{"pageNumber":"5017","pageRowStart":"125400","pageSize":"25","recordCount":184617,"records":[{"id":41879,"text":"ofr84726 - 1985 - Map of Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1983","interactions":[],"lastModifiedDate":"2023-09-01T20:49:26.854725","indexId":"ofr84726","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"84-726","title":"Map of Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1983","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84726","usgsCitation":"Moyle, W.R., and Glenn, F.M., 1985, Map of Antelope Valley-East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1983: U.S. Geological Survey Open-File Report 84-726, 1 Plate: 37.76 x 39.24 inches, https://doi.org/10.3133/ofr84726.","productDescription":"1 Plate: 37.76 x 39.24 inches","costCenters":[],"links":[{"id":420424,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13541.htm","linkFileType":{"id":5,"text":"html"}},{"id":79608,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0726/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley-East Kern Water Agency area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118.854,\n 35.361\n ],\n [\n -118.854,\n 34.382\n ],\n [\n -117.628,\n 34.382\n ],\n [\n -117.628,\n 35.361\n ],\n [\n -118.854,\n 35.361\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6555da","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":225657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glenn, Florence M.","contributorId":35293,"corporation":false,"usgs":true,"family":"Glenn","given":"Florence","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":225656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70180828,"text":"70180828 - 1985 - A histopathological survey of four fish species from the Beaufort Lagoon, Alaska","interactions":[],"lastModifiedDate":"2017-02-03T14:07:47","indexId":"70180828","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"A histopathological survey of four fish species from the Beaufort Lagoon, Alaska","docAbstract":"

No abstract available 

","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Fairbanks, AK","usgsCitation":"Goldberg, S., Yasutake, W.T., and West, R., 1985, A histopathological survey of four fish species from the Beaufort Lagoon, Alaska.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334710,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ee5","contributors":{"authors":[{"text":"Goldberg, S.R.","contributorId":47975,"corporation":false,"usgs":true,"family":"Goldberg","given":"S.R.","email":"","affiliations":[],"preferred":false,"id":662535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":662536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"West, R.L.","contributorId":40696,"corporation":false,"usgs":true,"family":"West","given":"R.L.","affiliations":[],"preferred":false,"id":662537,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70180830,"text":"70180830 - 1985 - Smolt quality and the effectiveness of Columbia River hatcheries","interactions":[],"lastModifiedDate":"2017-02-03T14:13:46","indexId":"70180830","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Smolt quality and the effectiveness of Columbia River hatcheries","docAbstract":"

No abstract available 

","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Bonneville Power Administration smoltification workshop","conferenceTitle":"Bonneville Power Administration smoltification workshop","conferenceDate":"May 1985","conferenceLocation":"Warm Springs, OR","language":"English","usgsCitation":"McIntyre, J., 1985, Smolt quality and the effectiveness of Columbia River hatcheries, in Bonneville Power Administration smoltification workshop, Warm Springs, OR, May 1985.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334712,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ee0","contributors":{"authors":[{"text":"McIntyre, J.D.","contributorId":27006,"corporation":false,"usgs":true,"family":"McIntyre","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":662539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180827,"text":"70180827 - 1985 - Biological and hydrological evaluation of the fish ladder at Brooks River Falls, Alaska","interactions":[],"lastModifiedDate":"2017-02-03T14:04:32","indexId":"70180827","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"title":"Biological and hydrological evaluation of the fish ladder at Brooks River Falls, Alaska","docAbstract":"

No abstract available 

","language":"English ","publisher":"National Park Service","usgsCitation":"Wilmot, R., and Burger, C.V., 1985, Biological and hydrological evaluation of the fish ladder at Brooks River Falls, Alaska.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334709,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5895a4d6e4b0fa1e59bc1ee7","contributors":{"authors":[{"text":"Wilmot, R.L.","contributorId":97662,"corporation":false,"usgs":true,"family":"Wilmot","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":662533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burger, C. V.","contributorId":58219,"corporation":false,"usgs":true,"family":"Burger","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":662534,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013365,"text":"70013365 - 1985 - 40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England","interactions":[],"lastModifiedDate":"2023-12-28T13:24:02.293607","indexId":"70013365","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England","docAbstract":"

40Ar/39Ar ages of coexisting biotite and hornblende from Proterozoic Y gneisses of the Berkshire and Green Mountain massifs, as well as 40Ar/39Ar and K-Ar mineral and whole-rock ages from Paleozoic metamorphic rocks, suggest that the thermal peak for the dominant metamorphic recrystallization in western New England occurred 465 ± 5 m.y. ago (Taconian). Although textural data indicate a complex metamorphic-tectonic history for Paleozoic rocks, no evidence in rocks at least as high as kyanite grade dictates an Acadian age for the Barrovian metamorphism. Available 40Ar/39Ar and K-Ar data suggest that the low-grade metamorphism and cleavage formation in Taconic allochthons and the higher-grade metamorphism and emplacement of the Berkshire massif allochthon are Taconian.

40Ar/39Ar age data from a poorly defined terrane beginning near the east margin of the Green Mountain massif and extending along the eastern one-third of the Berkshire massif as far south as Otis, Massachusetts, suggest that the area has been retrograded during a metamorphism that peaked at least 376 ± 5 m.y. ago (Acadian).

