{"pageNumber":"6546","pageRowStart":"163625","pageSize":"25","recordCount":184904,"records":[{"id":5230045,"text":"5230045 - 1967 - Factors influencing waterfowl counts on aerial surveys, 1961-66","interactions":[],"lastModifiedDate":"2012-02-02T00:15:27","indexId":"5230045","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","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":"105","title":"Factors influencing waterfowl counts on aerial surveys, 1961-66","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Martinson, R.K., and Kaczynski, C., 1967, Factors influencing waterfowl counts on aerial surveys, 1961-66: Special Scientific Report  - Wildlife 105, 78.","productDescription":"78","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94680,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785056?urlappend=%3Bseq=3"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d4d","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":343421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaczynski, C.F.","contributorId":76804,"corporation":false,"usgs":true,"family":"Kaczynski","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":343420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5230033,"text":"5230033 - 1967 - The green-winged teal: Its distribution, migration, and population dynamics","interactions":[],"lastModifiedDate":"2012-02-02T00:15:24","indexId":"5230033","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","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":"100","title":"The green-winged teal: Its distribution, migration, and population dynamics","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Moisan, G., Smith, R., and Martinson, R.K., 1967, The green-winged teal: Its distribution, migration, and population dynamics: Special Scientific Report  - Wildlife 100, 248.","productDescription":"248","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":94678,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785031?urlappend=%3Bseq=111"},{"id":202798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d542","contributors":{"authors":[{"text":"Moisan, G.","contributorId":64772,"corporation":false,"usgs":true,"family":"Moisan","given":"G.","email":"","affiliations":[],"preferred":false,"id":343397,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R.I.","contributorId":63116,"corporation":false,"usgs":true,"family":"Smith","given":"R.I.","email":"","affiliations":[],"preferred":false,"id":343396,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":343398,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5230046,"text":"5230046 - 1967 - Retention of extra-wide, lock-on, and regular bands on waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:27","indexId":"5230046","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","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":"108","title":"Retention of extra-wide, lock-on, and regular bands on waterfowl","docAbstract":"In tests of three types of bands -- extra-wide bands, lock-on bands, and regular U.S. Fish and Wildlife Service bands -- little difference was noted in the retention qualities of the three types on waterfowl.  Therefore, there appeared to be no advantage in using either the extra-wide or the lock-on type of band rather than the regular band now in use by waterfowl banders on this continent.  Waterfowl banded with two bands provided recovery data that were difficult to analyze but suggested that it might be worthwhile to identify banded birds with another type of mark and evaluate the retention of bands through subsequent recapture of the birds.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Martinson, R.K., and Henny, C.J., 1967, Retention of extra-wide, lock-on, and regular bands on waterfowl: Special Scientific Report  - Wildlife 108, iv, 19.","productDescription":"iv, 19","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94681,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785114?urlappend=%3Bseq=5"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60450b","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":343423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":343422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5230140,"text":"5230140 - 1967 - Test of grit types in alleviating lead poisoning in mallards","interactions":[],"lastModifiedDate":"2012-02-02T00:15:28","indexId":"5230140","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","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":"107","title":"Test of grit types in alleviating lead poisoning in mallards","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Godin, A., 1967, Test of grit types in alleviating lead poisoning in mallards: Special Scientific Report  - Wildlife 107, ii, 9.","productDescription":"ii, 9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112109,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486777?urlappend=%3Bseq=647"},{"id":202562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684b89","contributors":{"authors":[{"text":"Godin, A.J.","contributorId":48680,"corporation":false,"usgs":true,"family":"Godin","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":343590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5230082,"text":"5230082 - 1967 - Woodcock research and management, 1966","interactions":[],"lastModifiedDate":"2012-02-02T00:15:25","indexId":"5230082","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","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":"101","title":"Woodcock research and management, 1966","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Goudy, W., 1967, Woodcock research and management, 1966: Special Scientific Report  - Wildlife 101, 40.","productDescription":"40","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94683,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785031?urlappend=%3Bseq=383"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df868","contributors":{"authors":[{"text":"Goudy, W.H.","contributorId":43895,"corporation":false,"usgs":true,"family":"Goudy","given":"W.H.","affiliations":[],"preferred":false,"id":343476,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5230034,"text":"5230034 - 1967 - Protecting corn from blackbirds","interactions":[],"lastModifiedDate":"2012-02-02T00:15:24","indexId":"5230034","displayToPublicDate":"2009-06-09T10:33:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"476","title":"Protecting corn from blackbirds","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Mitchell, R., and Linehan, J.T., 1967, Protecting corn from blackbirds: Wildlife Leaflet 476, 8.","productDescription":"8","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656b04","contributors":{"authors":[{"text":"Mitchell, R.T.","contributorId":16112,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":343399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, J. T.","contributorId":43868,"corporation":false,"usgs":true,"family":"Linehan","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":343400,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210428,"text":"5210428 - 1967 - Relation between male courtship activities and nesting of American woodcock","interactions":[],"lastModifiedDate":"2012-02-02T00:15:19","indexId":"5210428","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Relation between male courtship activities and nesting of American woodcock","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Woodcock Research and Management, 1966","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Geis, A.D., 1967, Relation between male courtship activities and nesting of American woodcock, chap. <i>of</i> Woodcock Research and Management, 1966, p. 13-14.","productDescription":"40","startPage":"13","endPage":"14","numberOfPages":"40","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c31d","contributors":{"authors":[{"text":"Geis, A. D.","contributorId":72885,"corporation":false,"usgs":true,"family":"Geis","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":328429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5210029,"text":"5210029 - 1967 - What's being done about blackbird control at the Bureau of Sport Fisheries and Wildlife Research Center Eastern Branches?","interactions":[],"lastModifiedDate":"2012-02-02T00:15:17","indexId":"5210029","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"What's being done about blackbird control at the Bureau of Sport Fisheries and Wildlife Research Center Eastern Branches?","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the North American Conference on Blackbird Depredation in Agriculture","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Ohio State University","publisherLocation":"Columbus","collaboration":"OCLC 10832270","usgsCitation":"Seubert, J., 1967, What's being done about blackbird control at the Bureau of Sport Fisheries and Wildlife Research Center Eastern Branches?, chap. <i>of</i> Proceedings of the North American Conference on Blackbird Depredation in Agriculture, p. 42-45.","productDescription":"62","startPage":"42","endPage":"45","numberOfPages":"62","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4945","contributors":{"editors":[{"text":"Giltz, Maurice L.","contributorId":112217,"corporation":false,"usgs":true,"family":"Giltz","given":"Maurice","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":505935,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Seubert, J.L.","contributorId":80770,"corporation":false,"usgs":true,"family":"Seubert","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":327657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5210063,"text":"5210063 - 1967 - Some disease problems in Canada geese","interactions":[],"lastModifiedDate":"2012-02-02T00:15:14","indexId":"5210063","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1967","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Some disease problems in Canada