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It supplements another permanent catalog \"Publications of the Geological Survey, 1962-1970.\"","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70043703","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Publications of the Geological Survey, 1879-1961 (Fourth printing): Publications of the US Geological Survey, vi, 457 p., https://doi.org/10.3133/70043703.","productDescription":"vi, 457 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":267633,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70043703/report-thumb.jpg"},{"id":272661,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70043703/report.pdf"}],"edition":"Fourth printing","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad60e4b0b6328103b4e3","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":535409,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70030385,"text":"70030385 - 1980 - The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho","interactions":[],"lastModifiedDate":"2012-03-12T17:21:03","indexId":"70030385","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1517,"text":"Engineering Geology","active":true,"publicationSubtype":{"id":10}},"title":"The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho","docAbstract":"Silver and copper are the principal ores mined from the quartzite at the Crescent mine. Both the main ore-bearing veins and foliation in the quartzite are parallel to the nearly vertical formational contacts. Anisotropy of the quartzite is indicated by both dynamic and static tests. Disking and breakage of core from holes perpendicular to the foliation are about twice what they are in core from holes parallel to foliation. Natural cleavage as well as slabbing and blasting fractures around the tunnels are also controlled by the foliation. Extensive overcore deformation measurements indicate that most of the influence of the tunnels on the \"free\" stress field is between the rib and a depth of 2.7 m (1 tunnel diameter). The maximum principal stress axis in the free field is nearly horizontal; its magnitude is not much greater than the vertical component and calculations indicate a nearly hydrostatic free stress field. Stress considerably greater than the free field was measured between about 0.3-2.7 m behind the rib and is caused by a transfer of load from above the tunnel opening. Peak stress is in the vertical direction and about 1.7 m behind the rib. An air-injection survey shows that high permeabilities are confined to the highly fractured annulus around a tunnel to a depth of at least 0.6 m. Air-injection measurements could be taken in the interval of about 0.6-1.8 m, but more fractures with high permeabilities may also be present in the annulus from about 0.6-1.2 m. Permeabilities measured deeper than about 1.8 m by the air-injection technique are either very low or nonexistent. The absence of open and noncontinuous fractures beyond about 1.8 m is also indicated by very low porosities and permeabilities of core, very high stresses (which presumably would close fractures), the lack of stains or secondary fillings in disking fractures, a conspicuous lack of ground water in the tunnels, and the fact that fractures encountered in an experimental 0.9-m tunnel did not extend into the 1.8-m tunnel that was mined over it. Air-injection techniques exceed the accuracy of any field deformation measurement now in use, and they are sensitive to permeabilities as small as one microdarcy and to fracture widths as small as 250 nanometers. This technique was applied for future reference in mining design and, perhaps, to be used later to detect microfracturing prior to rockbursts. ?? 1980 Elsevier Scientific Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Engineering Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0013-7952(80)90021-6","issn":"00137","usgsCitation":"Miller, C., and Skinner, E., 1980, The nature of fracturing and stress distribution in quartzite around the 1128-M (3700-FT) level of the crescent mine, Coeur d'Alene mining district, Idaho: Engineering Geology, v. 16, no. 3-4, p. 321-338, https://doi.org/10.1016/0013-7952(80)90021-6.","startPage":"321","endPage":"338","numberOfPages":"18","costCenters":[],"links":[{"id":239302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":211921,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0013-7952(80)90021-6"}],"volume":"16","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae04e4b08c986b323eb9","contributors":{"authors":[{"text":"Miller, C.H.","contributorId":19148,"corporation":false,"usgs":true,"family":"Miller","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":426948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, E.H.","contributorId":31978,"corporation":false,"usgs":true,"family":"Skinner","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":426949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":81418,"text":"81418 - 1980 - Fish-stock assessment in the Great Lakes","interactions":[],"lastModifiedDate":"2023-03-29T16:22:18.474146","indexId":"81418","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Fish-stock assessment in the Great Lakes","docAbstract":"

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Computer simulation experiments were conducted to determine the effects of alternative sources of uncertainty on the willingness to pay for flood insurance. Two alternative insurance protection schemes were investigated: coinsurance and fixed coverage. The question investigated here is to what extent does the insurance scheme influence how purchasers respond to flood risks? Floods were assumed to be log normally distributed and the effects on the purchase of insurance of uncertainties in the parameters of the distribution were explored using response surface analysis. Results indicate that fixed coverage insurance provisions shift most of the uncertainty in the physical parameters governing natural disaster occurrences away from the insuree and onto the insurer. The results also show that the form of the damage function has little effect on the demand for flood insurance.

