• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Seismic Hazard Analysis of Low Seismic Regions, Visakhapatnam
Seismic Hazard Analysis of Low Seismic Regions, Visakhapatnam

... of earthquakes took place with low to high magnitudes. Some areas earlier considered stable have experienced severe damages caused by earthquakes. Noticeable earthquakes have occurred in stable regions like Latur in Maharashtra, Bhuj in Gujarat and Jabalpur in Chhattisgarh. Present study used probab ...
Lll - ESG4 Conference @ UCSB
Lll - ESG4 Conference @ UCSB

... We used pseudo-velocity response spectra to compare with our formulas. First, we calculated 5% damped acceleration response time histories with natural periods of T=0.1, 0.3, 1.0, 3.0, of two horizontal components and took the maximum value from their vector sum history. Second, we divide the maximu ...
preparing a data base for estimating seismic damage on buildings
preparing a data base for estimating seismic damage on buildings

... Within the data, the type of construction system comprises skeletal and panel constructions of reinforced cement and massive construction systems, with variants of reinforcement (horizontal or horizontal and vertical ring beams) and variants of inter-storey construction (stiff interstorey constructi ...
Geology 101 Name(s): Earthquakes and Seismic Hazards in
Geology 101 Name(s): Earthquakes and Seismic Hazards in

...  What type of plate boundary is associated with these Earthquakes? (hint: check figure 10-3 or 1-21 in your book if you can’t remember). ...
FRICTION PROBLEMS IN EARTHQUAKE SOURCE MECHANICS
FRICTION PROBLEMS IN EARTHQUAKE SOURCE MECHANICS

... The shear stress acting on both walls of the fault zone thickness is commonly used for the constitutive formulation. The shear stress acting on individual asperities, gauge fragments, and cracks contained in the fault zone or the shear stress acting on the real, macroscopic rupture surfaces formed i ...
Earthquake-induced Landslides in Colombia
Earthquake-induced Landslides in Colombia

... intense rainfalls where reported the same day inducing a rockslide that dammed the Suaza River (Ramirez, 1975). Rockfalls and rockslides developed in steep slopes in the serrated low hills of Tertiary sandstones south of Patia River were induced during the December 1979 earthquake. Coherent slides. ...
Investigation of Expected Seismic Performance on Existing Buildings: A Case Study
Investigation of Expected Seismic Performance on Existing Buildings: A Case Study

... ABSTRACT: In India the Himalayan belt lies near the fault separating Indo-Australian and Eurasian plate. But it is natural that this area is seismically active and lies in earthquake zone IV. Beside this fact, most of buildings in Himachal Pradesh have poor structural and constructional quality. In ...
1 (a) Explain elastic rebound theory
1 (a) Explain elastic rebound theory

... (b) Explain the classification of earthquake waves. (c) Explain fault, dip and their role in formation of earthquake. (d) Explain the principle of working of a seismograph with the help of sketches. (e) Explain magnitude of earthquake` (25 marks) OR 2 (a) Explain modified Mercalli’s scale of intensi ...
Deformation and seismicity near Sabancaya volcano, southern Peru
Deformation and seismicity near Sabancaya volcano, southern Peru

... global catalogs, however, since early 2013 seismicity has greatly increased—the U.S. Geological Survey (USGS) catalog reports nine earthquakes in 2013 within 50 km of Sabancaya and with depths less than 30 km, while only seven earthquakes total were reported between 1973 and 2012. Several Mw > 5 ear ...
Christchurch Earthquake
Christchurch Earthquake

... have a Higher Source Strength? No. • The event term is a source parameter, not a path  or site parameter • If the Christchurch event had a high event term,  we would expect its ground motions to be large  at all distances, which was not the case • This suggests that factors other than source, i.e.  ...
Exploring E Turkey - Scientific Research Publishing
Exploring E Turkey - Scientific Research Publishing

... connecting the seismic events with the atmospheric events. Weather precursors to earthquakes are the one-to-one correlation. Rainfall is always associated and accompanied with any one of the weather conditions like heat waves, wildfire, strong winds and snow fall. Among the list of weather precursor ...
Offshore faults summary - West Coast Regional Council
Offshore faults summary - West Coast Regional Council

... Seismic research by NIWA scientists off the West Coast of the South Island has identified faults capable of causing earthquakes with magnitudes of up to 7.8. Their work in reassessing the faults will be important for updating the New Zealand National Seismic Hazard Model which combines historic and ...
Geological Survey of Denmark and Greenland Bulletin 26
Geological Survey of Denmark and Greenland Bulletin 26

... Assessment of earthquake hazard is improved if geological and geodetic data are included in addition to seismological data. In earthquake regions like Japan and California, palaeoseismology combines data from geology and seismology, and networks of permanent GPS (global positioning system) stations ...
THE CASE FOR AN ADVANCED NATIONAL EARTHQUAKE
THE CASE FOR AN ADVANCED NATIONAL EARTHQUAKE

... Canadian seismic hazard maps have been successively refined as new information from significant earthquakes has been assessed. Three generations of seismic hazard maps have been produced at roughly 15-year intervals (1953, 1970, 1985; see Fig. 2), and a fourth generation is now justified (Basham, 19 ...
Predicting the Impact of Large Magnitude Earthquakes
Predicting the Impact of Large Magnitude Earthquakes

