{"pageNumber":"403","pageRowStart":"10050","pageSize":"25","recordCount":11370,"records":[{"id":38819,"text":"pp544A - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","interactions":[{"subject":{"id":38819,"text":"pp544A - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","indexId":"pp544A","publicationYear":"1966","noYear":false,"chapter":"A","title":"Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska"},"predicate":"IS_PART_OF","object":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"id":1}],"isPartOf":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"lastModifiedDate":"2022-02-15T20:52:49.535943","indexId":"pp544A","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","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":"A","title":"Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","docAbstract":"The earthquake of March 27, 1964, greatly affected the hydrology of Alaska and many other parts of the world. Its far-reaching effects were recorded as water-level fluctuations in gages operated on water wells and streams. The close-in effects were even more striking, however; sediment-laden ground water erupted at the surface, and even ice-covered lakes and streams responded by seiching. Lake and river ice was broken for distances of 450 miles from the epicenter by seismic shock and seiche action. The surging action temporarily dewatered some lakes. Fissuring of streambeds and lakeshores, in particular, caused a loss of water, and hydrologic recovery took weeks in some places. Landslides and snow avalanches temporarily blocked streams and diverted some permanently. The only stream or lake structures damaged were a tunnel intake and two earthen dams. The winter conditions-low stages of water and the extensive ice cover on lakes and streams-at the time of the earthquake greatly reduced the damaging potential. Ground water was drastically affected mostly in unconsolidated aquifers for at least 160 miles from the epicenter. Within 100 miles of the epicenter, vast quantities of sediment-laden water were ejected in most of the flood plains of the glaciofluvial valleys. A shallow water table and confinement by frost seemed to be requirements for the ejections, which were commonly associated with cratering and subsidence of the unconsolidated material. Subsidence was also common near the disastrous submarine landslides, and was probably caused by loss of water pressure and by lateral spreading of sediments. Effects on ground water in bedrock were not determinable because of lack of data and accessibility, particularly within 50 miles of the epicenter. Deep aquifers in unconsolidated sediments, which in most areas are under high hydrostatic pressure, were also greatly affected. Postearthquake water levels for a year were compared with long-term prequake levels to show permanent changes in an aquifer system. At Anchorage and in parts of the kenai Peninsula, artesian-pressure levels dropped as much as 15 feet. These lower pressures were probably caused either by grain rearrangement which increased the porosity within the aquifer or by a displacement of material that allowed water to discharge more freely at the submarine terminus of the aquifer. Seismically induced pressure on ground water was instrumental in causing most of the disastrous slides. Water quality was not changed except for temporary increases in turbidity in wells and streams. The sediment load in streams during the April spring run-off appeared to be greatly increased over previous years.","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/pp544A","usgsCitation":"Waller, R., 1966, Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska: U.S. Geological Survey Professional Paper 544, 28 p., https://doi.org/10.3133/pp544A.","productDescription":"28 p.","numberOfPages":"28","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":32612,"text":"pp544B - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","interactions":[{"subject":{"id":32612,"text":"pp544B - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","indexId":"pp544B","publicationYear":"1966","noYear":false,"chapter":"B","title":"Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"id":1}],"isPartOf":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"lastModifiedDate":"2022-01-31T21:02:54.236706","indexId":"pp544B","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","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":"B","title":"Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","docAbstract":"The Anchorage hydrologic system was greatly affected by the seismic shock. Immediate but temporary effects included increased stream discharge, seiche action on lakes, and fluctuations in ground-water levels. Generally, ground-water levels were residually lowered after the initial period of fluctuation. This lowering is attributed either to changes in the discharge zones offshore or to a change in the permeability of the aquifers by seismically induced