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No abstract available.

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The US Geological Survey has initiated a project to prepare a satellite image atlas of glaciers with the cooperation of a number of US and international organizations. The atlas will include the geographical distribution of glaciers as well as topics of glaciology and related environmental phenomena using Landsat, NOAA and other satellite data. The primary objectives of the atlas are to provide an inventory of available images of extant glaciers, to demonstrate their scientific value and to serve as the basis of Landsat image maps of glacierized areas.

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No abstract available.

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\"}}]}","contact":"

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","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdf8","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":533120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180028,"text":"70180028 - 1979 - Developing a state water plan: Ground-water conditions in Utah, spring of 1979","interactions":[],"lastModifiedDate":"2017-01-23T13:08:35","indexId":"70180028","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1979","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}},"seriesNumber":"18","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1979","docAbstract":"

This report is the sixteenth 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 to keep abreast of changing ground-water conditions.

This report, like the others in the series, 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.

This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1978. Water-level fluctuations, however, are described for the period spring 1978 to spring 1979. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.

","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":"Price, D., Jibson, W., Contratto, P., Mower, R.W., Steiger, J.I., Jensen, V., ReMillard, M.D., Emett, D.C., Sumison, C., Carroll, P., Neff, L., Sandberg, G.W., and Herbert, L.R., 1979, Developing a state water plan: Ground-water conditions in Utah, spring of 1979: Cooperative Investigations Report 18, vi, 68 p.","productDescription":"vi, 68 p.","numberOfPages":"76","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333720,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-186"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248be4b08aa8f945abf6","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":659892,"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":659893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Contratto, P. Kay","contributorId":15598,"corporation":false,"usgs":true,"family":"Contratto","given":"P. Kay","affiliations":[],"preferred":false,"id":659894,"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":659895,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Steiger, Judy I. jsteiger@usgs.gov","contributorId":3689,"corporation":false,"usgs":true,"family":"Steiger","given":"Judy","email":"jsteiger@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":659896,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659897,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"ReMillard, M. 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C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659899,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659900,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Carroll, P.A.","contributorId":178594,"corporation":false,"usgs":false,"family":"Carroll","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":659901,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Neff, L.J.","contributorId":178596,"corporation":false,"usgs":false,"family":"Neff","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659902,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sandberg, G. 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R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659904,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}} ,{"id":70176376,"text":"70176376 - 1979 - Seismology on Mars","interactions":[],"lastModifiedDate":"2016-09-12T01:51:08","indexId":"70176376","displayToPublicDate":"2016-04-12T00:00:00","publicationYear":"1979","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":"Seismology on Mars","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1979, Seismology on Mars: Earthquake Information Bulletin (USGS), v. 11, no. 4, p. 120-126.","productDescription":"7 p.","startPage":"120","endPage":"126","numberOfPages":"7","costCenters":[],"links":[{"id":328488,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Chryse Planitia and Utopia Planitia, distinct surfaces on the planet Mars","volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d6802be4b090824ff87a98"} ,{"id":70176375,"text":"70176375 - 1979 - Seismic gaps: Some questions and answers","interactions":[],"lastModifiedDate":"2016-09-12T01:42:00","indexId":"70176375","displayToPublicDate":"2016-04-05T00:00:00","publicationYear":"1979","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":"Seismic gaps: Some questions and answers","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1979, Seismic gaps: Some questions and answers: Earthquake Information Bulletin (USGS), v. 11, no. 6, p. 221-223.","productDescription":"3 p.","startPage":"221","endPage":"223","numberOfPages":"3","costCenters":[],"links":[{"id":328487,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d6802be4b090824ff87a96"} ,{"id":70176377,"text":"70176377 - 1979 - Understanding seismicity within the continents","interactions":[],"lastModifiedDate":"2016-09-12T02:02:04","indexId":"70176377","displayToPublicDate":"2016-02-17T00:00:00","publicationYear":"1979","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":"Understanding seismicity within the continents","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1979, Understanding seismicity within the continents: Earthquake Information Bulletin (USGS), v. 11, no. 3, p. 80-88.","productDescription":"9 p.","startPage":"80","endPage":"88","numberOfPages":"9","costCenters":[],"links":[{"id":328489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d6802ce4b090824ff87a9e"} ,{"id":70176378,"text":"70176378 - 1979 - Memorial: Perry Byerly","interactions":[],"lastModifiedDate":"2016-09-12T02:06:49","indexId":"70176378","displayToPublicDate":"2016-01-13T00:00:00","publicationYear":"1979","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":"Memorial: Perry Byerly","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Bolt, B.A., 1979, Memorial: Perry Byerly: Earthquake Information Bulletin (USGS), v. 11, no. 1, p. 30-31.","productDescription":"2 p.","startPage":"30","endPage":"31","numberOfPages":"2","costCenters":[],"links":[{"id":328490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57d6802ae4b090824ff87a91","contributors":{"editors":[{"text":"Spall, Henry","contributorId":77933,"corporation":false,"usgs":true,"family":"Spall","given":"Henry","email":"","affiliations":[],"preferred":false,"id":648563,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Bolt, B. A.","contributorId":152427,"corporation":false,"usgs":false,"family":"Bolt","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":648562,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175247,"text":"70175247 - 1979 - Trace metal bioavailability: Modeling chemical and biological interactions of sediment-bound zinc","interactions":[],"lastModifiedDate":"2016-08-03T10:46:39","indexId":"70175247","displayToPublicDate":"2015-12-16T02:15:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"26","title":"Trace metal bioavailability: Modeling chemical and biological interactions of sediment-bound zinc","docAbstract":"

