{"pageNumber":"6557","pageRowStart":"163900","pageSize":"25","recordCount":185189,"records":[{"id":38846,"text":"pp542E - 1967 - Effects of the earthquake of March 27, 1964, at Seward, Alaska","interactions":[{"subject":{"id":38846,"text":"pp542E - 1967 - Effects of the earthquake of March 27, 1964, at Seward, Alaska","indexId":"pp542E","publicationYear":"1967","noYear":false,"chapter":"E","title":"Effects of the earthquake of March 27, 1964, at Seward, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"id":1}],"isPartOf":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"lastModifiedDate":"2022-03-31T18:47:27.868901","indexId":"pp542E","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"542","chapter":"E","title":"Effects of the earthquake of March 27, 1964, at Seward, Alaska","docAbstract":"<p>Seward, in south-central Alaska, was one of the towns most devastated by the Alaska earthquake of March 27, 1964. The greater part of Seward is built on an alluvial fan-delta near the head of Resurrection Bay on the southeast coast of the Kenai Peninsula. It is one of the few ports in south-central Alaska that is ice free all year, and the town’s economy is almost entirely dependent upon its port facilities.</p>\n</br>\n<p>The Alaska earthquake of March 27, 1964, magnitude approximately 8.3–8.4, began at 6:36 p.m. Its epicenter was in the northern part of the Prince William Sound area; focal depth was 20–50 km.</p>\n</br>\n<p>Strong ground motion at Seward lasted 3–4 minutes. During the shaking, a strip of land 50–400 feet wide along the Seward waterfront, together with docks and other harbor facilities, slid into Resurrection Bay as a result of large-scale submarine landsliding. Fractures ruptured the ground for'severa1 hundred feet back from the landslide scarps. Additional ground was fractured in the Forest Acres subdivision and on the alluvial floor of the Resurrection River valley; fountaining and sand boils accompanied the ground fracturing. Slide-generated wares, possibly seiche waves, and seismic sea waves crashed onto shore; ware runup was as much as 30 feet above mean lower low water and caused tremendous damage; fire from burning oil tanks added to the destruction. Damage from strong ground motion itself was comparatively minor. Tectonic subsidence of about 3.6 feet resulted in low areas being inundated at high tide.</p>\n</br>\n<p>Thirteen people were killed and five were injured as a result of the earthquake. Eighty-six houses were totally destroyed and 260 were heavily damaged. The harbor facilities were almost completely destroyed, and the entire economic base of the town was wiped out. The total cost to replace the destroyed public and private facilities was estimated at $22 million.</p>\n</br>\n<p>Seward lies on the axis of the Chugach Mountains geosyncline. The main structural trend in the mapped area, where the rocks consist almost entirely of graywacke and phyllite, is from near north to N. 20° E. Beds and cleavage of the rocks commonly dip 70° W. or NW. to near vertical. Locally, the rocks are complexly folded or contorted. So major faults were found in the mapped area, but small faults, shear zones, and joints are common.</p>\n</br>\n<p>Surficial deposits of the area hare been divided for mapping into the following units: drift deposits, alluvial fan deposits, valley alluvium, intertidal deposits, landslide deposits, and artificial fill. Most of these units intergrade and were deposited more or less contemporaneously.</p>\n</br>\n<p>The drift deposits consist chiefly of till that forms moraines along the lower flanks of the Resurrection River valley and up tributary valleys. The till is predominantly silt and sand and lesser amounts of clay-size particles, gravel, cobbles, and boulders. Glacial outwash and stratified ice-contact deposits constitute the remainder of the drift deposits.</p>\n</br>\n<p>Fans and fan-deltas have been deposited at the valley mouths of tributary streams. Some, including the one upon which Seward built, project into Resurrection Bay, and deltaic-type deposits form their distal edges. The larger fans—composed chiefly of loosely compacted and poorly sorted silt, sand, and gravel—form broad aprons having low gradients. The fan deposits range in thickness from about 100 feet to possibly several hundred feet and, at least in some places, lie on a platform of compact drift. Smaller fans at the mouths of several canyons have steep gradients and considerable local relief.</p>\n</br>\n<p>Valley alluvium, deposited chiefly by the Resurrection River, consists mostly of coarse sand and fine to medium gravel. In the axial part of the valley it is probably more than 100 feet thick. Near the head of Resurrection Bay, the alluvium is underlain by at least 75 feet of marine deltaic sediments, which are in turn underlain by 600 or more feet of drift in the deepest part of the bedrock valley.</p>\n</br>\n<p>Beach, deltaic, and estuarine sediments, deposited on intertidal flats at the head of the bay and along far1 margins that extend into the bay, arc mapped as intertidal deposits. They consist mostly of silt, sand, and fine gravel, and lesser amounts of clay-size particles.</p>\n</br>\n<p>The earthquake reactivated old slides and trigged new ones in the mountains. Rock and snow avalanches, debris flows, and creep of talus deposits characterized slide activity on the steeper slops. The Seward waterfront had been extended before the earthquake by adding artificial fill consisting of loose sand and gravel; part of the lagoon area had been filled with refuse. After the earth- quake, fill, consisting of silt and sand dredged from the head of the bay, was pumped onto part of the lagoon area and also on land at the northwest corner of the bay.</p>\n</br>\n<p>Response to the disaster was immediate and decisive. City, State, and Federal agencies, as well as other organizations and individuals, gave unstintingly of their time and facilities. Within a few days, there was temporary restoration of water, sewerage, and electrical facilities.</p>\n</br>\n<p>The U.S. Army Corps of Engineers was authorized to select sites and construct a new dock for the Alaska Railroad, a new small-boat basin, and related facilities. The firm of Shannon and Wilson, Inc., under contract to the Corps of Engineers, investigated subsurface soils extensively to determine the factors responsible for the sliding along the Seward waterfront and to assist in site selection for reconstruction of the destroyed harbor facilities. Borings also made along the Seward waterfront and at the head of the bay, and laboratory tests were conducted on pertinent samples. These studies were augmented by geophysical studies both on land and in the bay. In addition, the Corps of Engineers made shallow borings on the intertidal flats at the head of the bay and performed pile-driving and load tests. Borings also were drilled and test pits were dug in the subdivision of Forest Acres.</p>\n</br>\n<p>Sliding along the Seward waterfront markedly deepened the water along the former shoreline. Post-earthquake slopes of the bay floor immediately offshore also are steeper in places than before the earthquake. The strong ground motion of the earthquake triggered the landsliding, but several factors may have contributed to the magnitude and characteristics of the slides. These factors are: (1) the long duration of strong ground motion, (2) the grain size and texture of the material involved in the sliding, (3) the probability that the finer grained materials liquefied and flowed seaward, and (4) the added load of manmade facilities built on the edge of the shore, Secondary effects of the slides themselves—sudden drawdown of water, followed by the weight of returning waves—also may have contributed to the destruction.