strain. Water supplies were disrupted temporarily by snowslides on streams and by sanding or turbidity in wells. Salt-water encroachment to wells on Fire Island seems to have increased. The approximate 3.7-foot lowering of land level and the diminished artesian head may permit further salt-water encroachment. Increased pore pressure in the Pleistocene Bootlegger Cove Clay led to liquefaction in silt and sand lenses that contributed to the disastrous bluff landslides. Measurements after the earthquake indicate that most pore pressures are declining, whereas some remain high or are increasing. Subsidence in the area was caused principally by tectonic readjustment, but differential compaction within the Bootlegger Cove Clay contributed to subsidences estimated to be as much as 0.6 foot beneath Anchorage.","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/pp544B","usgsCitation":"Waller, R., 1966, Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska: U.S. Geological Survey Professional Paper 544, Report: 18 p.; 1 Plate: 37.13 x 41.12 inches, https://doi.org/10.3133/pp544B.","productDescription":"Report: 18 p.; 1 Plate: 37.13 x 41.12 inches","numberOfPages":"18","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":119428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544b/report-thumb.jpg"},{"id":277808,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544b/pp544b_text.pdf"},{"id":277809,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0544b/pp544b_plate1.pdf"},{"id":277810,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544b/index.html"},{"id":395185,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4594.htm"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.2863,60.7338 ], [ -150.2863,61.4839 ], [ -148.46,61.4839 ], [ -148.46,60.7338 ], [ -150.2863,60.7338 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c890","contributors":{"authors":[{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":208793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32677,"text":"pp542D - 1966 - Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","interactions":[{"subject":{"id":32677,"text":"pp542D - 1966 - Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","indexId":"pp542D","publicationYear":"1966","noYear":false,"chapter":"D","title":"Effects of the earthquake of March 27, 1964, in the Homer area, 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":"2022-06-06T20:19:16.156352","indexId":"pp542D","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","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":"D","title":"Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","docAbstract":"<p>The March 27, 1964, earthquake shook the Homer area for about 3 minutes. Land effects consisted of a 2- to 6-foot subsidence of the mainland and Homer Spit, one earthflow at the mouth of a canyon, several landslides on the Homer escarpment and along the sea bluffs, and minor fissuring of the ground, principally at the edges of bluffs and on Homer Spit. Hydrologic effects consisted of at least one and possibly two submarine landslides at the end of the spit, seiche waves in Kachemak Bay, ice breakage on Beluga Lake, sanding of wells, and a temporary loss of water in some wells.</p>\n</br>\n<p>Seismic damage to the community was light in comparison with that of other communities closer to the epicenter. One submarine landslide, however, took out most of the harbor breakwater. The greatest damage was due to the subsidence of the spit, both tectonically (2–3 ft) and by differential compaction or lateral spreading (an additional 1–4 ft). Higher tides now flood much of the spit. The harbor and dock had to be replaced, and buildings on the end of the spit had to be elevated. Protection works for other buildings and the highway were needed. These works included application of fill to raise the highway and parts of the spit above high tides. Reconstruction costs and disaster loans totaled about $2½ million, but this amount includes added improvement costs over preexisting values.</p>\n</br>\n<p>Homer Spit in particular and the Homer area in general rank as areas where precautions must be taken in selecting building sites. The hazards of landslides, earthflows, compaction and submarine slumping—all of which might be triggered by an earthquake—should be considered in site selection.</p>\n</br>\n<p>In plan, Homer Spit resembles a scimitar with its curving blade pointed seaward. It is about 4 miles long and as much as 1,500 feet wide. The spit is composed largely of gravel intermixed with some sand.</p>\n</br>\n<p>After the earthquake and the resulting tectonic subsidence and compaction, much of the spit was below high-tide levels and consequently flooded periodically. The entire beach face has retreated. Much of the material eroded from the beach has been redeposited to form a new storm or frontal berm, locally migrating around buildings and covering roads. Beach recession of 10–15 feet is probably the overall average; maximum recession 1 year after the earthquake was 56 feet along one limited section of the distal end of the spit.