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Mohandes Magazine Fall-Winter Edition 2018

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Life on Active Faults: Connecting the Iranian<br />

diaspora to give hope and to help reduce, or<br />

mitigate the effects of natural disasters<br />

By Arsalan Mohajer, PhD., D.I.C., P.Geo.<br />

Earthquakes don’t kill, weak buildings do – poorly constructed buildings can be viewed as ticking<br />

time bombs, for vulnerable communities in certain active fault zones in Iran and elsewhere<br />

around the world. A comparative review of rates of casualties’ shows destructive impact in Iran is<br />

much higher than other earthquake prone countries that are better prepared.<br />

Yet again, on November 12, 2017 at 16:18 local time, a magnitude (M) 7.3 earthquake devastated a<br />

large area in the western Kermanshah province in Iran, near the Iraq border. It was the deadliest<br />

global Earthquake of 2017.<br />

The Energy released by a M7.3 earthquake, at 29km depth in western Iran was equivalent to 89 Hiroshima<br />

Atomic Bombs (89 x 15 Kiloton TNT).<br />

Local news reported over 700 dead and 9,000 injured in many villages and small towns of the province.<br />

Luckily, the mountainous area is not densely populated otherwise the extent of the disaster<br />

would have been much larger.<br />

Tehran awakes with an earthquake fright on December 20, 2017, too.<br />

Just before 11:30 p.m. local time, a M4.9 earthquake struck the west-end of the city of Tehran with a<br />

population of 8.3 million in Tehran proper, and 14 million including the surrounding communities<br />

(Fig. 1)<br />

The epicenter of the 2017 Tehran Earthquake was in the Malard region just east of a M5.7 earthquake<br />

in 1876, and northeast of Qazvin which experienced a M7 earthquake in 1962. Such a storied past<br />

indicates that the Tehran region is within an earthquake hazard zone and that another major earthquake<br />

is overdue. There are history of five damaging earthquakes in old city of Rey to the south, in<br />

addition to statistically significant recorded events since early 20th century in Tehran region. Therefore,<br />

probabilistic estimates of M7 earthquakes suggest a return period of 170-200 years. Nonetheless,<br />

based on deterministic evaluation of active faults in the region such occurrence is inevitable,<br />

and needs to be incorporated in design of the built environment.<br />

The over-due event in Tehran region could kill in hundreds of thousands, and could cause over a<br />

million-population displacement. Some of the main reasons for such calamity are; extensive vulnerability<br />

to old and weak buildings, relative complacency with enforcing building codes and soft soilstructure<br />

interaction at the southern part of the city, limited open spaces for rescue and recovery,<br />

and lack of preparedness drills at schools, offices and homes.<br />

30 MOHANDES MAGAZINE

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