{"pageNumber":"376","pageRowStart":"9375","pageSize":"25","recordCount":11004,"records":[{"id":33580,"text":"b1486 - 1979 - Upper Paleozoic carbonate bank in east-central Idaho: Snaky Canyon, Bluebird Mountain, and Arco Hills Formations, and their paleotectonic significance","interactions":[],"lastModifiedDate":"2023-08-29T18:45:14.09972","indexId":"b1486","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1486","title":"Upper Paleozoic carbonate bank in east-central Idaho: Snaky Canyon, Bluebird Mountain, and Arco Hills Formations, and their paleotectonic significance","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1486","usgsCitation":"Skipp, B., Hoggan, R.D., Schleicher, D.L., and Douglass, R.C., 1979, Upper Paleozoic carbonate bank in east-central Idaho: Snaky Canyon, Bluebird Mountain, and Arco Hills Formations, and their paleotectonic significance: U.S. Geological Survey Bulletin 1486, iii, 78 p., https://doi.org/10.3133/b1486.","productDescription":"iii, 78 p.","costCenters":[],"links":[{"id":61464,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1486/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163030,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1486/report-thumb.jpg"},{"id":420253,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92700.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114,\n              44.5\n            ],\n            [\n              -114,\n              43.411\n            ],\n            [\n              -112.5,\n              43.411\n            ],\n            [\n              -112.5,\n              44.5\n            ],\n            [\n              -114,\n              44.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a24e4b07f02db60e61c","contributors":{"authors":[{"text":"Skipp, Betty","contributorId":51268,"corporation":false,"usgs":true,"family":"Skipp","given":"Betty","affiliations":[],"preferred":false,"id":211589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoggan, R. D.","contributorId":104954,"corporation":false,"usgs":true,"family":"Hoggan","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":211591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schleicher, D. L.","contributorId":86009,"corporation":false,"usgs":true,"family":"Schleicher","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":211590,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Douglass, R. C.","contributorId":43827,"corporation":false,"usgs":true,"family":"Douglass","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":211588,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":37360,"text":"ssrw216 - 1979 - Environmental pollutants and eggshell thickness: Anhingas and wading birds in the eastern United States","interactions":[],"lastModifiedDate":"2020-03-19T13:40:37","indexId":"ssrw216","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"216","title":"Environmental pollutants and eggshell thickness: Anhingas and wading birds in the eastern United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Ohlendorf, H.M., Klaas, E.E., and Kaiser, T.E., 1979, Environmental pollutants and eggshell thickness: Anhingas and wading birds in the eastern United States: Special Scientific Report  - Wildlife 216, 94 p.","productDescription":"94 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":167106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia, Iowa, Louisiana, Maryland, Massachusetts, Michigan, Minnesota, Missouri, New Jersey, New York, North Carolina, Ohio, Rhode Island, South Carolina, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.470703125,\n              25.24469595130604\n            ],\n            [\n              -70.4443359375,\n              25.24469595130604\n            ],\n            [\n              -70.4443359375,\n              49.1242192485914\n            ],\n            [\n              -97.470703125,\n              49.1242192485914\n            ],\n            [\n              -97.470703125,\n              25.24469595130604\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60226b","contributors":{"authors":[{"text":"Ohlendorf, Harry M.","contributorId":60291,"corporation":false,"usgs":true,"family":"Ohlendorf","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":217928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klaas, Erwin E.","contributorId":101219,"corporation":false,"usgs":true,"family":"Klaas","given":"Erwin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":217930,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaiser, T. Earl","contributorId":84826,"corporation":false,"usgs":true,"family":"Kaiser","given":"T.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":217929,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70168611,"text":"70168611 - 1979 - The Survey’s first venture into seismology","interactions":[],"lastModifiedDate":"2016-03-22T16:52:02","indexId":"70168611","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The Survey’s first venture into seismology","docAbstract":"<p>The occurrence of two small but widely felt earthquakes in the Eastern United States in 1884 led an editor of the research journal <i>Science&nbsp;</i>to suggest, in the October 3 issue of the magazine, that an \"earthquake club\" be formed. Its purpose was so that observers and students of \"this branch of physical geography\" could become acquainted with each other and thus insure the proper collection and collation of their observations. Because this was its intent, he though the club should be \"unembarrassed by formal regulations\"; consequently, there is no record of whether such an organziation ever existed. But the other suggestion, thata of collecting earthquake records was acted on promptly. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Rabbitt, M.C., 1979, The Survey’s first venture into seismology: Earthquake Information Bulletin (USGS), v. 11, no. 2, p. 50-52.","productDescription":"3 p.","startPage":"50","endPage":"52","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318229,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56c99c5fe4b059daa47c9b0b","contributors":{"authors":[{"text":"Rabbitt, M. C.","contributorId":115566,"corporation":false,"usgs":true,"family":"Rabbitt","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":621019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190671,"text":"70190671 - 1979 - The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","interactions":[{"subject":{"id":9104,"text":"ofr7793 - 1977 - The Yellow Dog peridotite and a possible buried igneous complex of Lower Keweenawan Age in the northern peninsula of Michigan","indexId":"ofr7793","publicationYear":"1977","noYear":false,"title":"The Yellow Dog peridotite and a possible buried igneous complex of Lower Keweenawan Age in the northern peninsula of Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":70190671,"text":"70190671 - 1979 - The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","indexId":"70190671","publicationYear":"1979","noYear":false,"title":"The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan"},"id":1}],"lastModifiedDate":"2018-11-19T11:06:20","indexId":"70190671","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":282,"text":"Michigan Geological Survey Report of Investigation","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","docAbstract":"<p>Partly serpentinized peridotite of early Keweenawan age crops out in two places along a 20-kilometer-long zone of positive aeromagnetic anomalies in northern Marquette County, Michigan. Most of the area is mantled by Pleistocene drift with few bedrock exposures.</p><p>Petrographic and electron microprobe studies show that the peridotite was originally a plagioclase lherzolite containing 40 to 50 percent<span>&nbsp;</span>olivine (Fo8<sub>0</sub>) and approximately 10 to 15 percent each of enstatite (En<sub>78</sub>Wo<sub>04</sub>Fs<sub>18</sub>) and diopsidic augite (En<sub>47</sub>Wo<sub>42</sub>Fs<sub>11</sub>). The plagioclase varies from 5 to 10 percent, and according to Morris (1977) is labradorite with a composition of An<sub>57-65</sub>. Major oxide minerals (4 to 6 percent) are ilmenite and magnetite. Sulfides comprise 1 to 2 percent of the peridotite and are chiefly pyrrhotite, pentlandite, and chalcopyrite.</p><p>Ground magnetic, gravity, and very low frequency electro-magnetic (VLF-EM)<span>&nbsp;</span>surveys have refined the location and magnitude of anomalies previously known only from aeromagnetic studies. These surveys together with soil geochemical studies suggest that peridotite, and possibly other mafic rocks forming a differentiated igneous complex, may occur throughout a belt 20 kilometers long (east-west) and 1 to 2 kilometers wide (north-south).</p><p>Differentiated igneous complexes in many parts of the world are hosts for copper, nickel, chromium, or precious-metal deposits. The peridotite in the area of this study is anomalously rich in copper and sulfur compared to world-wide averages for peridotite. Positive electro-magnetic anomalies found near the peridotite outcrops may be caused by sulfide-rich zones in the igneous rocks and should be explored further for copper-nickel&nbsp;mineralization.