Houston home journal. (Perry, GA) 2007-current, September 12, 2007, Page 9, Image 87
Why the Earth
quakes and moves
THE UNIMAGINABLE forces be
hind earthquakes and volcanoes
are no secret Yet the notion that
these forces cause whole continents to
move is barely as old as the Beatles.
In the 19605, the process known as
plate tectonics became clear when re
searchers were mapping the deep sea
in detail. They realized the ocean floors
were spreading apart along mid-ocean
ridges, where upwelling magma con
stantly created new material; in other
places the continents were slowly col
liding. In essence, the map was moving.
Seven major plates and many smaller
ones make up the lithosphere, the outer
surface of the Earth that’s up to 155
miles thick in some
parts. Those enor
mous plates slide
over a layer of
molten rock, the
asthenosphere, at
the blistering rate
of 0.5 to 4 inches
per year.
The San Andreas
fault, where the Pa
cific and North
American plates
scrape crossways,
BIG MELT:
Cascades of lava
create a variety of
new landforms.
is a lively example of a “transform bound
ary.” Eviction can cause stress to build up
until it releases all at once in an earth
quake, like the one that hit the San FVan
cisco Bay area in 1989, causing 62 deaths
and an estimated $6 billion in damage.
The Himalayas are the most dramatic
illustration of a “convergent boundary,”
a slow-motion pileup of continental and
oceanic plates. Incredible forces have
lifted the world’s tallest mountain range
as the Indian plate grinds under the Eur
asian plate like a shoe under a rug. Con
vergence often creates volcanoes such as
those in the Andes.
The result is our puzzle-piece map of
the world, left ova* from the splitting up
of the supercontinent of Pangea about
200 million years ago. ca
Julian Smith
USA WEEKEND-Sept. 14-16,2007
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