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The changes in shoreline processes and beach morphology that were suddenly initiated by the earthquake were similar to those ordinarily caused by gradual changes in sea level operating over hundreds of years, while other more readily visible changes were similar to some of the effects of great but short-lived storms. Phenomena became available for observation within a few hours which would otherwise not have been available for many years.\n\nIn the subsided areas—including the shorelines of the Kenai Peninsula, Kodiak Island, and Cook Inlet—beaches tended to flatten in gradient and to recede shoreward. Minor beach features were altered or destroyed on submergence but began to reappear and to stabilize in their normal shapes within a few months after the earthquake. Frontal beach ridges migrated shoreward and grew higher and wider than they were before. Along narrow beaches backed by bluffs, the relatively higher sea level led to vigorous erosion of the bluff toes. Stream mouths were drowned and some were altered by seismic sea waves, but they adjusted within a few months to the new conditions.\n\nIn the uplifted areas, generally around Prince William Sound, virtually all beaches were stranded out of reach of the sea. New beaches are gradually developing to fit new sea levels, but the processes are slow, in part because the material on the lower parts of the old beaches is predominantly fine grained. Streams were lengthened in the emergent areas, and down cutting and bank erosion have increased.\n\nExcept at Homer and a few small villages, where groins, bulkheads, and cobble-filled baskets were installed, there has been little attempt to protect the postearthquake shorelines. The few structures that were built have been only partially successful because there was too little time to study the habits of the new shore features and to design appropriate protection measures. Emergence of large areas that were once below water and permanent submergence of once-useful land areas have led to many problems of land use and ownership in addition to the destruction or relocation of wildfowl, shellfish, and salmon habitats.","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/pp543J","usgsCitation":"Stanley, K.W., 1968, Effects of the Alaska earthquake of March 27, 1964, on shore processes and beach morphology: U.S. Geological Survey Professional Paper 543, vi, 21 p., https://doi.org/10.3133/pp543J.","productDescription":"vi, 21 p.","numberOfPages":"34","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277850,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543j/index.html"},{"id":395994,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99033.htm"},{"id":65742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543j/pp543j_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543j/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -154.8193359375,\n 56.68037378950137\n ],\n [\n -145.72265625,\n 56.68037378950137\n ],\n [\n -145.72265625,\n 63.93737246791484\n ],\n [\n -154.8193359375,\n 63.93737246791484\n ],\n [\n -154.8193359375,\n 56.68037378950137\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6106c9","contributors":{"authors":[{"text":"Stanley, Kirk W.","contributorId":8900,"corporation":false,"usgs":true,"family":"Stanley","given":"Kirk","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220494,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44050,"text":"ofr69240 - 1968 - Water-table contours in the vicinity of Sterling, Colorado, March 1968","interactions":[],"lastModifiedDate":"2022-05-13T20:16:28.150917","indexId":"ofr69240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"69-240","title":"Water-table contours in the vicinity of Sterling, Colorado, March 1968","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69240","collaboration":"Prepared in cooperation with the Colorado Water Conservation Board","usgsCitation":"Schneider, P., and Albin, D.R., 1968, Water-table contours in the vicinity of Sterling, Colorado, March 1968: U.S. Geological Survey Open-File Report 69-240, 1 Plate: 34.69 x 40.30 inches, https://doi.org/10.3133/ofr69240.","productDescription":"1 Plate: 34.69 x 40.30 inches","costCenters":[],"links":[{"id":400627,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0240/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0240/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Colorado","city":"Sterling","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.24264526367186,\n 40.61082491956405\n ],\n [\n -103.17878723144531,\n 40.61082491956405\n ],\n [\n -103.17878723144531,\n 40.6462615921222\n ],\n [\n -103.24264526367186,\n 40.6462615921222\n ],\n [\n -103.24264526367186,\n 40.61082491956405\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a3b","contributors":{"authors":[{"text":"Schneider, Paul A.","contributorId":32509,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul A.","affiliations":[],"preferred":false,"id":229056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albin, Donald R.","contributorId":67486,"corporation":false,"usgs":true,"family":"Albin","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229057,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2350,"text":"wsp1798D - 1968 - Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado","interactions":[{"subject":{"id":11158,"text":"ofr75291 - 1975 - Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","indexId":"ofr75291","publicationYear":"1975","noYear":false,"title":"Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":2350,"text":"wsp1798D - 1968 - Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado","indexId":"wsp1798D","publicationYear":"1968","noYear":false,"chapter":"D","title":"Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado"},"id":1}],"lastModifiedDate":"2022-02-01T19:09:14.577071","indexId":"wsp1798D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1798","chapter":"D","title":"Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sedimentation in small drainage basins","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1798D","usgsCitation":"Mundorff, J.C., 1968, Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado: U.S. Geological Survey Water Supply Paper 1798, Report: iv, 26 p.; 1 Plate: 15.00 × 19.32 