{"pageNumber":"1757","pageRowStart":"43900","pageSize":"25","recordCount":46599,"records":[{"id":70009808,"text":"70009808 - 1976 - The dissolution of calcite in CO<sub>2</sub>-saturated solutions at 25°C and 1 atmosphere total pressure","interactions":[],"lastModifiedDate":"2018-03-21T15:10:39","indexId":"70009808","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The dissolution of calcite in CO<sub>2</sub>-saturated solutions at 25°C and 1 atmosphere total pressure","docAbstract":"<p><span>The dissolution of Iceland spar in CO</span><sub>2</sub><span>-saturated solutions at 25&deg;C and 1 atm total pressure has been followed by measurement of pH as a function of time. Surface concentrations of reactant and product species have been calculated from bulk fluid data using mass transport theory and a model that accounts for homogeneous reactions in the bulk fluid. The surface concentrations are found to be close to bulk solution values. This indicates that calcite dissolution under the experimental conditions is controlled by the kinetics of surface reaction. The rate of calcite dissolution follows an empirical second order relation with respect to calcium and hydrogen ion from near the initial condition (pH 3.91) to approximately pH 5.9. Beyond pH 5.9 the rate of surface reaction is greatly reduced and higher reaction orders are observed. Calculations show that the rate of calcite dissolution in natural environments may be influenced by both transport and surface-reaction processes. In the absence of inhibition, relatively short times should be sufficient to establish equilibrium.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90176-9","issn":"00167037","usgsCitation":"Plummer, N., and Wigley, T., 1976, The dissolution of calcite in CO<sub>2</sub>-saturated solutions at 25°C and 1 atmosphere total pressure: Geochimica et Cosmochimica Acta, v. 40, no. 2, p. 191-202, https://doi.org/10.1016/0016-7037(76)90176-9.","productDescription":"12 p.","startPage":"191","endPage":"202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":218907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baac7e4b08c986b3229e1","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":357196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wigley, T.M.L.","contributorId":56788,"corporation":false,"usgs":true,"family":"Wigley","given":"T.M.L.","email":"","affiliations":[],"preferred":false,"id":357195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011024,"text":"70011024 - 1976 - Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70011024","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","docAbstract":"Hasselblad and Nikon stereographic photographs taken from Skylab between 9 June 1973 and 1 February 1974 give synoptic plan views of several entire eruption clouds emanating from Sakura-zima volcano in Kagoshima Bay, Kyushu, Japan. Analytical plots of these stereographic pairs, studied in combination with meteorological data, indicate that the eruption clouds did not penetrate the tropopause and thus did not create a stratospheric dust veil of long residence time. A horizontal eddy diffusivity of the order of 106 cm2 s-1 and a vertical eddy diffusivity of the order of 105 cm2 s-1 were calculated from the observed plume dimensions and from available meteorological data. These observations are the first, direct evidence that explosive eruption at an estimated energy level of about 1018 ergs per paroxysm may be too small under atmospheric conditions similar to those prevailing over Sakura-zima for volcanic effluents to penetrate low-level tropospheric temperature inversions and, consequently, the tropopause over northern middle latitudes. Maximum elevation of the volcanic clouds was determined to be 3.4 km. The cumulative thermal energy release in the rise of volcanic plumes for 385 observed explosive eruptions was estimated to be 1020 to 1021 ergs (1013 to 1014 J), but the entire thermal energy release associated with pyroclastic activity may be of the order of 2.5 ?? 1022 ergs (2.5 ?? 1015 J). Estimation of the kinetic energy component of explosive eruptions via satellite observation and meteorological consideration of eruption clouds is thus useful in volcanology as an alternative technique to confirm the kinetic energy estimates made by ground-based geological and geophysical methods, and to aid in construction of physical models of potential and historical tephra-fallout sectors with implications for volcano-hazard prediction. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Friedman, J.D., Heiken, G., Randerson, D., and McKay, D., 1976, Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4: Journal of Volcanology and Geothermal Research, v. 1, no. 4, p. 305-329.","startPage":"305","endPage":"329","numberOfPages":"25","costCenters":[],"links":[{"id":221790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a91e4b0c8380cd74242","contributors":{"authors":[{"text":"Friedman, J. D.","contributorId":99157,"corporation":false,"usgs":true,"family":"Friedman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":360106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heiken, G.","contributorId":11768,"corporation":false,"usgs":true,"family":"Heiken","given":"G.","email":"","affiliations":[],"preferred":false,"id":360104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randerson, D.","contributorId":94162,"corporation":false,"usgs":true,"family":"Randerson","given":"D.","email":"","affiliations":[],"preferred":false,"id":360105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKay, D.S.","contributorId":11329,"corporation":false,"usgs":true,"family":"McKay","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":360103,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010999,"text":"70010999 - 1976 - Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","interactions":[],"lastModifiedDate":"2013-01-21T16:12:50","indexId":"70010999","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","docAbstract":"An extended form of Q-mode factor analysis may be used if the row-sums of the data matrix are constant and can be helpful especially in developing and testing petrologic-mixing models for igneous systems. The first step is to represent the sample compositions as unit vectors in M-dimensional space and then to project them into space of fewer dimensions (m) as determined to be appropriate from a factor-variance diagram. Compositions thought to be those of possible end-members in the petrologic system then are represented as vectors in the M-dimensional space and projected into the same space as the sample vectors. If these vectors remain close to unity in length after projection, the corresponding compositions can serve as end-member compositions for the model. After m suitable end-member compositions have been identified, each sample composition is expressed as a mixture of the end-members by computation of the composition loadings. The interactive computer programs presented are useful in these procedures because of the trial-and-error nature of the modeling procedures. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90039-X","issn":"00983004","usgsCitation":"Miesch, A., 1976, Interactive computer programs for petrologic modeling with extended Q-mode factor analysis: Computers & Geosciences, v. 2, no. 4, p. 439-492, https://doi.org/10.1016/0098-3004(76)90039-X.","startPage":"439","endPage":"492","numberOfPages":"54","costCenters":[],"links":[{"id":221561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266212,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90039-X"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3cd5e4b0c8380cd630a6","contributors":{"authors":[{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":360059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190916,"text":"70190916 - 1976 - Selected hydrologic data, Uinta Basin area, Utah and Colorado","interactions":[],"lastModifiedDate":"2017-09-17T16:33:17","indexId":"70190916","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"26","title":"Selected hydrologic data, Uinta Basin area, Utah and Colorado","docAbstract":"<p>The Uinta Basin area in northeastern Utah and northwestern Colorado covers an area of slightly more than 10,000 mi<sup>2</sup> (25,900 km<sup>2</sup>). More than 95 percent of the basin is in Utah, thus most of the data in this report apply to Utah. Most of the water wells are concentrated in populated areas along the lower parts of the basin; records of only a representative number of these water sources are included in this report.<br></p><p>This report presents consolidated listings of data selected for use in hydrologic studies in the Uinta Basin area through June 1974. The data are principally taken from three studies made during 1971-74 by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights. Also incorporated in this report are data collected since 1935 by the Geological Survey and other organizations. This report is intended to make data conveniently available and to supplement interpretive reports that will be published separately. For some data sites, the volume of data is too great for complete inclusion here. For these sites, data summaries are provided, and for greater detail the reader is referred to the sources listed under Selected references.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Hood, J.W., Mundorff, J.C., and Price, D., 1976, Selected hydrologic data, Uinta Basin area, Utah and Colorado: Utah Basic-Data Release 26, v, 321.","productDescription":"v, 321","numberOfPages":"330","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345845,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345844,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-510&Title=Basic+Data+Report+26"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf899ce4b091459a5e0881","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":710685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":710686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14195,"text":"ofr76152 - 1976 - Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada","interactions":[],"lastModifiedDate":"2024-06-25T17:51:44.339312","indexId":"ofr76152","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-152","title":"Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76152","usgsCitation":"Hoover, D.B., Brougham, G.W., and Clark, J., 1976, Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada: U.S. Geological Survey Open-File Report 76-152, 7 p., https://doi.org/10.3133/ofr76152.","productDescription":"7 p.","costCenters":[],"links":[{"id":145688,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6682e3","contributors":{"authors":[{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brougham, Gary W.","contributorId":108122,"corporation":false,"usgs":true,"family":"Brougham","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, John","contributorId":34145,"corporation":false,"usgs":true,"family":"Clark","given":"John","affiliations":[],"preferred":false,"id":169056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010337,"text":"70010337 - 1976 - Q-mode factor analysis of compositional data","interactions":[],"lastModifiedDate":"2013-01-21T16:05:45","indexId":"70010337","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Q-mode factor analysis of compositional data","docAbstract":"An extended form of the method of Q-mode factor analysis may be used if the rows of the data matrix sum to a constant. The constant row-sum provides a means for scaling the factor model to conform to the units of the original data in such forms as proportions, percentages, or parts per million. The scale factors for an m-factor model are used to derive composition scores and loadings, which lead to the same reproduced data regardless of the choice of reference axes (end-members). Factor-variance diagrams may be constructed to show the proportion of the variance that will be accounted for in each compositional variable by models containing various numbers of end-members. The method may be used to develop a petrologic mixing model by searching for end-members that are geologically plausible. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90003-0","issn":"00983004","usgsCitation":"Miesch, A., 1976, Q-mode factor analysis of compositional data: Computers & Geosciences, v. 1, no. 3, p. 147-159, https://doi.org/10.1016/0098-3004(76)90003-0.","startPage":"147","endPage":"159","numberOfPages":"13","costCenters":[],"links":[{"id":218860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266206,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90003-0"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9067e4b0c8380cd7fd05","contributors":{"authors":[{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":358666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010931,"text":"70010931 - 1976 - Extended cabfac and Qmodel computer programs for Q-mode factor analysis of compositional data","interactions":[],"lastModifiedDate":"2013-01-21T16:11:23","indexId":"70010931","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Extended cabfac and Qmodel computer programs for Q-mode factor analysis of compositional data","docAbstract":"The computer program CABFAC for Q-mode factor analysis of geologic data has been extended for use with data having constant row-sums. Another program, QMODEL, reads an output file from CABFAC and can be used to develop a variety of Q-mode models. The models serve to reproduce estimates of the original data rather than of the data in normalized form. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90004-2","issn":"00983004","usgsCitation":"Klovan, J., and Miesch, A., 1976, Extended cabfac and Qmodel computer programs for Q-mode factor analysis of compositional data: Computers & Geosciences, v. 1, no. 3, p. 161-178, https://doi.org/10.1016/0098-3004(76)90004-2.","startPage":"161","endPage":"178","numberOfPages":"18","costCenters":[],"links":[{"id":221788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266211,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90004-2"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0e3de4b0c8380cd5336d","contributors":{"authors":[{"text":"Klovan, J.E.","contributorId":15072,"corporation":false,"usgs":true,"family":"Klovan","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":359911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":359912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010886,"text":"70010886 - 1976 - Concretionary manganese-iron oxides in streams and their usefulness as a sample medium for geochemical prospecting","interactions":[],"lastModifiedDate":"2025-03-06T16:13:00.38462","indexId":"70010886","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Concretionary manganese-iron oxides in streams and their usefulness as a sample medium for geochemical prospecting","docAbstract":"<div class=\"u-margin-s-bottom\">Correlation studies of 400 samples of sieved stream sediments and 325 samples of fluvial, concretionary Mn-Fe oxides from Maine resulted in the separation of elements into the following categories: (1) elements not scavenged by Mn-Fe oxides — B, Cr, K, Mg, Rb, Sc, Ti, V, and Zr; (2) elements probably not scavenged by Mn-Fe oxides — Ag, Be, Ca, Ga, La, Sb, and Y; (3) elements scavenged weakly by Mn-Fe oxides — Cu, Mo, Pb, and Sr; (4) elements scavenged strongly by Mn oxides — Ba, Cd, Co, Ni, Tl, and Zn; and (5) elements scavenged strongly by Fe oxides — As and In.</div><div class=\"u-margin-s-bottom\">Studies of the scavenged elements showed that the deviation from the mean is characteristically greater in oxide samples as compared to sieved sediments from the same locality. However, a significant increase in contrast between anomalous and background localities, when oxides are the sample medium, more than offsets the disadvantage of data scatter. The use of oxides as a sampling medium clearly and significantly accentuates anomalous localities.</div><div class=\"u-margin-s-bottom\">In general, non-ratioed data on oxides give very nearly the same results as data consisting of scavenged elements ratioed to Mn and Fe. However, ratioed data expand the geographic area of specific anomalies.</div><div class=\"u-margin-s-bottom\">Cd and Zn consistently show strong correlations with concretionary Mn-Fe oxides, but their concentrations in the oxides do not generally show as much contrast between anomalous and background localities as do Cu, Mo, and Pb. These latter elements are strongly scavenged where rocks are mineralized.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(76)90014-5","issn":"03756742","usgsCitation":"Nowlan, G., 1976, Concretionary manganese-iron oxides in streams and their usefulness as a sample medium for geochemical prospecting: Journal of Geochemical Exploration, v. 6, no. 1-2, p. 193-210, https://doi.org/10.1016/0375-6742(76)90014-5.","productDescription":"18 p.","startPage":"193","endPage":"210","numberOfPages":"18","costCenters":[],"links":[{"id":221332,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f9b1e4b0c8380cd4d728","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":359842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010887,"text":"70010887 - 1976 - Instrumental activation analysis of coal and fly ash with thermal and epithermal neutrons and short-lived nuclides","interactions":[],"lastModifiedDate":"2023-03-07T17:28:28.895005","indexId":"70010887","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Instrumental activation analysis of coal and fly ash with thermal and epithermal neutrons and short-lived nuclides","docAbstract":"<p><span>Instrumental neutron activation analysis is applied to the determination of about 25 elements in coals and fly ash by means of nuclides with half-lives of less than 48 h ; thermal and epithermal irradiations are used. The results indicate that epithermal activation is preferable for twelve of the elements (Ga, As, Br, Sr, In, Cs, Ba, La, Sm, Ho, W and U). Data for SRM 1632 (coal) and SRM 1633 (fly ash) compare favorably with the results obtained by other investigators.