Discover Civil may | Page 22

Construction Issue April 25, 2015, Nepal Earthquake, also known as the Gorkha Earthquake, shook Nepal with a magnitude of 7.8 leaving over 8,800 people dead and 23,000 injured. A major aftershock with a magnitude of 7.3 followed on 12 May killing more than 200 people and injuring more than 2,500 people. The earthquake also increased the risk of landslides and spread of disease epidemics in the country due to population displacement and impacts on water and sanitation systems. Millions of people were left homeless and driven away from their homes and livelihoods as they tried to escape the disaster. It was the worst natural disaster to strike Nepal since the 1934 Nepal Bihar Earthquake but it is very unlikely to be the last. Recently Japan too suffered back to back earthquakes on 14th & 16th of April 17, 2016 resulting in severe in and around Kumamoto, with numerous structures collapsing and catching fire. But the loss of life was far less than that of Nepal. Why? Japan is one of the most earthquake prone regions in the world, so its modern buildings and infrastructure are designed to resist collapse. Many lessons were learned from the Kobe earthquake of 1995 that killed 6,400 people and forced a reassessment of the building regulations for both residential offices and transport infrastructure. Keep in mind that Japan, one of the world’s most technologically advanced countries, has the best earthquake preparation and infrastructure in the world. Buildings stay upright, warning systems work, and citizens are drilled in emergency procedures. You’re probably more likely to survive an earthquake in Japan than China, India, or Indonesia, where building codes can be lax. Still, earthquakes are notoriously hard to predict. First of all we must understand, how do earthquake or tsunami happen? Well it’s all about movement of tectonic plates as we have been learning since our high school. Earthquakes happen along cracks in the earth's surface, called fault lines, and can be felt over large areas, although they usually last less than one minute. If we take a look at few recent earthquake in last decade we can clearly see that it’s all about the movement of tectonic plates. In 2001, the Gujarat Earthquake is believed to happen due to intraplate movement between Indian Plate and Eurasean Plate. In 2015, the devastating Nepal Earthquake was due to the plate movement between the same two plates. While a major part of Japan is on Eurasean Plate, Japan is situated, on the joint of four different plates. So we have got the Pacific plate and the Philippine