geese","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 2nd Annual Canada Goose Ecology Seminar, Seney, Michigan","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Herman, C.M., 1967, Some disease problems in Canada geese, chap. <i>of</i> Proceedings of the 2nd Annual Canada Goose Ecology Seminar, Seney, Michigan, p. 14-17.","startPage":"14","endPage":"17","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4986e4b07f02db5aeb1f","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010036,"text":"70010036 - 1967 - Tectonics of Antarctica","interactions":[],"lastModifiedDate":"2025-08-29T15:15:35.106212","indexId":"70010036","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1967","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 Antarctica","docAbstract":"<p><span>Antarctica consists of large and wholly continental east Antarctica and smaller west Antarctica which would form large and small islands, even after isostatic rebound, if its ice cap were melted. Most of east Antarctica is a Precambrian Shield, in much of which charnockites are characteristic. The high Transantarctic Mountains, along the Ross and Weddell Seas, largely follow a geosyncline of Upper Precambrian sedimentary rocks that were deformed, metamorphosed and intruded by granitic rocks during Late Cambrian or Early Ordovician time. The rocks of the orogen were peneplained, then covered by thin and mostly continental Devonian-Jurassic sediments, which were intruded by Jurassic diabase sheets and overlain by plateau-forming tholeiites. Late Cenozoic doming and block-faulting have raised the present high mountains.</span></p><p><span>Northeastern Victoria Land, the end of the Transantarctic Mountains south of New Zealand, preserves part of a Middle Paleozoic orogen. Clastic strata laid unconformably upon the Lower Paleozoic plutonic complex were metamorphosed at low grade, highly deformed and intruded by Late Devonian or Early Carboniferous granodiorites. The overlying Triassic continental sedimentary rocks have been broadly folded and normal-faulted.</span></p><p><span>Interior west Antarctica is composed of miogeosynclinal clastic and subordinate carbonate rocks which span the Paleozoic Era and which were deformed, metamorphosed at generally low grade, and intruded by granitic rocks during Early Mesozoic time and possibly during other times also. Patterns of orogenic belts, if systematic, cannot yet be defined; but fragmentation and rotation of crustal blocks by oroclinal folding and strike-slip faulting can be suggested. The Ellsworth Mountains, for example, consist of Cambrian-Permian metasedimentary rocks that strike northward toward the noncorrelative and latitudinally striking Mesozoic terrane of the Antarctic Peninsula in one direction and southward toward that of the Lower Paleozoic: terrane of the Transantarctic Mountains in the other; the three regions may be separated by great strike-slip faults.</span></p><p><span>The Antarctic Peninsula in west Antarctica, south of South America, consists of metavolcanic and metasedimentary rocks intruded by Late Cretaceous quartz diorite. The pre-granitic rocks are of Jurassic and Early Cretaceous ages wherever they have been dated by fossils, although some crystalline complexes may be older. The S-shape of the peninsula may represent oroclinal bending within Cenozoic time as part of a motion system in which a narrow continental bridge between South America and Antarctica was deformed and ruptured. Perhaps this bridge lagged behind as the larger continental plates drifted into the Pacific Ocean Basin.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(67)90019-4","issn":"00401951","usgsCitation":"Hamilton, W., 1967, Tectonics of Antarctica: Tectonophysics, v. 4, no. 4-6, p. 555-568, https://doi.org/10.1016/0040-1951(67)90019-4.","productDescription":"14 p.","startPage":"555","endPage":"568","costCenters":[],"links":[{"id":219663,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica","volume":"4","issue":"4-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba488e4b08c986b3203fa","contributors":{"authors":[{"text":"Hamilton, Warren","contributorId":14819,"corporation":false,"usgs":true,"family":"Hamilton","given":"Warren","affiliations":[],"preferred":false,"id":357744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010545,"text":"70010545 - 1967 - Glaucophane schists from California and New Caledonia","interactions":[],"lastModifiedDate":"2025-08-29T15:27:22.346952","indexId":"70010545","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Glaucophane schists from California and New Caledonia","docAbstract":"<p>In California and New Caledonia, metamorphism of eugeosynclinal rocks has produced blueschist facies in limited areas. The outcrop pattern and structure suggest that the shape of the zone of blueschist metamorphism is elongate parallel to major tectonic trends. </p><p>Juxtaposition of large ultramafic bodies, subparallel to the blueschist belts, indicates a close tectonic relationship between metamorphism and the tectonic emplacement of the ultramafic masses. </p><p>Initial emplacement of ultramafics along the depressed axis of the eugeosyncline may have produced deformation related to blueschist metamorphism. </p><p>Mineral assemblages developed in blueschist facies are characterized by having formed under conditions where pressure is predominant over temperature. That pressure is relatively high requires extremely low thermal gradients combined with a rheology that would allow development of tectonic overpressures.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(67)90012-1","issn":"00401951","usgsCitation":"Coleman, R.G., 1967, Glaucophane schists from California and New Caledonia: Tectonophysics, v. 4, no. 4-6, p. 479-498, https://doi.org/10.1016/0040-1951(67)90012-1.","productDescription":"20 p.","startPage":"479","endPage":"498","costCenters":[],"links":[{"id":218651,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"France, United States","state":"California","otherGeospatial":"New Caledonia","volume":"4","issue":"4-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a292ce4b0c8380cd5a70d","contributors":{"authors":[{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":359145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010460,"text":"70010460 - 1967 - The petrography of some Illinois Pleistocene and recent sands","interactions":[],"lastModifiedDate":"2025-07-24T15:53:24.908146","indexId":"70010460","displayToPublicDate":"2003-04-04T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3368,"text":"Sedimentary Geology","active":true,"publicationSubtype":{"id":10}},"title":"The petrography of some Illinois Pleistocene and recent sands","docAbstract":"<p><span>Some Recent and Pleistocene sands of Illinois and the nearby Missouri River were separated into three groups by petrographic characteristics that reflect source material. The sands derived largely or entirely from the glacial material of Illinois and the upper Mississippi, Wabash, and Lake Michigan drainage basins contain types of feldspars and rock fragments that indicate derivation from the Precambrian metamorphic rocks of the Canadian Shield. The sands of the Ohio River at the southern boundary of Illinois contain relatively large amounts of polycrystalline quartz and nonfeldspathic rock fragments that may have been derived from Paleozoic sedimentary rocks largely of Appalachian derivation, from glacial drift of the eastern states, or from both sources. A significant portion of the Missouri River sands and the Mississippi River sands below the mouth of the Missouri River consists of feldspars and rock fragments derived from the Cretaceous and Tertiary igneous rocks of the western United States. The volcanic rock fragments are especially indicative of a western source.</span></p><p><span>Petrographic characteristics of 23 samples of these sands were determined. The sources of the sands were interpreted principally from their rock fragments and light minerals, especially the feldspars, taking into account the variation in composition with changing grain size. Much of the plagioclase was untwinned, but certain varietal features proved useful in its identification.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0037-0738(67)90052-8","issn":"00370738","usgsCitation":"Hunter, R.E., 1967, The petrography of some Illinois Pleistocene and recent sands: Sedimentary Geology, v. 1, p. 57-75, https://doi.org/10.1016/0037-0738(67)90052-8.","productDescription":"19 