</p>\n</br>\n<p>Subsidence of the mainland has caused accelerated erosion of the beaches and headlands that have been—and are—source areas for the material deposited on Homer Spit. The resulting increased supply of gravel and sand probably will cause the spit to widen gradually on the Cook Inlet side. Similarly, the new frontal berm will probably grow to a height sufficient to prevent overtopping by all but the larger storm swashes. The nature of shore processes on the spit has not been materially altered by subsidence, but the rates of erosion and deposition have been accelerated. The lasting effect of subsidence (excluding flooding) will be enlargement of the beach on the Cook Inlet side and gradual wasting of the beach on the bay side of the spit.</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/pp542D","usgsCitation":"Waller, R., and Stanley, K.W., 1966, Effects of the earthquake of March 27, 1964, in the Homer area, Alaska: U.S. Geological Survey Professional Paper 542, Report: vi, 28 p.; Plate: 18.00 × 18.83 inches, https://doi.org/10.3133/pp542D.","productDescription":"Report: vi, 28 p.; Plate: 18.00 × 18.83 inches","numberOfPages":"36","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":32676,"text":"pp542C - 1966 - Effects of the earthquake of March 27, 1964, at Valdez, Alaska","interactions":[{"subject":{"id":32676,"text":"pp542C - 1966 - Effects of the earthquake of March 27, 1964, at Valdez, Alaska","indexId":"pp542C","publicationYear":"1966","noYear":false,"chapter":"C","title":"Effects of the earthquake of March 27, 1964, at Valdez, 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":"2022-04-28T19:29:26.11427","indexId":"pp542C","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","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":"C","title":"Effects of the earthquake of March 27, 1964, at Valdez, Alaska","docAbstract":"<p>Valdez is situated on the seaward edge of a large outwash delta composed of a thick section of saturated silty sand and gravel. The earthquake of March 27, 1964, triggered a massive submarine slide, involving approximately 98 million cubic yards of material that destroyed the harbor facilities and nearshore installations. Waves generated by the slide and subsequent strong seiches did additional damage in the downtown area. Stresses generated by the seismic shocks and the slide developed an extensive system of fissures throughout the unconsolidated deposits at the head of the fiord. These fissures plus the shocks caused structural damage to many of the buildings in Valdez and destroyed the sewer and water systems. Removal of support from the face of the delta by submarine sliding allowed some of the material to move seaward and caused parts of the shore area to subside below high-tide level.</p>\n</br>\n<p>A site for relocating the town of Valdez has been designated. It is situated on the Mineral Creek fan--an area underlain by coarse alluvial gravel. This relocation site is protected from sea waves by a series of bedrock ridges and islands that also provide a resistant buttress retaining and protecting the toe of the fan from danger of sliding or slumping. The absence of evidence of ground breakage on the Mineral Creek fan indicates that the coarse subsoils at the relocation site react favorably under seismic conditions.</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/pp542C","usgsCitation":"Coulter, H.W., and Migliaccio, R.R., 1966, Effects of the earthquake of March 27, 1964, at Valdez, Alaska: U.S. Geological Survey Professional Paper 542, Report: viii, 36 p.; 3 Plates: 38.5 x 23.76 inches or smaller, https://doi.org/10.3133/pp542C.","productDescription":"Report: viii, 36 p.; 3 Plates: 38.5 x 23.76 inches or smaller","numberOfPages":"46","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":6254,"text":"pp539 - 1966 - Potential effects of Project Chariot on local water supplies, northwestern Alaska","interactions":[{"subject":{"id":52268,"text":"ofr62103 - 1962 - Potential effects of Project Chariot on local water supplies","indexId":"ofr62103","publicationYear":"1962","noYear":false,"title":"Potential effects of Project Chariot on local water supplies"},"predicate":"SUPERSEDED_BY","object":{"id":6254,"text":"pp539 - 1966 - Potential effects of Project Chariot on local water supplies, northwestern Alaska","indexId":"pp539","publicationYear":"1966","noYear":false,"title":"Potential effects of Project Chariot on local water supplies, northwestern Alaska"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp539","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"539","title":"Potential effects of Project Chariot on local water supplies, northwestern Alaska","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp539","usgsCitation":"Piper, A., 1966, Potential effects of Project Chariot on local water