Available age and petrologic data from western New England indicate the presence of at least three separate metamorphic-structural domains of Taconian age: (1) a small area of relict high-pressure and low-temperature metamorphism in northern Vermont (T-1 domain), (2) a broad area in Vermont and eastern New York of normal Barrovian metamorphism from chlorite to garnet grade and characterized by a gentle metamorphic gradient (T-2 domain), and (3) a rather narrow belt of steep-gradient, Barrovian series metamorphic rocks extending from near the Cortlandt Complex northeastward through Dutchess County, New York, to the Berkshire massif in western Massachusetts (T-3 domain). Areas of maximum metamorphic intensity within the T-3 domain coincide with areas of maximum crustal thickening resulting from imbricate thrusting (Berkshire massif) or from recumbent folding (Manhattan Prong) of remobilized North American continental crust in the later stages of the Taconic orogeny.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1985)96<123:AAKDBO>2.0.CO;2","usgsCitation":"Sutter, J.F., Ratcliffe, N.M., and Mukasa, S., 1985, 40Ar/39Ar and K-Ar data bearing on the metamorphic and tectonic history of western New England: Geological Society of America Bulletin, v. 96, no. 1, p. 123-136, https://doi.org/10.1130/0016-7606(1985)96<123:AAKDBO>2.0.CO;2.","productDescription":"14 p.","startPage":"123","endPage":"136","numberOfPages":"14","costCenters":[],"links":[{"id":220304,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.71683860031261,\n 43.14936147487742\n ],\n [\n -73.71683860031261,\n 41.42652808796893\n ],\n [\n -72.88187766281217,\n 41.42652808796893\n ],\n [\n -72.88187766281217,\n 43.14936147487742\n ],\n [\n -73.71683860031261,\n 43.14936147487742\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"96","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e264e4b0c8380cd45b3a","contributors":{"authors":[{"text":"Sutter, J. F.","contributorId":59779,"corporation":false,"usgs":true,"family":"Sutter","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":365907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":365908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mukasa, S.B.","contributorId":89568,"corporation":false,"usgs":true,"family":"Mukasa","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":365909,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70168843,"text":"70168843 - 1985 - Earthquakes November-December 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:37:21","indexId":"70168843","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Earthquakes November-December 1984","docAbstract":"

Major earthquakes (7.0-7.9) were located in Sumatera, the Philippine Vanuatu Islands, Kamchatka, and the Mid-Atlantic Ocean during this reporting period. Earthquake-related deaths were reported from a magnitude 5.8 quake in India.

\n

There was no significant damage from earthquakes in the United States. 

","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1985, Earthquakes November-December 1984: Earthquake Information Bulletin (USGS), v. 17, no. 3, p. 110-114.","productDescription":"5 p.","startPage":"110","endPage":"114","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318590,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc4e4b015c306f84c34","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621973,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168841,"text":"70168841 - 1985 - Earthquakes, September-October 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:30:22","indexId":"70168841","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Earthquakes, September-October 1984","docAbstract":"

There were no major earthquakes (7.0-7.9) during this reporting period but earthquake related deaths wre reported from Japan Turkey. Algeria the USSR, and Yugoslavia had damaging earthquakes.

\n

In the United States, Wyoming experienced a couple of moderate earthquakes, and off the coast of northern California, a strong earthquake shook much of the northern coast of California and parts of the Oregon coast. 

","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1985, Earthquakes, September-October 1984: Earthquake Information Bulletin (USGS), v. 17, no. 2, p. 73-78.","productDescription":"6 p.","startPage":"73","endPage":"78","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfcce4b015c306f84c5d","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013268,"text":"70013268 - 1985 - GAINS AND LOSSES OF COMMINGLED WATERS IN A STREAM.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:25","indexId":"70013268","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"GAINS AND LOSSES OF COMMINGLED WATERS IN A STREAM.","docAbstract":"In a legal dispute in the State of Washington (Colville Confederated Tribes vs. Boyd Walton, Jr. , Farmer), it became necessary to determine the proportion of transmission losses sustained by developed water that was commingled with native water in a natural stream channel. Ground-water pumping and irrigation adjacent to the stream resulted in both gains and losses to flow along the study reach. The identification of the native and developed waters was accomplished by a detailed study of the reach that combined current-meter measurements with an analysis of the dilution of an injected brine.","conferenceTitle":"Development and Management Aspects of Irrigation and Drainage Systems.","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872624722","usgsCitation":"Nish, M., 1985, GAINS AND LOSSES OF COMMINGLED WATERS IN A STREAM., Development and Management Aspects of Irrigation and Drainage Systems., San Antonio, TX, USA, p. 114-122.","startPage":"114","endPage":"122","numberOfPages":"9","costCenters":[],"links":[{"id":219843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a143ae4b0c8380cd5496a","contributors":{"authors":[{"text":"Nish, Mac","contributorId":56792,"corporation":false,"usgs":true,"family":"Nish","given":"Mac","email":"","affiliations":[],"preferred":false,"id":365686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013264,"text":"70013264 - 1985 - IS ISLAND PARK A HOT DRY ROCK SYSTEM?","interactions":[],"lastModifiedDate":"2012-03-12T17:18:17","indexId":"70013264","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"IS ISLAND PARK A HOT DRY ROCK SYSTEM?","docAbstract":"The Island Park-Yellowstone National Park region comprises a complex caldera system which has formed over the last 2 m. y. The caldera system has been estimated to contain 50% of the total thermal energy remaining in all young igneous systems in the United States. As the result of a reexamination of the data and recent electrical work in the area, the authors now postulate that much of the area where the first- and second-stage calderas developed is underlain by a solidified but still hot pluton. They postulate that the pluton represents a significant hot-dry-rock resource for the United States.","largerWorkTitle":"Transactions - Geothermal Resources Council","conferenceTitle":"1985 International Symposium on Geothermal Energy. Geothermal Resources Council 1985 Annual Meeting.","conferenceLocation":"Kailua-Kona, HI, USA","language":"English","publisher":"Geothermal Resources Council","publisherLocation":"Davis, CA, USA","issn":"01935933","isbn":"093441260X","usgsCitation":"Hoover, D., Pierce, H., and Long, C.L., 1985, IS ISLAND PARK A HOT DRY ROCK SYSTEM?, in Transactions - Geothermal Resources Council, v. 9, no. pt 2, Kailua-Kona, HI, USA, p. 25-29.","startPage":"25","endPage":"29","numberOfPages":"5","costCenters":[],"links":[{"id":219789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"pt 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a37d6e4b0c8380cd611ec","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":365675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, Herbert A.","contributorId":83093,"corporation":false,"usgs":true,"family":"Pierce","given":"Herbert A.","affiliations":[],"preferred":false,"id":365676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":365677,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013133,"text":"70013133 - 1985 - Possible tsunami along the northwestern coast of the United States inferred from Indian traditions","interactions":[],"lastModifiedDate":"2023-10-28T15:47:08.736792","indexId":"70013133","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Possible tsunami along the northwestern coast of the United States inferred from Indian traditions","docAbstract":"

