{"pageNumber":"4472","pageRowStart":"111775","pageSize":"25","recordCount":165901,"records":[{"id":70197501,"text":"70197501 - 1986 - Paleomagnetism of the Tertiary Clarno Formation of central Oregon and its significance for the tectonic history of the Pacific Northwest","interactions":[],"lastModifiedDate":"2018-06-07T15:52:10","indexId":"70197501","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Paleomagnetism of the Tertiary Clarno Formation of central Oregon and its significance for the tectonic history of the Pacific Northwest","docAbstract":"<p><span>The Clarno Formation, a mostly Eocene and partly early Oligocene sequence of andesitic lavas and volcaniclastic rocks, is the oldest Tertiary formation exposed in north central Oregon. Remanent magnetization directions at 46 sites in the lavas provide a paleomagnetic pole at 84°N, 278°E with a 95% confidence cone of 7°. Comparison of this pole with the North American reference pole for Eocene time indicates that the Clarno Formation has rotated 16° clockwise with an uncertainty of 10° but has undergone no significant latitudinal displacement. Further comparison with paleomagnetic data from the Miocene Columbia River Basalt Group and Steens Basalt shows that large‐scale block rotations in the eastern Columbia Embayment ceased sometime between 38 m.y. and 15 m.y. A paleogeographic reconstruction for 38 m.y. is offered which is consistent with the observed rotation of the Clarno and with the other paleomagnetic data from the Pacific Northwest, which are briefly reviewed. This reconstruction shows that it is possible to account for virtually all of the paleomagnetically indicated rotations in pre‐Miocene Tertiary rocks of the Pacific Northwest by an extensional tectonic model. As a consequence, only part of the rotations in the pre‐Tertiary rocks of the eastern Columbia Embayment need to be the result of accretionary tectonics. The initiation of magmatism in the eastern Columbia Embayment that is represented by the Clarno Formation itself may have been contemporaneous with the beginning of crustal extension in the Pacific Northwest.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/JB091iB14p14089","usgsCitation":"Gromme, C.S., Beck, M.E., Wells, R., and Engebretson, D.C., 1986, Paleomagnetism of the Tertiary Clarno Formation of central Oregon and its significance for the tectonic history of the Pacific Northwest: Journal of Geophysical Research B: Solid Earth, v. 91, no. B14, p. 14089-14103, https://doi.org/10.1029/JB091iB14p14089.","productDescription":"15 p.","startPage":"14089","endPage":"14103","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354834,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"B14","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Gromme, C. Sherman","contributorId":22236,"corporation":false,"usgs":true,"family":"Gromme","given":"C.","email":"","middleInitial":"Sherman","affiliations":[],"preferred":false,"id":737474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beck, Myrl E. Jr.","contributorId":60700,"corporation":false,"usgs":true,"family":"Beck","given":"Myrl","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":737476,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Engebretson, David C.","contributorId":205487,"corporation":false,"usgs":false,"family":"Engebretson","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":737477,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70015720,"text":"70015720 - 1986 - Obstacles facing the venus radar mapper - The implications of gestalt formation in stereo-radargrammetry","interactions":[],"lastModifiedDate":"2012-03-12T17:18:54","indexId":"70015720","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1429,"text":"Earth, Moon and Planets","active":true,"publicationSubtype":{"id":10}},"title":"Obstacles facing the venus radar mapper - The implications of gestalt formation in stereo-radargrammetry","docAbstract":"The question of adapting to radar images the existing hardware that form topographic maps through stereo-photogrammetric models, is examined in principle. Such hardware utilizes a human/ computer hybrid. Although the problem of brightness differentials between corresponding landmarks can be dealt with pseudo-photoclinometrically, the main problem is whether the perspective in a radar image can be conceived to mimic that of a photographic image obtained by a suitably positioned camera. This conception is found to be possible, providing the characteristic relief subtends to a very small angle at the radar and at the fictitious camera. The photogrammetric model parameters must be determined a priori. ?? 1986 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth, Moon and Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00054133","issn":"01679295","usgsCitation":"Wildey, R., 1986, Obstacles facing the venus radar mapper - The implications of gestalt formation in stereo-radargrammetry: Earth, Moon and Planets, v. 35, no. 1, p. 47-54, https://doi.org/10.1007/BF00054133.","startPage":"47","endPage":"54","numberOfPages":"8","costCenters":[],"links":[{"id":205403,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00054133"},{"id":223680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6b0ae4b0c8380cd744ad","contributors":{"authors":[{"text":"Wildey, R.L.","contributorId":9700,"corporation":false,"usgs":true,"family":"Wildey","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":371615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70186156,"text":"70186156 - 1986 - Influence of irrigation on salinity and nitrate in a stream-aquifer system","interactions":[],"lastModifiedDate":"2024-01-10T00:23:04.002979","indexId":"70186156","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Influence of irrigation on salinity and nitrate in a stream-aquifer system","docAbstract":"<p><span>Changes in salinity and nitrate concentration in groundwater and surface water in the semiarid Arkansas River valley of southeastern Colorado, USA were related primarily to irrigation practices. Water is applied to fields by flood irrigation through ditches and furrows. Irrigation water is derived in nearly equal amounts from surface water and groundwater pumped from the shallow alluvial aquifer.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Conjunctive water use: understanding and managing surfacewater-groundwater interactions","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2nd Scientific Assembly of the International Association of Hydrological Sciences","conferenceDate":"July 1986","conferenceLocation":"Budapest, Hungary","language":"English","publisher":"International Association of Hydrological Sciences","usgsCitation":"Konikow, L.F., and Person, M., 1986, Influence of irrigation on salinity and nitrate in a stream-aquifer system, <i>in</i> Conjunctive water use: understanding and managing surfacewater-groundwater interactions, v. 156, Budapest, Hungary, July 1986, p. 217-229.","productDescription":"13 p.","startPage":"217","endPage":"229","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"156","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58de1954e4b02ff32c699cd1","contributors":{"authors":[{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":687690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Person, M.A.","contributorId":91108,"corporation":false,"usgs":true,"family":"Person","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":687691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015706,"text":"70015706 - 1986 - Tectonic significance of precambrian apatite fission-track ages from the midcontinent United States","interactions":[],"lastModifiedDate":"2023-12-10T21:29:54.748798","indexId":"70015706","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic significance of precambrian apatite fission-track ages from the midcontinent United States","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id4\"><p>Apparent apatite fission-track ages from drill core penetrating basement on the flank of the Transcontinental Arch in northwestern Iowa range from 934 ± 86 to 641 ± 90 Ma. These ages, the oldest reported in North America, record at least two thermal events. The 934 Ma age, which is synchronous with K-Ar ages in the Grenville Province and many K-Ar whole-rock and Rb-Sr isochron ages from the Lake Superior region, may document basement cooling caused by regional uplift and erosion of the crust. The remaining fission-track ages are products of a more recent thermal event, relative to the age of the samples, which raised temperatures into the zone of partial annealing. Heating may have occurred between the Middle Ordovician and Middle Cretaceous by burial of the basement with additional sediment. It is estimated that burial raised temperatures in the part of the basement sampled by the core to between 50 and 75°C. These temperature estimates imply paleogeothermal gradients of about 20°C/km, approximately two and one-half times present-day values, and burial of the basement by an additional 2–3 km of sediment.