inches, https://doi.org/10.3133/wsp1798D.","productDescription":"Report: iv, 26 p.; 1 Plate: 15.00 × 19.32 inches","costCenters":[],"links":[{"id":110022,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24988.htm","linkFileType":{"id":5,"text":"html"},"description":"24988"},{"id":28274,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28273,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1798d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798d/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Kiowa Creek basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.629,\n 39.0360\n ],\n [\n -104.577,\n 39.0360\n ],\n [\n -104.577,\n 39.0760\n ],\n [\n -104.629,\n 39.0760\n ],\n [\n -104.629,\n 39.0360\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeab4","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":949,"text":"wsp1860 - 1968 - Electrical analog analysis of ground-water depletion in central Arizona","interactions":[],"lastModifiedDate":"2022-02-15T20:58:25.416238","indexId":"wsp1860","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1860","title":"Electrical analog analysis of ground-water depletion in central Arizona","docAbstract":"The Salt River Valley and the lower Santa Cruz River basin are the two largest agricultural areas in Arizona. The extensive use of ground water for irrigation has resulted in the need for a thorough appraisal of the present and future ground-water resources. The ground-water reservoir provides 80 percent (3.2 million acre-feet) of the total annual water supply. The amount of water pumped greatly exceeds the rate at which the ground-water supply is being replenished and has resulted in water-level declines of as much as 20 feet per year in some places. The depletion problem is of economic importance because ground water will become more expensive as pumping lifts increase and well yields decrease. The use of electrical-analog modeling techniques has made it possible to predict future ground-water levels under conditions of continued withdrawal in excess of the rate of replenishment. The electrical system is a representation of the hydrologic system: resistors and capacitors represent transmissibility and storage coefficients. The analogy between the two systems is accepted when the data obtained from the model closely match the field data in this instance, measured water-level change since 1923. The prediction of future water-table conditions is accomplished by a simple extension of the pumping trends to determine the resultant effect on the regional water levels. \r\n\r\nThe results of this study indicate the probable depths to water in central Arizona in 1974 and 1984 if the aquifer characteristics are accurately modeled and if withdrawal of ground water continues at the same rate and under the tame areal distribution as existed between 1958 and 1964. The greatest depths to water in 1984 will be more than 700 feet near Stanfield and more than 650 feet in Deer Valley and northeast of Gilbert. South of Eloy and northwest of Litchfield Park, a static water level of more than 550 feet is predicted. The total water-level decline in the 20-year period 1964-84 at the deepest points of the major cones of depression will range from 150 to 300 feet, and the average decline in the entire central Arizona area will be about 100 feet.","language":"English","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1860","usgsCitation":"Anderson, T.W., 1968, Electrical analog analysis of ground-water depletion in central Arizona: U.S. Geological Survey Water Supply Paper 1860, Report: iii, 21 p.; 4 Plates: 44.69 × 26.00 inches or smaller, https://doi.org/10.3133/wsp1860.","productDescription":"Report: iii, 21 p.; 4 Plates: 44.69 × 26.00 inches or smaller","costCenters":[],"links":[{"id":396005,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25084.htm"},{"id":25451,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1860/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25450,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1860/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25454,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1860/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25453,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1860/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25452,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1860/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1860/report-thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.4835205078125,\n 32.59773394005744\n ],\n [\n -111.3299560546875,\n 32.59773394005744\n ],\n [\n -111.3299560546875,\n 33.660353121928814\n ],\n [\n -112.4835205078125,\n 33.660353121928814\n ],\n [\n -112.4835205078125,\n 32.59773394005744\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672556","contributors":{"authors":[{"text":"Anderson, T. W.","contributorId":105686,"corporation":false,"usgs":true,"family":"Anderson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68135,"text":"ha255 - 1968 - Floods in McHenry Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"255","title":"Floods in McHenry Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha255","usgsCitation":"Mycyk, R.T., and Walter, G.L., 1968, Floods in McHenry Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 255, 1 col. map ;58 x 43 cm., on sheet 80 x 122 cm., https://doi.org/10.3133/ha255.","productDescription":"1 col. map ;58 x 43 cm., on sheet 80 x 122 cm.","costCenters":[],"links":[{"id":186678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89436,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/255/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.36749999999999,42.25 ], [ -88.36749999999999,42.3675 ], [ -88.25,42.3675 ], [ -88.25,42.25 ], [ -88.36749999999999,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7010","contributors":{"authors":[{"text":"Mycyk, Roman T.","contributorId":58331,"corporation":false,"usgs":true,"family":"Mycyk","given":"Roman","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":277708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Gerald L.","contributorId":59880,"corporation":false,"usgs":true,"family":"Walter","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277709,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":58078,"text":"wdrCO671 - 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