Extractable concentrations of sediment-bound Zn, as modified by the physicochemical form of the metal in the sediments, controlled Zn concentrations in the deposit-feeding bivalvesScrobicularia plana (collected from 40 stations in 17 estuaries in southwest England) andMacoma balthica (from 28 stations in San Francisco Bay). Over a wide range of concentrations, a significant correlation was found between ammonium acetate-soluble concentrations of Zn in sediments and Zn concentrations in Scrobicularia. This correlation was insufficiently precise to be of predictive value for Scrobicularia, and did not hold for Macoma over the narrower range of Zn concentrations observed in San Francisco Bay. Strong correlation of Zn concentrations inScrobicularia and the bioavailability of sediment-bound Zn to Macoma with ratios of sorption substrate (oxides of iron and manganese, organic carbon, carbonates, humic materials) concentrations in sediments were found in both the English and San Francisco Bay study areas. These correlations were attributed to substrate competition for sorption of Zn within sediments, assuming: 1) competition for sorption of Zn was largely controlled by the relative concentrations of substrates present in the sediments and 2) the bioavailability of Zn to the deposit feeders was determined by the partitioning of Zn among the substrates. The correlations indicated that the availability of Zn to the bivalves increased when concentrations of either amorphous inorganic oxides or humic substances increased in sediments. Availability was reduced at increased concentrations of organic carbon and, in San Francisco Bay, ammonium acetate-soluble Mn. Concentrations of biologically available Zn in solution and low salinities may also have enhanced Zn uptake, although the roles of these variables were less obvious from the statistical analysis.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Chemical Modeling in Aqueous Systems","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Chemical Society Publications","publisherLocation":"Washington, D.C.","doi":"10.1021/bk-1979-0093.ch026","usgsCitation":"Luoma, S.N., and Bryan, G., 1979, Trace metal bioavailability: Modeling chemical and biological interactions of sediment-bound zinc, chap. 26 of Chemical Modeling in Aqueous Systems, p. 577-609, https://doi.org/10.1021/bk-1979-0093.ch026.","productDescription":"33 p.","startPage":"577","endPage":"609","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":326020,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2009-07-23","publicationStatus":"PW","scienceBaseUri":"57a315d4e4b006cb45558bb7","contributors":{"editors":[{"text":"Jenne, Everett A.","contributorId":85582,"corporation":false,"usgs":true,"family":"Jenne","given":"Everett","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":644542,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Luoma, S. N.","contributorId":120222,"corporation":false,"usgs":true,"family":"Luoma","given":"S.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":644540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryan, G.W.","contributorId":84402,"corporation":false,"usgs":true,"family":"Bryan","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":644541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70159096,"text":"70159096 - 1979 - Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2015-10-22T10:20:52","indexId":"70159096","displayToPublicDate":"2015-07-14T13:15:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada","docAbstract":"

The UE25a-3 drill hole, located in the Calico Hills area, southwestern part of the Nevada Test Site, was drilled as part of an effort to evaluate the Calico Hills area as a possible nuclear waste repository site. The purpose of the drill hole was to verify the existence of an intrusive crystalline body in the subsurface and to determine the stratigraphy, structure, and nature of fractures of the cored rocks. Cored samples were obtained for mineral, chemical, and material property analyses.

