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ES Ch 2 NOTES Earthquakes
ES Ch 2 NOTES Earthquakes

... ______________ structures. a) There are ________________________________ between a building and its foundation absorbs much of the ground motion. b) An open space around a building lets the building shake more gently than the ground it is built on. c) Shear walls that contain ___________ supports ad ...
Chilean Earthquake 2010
Chilean Earthquake 2010

... Concepion, Chiles second largest city The Nazca plate moved under and eastward of the South American plate making it a destructive plate boundary The epicentre occurred 21 miles below the earths surface The quake reported 7 aftershocks, five measured 6.0 above, in the 2 and a half hours following th ...
Earthquake Early Warning Rapid Response
Earthquake Early Warning Rapid Response

... until ...
Opportunity to Lead the Earthquake Monitoring Project at the U.S.
Opportunity to Lead the Earthquake Monitoring Project at the U.S.

... Opportunity to Lead the Earthquake Monitoring Project at the U.S. Geological Survey in Menlo Park, CA The U.S. Geological Survey Earthquake Science Center (ESC) in Menlo Park, California is hiring a Supervisory Geophysicist to lead our Earthquake Monitoring Project. This important and influential pe ...
Earthquake Lab Walkthrough
Earthquake Lab Walkthrough

... Measured (mm) = X mm 100 km distance (from pg. 2) *Make sure to cross multiply and divide ...
Word
Word

... 22. The minimum number of earthquake monitoring stations needed to determine the epicenter of an earthquake: A. 5 B. 4 C. 3 D. 2 E. 1 22. Three seismograph stations are needed to find the epicenter of an earthquake because: A. the more, the better B. at least one of the stations could have made a mi ...
scale to rate the total energy an earthquake releases
scale to rate the total energy an earthquake releases

... 13. The magnitudes take into account that seismic waves get __________ (meaning weaker) the farther the seismograph is from an earthquake. 14. Geologists use the ___________ ____________ scale to rate the total energy an earthquake releases. News reports may mention the Richter scale, the number quo ...
bogazici university - Kandilli Rasathanesi ve Deprem Araştırma
bogazici university - Kandilli Rasathanesi ve Deprem Araştırma

... http://nera-eu.org Description of the infrastructure:  Istanbul Earthquake Rapid Response System To provide earthquake rapid response information one hundred strong motion accelerometers were placed in populated areas of Istanbul to constitute a network that will enable rapid shake map and damage a ...
Influence of fault heterogeneity on the frequency
Influence of fault heterogeneity on the frequency

... Typical realizations produced between 4 to 6 individual earthquakes ranging in event magnitudes between those characteristic of the minimum patch size for nucleation and the size of the model fault. The resulting aggregate frequency-magnitude distributions were characterized well by a power-law scal ...
Preface
Preface

... northeastern Japan. Slip area of this great earthquake extends about 500 km long and about 200 km wide with the average slip of about 10–20 m, rupturing about two thirds of the megathrust zone east of the entire northeastern Japan arc. Northeastern Japan was severely damaged by this earthquake; espe ...
QUIZ 5 - Brooklyn College
QUIZ 5 - Brooklyn College

... 15. The mantle makes up roughly 80% of the Earth's volume. o ...
Homework Set 2
Homework Set 2

... 1. Like other fault types, thrust faults tend to be segmented. This poses a problem when trying to determine the along-strike length of blind thrust fault segments. Why is it important to determine the lengths of these segments and what evidence might we look for (or techniques we might use) to iden ...
Earthquake Damage Unit
Earthquake Damage Unit

... • May be caused in two ways • Faulting- causes a sudden drop or rise in the ocean floor • A large mass of sea water also drops or rises with the ocean floor • This water then churns and causes violent movement of water resulting in a Tsunami • Underwater landslides – water above a landslide is throw ...
Problem Set #1
Problem Set #1

... Earthquakes and Seismic Hazards, Fall 2001 ...
New Earthquake Review
New Earthquake Review

... 2. Define primary and secondary waves. 3. Which wave arrives first? 4. Which wave causes the most damage? ...
Earthquake Scavenger Hunt The study of earthquakes is called __
Earthquake Scavenger Hunt The study of earthquakes is called __

... resistant is called ____________________________________. 28. List 5 types of earthquake-resistant building technologies. ___________________________________________________ ___________________________________________________ 29. List 4 items you should have ready in case of an earthquake. _________ ...
PDF file of Chapter 11 lecture - Earthquakes
PDF file of Chapter 11 lecture - Earthquakes

... (P, S) and surface waves Different types of seismometers needed to record vertical and horizontal ground motion Records obtained called seismograms (above) ...
MARIKINA VALLEY FAULT
MARIKINA VALLEY FAULT

... MARIKINA VALLEY FAULT SYSTEM PHIVOLS: MARIKINA VALLEY FAULT (RIGHT LATERAL) CAPABLE OF TRIGGERING 7.2 MAGNETUDE EARTHQUAKE •CARBON 14 PALEOSEISMIC STUDY REVEALED 200 – 400 YEARS RECURRENCE INTERVAL OF MOVEMENT AT 6-7 MAGNETUDE • THE LAST EARTHQUAKE WAS 200 YEARS BP • DIGDIG FAULT IN NORTHERN LUZON ...
the adaptable Word resource
the adaptable Word resource

... Many factors affect the impact of an earthquake on a country. The distance from the epicentre and the magnitude of the earthquake are two factors for example. The level of the country’s economic development will also have a significant effect.  Less economically developed countries (LEDC) have few ...
A country`s wealth and the effects of an earthquake
A country`s wealth and the effects of an earthquake

... Many factors affect the impact of an earthquake on a country. The distance from the epicentre and the magnitude of the earthquake are two factors for example. The level of the country’s economic development will also have a significant effect.  Less economically developed countries (LEDC) have few ...
Presentation
Presentation

... Develop an argument either for or against one statement based on your experimentation with the earthquake machine. ...
Fukushima Earthquake
Fukushima Earthquake

... • This earthquake was of a magnitude of 9.0 on the Richter magnitude scale; • 15,845 confirmed deaths; • 5,893 injured; • 3,380 people missing • Over 125,000 buildings damaged or destroyed; • Insured losses from earthquake alone at US$14.5 to $34.6 billion. ...
Earthquake Terms
Earthquake Terms

... increase of about 30 times more energy released than the previous whole number represents. Therefore, an earthquake measuring 6.0 is about 30 more times more powerful than one measuring 5.0. Seismic Waves: Vibrations that travel outward from the earthquake fault at speeds of several miles per second ...
Earthquakes
Earthquakes

... and bridges, topple utility poles, and fracture gas and water mains. • S waves can put stress on buildings to tear them apart. Also trigger landslides or ...
Do Now: Earthquake review
Do Now: Earthquake review

... Although the San Andreas Fault is also plate boundary, the stresses applied are Strike-slip from shearing making it also a __________________________ fault. What is an upward fold in rock layers? anticline What type of fault is the result of one rock layer sliding over another at a low angle? Thrust ...
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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.
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