Earthquake Safety

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The document provides safety tips for different locations and situations during an earthquake. It recommends having a safety kit prepared beforehand and knowing what to do during shaking based on your location. The key actions are to drop, cover, and hold on wherever you are until the shaking stops. After an earthquake, expect aftershocks and check for damage and injuries before leaving shelter.

Technology

Earthquake SAFETY By: Nicholai B. Rombaon Period 6 Mr. Dave Genis

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Earthquake Safety Week 2017 from 15-21 January 2017 Bihar State Disaster Management Authority has announced Earthquake Safety Week. Bihar is located in the high seismic zone that falls on the boundary of the tectonic plate joining the Himalayan tectonic plate near the Bihar-Nepal Border and has six sub-surface fault lines moving towards the Gangetic planes in four directions. Of the 38 districts of Bihar, 8 districts fall in seismic zone V of which 2 districts (Madhubani and Supaul) fall entirely in seismic zone V while 24 districts fall in seismic zone IV and 6 districts in seismic zone III with most districts falling under multiple seismic zones (i.e. either seismic zone V & IV or seismic zone IV & III). The state has in the past experienced major earthquakes; the worst was the 1934 earthquake in which more than 10,000 people lost their lives, followed by 1988 earthquake and recent earthquake was the Sikkim earthquake in September 2011. The new and growing urban centres in the state where building codes and control mechanisms are not enforced, earthquake remains a major threat to cities. This could result in social infrastructures such as schools and hospitals that are not built to be earthquake resistant could lead to serve damage and loss of lives as well.

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Sagaing Fault Sagaing Fault is a major fault in Myanmar, a continental transform fault between the Indian plate and Sunda Plate that connects spreading centers in the Andaman Sea and the continental convergence zone along the Himalayan front. It passes through populated cities of Mandalay, Yamethin, Pyinmana, the capital Naypyidaw, Toungoo and Pegu before dropping off into the Gulf of Martaban, over 1200 kilometers.Global Positioning System campaigns revealed a right-lateral slip rate of 18 mm/yr.Different segments of the fault ruptured in May-1930, Dec-1930, 1931 and 1946.[4] The fault ruptured in 1930, causing a Magnitude 7.3 quake and likely a local tsunami at Bago, causing over 500 deaths. http://www.sagaingfault.info/ http://www.earthobservatory.sg/project/active-faults-and-seismic-hazard-myanmar#zoom=1&lat=18.97903&lon=102.39259&layers=0B0TT http://www.geologie.ens.fr/~vigny/articles/2002JB001999.pdf

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