supplies, northwestern Alaska: U.S. Geological Survey Professional Paper 539, 45 p., https://doi.org/10.3133/pp539.","productDescription":"45 p.","costCenters":[],"links":[{"id":121622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0539/report-thumb.jpg"},{"id":33475,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0539/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33476,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0539/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683941","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":152389,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33689,"text":"b1202C - 1966 - Geology and coal resources of the Beluga-Yentna region, Alaska","interactions":[{"subject":{"id":12560,"text":"ofr555 - 1955 - Notes on a coal deposit on the Beluga River, Alaska","indexId":"ofr555","publicationYear":"1955","noYear":false,"title":"Notes on a coal deposit on the Beluga River, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":33689,"text":"b1202C - 1966 - Geology and coal resources of the Beluga-Yentna region, Alaska","indexId":"b1202C","publicationYear":"1966","noYear":false,"chapter":"C","title":"Geology and coal resources of the Beluga-Yentna region, Alaska"},"id":1}],"lastModifiedDate":"2023-03-08T21:17:48.005337","indexId":"b1202C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1202","chapter":"C","title":"Geology and coal resources of the Beluga-Yentna region, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1202C","usgsCitation":"Barnes, F.F., 1966, Geology and coal resources of the Beluga-Yentna region, Alaska: U.S. Geological Survey Bulletin 1202, Report: iv, 54 p.; 7 Plates: 23.50 x 35.00 inches or smaller, https://doi.org/10.3133/b1202C.","productDescription":"Report: iv, 54 p.; 7 Plates: 23.50 x 35.00 inches or smaller","costCenters":[],"links":[{"id":61583,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61582,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61581,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61580,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109501,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20994.htm","linkFileType":{"id":5,"text":"html"},"description":"20994"},{"id":61584,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61579,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61578,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61585,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1202c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163963,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1202c/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beluga-Yentna region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -152.154,\n              61\n            ],\n            [\n              -150.25,\n              61\n            ],\n            [\n              -150.25,\n              62.721\n            ],\n            [\n              -152.154,\n              62.721\n            ],\n            [\n              -152.154,\n              61\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686335","contributors":{"authors":[{"text":"Barnes, Farrell F.","contributorId":58624,"corporation":false,"usgs":true,"family":"Barnes","given":"Farrell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":211782,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32611,"text":"pp543C - 1966 - Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska","interactions":[{"subject":{"id":32611,"text":"pp543C - 1966 - Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska","indexId":"pp543C","publicationYear":"1966","noYear":false,"chapter":"C","title":"Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska"},"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":"2022-02-18T20:09:59.377159","indexId":"pp543C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"C","title":"Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska","docAbstract":"Sedimentary and volcanic rocks of Mesozoic and early Tertiary age form a roughly arcuate pattern in and around Prince William Sound, the epicentral region of the Alaska earthquake of 1964. These rocks include the Valdez Group, a predominantly slate and graywacke sequence of Jurassic and Cretaceous age, and the Orca Group, a younger sequence of early Tertiary age. The Orca consists of a lower unit of dense-average 2.87 g per cm<sup>3</sup> (grams per cubic centimeter) pillow basalt and greenstone intercalated with sedimentary rocks and an upper unit of lithologically variable sandstone interbedded with siltstone or argillite. Densities of the clastic rocks in both the Valdez and Orca Groups average about 2.69 g per cm<sup>3</sup>. Granitic rocks of relatively low density (2.62 g per cm<sup>3</sup>) cut the Valdez and Orca Groups at several localities.