\n

Continuous cores were taken from 30.5 m (100ft) to total depth of 771.2 m (2,530.1 ft) of units J and I{?) (Late Mississippian age) of the Eleana Formation. The drill hole penetrated 416.1 m (1 ,365ft) of argillite, and 304.5 m (999ft) of thermally altered argillite of unit J, and 50.6 m (166ft) of marble of unit I(?). No crystalline rocks were intersected by the drill hole.

\n

Numerous high-angle faults and brecciated zones were intersected by the drill hole. The units cored were intensely fractured with fracture analysis of the core consisting of frequency of fractures, dips of fractures, open and closed (sealed) fractures and types of fracture sealing or coating material. Twenty-four hundred and thirty fractures, representing approximately 30 percent of the fractures present, indicate an average fracture frequency of 13.2 fractures per meter, predominantly high-angle dips with 66 percent of the fractures closed. Fractures in the argillite interval are sealed or coated predominantly with kaolinite, nacrite, and dickite. Calcite, chlorite, and magnetite are present in fractures in the altered argillite interval. Fractures in the marble interval are sealed or coated with calcite, dolomite, and ferruginous clay. The core index indicates that the lower half of the drilled interval is more competent than the upper half.

\n

Borehole geophysical logs were run by the Birdwell Division of Seismograph Service Corporation for geologic correlations and lithologic characterizations. The logs include: caliper, density, resistivity, spontaneous potential, Vibroseis, 3-D velocity, neutron, and gamma-ray logs. Lithologic boundaries and structures correlate to responses in the logs.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70159096","usgsCitation":"Maldonado, F., Muller, D.C., and Morrison, J., 1979, Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada, Report: iii, 43 p.; 1 Plate: 18.94 x 34.10 inches, https://doi.org/10.3133/70159096.","productDescription":"Report: iii, 43 p.; 1 Plate: 18.94 x 34.10 inches","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159096.jpg"},{"id":310369,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159096/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}},{"id":310368,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159096/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Calico Hills","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.93847656250001,\n 37.01132594307015\n ],\n [\n -114.85107421875,\n 35.36217605914681\n ],\n [\n -114.268798828125,\n 35.44277092585766\n ],\n [\n -114.3017578125,\n 37.09023980307208\n ],\n [\n -114.32373046875,\n 37.87485339352928\n ],\n [\n -114.444580078125,\n 38.25543637637947\n ],\n [\n -114.70825195312501,\n 38.736946065676\n ],\n [\n -117.8173828125,\n 38.71980474264239\n ],\n [\n -118.68530273437501,\n 38.38472766885085\n ],\n [\n -116.93847656250001,\n 37.01132594307015\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce8fe4b06217fc478b08","contributors":{"authors":[{"text":"Maldonado, Florian fmaldona@usgs.gov","contributorId":805,"corporation":false,"usgs":true,"family":"Maldonado","given":"Florian","email":"fmaldona@usgs.gov","affiliations":[],"preferred":true,"id":577591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muller, D. 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It is an area long used for outdoor recreation and includes a part of the Delaware Water Gap National Recreation Area. Water resources in the county are derived from precipitation. 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G.","affiliations":[],"preferred":false,"id":482216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047437,"text":"70047437 - 1979 - Geology and groundwater resources of western Crawford County, Pennsylvania","interactions":[{"subject":{"id":11017,"text":"ofr78204 - 1978 - Geology and hydrology of western Crawford County, Pennsylvania","indexId":"ofr78204","publicationYear":"1978","noYear":false,"title":"Geology and hydrology of western Crawford County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047437,"text":"70047437 - 1979 - Geology and groundwater resources of western Crawford County, Pennsylvania","indexId":"70047437","publicationYear":"1979","noYear":false,"title":"Geology and groundwater resources of western Crawford County, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T10:01:43","indexId":"70047437","displayToPublicDate":"2013-01-01T09:42:37","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"46","title":"Geology and groundwater resources of western Crawford County, Pennsylvania","docAbstract":"Western