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(86)90189-5","issn":"0012821X","usgsCitation":"Crowley, K., Naeser, C.W., and Babel, C., 1986, Tectonic significance of precambrian apatite fission-track ages from the midcontinent United States: Earth and Planetary Science Letters, v. 79, no. 3-4, p. 329-336, https://doi.org/10.1016/0012-821X(86)90189-5.","productDescription":"8 p.","startPage":"329","endPage":"336","numberOfPages":"8","costCenters":[],"links":[{"id":224331,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"79","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba47de4b08c986b320395","contributors":{"authors":[{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":371568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":371566,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Babel, C.A.","contributorId":63539,"corporation":false,"usgs":true,"family":"Babel","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":371567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70015713,"text":"70015713 - 1986 - Uranium series disequilibrium in a young surficial uranium deposit, northeastern Washington, U.S.A.","interactions":[],"lastModifiedDate":"2023-03-20T12:18:38.929131","indexId":"70015713","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":835,"text":"Applied Geochemistry","active":true,"publicationSubtype":{"id":10}},"title":"Uranium series disequilibrium in a young surficial uranium deposit, northeastern Washington, U.S.A.","docAbstract":"<p>A recently discovered ore-grade accumulation of U in organic-rich sediments of late Quaternary age provides an opportunity for studying the early association of U, U-daughters, and organic matter in a natural setting. The U occurs in valley-fill sediments of peat, peaty clay, silt, and sand along the north fork of Flodelle Creek, Stevens County, Washington. Radiometric techniques (delayed neutron, high-resolution gamma-ray spectrometry, thin-source alpha spectrometry) were employed to determine the abundance and distribution of U-series nuclides, the extent of secular equilibrium within the U decay series, and the apparent U-series ages of U incorporation.</p><p>Sixteen lithologically distinct intervals were sampled from a 292 cm core. Uranium contents range from 140 to 2790 ppm and are positively correlated with organic contents. Measured alpha activity ratios of<span>&nbsp;</span><sup>234</sup>U/<sup>238</sup>U (1.31–1.38) are very similar to those reported in coexisting waters, suggesting a rather constant isotopic composition of introduced U. Much lower Th contents of &lt;10–40 ppm are controlled by the type and abundance of silicate detritus. The youth of the host sediments (&lt;15 000 a) and the paucity of associated radioactivity suggested large excesses of U relative to radioactive daughters and such excesses were observed, particularly in the shallowest intervals. Apparent ages of U emplacement determined by the (alpha) activity ratio of<span>&nbsp;</span><sup>230</sup>Th daughter to<span>&nbsp;</span><sup>234</sup>U parent show a general increase with depth and fair agreement with estimated depositional ages. This observation suggests dominantly syndepositional or early post depositional emplacement of U followed by decay-generated buildup of<span>&nbsp;</span><sup>230</sup>Th daughter with time. However, interval by interval comparisons of the relative abundances of other daughters, particularly<span>&nbsp;</span><sup>226</sup>Ra and<span>&nbsp;</span><sup>210</sup>Pb, indicate variability caused by processes other than closed-system growth and decay, probably because chemically diverse daughters that are decay-generated<span>&nbsp;</span><i>in situ</i><span>&nbsp;</span>have differing mobilities and because upwelling ground water continuously adds more U and minor amounts of daughters. If<span>&nbsp;</span><sup>230</sup>Th is considered the least susceptible to these modifications, the data suggest some addition of<span>&nbsp;</span><sup>234</sup>U in the deepest intervals and some loss of<span>&nbsp;</span><sup>226</sup>Ra and/or gain of<span>&nbsp;</span><sup>222</sup>Rn throughout the studied core.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0883-2927(86)90055-7","issn":"08832927","usgsCitation":"Zielinski, R.A., Bush, C.A., and Rosholt, J., 1986, Uranium series disequilibrium in a young surficial uranium deposit, northeastern Washington, U.S.A.: Applied Geochemistry, v. 1, no. 4, p. 503-511, https://doi.org/10.1016/0883-2927(86)90055-7.","productDescription":"9 p.","startPage":"503","endPage":"511","numberOfPages":"9","costCenters":[],"links":[{"id":224437,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.05050660778001,\n              49.00261108256012\n            ],\n            [\n              -119.37861946664799,\n              49.00261108256012\n            ],\n            [\n              -119.37861946664799,\n              47.71849255236455\n            ],\n            [\n              -117.05050660778001,\n              47.71849255236455\n            ],\n            [\n              -117.05050660778001,\n              49.00261108256012\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdd5e4b08c986b32925c","contributors":{"authors":[{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":371586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, C. A.","contributorId":43344,"corporation":false,"usgs":true,"family":"Bush","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":371585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosholt, J.N.","contributorId":37749,"corporation":false,"usgs":true,"family":"Rosholt","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":371584,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70142601,"text":"70142601 - 1986 - A new view for resource managers","interactions":[],"lastModifiedDate":"2017-01-18T14:39:19","indexId":"70142601","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3230,"text":"Rangelands","active":true,"publicationSubtype":{"id":10}},"title":"A new view for resource managers","docAbstract":"<p>In decades past, the rancher depended upon reports from cowboys to gather information he needed to make management decisions. Today, the vast open ranges of the cowboy era are mostly gone in the United States-fenced into pastures, paddocks, or fields that are now discrete management units. But fencing in the rangeland, while it has replaced much of the need for cowboys, has not replaced the need for information about the health and vigor of the forage on each parcel of land. Can a satellite, orbiting at more than 400 miles in space, serve this purpose? As ranchers and resource specialists are asked to make more and more complex management decisions, with less manpower for conducting inventories, they are wise to seek help in today's rapidly developing technologies. For the past few decades the range technician has accomplished most of his range assessment from a pickup truck, traveling periodically to each unit to determine its status. Now, satellite images of the Earth's resources might be able to help the modern range person do an even more efficient job of monitoring the availability of feed for livestock and wildlife. Yet some important questions need to be answered first. Can this new information source be used to evaluate the ecological condition of these lands? Or are satellite images of our Earth and its variety of landscapes just \"pretty pictures,\" with little practical utility?</p>","language":"English","publisher":"Society for Range Management","usgsCitation":"Haas, R.H., 1986, A new view for resource managers: Rangelands, v. 8, no. 3, p. 99-102.","productDescription":"4 p.","startPage":"99","endPage":"102","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298353,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/3901179"},{"id":298354,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54fec429e4b02419550deba5","contributors":{"authors":[{"text":"Haas, Robert H.","contributorId":93388,"corporation":false,"usgs":true,"family":"Haas","given":"Robert","email":"","middleInitial":"H.