No abstract available.

","language":"English","publisher":"Seismological Society of America","doi":"10.1785/BSSA0750051455","issn":"00371106","usgsCitation":"Heaton, T.H., and Snavely, P., 1985, Possible tsunami along the northwestern coast of the United States inferred from Indian traditions: Bulletin of the Seismological Society of America, v. 75, no. 5, p. 1455-1460, https://doi.org/10.1785/BSSA0750051455.","productDescription":"6 p.","startPage":"1455","endPage":"1460","numberOfPages":"6","costCenters":[],"links":[{"id":480543,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20130115-110915450","text":"External Repository"},{"id":220351,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"75","issue":"5","noUsgsAuthors":false,"publicationDate":"1985-10-01","publicationStatus":"PW","scienceBaseUri":"505a7369e4b0c8380cd77004","contributors":{"authors":[{"text":"Heaton, Thomas H.","contributorId":84739,"corporation":false,"usgs":true,"family":"Heaton","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":365369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snavely, Parke D. Jr.","contributorId":80328,"corporation":false,"usgs":true,"family":"Snavely","given":"Parke D.","suffix":"Jr.","affiliations":[],"preferred":false,"id":365368,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013102,"text":"70013102 - 1985 - Durangite from the Black Range, New Mexico, and new data on durangite from Durango and Cornwall.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:36","indexId":"70013102","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1177,"text":"Canadian Mineralogist","active":true,"publicationSubtype":{"id":10}},"title":"Durangite from the Black Range, New Mexico, and new data on durangite from Durango and Cornwall.","docAbstract":"Durangite, associated with cassiterite, hematite, quartz, tridymite, cristobalite and clinopyroxene, occurs in small veinlets within flows, ash-flow tuffs and lithic tuffs in a tin mine near Boiler Peak, New Mexico. It is clear to semi-translucent, pale yellow-orange to medium orange-red with a vitreous lustre, pale yellow streak; H. 5-5.5%; irregular to conchoidal fracture and a good (110) cleavage; elongate along c with (110), (010), (021) and (111) the prominent forms; Dmeas 3.90, Dcalc 3.92 g/cm3; alpha medium yellow orange 1.634(3), beta pale yellow orange 1.663(3), gamma colourless 1.685(3); weak to moderate dispersion r < v. The structural formula is: (Na0.93Li0.07)SIGMA 1.00(Al0.89Fe0.07Mn0.06)SIGMA 1.02As0.99O4(F0.90(OH)0.07)SIGMA 0.97. Indexed XRD powder data are tabulated; a 6.574(1), b 8.505(2), c 7.019(1) A, beta 115.34o; space group C2/c; Z = 4. Additional X-ray and chemical data on durangite from Durango and Cornwall are also included.-L.T.T.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Mineralogist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00084476","usgsCitation":"Foord, E., Oakman, M., and Maxwell, C.H., 1985, Durangite from the Black Range, New Mexico, and new data on durangite from Durango and Cornwall.: Canadian Mineralogist, v. 23, no. 2, p. 241-246.","startPage":"241","endPage":"246","numberOfPages":"6","costCenters":[],"links":[{"id":219895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0417e4b0c8380cd5079d","contributors":{"authors":[{"text":"Foord, E.E.","contributorId":86835,"corporation":false,"usgs":true,"family":"Foord","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":365295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oakman, M.R.","contributorId":23163,"corporation":false,"usgs":true,"family":"Oakman","given":"M.R.","affiliations":[],"preferred":false,"id":365293,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maxwell, C. H.","contributorId":35343,"corporation":false,"usgs":true,"family":"Maxwell","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":365294,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013148,"text":"70013148 - 1985 - Dissolution of alkaline earth sulfates in the presence of montmorillonite","interactions":[],"lastModifiedDate":"2020-01-19T10:49:50","indexId":"70013148","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Dissolution of alkaline earth sulfates in the presence of montmorillonite","docAbstract":"In a study of the effect of montmorillonite on the dissolution of BaSO4 (barite), SrSO4 (celestite), and 226Ra from U mill tailings, it was found that: (1) More of these substances dissolve in an aqueous system that contains montmorillonite than dissolve in a similar system without clay, due to the ion exchange properties of the clay; (2) Na-montmorillonite is more effective in aiding dissolution than is Ca-montmorillonite; (3) the amount of Ra that moves from mill tailings to an exchanger increases as solution sulfate activity decreases. Leaching experiments suggest that 226Ra from H2SO4-circuit U mill tailings from Edgemont, South Dakota, is not present as pure Ra sulfate or as an impurity in anhydrite or gypsum; it is less soluble, and probably occurs as a trace constituent in barite.","language":"English","publisher":"Springer","doi":"10.1007/BF00568389","issn":"00496979","usgsCitation":"Eberl, D.D., and Landa, E.R., 1985, Dissolution of alkaline earth sulfates in the presence of montmorillonite: Water, Air, & Soil Pollution, v. 25, no. 2, p. 207-214, https://doi.org/10.1007/BF00568389.","productDescription":"8 p.","startPage":"207","endPage":"214","numberOfPages":"8","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a022de4b0c8380cd4ff13","contributors":{"authors":[{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":365404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landa, Edward R. erlanda@usgs.gov","contributorId":2112,"corporation":false,"usgs":true,"family":"Landa","given":"Edward","email":"erlanda@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":779758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70168845,"text":"70168845 - 1985 - Earthquakes, July-August 1984","interactions":[],"lastModifiedDate":"2016-03-24T15:41:57","indexId":"70168845","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Earthquakes, July-August 1984","docAbstract":"