</p>\n</br>\n<p>Submarine sliding at the northwest corner of the bay occurred in fine-grained deltaic deposits whose frontal slopes probably were in metastable equilibrium under static conditions. Uplift pressures from aquifers under hydrostatic head, combined with the probable liquefaction characteristics of the sediments when vibrated by strong ground motion, probably caused the material to slide and flow seaward as a heavy slurry.</p>\n</br>\n<p>Under static conditions, no major shoreline or submarine landsliding is expected in the Seward area; in the event of another severe earthquake, however, additional sliding is likely along the Seward waterfront and also in the deltaic deposits at the northwest corner of the bay. Fractured ground in back of the present shoreline along the Seward waterfront is an area of incipient landslides that would be unstable under strong shaking. For this reason the Scientific and Engineering Task Force placed the area in a high-risk classification and recommended no repair, rehabilitation, or new construction in this area involving use of Federal funds; it was further recommended that the area should be reserved for park or other uses that do not involve large congregations of people. The deltaic deposits at the head of the bay probably also would be susceptible to sliding during another large earthquake. This sliding would result in further landward retreat of the present shoreline toward the new railroad dock. Specifications for the new dock, whose seaward end is now approximately 1,100 feet from the back scarp of the subaqueous landslide, require design pro- visions to withstand seismic shock up to certain limits.</p>\n</br>\n<p>Earthquake-induced fracturing of the ground in the subdivision of Forest Acres was confined to the lower part of a broad alluvial fan. There, sewer and water lines were ruptured and the foundations of some homes were heavily damaged. Landsliding, such as occurred along the shoreline of the bay, was not a contributing cause of the fracturing. Two hypotheses are offered to explain the fracturing:</p>\n\n<p>1. Seismic energy was transformed into visible surface waves of such amplitude that the strength of surface layer was exceeded and rupturing occurred; tensional and compressional stresses alternately opened and closed the fractures and forced out water and mud.</p>\n\n<p>2. Compaction by vibration of the fine-grained deposits of the fan caused ground settlement and fracturing; ground water under temporary hydrostatic head was forced to the surface as fountains and carried the finer material with it.</p>\n</br>\n<p>Water waves that crashed onto shore, while shaking was still continuing, were generated chiefly by onshore and offshore landsliding. Waves that overran the shores about 25 minutes after shaking stopped and that continued to arrive for the next several hours are believed to be seismic sea waves (tsunamis) that originated in an uplifted area in the Gulf of Alaska. During the time of seismic sea-wave activity and perhaps preceding it, seiche wares also may have been generated within Resurrection Bay and complicated the wave effects along the shoreline.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on communities (Professional Paper 542)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542E","usgsCitation":"Lemke, R., 1967, Effects of the earthquake of March 27, 1964, at Seward, Alaska: U.S. Geological Survey Professional Paper 542, Report: viii, 43 p.; 2 Plates: 20.5 x 21.5 inches and 25.57 x 19.78 inches, https://doi.org/10.3133/pp542E.","productDescription":"Report: viii, 43 p.; 2 Plates: 20.5 x 21.5 inches and 25.57 x 19.78 inches","numberOfPages":"53","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":170343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0542e/report-thumb.jpg"},{"id":113268,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397947,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4587.htm"},{"id":113267,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0542e/pp542e_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104504,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0542e/index.html","linkFileType":{"id":5,"text":"html"},"description":"4587"}],"scale":"63360","datum":"Mean Sea Level","country":"United States","state":"Alaska","city":"Seward","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.4778,\n              60.0622\n            ],\n            [\n              -149.3333,\n              60.0622\n            ],\n            [\n              -149.3333,\n              60.1856\n            ],\n            [\n              -149.4778,\n              60.1856\n            ],\n            [\n              -149.4778,\n              60.0622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610336","contributors":{"authors":[{"text":"Lemke, Richard W.","contributorId":59409,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard W.","affiliations":[],"preferred":false,"id":220533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2356,"text":"wsp1846 - 1967 - Ground water in the vicinity of American Falls Reservoir, Idaho","interactions":[],"lastModifiedDate":"2013-11-21T14:50:07","indexId":"wsp1846","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1846","title":"Ground water in the vicinity of American Falls Reservoir, Idaho","docAbstract":"Analysis of ground- and surface-water relationships suggests that increasing\nthe capacity of the American Falls Reservoir by raising the height of the\ndam 15 feet would increase leakage from the reservoir by less than 0.2 percent\nof the average inflow to the reservoir, or less than 10,000 acre feet per year.\nThis amount is less than one-tenth of the evaporation rate from the reservoir.\nThe American Falls Reservoir lies near the south margin of the Snake\nRiver Plain in southeastern Idaho. The Snake River Plain is about 200 miles\nlong and averages nearly 60 miles in width. It is underlain by a thick sequence\nof basaltic lava flows, interbedded pyroclasties, and sedimentary deposits. The\nuppermost few thousand feet of this sequence is the Snake Plain aquifer, one of\nthe great aquifers of the United States.\nRecharge to the aquifer is chiefly by water percolating from the Snake River, its\ntributaries, and irrigated tracts, and by underflow from surrounding areas.\nGround water moves generally southwestward and discharges to the Snake River\nthrough springs in the American Falls Reservoir reach and in the Hagerman\nValley reach (between Twin Falls and Bliss). Total discharge from the aquifer\nis about 9,000 cfs (cubic feet per second).\nThe occurrence and movement of ground water in the viscinity of American\nFalls Reservoir are controlled by the local geology. Silt and tuff in the Neeley\nFormation and the Walcott Tuff and silt and fine sand in the FT ft Formation\nand American Falls Lake Beds have a low permeability. These rocks transmit\nlittle ground water compared with the basalt and intercalated pyroclasties and\ngravels of the Snake Plain aquifer. The less permeable deposits underlie the\nreservoir area and act as a barrier to the movement of ground water.\nUnder present conditions the water table on the periphery of the reservoir\nslopes toward the reservoir, except within 3 or 4 miles of the dam, where the\nwater table slopes away from the reservoir. Most of the springs discharge at\naltitudes above 4,370 feet, some 15 feet above the maximum reservoir stage.