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":541994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70142589,"text":"70142589 - 1986 - Vegetation and terrain mapping in Alaska using Landsat MSS and digital terrain data","interactions":[],"lastModifiedDate":"2017-01-18T14:40:06","indexId":"70142589","displayToPublicDate":"1986-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Vegetation and terrain mapping in Alaska using Landsat MSS and digital terrain data","docAbstract":"<p>During the past 5 years, the U.S. Geological Survey's (USGS) Earth Resources Observation Systems (EROS) Data Center Field Office in Anchorage, Alaska has worked cooperatively with Federal and State resource management agencies to produce land-cover and terrain maps for 245 million acres of Alaska. The need for current land-cover information in Alaska comes principally from the mandates of the Alaska National Interest Lands Conservation Act (ANILCA), December 1980, which requires major land management agencies to prepare comprehensive management plans. The land-cover mapping projects integrate digital Landsat data, terrain data, aerial photographs, and field data. The resultant land-cover and terrain maps and associated data bases are used for resource assessment, management, and planning by many Alaskan agencies including the U.S. Fish and Wildlife Service, U.S. Forest Service, Bureau of Land Management, and Alaska Department of Natural Resources. Applications addressed through use of the digital land-cover and terrain data bases range from comprehensive refuge planning to multiphased sampling procedures designed to inventory vegetation statewide. The land-cover mapping programs in Alaska demonstrate the operational utility of digital Landsat data and have resulted in a new land-cover mapping program by the USGS National Mapping Division to compile 1:250,000-scale land-cover maps in Alaska using a common statewide land-cover map legend.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Shasby, M., and Carneggie, D.M., 1986, Vegetation and terrain mapping in Alaska using Landsat MSS and digital terrain data: Photogrammetric Engineering and Remote Sensing, v. 52, no. 6, p. 779-786.","productDescription":"8 p.","startPage":"779","endPage":"786","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298340,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -179.736328125,\n              50.401515322782366\n            ],\n            [\n              -179.736328125,\n              71.7188822971392\n            ],\n            [\n              -141.064453125,\n              71.7188822971392\n            ],\n            [\n              -141.064453125,\n              50.401515322782366\n            ],\n            [\n              -179.736328125,\n              50.401515322782366\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54fec43fe4b02419550debf2","contributors":{"authors":[{"text":"Shasby, Mark shasbym@usgs.gov","contributorId":223,"corporation":false,"usgs":true,"family":"Shasby","given":"Mark","email":"shasbym@usgs.gov","affiliations":[],"preferred":false,"id":541960,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carneggie, David M.","contributorId":62758,"corporation":false,"usgs":true,"family":"Carneggie","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":541961,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70200593,"text":"70200593 - 1986 - Magmatic inclusions in silicic and intermediate volcanic rocks","interactions":[],"lastModifiedDate":"2018-10-24T15:22:15","indexId":"70200593","displayToPublicDate":"1984-05-10T15:21:31","publicationYear":"1986","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic inclusions in silicic and intermediate volcanic rocks","docAbstract":"<p><span>Fine‐grained ellipsoidal inclusions from a few millimeters to over l m in size are present in many intermediate to silicic lava flows and domes. Only recently has it become widely accepted that such inclusions are chilled blobs of magma. Their magmatic origin is manifested by vesicularity and high groundmass porosity, by ellipsoidal shapes, by mingling at contacts with the host, and by textural evidence for groundmass crystallization in an undercooled state. Groundmass textures reflect the degree of undercooling, which is a function of thermal contrast (Δ</span><i>T</i><span>) between inclusions and host magmas before mingling. Compositions of inclusions are invariably more mafic than their hosts and indicate that the magmatic systems were compositionally zoned. Many inclusions were formed from hybrid magmas. Four examples are given in order to document effects of decreasing Δ</span><i>C</i><span>(compositional contrast) and Δ</span><i>T</i><span>, as hosts for mafic andesitic to andesitic inclusions vary from high‐silica rhyolite (HSR) to silicic andesite. In the HSR example from the Coso volcanic field, California, inclusions track the evolution of zonation in a long‐lived magmatic system. At the other extreme, andesitic inclusions in silicic andesite from Crater Lake, Oregon, demonstrate zonation of a system of low Δ</span><i>T</i><span>&nbsp;and Δ</span><i>C</i><span>&nbsp;and show effects of in situ differentiation by gas filter‐pressing of residual liquid. Inclusions form when a relatively small proportion of mafic magma comes into contact with a larger proportion of silicic magma. Several mechanisms by which the magmas mix have been proposed: buoyant rise of vesiculated mafic magma or convective stirring at the interface between mafic and overlying silicic magma, forcible injection of mafic magma, diking of fractured silicic magma, and mixing during ascent in a conduit. No single mechanism explains all field observations. Many inclusions in plutons are analogous to magmatic inclusions in volcanic rocks but are likely to have suffered greater chemical and textural change during comparatively slow postentrapment cooling. Magmatic inclusions are evidence of open system behavior of the differentiated parts of magma bodies, and the inclusions themselves may behave as open systems where Δ</span><i>T</i><span>&nbsp;is low.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB091iB06p06091","usgsCitation":"Bacon, C.R., 1986, Magmatic inclusions in silicic and intermediate volcanic rocks: Journal of Geophysical Research B: Solid Earth, v. 91, no. B6, p. 6091-6112, https://doi.org/10.1029/JB091iB06p06091.","productDescription":"22 p.","startPage":"6091","endPage":"6112","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":358762,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"B6","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Bacon, Charles R. 0000-0002-2165-5618 cbacon@usgs.gov","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":2909,"corporation":false,"usgs":true,"family":"Bacon","given":"Charles","email":"cbacon@usgs.gov","middleInitial":"R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":749675,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70201450,"text":"wdrSC841 - 1986 - Water resources data for South Carolina, water year 1984","interactions":[],"lastModifiedDate":"2021-01-26T20:44:20.89528","indexId":"wdrSC841","displayToPublicDate":"1984-01-01T10:10:48","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"SC-84-1","title":"Water resources data for South Carolina, water year 1984","docAbstract":"<p><span>Water resources data for the 1984 water year for South Carolina consist of </span><span>records of stage, discharge, and water quality of streams; stage, contents, and </span><span>water quality of lakes and reservoirs; and water levels of ground-water wells. </span><span>This volume contains records for water discharge at 93 gaging stations, stage </span><span>only at 5 gaging stations, stage and contents at 11 lakes and reservoirs, water </span><span>quality at 49 gaging stations, and water levels at 62 observation wells. </span><span>Also </span><span>included are data for 40 crest-stage partial-record station. </span><span>Locations of these </span><span>sites are shown on figures 3, 4, 5, and 6. </span><span>Additional water data were collected </span><span>at various sites not involved in the systematic data-collection program. </span><span>These </span><span>data represent that part of the National Water Data System collected by the </span><span>U.S. Geological Survey and cooperating State and Federal agencies in South </span><span>Carolina. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrSC841","collaboration":"Prepared in cooperation with the State of South Carolina and with other local and Federal agencies","usgsCitation":"Bennett, C., Hayes, R., Gissendanner, J., and Jones, K., 1986, Water resources data for South Carolina, 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bennett, C.S.","contributorId":13273,"corporation":false,"usgs":true,"family":"Bennett","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":807778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, R.D.","contributorId":19197,"corporation":false,"usgs":true,"family":"Hayes","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":807779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gissendanner, J.W.","contributorId":39856,"corporation":false,"usgs":true,"family":"Gissendanner","given":"J.W.","affiliations":[],"preferred":false,"id":807780,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, K.H.","contributorId":93566,"corporation":false,"usgs":true,"family":"Jones","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":807781,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28719,"text":"wri844329 - 1985 - Percentage entrainment of constituent loads in urban runoff, south Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:16:16.017173","indexId":"wri844329","displayToPublicDate":"2021-12-12T20:35:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4329","title":"Percentage entrainment of constituent loads in urban runoff, south Florida","docAbstract":"Runoff quantity and quality data from four urban basins in south Florida were analyzed to determine the entrainment of total nitrogen, total phosphorus, total carbon, chemical oxygen demand, suspended solids, and total lead within the stormwater runoff. Land use of the homogeneously developed basins are residential (single family), highway, commercial, and apartment (multifamily).