</p>","language":"English","publisher":"State of Michigan Department of Natural Resources","publisherLocation":"Lansing, MI","usgsCitation":"Klasner, J.S., Snider, D.W., Cannon, W., and Slack, J.F., 1979, The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan: Michigan Geological Survey Report of Investigation 24, v, 31 p.","productDescription":"v, 31 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":345637,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345636,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.michigan.gov/documents/deq/RI_24opt_309211_7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b8f222e4b08b1644e0af0f","contributors":{"authors":[{"text":"Klasner, John S.","contributorId":46591,"corporation":false,"usgs":true,"family":"Klasner","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":710088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snider, David W.","contributorId":196332,"corporation":false,"usgs":true,"family":"Snider","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":710090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":710091,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012269,"text":"70012269 - 1979 - Petrology, composition, and age of intrusive rocks associated with the Quartz Hill molybdenite deposit, southeastern Alaska","interactions":[],"lastModifiedDate":"2023-09-26T14:34:51.484866","indexId":"70012269","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Petrology, composition, and age of intrusive rocks associated with the Quartz Hill molybdenite deposit, southeastern Alaska","docAbstract":"<p><span>A large porphyry molybdenum deposit (Quartz Hill deposit) was recently discovered in the heart of the Coast Range batholithic complex about 70 km east of Ketchikan, southeastern Alaska. Intrusive rocks associated with the mineral deposit form two composite epizonal to hypabyssal stocks and many dikes in country rocks. The stocks are characterized by a variety of textural rock types varying from equigranular or weakly seriate biotite granite to porphyries with aphanitic or very fine grained and aplitic groundmasses. These rocks contain about equal amounts of quartz, albitic plagioclase, and microperthitic microcline and less than 2.5% biotite. Unaltered rocks contain between 0.2 and 1% CaO, less than 1.7% combined Fe</span><sub>2</sub><span>O</span><sub>3</sub><span>, FeO, and MgO, and 74.4 to 77.7% SiO</span><sub>2</sub><span>. Total alkalis are between 8 and 9%, and K</span><sub>2</sub><span>O/Na</span><sub>2</sub><span>O is about 1.1. The range of major-oxide variation is small, but it is systematically related to lithology. Many trace-elements, including B, Pb, Sn, and Li have low concentrations. Intrusive rocks associated with the Quartz Hill deposit are more albitic and possibly trace-element depleted compared to some other rocks associated with porphyry molybdenum deposits.All observed metallization and alteration is within the Quartz Hill stock. Molybdenite forms fracture coatings and occurs in veins with quartz. Alteration is widespread and includes development of secondary quartz, pyrite, K-feldspar, biotite, white mica, chlorite, and zeolite. Field relations indicate that the stocks were emplaced after regional uplift and erosion of the Coast Range batholithic complex, and K–Ar data show that intrusion and alteration took place in late Oligocene time, about 27 to 30 Ma ago. Data from the Ketchikan quadrangle indicate that porphyry molybdenum metallization in the Coast Range batholithic complex is associated with regionally extensive but spotty, middle Tertiary or younger, felsic magmatism.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/e79-165","issn":"00084077","usgsCitation":"Hudson, T., Smith, J., and Elliott, R.L., 1979, Petrology, composition, and age of intrusive rocks associated with the Quartz Hill molybdenite deposit, southeastern Alaska: Canadian Journal of Earth Sciences, v. 16, no. 9, p. 1805-1822, https://doi.org/10.1139/e79-165.","productDescription":"18 p.","startPage":"1805","endPage":"1822","costCenters":[],"links":[{"id":222248,"rank":1,"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        \"coordinates\": [\n          [\n            [\n              -134.98399926363345,\n              56.25002201433318\n            ],\n            [\n              -134.98399926363345,\n              54.61996337638038\n            ],\n            [\n              -129.86277390708392,\n              54.61996337638038\n            ],\n            [\n              -129.86277390708392,\n              56.25002201433318\n            ],\n            [\n              -134.98399926363345,\n              56.25002201433318\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"16","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7858e4b0c8380cd78698","contributors":{"authors":[{"text":"Hudson, T.","contributorId":33446,"corporation":false,"usgs":true,"family":"Hudson","given":"T.","affiliations":[],"preferred":false,"id":363139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":363140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, Raymond L.","contributorId":82667,"corporation":false,"usgs":true,"family":"Elliott","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":363141,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":48460,"text":"ofr791664 - 1979 - Measured sections of Ordovician strata in east-central Kentucky","interactions":[],"lastModifiedDate":"2025-01-14T19:04:07.759196","indexId":"ofr791664","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1664","title":"Measured sections of Ordovician strata in east-central Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791664","collaboration":"Prepared in cooperation with the Kentucky Geological Survey.","usgsCitation":"Peterson, W.L., and Swadley, W.C., 1979, Measured sections of Ordovician strata in east-central Kentucky: U.S. Geological Survey Open-File Report 79-1664, 193 p., https://doi.org/10.3133/ofr791664.","productDescription":"193 p.","costCenters":[],"links":[{"id":466244,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1664/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170003,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1664/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"east-central Kentucky","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95.68847379016451,\n              28.729932154553637\n            ],\n            [\n              -95.68298221282795,\n              28.729932154553637\n            ],\n            [\n              -95.68298221282795,\n              28.73354374537847\n            ],\n            [\n              -95.68847379016451,\n              28.73354374537847\n            ],\n            [\n              -95.68847379016451,\n              28.729932154553637\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.98836476430037,\n              39.050936628931964\n            ],\n            [\n              -85.93336761292312,\n              39.050936628931964\n            ],\n            [\n              -85.93336761292312,\n              37.699945022991145\n            ],\n            [\n              -83.98836476430037,\n              37.699945022991145\n            ],\n            [\n              -83.98836476430037,\n              39.050936628931964\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","tableOfContents":"<p><br data-mce-bogus=\"1\"></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610dc2","contributors":{"editors":[{"text":"Weir, G. W.","contributorId":107290,"corporation":false,"usgs":true,"family":"Weir","given":"G.","middleInitial":"W.","affiliations":[],"preferred":false,"id":749920,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Peterson, W. L.","contributorId":42218,"corporation":false,"usgs":true,"family":"Peterson","given":"W.","middleInitial":"L.","affiliations":[],"preferred":false,"id":237567,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":237568,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012490,"text":"70012490 - 1978 - Age of the last major scabland flood of the Columbia Plateau in eastern Washington","interactions":[],"lastModifiedDate":"2025-07-14T15:18:37.546213","indexId":"70012490","displayToPublicDate":"2017-01-20T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Age of the last major scabland flood of the Columbia Plateau in eastern Washington","docAbstract":"<p><span>Pumice layers of set S from Mount St. Helens can be correlated with certain ash beds associated with young flood deposits of the channeled scabland. The correlation points to an age of about 13,000&nbsp;</span><span class=\"sup\">14</span><span>C yr B.P. for the last major flood to have crossed the scabland. Until recently, the last major episode of flooding was thought to be closer to 20,000 yr B.P., an age inferred chiefly from the relation of the flood to glacial events of the northern Rocky Mountains. Several investigations within the last few years have suggested that the last major flood occurred well after 20,000 yr B.P. Tentative correlations of ash beds of the scabland with set S pumice layers, the relations of flood and glacial events along the northwestern margin of the Columbia Plateau, and a radiocarbon date from the Snake River drainage southeast of the plateau all indicate an age much younger than 20,000 yr. The postulated age of about 13,000 yr B.P. is further supported by a radiocarbon date in the Columbia River valley downstream from the scabland tract. Basal peat from a bog on the Portland delta of Bretz, which is a downvalley deposit of the last major scabland flood, has been dated as 13,080 ± 300 yr B.P. (W-3404).