There were no major earthquakes (7.0-7.9) and no earthquake related deaths reported during this period but injuries and damage were experienced in Japan from earthquakes.

\n

There were no earthquake casualties reported in the United States but some minor damage was reported. 

","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1985, Earthquakes, July-August 1984: Earthquake Information Bulletin (USGS), v. 17, no. 1, p. 34-37.","productDescription":"4 p.","startPage":"34","endPage":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfc7e4b015c306f84c4f","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013123,"text":"70013123 - 1985 - Errors and parameter estimation in precipitation-runoff modeling: 2. Case study","interactions":[],"lastModifiedDate":"2020-01-19T10:38:48","indexId":"70013123","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","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":"Errors and parameter estimation in precipitation-runoff modeling: 2. Case study","docAbstract":"

A case study is presented which illustrates some of the error analysis, sensitivity analysis, and parameter estimation procedures reviewed in the first part of this paper. It is shown that those procedures, most of which come from statistical nonlinear regression theory, are invaluable in interpreting errors in precipitation-runoff modeling and in identifying appropriate calibration strategies.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR021i008p01214","usgsCitation":"Troutman, B.M., 1985, Errors and parameter estimation in precipitation-runoff modeling: 2. Case study: Water Resources Research, v. 21, no. 8, p. 1214-1222, https://doi.org/10.1029/WR021i008p01214.","productDescription":"9 p.","startPage":"1214","endPage":"1222","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"8","noUsgsAuthors":false,"publicationDate":"2008-01-08","publicationStatus":"PW","scienceBaseUri":"505a0a4ae4b0c8380cd522b5","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":195329,"corporation":false,"usgs":false,"family":"Troutman","given":"Brent","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":365346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013267,"text":"70013267 - 1985 - Isolation of anaerobic oxalate-degrading bacteria from freshwater lake sediments","interactions":[],"lastModifiedDate":"2020-01-19T11:19:01","indexId":"70013267","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":889,"text":"Archives of Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Isolation of anaerobic oxalate-degrading bacteria from freshwater lake sediments","docAbstract":"

Enrichment cultures that anaerobically degraded oxalate were obtained from lake sediment inocula. From these, 5 pure cultures of anaerobic oxalate-degrading bacteria were isolated and partially characterized. The isolates were Gram-negative, non-sporeforming, non-motile, obligate anaerobes. Oxalate was required for growth and was stoichiometrically converted to formate; 14CO2 was also recovered when 14C-oxalate was added. Maximal growth occurred when the oxalate concentration was 50 mM. Acetate stimulated growth in the presence of oxalate, however, 14C-experiments indicated that acetate was only utilized for cell carbon.

The isolates were either spiral-shaped or rod-shaped organisms. The first morphotype grew much more slowly than the second and exhibited 13-fold lower cell yields. These isolates represent a new strain of oxalate-degrading bacteria. The second morphotype was similar to the anaerobic oxalate-degrading bacteria previously found in rumen. This report extends the known habitats in which anaerobic oxalate-degrading organisms have been found to include aquatic sediments.