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(01)82274-1","usgsCitation":"Steinnes, E., and Rowe, J., 1976, Instrumental activation analysis of coal and fly ash with thermal and epithermal neutrons and short-lived nuclides: Analytica Chimica Acta, v. 87, no. 2, p. 451-462, https://doi.org/10.1016/S0003-2670(01)82274-1.","productDescription":"12 p.","startPage":"451","endPage":"462","numberOfPages":"12","costCenters":[],"links":[{"id":221333,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c43e4b0c8380cd62bd3","contributors":{"authors":[{"text":"Steinnes, E.","contributorId":79603,"corporation":false,"usgs":false,"family":"Steinnes","given":"E.","affiliations":[],"preferred":false,"id":359844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":359843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011148,"text":"70011148 - 1976 - Turbidity distribution in the Atlantic Ocean","interactions":[],"lastModifiedDate":"2023-09-25T16:15:45.112517","indexId":"70011148","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1372,"text":"Deep-Sea Research and Oceanographic Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"Turbidity distribution in the Atlantic Ocean","docAbstract":"<p><span>The regional coverage of Lamont nephelometer data in the North and South Atlantic can be used to map seawater turbidity at all depths. At the level of the clearest water, in the mid-depth regions, the turbidity distribution primarily reflects the pattern of productivity in the surface waters. This suggests that the ‘background’ turbidity level in the oceans is largely a function of biogenic fallout. The bottom waters of the western Atlantic generally exhibit large increases in turbidity. The most intense benthic nepheloid layers are in the southwestern Argentine basin and northern North American basin; the lowest bottom water turbidity in the western Atlantic is in the equatorial regions. Both the Argentine and North American basin bottom waters appear to derive their high turbidity largely from local resuspension of terrigenous input in these basins. In contrast to the west, the eastern Atlantic basins show very low turbidities with the exception of three regions: the Mediterranean outflow area, the Cape basin, and the West European basin.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0011-7471(76)90888-3","usgsCitation":"Eittreim, S., Thorndike, E.M., and Sullivan, L., 1976, Turbidity distribution in the Atlantic Ocean: Deep-Sea Research and Oceanographic Abstracts, v. 23, no. 12, p. 1115-1127, https://doi.org/10.1016/0011-7471(76)90888-3.","productDescription":"13 p.","startPage":"1115","endPage":"1127","numberOfPages":"13","costCenters":[],"links":[{"id":220880,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Atlantic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n  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M.","contributorId":43101,"corporation":false,"usgs":false,"family":"Thorndike","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sullivan, L.","contributorId":85327,"corporation":false,"usgs":true,"family":"Sullivan","given":"L.","email":"","affiliations":[],"preferred":false,"id":360396,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010958,"text":"70010958 - 1976 - Concentration and mineralogical residence of elements in rich oil shales of the Green River Formation, Piceance Creek basin, Colorado, and the Uinta Basin, Utah - A preliminary report","interactions":[],"lastModifiedDate":"2018-02-15T15:12:21","indexId":"70010958","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1213,"text":"Chemical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Concentration and mineralogical residence of elements in rich oil shales of the Green River Formation, Piceance Creek basin, Colorado, and the Uinta Basin, Utah - A preliminary report","docAbstract":"Ten samples from drillcore of two rich oil-shale beds from the Parachute Creek Member of the Eocene Green River Formation, Piceance Creek basin, Colorado, and Uinta Basin, Utah, were analyzed for 37 major, minor, and trace elements. For 23 of these elements, principal mineralogical residence is established or suggested and such studies may provide data which are useful for predicting the kinds and amounts of elements and compounds that might be released into the environment by oil-shale mining operations. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Chemical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0009-2541(76)90018-8","issn":"00092541","usgsCitation":"Desborough, G.A., Pitman, J.K., and Huffman, C., 1976, Concentration and mineralogical residence of elements in rich oil shales of the Green River Formation, Piceance Creek basin, Colorado, and the Uinta Basin, Utah - A preliminary report: Chemical Geology, v. 17, no. C, p. 13-26, https://doi.org/10.1016/0009-2541(76)90018-8.","startPage":"13","endPage":"26","numberOfPages":"14","costCenters":[],"links":[{"id":221014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266136,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0009-2541(76)90018-8"}],"volume":"17","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f97ae4b0c8380cd4d61a","contributors":{"authors":[{"text":"Desborough, G. A.","contributorId":34527,"corporation":false,"usgs":true,"family":"Desborough","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359971,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":359972,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huffman, C. Jr.","contributorId":20064,"corporation":false,"usgs":true,"family":"Huffman","given":"C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359970,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010350,"text":"70010350 - 1976 - The national coal-resources data system of the U.S. geological survey","interactions":[],"lastModifiedDate":"2013-01-21T16:09:12","indexId":"70010350","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"The national coal-resources data system of the U.S. geological survey","docAbstract":"The National Coal Resources Data System (NCRDS) was designed by the U.S. Geological Survey (USGS) to meet the increasing demands for rapid retrieval of information on coal location, quantity, quality, and accessibility. An interactive conversational query system devised by the USGS retrieves information from the data bank through a standard computer terminal. The system is being developed in two phases. Phase I, which currently is available on a limited basis, contains published areal resource and chemical data. The primary objective of this phase is to retrieve, calculate, and tabulate coal-resource data by area on a local, regional, or national scale. Factors available for retrieval include: state, county, quadrangle, township, coal field, coal bed, formation, geologic age, source and reliability of data, and coal-bed rank, thickness, overburden, and tonnage, or any combinations of variables. In addition, the chemical data items include individual values for proximate and ultimate analyses, BTU value, and several other physical and chemical tests. Information will be validated and deleted or updated as needed. Phase II is being developed to store, retrieve, and manipulate basic point source coal data (e.g., field observations, drill-hole logs), including geodetic location; bed thickness; depth of burial; moisture; ash; sulfur; major-, minor-, and trace-element content; heat value; and characteristics of overburden, roof rocks, and floor rocks. The computer system may be used to generate interactively structure-contour or isoline maps of the physical and chemical characteristics of a coal bed or to calculate coal resources. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90062-5","issn":"00983004","usgsCitation":"Carter, M., 1976, The national coal-resources data system of the U.S. geological survey: Computers & Geosciences, v. 2, no. 3, p. 331-340, https://doi.org/10.1016/0098-3004(76)90062-5.","startPage":"331","endPage":"340","numberOfPages":"10","costCenters":[],"links":[{"id":219366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266209,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90062-5"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badf8e4b08c986b323e95","contributors":{"authors":[{"text":"Carter, M.D.","contributorId":31382,"corporation":false,"usgs":true,"family":"Carter","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":358697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171425,"text":"70171425 - 1976 - Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","interactions":[],"lastModifiedDate":"2018-02-04T14:32:02","indexId":"70171425","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method","docAbstract":"<p>On the basis of a linear relationship between winter (October-April) precipitation and annual runoff from a drainage basin (Rasmussen and Tangborn, 1976) a physically reasonable model for predicting summer (May-September) streamflow from drainages in the North Cascades region was developed. This hydrometeorological prediction method relates streamflow for a season beginning on the day of prediction to the storage (including snow, ice, soil moisture, and groundwater) on that day. The spring storage is inferred from an input-output relationship based on the principle of conservation of mass: spring storage equals winter precipitation on the basin less winter runoff from the basin and less winter evapotranspiration, which is presumed to be small. The method of prediction is based on data only from the years previous to the one for which the prediction is made, and the system is revised each year as data for the previous year become available. To improve the basin storage estimate made in late winter or early spring, a short-season runoff prediction is made. The errors resulting from this short-term prediction are used to revise the storage estimate and improve the later prediction. This considerably improves the accuracy of the later prediction, especially for periods early in the summer runoff season. The optimum length for the test period appears to be generally less than a month for east side basins and between 1 and 2 months for those on the west side of the Cascade Range. The time distribution of the total summer runoff can be predicted when this test season is used so that on May 1 monthly streamflow for the May-September season can be predicted. It was found that summer precipitation and the time of minimum storage are two error sources that were amenable to analysis. For streamflow predictions in seasons beginning in early spring the deviation of the subsequent summer precipitation from a long-period average will contribute up to 53% of the prediction error. This contribution decreases to nearly zero during the summer and then rises slightly for late summer predictions. The reason for the smaller than expected effect of summer precipitation is thought to be due to the compensating effect of increased evaporative losses and increased infiltration when precipitation is greater than normal during the summer months. The error caused by the beginning winter month (assumed to be October in this study) not coinciding with the time of minimum storage was examined; it appears that October may be the best average beginning winter month for most drainages but that a more detailed study is needed. The optimum beginning of the winter season appears to vary from August to October when individual years are examined. These results demonstrate that standard precipitation and runoff measurements in the North Cascades region are adequate for constructing a predictive hydrologic model. This model can be used to make streamflow predictions that compare favorably with current multiple regression methods based on mountain snow surveys. This method has the added advantages of predicting the space and time distributions of storage and summer runoff.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR012i002p00203","usgsCitation":"Tangborn, W.V., and Rasmussen, L.A., 1976, Hydrology of the North Cascades region, Washington: 2. A proposed hydrometeorological streamflow prediction method: Water Resources Research, v. 12, no. 2, p. 203-216, https://doi.org/10.1029/WR012i002p00203.","productDescription":"14 p.","startPage":"203","endPage":"216","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321911,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cascade 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,{"id":70045449,"text":"70045449 - 1976 - Hydrologic data for urban studies in the Austin, Texas Metropolitan Area, 1974","interactions":[],"lastModifiedDate":"2016-08-10T16:21:15","indexId":"70045449","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Hydrologic data for urban studies in the Austin, Texas Metropolitan Area, 1974","docAbstract":"<p>The purpose of this report is to present rainfall and runoff data for the Waller Creek and Wilbarger Creek study areas for the 1974 water year (October 1, 1973 to September 30, 1974).