Experts
had warned of the danger to the people of Katmandu for decades. The
death toll in Nepal on Saturday was practically inevitable given the
tectonics, the local geology that made the shaking worse and the lax
construction of buildings that could not withstand the shaking.
GeoHazards
International, a nonprofit organization in Menlo Park, Calif., that
tries to help poorer, more vulnerable regions like Nepal prepare for
disasters, had noted that major earthquakes struck that region about
every 75 years. In
1934 — 81 years ago — more than 10,000 people died in a magnitude 8.1
earthquake in eastern Nepal, about six miles south of Mount Everest. A
smaller quake in 1988 with a magnitude of 6.8 killed more than 1,000
people.
Brian
Tucker, president and founder of GeoHazards, said that in the 1990s,
his organization predicted that if the 1934 quake were to happen again,
40,000 people would die because of migration to the city where tall,
flimsily built buildings would collapse.
In
an update just this month, GeoHazards wrote, “With an annual population
growth rate of 6.5 percent and one of the highest urban densities in
the world, the 1.5 million people living in the Katmandu Valley were
clearly facing a serious and growing earthquake risk.”
The organization helped set up a local nonprofit to continue preparations, including the reinforcement of schools and hospitals.
Saturday’s
earthquake occurred to the northwest of Katmandu at a relatively
shallow depth, about nine miles, which caused greater shaking at the
surface, but at magnitude 7.8, it released less energy than the 1934
quake.
Roger
Bilham, a professor of geological sciences at the University of
Colorado who has studied the history of earthquakes in that region, said
that the shaking lasted one to two minutes, and the fault slipped about
10 feet along the rupture zone, which stretched 75 miles, passing under
Katmandu.
The earthquake “translated the whole city southward by 10 feet,” Dr. Bilham said.
Aftershocks as large as magnitude 6.6 have occurred mostly to the northeast of Katmandu. It is possible that the Saturday quake is a preface to an even larger one, but Dr. Bilham said that was unlikely.
Katmandu
and the surrounding valley sit on an ancient dried-up lake bed, which
contributed to the devastation. “Very, very soft soil, and the soft soil
amplifies seismic motion,” Dr. Tucker said. Steep slopes in the area are also prone to avalanches like the one that the quake triggered on Mount Everest on Saturday. Katmandu is not the only place where a deadly earthquake has been expected.
But
not everywhere has been complacent. Over the past 76 years, many
earthquakes have occurred along a fault in northern Turkey, starting in
the eastern part of the country and progressing west, toward Istanbul.
An earthquake in 1999 killed more than 17,000 people, mostly in the city
of Izmit, east of Istanbul. The expectation is that the epicenter of
the next big earthquake will be in or around Istanbul.
“Istanbul
is the place that has been most aggressive in enforcing building
codes,” Dr. Tucker said. “I think Istanbul has been doing a good job.”"
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