Crawford County is in northwestern Pennsylvania. The project area is 15 to 20 miles south of Lake Erie and is bordered on the west by Ohio. Drift of Pleistocene age (Wisconsinan Age) covers most of the area, which is a maturely dissected plateau. The drift in the upland area is mostly till, which ranges in thickness from 0 to 25 feet. In the large stream valleys and deep buried valleys the drift is as much as 500 feet thick. The bedrock was mapped in detail and consists of rocks of Devonian, Mississippian, and Pennsylvanian age. Devonian rocks underlie the entire area and form the bedrock surface in most of the northern one third of the area and in the deep bedrock valleys. Mississippian formations underlie the uplands in the southern two thirds of the area; these are capped by thin remnants of Pennsylvanian rocks and knobs near the south edge of the area.","language":"English","publisher":"Pennsylvania Geological Survey","collaboration":"Prepared by the United States Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Schiner, G.R., and Gallaher, J.T., 1979, Geology and groundwater resources of western Crawford County, Pennsylvania: Water Resource Report 46, vii, 103 p.; Maps: 3 Sheets.","productDescription":"vii, 103 p.; Maps: 3 Sheets","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047437.PNG"},{"id":276096,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_015547.zip"}],"country":"United States","state":"Pennsylvania","county":"Crawford County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.519758,41.481003 ], [ -80.519758,41.851089 ], [ -79.613419,41.851089 ], [ -79.613419,41.481003 ], [ -80.519758,41.481003 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae4e4b0e21cafa49c53","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gallaher, John T.","contributorId":11585,"corporation":false,"usgs":true,"family":"Gallaher","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":482041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046176,"text":"70046176 - 1979 - Environment of ore deposition in the Creede mining district, San Juan Mountains, Colorado; Part IV, source of fluids, from oxygen, hydrogen, and carbon isotope studies","interactions":[{"subject":{"id":7888,"text":"ofr791243 - 1979 - Environment of ore deposition in the Creede Mining District, San Juan Mountains, Colorado: Part IV, Sources of fluids from oxygen, hydrogen, and carbon isotopic studies","indexId":"ofr791243","publicationYear":"1979","noYear":false,"title":"Environment of ore deposition in the Creede Mining District, San Juan Mountains, Colorado: Part IV, Sources of fluids from oxygen, hydrogen, and carbon isotopic studies"},"predicate":"SUPERSEDED_BY","object":{"id":70046176,"text":"70046176 - 1979 - Environment of ore deposition in the Creede mining district, San Juan Mountains, Colorado; Part IV, source of fluids, from oxygen, hydrogen, and carbon isotope studies","indexId":"70046176","publicationYear":"1979","noYear":false,"title":"Environment of ore deposition in the Creede mining district, San Juan Mountains, Colorado; Part IV, source of fluids, from oxygen, hydrogen, and carbon isotope studies"},"id":1}],"lastModifiedDate":"2022-12-23T15:35:57.750823","indexId":"70046176","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Environment of ore deposition in the Creede mining district, San Juan Mountains, Colorado; Part IV, source of fluids, from oxygen, hydrogen, and carbon isotope studies","docAbstract":"The hydrogen isotopic composition of fluids responsible for formation of the near-surface silver-base metal vein deposits at Creede was measured by direct analysis of inclusion fluids in sphalerite, quartz, and rhodochrosite and was estimated from analyses of illite and chlorite. The oxygen isotopic composition was determined directly on inclusion fluids in sphalerite and was estimated from analyses of quartz, illite, rhodochrosite, siderite, and adularia. The carbon isotopic composition was estimated from analyses of rhodochrosite and siderite. The ranges in isotopic composition for water and CO2 in the fluids associated with the formation of each of the minerals is given below (number of determinations given in parentheses):Mineral delta D (sub H2) O ppm delta 18 O (sub H2) O ppm delta 13 C (sub CO2) ppmSphalerite -81 to -54 (4) -10.1 to -4.5 (4)Quartz -97 to -86 (4) -5.9 to 1.8 (18)Illite -62 to -50 (8) -1.6 to 1.2(7)Chlorite -64 to -55 (10) -2.2 to 0.8 (10)Adularia 4.2 (1)Rhodochrosite -82 to -78 (2) 4.2 to 9.4 (9) -5.7 to -4.2 (9)Siderite 4.9 to 9.9 (6) -6.9 to -2.7 (6)The delta D (sub H2) O and delta 18 O (sub H2) O values of