</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.1016/0033-5894(78)90099-6","issn":"00335894","usgsCitation":"Mullineaux, D.R., Wilcox, R., Ebaugh, W., Fryxell, R., and Rubin, M., 1978, Age of the last major scabland flood of the Columbia Plateau in eastern Washington: Quaternary Research, v. 10, no. 2, p. 171-180, https://doi.org/10.1016/0033-5894(78)90099-6.","productDescription":"10 p.","startPage":"171","endPage":"180","costCenters":[],"links":[{"id":222207,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Columbia Plateau, eastern Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.61626687535127,\n              48.094362272240716\n            ],\n            [\n              -119.61626687535127,\n              46.99900541842095\n            ],\n            [\n              -117.10617240070286,\n              46.99900541842095\n            ],\n            [\n              -117.10617240070286,\n              48.094362272240716\n            ],\n            [\n              -119.61626687535127,\n              48.094362272240716\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e8f2e4b0c8380cd47fd0","contributors":{"authors":[{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilcox, R.E.","contributorId":107348,"corporation":false,"usgs":true,"family":"Wilcox","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":363744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebaugh, W.F.","contributorId":89521,"corporation":false,"usgs":true,"family":"Ebaugh","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":363743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fryxell, R.","contributorId":28369,"corporation":false,"usgs":true,"family":"Fryxell","given":"R.","email":"","affiliations":[],"preferred":false,"id":363740,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":363742,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70043728,"text":"70043728 - 1978 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","interactions":[{"subject":{"id":7913,"text":"ofr77312 - 1977 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","indexId":"ofr77312","publicationYear":"1977","noYear":false,"title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043728,"text":"70043728 - 1978 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","indexId":"70043728","publicationYear":"1978","noYear":false,"title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah"},"id":1}],"lastModifiedDate":"2016-12-09T11:24:07","indexId":"70043728","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"60","title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","docAbstract":"The Parowan-Cedar City drainage basin, Iron County, Utah, includes about 1,100 mi<sup>2</sup> (square miles)(2,800 km<sup>2</sup> [square kilometers])--520 mi<sup>2</sup> (1,300 km<sup>2</sup>) in the Parowan basin and 580 mi<sup>2</sup> (1,500 km<sup>2</sup>) in the Cedar City basin. Parowan and Cedar City Valleys are structural depressions formed by northeast-trending faults. Parowan Valley is essentially a closed basin, whereas Cedar City Valley is drained by two gaps in the mountains bordering the west side of the valley, and a small part of Cedar City Valley is drained at a gap at the south end. Water flowing into the basin from the highlands to the east is used to irrigate lands near Cedar City, Parowan, Paragonah, and Summit. The surface-water outflow from the basin is negligible.","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":"Bjorklund, L., Sunsion, C., and Sandberg, G.W., 1978, Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah: Technical Publication 60, viii, 93 p.","productDescription":"viii, 93 p.","numberOfPages":"110","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331779,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-480"},{"id":267715,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009m.pdf"}],"country":"United States","state":"Utah","county":"Iron County","otherGeospatial":"Parowan-Cedar City Drainage Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0539,37.4744 ], [ -114.0539,38.151 ], [ -112.4696,38.151 ], [ -112.4696,37.4744 ], [ -114.0539,37.4744 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad3ee4b0b6328103b42e","contributors":{"authors":[{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":474176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sunsion, C.T.","contributorId":99846,"corporation":false,"usgs":true,"family":"Sunsion","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":474178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474177,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","interactions":[{"subject":{"id":10425,"text":"ofr7815 - 1977 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"ofr7815","publicationYear":"1977","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"70043282","publicationYear":"1978","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"id":1}],"lastModifiedDate":"2016-12-12T14:46:33","indexId":"70043282","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"63","title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","docAbstract":"Beaver Valley includes 534 square miles in southwestern Utah, in the Basin and Range physiographic province. The project area consists of a valley plain underlain by unconsolidated to partly consolidated material. The valley plain is bounded by mountains that are composed of partly consolidated to consolidated rocks of Pennsylvanian through Tertiary age except for local thin unconsolidated surficial deposits of Quaternary age. The water needs of the valley are supplied mainly by four streams rising in the Tushar Mountains along the eastern side of the valley and by wells in the unconsolidated to partly consolidated materials of the valley plain. The objectives of this study were (1) to measure and analyze the discharge/recharges rates and (2) to measure and analyze the total amount of water in storage in the ground-water reservoirs.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., 1978, Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water: Technical Publication 63, vi, 90 p.","productDescription":"vi, 90 p.","numberOfPages":"100","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331971,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009p.pdf"},{"id":331970,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-530"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.9,\n              38.15\n            ],\n            [\n              -112.9,\n              38.5\n            ],\n            [\n              -112.4,\n              38.5\n            ],\n            [\n              -112.4,\n              38.15\n            ],\n            [\n              -112.9,\n              38.15\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e04e4b0893acf3fffc6","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038340,"text":"70038340 - 1978 - Water resources inventory of Connecticut Part 8: Quinnipiac River basin","interactions":[],"lastModifiedDate":"2014-06-27T15:17:28","indexId":"70038340","displayToPublicDate":"2012-05-01T10:04:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"27","title":"Water resources inventory of Connecticut Part 8: Quinnipiac River basin","docAbstract":"<p>The Quinnipiac River basin area in southcentral Connecticut covers 363 square miles, and includes all drainage basins that enter Long Island Sound from the Branford to the Wepawaug Rivers. Its population in 1970 was estimated at 535,000. Precipitation averages 47 inches per year and provides an abundant supply of water. Twenty-one inches returns to the atmosphere as evapotranspiration; the remainder flows directly to streams or percolates to the water table and discharges to Long Island Sound. Small amounts of water are exported from the basin by the New Britain Water Department, and small amounts are imported to the basin by the New Haven Water Company.</p>\n<br/>\n<p>The amount of water that can be developed at a given place depends upon precipitation, variability of streamflow, hydraulic properties and areal extent of the aquifers, and hydraulic connection between the aquifers and major streams. The quality of the water is determined by the physical environment and the effects of man.</p>\n<br/>\n<p>Stratified drift is the only aquifer capable of large sustained yields of water to individual wells. Yields of 64 screened wells tapping stratified drift range from 17 to 2,000 gpm (gallons per minute); their median yield is 500 gpm.</p>\n<br/>\n<p>Till is widespread and generally provides only small amounts of water. Wells in till normally yield only a few hundred gallons of water daily and commonly are inadequate during dry periods. Till is generally used only as an emergency or secondary source of water.</p>\n<br/>\n<p>Bedrock aquifers underlie the entire report area and include sedimentary, igneous, and metamorphic rock types. These aquifers supply small but reliable quantities of water to wells throughout the basin and are the chief source for many nonurban homes and farms. About 90 percent of the wells tapping bedrock yield at least 2 pgm, and much larger yields are occasionally reported. Maximum well yields of 305 gpm for sedimentary, 75 gpm for igneous, and 200 gpm for metamorphic bedrock have been reported.</p>\n<br/>\n<p>Water potentially available from stratified drift was estimated on the basis of hydraulic characteristics of the aquifers and evaluation of natural and induced recharge. Long-term yields estimated for 14 favorable areas of stratified drift range from 0.8 to 16.1 mgd (million gallons per day), but detailed verification studies are needed before development.</p>\n<br/>\n<p>The natural quality of water in the report area is good. The water is generally low in dissolved solid and is soft to moderately hard. Surface water is less mineralized than ground water, especially during high flow when it is primarily surface runoff. A median dissolved-solids concentration of 117 mg/l (milligrams per liter) and a median hardness of 58 mg/l was determined for water samples collected at 20 sites on 16 streams during high flow. A median dissolved-solids concentration of 146 mg/l and a median hardness of 82 mg/l was determined for samples collected at the same sites during low flow. In contrast water from 130 wells had a median dissolved-solids concentration of 188 mg/l and a median hardness of 110 mg/l.