Researchers have solved a longstanding mystery that has befuddled scientists and tourists alike: why rocks on a dry lake bed in Death Valley National Park in California occasionally move.
The explanation for the phenomenon
at Racetrack Playa — named for the long trails that the rocks, some of
which weigh hundreds of pounds, leave in the mud — is that the stones
are pushed by wind-driven ice that forms and then breaks up under
certain conditions.
“It’s a very rare phenomenon,” said Richard D. Norris, a paleobiologist at the Scripps Institution of Oceanography and lead author of a paper describing it in PLOS One. “A brief moment in time.”
Dr.
Norris and James M. Norris, a cousin and co-author, actually saw the
rocks moving in December when they went to check on the project. “It was
complete dumb luck,” Dr. Norris said. “Almost every rock on the playa
moved.”
Scientists
have offered theories about these “sailing stones” since at least the
1940s. Many thought that wind or ice played a role, but not in the ways
that the Norrises and colleagues uncovered. For their study, they
embedded special global positioning system devices, designed by James
Norris, in rocks of various sizes brought from outside the park, because
the park service did not allow them to disturb the existing playa
stones.
The
playa, about three square miles and pancake flat, is usually dry,
though rainwater runoff from the surrounding mountains occasionally
fills part of it to a depth of a few inches. It’s when this shallow pond
forms, and the nights are below freezing and the days are sunny and
warm, that the rocks may move, the researchers said.
On those occasions, the cold night air leaves a sheet of ice barely an eighth of an inch thick. Then the warmth of the sun causes the sheet to break up.
“One moment, it’s quiet and still,” Dr. Norris said. “The next, it’s crackle, crackle, pop, pop, pop.”
As
more ice melts, some of these lesser sheets have room to move. Driven
by light breezes, the sheets push up against rocks and nudge them. The
wind drives the water, too, which also helps push the ice against the
rocks.
The
movement is slow, no more than about 15 feet a minute. “The rocks are
creeping along,” Dr. Norris said, “like a baby on its stomach.”
The
researchers have not calculated the forces involved — that is grist for
a future study, they said — but clearly, they are enough to move the
rocks, aided by the reduced friction that comes from their sitting in
the shallow water.
The
movements are episodic — the conditions may be just right for a few
minutes, and then the sun causes more ice to break and the movement
stops. And once the water evaporates, it may be years before the rocks
move again, even if the playa floods again, because the precise
temperature and wind conditions may not occur.
“What
you see 99 percent of the time you’re out there are these fossilized
trails,” Dr. Norris said. “Everything has just stopped and gone into
hibernation.”
The
discovery also explains why many of the trails are parallel to one
another. The researchers found that the moving ice sheets were sometimes
so big that they would nudge rocks hundreds of feet apart, moving them
in the same direction.
Based
on existing theories, the cousins had thought that winds as high as 80
or 90 miles per hour might have moved the stones. So early in the
two-year study, they discussed buying a sturdy all-season tent for their
site visits.
They were surprised to see the rocks moving on a sunny day in a light breeze.
“We didn’t need the tent,” Dr. Norris said.
I'm sure those rocks will move to the center of the lake !!!
ReplyDeleteLikewise without the destruction from fishes and big waves,
all the stalactites produced by Viet floating communities
will coalesce at the bottom and in the middle of Tunle Sap Lake !!!
K . . S