fluids associated with the formation of sphalerite, quartz, illite/chlorite, and carbonate minerals differ substantially from one another, and these differences appear to have been maintained throughout the depositional history, regardless of the positions of the minerals in the paragenetic sequence.The data suggest that waters from three coexisting reservoirs fed the vein system alternately and episodically during vein formation, and apparently there was little mixing of the fluids from the different reservoirs. The hydrogen, oxygen, and carbon isotope data suggest that the carbonate waters were deep seated, probably dominantly magmatic, in origin. The sphalerite and illite/chlorite waters must have been dominantly meteoric in origin and substantially oxygen shifted by exchange with the volcanic country rocks. The quartz waters were also oxygen shifted meteoric waters but were some 40 per mil lower in deuterium content than the sphalerite and illite/chlorite waters.We propose that the quartz fluids entered the vein system from reservoirs beneath the mountainous areas to the north in the vicinity of the present Continental Divide, but that the sphalerite and illite/chlorite fluids entered the vein system from a topographically low area to the south along the structural moat of the Creede caldera. The difference in delta D between the two meteoric waters may reflect differences in altitude of the recharge areas for the two reservoirs or may be clue to isotopic evolution of the closed-basin lake and interstitial waters in the moat surrounding the Creede caldera.","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.74.8.1832","usgsCitation":"Bethke, P.M., and Rye, R.O., 1979, Environment of ore deposition in the Creede mining district, San Juan Mountains, Colorado; Part IV, source of fluids, from oxygen, hydrogen, and carbon isotope studies: Economic Geology, v. 74, no. 8, p. 1832-1851, https://doi.org/10.2113/gsecongeo.74.8.1832.","productDescription":"20 p.","startPage":"1832","endPage":"1851","costCenters":[],"links":[{"id":272978,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"San Juan Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.14,37.0 ], [ -108.14,38.2 ], [ -105.86,38.2 ], [ -105.86,37.0 ], [ -108.14,37.0 ] ] ] } } ] }","volume":"74","issue":"8","noUsgsAuthors":false,"publicationDate":"1979-12-01","publicationStatus":"PW","scienceBaseUri":"51a72366e4b09db86f875ccd","contributors":{"authors":[{"text":"Bethke, P. M.","contributorId":32921,"corporation":false,"usgs":true,"family":"Bethke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":479094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, R. O.","contributorId":66208,"corporation":false,"usgs":true,"family":"Rye","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":479095,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046237,"text":"70046237 - 1979 - White Marsh Quadrangle: geology, hydrology, and mineral resources","interactions":[{"subject":{"id":46945,"text":"ofr74347 - 1974 - Environmental geohydrology, folio No.1 (White Marsh 7 1/2-minute quadrangle)","indexId":"ofr74347","publicationYear":"1974","noYear":false,"title":"Environmental geohydrology, folio No.1 (White Marsh 7 1/2-minute quadrangle)"},"predicate":"SUPERSEDED_BY","object":{"id":70046237,"text":"70046237 - 1979 - White Marsh Quadrangle: geology, hydrology, and mineral resources","indexId":"70046237","publicationYear":"1979","noYear":false,"title":"White Marsh Quadrangle: geology, hydrology, and mineral resources"},"id":1}],"lastModifiedDate":"2013-06-03T15:05:05","indexId":"70046237","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":279,"text":"Quadrangle Atlas","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"4","title":"White Marsh Quadrangle: geology, hydrology, and mineral resources","language":"English","publisher":"Maryland Geological Survey","publisherLocation":"Baltimore, MD","usgsCitation":"Cleaves, E.T., Kuff, K.R., Otton, E.G., Crowley, W.P., and Reinhardt, J., 1979, White Marsh Quadrangle: geology, hydrology, and mineral resources: Quadrangle Atlas 4, Maps: 8 Sheets.","productDescription":"Maps: 8 Sheets","costCenters":[],"links":[{"id":273119,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryl","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.6,39.3 ], [ -76.6,39.6 ], [ -76.3,39.6 ], [ -76.3,39.3 ], [ -76.6,39.3 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51adbaece4b07c214e64bd5a","contributors":{"authors":[{"text":"Cleaves, Emery T.","contributorId":80249,"corporation":false,"usgs":true,"family":"Cleaves","given":"Emery","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":479256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuff, Karen