Publications
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Effects of the earthquake of March 27, 1964, on the Alaska Railroad Effects of the earthquake of March 27, 1964, on the Alaska Railroad
In the 1964 Alaska earthquake, the federally owned Alaska Railroad sustained damage of more than $35 million: 54 percent of the cost for port facilities; 25 percent, roadbed and track; 9 percent, buildings and utilities; 7 percent, bridges and culverts; and 5 percent, landslide removal. Principal causes of damage were: (1) landslides, landslide-generated waves, and seismic sea waves that...
Authors
David S. McCulloch, Manuel G. Bonilla
Bibliography of the lunar surface Bibliography of the lunar surface
The term "surface" in this bibliography is defined to include landforms and surface materials and the nature of, and processes responsible for, their physical characteristics. References are divided into two listings: (1) Surface features and materials; and (2) Telescopic observations. The former is accompanied by a subject index, the latter by a locality index.
Authors
Jacquelyn H. Freeberg
A computer program to trace seismic ray distribution in complex two-dimensional geological models A computer program to trace seismic ray distribution in complex two-dimensional geological models
A computer program has been developed to trace seismic rays and their amplitudes and energies through complex two-dimensional geological models, for which boundaries between elastic units are defined by a series of digitized X-, Y-coordinate values. Input data for the program includes problem identification, control parameters, model coordinates and elastic parameter for the elastic...
Authors
Nazieh K. Yacoub, James H. Scott
Micromineralogy of silver-bearing sphalerite from Flat River, Missouri Micromineralogy of silver-bearing sphalerite from Flat River, Missouri
Detailed mineralogical and chemical study of sphalerite-rich lead ores from Flat River, Mo., confirms the presence of anomalous amounts of silver in the sphalerite. Although silver is closely associated with chlorine and no silver sulfide minerals were identified, geochemical considerations indicate the silver may be in the form of discrete submicron-size grains of sulfide rather than...
Authors
Charles M. Taylor, Arthur S. Radtke
Structural geology of the Quad-Wyoming-Line Creeks area, Beartooth Mountains, Montana Structural geology of the Quad-Wyoming-Line Creeks area, Beartooth Mountains, Montana
The Quad-Wyoming-Line Creeks area is in the northeastern part of the Beartooth Mountains of Montana. The rocks of the area consist mainly of banded migmatite, granitic gneisses, amphibolite, quartzite, and agmatite; small amounts of biotite schist and biotite gneiss, iron-silicate rocks, ultramafic rocks, mafic dikes, and felsic porphyries are also present. Quartzite outcrops...
Authors
Lawrence C. Rowan
Photogrammetry with surface-based images Photogrammetry with surface-based images
Stereoscopic pictures returned by surface-based imaging systems can be used to reconstruct the topography of landing sites on Mars and other planets. Large surface relief with respect to distance and the large scale variation inherent in surface-based pictures produce problems in stereoscopic measurement very different from those presented by high altitude photography. Optical-mechanical...
Authors
Raymond M. Batson
Geologic setting of the lunar samples returned by the Apollo 11 mission Geologic setting of the lunar samples returned by the Apollo 11 mission
The Apollo 11 LM landed approximately 20 km south-southwest of the crater Sabine D in the southwestern part of Mare Tranquillitatis ( fig. 3-1 ). The landing site is 41.5 km north-northeast of the western promontory of the Kant Plateau (ref. 3-1 ), which is the nearest highland region. The Surveyor 5 spacecraft is approximately 25 km north-northwest of the Apollo 11 landing site, and the...
Authors
E.M. Shoemaker, N. G. Bailey, R. M. Batson, D.H. Dahlem, T.H. Foss, M. J. Grolier, E. N. Goddard, M. H. Hait, H. E. Holt, K.B. Larson, J. J. Rennilson, G. G. Schaber, D. L. Schleicher, H.H. Schmitt, R. L. Sutton, G.A. Swann, A. C. Waters, M.N. West
Effects of the earthquake of March 27, 1964, on various communities Effects of the earthquake of March 27, 1964, on various communities
The 1964 earthquake caused wide-spread damage to inhabited places throughout more than 60,000 square miles of south-central Alaska. This report describes damage to all communities in the area except Anchorage, Whittier, Homer, Valdez, Seward, the communities of the Kodiak group of islands, and communities in the Copper River Basin; these were discussed in previous chapters of the...
Authors
George Plafker, Reuben Kachadoorian, Edwin B. Eckel, Lawrence R. Mayo
Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska
During the 1964 Alaska earthquake, tectonic deformation uplifted the southern end of Montague Island as much as 33 feet or more. The uplifted shoreline is rapidly being modified by subaerial and marine processes. The new raised beach is formed in bedrock, sand, gravel, and deltaic bay-head deposits, and the effect of each erosional process was measured in each material. Fieldwork was...
Authors
M. J. Kirkby, Anne V. Kirkby