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70045449","collaboration":"Prepared in cooperation with the Texas  Water Development Board","usgsCitation":"Mitchell, R., 1976, Hydrologic data for urban studies in the Austin, Texas Metropolitan Area, 1974: Open-File Report, 60 p., https://doi.org/10.3133/70045449.","productDescription":"60 p.","numberOfPages":"59","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1973-10-01","temporalEnd":"1974-09-30","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":272737,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045449/report.pdf"},{"id":271012,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045449/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72ece4b00154e4368c0a","contributors":{"authors":[{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":477513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39604,"text":"pp964 - 1976 - A land use and land cover classification system for use with remote sensor data","interactions":[],"lastModifiedDate":"2025-03-31T20:29:22.250598","indexId":"pp964","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"964","title":"A land use and land cover classification system for use with remote sensor data","docAbstract":"The framework of a national land use and land cover classification system is\r\npresented for use with remote sensor data. The classification system has been\r\ndeveloped to meet the needs of Federal and State agencies for an up-to-date\r\noverview of land use and land cover throughout the country on a basis that is\r\nuniform in categorization at the more generalized first and second levels and\r\nthat will be receptive to data from satellite and aircraft remote sensors. The\r\nproposed system uses the features of existing widely used classification\r\nsystems that are amenable to data derived from remote sensing sources. It is\r\nintentionally left open-ended so that Federal, regional, State, and local\r\nagencies can have flexibility in developing more detailed land use\r\nclassifications at the third and fourth levels in order to meet their\r\nparticular needs and at the same time remain compatible with each other and\r\nthe national system. Revision of the land use classification system as presented in U.S. Geological Survey Circular 671 was undertaken in order to\r\nincorporate the results of extensive testing and review of the categorization\r\nand definitions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp964","usgsCitation":"Anderson, J.R., Hardy, E.E., Roach, J.T., and Witmer, R.E., 1976, A land use and land cover classification system for use with remote sensor data: U.S. Geological Survey Professional Paper 964, iii, 28 p., https://doi.org/10.3133/pp964.","productDescription":"iii, 28 p.","costCenters":[{"id":360,"text":"Land Cover Institute","active":false,"usgs":true}],"links":[{"id":67189,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0964/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170065,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0964/report-thumb.jpg"}],"publicComments":"A revision of the land use classification system in Circular 671","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae412","contributors":{"authors":[{"text":"Anderson, James R.","contributorId":20213,"corporation":false,"usgs":true,"family":"Anderson","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":221768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardy, Ernest E.","contributorId":40202,"corporation":false,"usgs":true,"family":"Hardy","given":"Ernest","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roach, John T.","contributorId":104480,"corporation":false,"usgs":true,"family":"Roach","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":221771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Witmer, Richard E.","contributorId":59472,"corporation":false,"usgs":true,"family":"Witmer","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":221770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":67964,"text":"ha570 - 1976 - Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T13:40:21","indexId":"ha570","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"570","title":"Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Menan Buttes quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha570","usgsCitation":"Thomas, C., Ray, H.A., and Harenberg, W.A., 1976, Teton Dam flood of June 1976, Menan Buttes quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 570, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha570.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":185733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89193,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/570/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Menan Buttes Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.0,43.75 ], [ -112.0,43.875 ], [ -111.875,43.875 ], [ -111.875,43.75 ], [ -112.0,43.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684660","contributors":{"authors":[{"text":"Thomas, Cecil A.","contributorId":107373,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil A.","affiliations":[],"preferred":false,"id":277410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ray, Herman A.","contributorId":106199,"corporation":false,"usgs":true,"family":"Ray","given":"Herman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277409,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harenberg, William A.","contributorId":31773,"corporation":false,"usgs":true,"family":"Harenberg","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277408,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56786,"text":"wdrMDDE742 - 1975 - Water resources data Maryland and Delaware, water year 1974, Part 2. Water quality records","interactions":[],"lastModifiedDate":"2021-01-22T19:28:04.499782","indexId":"wdrMDDE742","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-74-2","displayTitle":"Water Resources Data Maryland and Delaware, Water Year 1974, Part 2. Water Quality Records","title":"Water resources data Maryland and Delaware, water year 1974, Part 2. Water quality records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE742","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data Maryland and Delaware, water year 1974, Part 2. Water