\nThus, reservoir stage has little effect on ground-water inflow to the reservoir.\nA fairly close relationship exists between the annual amount of surface water\ndiverted for irrigation of lands up the Snake River from the reservoir and the\nannual ground-water discharge through springs for the period 1911-60. After\nabout 1952, greatly increased ground-water withdrawals from wells, which increased\nconsumptive use, virtually balanced increased diversions from the surface-\nwater system for irrigation, so that ground-water inflow to the reservoir\nremained about constant.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1846","collaboration":"Prepared in cooperation with the U.S. Bureau of Reclamation","usgsCitation":"Mundorff, M.J., 1967, Ground water in the vicinity of American Falls Reservoir, Idaho: U.S. Geological Survey Water Supply Paper 1846, Report: iv, 58 p.; Plate 1: 15 inches x 12.39 inches; Plate 2: 39 inches x 29.85 inches; Plate 3: 30 inches x 18.71 inches; Plate 4: 27 inches x 18.24 inches; Plate 5: 39 inches x 29.87, https://doi.org/10.3133/wsp1846.","productDescription":"Report: iv, 58 p.; Plate 1: 15 inches x 12.39 inches; Plate 2: 39 inches x 29.85 inches; Plate 3: 30 inches x 18.71 inches; Plate 4: 27 inches x 18.24 inches; Plate 5: 39 inches x 29.87","costCenters":[],"links":[{"id":137784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1846/report-thumb.jpg"},{"id":28286,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28287,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28288,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28289,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28290,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1846/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1846/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"American Falls Reservoir","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ], [ -0.01638888888888889,0.0011111111111111111 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d814","contributors":{"authors":[{"text":"Mundorff, Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38815,"text":"pp543F - 1967 - Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","interactions":[{"subject":{"id":38815,"text":"pp543F - 1967 - Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","indexId":"pp543F","publicationYear":"1967","noYear":false,"chapter":"F","title":"Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-02-18T20:13:03.475534","indexId":"pp543F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"F","title":"Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake","docAbstract":"The great 1964 Alaska earthquake caused considerable ground breakage in the Cook Inlet area of south-central Alaska. The breakage occurred largely in thick deposits of unconsolidated sediments. The most important types of ground breakage were (1) fracturing or cracking and the extrusion of sand and gravel with ground water along fractures in various types of landforms, and (2) slumping and lateral extension of unconfined faces, particularly along delta fronts.\n\nThe principal concentration of ground breakage within the area covered by this report was in a northeast-trending zone about 60 miles long and 6 miles wide in the northern part of the Kenai Lowland. The zone cut across diverse topography and stratigraphy. Cracks were as much as 30 feet across and 25 feet deep. Sand, gravel, and pieces of coal and lignite were extruded along many fissures. It is suggested that the disruption in this zone may be due to movement along a fault in the underlying Tertiary rocks.\n\nThe outwash deltas of Tustumena and Skilak Lakes in the Kenai Lowland, of Eklutna Lake and Lake George in the Chugach Mountains, of Bradley Lake in the Kenai Mountains, and at the outlet of upper Beluga Lake at the base of the Alaska Range showed much slumping, as did the delta of the Susitna River. Parts of the flood plains of the Skilak River, Fox River, and Eagle River were extensively cracked.\n\nA few avalanches and slumps occurred along the coast of Cook Inlet in scattered localities. Some tidal flats were cracked. However, in view of the many thick sections of unconsolidated sediments and the abundance of steep slopes, the cracking was perhaps less than might have been expected.\n\nObservations along the coasts indicated changes in sea level which, although caused partly by compaction of unconsolidated sediments, may largely be attributed to crus1tal deformation accompanying the earthquake. Most of the Cook Inlet area was downwarped, although the northwest side of Cook Inlet may have been slightly unwarped. Maximum change in the Cook Inlet area was probably less than 6 feet. Little or no regional tilting was detected in the lake basins of Tustumena and Skilak Lakes.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543F","usgsCitation":"Foster, H.L., and Karlstrom, T., 1967, Ground breakage and associated effects in the Cook Inlet area, Alaska, resulting from the March 27, 1964, earthquake: U.S. Geological Survey Professional Paper 543, Report: v, 28 p.; 3 Plates: 19.81 x 30.95 inches or smaller, https://doi.org/10.3133/pp543F.","productDescription":"Report: v, 28 p.; 3 Plates: 19.81 x 30.95 inches or smaller","numberOfPages":"36","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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V.","contributorId":77929,"corporation":false,"usgs":true,"family":"Karlstrom","given":"Thor N. V.","affiliations":[],"preferred":false,"id":220491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38820,"text":"pp544D - 1967 - Effects of the March 1964 Alaska earthquake on glaciers","interactions":[],"lastModifiedDate":"2022-02-15T20:43:32.459277","indexId":"pp544D","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"D","title":"Effects of the March 1964 Alaska earthquake on glaciers","docAbstract":"The 1964 Alaska earthquake occurred in a region where there are many hundreds of glaciers, large and small. Aerial photographic investigations indicate that no snow and ice avalanches of large size occurred on glaciers despite the violent shaking. Rockslide avalanches extended onto the glaciers in many localities, seven very large ones occurring in the Copper River region 160 kilometers east of the epicenter. Some of these avalanches traveled several kilometers at low gradients; compressed air may have provided a lubricating layer. If long-term changes in glaciers due to tectonic changes in altitude and slope occur, they will probably be very small. No evidence of large-scale dynamic response of any glacier to earthquake shaking or avalanche loading was found in either the Chugach or Kenai Mountains 16 months after the 1964 earthquake, nor was there any evidence of surges (rapid advances) as postulated by the Earthquake-Advance Theory of Tarr and Martin.