</p>\n<br/>\n<p>Iron and manganese occur in objectionable concentrations in parts of the report area, particularly in water from streams draining swamps and in water from aquifers rich in iron- and manganese-bearing minerals. Concentrations of iron in excess of 0.3 mg/l were found in 40 percent of the high-streamflow samples, 59 percent of the low-streamflow samples and 20 percent of the ground-water samples.</p>\n<br/>\n<p>Human activities have modified the quality of water in much of the basin. Wide and erratic fluctuations in concentration of dissolved solids in streams, high bacterial content of the Quinnipiac River, and locally high nitrate and chloride concentrations in ground water are evidence of man's influence. Streams, wetlands, and some aquifers along the southern boundary of the basin contain salty water. Overpumping has caused extensive saltwater intrusion in aquifers in the southern and eastern parts of New Haven.</p>\n<br/>\n<p>The total amount of fresh water used in the area during 1970 is estimated at 35,710 million gallons, or 183 gallons per day per capita. Public water-supply systems met the domestic requirements of about 90 percent of the population; all the systems supplied water that met the drinking water standards of the Connecticut Department of Health.</p>","language":"English","publisher":"Connecituct Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Mazzaferro, D.L., Handman, E.H., and Thomas, M.P., 1978, Water resources inventory of Connecticut Part 8: Quinnipiac River basin: Connecticut Water Resources Bulletin 27, Report: v, 86 p.; 5 Plates: 31.07 x 54.28 inches and smaller.","productDescription":"Report: v, 86 p.; 5 Plates: 31.07 x 54.28 inches and smaller","numberOfPages":"96","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258819,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0027/report.pdf","size":"33897","linkFileType":{"id":1,"text":"pdf"}},{"id":258820,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0027/report-thumb.jpg"},{"id":286041,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038340/plate-c.pdf"},{"id":286042,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038340/plate-d.pdf"},{"id":286043,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038340/plate-e.pdf"},{"id":286039,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038340/plate-a.pdf"},{"id":286040,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038340/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Quinnipiac River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.083333,41.183333 ], [ -73.083333,41.708333 ], [ -72.683333,41.708333 ], [ -72.683333,41.183333 ], [ -73.083333,41.183333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7ee4b08c986b32d69c","contributors":{"authors":[{"text":"Mazzaferro, David L.","contributorId":89539,"corporation":false,"usgs":true,"family":"Mazzaferro","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Handman, Elinor H.","contributorId":31748,"corporation":false,"usgs":true,"family":"Handman","given":"Elinor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":463906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5223484,"text":"5223484 - 1978 - Nomenclature of the black-bellied whistling-duck","interactions":[],"lastModifiedDate":"2017-05-16T09:37:34","indexId":"5223484","displayToPublicDate":"2010-06-16T12:19:30","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Nomenclature of the black-bellied whistling-duck","docAbstract":"<p><span>There are two distinguishable subspecies of the Black-bellied Whistling-Duck, one in South America to eastern Panama and one from western Panama through Central America to the southernmost United States. The type locality of the species is the West Indies, but there is little evidence that birds from that area are anything but vagrants or birds imported from South America. All records of this species in the West Indies are attributable to the subspecies that occurs naturally in South America. The plate and description on which the name of the species is based seem to be of the South American form. It thus becomes clear that the South American and West Indian populations of Black-bellied Whistling-Duck must bear the name <i>Dendrocygna</i> <i>autumnalis autumnalis</i> (Linnaeus) 1758 and that <i>Dendrocygna discolor</i> Sclater and Salvin 1873 is a junior synonym. The earliest available name for the birds north of Panama is <i>D. a. fulgens</i> Friedmann 1947, of which <i>D. a. lucida</i> Friedmann 1947 is a synonym.</span></p>","language":"English","publisher":"American Ornithological Society","usgsCitation":"Banks, R.C., 1978, Nomenclature of the black-bellied whistling-duck: The Auk, v. 95, no. 2, p. 348-352.","productDescription":"5 p.","startPage":"348","endPage":"352","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":341288,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4085452"}],"volume":"95","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6970ee","contributors":{"authors":[{"text":"Banks, Richard C.","contributorId":102933,"corporation":false,"usgs":true,"family":"Banks","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":338844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221425,"text":"5221425 - 1978 - Organochlorine residues and eggshell thinning in anhingas and waders","interactions":[],"lastModifiedDate":"2018-02-27T17:36:37","indexId":"5221425","displayToPublicDate":"2010-06-16T12:19:20","publicationYear":"1978","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Organochlorine residues and eggshell thinning in anhingas and waders","docAbstract":"<p> Residues of organochlorine compounds occur commonly in environmental samples and have been associated with adverse effects in numerous avian species (Cooke 1973; L. F. Stickel 1973; W. H. Stickel 1975; Ohlendorf et al. 1977; H. M. Ohlendorf, R. W. Risebrough, and K. Vermeer, unpublished manuscript). The affected species are usually terminal consumers, generally those feeding on aquatic organisms (primarily fish) or birds. </p><p> Brown Pelicans (<i>Pelecanus occidentalis</i>), Double-crested Cormorants <i>(Phalacrocorax auritus)</i>, and certain herons are among the species that have exhibited shell thinning in some regions (see Ohlendorf et al. 1977 for review). In 1972, we began a study to determine: (1) geographic differences in the occurrence of environmental pollutants in Anhingas (<i>Anhinga anhinga</i>) and waders in the eastern United States; (2) differences in environmental pollutant levels among those species nesting at the same localities; and (3) whether eggshell thickness had changed since the widespread use of organochlorine pesticides began in the mid-1940's.</p><p> The wader species included in our study were: Great Blue Heron (<i>Ardea herodias</i>), Green Heron (<i>Butorides virescens</i>), Little Blue Heron (<i>Florida caerulea</i>), Cattle Egret (<i>Bubulcus ibis</i>), Reddish Egret (<i>Dichromanassa rufescens</i>), Great Egret (<i>Casmerodius albus</i>), Snowy Egret (<i>Egretta thula</i>), Louisiana Heron (<i>Hydranassa tricolor</i>), Black-crowned Night Heron (<i>Nycticorax nycticorax</i>), Yellow-crowned Night Heron (<i>Nyctanassa violacea</i>), Least Bittern (<i>Ixobrychus exilis</i>), American Bittern (<i>Botaurus lentiginosus</i>), Wood Stork (<i>Mycteria americana</i>), Glossy Ibis (<i>Plegadis falcinellus</i>), White Ibis (<i>Eudocimus</i> <i>albus</i>), and Roseate Spoonbill (<i>Ajaia</i> <i>ajaja</i>). </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 1977 conference of the colonial waterbird group","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"1977 conference of the colonial waterbird group","conferenceDate":"October 20-23, 1977","conferenceLocation":"DeKalb, IL","language":"English","publisher":"Waterbird Society","doi":"10.2307/1520919","usgsCitation":"Ohlendorf, H.M., Klaas, E.E., and Kaiser, T.E., 1978, Organochlorine residues and eggshell thinning in anhingas and waders, <i>in</i> Proceedings of the 1977 conference of the colonial waterbird group, v. 1, DeKalb, IL, October 20-23, 1977, p. 185-195, https://doi.org/10.2307/1520919.","productDescription":"11 p.","startPage":"185","endPage":"195","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d6f8","contributors":{"compilers":[{"text":"Southern, William E.","contributorId":68919,"corporation":false,"usgs":false,"family":"Southern","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":729782,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":"Ohlendorf, Harry M.","contributorId":60291,"corporation":false,"usgs":true,"family":"Ohlendorf","given":"Harry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":333815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klaas, Erwin E.","contributorId":101219,"corporation":false,"usgs":true,"family":"Klaas","given":"Erwin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":333814,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaiser, T. Earl","contributorId":84826,"corporation":false,"usgs":true,"family":"Kaiser","given":"T.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":333816,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162731,"text":"70162731 - 1978 - lowaphyllum (rugose coral) from the Upper Devonian of Arizona","interactions":[],"lastModifiedDate":"2022-06-15T14:32:31.792124","indexId":"70162731","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"displayTitle":"<i>lowaphyllum</i> (rugose coral) from the Upper Devonian of Arizona","title":"lowaphyllum (rugose coral) from the Upper Devonian of Arizona","docAbstract":"<p>The rugose coral genus <i>lowaphyllum</i> is uncommon but widely distributed in rocks of Devonian age. It is here reported for the first time from western North America (Late Devonian). <i>lowaphyllum</i> is also known from the late Middle and Late Devonian of Eastern North America, but the lack of Early and early Middle Devonian species anywhere in North America leaves open the question of derivation of these forms and their relationship to Early Devonian species in Europe and Australia.