p.","startPage":"57","endPage":"75","costCenters":[],"links":[{"id":218951,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.366031,42.500274],[-88.786681,42.491983],[-88.115285,42.496219],[-87.800561,42.49192],[-87.79823,42.473054],[-87.80537,42.384721],[-87.820858,42.361584],[-87.834769,42.301522],[-87.828569,42.269922],[-87.800066,42.208024],[-87.741662,42.128227],[-87.712206,42.096455],[-87.682359,42.075729],[-87.671462,42.058334],[-87.668982,42.029142],[-87.630953,41.933132],[-87.624052,41.904232],[-87.611659,41.892216],[-87.616537,41.882396],[-87.616251,41.868933],[-87.60945,41.845233],[-87.600549,41.826833],[-87.580948,41.804334],[-87.576347,41.786034],[-87.560646,41.766034],[-87.542845,41.752135],[-87.530745,41.748235],[-87.524141,41.72399],[-87.526376,40.491574],[-87.533227,39.883127],[-87.531646,39.347888],[-87.544013,39.352907],[-87.5544,39.340488],[-87.578331,39.340343],[-87.589084,39.333831],[-87.600397,39.312904],[-87.597545,39.296388],[-87.61005,39.282232],[-87.605543,39.261122],[-87.593486,39.247452],[-87.583535,39.243579],[-87.574558,39.218404],[-87.588614,39.197824],[-87.620796,39.17479],[-87.640435,39.166727],[-87.64599,39.1449],[-87.643145,39.128562],[-87.632245,39.118702],[-87.630376,39.104305],[-87.619134,39.100557],[-87.613513,39.085568],[-87.596373,39.079639],[-87.572588,39.057286],[-87.575027,39.034062],[-87.569696,39.019413],[-87.579117,39.001607],[-87.578319,38.988786],[-87.529496,38.971925],[-87.512187,38.954417],[-87.518826,38.923205],[-87.527645,38.907688],[-87.544089,38.895093],[-87.553384,38.863344],[-87.525893,38.848795],[-87.521681,38.826576],[-87.527342,38.818121],[-87.496537,38.778571],[-87.496494,38.742728],[-87.516707,38.716333],[-87.519609,38.697198],[-87.531231,38.684036],[-87.593678,38.667402],[-87.62012,38.639489],[-87.627348,38.60544],[-87.62389,38.593984],[-87.637752,38.588512],[-87.651529,38.568166],[-87.650704,38.55624],[-87.660732,38.541092],[-87.653802,38.517382],[-87.657084,38.507169],[-87.714047,38.47988],[-87.739522,38.475069],[-87.74317,38.459019],[-87.730134,38.446518],[-87.74104,38.435576],[-87.745254,38.408996],[-87.779996,38.370842],[-87.806075,38.363143],[-87.822721,38.346912],[-87.832723,38.324853],[-87.831972,38.307241],[-87.838243,38.29375],[-87.853046,38.289264],[-87.875476,38.301376],[-87.88041,38.299581],[-87.887849,38.285299],[-87.908223,38.274012],[-87.92168,38.289712],[-87.928858,38.292404],[-87.938727,38.289264],[-87.952125,38.273763],[-87.945904,38.256966],[-87.950838,38.247097],[-87.960225,38.237118],[-87.975511,38.232742],[-87.982688,38.221527],[-87.984234,38.20996],[-87.975819,38.197834],[-87.9595,38.184376],[-87.928858,38.168594],[-87.922577,38.160071],[-87.92168,38.148407],[-87.945472,38.126616],[-87.974272,38.121981],[-87.999734,38.100857],[-87.998389,38.090091],[-87.984931,38.069008],[-87.990314,38.056447],[-88.020369,38.046578],[-88.02979,38.025046],[-88.012574,37.977062],[-88.012929,37.966544],[-88.036124,37.942746],[-88.044145,37.926805],[-88.031584,37.901685],[-88.033378,37.894059],[-88.054462,37.877461],[-88.058499,37.865349],[-88.053116,37.847854],[-88.043247,37.836639],[-88.051771,37.813761],[-88.045939,37.807481],[-88.029382,37.803601],[-88.02803,37.799224],[-88.035827,37.791917],[-88.042602,37.76712],[-88.059588,37.742608],[-88.122412,37.709685],[-88.151646,37.675098],[-88.160187,37.657592],[-88.156827,37.632801],[-88.142225,37.603737],[-88.139973,37.586451],[-88.13341,37.574273],[-88.105585,37.55618],[-88.088049,37.535124],[-88.069018,37.525297],[-88.061342,37.505327],[-88.064234,37.484548],[-88.072386,37.483563],[-88.087664,37.471059],[-88.132628,37.471555],[-88.281667,37.452596],[-88.312585,37.440591],[-88.333183,37.42721],[-88.348405,37.410726],[-88.365471,37.401663],[-88.408808,37.425216],[-88.450127,37.411717],[-88.470224,37.396255],[-88.476592,37.386875],[-88.484462,37.345609],[-88.515939,37.284043],[-88.506942,37.266656],[-88.509328,37.26213],[-88.487277,37.244077],[-88.471753,37.220155],[-88.447764,37.203527],[-88.431488,37.160298],[-88.424403,37.152428],[-88.444605,37.098601],[-88.458948,37.073796],[-88.504437,37.065265],[-88.545403,37.070003],[-88.576718,37.085852],[-88.589207,37.099655],[-88.625889,37.119458],[-88.693983,37.141155],[-88.732105,37.143956],[-88.80572,37.188595],[-88.916934,37.224291],[-88.942111,37.228811],[-88.98326,37.228685],[-89.029981,37.211144],[-89.076221,37.175125],[-89.092934,37.156439],[-89.111189,37.119052],[-89.134931,37.103278],[-89.14132,37.093865],[-89.154504,37.088907],[-89.168087,37.074218],[-89.181369,37.046305],[-89.178975,37.020928],[-89.166447,37.003337],[-89.132685,36.9822],[-89.170008,36.970298],[-89.185491,36.973518],[-89.192097,36.979995],[-89.200793,37.016164],[-89.234053,37.037277],[-89.25493,37.072014],[-89.259936,37.064071],[-89.307726,37.069654],[-89.310819,37.057897],[-89.304752,37.047565],[-89.277715,37.03614],[-89.260003,37.023288],[-89.257608,37.015496],[-89.263527,37.00005],[-89.278628,36.98867],[-89.29213,36.992189],[-89.322982,37.01609],[-89.378277,37.039605],[-89.385434,37.05513],[-89.375712,37.080505],[-89.37871,37.094586],[-89.38805,37.107481],[-89.41173,37.122507],[-89.42558,37.138235],[-89.461862,37.199517],[-89.4675,37.221844],[-89.458246,37.247066],[-89.470525,37.253357],[-89.488728,37.251507],[-89.517032,37.28192],[-89.511842,37.310825],[-89.489005,37.333368],[-89.447556,37.340475],[-89.432836,37.347056],[-89.421054,37.387668],[-89.439769,37.4372],[-89.475525,37.471388],[-89.516447,37.535558],[-89.521925,37.560735],[-89.519808,37.582748],[-89.486062,37.580853],[-89.477548,37.585885],[-89.475932,37.592998],[-89.517718,37.641217],[-89.51204,37.680985],[-89.516685,37.692762],[-89.531427,37.700334],[-89.583316,37.713261],[-89.596566,37.732886],[-89.615586,37.74235],[-89.615933,37.748184],[-89.64953,37.745498],[-89.663352,37.750052],[-89.667993,37.759484],[-89.66038,37.786296],[-89.669644,37.799922],[-89.71748,37.825724],[-89.739873,37.84693],[-89.754104,37.846358],[-89.779828,37.853896],[-89.786369,37.851734],[-89.80036,37.868625],[-89.798041,37.879655],[-89.842649,37.905196],[-89.862949,37.896906],[-89.881475,37.879591],[-89.901832,37.869822],[-89.923185,37.870672],[-89.950594,37.881526],[-89.973642,37.917661],[-89.974918,37.926719],[-89.959646,37.940196],[-89.947429,37.940336],[-89.932467,37.947497],[-89.925085,37.960021],[-89.933797,37.959143],[-89.942099,37.970121],[-89.997103,37.963225],[-90.03241,37.995258],[-90.051357,38.003584],[-90.057269,38.014362],[-90.08826,38.015772],[-90.11052,38.026547],[-90.126194,38.040702],[-90.126396,38.054897],[-90.130788,38.062341],[-90.158533,38.074735],[-90.17222,38.069636],[-90.218708,38.094365],[-90.243116,38.112669],[-90.274928,38.157615],[-90.290765,38.170453],[-90.331554,38.18758],[-90.356176,38.217501],[-90.373929,38.281853],[-90.370819,38.333554],[-90.349743,38.377609],[-90.295316,38.426753],[-90.285215,38.443453],[-90.260314,38.528352],[-90.224212,38.575051],[-90.196011,38.594451],[-90.18451,38.611551],[-90.17801,38.63375],[-90.18111,38.65955],[-90.18641,38.67475],[-90.20921,38.70275],[-90.21141,38.72135],[-90.20521,38.73215],[-90.176309,38.754449],[-90.166409,38.772649],[-90.123107,38.798048],[-90.109107,38.837448],[-90.113327,38.849306],[-90.19521,38.886748],[-90.223041,38.907389],[-90.250248,38.919344],[-90.309454,38.92412],[-90.395816,38.960037],[-90.440078,38.967364],[-90.450792,38.967764],[-90.472122,38.958838],[-90.482419,38.94446],[-90.486974,38.925982],[-90.500117,38.910408],[-90.54403,38.87505],[-90.583388,38.86903],[-90.628485,38.891617],[-90.639917,38.908272],[-90.663372,38.928042],[-90.675949,38.96214],[-90.678193,38.991851],[-90.713629,39.053977],[-90.682744,39.088348],[-90.681086,39.10059],[-90.686051,39.117785],[-90.707902,39.15086],[-90.717113,39.213912],[-90.72996,39.255894],[-90.751599,39.265432],[-90.793461,39.309498],[-90.816851,39.320496],[-90.8475,39.345272],[-90.893777,39.367343],[-90.904862,39.379403],[-90.928745,39.387544],[-90.940766,39.403984],[-90.993789,39.422959],[-91.03827,39.448436],[-91.059439,39.46886],[-91.064305,39.494643],[-91.079769,39.507728],[-91.100307,39.538695],[-91.153628,39.548248],[-91.168419,39.564928],[-91.174232,39.591975],[-91.181936,39.602677],[-91.229317,39.620853],[-91.27614,39.665759],[-91.302485,39.679631],[-91.367753,39.729029],[-91.369953,39.745042],[-91.365125,39.758723],[-91.363444,39.792804],[-91.377971,39.811273],[-91.432919,39.840554],[-91.446385,39.870394],[-91.443513,39.893583],[-91.420878,39.914865],[-91.41936,39.927717],[-91.463683,39.981845],[-91.494878,40.036453],[-91.489606,40.057435],[-91.509245,40.121876],[-91.511749,40.147091],[-91.508324,40.156326],[-91.513079,40.178537],[-91.504477,40.198262],[-91.505828,40.238839],[-91.490524,40.259498],[-91.492727,40.278217],[-91.46214,40.342414],[-91.439342,40.366569],[-91.415695,40.381381],[-91.381958,40.387632],[-91.372921,40.399108],[-91.373721,40.417891],[-91.381769,40.442555],[-91.364915,40.484168],[-91.364211,40.500043],[-91.384531,40.530948],[-91.404125,40.539127],[-91.405241,40.554641],[-91.379752,40.57445],[-91.359873,40.601805],[-91.339719,40.613488],[-91.306524,40.626231],[-91.253074,40.637962],[-91.18698,40.637297],[-91.123928,40.669152],[-91.110927,40.703262],[-91.115735,40.725168],[-91.110424,40.745528],[-91.091703,40.779708],[-91.097649,40.805575],[-91.092993,40.821079],[-91.05643,40.848387],[-91.044653,40.868356],[-91.021562,40.884021],[-91.009536,40.900565],[-90.962916,40.924957],[-90.952233,40.954047],[-90.958142,40.979767],[-90.945949,41.006495],[-90.942253,41.034702],[-90.94899,41.07025],[-90.946259,41.094734],[-90.99496,41.160624],[-91.007586,41.166183],[-91.027214,41.163373],[-91.041536,41.166138],[-91.07298,41.207151],[-91.112333,41.239003],[-91.114186,41.250029],[-91.08688,41.294371],[-91.074841,41.305578],[-91.06652,41.365246],[-91.05158,41.385283],[-91.04589,41.414085],[-91.027787,41.423603],[-90.979815,41.434321],[-90.930016,41.421404],[-90.846558,41.455141],[-90.750142,41.449632],[-90.655839,41.462132],[-90.605937,41.494232],[-90.602137,41.506032],[-90.595237,41.511032],[-90.567236,41.517532],[-90.556235,41.524232],[-90.540935,41.526133],[-90.500633,41.518033],[-90.461432,41.523533],[-90.41283,41.565333],[-90.343228,41.587833],[-90.339528,41.598633],[-90.343452,41.646959],[-90.334525,41.679559],[-90.313435,41.698082],[-90.317668,41.72269],[-90.310708,41.742214],[-90.278633,41.767358],[-90.181973,41.80707],[-90.181901,41.843216],[-90.153584,41.906614],[-90.152659,41.933058],[-90.163847,41.944934],[-90.164135,41.956178],[-90.146225,41.981329],[-90.140061,42.003252],[-90.150916,42.02944],[-90.163446,42.040407],[-90.168358,42.075779],[-90.161504,42.098912],[-90.162895,42.116718],[-90.17097,42.125198],[-90.190452,42.125779],[-90.201404,42.130937],[-90.207421,42.149109],[-90.216107,42.15673],[-90.250129,42.171469],[-90.282173,42.178846],[-90.328273,42.201047],[-90.356964,42.205445],[-90.391108,42.225473],[-90.400653,42.239293],[-90.419326,42.254467],[-90.430884,42.27823],[-90.415937,42.322699],[-90.419027,42.328505],[-90.477279,42.383794],[-90.555018,42.416138],[-90.560439,42.432897],[-90.567968,42.440389],[-90.606328,42.451505],[-90.646727,42.471904],[-90.654027,42.478503],[-90.656527,42.489203],[-90.640927,42.508302],[-90.07367,42.508275],[-89.366031,42.500274]]]},\"properties\":{\"name\":\"Illinois\",\"nation\":\"USA  \"}}]}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae8de4b08c986b32419c","contributors":{"authors":[{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":358974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197602,"text":"70197602 - 1967 - Techniques for computing rate and volume of stream depletion by wells","interactions":[],"lastModifiedDate":"2022-05-25T19:03:18.799932","indexId":"70197602","displayToPublicDate":"1999-11-28T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Techniques for computing rate and volume of stream depletion by wells","docAbstract":"<p>The effects on flow of a nearby stream from pumping a well can be calculated readily using dimensionless curves and tables. Computations can be made of: (1) The rate of stream depletion at any time during the pumping period or after the cessation of pumping; (2) The volume induced from the stream during any time, both during pumping or after the cessation of pumping; and (3) The effects, both in rate and volume of stream depletion, of any selected pattern of intermittent pumping. Sample computations illustrate the use of the curves and tables. An example shows that intermittent pumping may have a pattern of stream depletion not greatly different from a. pattern for steady pumping of an equal volume.