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544D","usgsCitation":"Post, A., 1967, Effects of the March 1964 Alaska earthquake on glaciers: U.S. Geological Survey Professional Paper 544, vi, 42 p., https://doi.org/10.3133/pp544D.","productDescription":"vi, 42 p.","numberOfPages":"42","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":396002,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99035.htm"},{"id":277813,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544d/index.html"},{"id":65743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544d/pp544d_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544d/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.1279296875,\n              59.265880628258095\n            ],\n            [\n              -140.73486328125,\n              59.265880628258095\n            ],\n            [\n              -140.73486328125,\n              61.762728830472696\n            ],\n            [\n              -151.1279296875,\n              61.762728830472696\n            ],\n            [\n              -151.1279296875,\n              59.265880628258095\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61055d","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":220496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32613,"text":"pp544C - 1967 - Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>","interactions":[],"lastModifiedDate":"2013-09-18T15:32:00","indexId":"pp544C","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"C","title":"Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>","docAbstract":"The Alaska earthquake of March 27, 1964, had widespread hydrologic effects throughout practically all of the United States. More than 1,450 water-level recorders, scattered throughout all the 50 States except Connecticut, Delaware, and Rhode Island, registered the earthquake. Half of the water-level records were obtained from ground-water observation wells and half at surface-water gaging stations. The earthquake is also known to have registered on water-level recorders on wells in Canada, England, Denmark, Belgium, Egypt, Israel, Libya, Philippine Islands, South-West Africa, South Africa, and Northern Territory of Australia. The Alaska earthquake is the first for which widespread surface-water effects are known. The effects were recorded at stations on flowing streams, rivers, reservoirs, lakes, and ponds. The 755 surface-water stations recording effects are spread through 38 States, but are most numerous in the south-central and southeastern States, especially in Florida and Louisiana. Most of the fluctuations recorded can be referred to more precisely as seismic seiches; however, a few stations recorded the quake as a minor change in stage. The largest recorded seiche outside Alaska was 1.83 feet on a reservoir in Michigan. The next largest was 1.45 feet on Lake Ouachita in Arkansas. The largest fluctuation in a well was 23 feet registered by a pressure recorder near Belle Fourche, S. Dak. Fluctuations of more than 10 feet were reported from wells in Alabama, Florida, Georgia, Illinois, Missouri, and Pennsylvania. A 3.40-foot fluctuation was recorded in a well in Puerto Rico. The Alaska earthquake was registered by about seven times as many water-level recorders as recorded the Hebgen Lake, Mont., earthquake of August 19, 1959.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544C","collaboration":"This report is Chapter C in <i>The Alaska earthquake, March 27, 1964: effects on hydrologic regimen</i>.  For more information, see: <a href=\"http://pubs.usgs.gov/pp/0544/index.html\" target=\"_blank\">Professional Paper 544</a>.","usgsCitation":"Vorhis, R.C., Rexin, E.E., and Coble, R.W., 1967, Hydrologic effects of the earthquake of March 27, 1964, outside Alaska, with sections on Hydroseismograms from the Nunn-Bush Shoe Co. well, Wisconsin, and Alaska earthquake effects on ground water in Iowa: Chapter C in <i>The Alaska earthquakes, March 27, 1964: effects on hydrologic regimen</i>: U.S. Geological Survey Professional Paper 544, p. C1-C54, https://doi.org/10.3133/pp544C.","productDescription":"p. C1-C54","numberOfPages":"54","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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W.","contributorId":49380,"corporation":false,"usgs":true,"family":"Coble","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208794,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32619,"text":"pp554D - 1967 - Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2018-11-08T07:33:18","indexId":"pp554D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"554","chapter":"D","title":"Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California","docAbstract":"Cenozoic volcanic rocks of the Devils Postpile quadrangle are of late Pliocene to Recent age and are divided into 11 map units. The suite is alkalic-calcic and ranges in composition from basalt to rhyolite. It includes a rhyolitic welded ash-flow tuff which is probably correlative with the Bishop Tuff, although the two units are geographically isolated by the Sierra Nevada drainage divide. The Devils Postpile itself is a classic example of columnar jointing in the lower part of a lava flow.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1966","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp554D","collaboration":"Prepared in cooperation with the California Division of Mines and Geology","usgsCitation":"Huber, N.K., and Rinehart, C.D., 1967, Cenozoic Volcanic Rocks of the Devils Postpile Quadrangle, Eastern Sierra Nevada, California: U.S. Geological Survey Professional Paper 554, p. D1-D21, https://doi.org/10.3133/pp554D.","productDescription":"p. D1-D21","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":60483,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0554d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60484,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0554d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0554d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6f58","contributors":{"authors":[{"text":"Huber, N. King","contributorId":51284,"corporation":false,"usgs":true,"family":"Huber","given":"N.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":208805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinehart, C. Dean","contributorId":88326,"corporation":false,"usgs":true,"family":"Rinehart","given":"C.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":208806,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32626,"text":"pp575B - 1967 - Geological Survey research 1967, Chapter B","interactions":[],"lastModifiedDate":"2025-01-14T23:00:01.31529","indexId":"pp575B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"575","chapter":"B","title":"Geological Survey research 1967, Chapter B","docAbstract":"<p>This collection of 49 short papers is the first published chapter of \"Geological Survey Research 1967.\" The papers report on scientific and economic results of current work. by members of the Geologic, Topographic, and Water Resources Divisions of the U.S. Geological Survey.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1967 (Professional Paper 575)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp575B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Geological Survey research 1967, Chapter B: U.S. Geological Survey Professional Paper 575, v, 265 p., https://doi.org/10.3133/pp575B.","productDescription":"v, 265 p.","numberOfPages":"270","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":466359,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93412.htm","text":"Tertiary stratigraphy and geohydrology in southwestern Georgia","linkFileType":{"id":5,"text":"html"}},{"id":466358,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30354.htm","text":"Distinctive brines in Great Salt Lake, Utah","linkFileType":{"id":5,"text":"html"}},{"id":466357,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30354.htm","text":"Rate and extent of migration of a \"one-shot\" contaminant in an alluvial aquifer in Keizer, Oregon","linkFileType":{"id":5,"text":"html"}},{"id":466356,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30353.htm","text":"Effect of urban development on quality of ground water, Raleigh, North