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Oliver, W.A., 1978, lowaphyllum (rugose coral) from the Upper Devonian of Arizona: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 797-805.","productDescription":"9 p.","startPage":"797","endPage":"805","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315076,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315075,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Arizona","otherGeospatial":"Haunted Canyon, J. K. Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.9451904296875,\n              32.45415593941475\n            ],\n            [\n              -111.9451904296875,\n              35.178298352001185\n            ],\n            [\n              -109.1876220703125,\n              35.178298352001185\n            ],\n            [\n              -109.1876220703125,\n              32.45415593941475\n            ],\n            [\n              -111.9451904296875,\n              32.45415593941475\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b40e4b0403299f53988","contributors":{"authors":[{"text":"Oliver, William Albert Jr.","contributorId":44521,"corporation":false,"usgs":true,"family":"Oliver","given":"William","suffix":"Jr.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":590312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162722,"text":"70162722 - 1978 - A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>","interactions":[],"lastModifiedDate":"2016-01-29T12:13:35","indexId":"70162722","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>","docAbstract":"<p>The original interpretation of <i>Olivellites plummeri</i> Fenton and Fenton as the trace of an infaunal gastropod, is reconsidered and rejected. The original slab bearing several examples of <i>O. plummeri</i> has been reexamined and reillustrated. The slab came from the type-locality of <i>O. plummeri</i>&nbsp;in Eastland County, Tex., and is a shallow sub tidal sandstone of the Graham Formation; the sandstone, which has yielded additional specimens, is presumably a reworked delta-front deposit. <i>Olivellites</i> was also observed in the Caddo Creek Formation in Stephens County, Tex., but, to date, it has not been found elsewhere in north-central Texas. Interpretation of Paleozoic ichnofossils by analogy with modern traces is limited; behavioral characteristics may be the products of post-Paleozoic innovation. The internal morphology and path of <i>Olivellites</i> are unlike those of any modern gastropod trail, and the genus is removed from the Mollusca.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Yochelson, E.L., and Schindel, D.E., 1978, A reexamination of the Pennsylvanian trace fossil <i>Olivellites</i>: Journal of Research of the U.S. Geological Survey, v. 6, no. 6, p. 789-796.","productDescription":"8 p.","startPage":"789","endPage":"796","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":315071,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue6/report.pdf","text":"Report","size":"26.93 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","county":"Eastland County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.96312713623045,\n              32.32485582675006\n            ],\n            [\n              -98.96312713623045,\n              32.43822086674334\n            ],\n            [\n              -98.8275146484375,\n              32.43822086674334\n            ],\n            [\n              -98.8275146484375,\n              32.32485582675006\n            ],\n            [\n              -98.96312713623045,\n              32.32485582675006\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ac9b44e4b0403299f539b8","contributors":{"authors":[{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":590300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schindel, David E.","contributorId":152692,"corporation":false,"usgs":false,"family":"Schindel","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":590301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012557,"text":"70012557 - 1978 - Tectonics of the North American Cordillera near the Fortieth Parallel","interactions":[],"lastModifiedDate":"2025-09-02T16:03:22.978977","indexId":"70012557","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Tectonics of the North American Cordillera near the Fortieth Parallel","docAbstract":"<p>The North American Cordillera near the Fortieth Parallel consists of the following tectonic units: </p><p>1. (A) To the east is a reactivated cratonic area, in the Southern Rocky Mountains and Colorado Plateau, in which the supracrustal rocks (Cambrian to Cretaceous) were broadly deformed during the late Cretaceous-Paleocene Laramide orogeny, and the Precambrian basement was raised in folds of wide amplitude. </p><p>2. (B) West of it is a miogeosynclinal belt, in the eastern Great Basin, in which a thick sequence of Paleozoic carbonates and related deposits was thrust eastward along low-angle faults during the middle to late Cretaceous Sevier orogeny. The miogeosyncline is the downwarped western margin of the original North American continent, and its rocks accumulated on Precambrian basement. </p><p>3. (C) Beyond is a eugeosynclinal belt, in the western Great Basin, in which Paleozoic graywackes, cherts, and volcanics were thrust easteastward along low-angle faults during several Paleozoic orogenies - the mid-Paleozoic Antler orogeny which produced the Roberts thrust on the east, and the end-Paleozoic Sonoma orogeny which produced the Golconda thrust farther west. The Paleozoic eugeosynclinal rocks accumulated on oceanic basement. They are overlapped from the west by Triassic and Jurassic shelf deposits, which pass westward into eugeosynclinal deposits. </p><p>4. (D) A volcanic island-arc belt existed on the sites of the Sierra Nevada in Paleozoic and early Mesozoic time, which produced thick bodies of sediments and volcanics. During the mid-Mesozoic Nevadan orogeny these were steeply deformed and thrust westward over subduction zones, and were intruded by granitic rocks that rose from the upper mantle to form great batholiths. </p><p>5. (E) West of the Sierra Nevada, in the Great Valley, is a great sedimentary embankment of later Mesozoic flysch or turbidite, largely younger than the supracrustal rocks of the Sierra Nevada and the Nevadan orogeny. It was formed of the erosional products of the supracrustal and granitic rocks of the Sierra Nevada. </p><p>6. (F) This sequence is, in turn, thrust westward over the Mesozoic Franciscan terrane of the Coast Ranges, which forms the westernmost belt of the Cordillera, and which is being treated in other papers in this symposium. </p><p>The net effect of the prolonged events that produced the Cordillera in this segment has been the addition of successive tectonic belts to the North American continent at the expense of the Pacific Ocean basin during Phanerozoic time.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(78)90034-3","issn":"00401951","usgsCitation":"King, P., 1978, Tectonics of the North American Cordillera near the Fortieth Parallel: Tectonophysics, v. 47, no. 3-4, p. 275-294, https://doi.org/10.1016/0040-1951(78)90034-3.","productDescription":"20 p.","startPage":"275","endPage":"294","costCenters":[],"links":[{"id":222210,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.57945713391274,\n              42.87578330166886\n            ],\n            [\n              -125.57945713391274,\n              35.03289778190745\n            ],\n            [\n              -102.07836332194293,\n              35.03289778190745\n            ],\n            [\n              -102.07836332194293,\n              42.87578330166886\n            ],\n            [\n              -125.57945713391274,\n              42.87578330166886\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba48de4b08c986b32041a","contributors":{"authors":[{"text":"King, Philip B.","contributorId":34580,"corporation":false,"usgs":true,"family":"King","given":"Philip B.","affiliations":[],"preferred":false,"id":363900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221448,"text":"5221448 - 1978 - Effects of No. 2 fuel oil on common eider eggs","interactions":[],"lastModifiedDate":"2025-05-12T16:33:39.262902","indexId":"5221448","displayToPublicDate":"2003-04-07T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2676,"text":"Marine Pollution Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Effects of No. 2 fuel oil on common eider eggs","docAbstract":"An oil spill near a breeding colony could result in the transfer of oil from the plumage and feet of incubating birds to their eggs. Microlitre amounts of No. 2 fuel oil were applied externally to common eider eggs in an island breeding colony in Maine. Clutches of eggs treated with 20 ?l of fuel oil had significantly greater embryonic mortality than the control clutches when they were examined 7 days after treatment. The results are similar to those of an earlier study of artificially incubated common eider eggs and indicate that nest site conditions do not affect embryotoxicity of No. 2 fuel oil.","language":"English","publisher":"Elsevier","doi":"10.1016/0025-326X(78)90590-8","usgsCitation":"Albers, P., and Szaro, R.C., 1978, Effects of No. 2 fuel oil on common eider eggs: Marine Pollution Bulletin, v. 9, no. 5, p. 