http://www.nsf.gov/od/lpa/news/press/00/pr0038.htm

News - May 30, 2000

NSF PR 00-38
Media contacts:  Cheryl Dybas, National
 Science Foundation   (703) 306-1070  [EMAIL PROTECTED]
   Shelley M. Lauzon, Woods Hole
 Oceanographic Institution  (508) 289-2270  [EMAIL PROTECTED]
Program contact:  Bil Haq   (703) 306-1586  [EMAIL PROTECTED]




Seafloor Off Mid-Atlantic Coast Highly Charged with Gas

Vigorous gas expulsion could weaken shelf edge

A team of scientists investigating whether possible cracks along the outer
continental shelf off the mid-Atlantic coast might lead to a tsunami-causing
landslide has discovered that the entire area is charged with gas.

Based on preliminary results from a just-completed two-week cruise to the
area funded by the National Science Foundation (NSF), the scientists say the
suspected cracks are a system of large depressions along the shelf edge that
appear to have been excavated by gas erupting through the seafloor.

"We don't know the source of the gas," team leader Neal Driscoll of the
Woods Hole Oceanographic Institution (WHOI) said. "But it is clear that gas
has played an important role in the formation of these features. The gas is
trapped under layers of sediment on the shelf edge until some circumstance
causes it to escape, blowing holes in the seafloor to form these large
pockmark features we thought were cracks."

In a paper published in the journal Geology days before their May 7
departure for the Mid-Atlantic coast, Driscoll and colleagues Jeffrey
Weissel of the Lamont-Doherty Earth Observatory of Columbia University and
John Goff of the University of Texas Institute for Geophysics, speculated
that rising gas might play a part in triggering shelf-edge collapse. Even
so, they were surprised at the quantity of gas and the apparent vigor of the
"blowout" process.

"Our seismic data show that gas is pervasive in and around the blow-outs,"
Goff said. "Gas has a characteristic signal, which commonly shows up as a
bright, high-amplitude reflection that obscures any deeper signals."

"These are exciting findings," said Mike Purdy, director of NSF's division
of ocean sciences. "We now know that biological, chemical and physical
processes, like those that created the gas reservoirs and gas expulsions
described by these investigators, are going on every day in the depths of
the sea. Driscoll, Goff and Weissel have reaffirmed that exciting and
significant discoveries are waiting to be made on the ocean floor. The
importance of exploring our own planet is again made very clear."

"We were a bit taken aback, to be sure," Weissel said. "A great deal more
work is needed before any definitive statements can be made. Regardless of
the source, it is apparent that gas charging plays a critical role in the
area, and that the ongoing process of blowouts could conceivably weaken the
shelf edge and contribute to a submarine landslide/tsunami scenario."

The scientists say the features, some as large as 2,000 meters (6,500 feet)
across, 50 meters (165 feet deep) and up to 5,000 meters (16,400 feet) long,
occur in a line along the shelf edge. That suggests there is some geological
mechanism at work underneath the features, or their trend and shapes might
be due to their proximity to the shelf edge. A submarine landslide and
resulting tsunami along the shelf, although a very low risk when compared to
the chance of hurricanes and severe storms striking the area, remains
possible.

The May 7-20 research cruise was funded under a grant from NSF's Marine
Geology & Geophysics program and was conducted aboard the Research Vessel
Cape Hatteras, operated out of Beaufort, North Carolina, by Duke University
and the University of North Carolina Consortium. The NSF grant will also
cover the next year of data synthesis and analysis, and the eventual
publication of the detailed results.

-NSF-

================================
Robert F. Tatman
[EMAIL PROTECTED]
Jenkintown, PA, USA
"Y Gwir Yn Erbyn y Byd"--Y Bardd Cymraeg
"The Truth Against the World"--motto of the Welsh bards

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