Carolina","linkFileType":{"id":5,"text":"html"}},{"id":466355,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30352.htm","text":"Hydrology of glaciated valleys in the Jamestown area of southwestern New York","linkFileType":{"id":5,"text":"html"}},{"id":466354,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30351.htm","text":"Results of some geophysical investigations in the Wood Hills area of northeastern Nevada","linkFileType":{"id":5,"text":"html"}},{"id":466353,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30350.htm","text":"Hydrothermal alteration of basaltic andesite and other rocks in drill hole GS-6, Steamboat Springs, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":466352,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30349.htm","text":"Varved lake beds in northern Idaho and northeastern Washington","linkFileType":{"id":5,"text":"html"}},{"id":466351,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30348.htm","text":"Effect of landslides on the course of Whitetail Creek, Jefferson County, Montana","linkFileType":{"id":5,"text":"html"}},{"id":466345,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30342.htm","text":"Silver and mercury geochemical anomalies in the Comstock, Tonopah, and Silver Reef districts, Nevada - 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Umatilla syncline, Oregon and Washington","linkFileType":{"id":5,"text":"html"}},{"id":163159,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0575b/report-thumb.jpg"},{"id":113043,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0575b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877fa","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58092,"text":"wdrWI6612 - 1967 - Water resources data for Wisconsin, 1966; Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:32","indexId":"wdrWI6612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-66-1-2","title":"Water resources data for Wisconsin, 1966; Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrWI6612","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for Wisconsin, 1966; Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report WI-66-1-2, 228 p., https://doi.org/10.3133/wdrWI6612.","productDescription":"228 p.","numberOfPages":"228","costCenters":[],"links":[{"id":182568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1966/wi-66-1-2/report-thumb.jpg"},{"id":88321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/wi-66-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f168f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32617,"text":"pp553 - 1967 - Cenozoic pectinids of Alaska, Iceland, and other northern regions","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"pp553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"553","title":"Cenozoic pectinids of Alaska, Iceland, and other northern regions","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/pp553","usgsCitation":"MacNeil, F.S., 1967, Cenozoic pectinids of Alaska, Iceland, and other northern regions: U.S. Geological Survey Professional Paper 553, 57 p., https://doi.org/10.3133/pp553.","productDescription":"57 p.","costCenters":[],"links":[{"id":119431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0553/report-thumb.jpg"},{"id":60477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0553/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6f1e","contributors":{"authors":[{"text":"MacNeil, F. Stearns","contributorId":31760,"corporation":false,"usgs":true,"family":"MacNeil","given":"F.","email":"","middleInitial":"Stearns","affiliations":[],"preferred":false,"id":208802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37500,"text":"ssrw102 - 1967 - The breeding bird survey, 1966","interactions":[],"lastModifiedDate":"2017-06-14T15:22:31","indexId":"ssrw102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"102","title":"The breeding bird survey, 1966","docAbstract":"<p><span>A Breeding Bird Survey of a large section on North America was conducted during June 1966. Cooperators ran a total of 585 Survey routes in 26 eastern States and 4 Canadian Provinces. Future coverage of established routes will enable changes in the abundance of North American breeding birds to be measured. Routes are selected at random on the basis of one-degree blocks of latitude and longitude. Each 241/2-mile route, with 3-minute stops spaced one-half mile apart, is driven by automobile. All birds heard or seen at the stops are recorded on special forms and the data are then transferred to machine punch cards. The average number of birds per route is tabulated by State, along with the total number of each species and the percent of routes and stops upon which they were recorded. Maps are presented showing the range and abundance of selected species. Also, a year-to-year comparison is made of populations of selected species on Maryland routes in 1965 and 1966.</span></p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Robbins, C.S., and Van Velzen, W.T., 1967, The breeding bird survey, 1966: Special Scientific Report  - Wildlife 102, 43 p.","productDescription":"43 p.","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":165366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94324,"rank":9999,"type":{"id":15,"text":"Index Page"},"url":"https://hdl.handle.net/2027/mdp.39015013567543?urlappend=%3Bseq=5"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629d78","contributors":{"authors":[{"text":"Robbins, Chandler S. crobbins@usgs.gov","contributorId":4275,"corporation":false,"usgs":true,"family":"Robbins","given":"Chandler","email":"crobbins@usgs.gov","middleInitial":"S.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":218181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Velzen, Willet T.","contributorId":100448,"corporation":false,"usgs":true,"family":"Van Velzen","given":"Willet","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":218182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32615,"text":"pp545A - 1967 - Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage","interactions":[{"subject":{"id":32615,"text":"pp545A - 1967 - Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage","indexId":"pp545A","publicationYear":"1967","noYear":false,"chapter":"A","title":"Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":1}],"isPartOf":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"lastModifiedDate":"2022-01-07T21:49:29.465278","indexId":"pp545A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"545","chapter":"A","title":"Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage","docAbstract":"The March 27, 1964, Alaska earthquake and its associated aftershocks caused damage requiring several million dollars worth of repair to the Eklwtna Hydroelectric Project, 34 miles northeast of Anchorage. Electric service from the Eklutna powerplant was interrupted during the early phase of the March 27 earthquake, built was restored (intermittently) until May 9,1964, when the plant was closed for inspection and repair. Water for Eklutna project is transported from Eklutna Lake to the powerplant at tidewater on Knik Arm of Cook Inlet by an underwater intake connected to a 4.46-mile tunnel penstock. The primary damage caused by the earthquake was 1at the intake structure in Eklutna Lake. No damage to the power tunnel was observed. The piles-supported powerplant and appurtenant structures, Anchorage and Palmer substations, and the transmission lines suffered minor dammage. Most damage occurred to facilities constructed on un-consolidated sediments and overburden which densified and subsided during the earthquake. Structures built on bedrock experienced little or no damage. Underground communication and electrical systems in Anchorage were examined with a small-diameter television camera to locate damaged areas requiring repair. Most of the damage was concentrated at or near valley slopes. Those parts of the systems within the major slide areas of the city were destroyed.