</p><p>The residual effects of pumping, that is, effects after cessation of pumping, on streamflow may easily be greater than the effects during the pumping period. Adequate advance planning that includes consideration of residual effects thus is essential to effective administration of a stream-aquifer system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70197602","collaboration":"Prepared in cooperation with the Colorado Water Conservation Board and the Southeastern Colorado Water Conservancy District.","usgsCitation":"Jenkins, C., 1967, Techniques for computing rate and volume of stream depletion by wells: Open-File Report, iii, 40 p., https://doi.org/10.3133/70197602.","productDescription":"iii, 40 p.","costCenters":[],"links":[{"id":354997,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70197602/report-thumb.jpg"},{"id":401067,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70197602/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jenkins, C.T.","contributorId":106099,"corporation":false,"usgs":true,"family":"Jenkins","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":737879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52630,"text":"ofr67207 - 1967 - Far infrared luminescence","interactions":[],"lastModifiedDate":"2014-07-14T11:25:24","indexId":"ofr67207","displayToPublicDate":"1994-10-01T00:00:00","publicationYear":"1967","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":"67-207","title":"Far infrared luminescence","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr67207","collaboration":"Prepared by the Geological Survey for the National Aeronautics and Space Administration (NASA) under NASA contract no. R-146-09-020-006 and T-65754.","usgsCitation":"Stoddard, A., 1967, Far infrared luminescence: U.S. Geological Survey Open-File Report 67-207, 21 p., https://doi.org/10.3133/ofr67207.","productDescription":"21 p.","numberOfPages":"21","costCenters":[],"links":[{"id":100213,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0207/report.pdf","size":"980","linkFileType":{"id":1,"text":"pdf"}},{"id":178449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0207/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f75aa","contributors":{"authors":[{"text":"Stoddard, A.E.","contributorId":26750,"corporation":false,"usgs":true,"family":"Stoddard","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":245675,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38847,"text":"pp542F - 1967 - Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands","interactions":[{"subject":{"id":38847,"text":"pp542F - 1967 - Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands","indexId":"pp542F","publicationYear":"1967","noYear":false,"chapter":"F","title":"Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands"},"predicate":"IS_PART_OF","object":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"id":1}],"isPartOf":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"lastModifiedDate":"2022-02-15T20:39:34.466499","indexId":"pp542F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"542","chapter":"F","title":"Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands","docAbstract":"<p>The great earthquake (Richter magnitude of 8.4–8.5) that struck south-central Alaska at 5:36 p.m., Alaska standard time, on March 27, 1964 (03:36, March 28, Greenwich mean time), was felt in every community on Kodiak Island and the nearby islands. It was the most severe earthquake to strike this part of Alaska in modern time, and took the lives of 18 persons in the area by drowning; this includes two in Kodiak and three at Kaguyak. Property damage and loss of income to the communities is estimated at more than $45 million.</p>\n</br>\n<p>The largest community, Kodiak, had the greatest loss from the earthquake. Damage was caused chiefly by 5.6 feet of tectonic subsidence and a train of 10 seismic sea waves that inundated the low-lying areas of the town. The seismic sea waves destroyed all but one of the docking facilities and more than 215 structures; many other structures were severely damaged. The waves struck the town during the evening hours of March 27 and early morning hours of March 28. They moved from the southwest and northeast: and reached their maximum height of 20–30 feet above mean lower low water at Shahafka Cove between 11:00 and 11:45 p.m., March 27. The violently destructive seismic sea waves not only severely damaged homes, shops, and naval-station structures but also temporarily crippled the fishing industry in Kodiak by destroying the processing plants and most of the fishing vessels. The waves scoured out 10 feet of sediments in the channel between Kodiak Island and Near Island and exposed bedrock. This bedrock presented a major post-earthquake construction problem because no sediments remained into which piles could be driven for foundations of waterfront facilities.</p>\n</br>\n<p>Because of tectonic subsidence, high tides now flood Mission and Potatopatch Lakes which, before the earthquake, had not been subject to tidal action. The subsidence also accelerated erosion of the unconsolidated sediments along the shoreline in the city of Kodiak.</p>\n</br>\n<p>Seismic shaking lasted 4½–5½ minutes at Kodiak and had a rolling motion. Inasmuch as most of Kodiak is underlain by bedrock or by only a thin veneer of unconsolidated sediments, very little if any damage occurred from ground motion or seismic shaking. The ground motion, however, did cause a massive short circuit and power failure at Kodiak.</p>\n</br>\n<p>The Kodiak Naval Station, 5 miles southwest of Kodiak, was also severely damaged by the earthquake. The station was inundated by at least 10 seismic sea waves which reached a maximum height of 25 feet above post-earthquake mean lower low water between 11:16 and 11:34 p.m. on March 27, 1964. The first seismic sea wave that inundated the station did not do severe damage because it behaved much like a rapid rise of tide, but the subsequent and more violent waves destroyed most of the docking facilities and several other shoreline structures. The waves struck the station from the southwest and from the east.</p>\n</br>\n<p>The shoreline structures that were not destroyed required rehabilitation because the 5.6 feet of tectonic subsidence put them under water during the highest tides. Furthermore the subsidence accelerated erosion during high tide of the soft unconsolidated sediments and fill in the low-lying areas of the station.</p>\n</br>\n<p>Seismic shaking did little damage to the station housing facility, but it was responsible for compaction of sediments, lateral displacement of a seawall, and the development of fissures in the aircraft parking area. The ground motion was as south-southeast–north-northwest to north-south in direction.</p>\n</br>\n<p>An unusual case of radioactive contamination was reported at the naval station. The inundating seismic sea waves entered a building in which radionuclides were stored. The contamination was restricted to the building only, however, and did not spread throughout the station.</p>\n</br>\n<p>Afognak was abandoned because of the extensive damage incurred from tectonic subsistence and seismic sea waves. The seismic effects, estimated Mercalli intensity VI-VII, did not directly cause any significant property damage at Afognak Serious long-term damage, however, resulted from tectonic subsidence estimated to be from 3½ to 5½ feet. The subsidence has resulted in rapid erosion of the coast, landward shift and building up of bench berms to the new higher sea levels, and flooding of extensive low-lying areas behind the barrier beaches. Inundation of low-lying parts of the village by a train of seismic sea waves having maximum heights of 10.8 feet above post-earthquake tide level (14.5 ft above post-earthquake mean lower low water) caused losses of about half a million dollars to homes, vehicles, bridges, and personal possessions.</p>\n</br>\n<p>Uzinki was damaged by tectonic subsidence and seismic sea waves. No significant damage resulted from the ground motion during the earthquake; the Mercalli intensity was about VI. However, tectonic subsidence, estimated to be 5 feet, caused inundation of a narrow zone along the waterfront. Structures and vessels were damaged as a result of the seismic sea waves that repeatedly flooded the waterfront area after the earthquake.</p>\n</br>\n<p>Old Harbor was damaged by seismic shock, subsidence, and seismic sea waves. The tremors, which had a Mercalli intensity estimated at VII-VIII, toppled two concrete-block chimneys, cracked interior walls, and caused minor breakage of personal property in the homes. Regional tectonic subsidence and superficial subsidence of the unconsolidated deposits on which the village is situated apparently caused incursion of salt water into the school well. A quarter of million yards of fill was required to raise the waterfront areas to their pre-earthquake elevations relative to sea level. Seismic sea waves having a maximum runup of about 12 feet above tide level (16 ft above post-earthquake mean lower low water) destroyed 34 of the 35 residences in the village and presumably drowned one man who lived immediately across the strait from Old Harbor.