","language":"English","publisher":"Springer","doi":"10.1007/BF00446732","issn":"03028933","usgsCitation":"Smith, R.L., Strohmaier, F., and Oremland, R.S., 1985, Isolation of anaerobic oxalate-degrading bacteria from freshwater lake sediments: Archives of Microbiology, v. 141, no. 1, p. 8-13, https://doi.org/10.1007/BF00446732.","productDescription":"6 p.","startPage":"8","endPage":"13","numberOfPages":"6","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":219792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3f51e4b0c8380cd6443b","contributors":{"authors":[{"text":"Smith, R. L.","contributorId":93904,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":365684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strohmaier, F.E.","contributorId":37893,"corporation":false,"usgs":true,"family":"Strohmaier","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":365683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oremland, Ronald S. 0000-0001-7382-0147 roremlan@usgs.gov","orcid":"https://orcid.org/0000-0001-7382-0147","contributorId":931,"corporation":false,"usgs":true,"family":"Oremland","given":"Ronald","email":"roremlan@usgs.gov","middleInitial":"S.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":779764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013265,"text":"70013265 - 1985 - Ages of subsurface stratigraphic intervals in the Quaternary of Enewetak Atoll, Marshall Islands","interactions":[],"lastModifiedDate":"2013-01-26T15:41:08","indexId":"70013265","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Ages of subsurface stratigraphic intervals in the Quaternary of Enewetak Atoll, Marshall Islands","docAbstract":"Drill cores of Enewetak Atoll, Marshall Islands, reveal six stratigraphic intervals, numbered in downward sequence, which represent vertical coral growth during Quaternary interglaciations. Radiocarbon dates indicate that the Holocene sea transgressed the emergent reef platform by about 8000 yr B.P. The reef grew rapidly upward (about 5 to 10 mm/yr) until about 6500 yr B.P. Afterward vertical growth slowed to about 0.5 mm/yr, then lateral development became dominant during the last several thousand years. The second interval is dated at 131,000 ?? 3000 yr B.P. by uranium series. This unit correlates with oxygen-isotope substage 5e and with terrace VIIa of Huon Peninsula, New Guinea, and of Main Reef-2 terrace at Atauro Island. The third interval is not dated because corals were recrystallized and it is tentatively correlated with either oxygen-isotope stages 7 or 9. The age of the fourth interval is estimated at 454,000 ?? 100,000 yr B.P. from measured 234U 238U activity ratios. This unit is correlated with either oxygen-isotope stage 9, 11, or 13. ?? 1985.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Quaternary Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0033-5894(85)90071-7","issn":"00335894","usgsCitation":"Szabo, B.J., Tracey, J.I., and Goter, E., 1985, Ages of subsurface stratigraphic intervals in the Quaternary of Enewetak Atoll, Marshall Islands: Quaternary Research, v. 23, no. 1, p. 54-61, https://doi.org/10.1016/0033-5894(85)90071-7.","startPage":"54","endPage":"61","numberOfPages":"8","costCenters":[],"links":[{"id":266550,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0033-5894(85)90071-7"},{"id":219790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e905e4b0c8380cd48046","contributors":{"authors":[{"text":"Szabo, Barney J.","contributorId":6848,"corporation":false,"usgs":true,"family":"Szabo","given":"Barney","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":365678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":365679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goter, E.R.","contributorId":71691,"corporation":false,"usgs":true,"family":"Goter","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":365680,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013124,"text":"70013124 - 1985 - Land subsidence caused by ground water withdrawal in urban areas","interactions":[],"lastModifiedDate":"2012-03-12T17:18:36","indexId":"70013124","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1746,"text":"GeoJournal","active":true,"publicationSubtype":{"id":10}},"title":"Land subsidence caused by ground water withdrawal in urban areas","docAbstract":"At least eight urban areas in the world have encountered significant economic impact from land subsidence caused by pumping of ground water from unconsolidated sediment. The areas, most of which are coastal, include Bangkok, Houston, Mexico City, Osaka, San Jose, Shanghai, Tokyo, and Venice. Flooding related to decreased ground elevation is the principal adverse effect of the subsidence. Lesser effects include regional tilting, well-casing failures, \"rising\" buildings, and ground failure or rupture. Subsidence of most of these urban areas began before the phenomenon was discovered and understood. Thus, the subsidence problems were unanticipated. Methods to arrest subsidence typically have included control of ground water pumping and development of surface water to offset the reductions of ground water pumping. Ground water recharge has also been practiced. Areas threatened by flooding have been protected by extensive networks of dikes and sea walls, locks, and pumping stations to remove storm runoff. ?? 1985 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GeoJournal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00186338","issn":"03432521","usgsCitation":"Holzer, T., and Johnson, A., 1985, Land subsidence caused by ground water withdrawal in urban areas: GeoJournal, v. 11, no. 3, p. 245-255, https://doi.org/10.1007/BF00186338.","startPage":"245","endPage":"255","numberOfPages":"11","costCenters":[],"links":[{"id":205012,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00186338"},{"id":220179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a41b0e4b0c8380cd65709","contributors":{"authors":[{"text":"Holzer, T.L.","contributorId":35739,"corporation":false,"usgs":true,"family":"Holzer","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":365347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":365348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013147,"text":"70013147 - 1985 - ON PREDICTING INFRAGRAVITY ENERGY IN THE SURF ZONE.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:29","indexId":"70013147","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"ON PREDICTING INFRAGRAVITY ENERGY IN THE SURF ZONE.","docAbstract":"Flow data were obtained in the surf zone across a barred profile during a storm. RMS cross-shore velocities due to waves in the intragravity band (wave periods greater than 20 s) had maxima in excess of 0. 