\r\n\r\nA computational procedure was used to calculate, for all storms that had water-quality data, the percentage of constituent load entrainment in specified depths of runoff. The plot of percentage of constituent load entrained as a function of runoff is termed the percentage-entrainment curve.\r\n\r\nPercentage-entrainment curves were developed for three different source areas of basin runoff: (1) the hydraulically effective impervious area, (2) the contributing area, and (3) the drainage area. With basin runoff expressed in inches over the contributing area, the depth of runoff required to remove 90 percent of the constituent load ranged from about 0.4 inch to about 1.4 inches; and to remove 80 percent, from about 0.3 to 0.9 inch.\r\n\r\nAnalysis of variance, using depth of runoff from the contributing area as the response variable, showed that the factor 'basin' is statistically significant, but that the factor 'constituent' is not statistically significant in the forming of the percentage-entrainment curve. Evidently the sewerage design, whether elongated or concise in plan dictates the shape of the percentage-entrainment curve.\r\n\r\nThe percentage-entrainment curves for all constituents were averaged for each basin and plotted against basin runoff for three source areas of runoff-the hydraulically effective impervious area, the contributing area, and the drainage area. The relative positions of the three curves are directly related to the relative sizes of the three source areas considered.\r\n\r\nOne general percentage-entrainment curve based on runoff from the contributing area was formed by averaging across both constituents and basins. Its coordinates are: 0.25 inch of runoff for 50-percent entrainment, 0.65 inch of runoff for 80-percent entrainment, and 0.95 inch of runoff for 90-percent entrainment. The general percentage-entrainment curve based on runoff from the hydraulically effective impervious area has runoff values of 0.35, 0.95, 1.6 inches, respectively.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844329","collaboration":"Prepared in cooperation with the Florida Department of Transportation","usgsCitation":"Miller, R.A., 1985, Percentage entrainment of constituent loads in urban runoff, south Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4329, vi, 44 p., https://doi.org/10.3133/wri844329.","productDescription":"vi, 44 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":57550,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4329/84-4329.pdf","text":"Report","size":"4.24 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 84-4329"},{"id":124610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4329/coverthb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.7220458984375,\n              25.16517336866393\n            ],\n            [\n              -79.8431396484375,\n              25.16517336866393\n            ],\n            [\n              -79.8431396484375,\n              26.701452590314368\n            ],\n            [\n              -80.7220458984375,\n              26.701452590314368\n            ],\n            [\n              -80.7220458984375,\n              25.16517336866393\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ed14","contributors":{"authors":[{"text":"Miller, R. A.","contributorId":95090,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200284,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30339,"text":"wri854152 - 1985 - Drought of 1980-82 in southeast Florida with comparison to the 1961-62 and 1970-71 droughts","interactions":[],"lastModifiedDate":"2021-12-13T12:16:53.684406","indexId":"wri854152","displayToPublicDate":"2021-12-12T20:30:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4152","title":"Drought of 1980-82 in southeast Florida with comparison to the 1961-62 and 1970-71 droughts","docAbstract":"South-central Florida (the Kissimmee Basin) experienced a severe drought during 1980-82, causing Lake Okeechobee--the largest surface-water storage area in south Florida--to reach the lowest stage ever recorded, 9.75 feet above sea level, on July 29, 1981. A prolonged period of deficient rainfall extended from June 1980 to March 1982. On the southeast coast, drought conditions were mitigated on August 16, 1981, when rainfall from Tropical Storm Dennis replenished the coastal aquifers and filled the water conservation areas to near scheduled levels. South Dade County was the only area in south Florida not affected by the drought. Rainfall in the southeast coastal areas had a statistical recurrence ranging from 5 to 20 years whereas the recurrence intervals from some stations in south-central Florida were in excess of 100 years. The 1980-81 drought in southeast Flrodia was not as severe as the 1961-62 or the 1970-71 droughts in terms of rainfall conditions or the effect on water levels. The effects of the drought were less severe because of a combination of water-management practices and periodic rainfall during the otherwise rain-deficient period. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri854152","collaboration":"Prepared in cooperation with the South Florida Water Management District","usgsCitation":"Waller, B., 1985, Drought of 1980-82 in southeast Florida with comparison to the 1961-62 and 1970-71 droughts: U.S. Geological Survey Water-Resources Investigations Report 85-4152, iv, 29 p., https://doi.org/10.3133/wri854152.","productDescription":"iv, 29 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":122705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4152/coverthb.jpg"},{"id":59133,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4152/report.pdf","text":"Report","size":"1.66 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 85-4152"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.7220458984375,\n              25.16517336866393\n            ],\n            [\n              -79.8431396484375,\n              25.16517336866393\n            ],\n            [\n              -79.8431396484375,\n              26.701452590314368\n            ],\n            [\n              -80.7220458984375,\n              26.701452590314368\n            ],\n            [\n              -80.7220458984375,\n              25.16517336866393\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c1ad","contributors":{"authors":[{"text":"Waller, B.G.","contributorId":75970,"corporation":false,"usgs":true,"family":"Waller","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":203086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57489,"text":"wdrMDDE841 - 1985 - Water resources data for Maryland and Delaware, water year 1984","interactions":[],"lastModifiedDate":"2021-01-22T19:33:48.666662","indexId":"wdrMDDE841","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-84-1","displayTitle":"Water Resources Data for Maryland and Delaware, Water Year 1984","title":"Water resources data for Maryland and Delaware, water year 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE841","usgsCitation":"James, R., Simmons, R., and Strain, B., 1985, Water resources data for Maryland and Delaware, water year 1984: U.S. Geological Survey Water Data Report MD-DE-84-1, 321 p., https://doi.org/10.3133/wdrMDDE841.","productDescription":"321 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":381783,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/md-de-84-1/wdrMDDE841.pdf","text":"Report","size":"14.