http://www.washingtonpost.com/wp-dyn/content/article/2005/10/22/AR2005102201061.html

Unearthing Clues to a Cataclysm
Buried Crater Near Norfolk Thought to Be Result of an Object Striking Earth

By Michael E. Ruane
Washington Post Staff Writer
Sunday, October 23, 2005; C01



EASTVILLE, Va. A white fireball two miles across thunders from the sky at 
30,000 mph and crashes
into the ocean off the Virginia coast. The impact vaporizes billions of tons of 
water, rips a hole
in the sea floor six miles deep and fractures the bedrock far into the Earth.

The splash is 30 miles high. Debris is lofted over the horizon and rains down 
on an area of 3
million square miles, as distant as the Antarctic. Towering tsunamis surge 
toward the Blue Ridge
Mountains.

Nearby life -- ferocious-looking sea creatures and dog-sized proto-horses along 
the tropical
shoreline -- is blasted and then swept into the abyss by the boiling ocean. A 
calamity of
unimaginable scale, it is probably the most stupendous geological event ever on 
the East Coast.

For more than a decade, geologists have believed that a gigantic object, an 
asteroid or a comet,
struck the Earth north of Norfolk about 35 million years ago in a cataclysmic 
occurrence that left
behind a 53-mile-wide, long-buried crater.

An international team of scientists, seeking clues to the origins of the 
planets, has assembled in a
windblown bean field near the crater's center to try to determine, among other 
things, exactly what
happened when the object struck.

Since early last month, the team has been working with a large drilling rig 
that uses diamond-tipped
bits and brings up core samples to bore through eons of sedi ment toward the 
floor of the crater and
the place where the impactor hit, believed to be about 7,000 feet below the 
surface.

As a farmer harvested his soybean crop just north of Cape Charles on Virginia's 
Eastern Shore and
the wind off the Chesapeake Bay blew dust and grasshoppers across the drilling 
site, it was hard to
imagine the scale of what geologists believe happened there.

"This is so big that we can't really picture it," said David S. Powars, a U.S. 
Geological Survey
geologist, who said he first suspected the presence of an impact crater in the 
1980s. "You could
take the whole nuclear arsenal in its heyday: Russia, China, U.S. . . . That's 
a firecracker
compared to what this explosion would be."

The men and women of the small but intense crater community who gather at the 
spot attempt to
picture it every day. "I dream this all the time," Powars said. "People say, 
'Did you sleep?' I say,
'I worked all night dreaming it.' I try, but I'll be honest: I can't imagine 
the event."

Their work is the culmination of a five-year project in which the USGS has 
drilled six holes probing
the crater's landscape. This hole will be the program's deepest, and the last, 
officials say.

Since the formal announcement in 1995 of what is now called the Chesapeake Bay 
Impact Crater,
studies have detailed its dimensions and outline, experts say. Last year 
scientists for the first
time found rock that had been melted by the impact and fossils of 
microorganisms that had been
smashed in the event.

There are scores of known impact sites around the world and millions more on 
planets and moons
across the solar system. The one near Norfolk is Earth's seventh-largest site 
and the biggest in the
United States.

On Earth, such impacts can dramatically alter the landscape in seconds, 
geologists say. And some
scientists believe that understanding the moment of impact, "the soul . . . the 
spirit" of the
collision, as one said, might be a key to understanding the formation of the 
solar system.

"If you think about how the Earth was formed," geologist Henning Dypvik of the 
University of Oslo
said Wednesday at the drilling site. "The Earth was formed by a meteorite that 
came from here, an
asteroid that came from there and a comet that came from here."

He moved his hands as if making a snowball. "This is the base process for the 
formation of the Earth
and the universe," he said. "By studying [impacts], by understanding the 
mechanisms, then we can
know much more about the Earth and the formation of the planetary system."

