Sunday, April 26, 2015

Nepal's Seismic Time Bomb

At LAT, "Katmandu's poorly constructed buildings worsen quake outcome":
An exploding urban population that led to taller and often poorly constructed buildings, along with an unusually hazardous combination of geological conditions, had for years prompted warnings from scientists that the Katmandu Valley of Nepal was a seismic time bomb waiting to go off.

Saturday morning, it did.

The magnitude 7.8 earthquake and a magnitude 6.6 aftershock toppled buildings, set off a destructive avalanche on Mt. Everest and killed at least 1,805 people Saturday afternoon. That number is projected to rise as high as 10,000.

Brian Tucker, president of GeoHazards International, a California-based nonprofit that works with vulnerable communities to reduce the risks of natural disasters, spent much of the 1990s in Nepal. He was assessing what would happen if there was a reoccurrence of the magnitude 8.2 earthquake that struck the area in 1934 and left more than 10,000 dead in the Katmandu Valley. The analysis projected 40,000 deaths if a similar temblor occurred.

Others who have studied quake risks in the area more recently predicted a death toll of 100,000 or more from a large earthquake, including Roger Bilham, a professor of geology at the University of Colorado who studies Himalayan seismic activity. Just days ago, Bilham spoke to seismologists gathered in Pasadena about the risks of a major quake elsewhere in the Himalayan range. Bilham said the area west of Katmandu has been overdue for a temblor of around magnitude 8.

"Unfortunately, now it's happened, and it's a tragedy beyond belief," he said.

The area has a history of frequent seismic activity, although events as large as the one that occurred Saturday happen about once every 80 years, said Ole Kaven, a research geophysicist with U.S. Geological Survey.

Unlike the earthquakes that typically strike California, with two plates sliding past each other horizontally, the earthquake in Nepal was caused by a thrust fault, in which two plates collide. The fault also is shallow, meaning that the shaking occurs near the surface, rather than deep in the earth.

U.S. Geological Survey seismologist Lucy Jones said faults like the one that caused this earthquake are most often found under water and can produce devastating tsunamis. But the Himalayan region is different.

"This is the one place where we have a lot of people living on top of a megathrust," she said...

Also at WSJ, "How the Nepal Earthquake Happened."