</p>\n</br>\n<p>At Kaguyak, seismic sea waves having a maximum runup of about 25 feet above mean lower low water carried away all 10 buildings in the village, took three lives, and damaged an unknown number of fishing vessels. The village site has been abandoned. The communities of Akhiok, Karluk, and Larsen Bay were virtually undamaged by the earthquake tremors, which had estimated Mercalli intensities of VI-VII, but tectonic subsidence of about 2–2½ feet at Larsen Bay made it necessary to raise the cannery dock level at an estimated cost of $80,000.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on communities (Professional Paper 542)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542F","usgsCitation":"Kachadoorian, R., and Plafker, G., 1967, Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands: U.S. Geological Survey Professional Paper 542, Report: vi, 41 p.; 1 Plate: 20.53 x 16.53 inches, https://doi.org/10.3133/pp542F.","productDescription":"Report: vi, 41 p.; 1 Plate: 20.53 x 16.53 inches","numberOfPages":"49","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":396001,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4588.htm"},{"id":170406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0542f/report-thumb.jpg"},{"id":113270,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542f/pp542f_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0542f/pp542f_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":111458,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0542f/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Kodiak Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153.34442138671875,\n              57.671848402248166\n            ],\n            [\n              -152.10296630859375,\n              57.671848402248166\n            ],\n            [\n              -152.10296630859375,\n              58.1793925460941\n            ],\n            [\n              -153.34442138671875,\n              58.1793925460941\n            ],\n            [\n              -153.34442138671875,\n              57.671848402248166\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610277","contributors":{"authors":[{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":220535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":220534,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38846,"text":"pp542E - 1967 - Effects of the earthquake of March 27, 1964, at Seward, Alaska","interactions":[{"subject":{"id":38846,"text":"pp542E - 1967 - Effects of the earthquake of March 27, 1964, at Seward, Alaska","indexId":"pp542E","publicationYear":"1967","noYear":false,"chapter":"E","title":"Effects of the earthquake of March 27, 1964, at Seward, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"id":1}],"isPartOf":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"lastModifiedDate":"2022-03-31T18:47:27.868901","indexId":"pp542E","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"542","chapter":"E","title":"Effects of the earthquake of March 27, 1964, at Seward, Alaska","docAbstract":"<p>Seward, in south-central Alaska, was one of the towns most devastated by the Alaska earthquake of March 27, 1964. The greater part of Seward is built on an alluvial fan-delta near the head of Resurrection Bay on the southeast coast of the Kenai Peninsula. It is one of the few ports in south-central Alaska that is ice free all year, and the town’s economy is almost entirely dependent upon its port facilities.</p>\n</br>\n<p>The Alaska earthquake of March 27, 1964, magnitude approximately 8.3–8.4, began at 6:36 p.m. Its epicenter was in the northern part of the Prince William Sound area; focal depth was 20–50 km.</p>\n</br>\n<p>Strong ground motion at Seward lasted 3–4 minutes. During the shaking, a strip of land 50–400 feet wide along the Seward waterfront, together with docks and other harbor facilities, slid into Resurrection Bay as a result of large-scale submarine landsliding. Fractures ruptured the ground for'severa1 hundred feet back from the landslide scarps. Additional ground was fractured in the Forest Acres subdivision and on the alluvial floor of the Resurrection River valley; fountaining and sand boils accompanied the ground fracturing. Slide-generated wares, possibly seiche waves, and seismic sea waves crashed onto shore; ware runup was as much as 30 feet above mean lower low water and caused tremendous damage; fire from burning oil tanks added to the destruction. Damage from strong ground motion itself was comparatively minor. Tectonic subsidence of about 3.6 feet resulted in low areas being inundated at high tide.</p>\n</br>\n<p>Thirteen people were killed and five were injured as a result of the earthquake. Eighty-six houses were totally destroyed and 260 were heavily damaged. The harbor facilities were almost completely destroyed, and the entire economic base of the town was wiped out. The total cost to replace the destroyed public and private facilities was estimated at $22 million.</p>\n</br>\n<p>Seward lies on the axis of the Chugach Mountains geosyncline. The main structural trend in the mapped area, where the rocks consist almost entirely of graywacke and phyllite, is from near north to N. 20° E. Beds and cleavage of the rocks commonly dip 70° W. or NW. to near vertical. Locally, the rocks are complexly folded or contorted. So major faults were found in the mapped area, but small faults, shear zones, and joints are common.</p>\n</br>\n<p>Surficial deposits of the area hare been divided for mapping into the following units: drift deposits, alluvial fan deposits, valley alluvium, intertidal deposits, landslide deposits, and artificial fill. Most of these units intergrade and were deposited more or less contemporaneously.</p>\n</br>\n<p>The drift deposits consist chiefly of till that forms moraines along the lower flanks of the Resurrection River valley and up tributary valleys. The till is predominantly silt and sand and lesser amounts of clay-size particles, gravel, cobbles, and boulders. Glacial outwash and stratified ice-contact deposits constitute the remainder of the drift deposits.</p>\n</br>\n<p>Fans and fan-deltas have been deposited at the valley mouths of tributary streams. Some, including the one upon which Seward built, project into Resurrection Bay, and deltaic-type deposits form their distal edges. The larger fans—composed chiefly of loosely compacted and poorly sorted silt, sand, and gravel—form broad aprons having low gradients. The fan deposits range in thickness from about 100 feet to possibly several hundred feet and, at least in some places, lie on a platform of compact drift. Smaller fans at the mouths of several canyons have steep gradients and considerable local relief.</p>\n</br>\n<p>Valley alluvium, deposited chiefly by the Resurrection River, consists mostly of coarse sand and fine to medium gravel. In the axial part of the valley it is probably more than 100 feet thick. Near the head of Resurrection Bay, the alluvium is underlain by at least 75 feet of marine deltaic sediments, which are in turn underlain by 600 or more feet of drift in the deepest part of the bedrock valley.</p>\n</br>\n<p>Beach, deltaic, and estuarine sediments, deposited on intertidal flats at the head of the bay and along far1 margins that extend into the bay, arc mapped as intertidal deposits. They consist mostly of silt, sand, and fine gravel, and lesser amounts of clay-size particles.</p>\n</br>\n<p>The earthquake reactivated old slides and trigged new ones in the mountains. Rock and snow avalanches, debris flows, and creep of talus deposits characterized slide activity on the steeper slops. The Seward waterfront had been extended before the earthquake by adding artificial fill consisting of loose sand and gravel; part of the lagoon area had been filled with refuse. After the earth- quake, fill, consisting of silt and sand dredged from the head of the bay, was pumped onto part of the lagoon area and also on land at the northwest corner of the bay.</p>\n</br>\n<p>Response to the disaster was immediate and decisive. City, State, and Federal agencies, as well as other organizations and individuals, gave unstintingly of their time and facilities. Within a few days, there was temporary restoration of water, sewerage, and electrical facilities.</p>\n</br>\n<p>The U.S. Army Corps of Engineers was authorized to select sites and construct a new dock for the Alaska Railroad, a new small-boat basin, and related facilities. The firm of Shannon and Wilson, Inc., under contract to the Corps of Engineers, investigated subsurface soils extensively to determine the factors responsible for the sliding along the Seward waterfront and to assist in site selection for reconstruction of the destroyed harbor facilities. Borings also made along the Seward waterfront and at the head of the bay, and laboratory tests were conducted on pertinent samples. These studies were augmented by geophysical studies both on land and in the bay. In addition, the Corps of Engineers made shallow borings on the intertidal flats at the head of the bay and performed pile-driving and load tests. Borings also were drilled and test pits were dug in the subdivision of Forest Acres.