5 m/s over the bar crest. For comparison to measured spectra, synthetic spectra of cross-shore flow were computed using measured nearshore profiles. The structure, in the infragravity band, of these synthetic spectra corresponded reasonably well with the structure of the measured spectra. Total variances of measured cross-shore flow within the infragravity band were nondimensionalized by dividing by total infragravity variances of synthetic spectra. These nondimensional variances were independent of distance offshore and increased with the square of the breaker height. Thus, cross-shore flow due to infragravity waves can be estimated with knowledge of the nearshore profile and incident wave conditions. Refs.","largerWorkTitle":"Proceedings of the Coastal Engineering Conference","conferenceTitle":"Nineteenth Coastal Engineering Conference, Proceedings of the International Conference.","conferenceLocation":"Houston, TX, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872624382","usgsCitation":"Sallenger, and Holman, R.A., 1985, ON PREDICTING INFRAGRAVITY ENERGY IN THE SURF ZONE., in Proceedings of the Coastal Engineering Conference, v. 2, Houston, TX, USA, p. 1940-1951.","startPage":"1940","endPage":"1951","numberOfPages":"12","costCenters":[],"links":[{"id":220570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a69e8e4b0c8380cd73f83","contributors":{"editors":[{"text":"Edge, Billy L.","contributorId":64575,"corporation":false,"usgs":true,"family":"Edge","given":"Billy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":508482,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Sallenger, Jr.","contributorId":105768,"corporation":false,"usgs":true,"family":"Sallenger","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":365403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holman, Robert A.","contributorId":37896,"corporation":false,"usgs":false,"family":"Holman","given":"Robert","email":"","middleInitial":"A.","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":365402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013122,"text":"70013122 - 1985 - Evidence for lower crustal ductile strain localization in southern New York","interactions":[],"lastModifiedDate":"2012-03-12T17:18:36","indexId":"70013122","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Evidence for lower crustal ductile strain localization in southern New York","docAbstract":"Historic triangulation data have been analysed to determine whether intraplate seismicity is associated with ongoing ductile deformation in the lower crust. The model we have attempted to test is basically analogous to strain accumulation and release along plate-boundary strike-slip faults like the San Andreas Fault in California. That is, beneath an elastic-seismogenic upper crust ???20 km thick, strain is preferentially localized within ductile shear zones in the lower crust due to broad-scale plate driving forces. The localized lower-crustal ductile strain causes stress and strain to accumulate elastically in the brittle crust which is eventually released in crustal earthquakes. At greater depths, this localized shear deformation probably develops into pervasive ductile flow. Numerous geodetic measurements along the San Andreas Fault confirm that earthquakes in the brittle upper crust are produced by the release of elastic strain that results from ongoing ductile shear or slip in the lower crust1,2. We have found evidence of high rates of crustal deformation in southern New York which suggest that localized ductile shear is occurring in the lower crust. ?? 1985 Nature Publishing Group.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Nature","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1038/317705a0","issn":"00280836","usgsCitation":"Zoback, M.D., Prescott, W., and Krueger, S., 1985, Evidence for lower crustal ductile strain localization in southern New York: Nature, v. 317, no. 6039, p. 705-707, https://doi.org/10.1038/317705a0.","startPage":"705","endPage":"707","numberOfPages":"3","costCenters":[],"links":[{"id":205011,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1038/317705a0"},{"id":220177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"317","issue":"6039","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0d48e4b0c8380cd52f0b","contributors":{"authors":[{"text":"Zoback, Mark D.","contributorId":80275,"corporation":false,"usgs":true,"family":"Zoback","given":"Mark","middleInitial":"D.","affiliations":[],"preferred":false,"id":365344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prescott, W.H.","contributorId":96337,"corporation":false,"usgs":true,"family":"Prescott","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":365345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krueger, S.W.","contributorId":26067,"corporation":false,"usgs":true,"family":"Krueger","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":365343,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013146,"text":"70013146 - 1985 - TOPOGRAPHY, STRESSES, AND STABILITY AT YUCCA MOUNTAIN, NEVADA.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:30","indexId":"70013146","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"TOPOGRAPHY, STRESSES, AND STABILITY AT YUCCA MOUNTAIN, NEVADA.","docAbstract":"Plane-strain solutions are used to analyze the influence of topography on the state of stress at Yucca Mountain, Nye County, Nevada. The results are in good agreement with the measured stress components obtained in drill holes by the hydraulic-fracturing technique, particularly those measured directly beneath the crest of the ridge, and indicate that these stresses are gravitationally induced. A separate analysis takes advantage of the fact that a well-developed set of vertical faults and fractures, subparallel to the ridge trend, imparts a vertical transverse isotropy to the rock and that, as a consequence of gravitational loading, unequal horizontal stresses are induced in directions perpendicular and parallel to the anisotropy.","largerWorkTitle":"Proceedings - Symposium on Rock Mechanics","conferenceTitle":"Research & Engineering Applications in Rock Masses, Proceedings of the 26th US Symposium on Rock Mechanics.","conferenceLocation":"Rapid City, SD, USA","language":"English","publisher":"A. A. Balkema","publisherLocation":"Rotterdam, Neth","issn":"0085574X","isbn":"906191602X","usgsCitation":"Wolfs, H., and Savage, W.Z., 1985, TOPOGRAPHY, STRESSES, AND STABILITY AT YUCCA MOUNTAIN, NEVADA., in Proceedings - Symposium on Rock Mechanics, v. 2, Rapid City, SD, USA, p. 1121-1129.","startPage":"1121","endPage":"1129","numberOfPages":"9","costCenters":[],"links":[{"id":220519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba38fe4b08c986b31fd63","contributors":{"authors":[{"text":"Wolfs, Henri","contributorId":73747,"corporation":false,"usgs":true,"family":"Wolfs","given":"Henri","email":"","affiliations":[],"preferred":false,"id":365400,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savage, William Z.","contributorId":107686,"corporation":false,"usgs":true,"family":"Savage","given":"William","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":365401,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013125,"text":"70013125 - 1985 - Hydrocarbon source rock evaluation of Middle Proterozoic Solor Church Formation, North American Mid-Continent Rift System, Rice County, Minnesota","interactions":[],"lastModifiedDate":"2023-01-12T17:08:59.798288","indexId":"70013125","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hydrocarbon source rock evaluation of Middle Proterozoic Solor Church Formation, North American Mid-Continent Rift System, Rice County, Minnesota","docAbstract":"

