3 edition of Three component long-period data for the 1949 South Puget Sound, Washington earthquake found in the catalog.
Three component long-period data for the 1949 South Puget Sound, Washington earthquake
|Statement||Glenn Eli Baker|
|Series||Open-file report -- 85-613, U.S. Geological Survey open-file report -- 85-613|
|Contributions||Geological Survey (U.S.)|
|The Physical Object|
INTRODUCTION Canada extends over about 10 million , making it the second largest country in the world. It has km of coastline bordering three oceans, elevations ranging from sea level to m on Mt. Logan, and is subject to extreme weather conditions; [degrees]C to 45[degrees]C; up to 49 cm of rain in a hour period, and up to . As of 30 June , the Washington National Guard had a strength of 60 officers and 1, enlisted men and was organized as follows: LIST OF OFFICERS AND ORGANIZATIONS OF THE WASHINGTON NATIONAL GUARD COMMANDER-IN-CHIEF - Acting Governor Louis F. Hart Adjutant General - Brig. Gen. Maurice Thompson, Seattle STATE STAFF CORPS AND .
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Get this from a library. Three component long-period data for the South Puget Sound, Washington earthquake. [Glenn Eli Baker; Geological Survey (U.S.)]. Teleseismic P, SH, and SV first motions and SH to SV amplitude ratios recorded at eight teleseismic receivers from the magnitude Olympia, Washington, earthquake in combination with data from three stations at regional distances were utilized in a grid testing routine to constrain focal mechanism.
Identification of the pP phase places the event at 54 km Cited by: Source Investigation and Comparison of the, and Earthquakes, Cascadia Subduction Zone, Western Washington October Pure and Applied Geophysics (10) 3 Earthquake Basics 1.
Introduction. The problem is that earthquakes start out many miles beneath the surface, too deep for us to observe them directly.
So we study them from afar by (1) observing the geological changes at the ground surface, (2) analyzing the symphony of earthquake vibrations recorded on seismographs, and (3) monitoring the tectonic changes in.
(a) Map of the Puget Sound area. (b) Map of the Seattle basin area. Black rectangle delineates the area covered by the 3D velocity model.
Thin solid lines indicate the locations of north–south. Suggested Citation: "3. Facing the Earthquake Threat." National Research Council.
Living on an Active Earth: Perspectives on Earthquake Science. Washington, DC: The National Academies Press. doi: / E arthquakes rival all other natural disasters inthethreat they pose to human life and habitat.
The Northern Pacific built its main line from Kalama on the Columbia River to Tacoma on Puget Sound, closely following the Cowlitz Trail route through the South Sound country. The Lewis County Historical Museum, and the Tenino Depot Museum are both housed in classic depots dating from the heyday of the Northern Pacific Railroad.
With the modern three-component networks in the Northwest and adjacent parts of Canada, it is possible to determine the push or pull relationship at many stations, leading to information about whether the earthquake is on a reverse fault, a normal fault, or a strike-slip fault (Figure ).
earthquake-related lore from the Puget Sound area. A’yahos, the AD Seattle earthquake and. earthquake lore from the Puget Sound area. along the Seattle fault. The Seattle fault is a multi-stranded east –west. striking reverse fault cutting across Puget Sound, through downtown Seattle, and across Lake.
Washington. Although geophysical. earthquake-related lore from the Puget Sound area. A’yahos, the AD Seattle earthquake and. earthquake lore from the Puget Sound area. along the Seattle fault.
The Seattle fault is a multi-stranded east –west. striking reverse fault cutting across Puget Sound, through downtown Seattle, and across Lake.
Washington. Although geophysical. Full text of "Use of Seismic Intensity Data to Predict the Effects of Earthquakes and Underground Nuclear Explosions in Various Geologic Settings" See other formats.
SEISMIC WAVES AND EARTHQUAKE LOCATION J.R. Kayal Geological Survey of India, 27, J.L. Nehru Road Road, Kolkata – email: [email protected] SEISMIC WAVES Two basic types of elastic waves or seismic waves are generated by an earthquake; these are body waves and surface waves.
example, km [ mi] of a m [ ft] high cliff was dislodged into Puget Sound near Tacoma during the Earthquake of Olympia, Washington. Settlement and liquifaction may occur on filled land where a high water table exists. Such areas exist along the Port Orchard to Retsil area and parts of the south Bremerton area.
Full text of "Draft environmental impact statement on the proposed Montana Power Company, Puget Sound Power & Light Company, Portland General Electric Company, Pacific Power and Light Company, and Washington Water Power Company Colstrip Electric Generating Units 3 & 4, kilovolt transmission lines from Colstrip to Hot Springs, Montana, and associated facilities".
So the Olympia, Washington, Earthquake of on Apwould be considered to have released the energy of more than thirty earthquakes the size of the Klamath Falls, Oregon, Earthquake of Septemwhich was magnitude 6.
LIST OF TABLES Table Page River discharge data for the Pacific Northwest 24 Monthly averages of wind direction and scalar speed (mph) at selected shore stations 30 Frequency and velocity of winds at three stations on the Washington-Oregon coast 32 Resultant wind speed (knots) and direction by month measured from lightships.
Three days later, 17 April (14 April was lost crossing the ° Meridian), the Sabine fueled the Enterprise group, and the Cimarron did the same for the Hornet group, with some destroyers getting their fuel from the heavy ships. This was at latitude 35°'30' N.
Historical Section. Bureau of Naval Personnel. "The Sicilian Campaign: Operation 'Husky,' July-August, " (Washington, DC: ). [This manuscript, identified as United States Naval Administrative History of World War II #c, is located in the Navy Department Library's Rare Book.
The first step in hazard assessment is to identify the probable seismic sources around a given site. Figure 3 shows the seismo-tectonic setup of Manipur (GSI ) superposed with the epicentres of past can be seen from figures 3 and 4 that there are many active faults surrounding Manipur.
These faults can be attributed to tectonic activity in the. Errors brought to the attention of the publisher and verified to the satisfaction of the publisher will be corrected in future editions.
Macmillan Reference USA Park Avenue South, 9th Floor New York, NY Macmillan Reference USA Drake Road Farmington Hills, MI LIBRARY OF CONGRESS CATALOGING-IN-PUBLICATION DATA. Department of Civil Engineering University of Southern California Los Angeles, CAU.S.A. ABSTRACT The modern techniques for digitization of strong-motion accelerograms and subsequent data processing were first developed in the late s and early s, at which time the only available digitization technology was semi-automatic.Figure 2.
This vertical coastal cliff of basalt in the San Juan Islands of northern Puget Sound, Washington, has a narrow erosional ramp at the base, but no beach. Because of the strength of the rock and low wave energy, the erosion rate is negligible, with .The Nisqually, Wash.
quake at a.m. on Feb. 28, registered on the Richter Scale and was felt throughout the greater Puget Sound region. That quake gave staff members a forewarning of what it was like to experience a sizable seismic shaking, as the epicenter is just 50 miles south of Bremerton.