quality records: U.S. Geological Survey Water Data Report MD-DE-74-2, 127 p., https://doi.org/10.3133/wdrMDDE742.","productDescription":"127 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":175199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1974/md-de-74-2/wdrMDDE742_coverthb.jpg"},{"id":381772,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/md-de-74-2/wdrMDDE742.pdf","text":"Report","size":"4.89 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-74-2"}],"country":"United States","state":"Delaware, 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4395","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180024,"text":"70180024 - 1975 - Developing a state water plan: Ground-water conditions in Utah, spring of 1975","interactions":[],"lastModifiedDate":"2017-01-23T12:56:32","indexId":"70180024","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1975","docAbstract":"<p>This report is the twelfth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.</p><p>This report, like the others (see references, p. 16), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1974. Water-level fluctuations, however, are described for the period spring 1974 to spring 1975. Many of the data used in the report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Eychaner, J.H., Jibson, W., Bolke, E., Mower, R.W., Herbert, L.R., Cordova, R., Jensen, V., ReMillard, M.D., Sandberg, G.W., Sumison, C., and Bjorklund, L., 1975, Developing a state water plan: Ground-water conditions in Utah, spring of 1975: Cooperative Investigations Report, viii, 64 p.","productDescription":"viii, 64 p.","numberOfPages":"72","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333713,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333712,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-190"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248fe4b08aa8f945abfe","contributors":{"authors":[{"text":"Eychaner, James H.","contributorId":102050,"corporation":false,"usgs":true,"family":"Eychaner","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":659848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":659849,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659850,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659851,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659852,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659853,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659854,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659855,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659856,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659857,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659858,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70178959,"text":"70178959 - 1975 - 1974 earthquake summary reported by the National Earthquake Information Service","interactions":[],"lastModifiedDate":"2016-12-14T11:42:00","indexId":"70178959","displayToPublicDate":"2016-06-15T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"1974 earthquake summary reported by the National Earthquake Information Service","docAbstract":"<p>For the second consecutive year, earthquake activity in the United States and around the world was below the long term average according to the National Earthquake Information Service (NEIS) in Golden, Colorado. However, more than 5,300 earthquake-related deaths were reported in 1974, up sharply from the approximately 650 deaths in 1973. On the basis of data collected by nearly 600 cooperating seismograph stations around the world, the NEIS reported 13 major shocks and no great shocks as compared with a long term average of 18 major and one great earthquake per year.<br></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1975, 1974 earthquake summary reported by the National Earthquake Information Service: Earthquake Information Bulletin (USGS), v. 7, no. 2, p. 21-23.","productDescription":"3 p.","startPage":"21","endPage":"23","numberOfPages":"3","costCenters":[],"links":[{"id":331959,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584fc56ee4b00645734c5413","contributors":{"editors":[{"text":"Mallis, Robert","contributorId":77935,"corporation":false,"usgs":true,"family":"Mallis","given":"Robert","email":"","affiliations":[],"preferred":false,"id":655631,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":70042719,"text":"70042719 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","interactions":[{"subject":{"id":14933,"text":"ofr75304 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","indexId":"ofr75304","publicationYear":"1975","noYear":false,"title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70042719,"text":"70042719 - 1975 - A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","indexId":"70042719","publicationYear":"1975","noYear":false,"title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin"},"id":1}],"lastModifiedDate":"2013-01-18T15:34:06","indexId":"70042719","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":259,"text":"Information Circular","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"30","title":"A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin","docAbstract":"The extensive use of ground water for water supply within Dane County has resulted in the need for an appraisal of the area's ground-water resources. Water-resources planners and other water-oriented groups have expressed concern over ground-water level declines and reductions in streamflow that are occurring as a result of heavy pumping. Digital-computer modeling techniques were used to estimate hydrologic changes in the aquifer system that would be caused by continued development. The system was modeled as a two-aquifer system consisting of a confined sandstone aquifer overlain by a leaky unconfined aquifer and underlain by impermeable bedrock. The physical properties of the aquifer system needed for the model were approximated using aquifer-test data and well-log data and by matching observed hydrologic changes in the system with corresponding changes computed by the model. Computed hydrologic changes do not represent a serious depletion of the available ground-water supply for the foreseeable future. Maximum added regional declines in ground-water