138-139, https://doi.org/10.1016/0025-326X(78)90590-8.","productDescription":"2 p.","startPage":"138","endPage":"139","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","otherGeospatial":"Bangs Island, East Casco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.18236357335988,\n              43.759784030767946\n            ],\n            [\n              -70.18236357335988,\n              43.6761981129479\n            ],\n            [\n              -70.0670930378678,\n              43.6761981129479\n            ],\n            [\n              -70.0670930378678,\n              43.759784030767946\n            ],\n            [\n              -70.18236357335988,\n              43.759784030767946\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"9","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624fc6","contributors":{"authors":[{"text":"Albers, P.H.","contributorId":26646,"corporation":false,"usgs":true,"family":"Albers","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":333871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szaro, Robert C.","contributorId":21240,"corporation":false,"usgs":false,"family":"Szaro","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":333870,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46112,"text":"ofr78110 - 1978 - Map showing depth to water table, September 1976, and area inundated by the June 1975 flood, Helena Valley, Lewis and Clark County, Montana","interactions":[],"lastModifiedDate":"2021-08-25T20:19:02.503085","indexId":"ofr78110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-110","title":"Map showing depth to water table, September 1976, and area inundated by the June 1975 flood, Helena Valley, Lewis and Clark County, Montana","docAbstract":"Depth to water table, September 1976, and area inundated by the June 1975 flood in the Helena valley, Montana, are mapped on two sheets, Helena and East Helena 7.5-minute quadrangles, at scale 1:48,000. Depth to water table was mapped using water-level measurements from existing shallow observation wells and selected domestic wells, and from field reconnaissance of topography. A hydrograph shows water-level fluctuation in two wells located in different parts of the valley. Area inundated by the June 1975 flood was mapped from aerial photos along Prickly Pear and Tenmile Creeks and by field reconnaissance along Silver Creek. (Woodard-USGS)","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr78110","usgsCitation":"Wilke, K.R., and Johnson, M.V., 1978, Map showing depth to water table, September 1976, and area inundated by the June 1975 flood, Helena Valley, Lewis and Clark County, Montana: U.S. Geological Survey Open-File Report 78-110, 2 Plates: 18.00 × 28.50 inches and 17.50 × 28.50 inches, https://doi.org/10.3133/ofr78110.","productDescription":"2 Plates: 18.00 × 28.50 inches and 17.50 × 28.50 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":83063,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0110/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83062,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0110/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":388508,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14599.htm"}],"country":"United States","state":"Montana","county":"Lewis and Clark County","otherGeospatial":"Helena Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,46.5 ], [ -112.25,46.75 ], [ -111.75,46.75 ], [ -111.75,46.5 ], [ -112.25,46.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d6bc","contributors":{"authors":[{"text":"Wilke, Kathleen R.","contributorId":17589,"corporation":false,"usgs":true,"family":"Wilke","given":"Kathleen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":232635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, M. V.","contributorId":95476,"corporation":false,"usgs":true,"family":"Johnson","given":"M.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":232636,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46083,"text":"ofr78937 - 1978 - Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978","interactions":[],"lastModifiedDate":"2022-01-03T22:22:13.733594","indexId":"ofr78937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-937","title":"Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978","docAbstract":"The U.S. Geological Survey has released to the open file a map showing ground-water subunits and areas, and depth to water for spring 1978, in the Antelope Valley-East Kern Water Agency area, California.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78937","usgsCitation":"Blankenbaker, G.G., 1978, Antelope Valley - East Kern Water Agency area, California, showing ground-water subunits and areas, location of wells, and lines of equal depth to water for spring 1978: U.S. Geological Survey Open-File Report 78-937, 1 Plate: 43.00 × 41.00 inches, https://doi.org/10.3133/ofr78937.","productDescription":"1 Plate: 43.00 × 41.00 inches","costCenters":[],"links":[{"id":162625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393811,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14962.htm"},{"id":99640,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0937/plate-1.pdf","size":"8956","linkFileType":{"id":1,"text":"pdf"}}],"scale":"124000","country":"United States","state":"California","otherGeospatial":"Antelope Valley - East Kern Water Agency area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75,\n              34.4260\n            ],\n            [\n              -117.655,\n              34.4260\n            ],\n            [\n              -117.655,\n              35.3610\n            ],\n            [\n              -118.75,\n              35.3610\n            ],\n            [\n              -118.75,\n              34.4260\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b45f","contributors":{"authors":[{"text":"Blankenbaker, G. G.","contributorId":17993,"corporation":false,"usgs":true,"family":"Blankenbaker","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":232589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56278,"text":"wdrWA772 - 1978 - Water resources data for Washington, water year 1977, Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-23T18:25:59.659692","indexId":"wdrWA772","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"WA-77-2","title":"Water resources data for Washington, water year 1977, Vol. 2 - Eastern Washington","docAbstract":"<p>Water resources data for the 1977 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water-quality of ground water. This report, in two volumes, contains discharge records for 258 gaging stations; stage only records for 4 gaging stations; stage and contents for 44 lakes and reservoirs; water quality for 162 gaging stations, 7 lakes, 50 wells and 71 miscellaneous sites; and water levels for 173 observation wells. Also included are 146 crest-stage partial-record stations and 19 low-flow partial-record stations. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA772","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Washington, water year 1977, Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-77-2, xi, 419 p., https://doi.org/10.3133/wdrWA772.","productDescription":"xi, 419 p.","costCenters":[],"links":[{"id":174643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1977/wa-77-2/report-thumb.jpg"},{"id":410998,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/wa-77-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f176f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532469,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61080,"text":"mf880F - 1978 - Geochemical maps showing the distribution and abundance of gold in stream sediments and of gold and silver in heavy-mineral concentrates in the Seward and Blying Sound quadrangles, Alaska","interactions":[],"lastModifiedDate":"2025-04-23T13:28:42.448896","indexId":"mf880F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"880","chapter":"F","title":"Geochemical maps showing the distribution and abundance of gold in stream sediments and of gold and silver in heavy-mineral concentrates in the Seward and Blying Sound quadrangles, Alaska","docAbstract":"<p><span>Reconnaissance geochemical and mineralogical sampling was done in the Seward and Blying Sound quadrangles during 1975 and 1976 as part of the Alaska Mineral Resources Assessment Program (AMRAP). These maps show the distribution and abundance of gold and silver in heavy-mineral concentrates.&nbsp;</span></p><p><span>Stream-sediment and heavy-mineral concentrate samples were collected from active stream channels and locally, from the interface of streambeds with intermediate- to low-tide beaches. Most of the stream sediment is fine- to coarse-grained sand, with a clay-silt fraction in streams discharging from glaciers. Stream sediment samples were air dried and sieved through a 80-mesh (0.2 mm) sieve, and the minus-80 mesh fraction was saved for analysis. A split of each sample was analyzed for gold by a 10 gram atomic-absorption method (Ward and others, 1969). Another split was analyzed for 16 elements by a semiquantitative spectrographic method (Grimes and Marranzino, 1968).</span></p><p><span>The heavy-mineral concentrates were obtained by panning stream sediments in the field to remove most of the light minerals. The panned samples were sieved though a 20-mesh (0.8 mm) screen in the laboratory, and the minus-20 mesh fraction was further separated with bromoform (specific gravity: 2.86) to remove any remaining light-mineral grains. Magnetite and other strongly magnetic heavy minerals were removed from the heavy-mineral fraction by use of a hand magnet. The remaining sample was passed through a Frantz Isodynamic Separator<sup>1</sup> and a nonmagnetic fraction was obtained at a setting of 0.6 amperes. A split of this fraction was pulverized and analyzed for 16 elements including gold and silver by semiquantitative spectrographic method used for analyzing the stream sediment. The remaining split of the nonmagnetic fraction was examined for its mineralogic composition using a binocular microscope and X-ray diffraction. The nonmagnetic concentrates primarily contain muscovite, sphene, zircon, apatite, rutile, and anatase. Ore minerals such as gold, scheelite, minium, and most sulfides are also found in this fraction.