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-84-1"},{"id":174925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/md-de-84-1/wdrMDDE841_coverthb.jpg"}],"country":"United States","state":"Delaware, 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce2d","contributors":{"authors":[{"text":"James, R.W.","contributorId":70434,"corporation":false,"usgs":true,"family":"James","given":"R.W.","affiliations":[],"preferred":false,"id":257150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, R.H.","contributorId":19982,"corporation":false,"usgs":true,"family":"Simmons","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":257149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Strain, B.F.","contributorId":76388,"corporation":false,"usgs":true,"family":"Strain","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":257151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70210941,"text":"70210941 - 1985 - Geologic history of Goban Spur, Northwest Europe continental margin","interactions":[],"lastModifiedDate":"2020-07-09T14:22:32.832878","indexId":"70210941","displayToPublicDate":"2020-07-07T11:09:46","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Geologic history of Goban Spur, Northwest Europe continental margin","docAbstract":"<p>Drilling on Leg 80 of the Deep Sea Drilling Project-International Phase of Ocean Drilling was conducted on a transect of four sites (548-551) across the continent-ocean boundary at Goban Spur, a prominent southwest-trending structural and topographic high on the Irish continental slope. Drilling results have been integrated with physiographic, gravimetric, paleomagnetic, and seismostratigraphic data to provide a comprehensive interpretation of the geologic history of this sediment-starved passive margin. </p><p>The geologic history of Goban Spur and adjacent regions may be divided into three periods: (1) a pre-rift period, beginning at the end of the Hercynian orogeny, was marked by several phases of regional faulting. From the late Paleozoic to the Triassic, a major phase was responsible for the development of northeast-trending grabens and horsts, which were especially active areas of deposition during the early and middle Mesozoic. A second phase created northwesttrending listric, normal fault systems which delineated the pre-Atlantic rift system of the Early Cretaceous. (2) A terminal period of active rifting began approximately at the Jurassic/Cretaceous boundary (late Cimmerian phase), and was marked by a regional emergence. Syn-rift deposition is recorded at Goban Spur by accumulation of a transgressive sequence of hyposaline to pelagic sediments, chiefly Barremian. Interpretation of seismic profiles indicates that (?)Aptian sequences also were deposited in the deeper half-grabens during this phase of rifting. Volcanic rocks appear to be rare or absent in the syn-rift deposits on Goban Spur. (3) The post-rifting period began when ocean crust was accreted in a trough approximately 2000 m deep, beneath what is now the Porcupine Abyssal Plain. This period was marked by the outpouring of pillows and flows of typical oceanic tholeiites, some of which were recovered at Site 550. At the same time, the seaward edge of the continental crust appears to have been deeply intruded by oceanic tholeiites, forming an intermediate crust of transitional geophysical characteristics. </p><p>Post-rift sedimentation started in the early Albian, and was accompanied by continuous regional subsidence. Before the Campanian, variable depositional environments produced quite diverse sedimentary sequences in the isolated halfgrabens. Carbonaceous shales were recovered in Cenomanian strata of the deepest site (550) and in lower Turonian beds at sites of intermediate depth (549-551). Depositional environments became more uniform across the margin after the late Campanian, and sedimentation was clearly influenced by more regional or global oceanographic events. Sea-level oscillations, climatic variations, changes in bottom circulation, and vertical fluctuations of the carbonate compensation depth (CCD) were responsible for lithologic changes and major hiatuses. </p>","language":"English","publisher":"Texas A&M","doi":"10.2973/dsdp.proc.80.158.1985","usgsCitation":"de Graciansky, P., and Poag, C., 1985, Geologic history of Goban Spur, Northwest Europe continental margin: Initial reports of the Deep Sea Drilling Project, v. 80, no. 2, p. 1187-1216, https://doi.org/10.2973/dsdp.proc.80.158.1985.","productDescription":"30 p.","startPage":"1187","endPage":"1216","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":487514,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2973/dsdp.proc.80.158.1985","text":"Publisher Index Page"},{"id":376154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Goban Spur","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -30.585937499999996,\n              50.51342652633956\n            ],\n            [\n              -8.349609375,\n              50.51342652633956\n            ],\n            [\n              -8.349609375,\n              63.860035895395306\n            ],\n            [\n              -30.585937499999996,\n              63.860035895395306\n            ],\n            [\n              -30.585937499999996,\n              50.51342652633956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"80","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"de Graciansky, P.C.","contributorId":228807,"corporation":false,"usgs":false,"family":"de Graciansky","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":792246,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poag, Claude (Wylie) 0000-0002-6240-4065 wpoag@usgs.gov","orcid":"https://orcid.org/0000-0002-6240-4065","contributorId":195779,"corporation":false,"usgs":true,"family":"Poag","given":"Claude (Wylie)","email":"wpoag@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":792247,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012781,"text":"70012781 - 1985 - Plutonium, americium, and neptunium speciation in selected groundwaters","interactions":[],"lastModifiedDate":"2025-05-22T16:48:18.816451","indexId":"70012781","displayToPublicDate":"2017-05-13T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2910,"text":"Nuclear Technology","active":true,"publicationSubtype":{"id":10}},"title":"Plutonium, americium, and neptunium speciation in selected groundwaters","docAbstract":"<p><span>As part of a continuing study, plutonium, americium, and neptunium speciation was determined at 25 and 90°C in four groundwaters from diverse sources: the Sparta aquifer in Louisiana, near the Vacherie salt dome; Mansfield No. 2 well in the Palo Duro Basin, Texas; the Stripa mine in Sweden; and the Waste Isolation Pilot Plant (WIPP) in New Mexico. Plutonium generally was soluble in Sparta and Stripa waters, regardless of temperature or initial oxidation state. Solubility in Mansfield water was high, except in 90 °C experiments using low-oxidation-state plutonium. The WIPP water had the least ability to maintain plutonium in solution; solubility after 30 days exceeded 50% only in experiments at 25 °C using Pu(V) and Pu(VI). Neptunium generally was soluble in all waters and was present exclusively as Np(V) and Np(VI), regardless of initial oxidation state. The solubility of americium was consistently high in Sparta groundwater at both temperatures and in Mansfield and WIPP waters at 25°C, but was &lt; 50% after 30 days in Stripa water at both temperatures and in Mansfield and WIPP waters at 90°C. The results indicated that plutonium and neptunium solubilities were determined by the oxidation-reduction properties of the waters, i.e., their abilities to convert these elements to soluble oxidation states. This was not the case for americium, however; Am(IV) was not detected, and the solubility of this element was determined entirely by the chemical properties of Am(III).</span></p>","language":"English","publisher":"American Nuclear Society","doi":"10.13182/NT85-A33619","issn":"00295450","usgsCitation":"Cleveland, J., Rees, T., and Nash, K., 1985, Plutonium, americium, and neptunium speciation in selected groundwaters: Nuclear Technology, v. 69, no. 3, p. 380-387, https://doi.org/10.13182/NT85-A33619.","productDescription":"8 p.","startPage":"380","endPage":"387","costCenters":[],"links":[{"id":222101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"69","issue":"3","noUsgsAuthors":false,"publicationDate":"2017-05-13","publicationStatus":"PW","scienceBaseUri":"505a7c9ee4b0c8380cd79aaa","contributors":{"authors":[{"text":"Cleveland, J.M.","contributorId":66734,"corporation":false,"usgs":true,"family":"Cleveland","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":364512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rees, T.F.","contributorId":26068,"corporation":false,"usgs":true,"family":"Rees","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":364510,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nash, K.L.","contributorId":27191,"corporation":false,"usgs":true,"family":"Nash","given":"K.L.","affiliations":[],"preferred":false,"id":364511,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012863,"text":"70012863 - 1985 - Leaching of plutonium from a radioactive waste glass by eight groundwaters from the western United States","interactions":[],"lastModifiedDate":"2025-05-22T16:44:50.53224","indexId":"70012863","displayToPublicDate":"2017-05-13T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2910,"text":"Nuclear Technology","active":true,"publicationSubtype":{"id":10}},"title":"Leaching of plutonium from a radioactive