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities (Professional Paper 545)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp545A","usgsCitation":"Logan, M.H., and Burton, L.R., 1967, Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage: U.S. Geological Survey Professional Paper 545, vi, 30 p., https://doi.org/10.3133/pp545A.","productDescription":"vi, 30 p.","numberOfPages":"38","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":60476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0545a/pp545a_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0545a/report-thumb.jpg"},{"id":277802,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0545a/"}],"country":"United States","state":"Alaska","city":"Anchorage","otherGeospatial":"Eklutna Hydroelectric Project","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -149.1789,\n              61.4869\n            ],\n            [\n              -149.0944,\n              61.4869\n            ],\n            [\n              -149.0944,\n              61.4\n            ],\n            [\n              -149.1789,\n              61.4\n            ],\n            [\n              -149.1789,\n              61.4869\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610250","contributors":{"authors":[{"text":"Logan, Malcolm H.","contributorId":42127,"corporation":false,"usgs":true,"family":"Logan","given":"Malcolm","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":208799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burton, Lynn R.","contributorId":103962,"corporation":false,"usgs":true,"family":"Burton","given":"Lynn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":208800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":65993,"text":"i316 - 1967 - Glacial map of Ohio","interactions":[],"lastModifiedDate":"2022-04-12T19:16:41.559264","indexId":"i316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"316","title":"Glacial map of Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i316","usgsCitation":"Goldthwait, R.P., White, G.W., and Forsyth, J.L., 1967, Glacial map of Ohio (Revised Edition): U.S. Geological Survey IMAP 316, 1 Plate: 38.65 × 36.40 inches, https://doi.org/10.3133/i316.","productDescription":"1 Plate: 38.65 × 36.40 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,{"id":38747,"text":"pp599A - 1967 - Seismic detection of near-surface cavities","interactions":[],"lastModifiedDate":"2012-02-02T00:09:54","indexId":"pp599A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"599","chapter":"A","title":"Seismic detection of near-surface cavities","language":"ENGLISH","doi":"10.3133/pp599A","usgsCitation":"Watkins, J.S., Godson, R.H., and Watson, K., 1967, Seismic detection of near-surface cavities: U.S. Geological Survey Professional Paper 599, p. A1-A12, https://doi.org/10.3133/pp599A.","productDescription":"p. A1-A12","costCenters":[],"links":[{"id":119640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0599a/report-thumb.jpg"},{"id":65611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0599a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8c6","contributors":{"authors":[{"text":"Watkins, J. S.","contributorId":18821,"corporation":false,"usgs":true,"family":"Watkins","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Godson, R. H.","contributorId":98719,"corporation":false,"usgs":true,"family":"Godson","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":220384,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watson, Kenneth","contributorId":91109,"corporation":false,"usgs":true,"family":"Watson","given":"Kenneth","email":"","affiliations":[],"preferred":false,"id":220383,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39124,"text":"pp272H - 1967 - Analysis of techniques used to measure evaporation from Salton Sea, California","interactions":[],"lastModifiedDate":"2012-02-02T00:09:54","indexId":"pp272H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"272","chapter":"H","title":"Analysis of techniques used to measure evaporation from Salton Sea, California","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies of evaporation","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp272H","usgsCitation":"Hughes, G., 1967, Analysis of techniques used to measure evaporation from Salton Sea, California: U.S. Geological Survey Professional Paper 272, p. 151-176, https://doi.org/10.3133/pp272H.","productDescription":"p. 151-176","costCenters":[],"links":[{"id":122163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0272h/report-thumb.jpg"},{"id":66612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0272h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68014d","contributors":{"authors":[{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":220998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63947,"text":"gp607 - 1967 - Aeromagnetic map of the Crystal Falls quadrangle and part of the Florence quadrangle, Iron County, Michigan","interactions":[],"lastModifiedDate":"2012-02-10T00:11:10","indexId":"gp607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"607","title":"Aeromagnetic map of the Crystal Falls quadrangle and part of the Florence quadrangle, Iron County, Michigan","language":"ENGLISH","doi":"10.3133/gp607","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Crystal Falls quadrangle and part of the Florence quadrangle, Iron County, Michigan: U.S. Geological Survey Geophysical Investigations Map 607, 1 map., https://doi.org/10.3133/gp607.","productDescription":"1 map.","costCenters":[],"links":[{"id":250300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0607/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":250301,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0607/plate-1.pdf","size":"3973","linkFileType":{"id":1,"text":"pdf"}},{"id":253798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0607/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,46 ], [ -88.5,46.25 ], [ -88.25,46.25 ], [ -88.25,46 ], [ -88.5,46 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c1d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62023,"text":"mr51 - 1967 - Iron in the United States, exclusive of Alaska and Hawaii","interactions":[],"lastModifiedDate":"2025-05-13T15:04:13.648266","indexId":"mr51","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"51","title":"Iron in the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>The iron-ore deposits in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map; many iron-bearing deposits that are of lesser or only potential value are also shown. Because these deposits range widely in extent, two general categories of symbols are used, each of which is subdivided as explained below. The first category is for deposits of such restricted extent that they can be represented by a \"spot\": the second is for deposits which, although not necessarily extremely large in terms of volume or tonnage, are either continuous (or essentially so) or clustered in reasonably well-defined districts of numerous small occurrences.