levels (drawdowns) from 1970 to 1990 were computed to be approximately 10 feet (3 metres) in the unconfined aquifer and approximately 40 feet (12 metres) in the confined aquifer. It is computed that for the same period the average annual streamflow from the upper Yahara River basin would be reduced by approximately 29 cubic feet per second (0.82 cubic metre per second). These changes are computed based on estimated development trends for the confined sandstone aquifer.","language":"English","publisher":"Wisconsin Geological and Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by the United States Department of the Interior Geological Survey in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"McLeod, R., 1975, A digital-computer model for estimating hydrologic changes in the aquifer system in Dane County, Wisconsin: Information Circular 30, vii, 40 p.; ill.; maps.","productDescription":"vii, 40 p.; ill.; maps","startPage":"i","endPage":"40","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":265977,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265976,"type":{"id":11,"text":"Document"},"url":"https://wisconsingeologicalsurvey.org/pdfs/IC30.pdf"}],"country":"United States","state":"Wisconsin","county":"Dane County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.8394,42.8448 ], [ -89.8394,43.2943 ], [ -89.0084,43.2943 ], [ -89.0084,42.8448 ], [ -89.8394,42.8448 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d34e4b061045bf9aba5","contributors":{"authors":[{"text":"McLeod, R.S.","contributorId":7283,"corporation":false,"usgs":true,"family":"McLeod","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":472112,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038737,"text":"wri5175 - 1975 - Flood of July 21, 1975 in Mercer County, New Jersey","interactions":[],"lastModifiedDate":"2012-06-19T01:01:45","indexId":"wri5175","displayToPublicDate":"2012-06-18T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"51-75","title":"Flood of July 21, 1975 in Mercer County, New Jersey","docAbstract":"Intense rainfall during the evening of July 20 and early morning hours of July 21, 1975 caused flooding of unprecedented magnitude in highly urbanized Mercer County, New Jersey. Over 6 inches (152 millimetres) of rainfall was recorded during a 10-hour period at Trenton, the capital of New Jersey. No lives were lost but damages to highways and bridges, to industrial, business, and residential buildings, to farmlands and crops, and to water supply systems were severe. This report illustrates the magnitude of the flood and provides hydrologic data needed for planning and design to control or lessen damages from future floods. It includes discussions of the antecedent conditions and meteorological aspects of the storm; a description of the flood and comparison to previous floods; a summary of flood stages and discharges; a discussion of flood frequency; and photomosaics which show inundated areas. More than 200 high-water marks are described as to location and elevation above mean sea level.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri5175","collaboration":"Prepared in cooperation with the New Jersey Department of Environmental Protection","usgsCitation":"Stankowski, S.J., Schopp, R.D., and Velnich, A.J., 1975, Flood of July 21, 1975 in Mercer County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 51-75, vi, 69 p., https://doi.org/10.3133/wri5175.","productDescription":"vi, 69 p.","onlineOnly":"Y","temporalStart":"1975-07-20","temporalEnd":"1975-07-21","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":257660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_51_75.gif"},{"id":257659,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1975/51/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey","county":"Mercer","city":"Trenton","otherGeospatial":"Delaware River;Assunpink Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.81666666666666,40.2 ], [ -74.81666666666666,40.333333333333336 ], [ -74.56666666666666,40.333333333333336 ], [ -74.56666666666666,40.2 ], [ -74.81666666666666,40.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1116e4b0c8380cd53ee9","contributors":{"authors":[{"text":"Stankowski, Stephen J.","contributorId":31389,"corporation":false,"usgs":true,"family":"Stankowski","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":464812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schopp, Robert D.","contributorId":10426,"corporation":false,"usgs":true,"family":"Schopp","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":464810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Velnich, Anthony J.","contributorId":15263,"corporation":false,"usgs":true,"family":"Velnich","given":"Anthony","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":464811,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038682,"text":"wdrCA7411 - 1975 - Water resources data for California, 1974; Part 1: Surface water records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA7411","displayToPublicDate":"2012-06-04T10:53:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-74-1-1","title":"Water resources data for California, 1974; Part 1: Surface water records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","docAbstract":"Surface-water records for the 1974 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Lee R. Peterson, district chief. These data represent that portion of the National Water Data System collected by the Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA7411","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for California, 1974; Part 1: Surface water records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-74-1-1, xv, 495 p., https://doi.org/10.3133/wdrCA7411.","productDescription":"xv, 495 p.","temporalStart":"1973-10-01","temporalEnd":"1974-09-30","costCenters":[],"links":[{"id":257493,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1974/ca-74/WDR-1974-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":257519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_74_1_1.jpg"}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc958e4b08c986b32cce7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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