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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i597","usgsCitation":"Scott, G., 1969, Geologic map of the Southwest and Southeast Pueblo quadrangles, Colorado: U.S. Geological Survey IMAP 597, HTML Document, https://doi.org/10.3133/i597.","productDescription":"HTML Document","costCenters":[],"links":[{"id":187574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106860,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9393.htm","linkFileType":{"id":5,"text":"html"},"description":"9393"}],"scale":"24000","country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.75,38.1175 ], [ -104.75,38.25 ], [ -104.5,38.25 ], [ -104.5,38.1175 ], [ -104.75,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b21c","contributors":{"authors":[{"text":"Scott, Glenn R.","contributorId":33324,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn R.","affiliations":[],"preferred":false,"id":275587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55952,"text":"ofr69280 - 1969 - Memorandum on the ground-water resources at Emerald Mound, Natchez Trace Parkway, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:12:19","indexId":"ofr69280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-280","title":"Memorandum on the ground-water resources at Emerald Mound, Natchez Trace Parkway, Mississippi","language":"ENGLISH","doi":"10.3133/ofr69280","usgsCitation":"Thomson, F., 1969, Memorandum on the ground-water resources at Emerald Mound, Natchez Trace Parkway, Mississippi: U.S. Geological Survey Open-File Report 69-280, 4 p., https://doi.org/10.3133/ofr69280.","productDescription":"4 p.","costCenters":[],"links":[{"id":184294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613f54","contributors":{"authors":[{"text":"Thomson, F.H.","contributorId":8132,"corporation":false,"usgs":true,"family":"Thomson","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":254549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55934,"text":"ofr69230 - 1969 - Summary of microearthquakes along the San Andreas fault system in central California, April to June 30, 1968","interactions":[],"lastModifiedDate":"2012-02-02T00:12:18","indexId":"ofr69230","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-230","title":"Summary of microearthquakes along the San Andreas fault system in central California, April to June 30, 1968","language":"ENGLISH","doi":"10.3133/ofr69230","usgsCitation":"Roller, J.C., Eaton, J.P., and Lee, W., 1969, Summary of microearthquakes along the San Andreas fault system in central California, April to June 30, 1968: U.S. Geological Survey Open-File Report 69-230, 24 p. (incl. 20 p. tables, 1 fig.), https://doi.org/10.3133/ofr69230.","productDescription":"24 p. (incl. 20 p. tables, 1 fig.)","costCenters":[],"links":[{"id":184487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699119","contributors":{"authors":[{"text":"Roller, John C.","contributorId":60642,"corporation":false,"usgs":true,"family":"Roller","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, Jerry P.","contributorId":22341,"corporation":false,"usgs":true,"family":"Eaton","given":"Jerry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":254518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, William Hung Kan","contributorId":83502,"corporation":false,"usgs":true,"family":"Lee","given":"William Hung Kan","affiliations":[],"preferred":false,"id":254520,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":55884,"text":"ofr694 - 1969 - Floods in Marengo South quadrangle, northeastern Illinois","interactions":[{"subject":{"id":55884,"text":"ofr694 - 1969 - Floods in Marengo South quadrangle, northeastern Illinois","indexId":"ofr694","publicationYear":"1969","noYear":false,"title":"Floods in Marengo South quadrangle, northeastern Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":68599,"text":"ha463 - 1972 - Floods in Marengo South Quadrangle, Northeastern Illinois","indexId":"ha463","publicationYear":"1972","noYear":false,"title":"Floods in Marengo South Quadrangle, Northeastern Illinois"},"id":1}],"supersededBy":{"id":68599,"text":"ha463 - 1972 - Floods in Marengo South Quadrangle, Northeastern Illinois","indexId":"ha463","publicationYear":"1972","noYear":false,"title":"Floods in Marengo South Quadrangle, Northeastern Illinois"},"lastModifiedDate":"2012-02-02T00:12:01","indexId":"ofr694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-4","title":"Floods in Marengo South quadrangle, northeastern Illinois","language":"ENGLISH","doi":"10.3133/ofr694","usgsCitation":"Allen, H., 1969, Floods in Marengo South quadrangle, northeastern Illinois: U.S. Geological Survey Open-File Report 69-4, 10 p., 16 figs., https://doi.org/10.3133/ofr694.","productDescription":"10 p., 16 figs.","costCenters":[],"links":[{"id":182229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e64e3","contributors":{"authors":[{"text":"Allen, H.E.","contributorId":40272,"corporation":false,"usgs":true,"family":"Allen","given":"H.E.","affiliations":[],"preferred":false,"id":254414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13721,"text":"ofr69102 - 1969 - Preliminary report on the engineering geology of the Eldorado Springs quadrangle, Boulder and Jefferson