</p>\n</br>\n<p>Sliding along the Seward waterfront markedly deepened the water along the former shoreline. Post-earthquake slopes of the bay floor immediately offshore also are steeper in places than before the earthquake. The strong ground motion of the earthquake triggered the landsliding, but several factors may have contributed to the magnitude and characteristics of the slides. These factors are: (1) the long duration of strong ground motion, (2) the grain size and texture of the material involved in the sliding, (3) the probability that the finer grained materials liquefied and flowed seaward, and (4) the added load of manmade facilities built on the edge of the shore, Secondary effects of the slides themselves—sudden drawdown of water, followed by the weight of returning waves—also may have contributed to the destruction.</p>\n</br>\n<p>Submarine sliding at the northwest corner of the bay occurred in fine-grained deltaic deposits whose frontal slopes probably were in metastable equilibrium under static conditions. Uplift pressures from aquifers under hydrostatic head, combined with the probable liquefaction characteristics of the sediments when vibrated by strong ground motion, probably caused the material to slide and flow seaward as a heavy slurry.</p>\n</br>\n<p>Under static conditions, no major shoreline or submarine landsliding is expected in the Seward area; in the event of another severe earthquake, however, additional sliding is likely along the Seward waterfront and also in the deltaic deposits at the northwest corner of the bay. Fractured ground in back of the present shoreline along the Seward waterfront is an area of incipient landslides that would be unstable under strong shaking. For this reason the Scientific and Engineering Task Force placed the area in a high-risk classification and recommended no repair, rehabilitation, or new construction in this area involving use of Federal funds; it was further recommended that the area should be reserved for park or other uses that do not involve large congregations of people. The deltaic deposits at the head of the bay probably also would be susceptible to sliding during another large earthquake. This sliding would result in further landward retreat of the present shoreline toward the new railroad dock. Specifications for the new dock, whose seaward end is now approximately 1,100 feet from the back scarp of the subaqueous landslide, require design pro- visions to withstand seismic shock up to certain limits.</p>\n</br>\n<p>Earthquake-induced fracturing of the ground in the subdivision of Forest Acres was confined to the lower part of a broad alluvial fan. There, sewer and water lines were ruptured and the foundations of some homes were heavily damaged. Landsliding, such as occurred along the shoreline of the bay, was not a contributing cause of the fracturing. Two hypotheses are offered to explain the fracturing:</p>\n\n<p>1. Seismic energy was transformed into visible surface waves of such amplitude that the strength of surface layer was exceeded and rupturing occurred; tensional and compressional stresses alternately opened and closed the fractures and forced out water and mud.</p>\n\n<p>2. Compaction by vibration of the fine-grained deposits of the fan caused ground settlement and fracturing; ground water under temporary hydrostatic head was forced to the surface as fountains and carried the finer material with it.</p>\n</br>\n<p>Water waves that crashed onto shore, while shaking was still continuing, were generated chiefly by onshore and offshore landsliding. Waves that overran the shores about 25 minutes after shaking stopped and that continued to arrive for the next several hours are believed to be seismic sea waves (tsunamis) that originated in an uplifted area in the Gulf of Alaska. During the time of seismic sea-wave activity and perhaps preceding it, seiche wares also may have been generated within Resurrection Bay and complicated the wave effects along the shoreline.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on communities (Professional Paper 542)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542E","usgsCitation":"Lemke, R., 1967, Effects of the earthquake of March 27, 1964, at Seward, Alaska: U.S. Geological Survey Professional Paper 542, Report: viii, 43 p.; 2 Plates: 20.5 x 21.5 inches and 25.57 x 19.78 inches, https://doi.org/10.3133/pp542E.","productDescription":"Report: viii, 43 p.; 2 Plates: 20.5 x 21.5 inches and 25.57 x 19.78 inches","numberOfPages":"53","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":170343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0542e/report-thumb.jpg"},{"id":113268,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397947,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4587.htm"},{"id":113267,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104504,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0542e/index.html","linkFileType":{"id":5,"text":"html"},"description":"4587"}],"scale":"63360","datum":"Mean Sea Level","country":"United States","state":"Alaska","city":"Seward","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.4778,\n              60.0622\n            ],\n            [\n              -149.3333,\n              60.0622\n            ],\n            [\n              -149.3333,\n              60.1856\n            ],\n            [\n              -149.4778,\n              60.1856\n            ],\n            [\n              -149.4778,\n              60.0622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610336","contributors":{"authors":[{"text":"Lemke, Richard W.","contributorId":59409,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard W.","affiliations":[],"preferred":false,"id":220533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38815,"text":"pp543F - 1967 - Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","interactions":[{"subject":{"id":38815,"text":"pp543F - 1967 - Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","indexId":"pp543F","publicationYear":"1967","noYear":false,"chapter":"F","title":"Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-02-18T20:13:03.475534","indexId":"pp543F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"F","title":"Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","docAbstract":"The great 1964 Alaska earthquake caused considerable ground breakage in the Cook Inlet area of south-central Alaska. The breakage occurred largely in thick deposits of unconsolidated sediments. The most important types of ground breakage were (1) fracturing or cracking and the extrusion of sand and gravel with ground water along fractures in various types of landforms, and (2) slumping and lateral extension of unconfined faces, particularly along delta fronts.\n\nThe principal concentration of ground breakage within the area covered by this report was in a northeast-trending zone about 60 miles long and 6 miles wide in the northern part of the Kenai Lowland. The zone cut across diverse topography and stratigraphy. Cracks were as much as 30 feet across and 25 feet deep. Sand, gravel, and pieces of coal and lignite were extruded along many fissures. It is suggested that the disruption in this zone may be due to movement along a fault in the underlying Tertiary rocks.\n\nThe outwash deltas of Tustumena and Skilak Lakes in the Kenai Lowland, of Eklutna Lake and Lake George in the Chugach Mountains, of Bradley Lake in the Kenai Mountains, and at the outlet of upper Beluga Lake at the base of the Alaska Range showed much slumping, as did the delta of the Susitna River. Parts of the flood plains of the Skilak River, Fox River, and Eagle River were extensively cracked.\n\nA few avalanches and slumps occurred along the coast of Cook Inlet in scattered localities. Some tidal flats were cracked. However, in view of the many thick sections of unconsolidated sediments and the abundance of steep slopes, the cracking was perhaps less than might have been expected.\n\nObservations along the coasts indicated changes in sea level which, although caused partly by compaction of unconsolidated sediments, may largely be attributed to crus1tal deformation accompanying the earthquake. Most of the Cook Inlet area was downwarped, although the northwest side of Cook Inlet may have been slightly unwarped. Maximum change in the Cook Inlet area was probably less than 6 feet. Little or no regional tilting was detected in the lake basins of Tustumena and Skilak Lakes.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543F","usgsCitation":"Foster, H.L., and Karlstrom, T., 1967, Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake: U.S. Geological Survey Professional Paper 543, Report: v, 28 p.; 3 Plates: 19.81 x 30.95 inches or smaller, https://doi.org/10.3133/pp543F.","productDescription":"Report: v, 28 p.; 3 Plates: 19.81 x 30.95 inches or smaller","numberOfPages":"36","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":65737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543f/pp543f_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65736,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543f/pp543f_plate3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65735,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543f/pp543f_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543f/report-thumb.jpg"},{"id":396180,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4591.htm"},{"id":104506,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543f/index.html","linkFileType":{"id":5,"text":"html"},"description":"4591"},{"id":65734,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543f/pp543f_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -154.33,58.78 ], [ -154.33,61.56 ], [ -148.94,61.56 ], [ -148.94,58.78 ], [ -154.33,58.78 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dcf3","contributors":{"authors":[{"text":"Foster, Helen L.","contributorId":56195,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlstrom, Thor N. V.","contributorId":77929,"corporation":false,"usgs":true,"family":"Karlstrom","given":"Thor N. V.","affiliations":[],"preferred":false,"id":220491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38820,"text":"pp544D - 1967 - Effects of the March 1964 Alaska earthquake on