... bringing together researchers from six countries, Chavez connected with computational scientists at the Science & Technology Facilities Council’s (STFC) Daresbury Laboratory. With access to the Cray XT4 supercomputer HECToR, the UK’s largest, fastest and most powerful academic supercomputer, the Dar ...
Get PDF - Wiley Online Library
Get PDF - Wiley Online Library

... the following deformation sources, with parameters shown in Table 1. Left-lateral oblique thrust motion is associated with the main shock and bounds the southeast margin of the aftershock zone. Movement occurred on shallow low-angle northward thrusts in the West Coyote Hills and on a fairly extensiv ...
I gained more knowledge and skills. I was also able to network and
I gained more knowledge and skills. I was also able to network and

... implement practical measures to safeguard these buildings. This can be done with support from other institutions that have in-depth knowledge on this field. In addition, academic institutions and professional organizations need to enhance their capacity in earthquake disaster mitigation. The other s ...
Seismic Assessment of Existing Buildings
Seismic Assessment of Existing Buildings

... The responsible by the construction process should present external revision documents, assuming the responsibility for the quality of the final product and, if possible, insurance covering seismic risk. ...
Earthquakes in Eastern Canada - Comptes
Earthquakes in Eastern Canada - Comptes

... In light of the number and the magnitude of some eastern Canadian earthquakes (Table 1), it is remarkable that only two possible cases of direct casualties are known. Direct casualties are those caused directly by the earthquake vibrations or the surface rupture and not by the consequences (such as ...
Exercise 2: Geologic Structures
Exercise 2: Geologic Structures

... relocations (catalog from Hauksson (2000) with a vertical error cutoff of 1.5 km). We specifically investigate (1) the deepening of the aftershocks relative to the background seismicity, (2) the time constant of the postseismic shallowing of the deepest earthquakes. Figure 18.1 shows the time-depend ...
STRONG-MOTION SEISMOGRAPH NETWORK OPERATED BY
STRONG-MOTION SEISMOGRAPH NETWORK OPERATED BY

... deeper boreholes are constructed and 21 of them are deeper than 1000 m (Table 2). Instrumentation used for the K-NET and KiK-net is basically the same. The sensor being used is a V403 or V404 tri-axial force-balance accelerometer with a natural frequency of 450 Hz and a damping factor of 0.707, whi ...
Earthquake Vulnerability and the State-of-the
Earthquake Vulnerability and the State-of-the

... Design into the Retrofitting and New Construction of Buildings Whenever possible, ground improvement techniques or seismic isolation of buildings should be concomitant with structural retrofitting of buildings. The structural approach has been increasingly being studied during the last decades, citi ...
Wood-Frame Construction in Past Earthquakes
Wood-Frame Construction in Past Earthquakes

... Wood-frame construction is by far the most common housing type in Canada, the USA and New Zealand for singlefamily and low-rise multi-family dwellings. This type of building is also gaining acceptance in other parts of the world, including Japan. In the last few decades a large number of wood-frame ...
Unit - mrsmertens
Unit - mrsmertens

... released. When an earthquake occurs, seismic waves travel through the earth and can be measured by a seismograph (see the background section of the Earthquake Fingerprints activity for more information). Most earthquakes (particularly the largest ones) occur at the boundary between two tectonic plat ...
Periodic Slow Earthquakes from the Cascadia Subduction Zone
Periodic Slow Earthquakes from the Cascadia Subduction Zone

... Continuous geodetic measurements from convergent margins have shown that deep transient creep events can release large amounts of strain energy without detectable seismic shaking, and they are thus known as slow or silent earthquakes. Because subduction zones generate the largest earthquakes, seismi ...
< 1 ... 8 9 10 11 12 13 14 15 16 ... 23 >

April 2015 Nepal earthquake



The April 2015 Nepal earthquake (also known as the Gorkha earthquake) killed more than 9,000 people and injured more than 23,000. It occurred at 11:56 NST on 25 April, with a magnitude of 7.8Mw or 8.1Ms and a maximum Mercalli Intensity of IX (Violent). Its epicenter was east of the district of Lamjung, and its hypocenter was at a depth of approximately 8.2 km (5.1 mi). It was the worst natural disaster to strike Nepal since the 1934 Nepal–Bihar earthquake.The earthquake triggered an avalanche on Mount Everest, killing at least 19, making April 25, 2015 the deadliest day on the mountain in history. The earthquake triggered another huge avalanche in the Langtang valley, where 250 people were reported missing.Hundreds of thousands of people were made homeless with entire villages flattened, across many districts of the country. Centuries-old buildings were destroyed at UNESCO World Heritage sites in the Kathmandu Valley, including some at the Kathmandu Durbar Square, the Patan Durbar Square, the Bhaktapur Durbar Square, the Changu Narayan Temple and the Swayambhunath Stupa. Geophysicists and other experts had warned for decades that Nepal was vulnerable to a deadly earthquake, particularly because of its geology, urbanization, and architecture.Continued aftershocks occurred throughout Nepal at the intervals of 15–20 minutes, with one shock reaching a magnitude of 6.7 on 26 April at 12:54:08 NST. The country also had a continued risk of landslides.A major aftershock occurred on 12 May 2015 at 12:51 NST with a moment magnitude (Mw) of 7.3. The epicenter was near the Chinese border between the capital of Kathmandu and Mt. Everest. More than 200 people were killed and more than 2,500 were injured by this aftershock.
  • studyres.com © 2026
  • DMCA
  • Privacy
  • Terms
  • Report