Counties, Colorado","interactions":[],"lastModifiedDate":"2025-07-28T16:39:44.944153","indexId":"ofr69102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-102","title":"Preliminary report on the engineering geology of the Eldorado Springs quadrangle, Boulder and Jefferson Counties, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69102","usgsCitation":"Gardner, M.E., 1969, Preliminary report on the engineering geology of the Eldorado Springs quadrangle, Boulder and Jefferson Counties, Colorado: U.S. Geological Survey Open-File Report 69-102, Report: 9 p.; 5 Plates: 18.15 x 33.68 inches or smaller, https://doi.org/10.3133/ofr69102.","productDescription":"Report: 9 p.; 5 Plates: 18.15 x 33.68 inches or smaller","costCenters":[],"links":[{"id":493027,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8354.htm","linkFileType":{"id":5,"text":"html"}},{"id":42286,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0102/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42285,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0102/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42290,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42289,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0102/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42288,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0102/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42287,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0102/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147285,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0102/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Boulder County, Jefferson County","otherGeospatial":"Eldorado Springs quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.25,\n 40\n ],\n [\n -105.375,\n 40\n ],\n [\n -105.375,\n 39.875\n ],\n [\n -105.25,\n 39.875\n ],\n [\n -105.25,\n 40\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c931","contributors":{"authors":[{"text":"Gardner, Maxwell E.","contributorId":55016,"corporation":false,"usgs":true,"family":"Gardner","given":"Maxwell","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55914,"text":"ofr69173 - 1969 - Water temperatures in the Columbia River basin, water year 1968","interactions":[{"subject":{"id":55914,"text":"ofr69173 - 1969 - Water temperatures in the Columbia River basin, water year 1968","indexId":"ofr69173","publicationYear":"1969","noYear":false,"title":"Water temperatures in the Columbia River basin, water year 1968"},"predicate":"SUPERSEDED_BY","object":{"id":3632,"text":"cir551 - 1968 - Water temperatures in the lower Columbia River","indexId":"cir551","publicationYear":"1968","noYear":false,"title":"Water temperatures in the lower Columbia River"},"id":1}],"supersededBy":{"id":3632,"text":"cir551 - 1968 - Water temperatures in the lower Columbia River","indexId":"cir551","publicationYear":"1968","noYear":false,"title":"Water temperatures in the lower Columbia River"},"lastModifiedDate":"2012-02-02T00:12:20","indexId":"ofr69173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-173","title":"Water temperatures in the Columbia River basin, water year 1968","language":"ENGLISH","doi":"10.3133/ofr69173","usgsCitation":"Moore, A., 1969, Water temperatures in the Columbia River basin, water year 1968: U.S. Geological Survey Open-File Report 69-173, 17 p., 18 figs., https://doi.org/10.3133/ofr69173.","productDescription":"17 p., 18 figs.","costCenters":[],"links":[{"id":184506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f00a3","contributors":{"authors":[{"text":"Moore, A.M.","contributorId":87909,"corporation":false,"usgs":true,"family":"Moore","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":254466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17964,"text":"ofr699 - 1969 - Preliminary geologic interpretation of aeromagnetic data in the Nixon Fork district, Alaska","interactions":[{"subject":{"id":17964,"text":"ofr699 - 1969 - Preliminary geologic interpretation of aeromagnetic data in the Nixon Fork district, Alaska","indexId":"ofr699","publicationYear":"1969","noYear":false,"title":"Preliminary geologic interpretation of aeromagnetic data in the Nixon Fork district, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":39568,"text":"pp700D - 1970 - Geological Survey research 1970, Chapter D","indexId":"pp700D","publicationYear":"1970","noYear":false,"chapter":"D","title":"Geological Survey research 1970, Chapter D"},"id":1}],"supersededBy":{"id":39568,"text":"pp700D - 1970 - Geological Survey research 1970, Chapter D","indexId":"pp700D","publicationYear":"1970","noYear":false,"title":"Geological Survey research 1970, Chapter D"},"lastModifiedDate":"2024-01-17T19:39:16.691625","indexId":"ofr699","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-9","title":"Preliminary geologic interpretation of aeromagnetic data in the Nixon Fork district, Alaska","docAbstract":"An aeromagnetic map covering 480 square miles was compiled for the Nixon Fork district, which is located approximately 35 miles northeast of McGrath, Alaska. The survey was flown in search of concealed intrusive rocks which may have produced contact metamorphic deposits in limestone similar to the known lode deposits which have been the principal source of gold in the district.