Hydrocarbon source rock evaluation of the Middle Proterozoic Solor Church Formation (Keweenawan Supergroup) as sampled in the Lonsdale 65-1 well, Rice County, Minnesota, shows that: (1) the rocks are organic matter lean (24 of 25 samples have less than 0.8% organic carbon); (2) the organic matter is thermally post-mature, probably near the transition between the wet gas phase of catagenesis and metagenesis (dry gas zone); and (3) the rocks have minimal potential for producing additional hydrocarbons (genetic potential < 0.30 mg HC/g rock). Although no direct evidence exists from which to determine maximum burial depths, the observed thermal maturity of the organic matter requires significantly greater burial depths, a higher geothermal gradient, or both. It is likely, t least on the Saint Croix horst, that thermal maturation of the organic matter in the Solor Church took place relatively early, and that any hydrocarbons generated during this early phase were probably lost prior to deposition of the overlying Middle Proterozoic Fond du Lac Formation (Keweenawan Supergroup).

","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/AD462BB4-16F7-11D7-8645000102C1865D","usgsCitation":"Hatch, J.R., and Morey, G.B., 1985, Hydrocarbon source rock evaluation of Middle Proterozoic Solor Church Formation, North American Mid-Continent Rift System, Rice County, Minnesota: American Association of Petroleum Geologists Bulletin, v. 69, no. 8, p. 1208-1216, https://doi.org/10.1306/AD462BB4-16F7-11D7-8645000102C1865D.","productDescription":"9 p.","startPage":"1208","endPage":"1216","numberOfPages":"9","costCenters":[],"links":[{"id":220231,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Rice County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -93.34920505219071,\n 43.49815750458026\n ],\n [\n -91.24259975342454,\n 43.50707256780825\n ],\n [\n -91.47254369055457,\n 43.95930280923483\n ],\n [\n -92.06314675447041,\n 44.348847259526906\n ],\n [\n -92.59270667841201,\n 44.59717035689479\n ],\n [\n -92.86104592929777,\n 44.755448965887155\n ],\n [\n -92.73938330627067,\n 45.025361158132085\n ],\n [\n -92.74821295076435,\n 45.25818490407394\n ],\n [\n -92.63944315222153,\n 45.458072064433395\n ],\n [\n -92.91327410861959,\n 45.62864851581449\n ],\n [\n -92.32555873070334,\n 46.04614819631604\n ],\n [\n -93.62550429518382,\n 46.059401440466786\n ],\n [\n -93.34920505219071,\n 43.49815750458026\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"69","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2e8be4b0c8380cd5c647","contributors":{"authors":[{"text":"Hatch, J. R.","contributorId":14775,"corporation":false,"usgs":true,"family":"Hatch","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":365350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morey, G. B.","contributorId":14406,"corporation":false,"usgs":true,"family":"Morey","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":365349,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013612,"text":"70013612 - 1985 - Adsorption and desorption of hexavalent chromium in an alluvial aquifer near Telluride, Colorado","interactions":[],"lastModifiedDate":"2020-01-19T11:06:20","indexId":"70013612","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2262,"text":"Journal of Environmental Quality","active":true,"publicationSubtype":{"id":10}},"title":"Adsorption and desorption of hexavalent chromium in an alluvial aquifer near Telluride, Colorado","docAbstract":"

A laboratory investigation of reactions between hexavalent chromium [Cr(VI)] and alluvium was conducted to evaluate reactions of Cr(VI) contaminating an alluvial aquifer near Telluride, CO and to determine the mechanisms responsible for these reactions. Uncontaminated alluvium and groundwater (spiked with CrO42−) from the study site were used in batch and column experiments. Results of these experiments show that Cr(VI) was adsorbed by the alluvium. Distribution coefficients from batch experiments ranged from 52 L/kg at an equilibrium CrO42− concentration of 0.4 µmol/L to 1.7 L/kg at an equilibrium concentration of 1400 µmol/L. The zero point of charge for the alluvium was approximately 8.3, and the alluvium had a positive net charge at the groundwater pH of 6.8. Visual and chemical evidence indicated that Fe oxide and hydroxide coatings on the alluvial particles principally were responsible for the adsorption of Cr(VI). During column experiments, Cr(VI) initially was desorbed easily from the alluvium by Cr‐free groundwater; however, the rate of desorption decreased rapidly, and > 60 pore volumes of groundwater were required to decrease the effluent concentration of Cr(VI) to 3 µmol/L [drinking water standard for Cr(VI) = 1 µmol/L]. The quantity of Cr(VI) adsorbed varied with the type and concentration of other anions in solution.