glaciers","interactions":[],"lastModifiedDate":"2022-02-15T20:43:32.459277","indexId":"pp544D","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"D","title":"Effects of the March 1964 Alaska earthquake on glaciers","docAbstract":"The 1964 Alaska earthquake occurred in a region where there are many hundreds of glaciers, large and small. Aerial photographic investigations indicate that no snow and ice avalanches of large size occurred on glaciers despite the violent shaking. Rockslide avalanches extended onto the glaciers in many localities, seven very large ones occurring in the Copper River region 160 kilometers east of the epicenter. Some of these avalanches traveled several kilometers at low gradients; compressed air may have provided a lubricating layer. If long-term changes in glaciers due to tectonic changes in altitude and slope occur, they will probably be very small. No evidence of large-scale dynamic response of any glacier to earthquake shaking or avalanche loading was found in either the Chugach or Kenai Mountains 16 months after the 1964 earthquake, nor was there any evidence of surges (rapid advances) as postulated by the Earthquake-Advance Theory of Tarr and Martin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544D","usgsCitation":"Post, A., 1967, Effects of the March 1964 Alaska earthquake on glaciers: U.S. Geological Survey Professional Paper 544, vi, 42 p., https://doi.org/10.3133/pp544D.","productDescription":"vi, 42 p.","numberOfPages":"42","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":396002,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99035.htm"},{"id":277813,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544d/index.html"},{"id":65743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544d/pp544d_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544d/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.1279296875,\n              59.265880628258095\n            ],\n            [\n              -140.73486328125,\n              59.265880628258095\n            ],\n            [\n              -140.73486328125,\n              61.762728830472696\n            ],\n            [\n              -151.1279296875,\n              61.762728830472696\n            ],\n            [\n              -151.1279296875,\n              59.265880628258095\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61055d","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":220496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2356,"text":"wsp1846 - 1967 - Ground water in the vicinity of American Falls Reservoir, Idaho","interactions":[],"lastModifiedDate":"2013-11-21T14:50:07","indexId":"wsp1846","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1846","title":"Ground water in the vicinity of American Falls Reservoir, Idaho","docAbstract":"Analysis of ground- and surface-water relationships suggests that increasing\nthe capacity of the American Falls Reservoir by raising the height of the\ndam 15 feet would increase leakage from the reservoir by less than 0.2 percent\nof the average inflow to the reservoir, or less than 10,000 acre feet per year.\nThis amount is less than one-tenth of the evaporation rate from the reservoir.\nThe American Falls Reservoir lies near the south margin of the Snake\nRiver Plain in southeastern Idaho. The Snake River Plain is about 200 miles\nlong and averages nearly 60 miles in width. It is underlain by a thick sequence\nof basaltic lava flows, interbedded pyroclasties, and sedimentary deposits. The\nuppermost few thousand feet of this sequence is the Snake Plain aquifer, one of\nthe great aquifers of the United States.\nRecharge to the aquifer is chiefly by water percolating from the Snake River, its\ntributaries, and irrigated tracts, and by underflow from surrounding areas.\nGround water moves generally southwestward and discharges to the Snake River\nthrough springs in the American Falls Reservoir reach and in the Hagerman\nValley reach (between Twin Falls and Bliss). Total discharge from the aquifer\nis about 9,000 cfs (cubic feet per second).\nThe occurrence and movement of ground water in the viscinity of American\nFalls Reservoir are controlled by the local geology. Silt and tuff in the Neeley\nFormation and the Walcott Tuff and silt and fine sand in the FT ft Formation\nand American Falls Lake Beds have a low permeability. These rocks transmit\nlittle ground water compared with the basalt and intercalated pyroclasties and\ngravels of the Snake Plain aquifer. The less permeable deposits underlie the\nreservoir area and act as a barrier to the movement of ground water.\nUnder present conditions the water table on the periphery of the reservoir\nslopes toward the reservoir, except within 3 or 4 miles of the dam, where the\nwater table slopes away from the reservoir. Most of the springs discharge at\naltitudes above 4,370 feet, some 15 feet above the maximum reservoir stage.\nThus, reservoir stage has little effect on ground-water inflow to the reservoir.\nA fairly close relationship exists between the annual amount of surface water\ndiverted for irrigation of lands up the Snake River from the reservoir and the\nannual ground-water discharge through springs for the period 1911-60. After\nabout 1952, greatly increased ground-water withdrawals from wells, which increased\nconsumptive use, virtually balanced increased diversions from the surface-\nwater system for irrigation, so that ground-water inflow to the reservoir\nremained about constant.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1846","collaboration":"Prepared in cooperation with the U.S. Bureau of Reclamation","usgsCitation":"Mundorff, M.J., 1967, Ground water in the vicinity of American Falls Reservoir, Idaho: U.S. Geological Survey Water Supply Paper 1846, Report: iv, 58 p.; Plate 1: 15 inches x 12.39 inches; Plate 2: 39 inches x 29.85 inches; Plate 3: 30 inches x 18.71 inches; Plate 4: 27 inches x 18.24 inches; Plate 5: 39 inches x 29.87, https://doi.org/10.3133/wsp1846.","productDescription":"Report: iv, 58 p.; Plate 1: 15 inches x 12.39 inches; Plate 2: 39 inches x 29.85 inches; Plate 3: 30 inches x 18.71 inches; Plate 4: 27 inches x 18.24 inches; Plate 5: 39 inches x 29.87","costCenters":[],"links":[{"id":137784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1846/report-thumb.jpg"},{"id":28286,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28287,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28288,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28289,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28290,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1846/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"American Falls Reservoir","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d814","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32613,"text":"pp544C - 1967 - Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>","interactions":[],"lastModifiedDate":"2013-09-18T15:32:00","indexId":"pp544C","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"C","title":"Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>","docAbstract":"The Alaska earthquake of March 27, 1964, had widespread hydrologic effects throughout practically all of the United States. More than 1,450 water-level recorders, scattered throughout all the 50 States except Connecticut, Delaware, and Rhode Island, registered the earthquake. Half of the water-level records were obtained from ground-water observation wells and half at surface-water gaging stations. The earthquake is also known to have registered on water-level recorders on wells in Canada, England, Denmark, Belgium, Egypt, Israel, Libya, Philippine Islands, South-West Africa, South Africa, and Northern Territory of Australia. The Alaska earthquake is the first for which widespread surface-water effects are known. The effects were recorded at stations on flowing streams, rivers, reservoirs, lakes, and ponds. The 755 surface-water stations recording effects are spread through 38 States, but are most numerous in the south-central and southeastern States, especially in Florida and Louisiana. Most of the fluctuations recorded can be referred to more precisely as seismic seiches; however, a few stations recorded the quake as a minor change in stage. The largest recorded seiche outside Alaska was 1.83 feet on a reservoir in Michigan. The next largest was 1.45 feet on Lake Ouachita in Arkansas. The largest fluctuation in a well was 23 feet registered by a pressure recorder near Belle Fourche, S. Dak. Fluctuations of more than 10 feet were reported from wells in Alabama, Florida, Georgia, Illinois, Missouri, and Pennsylvania. A 3.40-foot fluctuation was recorded in a well in Puerto Rico. The Alaska earthquake was registered by about seven times as many water-level recorders as recorded the Hebgen Lake, Mont., earthquake of August 19, 1959.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544C","collaboration":"This report is Chapter C in <i>The Alaska earthquake, March 27, 1964: effects on hydrologic regimen</i>.  