The exposed quartz monzonite stocks with which the lode deposits are associated produce negative magnetic anomalies. Slight to moderately strong positive anomalies correlate with granitic intrusives in contact with Upper Cretaceous rocks in the Iditarod-Nixon Fork fault zone. No significant mineral deposits have been found in conjunction with these granitic bodies.
Positive anomalies, delineating buried intrusives, occur near the east and west boundaries of the mapped area. The nature of the westernmost intrusive is unknown.
An area of possible economic interest lies between Limestone Mountain and Whirlwind-Canyon Creeks in the eastern sector of the mapped area. An elliptical positive anomaly is superimposed on an elongate, slightly negative anomaly. This negative anomaly may represent an intrusive similar to the quartz monzonite with which the lode deposits are affiliated. The positive anomaly may be a near-vertical mafic dike intruded to within 50 feet of the surface of a limestone ridge. Limestone in the vicinity of the dike may be a favorable area for prospecting for lode deposits similar to the known gold-producing deposits of the district.
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A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":254468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Singer, J.A.","contributorId":16097,"corporation":false,"usgs":true,"family":"Singer","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":254467,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38798,"text":"pp562C - 1969 - The behavior of large particles falling in quiescent liquids","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp562C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"562","chapter":"C","title":"The behavior of large particles falling in quiescent liquids","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sediment transport in alluvial channels","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp562C","usgsCitation":"Stringham, G., Simons, D., and Guy, H., 1969, The behavior of large particles falling in quiescent liquids: U.S. Geological Survey Professional Paper 562, p. 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C1-C36","costCenters":[],"links":[{"id":120533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0562c/report-thumb.jpg"},{"id":65674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0562c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696eb","contributors":{"authors":[{"text":"Stringham, G.E.","contributorId":50405,"corporation":false,"usgs":true,"family":"Stringham","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":220461,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, D.B.","contributorId":50501,"corporation":false,"usgs":true,"family":"Simons","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":220462,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guy, H.P.","contributorId":73571,"corporation":false,"usgs":true,"family":"Guy","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":220463,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38817,"text":"pp543I - 1969 - Tectonics of the March 27, 1964, Alaska earthquake","interactions":[{"subject":{"id":38817,"text":"pp543I - 1969 - Tectonics of the March 27, 1964, Alaska earthquake","indexId":"pp543I","publicationYear":"1969","noYear":false,"chapter":"I","title":"Tectonics of the March 27, 1964, Alaska 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":"2022-06-28T18:18:07.763935","indexId":"pp543I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"I","title":"Tectonics of the March 27, 1964, Alaska earthquake","docAbstract":"The March 27, 1964, earthquake was accomp anied by crustal deformation-including warping, horizontal distortion, and faulting-over probably more than 110,000 square miles of land and sea bottom in south-central Alaska. Regional uplift and subsidence occurred mainly in two nearly parallel elongate zones, together about 600 miles long and as much as 250 miles wide, that lie along the continental margin. From the earthquake epicenter in northern Prince William Sound, the deformation extends eastward 190 miles almost to long 142° and southwestward slightly more than 400 miles to about long 155°. It extends across the two zones from the chain of active volcanoes in the Aleutian Range and Wrangell Mountains probably to the Aleutian Trench axis.