And then there is the question: What if such an object struck today? Even one a 
fraction of the size
of the Chesapeake's would cause a disaster, said Powars, a Washington native 
and one of the people
who discovered the crater. An impact by something a half-mile in size, and "the 
East Coast is in
trouble," he said. "Lights out."

Impact science is fairly young, the geologists said. As recently as 20 years 
ago, the study of Earth
impacts by "rocks . . . from heaven," as Dypvik put it, was considered crazy. 
The Earth's visible
craters were thought to be remnants of volcanoes, he said.

Gradually, the scientific community realized that the Earth, like other 
planets, had been peppered
over billions of years by renegade objects streaking through space. There are 
now more than 170
impact "structures" identified around the globe, more than 50 in North America.

The Earth's biggest, 186 miles across, is at Vredefort, South Africa.

The third-largest, the 100-mile-wide Chicxulub crater on Mexico's Yucatan 
Peninsula, is believed to
be the result of an impact 65 million years ago that blew so much debris into 
the atmosphere that it
darkened the Earth for months and led to the extinction of the dinosaurs.

Geologists don't believe that kind of thing happened after the Chesapeake 
impact. It "would have
killed off the local population" for hundreds of miles up and down the coast, 
said Jean Self-Trail,
a Geological Survey micropaleontologist. "But we don't really have any evidence 
that there was a
massive die-off."

Small impacts happen almost all the time on Earth, said Jens Ormo, a Swedish 
crater expert working
at Chesapeake site for the Spanish space agency. The big, so-called 
hypervelocity impacts are quite
rare. He said one of the most recent occurred about 50,000 years ago and formed 
Arizona's Barringer
crater.

The Chesapeake crater is the result of what geologists say was a marine impact. 
The object struck in
several hundred feet of water far off the coastline, which was west of Richmond 
during the period of
high global sea levels.

"It basically vaporized billions of tons of seawater," Powars said. "Billions 
of tons! And that's
not exaggerating." There was a momentary hole in the water down to the sea 
bottom. "Then you had the
water coming back in on this hot mixture of stuff, basically melted rock and 
sediments that fell
back in . . . [creating] incredible steam explosions."

"It was a very volatile impact," Powars said. Another big marine impact crater 
in the Barents Sea
off the northern coast of Norway is named Mjolnir, for the legendary hammer of 
the Scandinavian god
Thor. There, geologists believe, the impact temporarily ignited sediments on 
the bottom of the
ocean.

The Chesapeake crater, which geologists describe as shaped like an upside-down 
broad-brimmed hat, is
centered near Cape Charles and extends north along the Delmarva Peninsula to 
about Wachapreague, Va.
It goes west across the bay into Gloucester County, south to Norfolk and east 
into the ocean.

Powars said he first suspected the crater after routine geological drilling in 
the area found
disorganized sediments underground. It was revealed after oil company 
explorations showed the
outline of a crater. The impact object, probably an asteroid, disintegrated, 
the geologists said,
but traces of it might be found if the drilling reaches deep enough.

The crater has been extremely well preserved because it is buried under land 
and sea sediment, the
geologists said. But it is accessible via land and could become among the 
most-studied in the world.

"I often say how much I would love to see [an impact like] this happen," Powars 
said, "as long as I
was on something that keeps me alive."

Two years ago, a pair of California scholars, Steven N. Ward and Erik Asphaug, 
published a paper
about the potential impact of an asteroid that scientists think has a minute 
possibility of striking
Earth in 2880.

The asteroid, called 1950 DA, is about a half-mile in diameter. The two men 
calculated that if it
struck the sea at 40,000 mph, 370 miles off the East Coast, it would blow an 
11-mile hole in the sea
floor and within two hours would send 300-foot tsunamis crashing against the 
coast from Cape Cod,
Mass., to Cape Hatteras, N.C.

The chances of impact are highly remote, and their paper was just "a focus of 
thought," the authors
wrote. "Humanity lives with a calculus of infinite devastation times 
infinitesimal probability."

© 2005 The Washington Post Company
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