waste glass by eight groundwaters from the western United States","docAbstract":"The leachability of a radioactive waste glass formulated to Battelle Pacific Northwest Laboratory specification 80-270 has been studied using eight actual groundwaters with a range of chemical compositions as leachants. Waters collected from the Grande Ronde Basalt (Washington State) and from alluvial deposits in the Hualapai Valley (Arizona) were the most effective at removing plutonium from this glass. Leaching was shown to be incongruent; plutonium was removed from the glass more slowly than the overall glass matrix. The results of these experiments indicate the need to study the leachability of actual waste forms using the actual projected groundwaters that are most likely to come into contact with the waste should a radioactive waste repository be breached.","language":"English","publisher":"American Nuclear Society","doi":"10.13182/NT85-A33672","issn":"00295450","usgsCitation":"Rees, T., Cleveland, J., and Nash, K., 1985, Leaching of plutonium from a radioactive waste glass by eight groundwaters from the western United States: Nuclear Technology, v. 70, no. 1, p. 133-140, https://doi.org/10.13182/NT85-A33672.","productDescription":"8 p.","startPage":"133","endPage":"140","numberOfPages":"8","costCenters":[],"links":[{"id":222446,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.22304850505517,\n              48.96938338954959\n            ],\n            [\n              -125.22304850505517,\n              32.02637914252497\n            ],\n            [\n              -102.34258038032547,\n              32.02637914252497\n            ],\n            [\n              -102.34258038032547,\n              48.96938338954959\n            ],\n            [\n              -125.22304850505517,\n              48.96938338954959\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"70","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-05-13","publicationStatus":"PW","scienceBaseUri":"505a45a1e4b0c8380cd67450","contributors":{"authors":[{"text":"Rees, T.F.","contributorId":26068,"corporation":false,"usgs":true,"family":"Rees","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":364700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cleveland, J.M.","contributorId":66734,"corporation":false,"usgs":true,"family":"Cleveland","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":364702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nash, K.L.","contributorId":27191,"corporation":false,"usgs":true,"family":"Nash","given":"K.L.","affiliations":[],"preferred":false,"id":364701,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180231,"text":"70180231 - 1985 - Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180231,"text":"70180231 - 1985 - Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180231","publicationYear":"1985","noYear":false,"title":"Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2017-06-07T16:28:18","indexId":"70180231","displayToPublicDate":"2017-01-25T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>The more prominent of the two visible intracaldera cones of Mount Veniaminof went into eruption in early June 1983 and continued until early April 1984. Veniaminof is a 2,507-m-high composite cone having an 8 x 11-km summit caldera which formed 3,300-3,700 yr B.P. (Miller and Smith, 1977). The active 1.6x1.2-km cone protrudes 200 m through the glacial ice filling the caldera; it lies in a 60-m-long belt of cinder cones that is transverse to the trend of the Aleutian arc (fig. 44). </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180231","usgsCitation":"Yount, M.E., Miller, T.P., Emanuel, R.P., and Wilson, F.H., 1985, Eruption in an ice-filled caldera, Mount Veniaminof, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 2 p., https://doi.org/10.3133/70180231.","productDescription":"2 p.","startPage":"59","endPage":"60","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"links":[{"id":333998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333997,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=71","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula, Mount Veniaminof","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7bfe4b0ba3b075e0637","contributors":{"authors":[{"text":"Yount, M. Elizabeth","contributorId":178741,"corporation":false,"usgs":false,"family":"Yount","given":"M.","email":"","middleInitial":"Elizabeth","affiliations":[],"preferred":false,"id":660828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":660829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emanuel, Richard P.","contributorId":98287,"corporation":false,"usgs":true,"family":"Emanuel","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":660830,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660831,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70180236,"text":"70180236 - 1985 - Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180236,"text":"70180236 - 1985 - Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180236","publicationYear":"1985","noYear":false,"title":"Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2018-05-07T21:26:33","indexId":"70180236","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>Extensive seacliff exposures of marble, metadolostone, and schist occur on the north shore of Seward Peninsula in the Kotzebue A-1 and A-2 Quadrangles (fig. 12). Some of the exposed units have no analogs when compared to rocks mapped to the south in the Bendeleben and Solomon Quadrangles. Others are similar to units exposed to the south, but they differ in metamorphic grade and minor, though significant, compositional characteristics. Carbonate rocks predominate from Ninemile Point westward; schists of varying composition occur with carbonate rocks to the east. The carbonate-dominated section is separated in the vicinity of Ninemile Point from the schist-dominated section by a major fault zone, thought to be the northern extension of the Kugruk fault zone of Sainsbury (1974). </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180236","usgsCitation":"Dumoulin, J.A., and Till, A.B., 1985, Sea cliff exposures of metamorphosed carbonate and schist, northern Seward Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 5 p., https://doi.org/10.3133/70180236.","productDescription":"5 p.","startPage":"19","endPage":"22","numberOfPages":"5","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334021,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334020,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=30","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7bfe4b0ba3b075e0639","contributors":{"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":660850,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180229,"text":"70180229 - 1985 - Digital image processing techniques for detecting surface alteration - An application on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180229,"text":"70180229 - 1985 - Digital image processing techniques for detecting surface alteration - An application on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180229","publicationYear":"1985","noYear":false,"title":"Digital image processing techniques for detecting surface alteration - An application on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2017-01-27T11:14:18","indexId":"70180229","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Digital image processing techniques for detecting surface alteration - An application on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>The tectonic evolution of the Alaska Peninsula makes it a likely area for the discovery of significant mineral deposits. However, because of problems associated with remoteness and poor weather, little detailed mineral exploration work has been carried on there. This study focuses on using Landsat multispectral scanner data for the Port Moller, Stepovak Bay, and Simeon of Island Quadrangles to detect surface alteration, probably limonitic (iron oxide staining) and(or) argillic (secondary clay minerals) in character, that could be indicative of mineral deposits. The techniques used here are useful for mapping deposits that have exposed surface alteration of at least an hectare, the approximate spatial resolution of the Landsat data. Virtually cloud-free Landsat coverage was used, but to be detected, the alteration area must also be unobscured by vegetation. Not all mineral deposits will be associated with surface alteration, and not all areas of surface alteration will have valuable mineral deposits. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180229","usgsCitation":"York, J., Wilson, F.H., and Gamble, B.M., 1985, Digital image processing techniques for detecting surface alteration - An application on the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 3 p., https://doi.org/10.3133/70180229.","productDescription":"3 p.","startPage":"56","endPage":"58","numberOfPages":"3","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333994,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=68","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e064c","contributors":{"authors":[{"text":"York, James","contributorId":69604,"corporation":false,"usgs":true,"family":"York","given":"James","email":"","affiliations":[],"preferred":false,"id":660825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660826,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gamble, Bruce M. bgamble@usgs.gov","contributorId":560,"corporation":false,"usgs":true,"family":"Gamble","given":"Bruce","email":"bgamble@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":660827,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180233,"text":"70180233 - 1985 - Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180233,"text":"70180233 - 1985 - Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180233","publicationYear":"1985","noYear":false,"title":"Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2017-05-19T18:13:51","indexId":"70180233","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>A zone of structural disruption and complexity along the Pacific coast margin of the Alaska Peninsula (fig. 41) may be related to the Alaska Peninsula and the Chugach terrane boundary. The best exposure of this zone is located on the east shore of Humpback Bay (figs. 42, 43; also Burk, 1965, pl. 8, fig. 4); other exposures are located on the east side of Ivanof Bay, the north and south sides of Lefthand Bay, and in other coastal localities in the area. In some places, such as on the Kupreanof Peninsula, it is not recognized. This zone may extend discontinuously for 110-160 km along the coast; the width of the zone varies from 0.5 to 1 km. Our current data and tentative interpretations are described here, pending completion of additional field research, laboratory, and office studies. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180233","usgsCitation":"Wilson, F.H., Case, J.E., and Detterman, R.L., 1985, Preliminary description of a Miocene zone of structural complexity, Port Moller and Stepovak Bay quadrangles, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 2 p., https://doi.org/10.3133/70180233.","productDescription":"2 p.","startPage":"55","endPage":"56","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334006,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=67","text":"Start page in larger work"},{"id":334007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Port Moller quadrangle, Stepovak Bay quadrangle","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7bfe4b0ba3b075e063b","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":660835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, James E.","contributorId":68702,"corporation":false,"usgs":true,"family":"Case","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660836,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660837,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180232,"text":"70180232 - 1985 - Newly discovered Holocene volcanic vents, Port Moller and Stepovak Bay quadrangles, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","interactions":[{"subject":{"id":70180232,"text":"70180232 - 1985 - Newly discovered Holocene volcanic vents, Port Moller and Stepovak Bay quadrangles, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","indexId":"70180232","publicationYear":"1985","noYear":false,"title":"Newly discovered Holocene volcanic vents, Port Moller and Stepovak Bay quadrangles, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>"},"predicate":"IS_PART_OF","object":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"id":1}],"isPartOf":{"id":4437,"text":"cir945 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1983","indexId":"cir945","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1983"},"lastModifiedDate":"2017-01-27T11:15:30","indexId":"70180232","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"945","title":"Newly discovered Holocene volcanic vents, Port Moller and Stepovak Bay quadrangles, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>","docAbstract":"<p>Reconnaissance mapping in 1982-83 suggests previously unreported Holocene volcanic activity in the area 14-24 km southwest of Kupreanof Volcano (fig. 45). One young volcanic vent has been observed along the divide between Stepovak Bay and Bear Lake, and the locations of two others are inferred from the position of morphologically young lava flows mapped in valleys draining into Clark Bay, Grub Gulch, and Ramsey Bay. Other morphologically young flows extending northwest from the divide are evident on aerial photographs. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1983 (Circular 945)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180232","usgsCitation":"Yount, M.E., Wilson, F.H., and Miller, J.W., 1985, Newly discovered Holocene volcanic vents, Port Moller and Stepovak Bay quadrangles, Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1983</i>: U.S. Geological Survey Circular 945, 3 p., https://doi.org/10.3133/70180232.","productDescription":"3 p.","startPage":"60","endPage":"62","numberOfPages":"3","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334003,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334002,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0945/report.pdf#page=72","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula, Port Moller quadrangle, Stepovak Bay quadrangle","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e064a","contributors":{"authors":[{"text":"Yount, M. Elizabeth","contributorId":178741,"corporation":false,"usgs":false,"family":"Yount","given":"M.","email":"","middleInitial":"Elizabeth","affiliations":[],"preferred":false,"id":660832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, John W.","contributorId":70357,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":660834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180057,"text":"70180057 - 1985 - The continued rise of Great Salt Lake, Utah","interactions":[{"subject":{"id":70180057,"text":"70180057 - 1985 - The continued rise of Great Salt Lake, Utah","indexId":"70180057","publicationYear":"1985","noYear":false,"title":"The continued rise of Great Salt Lake, Utah"},"predicate":"IS_PART_OF","object":{"id":70039036,"text":"70039036 - 1985 - United States Geological Survey Yearbook, fiscal year 1984","indexId":"70039036","publicationYear":"1985","noYear":false,"title":"United States Geological Survey Yearbook, fiscal year 1984"},"id":1}],"isPartOf":{"id":70039036,"text":"70039036 - 1985 - United States Geological Survey Yearbook, fiscal year 1984","indexId":"70039036","publicationYear":"1985","noYear":false,"title":"United States Geological Survey Yearbook, fiscal year 1984"},"lastModifiedDate":"2017-01-23T16:17:11","indexId":"70180057","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"The continued rise of Great Salt Lake, Utah","docAbstract":"<p>The Great Salt Lake rose 5.0 feet from September 25,1983, to July 1, 1984, the second largest seasonal rise on record since 1847. The maximum seasonal rise was observed the previous year when the lake rose 5.1 feet from September 18,1982, to June 30,1983. The lake declined only 0.5 foot during summer 1983; thus, the net rise from September 18,1982, to July 1,1984, was 9.6 feet. By comparison, the previously recorded maximum net rise over a similar period of time was 4.75 feet from 1970 to 1972.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"United States Geological Survey Yearbook, Fiscal Year 1984","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washginton, D.C.","doi":"10.3133/70180057","usgsCitation":"Arnow, T., 1985, The continued rise of Great Salt Lake, Utah: Yearbook, 2 p., https://doi.org/10.3133/70180057.","productDescription":"2 p.","startPage":"97","endPage":"98","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248ae4b08aa8f945abf2","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":660184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179791,"text":"70179791 - 1985 - Water use data for public water suppliers and self supplied industry in Utah: 1982, 1983","interactions":[],"lastModifiedDate":"2017-01-19T09:23:17","indexId":"70179791","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5267,"text":"Utah Division of Water Rights Water-Use Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Water use data for public water suppliers and self supplied industry in Utah: 1982, 1983","docAbstract":"<p><span>This publication is the fifth in a continuing series of reports presenting water use data for Utah. The data are collected by the State of Utah, Division of Water Rights, for the National Water Use Information Program. This is a cooperative effort with the U.S. Geological Survey.