\n\nUplift that averages 6 feet over broad areas occurred mainly along the coast of the Gulf of Alaska, on the adjacent Continental Shelf, and probably on the continental slope. This uplift attained a measured maximum on land of 38 feet in a northwest-trending narrow belt less than 10 miles wide that is exposed on Montague Island in southwestern Prince William Sound. Two earthquake faults exposed on Montague Island are subsidiary northwest-dipping reverse faults along which the northwest blocks were relatively displaced a maximum of 26 feet, and both blocks were upthrown relative to sea level. From Montague Island, the faults and related belt of maximum uplift may extend southwestward on the Continental Shelf to the vicinity of the Kodiak group of islands. To the north and northwest of the zone of uplift, subsidence forms a broad asymmetrical downwarp centered over the Kodiak-Kenai-Chugach Mountains that averages 2½ feet and attains a measured maximum of 7½ feet along the southwest coast of the Kenai Peninsula. Maximum indicated uplift in the Alaska and Aleutian Ranges to the north of the zone of subsidence was l½ feet. Retriangulation over roughly 25,000 square miles of the deformed region in and around Prince William Sound shows that vertical movements there were accompanied by horizontal distortion, involving systematic shifts of about 64 feet in a relative seaward direction. Comparable horizontal movements are presumed to have affected those parts of the major zones of uplift and subsidence for which retriangulation data are unavailable.\n\nRegional vertical deformation generated a train of destructive long-period seismic sea waves in the Gulf of Alaska as well as unique atmospheric and ionospheric disturbances that were recorded at points far distant from Alaska. Warping resulted in permanent tilt of larger lake basins and temporary reductions in discharge of some major rivers. Uplift and subsidence relative to sea level caused profound modifications in shoreline morphology with attendant catastrophic effects on the nearshore biota and costly damage to coasta1 installations. Systematic horizontal movements of the land relative to bodies of confined or semiconfined water may have caused unexplained short-period waves—some of which were highly destructive—observed during or immediately after the earthquake at certain coastal localities and in Kenai Lake. Porosity increases, probably related to horizontal displacements in the zone of subsidence, were reflected in lowered well-water levels and in losses of surface water.\n\nThe primary fault, or zone of faults, along which the earthquake occurred is not exposed at the surface on land. Focal-mechanism studies, when considered in conjunction with the pattern of deformation and seismicity, suggest that it was a complex thrust fault (megathrust) dipping at a gentle angle beneath the continental margin from the vicinity of the Aleutian Trench. Movement on the megathrust was accompanied by subsidiary reverse faulting, and perhaps wrench faulting, within the upper plate. Aftershock distribution suggests movement on a segment of the megathrust, some 550–600 miles long and 110–180 miles wide, that underlies most of the major zone of uplift and the seaward part of the major zone of subsidence.\n\nAccording to the postulated model, the observed and inferred tectonic displacements that accompanied the earthquake resulted primarily from (1) relative seaward displacement and uplift of the seaward part of the block by movement along the dipping megathrust and subsidiary faults that break through the upper plate to the surface, and (2) simultaneous elastic horizontal extension and vertical attenuation (subsidence) of the crustal slab behind the upper plate. Slight uplift inland from the major zones of deformation presumably was related to elastic strain changes resulting from the overthrusting; however, the data are insufficient to permit conclusions regarding its cause.\n\nThe belt of seismic activity and major zones of tectonic deformation associated with the 1964 earthquake, to a large extent, lie between and parallel to the Aleutian Volcanic Arc and the Aleutian Trench, and are probably genetically related to the arc. Geologic data indicate that the earthquake-related tectonic movements were but the most recent pulse in an episode of deformation that probably began in late Pleistocene time and has continued intermittently to the present. Evidence for progressive coastal submergence in the deformed region for several centuries preceding the earthquake, in combin1ation with transverse horizontal shortening indicated by the retriangulation data, suggests pre-earthquake strain directed at a gentle angle downward beneath the arc. The duration of strain accumulation in the epicentral region, as interpreted from the time interval during which the coastal submergence occurred, probably is 930–1,360 years.","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/pp543I","usgsCitation":"Plafker, G., 1969, Tectonics of the March 27, 1964, Alaska earthquake: U.S. Geological Survey Professional Paper 543, Report: viii, 74 p.; 2 Plates: 27.08 x 21.87 inches and 16.09 x 20.66 inches, https://doi.org/10.3133/pp543I.","productDescription":"Report: viii, 74 p.; 2 Plates: 27.08 x 21.87 inches and 16.09 x 20.66 inches","numberOfPages":"88","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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