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr51","usgsCitation":"Carr, M.S., Guild, P.W., and Wright, W., 1967, Iron in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 51, Report: 20 p.; 1 Plate: 64.10 x 41.00 inches, https://doi.org/10.3133/mr51.","productDescription":"Report: 20 p.; 1 Plate: 64.10 x 41.00 inches","costCenters":[],"links":[{"id":485810,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/51/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485634,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1783.htm","linkFileType":{"id":5,"text":"html"}},{"id":179789,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/51/report-thumb.jpg"},{"id":260471,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/51/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667339","contributors":{"authors":[{"text":"Carr, Martha S.","contributorId":8169,"corporation":false,"usgs":true,"family":"Carr","given":"Martha","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":266733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guild, Philip White","contributorId":94285,"corporation":false,"usgs":true,"family":"Guild","given":"Philip","email":"","middleInitial":"White","affiliations":[],"preferred":false,"id":266734,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, W.B.","contributorId":101296,"corporation":false,"usgs":true,"family":"Wright","given":"W.B.","affiliations":[],"preferred":false,"id":266735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":157,"text":"wsp1952 - 1967 - Quality of surface waters for irrigation, Western states, 1963","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1952","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1952","title":"Quality of surface waters for irrigation, Western states, 1963","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1952","usgsCitation":"Love, S.K., 1967, Quality of surface waters for irrigation, Western states, 1963: U.S. Geological Survey Water Supply Paper 1952, viii, 148 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1952.","productDescription":"viii, 148 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1952/report-thumb.jpg"},{"id":24767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1952/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1952/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db65490b","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142028,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42325,"text":"ofr67248 - 1967 - Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","interactions":[],"lastModifiedDate":"2022-11-22T21:58:09.747382","indexId":"ofr67248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"67-248","title":"Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67248","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California: U.S. Geological Survey Open-File Report 67-248, 1 Plate: 30.88 × 40.85 inches, https://doi.org/10.3133/ofr67248.","productDescription":"1 Plate: 30.88 × 40.85 inches","costCenters":[],"links":[{"id":409554,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8203.htm","linkFileType":{"id":5,"text":"html"}},{"id":80088,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118,\n              38\n            ],\n            [\n              -118,\n              37.5\n            ],\n            [\n              -117.5,\n              37.5\n            ],\n            [\n              -117.5,\n              38\n            ],\n            [\n              -118,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a38","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68174,"text":"ha233 - 1967 - Floods in Zion Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"233","title":"Floods in Zion Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha233","isbn":"0607762357","usgsCitation":"May, V.J., and Mycyk, R.T., 1967, Floods in Zion Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 233, 1 col. map ;58 x 37 cm., on sheet 77 x 127 cm., https://doi.org/10.3133/ha233.","productDescription":"1 col. map ;58 x 37 cm., on sheet 77 x 127 cm.","costCenters":[],"links":[{"id":186052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89483,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/233/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.86749999999999,42.3675 ], [ -87.86749999999999,42.5 ], [ -87.76666666666667,42.5 ], [ -87.76666666666667,42.3675 ], [ -87.86749999999999,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b121c","contributors":{"authors":[{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":277777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mycyk, Roman T.","contributorId":58331,"corporation":false,"usgs":true,"family":"Mycyk","given":"Roman","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":277776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52607,"text":"ofr67148 - 1967 - Drilling of deep-test-monitor well at Jacksonville, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr67148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"67-148","title":"Drilling of deep-test-monitor well at Jacksonville, Florida","language":"ENGLISH","doi":"10.3133/ofr67148","usgsCitation":"Leve, G., and Goolsby, D.A., 1967, Drilling of deep-test-monitor well at Jacksonville, Florida: U.S. Geological Survey Open-File Report 67-148, 16 p., https://doi.org/10.3133/ofr67148.","productDescription":"16 p.","costCenters":[],"links":[{"id":177218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db633fa2","contributors":{"authors":[{"text":"Leve, G.W.","contributorId":64294,"corporation":false,"usgs":true,"family":"Leve","given":"G.W.","affiliations":[],"preferred":false,"id":245635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1715,"text":"wsp1608H - 1967 - Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1608H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1608","chapter":"H","title":"Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","docAbstract":"Rising water tables and the salinization of land as the result of canal irrigation threaten the agricultural economy of the Punjab. Since 1954 the Water and Soils Investigation Division of the West Pakistan Water and Power Development Authority has inventoried the water and soils resources of the Punjab and investigated the relations between irrigation activities, the natural hydrologic factors, and the incidence of waterlogging and subsurface-drainage problems. This report summarizes the findings of the investigation, which was carried out under a cooperative agreement between the Government of Pakistan and the U.S. Agency for International Development, and its predecessor, the U.S. International Cooperation Administration. \r\n\r\nLeakage from the canal systems, some of which have been in operation for more than 100 years, is the principal cause of rising water levels and constitutes the major component of ground-water recharge in the Punjab. Geologic studies have shown that virtually the entire Punjab is underlain to depths of 1,000 feet or more by unconsolidated alluvium, which is saturated to within a few feet of land surface. The alluvium varies in texture from medium sand to silty clay, but sandy sediments predominate. Large capacity wells, yielding 4 cfs or more, can be developed almost everywhere. Ground water occurring within a depth of 500 feet below the surface averages less than 1,000 ppm of dissolved solids throughout approximately two-thirds of the Punjab. It is estimated that the volume of usable ground water in storage in this part of the alluvial aquifer is on the order of 2 billion acre-feet. In the other one-third of the Punjab, total dissolved solids range from 1,000 to about 20,000 ppm. In about one-half of this area (one-sixth of the area of the Punjab) some ground