</span></p><p><span>Sample sites and gold and silver values (in parts per million) are indicated by symbols as defined in the histograms. The maps show two populations for gold in stream sediments and for gold and silver heavy mineral concentrates. One population consists of generally higher gold and silver values found in samples collected in the sedimentary terrane in the western half of the area. The other population consists of generally lower gold and silver values found in samples collected in areas of sheeted basalt dikes, pillow basalts, and sedimentary terrane in the eastern half of the area. The anomalous silver values found on Knight Island and Latouche Island are associated with chalcopyright- and pyrite-bearing rocks.&nbsp;</span></p><p><span><sup>1&nbsp;</sup>The use of trade names is for descriptive purposes only and does not constitute endorsement of those products by the U.S. Geological Survey.&nbsp;<br data-mce-bogus=\"1\"></span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf880F","isbn":"0607803509","usgsCitation":"Tripp, R.B., Crim, W., and O’Leary, R.M., 1978, Geochemical maps showing the distribution and abundance of gold in stream sediments and of gold and silver in heavy-mineral concentrates in the Seward and Blying Sound quadrangles, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 880, 2 Plates: 44.15 x 33.92 inches and 57.52 x 40.93 inches, https://doi.org/10.3133/mf880F.","productDescription":"2 Plates: 44.15 x 33.92 inches and 57.52 x 40.93 inches","costCenters":[],"links":[{"id":417372,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0880-F/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":417371,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0880-F/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":388926,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4103.htm"},{"id":180375,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0880-F/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Blying Sound quadrangle, Seward quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,59.5 ], [ -150,61 ], [ -147,61 ], [ -147,59.5 ], [ -150,59.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf37","contributors":{"authors":[{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":264949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crim, W.D.","contributorId":8820,"corporation":false,"usgs":true,"family":"Crim","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":264947,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68705,"text":"oc86 - 1978 - Preliminary stratigraphic cross section showing radioactive zones in the Devonian dark shales in the eastern part of the Appalachian Basin","interactions":[{"subject":{"id":42754,"text":"ofr77842 - 1977 - Preliminary stratigraphic cross section of the Devonian in the eastern part of the Appalachian Basin showing radioactive shale zones","indexId":"ofr77842","publicationYear":"1977","noYear":false,"title":"Preliminary stratigraphic cross section of the Devonian in the eastern part of the Appalachian Basin showing radioactive shale zones"},"predicate":"SUPERSEDED_BY","object":{"id":68705,"text":"oc86 - 1978 - Preliminary stratigraphic cross section showing radioactive zones in the Devonian dark shales in the eastern part of the Appalachian Basin","indexId":"oc86","publicationYear":"1978","noYear":false,"title":"Preliminary stratigraphic cross section showing radioactive zones in the Devonian dark shales in the eastern part of the Appalachian Basin"},"id":1}],"lastModifiedDate":"2017-09-20T10:02:30","indexId":"oc86","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86","title":"Preliminary stratigraphic cross section showing radioactive zones in the Devonian dark shales in the eastern part of the Appalachian Basin","docAbstract":"<p>The&nbsp;U.S. Geological Survey (USGS), in a cooperative agreement with the U.S. Department of Energy (DOE), is participating in the Eastern Gas Shales Project. The purpose of the DOE project is to increase the production of natural gas from eastern United States shales in petroliferous basins through improved exploration and extraction techniques. The USGS participation includes stratigraphic studies which will contribute to the characterization and appraisal of the natural gas resources of Devonian shale in the Appalachian basin.<br></p><p>This cross section differs from others in this series partly because many of the shales in the eastern part of the basin are less radioactive than those farther west and because in this area shales that may be gas-productive are not necessarily highly radioactive and black.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/oc86","isbn":"0607823887","collaboration":"Prepared in cooperation with the Department of Energy Interagency Agreement # EX-76-C-01-2287","usgsCitation":"West, M.N., 1978, Preliminary stratigraphic cross section showing radioactive zones in the Devonian dark shales in the eastern part of the Appalachian Basin: U.S. Geological Survey Oil and Gas Investigation Chart 86, 2 Sheets: 45.22 x 40.89 inches, https://doi.org/10.3133/oc86.","productDescription":"2 Sheets: 45.22 x 40.89 inches","costCenters":[],"links":[{"id":186454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104868,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5238.htm","linkFileType":{"id":5,"text":"html"},"description":"5238"}],"scale":"2534400","country":"United States","state":"Delaware, Maryland, New Jersey, New York, Pennsylvania, Virginia, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.5,\n              38\n            ],\n            [\n              -75,\n              38\n            ],\n            [\n              -75,\n              43\n            ],\n            [\n              -80.5,\n              43\n            ],\n            [\n              -80.5,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a733","contributors":{"authors":[{"text":"West, Mareta N.","contributorId":12097,"corporation":false,"usgs":true,"family":"West","given":"Mareta","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":278790,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66275,"text":"i1087 - 1978 - Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado","interactions":[],"lastModifiedDate":"2017-02-16T11:09:56","indexId":"i1087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1087","title":"Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado","docAbstract":"<p>The White River is the largest stream in the southeastern part of the Uinta Basin in Utah and Colorado. This map shows the changes that have occurred in the location of the main channel of the river from 1936 to 1974. The map indicated that certain reaches of the river are subject to different rates of channel migration. Also shown is the boundary of the flood plain, which is mapped at the point of abrupt break in slope. This map documents the position of the river channel prior to any withdrawals of water or alteration of the flow characteristics of the white river that may occur in order to meet water requirements principally associated with the proposed oil-shale industry or other development in the area.</p><p>The channel locations were determined from aerial photographs taken at four different time periods for the following Federal agencies: In 1936, U.S. Soil Conservation Services; 1953, U.S. Corps of Engineers; 1965, U.S. Geological Survey; and in 1974, U.S. Bureau of Land Management. The 1936 delineation, which is actually based upon photographs that were taken in 1936 and 1937, was made by projection of the original photographs on a base map that was prepared from 1:24,000 scale topographic maps. The 1953, 1965, and 1974 delineations were produced from stereographic models. The 1965 delineation was compiled from photographs that were taken during 1962-65. The delineation is labeled as 1965 for simplicity, however, because the photographs for 1965 cover about 60 percent of the study read of the river, and because no changed were discernable in those areas of repetitive photographic coverage.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1087","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Jurado, A., and Fields, F.K., 1978, Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado: U.S. Geological Survey IMAP 1087, 1 Map: 33.95 x 39.64 Inches; Cover: 9.20 x 11.87 inches, https://doi.org/10.3133/i1087.","productDescription":"1 Map: 33.95 x 39.64 Inches; Cover: 9.20 x 11.87 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":255735,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1087/plate-1.pdf","text":"Map I-1087","size":"8.57 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255736,"rank":300,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/1087/report.pdf","text":"Folio Cover","size":"29.2 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1087/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin, White River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.70083333333334,39.916666666666664 ], [ -109.70083333333334,40.1175 ], [ -109,40.1175 ], [ -109,39.916666666666664 ], [ -109.70083333333334,39.