":false,"usgs":true,"family":"Stulik","given":"R.S.","affiliations":[],"preferred":false,"id":163137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001,"text":"wsp2042 - 1978 - Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation","interactions":[],"lastModifiedDate":"2017-07-07T08:37:22","indexId":"wsp2042","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"2042","title":"Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation","docAbstract":"A map of the Ohio River basin above the Muskingum River shows patterns of mean annual runoff for the new climatologic and hydrologic reference period, 1941-70, and provides an up-to-date, consistent basis for consideration of this streamflow characteristic. The primary data base consisted of 98 long-term gaging-station records collected within this 27,300-square-mile (70,700-square-kilometer) headwater area of the Ohio River basin. Supplemental information was derived from 83 short-term records. \r\n\r\nMean annual runoff is at a regional minimum of less than 12 inches (300 millimeters) in an area extending from the northern West Virginia panhandle to the headwaters of the Mahoning River in Ohio. Mean annual runoff of more than 32 inches {810 millimeters) occurs in parts of the upper Cheat River basin in West Virginia. The zone of high runoff trends northeastward along the western slopes of tile Allegheny Mountains; magnitudes diminish to about 25 inches (630 millimeters) at the eastern basin boundary near Ebensburg, Pa. Runoff of this magnitude occurs also in a band across tile upper Allegheny River basin in Pennsylvania. \r\n\r\nRatios of mean annual discharge to the 30-year reference-period average were computed for each year of record for all long-term gaging stations. Annual discharges have ranged from about 30 percent to 200 percent of the 30-year mean. Graphed summaries of the annual ratios document the relative duration and magnitude of wet and dry periods during the past 65 years in the upper Ohio River basin.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2042","usgsCitation":"Beall, R.M., 1978, Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation: U.S. Geological Survey Water Supply Paper 2042, iv, 32 p. :ill. (1 fold. in pocket), maps (1 fold. col. in pocket) ;23 cm. --, https://doi.org/10.3133/wsp2042.","productDescription":"iv, 32 p. :ill. (1 fold. in pocket), maps (1 fold. col. in pocket) ;23 cm. --","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2042/report-thumb.jpg"},{"id":94696,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2042/plate-table_3.pdf","size":"1104","linkFileType":{"id":1,"text":"pdf"}},{"id":25572,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610780","contributors":{"authors":[{"text":"Beall, Robert M.","contributorId":90695,"corporation":false,"usgs":true,"family":"Beall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":142998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","interactions":[{"subject":{"id":70180237,"text":"70180237 - 1978 - New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>","indexId":"70180237","publicationYear":"1978","noYear":false,"title":"New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>"},"predicate":"IS_PART_OF","object":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"id":1},{"subject":{"id":70180239,"text":"70180239 - 1978 - New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska","indexId":"70180239","publicationYear":"1978","noYear":false,"title":"New potassium-argon data on the age of mineralization and metamorphism in the Willow Creek mining district, southern Talkeetna Mountains, Alaska"},"predicate":"IS_PART_OF","object":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"id":2}],"lastModifiedDate":"2024-11-05T20:26:31.603152","indexId":"cir772B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"772-B","title":"The United States Geological Survey in Alaska: Accomplishments during 1977","docAbstract":"<p>United States Geological Survey projects in Alaska study a wide range of topics of economic and scientific interest. Work done in 1977 includes contributions to economic geology, regional geology, stratigraphy, engineering geology, hydrology, and marine geology. Many maps and reports covering various aspects of the geology and mineral and water resources of the State were published. In addition, the published 1:1,000,000-scale map of the State has been revised in two areas. A bibliography containing 263 reports on Alaska published in 1977 is included.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir772B","usgsCitation":"1978, The United States Geological Survey in Alaska: Accomplishments during 1977: U.S. Geological Survey Circular 772-B, v, 115 p., https://doi.org/10.3133/cir772B.","productDescription":"v, 115 p.","numberOfPages":"121","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":463741,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24025.htm","text":"New geologic map of the Goodnews - Hegemeister Island quadrangles region, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":463739,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23885.htm","text":"Generalized physiography and geology of the Beluga coal field and vicinity, 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,{"id":23554,"text":"ofr78356 - 1978 - Linear ground-water flow, flood-wave response program for programmable calculators","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"ofr78356","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-356","title":"Linear ground-water flow, flood-wave response program for programmable calculators","docAbstract":"Two programs are documented which solve a discretized analytical equation derived to determine head changes at a point in a one-dimensional ground-water flow system. The programs, written for programmable calculators, are in widely divergent but commonly encountered languages and serve to illustrate the adaptability of the linear model to use in situations where access to true computers is not possible or economical. The analytical method assumes a semi-infinite aquifer which is uniform in thickness and hydrologic characteristics, bounded on one side by an impermeable barrier and on the other parallel side by a fully penetrating stream in complete hydraulic connection with the aquifer. Ground-water heads may be calculated for points along a line which is perpendicular to the impermeable barrie and the fully penetrating stream. Head changes at the observation point are dependent on (1) the distance between that point and the impermeable barrier, (2) the distance between the line of stress (the stream) and the impermeable barrier, (3) aquifer diffusivity, (4) time, and (5) head changes along the line of stress. The primary application of the programs is to determine aquifer diffusivity by the flood-wave response technique. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78356","issn":"0094-9140","usgsCitation":"Kernodle, J.M., 1978, Linear ground-water flow, flood-wave response program for programmable calculators: U.S. Geological Survey Open-File Report 78-356, iv, 69 p. :ill. ;27 cm., https://doi.org/10.3133/ofr78356.","productDescription":"iv, 69 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":113011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0356/report.pdf","size":"1974","linkFileType":{"id":1,"text":"pdf"}},{"id":156522,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0356/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d41","contributors":{"authors":[{"text":"Kernodle, John Michael","contributorId":99171,"corporation":false,"usgs":true,"family":"Kernodle","given":"John","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":190308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11315,"text":"ofr78226 - 1978 - Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado","interactions":[],"lastModifiedDate":"2018-10-25T10:40:54","indexId":"ofr78226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-226","title":"Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado","docAbstract":"<p>A hydrologic reconnaissance of a 74-kilometer reach of the Yampa River in Dinosaur National Monument was made during low flow in mid-August 1976. Stream discharge, which was measured along this reach every 16 to 24 kilometers, ranged from 9.4 to 10.6 cubic meters per second. Variations in streamflow were explained, in part, by underflow, loss to ground water, and evaporation. Specific conductance was measured about every 2 kilometers and indicated a downstream increase on the order of 11 to 12 percent for the reach. Except for mercury, bottom-sediment trace-element concentrations in the study reach were less than maximum concentrations determined during August-September 1976 for bottom sediments at unperturbed sites upstream in the Yampa River basin. At one of five sampling sites, the mercury concentration in bottom sediments exceeded the maximum measured upstream level.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78226","usgsCitation":"Steele, T.D., Wentz, D.A., and Warner, J.W., 1978, Hydrologic reconnaissance of the Yampa River during low flow, Dinosaur National Monument, northwestern Colorado: U.S. Geological Survey Open-File Report 78-226, ii, 10 p., https://doi.org/10.3133/ofr78226.","productDescription":"ii, 10 p.","costCenters":[],"links":[{"id":142576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0226/report-thumb.jpg"},{"id":358795,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Dinosaur National Monument","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.05029296875,\n              40.43022363450862\n            ],\n            [\n              -108.50372314453125,\n              40.43022363450862\n            ],\n            [\n              -108.50372314453125,\n              40.71603763556807\n            ],\n            [\n              -109.05029296875,\n              40.71603763556807\n            ],\n            [\n              -109.05029296875,\n              40.43022363450862\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60545d","contributors":{"authors":[{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":162916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wentz, Dennis A. dawentz@usgs.gov","contributorId":1838,"corporation":false,"usgs":true,"family":"Wentz","given":"Dennis","email":"dawentz@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":162915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warner, James W.","contributorId":106119,"corporation":false,"usgs":true,"family":"Warner","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":162917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11041,"text":"ofr78567 - 1978 - Hydrologic data for water-table aquifers in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr78567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-567","title":"Hydrologic data for water-table aquifers in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado","docAbstract":"As part of the U.S. Geological Survey 's investigations of the hydrology and geology in the Front Range Urban Corridor of Colorado, hydrologic data relating to water-table aquifers were compiled during 1976-77. These data consisting of records of 446 wells and chemical analyses of water from 208 wells in the Boulder--Fort Collins--Greeley area, are presented in tabular form. The well-data tables contain records that were collected during 1976-77. The chemical analysis tables contain records that were collected during 1956-77. State and local officials in the Boulder--Fort Collins--Greeley area may find these data useful in planning for residential, commercial, and industrial development. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78567","usgsCitation":"Schneider, P., and Hillier, D.E., 1978, Hydrologic data for water-table aquifers in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado: U.S. Geological Survey Open-File Report 78-567, iv, 55 p. :maps (1 col., fold. in pocket) ;29 cm.; (67 p., 1 sheet - PGS), https://doi.org/10.3133/ofr78567.","productDescription":"iv, 55 p. :maps (1 col., fold. in pocket) ;29 cm.; (67 p., 1 sheet - PGS)","costCenters":[],"links":[{"id":142603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0567/report-thumb.jpg"},{"id":38810,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0567/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0567/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60793d","contributors":{"authors":[{"text":"Schneider, Paul A.","contributorId":32509,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul A.","affiliations":[],"preferred":false,"id":162426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillier, Donald E.","contributorId":105282,"corporation":false,"usgs":true,"family":"Hillier","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162427,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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