R.","contributorId":30896,"corporation":false,"usgs":true,"family":"Kuff","given":"Karen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":479254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Otton, Edmond G.","contributorId":96989,"corporation":false,"usgs":true,"family":"Otton","given":"Edmond","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":479258,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crowley, William P.","contributorId":60521,"corporation":false,"usgs":true,"family":"Crowley","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":479255,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reinhardt, Juergen","contributorId":88714,"corporation":false,"usgs":true,"family":"Reinhardt","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":479257,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70042713,"text":"70042713 - 1979 - Atlas of Mars: the 1:5,000,000 map series","interactions":[{"subject":{"id":12603,"text":"ofr7483 - 1974 - Mapping the planet Mars by Mariner 9","indexId":"ofr7483","publicationYear":"1974","noYear":false,"title":"Mapping the planet Mars by Mariner 9"},"predicate":"SUPERSEDED_BY","object":{"id":70042713,"text":"70042713 - 1979 - Atlas of Mars: the 1:5,000,000 map series","indexId":"70042713","publicationYear":"1979","noYear":false,"title":"Atlas of Mars: the 1:5,000,000 map series"},"id":1},{"subject":{"id":12604,"text":"ofr7320 - 1973 - Mars cartography: the 1:5,000,000 map series","indexId":"ofr7320","publicationYear":"1973","noYear":false,"title":"Mars cartography: the 1:5,000,000 map series"},"predicate":"SUPERSEDED_BY","object":{"id":70042713,"text":"70042713 - 1979 - Atlas of Mars: the 1:5,000,000 map series","indexId":"70042713","publicationYear":"1979","noYear":false,"title":"Atlas of Mars: the 1:5,000,000 map series"},"id":2},{"subject":{"id":41645,"text":"ofr74134 - 1974 - Atlas of Mars; Mariner 9, \"B\" camera pictures, indexed by 1:5,000,000 scale quadrangles","indexId":"ofr74134","publicationYear":"1974","noYear":false,"title":"Atlas of Mars; Mariner 9, \"B\" camera pictures, indexed by 1:5,000,000 scale quadrangles"},"predicate":"SUPERSEDED_BY","object":{"id":70042713,"text":"70042713 - 1979 - Atlas of Mars: the 1:5,000,000 map series","indexId":"70042713","publicationYear":"1979","noYear":false,"title":"Atlas of Mars: the 1:5,000,000 map series"},"id":3},{"subject":{"id":41652,"text":"ofr74135 - 1974 - Atlas of Mars; photoindex of Mariner 9, \"B\" camera coverage on Mars charts MC 130, scale 1:5,000,000","indexId":"ofr74135","publicationYear":"1974","noYear":false,"title":"Atlas of Mars; photoindex of Mariner 9, \"B\" camera coverage on Mars charts MC 130, scale 1:5,000,000"},"predicate":"SUPERSEDED_BY","object":{"id":70042713,"text":"70042713 - 1979 - Atlas of Mars: the 1:5,000,000 map series","indexId":"70042713","publicationYear":"1979","noYear":false,"title":"Atlas of Mars: the 1:5,000,000 map series"},"id":4}],"lastModifiedDate":"2013-01-18T13:10:33","indexId":"70042713","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":48,"text":"NASA SP","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"438","title":"Atlas of Mars: the 1:5,000,000 map series","docAbstract":"This atlas comprises small-scale maps and photomosaics covering the entire surface of the planet Mars. The cartographic contents are reduced-scale versions of the 1:5,000,000 topographic series of 30 quadrangles compiled by the U.S. Geological Survey in cooperation with the National Aeronautics and Space Administration (NASA).","language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Batson, R.M., Bridges, P., and Inge, J., 1979, Atlas of Mars: the 1:5,000,000 map series: NASA SP 438, xi, 146 p.; Maps.","productDescription":"xi, 146 p.; Maps","startPage":"i","endPage":"146","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265937,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"5000000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d40e4b061045bf9abdc","contributors":{"authors":[{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472106,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bridges, P.M.","contributorId":7684,"corporation":false,"usgs":true,"family":"Bridges","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":472104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Inge, J.L.","contributorId":44625,"corporation":false,"usgs":true,"family":"Inge","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":472105,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}