\n\nBoth the Valdez and the Orca Groups were complexly folded and extensively faulted during at least three major episodes of deformation: an early period of Cretaceous or early Tertiary orogeny, a second orogeny that probably culminated in late Eocene or early Oligocene time and was accompanied or closely followed by emplacement of granitic batholiths, and a third episode of deformation that began in late Cenozoic time and continued intermittently to the present.\n\nAbout 500 gravity stations were established in the Prince William Sound region in conjunction with postearthquake geologic investigations. Simple Bouguer anomaly contours trend approximately parallel to the arcuate geologic structure around the sound. Bouguer anomalies decrease northward from +40 mgal (milligals) at the southwestern end of Montague Island to -70 mgal at College and Harriman Fiords. Most of this change may be interpreted as a regional gradient caused by thickening of the continental crust. Superimposed on the gradient is a prominent gravity high of as much as 65 mgal that extends from Elrington Island on the southwest, across Knight and Glacier Islands to the Ellamar Peninsula and Valdez on the northeast. This high coincides with the wide belt of greenstone and pillow basalt of the Orca Group and largely reflects the high density of these volcanic rocks. A large low in the east-central part of the sound is inferred to have a composite origin, and results from the combined effects of low-density sedimentary and granitic rocks.\n\nThe Prince William Sound gravity high extends southwest-northeast without major horizontal offset for more than 100 miles. Thus the belt of volcanic rocks causing the high constitutes a major virtually continuous, geologic element of south-central Alaska.","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/pp543C","usgsCitation":"Case, J.E., Barnes, D., Plafker, G., and Robbins, S.L., 1966, Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska: U.S. Geological Survey Professional Paper 543, v, 12 p., https://doi.org/10.3133/pp543C.","productDescription":"v, 12 p.","numberOfPages":"20","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":396179,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99028.htm"},{"id":277724,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543c/index.html"},{"id":122514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543c/report-thumb.jpg"},{"id":60474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543c/pp543c_text.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Prince William Sound","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.1772,59.6961 ], [ -149.1772,61.3614 ], [ -145.3767,61.3614 ], [ -145.3767,59.6961 ], [ -149.1772,59.6961 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672061","contributors":{"authors":[{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, D.F.","contributorId":48960,"corporation":false,"usgs":true,"family":"Barnes","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":208790,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":208789,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208791,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":15595,"text":"ofr66108 - 1966 - Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","interactions":[{"subject":{"id":18667,"text":"ofr_66108_1965 - 1965 - Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","indexId":"ofr_66108_1965","publicationYear":"1965","noYear":false,"title":"Results of stream-sediment sampling in the Iliamna quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":15595,"text":"ofr66108 - 1966 - Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","indexId":"ofr66108","publicationYear":"1966","noYear":false,"title":"Results of stream-sediment sampling in the Iliamna quadrangle, Alaska"},"id":1}],"lastModifiedDate":"2022-02-07T22:40:12.264047","indexId":"ofr66108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-108","title":"Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr66108","usgsCitation":"Reed, B.L., and Detterman, R.L., 1966, Results of stream-sediment sampling in the Iliamna quadrangle, Alaska (Revised edition): U.S. Geological Survey Open-File Report 66-108, Report: 4 p.; 2 Plates: 23.78 × 17.35 inches and 13.79 × 17.47 inches, https://doi.org/10.3133/ofr66108.","productDescription":"Report: 4 p.; 2 Plates: 23.78 × 17.35 inches and 13.79 × 17.47 inches","costCenters":[],"links":[{"id":44563,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0108/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44562,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0108/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":106366,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8120.htm","linkFileType":{"id":5,"text":"html"},"description":"8120"},{"id":44561,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0108/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0108/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Iliamna quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -154.783,\n              59.142\n            ],\n            [\n              -153.4,\n              