","language":"English","publisher":"Wiley","doi":"10.2134/jeq1985.00472425001400010030x","issn":"00472425","usgsCitation":"Stollenwerk, K.G., and Grove, D., 1985, Adsorption and desorption of hexavalent chromium in an alluvial aquifer near Telluride, Colorado: Journal of Environmental Quality, v. 14, no. 1, p. 150-155, https://doi.org/10.2134/jeq1985.00472425001400010030x.","productDescription":"6 p.","startPage":"150","endPage":"155","numberOfPages":"6","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":219992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","city":"Telluride","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.99560546875,\n 37.84232584933158\n ],\n [\n -107.666015625,\n 37.84232584933158\n ],\n [\n -107.666015625,\n 38.05025395161289\n ],\n [\n -107.99560546875,\n 38.05025395161289\n ],\n [\n -107.99560546875,\n 37.84232584933158\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6fbe4b0c8380cd47778","contributors":{"authors":[{"text":"Stollenwerk, Kenneth G. kgstolle@usgs.gov","contributorId":578,"corporation":false,"usgs":true,"family":"Stollenwerk","given":"Kenneth","email":"kgstolle@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":779762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grove, D.B.","contributorId":56689,"corporation":false,"usgs":true,"family":"Grove","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":366480,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70013907,"text":"70013907 - 1985 - Prediction of central California earthquakes from soil-gas helium fluctuations","interactions":[],"lastModifiedDate":"2012-03-12T17:19:32","indexId":"70013907","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"Prediction of central California earthquakes from soil-gas helium fluctuations","docAbstract":"The observations of short-term decreases in helium soil-gas concentrations along the San Andreas Fault in central California have been correlated with subsequent earthquake activity. The area of study is elliptical in shape with radii approximately 160??80 km, centered near San Benito, and with the major axis parallel to the Fault. For 83 percent of the M>4 earthquakes in this area a helium decrease preceded seismic activity by 1.5 to 6.5 weeks. There were several earthquakes without a decrease and several decreases without a corresponding earthquake. Owing to complex and unresolved interaction of many geophysical and geochemical parameters, no suitable model is yet developed to explain the observations. ?? 1985 Birkha??user Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pure and Applied Geophysics PAGEOPH","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Birkha??user-Verlag","doi":"10.1007/BF00874605","issn":"00334553","usgsCitation":"Reimer, G., 1985, Prediction of central California earthquakes from soil-gas helium fluctuations: Pure and Applied Geophysics PAGEOPH, v. 122, no. 2-4, p. 369-375, https://doi.org/10.1007/BF00874605.","startPage":"369","endPage":"375","numberOfPages":"7","costCenters":[],"links":[{"id":205682,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00874605"},{"id":226116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"122","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a81ebe4b0c8380cd7b7d4","contributors":{"authors":[{"text":"Reimer, G.M.","contributorId":59800,"corporation":false,"usgs":true,"family":"Reimer","given":"G.M.","affiliations":[],"preferred":false,"id":367141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013128,"text":"70013128 - 1985 - Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida","interactions":[],"lastModifiedDate":"2020-01-19T10:51:51","indexId":"70013128","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida","docAbstract":"Operation of a wood-preserving facility for nearly 80 years at Pensacola, FL, contaminated the near-surface groundwater with creosote and pentachlorophenol. The major source of aquifer contamination was unlined surface impoundments that were in direct hydraulic contact with the groundwater. Episodes of overtopping the impoundments and overland flow of treatment liquor and waste were also significant to the migration and contamination of the groundwater. Solutes contaminating the ground-water are mainly naphthalene and substituted phenols. Sorption did not influence retardation of solutes in transport in the groundwater. Phenol and the mono substituted methylphenols appear to be undergoing bio-transformation. Pentachlorophenol (PCP) was not found in significant concentrations in the groundwater possibly because the solubility of PCP is approximately 5 mg/L at pH 6, near the average acidity for the groundwater.","language":"English","publisher":"ACS","doi":"10.1021/es00140a012","issn":"0013936X","usgsCitation":"Goerlitz, D., Troutman, D., Godsy, E., and Franks, B., 1985, Migration of wood-preserving chemicals in contaminated groundwater in a sand aquifer at Pensacola, Florida: Environmental Science & Technology, v. 19, no. 10, p. 955-961, https://doi.org/10.1021/es00140a012.","productDescription":"7 p.","startPage":"955","endPage":"961","numberOfPages":"7","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":220234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida ","city":"Pensacola ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.099609375,\n 30.259067203213018\n ],\n [\n -86.253662109375,\n 30.259067203213018\n ],\n [\n -86.253662109375,\n 30.713503990354965\n ],\n [\n -87.099609375,\n 30.713503990354965\n ],\n [\n -87.099609375,\n 30.259067203213018\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"19","issue":"10","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5713e4b0c8380cd6da32","contributors":{"authors":[{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":365356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troutman, D.E.","contributorId":66301,"corporation":false,"usgs":true,"family":"Troutman","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":365358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":365357,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Franks, B.J.","contributorId":107739,"corporation":false,"usgs":true,"family":"Franks","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":365359,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70013419,"text":"70013419 - 1985 - NUMERICAL MODELING OF FINE SEDIMENT PHYSICAL PROCESSES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:29","indexId":"70013419","displayToPublicDate":"1985-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"NUMERICAL MODELING OF FINE SEDIMENT PHYSICAL PROCESSES.","docAbstract":"Fine sediment in channels, rivers, estuaries, and coastal waters undergo several physical processes including flocculation, floc disruption, deposition, bed consolidation, and resuspension. This paper presents a conceptual model and reviews mathematical models of these physical processes. Several general fine sediment models that simulate some of these processes are reviewed. These general models do not directly simulate flocculation and floc disruption, but the conceptual model and existing functions are shown to adequately model these two processes for one set of laboratory data.","conferenceTitle":"Hydraulics and Hydrology in the Small Computer Age, Proceedings of the Specialty Conference.","conferenceLocation":"Lake Buena Vista, FL, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, USA","isbn":"0872624749","usgsCitation":"Schoellhamer, D., 1985, NUMERICAL MODELING OF FINE SEDIMENT PHYSICAL PROCESSES., Hydraulics and Hydrology in the Small Computer Age, Proceedings of the Specialty Conference., Lake Buena Vista, FL, USA, p. 242-247.","startPage":"242","endPage":"247","numberOfPages":"6","costCenters":[],"links":[{"id":220369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6176e4b0c8380cd7199f","contributors":{"authors":[{"text":"Schoellhamer, David H. 0000-0001-9488-7340 dschoell@usgs.gov","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":631,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"David H.","email":"dschoell@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":366030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}