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6296","contributors":{"authors":[{"text":"Jurado, Antonio","contributorId":73264,"corporation":false,"usgs":true,"family":"Jurado","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":274283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":274284,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58370,"text":"mf880E - 1978 - Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska","interactions":[],"lastModifiedDate":"2023-05-23T20:58:22.987417","indexId":"mf880E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"880","chapter":"E","title":"Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska","docAbstract":"<p>Reconnaissance geochemical and mineralogical sampling was done in the Seward and Blying Sound quadrangles during 1975 and 1976 as part of the Alaska Mineral Resources Assessment Program (AMRAP). This map shows the distribution and abundance of copper in stream-sediment samples.&nbsp;</p><p>Stream-sediment samples were collected at 569 sites from active stream channels and locally, from the interface of streambeds with intermediate- to low-tide beaches. Most of the stream sediment is fine- to coarse-grained sand, with a clay-silt fraction in streams discharging from glaciers.&nbsp;</p><p>The stream sediment samples were air dried and sieved through a 80-mesh (0.2 mm) sieve, and the minus-80 mesh fraction was saved for analysis. A split of each sample was analyzed for copper and 15 other elements by a semiquantitative spectrographic method (Grimes and Marranzino, 1968). Other splits were analyzed for gold and zinc by atomic absorption methods (Warren and others, 1969).</p><p>Sample sites and copper values (in parts per million) are indicated on the map by symbols identified in the histogram. The weakly anomalous values are considered to be significant only where they were detected in stream-sediment or heavy-mineral concentrate samples that also contained strongly anomalous values of other metals such as arsenic, gold, lead or tungsten.</p><p>The map shows two populations for copper in stream sediments. One population consisting of generally lower copper values represents the samples collected from the sedimentary terrane in the central and western parts of the quadrangles. The other population consisting of generally higher copper values includes samples collected in areas of sheeted basalt dikes and pillow basalts in the eastern part of the quadrangles and from the sedimentary terrane of Latouche Island; in these areas chalcopyrite and pyrite were observed as fine-grained disseminations in the rocks and as mineral particles in the heavy-mineral concentrates.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf880E","isbn":"0607803495","usgsCitation":"Tripp, R.B., Crim, W., Cooley, E., and Day, G., 1978, Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 880, 1 Plate: 40.54 x 34.52 inches, https://doi.org/10.3133/mf880E.","productDescription":"1 Plate: 40.54 x 34.52 inches","costCenters":[],"links":[{"id":417367,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0880-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182959,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0880-E/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Blying Sound Quadrangle, Seward Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,59.5 ], [ -150,61 ], [ -147,61 ], [ -147,59.5 ], [ -150,59.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0d8","contributors":{"authors":[{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":258919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crim, W.D.","contributorId":8820,"corporation":false,"usgs":true,"family":"Crim","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":258916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":258918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":258917,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":64952,"text":"i855G - 1978 - Geologic map of the Boulder-Fort Collins-Greeley area, Colorado","interactions":[],"lastModifiedDate":"2022-11-01T21:30:13.157106","indexId":"i855G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"855","chapter":"G","title":"Geologic map of the Boulder-Fort Collins-Greeley area, Colorado","docAbstract":"This digital map shows the geographic extent of rock stratigraphic units (formations) as compiled by Colton in 1976 under the Front Range Urban Corridor Geology Program.  Colton used his own geologic mapping and previously published geologic maps to compile one map having a single classification of geologic units.  The resulting published color paper map (USGS Map I-855-G, Colton, 1978) was intended for land-use planning and to depict the regional geology.  In 1997-1999, another USGS project designed to address urban growth issues was undertaken. This project, the USGS Front Range Infrastructure Resources Project, undertook to digitize Colton's map at 1:100,000 scale, making it useable in Geographical Information Systems (GIS). That product is described here.\r\n      In general, the digitized map depicts in its western part Precambrian igneous and metamorphic rocks, Pennsylvanian and younger sedimentary rock units, major faults, and brecciated zones along an eastern strip (5-20 km wide) of the Front Range.  The central and eastern parts of the map (Colorado Piedmont) show a mantle of Quaternary unconsolidated deposits and interspersed outcrops of sedimentary rock of Cretaceous or Tertiary age. A surficial mantle of unconsolidated deposits of Quaternary age is differentiated and depicted as eolium (wind-blown sand and silt), alluvium (river gravel, sand, and silt of variable composition), colluvium, and a few landslide deposits.  At the mountain front, north-trending, Paleozoic and Mesozoic formations of sandstone, shale, and minor limestone dip mostly eastward and form folds, fault blocks, hogbacks and intervening valleys.  Local dikes and sills of Tertiary rhyodacite and basalt intrude rocks near the range front, mostly in the Boulder area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i855G","usgsCitation":"Colton, R.B., 1978, Geologic map of the Boulder-Fort Collins-Greeley area, Colorado (Version 1.1): U.S. Geological Survey IMAP 855, 1 Plate: 40.69 × 31.15 inches; Dataset; Metadata, https://doi.org/10.3133/i855G.","productDescription":"1 Plate: 40.69 × 31.15 inches; Dataset; Metadata","costCenters":[],"links":[{"id":107012,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9734.htm","linkFileType":{"id":5,"text":"html"},"description":"9734"},{"id":190278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6091,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/855/G/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.375,\n              40.625\n            ],\n            [\n              -105.375,\n              40\n            ],\n            [\n              -104.625,\n              40\n            ],\n            [\n              -104.625,\n              40.625\n            ],\n            [\n              -105.375,\n              40.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d474","contributors":{"authors":[{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":272415,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7355,"text":"ofr78706 - 1978 - Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","interactions":[],"lastModifiedDate":"2026-02-19T18:42:07.880284","indexId":"ofr78706","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"78-706","title":"Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","docAbstract":"<p>During the L1-78-SC cruise of the USGS research vessel S. P. Lee (April 25 - May 11, 1978) seven sonobuoy profiles and 200 km of 24-channel seismic reflection data were recorded in the outer southern California Continental Borderland. These data were obtained, at the request of the Deep Sea Drilling Project (DSDP), to evaluate possible drill sites along the southern California continental margin.&nbsp;</p><p>The drill sites shown in Figure 1 were proposed by the Ocean Paleo-environmental Panel for DSDP Leg 63--secheduled for Sept. - Nov. 1978. These sites were selected in order to provide an expanded Neogene record of paleoceanographic-paleoclimatic events and associated evolutionary development of planktic communities along the eastern side of the north Pacific Ocean. Site selection was made prior to this survey on the basis of available single-channel seismic reflection profiles. Thus, the proposed sites shown on Fig. 1 may be relocated or eliminated when the data presented in this report are incorporated with earlier data. The combined data will be evaluated for safety and pollution hazards by Leg 63 site proponents and the DSDP safety panels.&nbsp;</p><p>The ship's tracks (Fig. 1) were located by an integrated Satellite-Loran C-Doppler Sonar navigation system. Average survey speed was about 5 kts. A 1326 cu in (21,723 CC) tuned air gun array provided the sound source for both reflection and refraction profiles. The air gun array was fired at 50 m (about 18 sec.) intervals by the integrated navigation system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78706","usgsCitation":"Crouch, J.K., Holmes, M., McCulloh, T.H., Long, A.T., and Brune, R., 1978, Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland: U.S. Geological Survey Open-File Report 78-706, 3 p., 10 sheets :ill., map ;29 cm., https://doi.org/10.3133/ofr78706.","productDescription":"25 p.","costCenters":[],"links":[{"id":500217,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0706/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141393,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0706/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"California 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