</span><span>&nbsp; </span><span>Most states contribute information in some form to the program.</span></p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah, Division of Water Rights","usgsCitation":"Johnson, B., 1985, Water use data for public water suppliers and self supplied industry in Utah: 1982, 1983: Utah Division of Water Rights Water-Use Report 5, viii, 137 p.","productDescription":"viii, 137 p.","numberOfPages":"143","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333290,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333289,"rank":1,"type":{"id":15,"text":"Index 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,{"id":70179626,"text":"70179626 - 1985 - Ground water in Utah - A summary description of the resource and its related physical environment","interactions":[],"lastModifiedDate":"2017-01-17T10:11:16","indexId":"70179626","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5257,"text":"Utah Department of Natural Resources Water Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3","title":"Ground water in Utah - A summary description of the resource and its related physical environment","docAbstract":"<p>Ground water is one of Utah’s most extensive and valuable natural resources. Because of its widespread occurrence in both wet and dry areas, ground water has been, and is a major factor affecting economic growth and development of the State. In some areas, ground water is used to supplement streamflow for irrigation, public supply, and other uses. In other areas, it is the only water available for use. Many communities obtain their entire water supply from ground-water sources (wells and springs) as do numerous rural and suburban households throughout the State.</p><p>The ground-water reservoirs of Utah contain tremendous quantities of water – many times more than the quantity stored in all the lakes (including Great Salt Lake) and the surface-water reservoirs of the State combined. Water that discharges from those underground reservoirs in seeps and springs is vital in sustaining the flow of streams during dry summer months and in providing the water needed to maintain important wetland habitats. Those same underground reservoirs also provide large quantities of water in carryover storage for use during prolonged droughts.</p><p>The U.S. Geological survey, under cooperative programs with the Utah department of Natural resources and other Federal, State, and local agencies has been studying Utah’s ground-water resources since 1897. Much information has been gained during those studies about the occurrence, availability, and quality of ground water; the withdrawal and use of the water; and the effects of withdrawal. This report summarizes that information in nontechnical language, which is designed for all readers. Readers interested in more detailed information about ground water in specific areas of Utah are referred to the reports listed by LaPray and Hamblin (1980).</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Price, D., and Arnow, T., 1985, Ground water in Utah - A summary description of the resource and its related physical environment: Utah Department of Natural Resources Water Circular 3, iv, 49 p.","productDescription":"iv, 49 p.","numberOfPages":"57","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":332963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":332961,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-6-060"}],"country":"United 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,{"id":70179993,"text":"70179993 - 1985 - Developing a state water plan: Ground-water conditions in Utah, spring of 1985","interactions":[],"lastModifiedDate":"2017-01-20T17:38:13","indexId":"70179993","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1985","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":"25","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1985","docAbstract":"<p>This is the twenty-second in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published 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.</p><p>This report, like the others in the series, contains information on well construction, ground-water withdrawals from wells, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing ground-water level contours are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water development in the State for the calendar year 1984. Water-level fluctuations, however, are described from the spring of 1984 to the spring of 1985. 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.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Seiler, R.L., Herbert, L.R., Bischoff, D.A., Clark, D.W., Pyper, G., Burden, C.B., Jensen, V., Enright, M., Emett, D.C., Sether, B., Eckenwiler, M., and Sandberg, G.W., 1985, Developing a state water plan: Ground-water conditions in Utah, spring of 1985: Cooperative Investigations Report 25, vii, 84 p.","productDescription":"vii, 84 p.","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333652,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333651,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-180"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5883303be4b0d0023163782a","contributors":{"authors":[{"text":"Seiler, Ralph L.","contributorId":13609,"corporation":false,"usgs":true,"family":"Seiler","given":"Ralph","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":659577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659578,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bischoff, Donald A. bischoff@usgs.gov","contributorId":4030,"corporation":false,"usgs":true,"family":"Bischoff","given":"Donald","email":"bischoff@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":659579,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659580,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pyper, George","contributorId":178537,"corporation":false,"usgs":false,"family":"Pyper","given":"George","email":"","affiliations":[],"preferred":false,"id":659581,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Burden, Carole B. cburden@usgs.gov","contributorId":852,"corporation":false,"usgs":true,"family":"Burden","given":"Carole","email":"cburden@usgs.gov","middleInitial":"B.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":659582,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659583,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Enright, Michael","contributorId":99979,"corporation":false,"usgs":true,"family":"Enright","given":"Michael","email":"","affiliations":[],"preferred":false,"id":659584,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659585,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sether, B.A.","contributorId":61504,"corporation":false,"usgs":true,"family":"Sether","given":"B.A.","affiliations":[],"preferred":false,"id":659586,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Eckenwiler, M.R.","contributorId":9674,"corporation":false,"usgs":true,"family":"Eckenwiler","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":659587,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659588,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70178908,"text":"70178908 - 1985 - Seepage study of six canals in Salt Lake County, Utah, 1982-1983","interactions":[],"lastModifiedDate":"2016-12-12T11:15:30","indexId":"70178908","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"82","title":"Seepage study of six canals in Salt Lake County, Utah, 1982-1983","docAbstract":"<p>A study of selected reaches of the Utah and Salt Lake, Utah Lake Distributing, Provo Reservoir, Draper Irrigation, East Jordan, and Jordan and Salt Lake City Canals in Salt Lake County, Utah, was made to determine gains or losses of flow in those reaches. Three to five sets of seepage measurements were made on each canal during 1982 or 1983. Adjustments for fluctuations in flow were made from information obtained from water-stage recorders operated at selected locations during the time of each seepage run.</p><p>The study showed an overall net loss of about 9.5 cubic feet per second in the Utah and Salt Lake Canal, 11.0 cubic feet per second in the Utah Lake Distributing canal, 20.5 cubic feet per second in the Provo Reservoir canal, 1.5 cubic feet per second in the Draper Irrigation Canal, and 4.0 cubic feet per second in the East Jordan canal. It also showed a net gain of about 6.0 cubic feet per second in the Jordan and Salt Lake City Canal. The gains and losses are attributed primarily to the relation of the canals to the depth of the water table near the canals.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Herbert, L.R., Cruff, R., and Waddell, K., 1985, Seepage study of six canals in Salt Lake County, Utah, 1982-1983: Technical Publication 82, iv, 95 p.","productDescription":"iv, 95 p","numberOfPages":"102","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331891,"rank":1,"type":{"id":15,"text":"Index 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