59.142\n            ],\n            [\n              -153.4,\n              60\n            ],\n            [\n              -154.783,\n              60\n            ],\n            [\n              -154.783,\n              59.142\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Revised edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605669","contributors":{"authors":[{"text":"Reed, Bruce L.","contributorId":19928,"corporation":false,"usgs":true,"family":"Reed","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","interactions":[{"subject":{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","indexId":"pp543A","publicationYear":"1966","noYear":false,"chapter":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska"},"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":"2022-06-28T19:38:48.241938","indexId":"pp543A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","docAbstract":"The March 27, 1964, earthquake dislodged slides from nine deltas in Kenai Lake, south-central Alaska. Sliding removed protruding parts of deltas-often the youngest parts-and steepened delta fronts, increasing the chances of further sliding. Fathograms show that debris from large slides spread widely over the lake floor, some reaching the toe of the opposite shore; at one place debris traveled 5,000 feet over the horizontal lake floor.\n\nSlides generated two kinds of local waves: a backfill and far-shore wave. Backfill waves were formed by water that rushed toward the delta to fill the void left by the sinking slide mass, overtopped the slide scrap, and came ashore over the delta. Some backfill waves had runup heights of 30 feet and ran inland more than 300 feet, uprooting and breaking off large trees. Far-shore waves hit the shore opposite the slides. They were formed by slide debris that crossed the lake floor and forced water ahead of it, which then ran up the opposite slope, burst above the lake surface, and struck the shore. One far-shore wave had a runup height of 72 feet.\n\nKenai Lake was tilted and seiched; a power spectrum analysis of a limnogram shows a wave having the period of the calculated uninodal seiche (36 minutes) and several shorter period waves. In constricted and shallow reaches, waves caused by seiching had 20- and 30-foot runup heights.\n\nDeep lateral spreading of sediments toward delta margins displaced deeply driven railroad-bridge piles, and set up stress fields in the surface sediments which resulted in the formation of many shear and some tension fractures on the surface of two deltas.","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/pp543A","usgsCitation":"McCulloch, D.S., 1966, Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska: U.S. Geological Survey Professional Paper 543, Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches, https://doi.org/10.3133/pp543A.","productDescription":"Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches","numberOfPages":"49","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":402630,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4590.htm","linkFileType":{"id":5,"text":"html"}},{"id":277653,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543a/index.html"},{"id":60502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60501,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543a/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kenai Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.835071,60.335719 ], [ -149.835071,60.494895 ], [ -149.346197,60.494895 ], [ -149.346197,60.335719 ], [ -149.835071,60.335719 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee60a","contributors":{"authors":[{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":208818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1796,"text":"wsp1838 - 1966 - Reservoirs in the United States","interactions":[],"lastModifiedDate":"2017-09-06T15:39:02","indexId":"wsp1838","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1838","title":"Reservoirs in the United States","docAbstract":"<p>This report summarizes the storage capacities and related data of reservoirs and controlled natural lakes for the contermimous United States, Alaska, Hawaii, and the Commonwealth of Puerto Rico. Data are given for all storage facilities having a usable capacity of 5,000 acre-feet or more and completed or under construction as of Jan 1, 1963.</p><p>A descriptive list of reservoirs m the United States completed as of Jan 1, 1947, was first published (Geol Survey Circular 23) in March 1948. In 1956 Water-Supply Paper 1360-A, \"Reservoirs m the United States,\" by N.O. Thomas and G.E. Harbeck, Jr, updated this listing and included lists of reservoirs completed or under construction as of Jan 1, 1954. Some of the data shown for reservoirs constructed before 1954 may have been corrected here on the basis of the latest available reservoir survey.</p><p>This report lists 1562 reservoirs and lakes, their usable storage totals 359,360,000 acre-feet, and the corresponding surface area IS 14,831,000 acres.