The earthquake in Nepal
was so violent it moved mountains. Satellite imagery shows that the
parts of the Himalayas sank three feet—and the area around it as much as
five feet—as tectonic plates snapped under extreme pressure. But the
mountains will regain their height, slowly but surely, thanks to the
geologic forces at work.
himalayas
The European Space Agency’s Sentinel-1A radar satellite captured before
and after images of the area hit by the earthquake. The image below show
how the Eurasian plate bent, the land falling in some places (yellow)
and rising in others (blue). The area of the Himalaya’s Langtang range
sank by three feet. Everest, which was further away from the earthquake,
sank about an inch.
The Himalayas were formed, after all, by the Indian plate pushing into
the Eurasian plate. And the mountains are still growing thanks to the
constant pressure at the fault. In the earthquake, though, the plate
under Kathmandu snapped like a rubber band, causing the opposite to
happen. Tim Wright, professor of satellite geodesy at the University of
Leeds, explained what happened to the BBC:
“Between earthquake events, Nepal is being squashed and the part
(including Kathmandu) nearest the big fault underneath it is being
dragged down by the Indian plate, and [areas] further back are being
lifted up as you imagine squashing something is going to push things
up,” says Prof Wright.
“Now, during the earthquake itself what happens is the opposite. The
part that was dragged down because it was stuck at the fault – that
slips freely and rebounds up, and the part that was being squashed
upwards drops down.”
The earthquake was one sudden and violent event, but in the long run,
the Himalayas will slowly regain their height. The Indian plate will
push into the Eurasian plate, as it has for millions of years, and the
Himalayas mountains will get taller, as they have for been millions of
years.
Read More at earthchangesmedia.com/the-himalayas-dropped-3-feet-after-the-nepal-earthquake © Earth Changes Media
Sunday, May 17, 2015
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