water can be utilized by diluting with surface water from canals. \r\n\r\nThe ground-water reservoir underlying the Punjab is an unexploited resource of enormous economic value. It is recognized that the scientific management of this ground-water reservoir is the key to permanent irrigation agriculture in the Punjab. The West Pakistan Water .and Power Development Authority has prepared a long-range program for reclaiming the irrigated lands of the Punjab. The essential feature of this program is a proposed network of tubewells (drilled wells) located with an .average density of about one per square mile. Groundwater withdrawals will serve the dual purpose of helping to supply irrigation requirements and of providing subsurface drainage. Despite the feasibility and inherent advantages of tubewell reclamation methods, it is inevitable that just as the superposition of the canal system on the native environment caused undesirable side effects, large-scale ground-water withdrawals again will disturb the hydrologic regimen. The distribtution of withdrawals and maintenance of a favorable salt balance are two distinct, but related aspects of the ground-water budget that present potential hazards that must be considered in the design and management of the tubewell projects. The availability of ground water for irrigation diminishes from northeast to southwest, or downgradient along the doab (an area lying between two rivers) and is negligible in the centers of the lower parts of the doabs, where the ground water is too highly mineralized for use. Ground-water supplies must be developed in areas where they are available and it might become necessary, under a program of maximum exploitation of ground-water resources, to transfer supplies from outside sources to points of use in the lower parts of the doabs. \r\n\r\nSeveral factors inherent in the tubewell system will tend to depreciate the quality of ground water with time. Among these are the addition of salts leached from the soils, increased concentration of salts due .to repeated cycles of recirculation, and the possible lateral and upward encroachment of saline water in response to pumping. 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,{"id":4070,"text":"cir549 - 1967 - Economic significance of revised age relations of rocks in the Cornucopia mining district, Elko County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir549","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"549","title":"Economic significance of revised age relations of rocks in the Cornucopia mining district, Elko County, Nevada","docAbstract":"Recent geologic work in the Cornucopia mining district, a small silver-gold mining district in northwestern Elko County, Nev., has resulted in significant revision of the geological interpretation. Rocks formerly thought to be premineralization in age, but unmineralized, are now known to be postmineral extrusives, resting unconformably on the altered andesite in which the ore bodies are found. Extensions of the known productive veins may be expected at shallow depth beneath the younger volcanic rocks, and are separated from the mined part of the veins by postmineral high-angle faults that have brought the younger volcanic rocks into fault contact with the mineralized andesite. Some veins are apparently terminated against premineral faults.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior,","doi":"10.3133/cir549","usgsCitation":"Coats, R.R., 1967, Economic significance of revised age relations of rocks in the Cornucopia mining district, Elko County, Nevada: U.S. Geological Survey Circular 549, iii, 4 p. :maps. ;27 cm., https://doi.org/10.3133/cir549.","productDescription":"iii, 4 p. :maps. ;27 cm.","costCenters":[],"links":[{"id":117499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1967/0549/report-thumb.jpg"},{"id":31165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1967/0549/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62597e","contributors":{"authors":[{"text":"Coats, Robert Roy","contributorId":77131,"corporation":false,"usgs":true,"family":"Coats","given":"Robert","email":"","middleInitial":"Roy","affiliations":[],"preferred":false,"id":148117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4072,"text":"cir545 - 1967 - Marine sediment sample preparation for analysis for low concentrations of fine detrital gold","interactions":[],"lastModifiedDate":"2017-08-27T17:54:55","indexId":"cir545","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"545","title":"Marine sediment sample preparation for analysis for low concentrations of fine detrital gold","docAbstract":"Analyses by atomic absorption for detrital gold in more than 2,000 beach, offshore, marine-terrace, and alluvial sands from southern Oregon have shown that the values determined from raw or unconcentrated sediment containing small amounts of gold are neither reproducible nor representative of the initial sample. This difficulty results from a 'particle sparsity effect', whereby the analysis for gold in a given sample depends more upon the occurrence of random flakes of gold in the analyzed portion than upon the actual gold content of the sample. \r\n\r\nThe particle sparsity effect can largely be eliminated by preparing a gold concentrate prior to analysis. A combination of sieve, gravimetric, and magnetic separation produces a satisfactory concentrate that yields accurate and reproducible analyses. In concentrates of nearly every marine and beach sand studied, the gold occurs in the nonmagnetic fraction smaller than 0.124 mm and with a specific gravity greater than 3.3. The grain size of gold in stream sediments is somewhat more variable. \r\n\r\nAnalysis of concentrates provides a means of greatly increasing the sensitivity of the analytical technique in relation to the initial sample. Gold rarely exceeds 1 part per million in even the richest black sand analyzed; to establish the distribution of gold (and \r\nplatinum) in marine sediments and its relationship to source and environmental factors, one commonly needs to know their content to the part per billion range. Analysis of a concentrate and recalculation to the value in the initial sample permits this degree of sensitivity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir545","usgsCitation":"Clifton, H.E., Hubert, A., and Phillips, R.L., 1967, Marine sediment sample preparation for analysis for low concentrations of fine detrital gold: U.S. Geological Survey Circular 545, 11 p. :map ;26 cm., https://doi.org/10.3133/cir545.","productDescription":"11 p. :map ;26 cm.","costCenters":[],"links":[{"id":124628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1967/0545/report-thumb.jpg"},{"id":31166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1967/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604414","contributors":{"authors":[{"text":"Clifton, H. Edward","contributorId":46503,"corporation":false,"usgs":true,"family":"Clifton","given":"H.","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":148120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubert, Arthur","contributorId":17977,"corporation":false,"usgs":true,"family":"Hubert","given":"Arthur","affiliations":[],"preferred":false,"id":148119,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, R. Lawrence","contributorId":81478,"corporation":false,"usgs":true,"family":"Phillips","given":"R.","email":"","middleInitial":"Lawrence","affiliations":[],"preferred":false,"id":148121,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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