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1838","usgsCitation":"Martin, R., and Hanson, R.L., 1966, Reservoirs in the United States: U.S. Geological Survey Water Supply Paper 1838, vi, 115 p.; 1 Plate: 29.19 in. x 19.47 in., https://doi.org/10.3133/wsp1838.","productDescription":"vi, 115 p.; 1 Plate: 29.19 in. x 19.47 in.","numberOfPages":"121","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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,{"id":32675,"text":"pp541 - 1966 - The Alaska earthquake, March 27, 1964: Field investigations and reconstruction effort","interactions":[],"lastModifiedDate":"2022-05-11T20:32:44.092411","indexId":"pp541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"541","title":"The Alaska earthquake, March 27, 1964: Field investigations and reconstruction effort","docAbstract":"One of the greatest geotectonic events of our time occurred in southern Alaska late in the afternoon of March 27, 1964. Beneath a leaden sky, the chill of evening was just settling over the Alaskan countryside. Light snow was falling on some communities. It was Good Friday, schools were closed, and the business day was ending. Suddenly without warning half of Alaska was rocked and jarred by the most violent earthquake to occur in North America this century.\n\nThe descriptive summary that follows is based on the work of many investigators. A large and still-growing scientific literature has accumulated since the earthquake, and this literature has been freely drawn upon here. In particular, the writers have relied upon the findings of their colleagues in the Geological Survey. Some of these findings have been published, but some are still being prepared for publication. Moreover, some field investigations are still in progress.\n\nThis is the first in a series of six reports that the U.S. Geological Survey published on the results of a comprehensive geologic study that began, as a reconnaissance survey, within 24 hours after the March 27, 1964, Magnitude 9.2 Great Alaska Earthquake and extended, as detailed investigations, through several field seasons. The 1964 Great Alaska earthquake was the largest earthquake in the U.S. since 1700. Professional Paper 541, in 1 part, describes Field Investigations and Reconstruction Effort.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp541","usgsCitation":"Hansen, W.R., Eckel, E.B., Schaem, W.E., Lyle, R.E., George, W., and Chance, G., 1966, The Alaska earthquake, March 27, 1964: Field investigations and reconstruction effort: U.S. Geological Survey Professional Paper 541, ix, 111 p., https://doi.org/10.3133/pp541.","productDescription":"ix, 111 p.","numberOfPages":"123","additionalOnlineFiles":"N","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":38848,"text":"pp543B - 1966 - Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska","interactions":[{"subject":{"id":38848,"text":"pp543B - 1966 - Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska","indexId":"pp543B","publicationYear":"1966","noYear":false,"chapter":"B","title":"Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska"},"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":"2022-02-18T20:06:22.524544","indexId":"pp543B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"B","title":"Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska","docAbstract":"The Alaska earthquake of March 27, 1964, caused widespread geomorphic changes in the Martin-Bering Rivers area-900 square miles of uninhabited mountains, alluvial flatlands, and marshes north of the Gulf of Alaska, and east of the Copper River. This area is at lat 60°30’ N. and long 144°22’ W., 32 miles east of Cordova, and approximately 130 miles east-southeast of the epicenter of the earthquake.\n\nThe geomorphic effects observed were: (1) earthquake-induced ground fractures, (2) mudvent deposits, (3) “earthquake-fountain” craters, (4) subsidence, (5) mudcones, (6) avalanches, (7) subaqueous landslides, (8) turbidity changes in ice-basined lakes on the Martin River glacier, (9) filling of ice-walled sinkholes, (10) gravel-coated snow cones, (11) lake ice fractures, and (12) uplift accompanied the earthquake.\n\nIn addition to geomorphic effects, the earthquake affected the animal populations of the area. These include migratory fish, terrestrial mollusks, fur-bearing animals, and man.\n\nThe Alaska earthquake clearly delineated areas of alluvial fill, snow and rock avalanche corridors, and deltas of the deeper lakes as unsuitable for future construction.","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/pp543B","usgsCitation":"Tuthill, S.J., and Laird, W.M., 1966, Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska: U.S. Geological Survey Professional Paper 543, 28 p., https://doi.org/10.3133/pp543B.","productDescription":"28 p.","numberOfPages":"37","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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