For more information, see: <a href=\"http://pubs.usgs.gov/pp/0544/index.html\" target=\"_blank\">Professional Paper 544</a>.","usgsCitation":"Vorhis, R.C., Rexin, E.E., and Coble, R.W., 1967, Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>: U.S. Geological Survey Professional Paper 544, p. C1-C54, https://doi.org/10.3133/pp544C.","productDescription":"p. C1-C54","numberOfPages":"54","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":119429,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544c/report-thumb.jpg"},{"id":60475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544c/pp544c_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277811,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544c/"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.014444444444444444,-90 ], [ -0.014444444444444444,0.0025 ], [ 0.01888888888888889,0.0025 ], [ 0.01888888888888889,-90 ], [ -0.014444444444444444,-90 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e4e","contributors":{"authors":[{"text":"Vorhis, Robert C.","contributorId":52555,"corporation":false,"usgs":true,"family":"Vorhis","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":208795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rexin, Elmer E.","contributorId":60110,"corporation":false,"usgs":true,"family":"Rexin","given":"Elmer","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208796,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coble, R. W.","contributorId":49380,"corporation":false,"usgs":true,"family":"Coble","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208794,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32663,"text":"pp524H - 1967 - Ash flows and related volcanic rocks associated with the Creede Caldera, San Juan Mountains, Colorado","interactions":[],"lastModifiedDate":"2025-04-15T17:49:48.497215","indexId":"pp524H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"524","chapter":"H","title":"Ash flows and related volcanic rocks associated with the Creede Caldera, San Juan Mountains, Colorado","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1965 (Professional Paper 524)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp524H","usgsCitation":"Ratte, J., and Steven, T.A., 1967, Ash flows and related volcanic rocks associated with the Creede Caldera, San Juan Mountains, Colorado: U.S. Geological Survey Professional Paper 524, Report: 58 p.; 1 Plate: 22.75 x 15.63 inches, https://doi.org/10.3133/pp524H.","productDescription":"Report: 58 p.; 1 Plate: 22.75 x 15.63 inches","costCenters":[],"links":[{"id":484608,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4561.htm","linkFileType":{"id":5,"text":"html"}},{"id":60562,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0524h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60561,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0524h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0524h/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Creede Caldera, San Juan Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.0833,\n              38\n            ],\n            [\n              -107.0833,\n              37.6667\n            ],\n            [\n              -106.6667,\n              37.6667\n            ],\n            [\n              -106.6667,\n              38\n            ],\n            [\n              -107.0833,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672be6","contributors":{"authors":[{"text":"Ratte, J.C.","contributorId":10416,"corporation":false,"usgs":true,"family":"Ratte","given":"J.C.","affiliations":[],"preferred":false,"id":208885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":208886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41335,"text":"ofr67165 - 1967 - Preliminary geologic map of Causey Dam quadrangle, Weber County, Utah","interactions":[{"subject":{"id":41335,"text":"ofr67165 - 1967 - Preliminary geologic map of Causey Dam quadrangle, Weber County, Utah","indexId":"ofr67165","publicationYear":"1967","noYear":false,"title":"Preliminary geologic map of Causey Dam quadrangle, Weber County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":62401,"text":"gq790 - 1969 - Geologic map of the Causey Dam quadrangle, Weber County, Utah","indexId":"gq790","publicationYear":"1969","noYear":false,"title":"Geologic map of the Causey Dam quadrangle, Weber County, Utah"},"id":1}],"supersededBy":{"id":62401,"text":"gq790 - 1969 - Geologic map of the Causey Dam quadrangle, Weber County, Utah","indexId":"gq790","publicationYear":"1969","noYear":false,"title":"Geologic map of the Causey Dam quadrangle, Weber County, Utah"},"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr67165","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-165","title":"Preliminary geologic map of Causey Dam quadrangle, Weber County, Utah","language":"ENGLISH","doi":"10.3133/ofr67165","usgsCitation":"Mullens, T.E., 1967, Preliminary geologic map of Causey Dam quadrangle, Weber County, Utah: U.S. Geological Survey Open-File Report 67-165, 1 map, https://doi.org/10.3133/ofr67165.","productDescription":"1 map","costCenters":[],"links":[{"id":106389,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8170.htm","linkFileType":{"id":5,"text":"html"},"description":"8170"},{"id":176311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c0dd","contributors":{"authors":[{"text":"Mullens, Thomas E.","contributorId":14817,"corporation":false,"usgs":true,"family":"Mullens","given":"Thomas","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224849,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32619,"text":"pp554D - 1967 - Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2018-11-08T07:33:18","indexId":"pp554D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"554","chapter":"D","title":"Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California","docAbstract":"Cenozoic volcanic rocks of the Devils Postpile quadrangle are of late Pliocene to Recent age and are divided into 11 map units. The suite is alkalic-calcic and ranges in composition from basalt to rhyolite. It includes a rhyolitic welded ash-flow tuff which is probably correlative with the Bishop Tuff, although the two units are geographically isolated by the Sierra Nevada drainage divide. The Devils Postpile itself is a classic example of columnar jointing in the lower part of a lava flow.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1966","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp554D","collaboration":"Prepared in cooperation with the California Division of Mines and Geology","usgsCitation":"Huber, N.K., and Rinehart, C.D., 1967, Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California: U.S. Geological Survey Professional Paper 554, p. D1-D21, https://doi.org/10.3133/pp554D.","productDescription":"p. D1-D21","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":60483,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0554d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60484,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0554d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0554d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6f58","contributors":{"authors":[{"text":"Huber, N. King","contributorId":51284,"corporation":false,"usgs":true,"family":"Huber","given":"N.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":208805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinehart, C. Dean","contributorId":88326,"corporation":false,"usgs":true,"family":"Rinehart","given":"C.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":208806,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61717,"text":"gq650 - 1967 - Geologic map of the Elkton quadrangle, Todd County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"gq650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"650","title":"Geologic map of the Elkton quadrangle, Todd County, Kentucky","language":"ENGLISH","doi":"10.3133/gq650","usgsCitation":"Shawe, F.R., 1967, Geologic map of the Elkton quadrangle, Todd County, Kentucky: U.S. Geological Survey Geologic Quadrangle 650, 1 map., https://doi.org/10.3133/gq650.","productDescription":"1 map.","costCenters":[],"links":[{"id":103374,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1960.htm","linkFileType":{"id":5,"text":"html"},"description":"1960"},{"id":248015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0650/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0650/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.25,36.75 ], [ -87.25,36.8675 ], [ -87.11749999999999,36.8675 ], [ -87.11749999999999,36.75 ], [ -87.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b57","contributors":{"authors":[{"text":"Shawe, Fred R.","contributorId":91516,"corporation":false,"usgs":true,"family":"Shawe","given":"Fred","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34102,"text":"b1230I - 1967 - Mineral resources of the High Uintas primitive area, Utah","interactions":[],"lastModifiedDate":"2025-04-07T20:52:50.432635","indexId":"b1230I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1230","chapter":"I","title":"Mineral resources of the High Uintas primitive area, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1230I","usgsCitation":"Crittenden, M.D., Wallace, C.A., and Sheridan, M., 1967, Mineral resources of the High Uintas primitive area, Utah: U.S. Geological Survey Bulletin 1230, 27 p, https://doi.org/10.3133/b1230I.","productDescription":"27 p","costCenters":[],"links":[{"id":62028,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1230i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1230i/report-thumb.jpg"},{"id":62027,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1230i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484301,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21309.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"High Uintas primitive area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.863,\n              40.874\n            ],\n            [\n              -110.863,\n              40.525\n            ],\n            [\n              -110.092,\n              40.525\n            ],\n            [\n              -110.092,\n              40.874\n            ],\n            [\n              -110.863,\n              40.874\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2c0","contributors":{"authors":[{"text":"Crittenden, Max D. Jr.","contributorId":28951,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":212458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, C. A.","contributorId":15596,"corporation":false,"usgs":true,"family":"Wallace","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":212456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sheridan, M.J.","contributorId":21608,"corporation":false,"usgs":true,"family":"Sheridan","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":212457,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}