Elvia H. Thompson
Headquarters, Washington            March 6, 2003
(Phone: 202/358-1696)

Alan Buis
Jet Propulsion Laboratory, Pasadena, Calif.
(Phone: 818/354-0474)

Eric Berryman
National Imagery & Mapping Agency, Bethesda, Md.
(Phone: 301/227-3132)

RELEASE: 03-096

NASA'S NEWEST MAPS REVEAL A CONTINENT'S GRANDEUR AND A SECRET

     From Canada to Central America, the many grandeurs of 
North America's diverse topography star in a just-released 
high-resolution map from NASA's Shuttle Radar Topography 
Mission (SRTM). But a relatively obscure feature, all but 
hidden in the flat limestone plateau of Mexico's Yucatan 
Peninsula, is what emerges as the initial showstopper from 
the mission's first released continental data set.

The existence of the impact crater, Chicxulub, was first 
proposed in 1980. In the 1990s, satellite data and ground 
studies allowed it to gain prominence among most scientists 
as the long sought-after "smoking gun" responsible for the 
demise of the dinosaurs and more than 70 percent of Earth's 
living species 65 million years ago. The SRTM has provided 
the most telling visible evidence to date of a 180-kilometer 
(112-mile) wide, 900-meter (3,000-foot) deep impact crater, 
the result of a collision with a giant comet or asteroid on 
one of Earth's all-time worst days. 

The North America and Yucatan Peninsula images created from 
the map are available on the JPL Planetary Photo journal at: 

http://photojournal.jpl.nasa.gov/catalog/PIA03377
http://photojournal.jpl.nasa.gov/catalog/PIA03379

"This new, complete North American data set greatly expands 
our topographic knowledge of Canada, southern Alaska and its 
Aleutian Islands, Mexico and Central America," said Dr. 
Michael Kobrick, SRTM project scientist at NASA's Jet 
Propulsion Laboratory (JPL), Pasadena, Calif.

"There are spectacular features that pop out in these maps as 
never before, and more subtle features, like Chicxulub, 
become apparent for the first time. In fact, much of the 
surface expression of Chicxulub is so subtle; if you walked 
across it you probably wouldn't notice it. That's where the 
view from space becomes invaluable, " Kobrick said.

The Chicxulub data show a subtle, yet unmistakable, 
topographic indication of the impact crater's outer boundary: 
a semicircular trough 3 to 5 meters (10 to 15 feet) deep and 
5 kilometers (3 miles) wide. Scientists believe the impact, 
centered off Yucatan's coast in the Caribbean, disturbed the 
subsurface rocks, making them unstable. The rocks were 
subsequently buried by limestone sediments, which erode 
easily. The crater rim's instability caused the limestone to 
fracture along the rim, forming the trough. In addition, the 
collapse of numerous limestone caverns above the crater rim 
resulted in an arcing chain of sinkholes, called cenotes, 
that are visible as small, circular depressions. 

Exactly how the Chicxulub impact caused Earth's mass 
extinctions is not known. Some scientists think it threw 
massive quantities of dust into the atmosphere, blocking the 
sun and stopping plants from growing. Others believe sulfur 
released by the impact lead to global sulfuric acid clouds 
that blocked the sun and also fell as acid rain. Another 
possibility is global wildfires triggered by atmospheric 
reentry of red-hot debris.

The remainder of the North American data paints a dynamic 
portrait of a geologically complex continent. Active 
structural deformations of Earth's crust along and near the 
Pacific/North American tectonic plate boundary create the 
diverse topographic relief of the Pacific coast. Across the 
Great Plains, erosional patterns dominate, with stream 
channels surrounding and penetrating remnants of older smooth 
slopes. In Canada and the northern U.S., evidence of glaciers 
from the last ice age abounds. 

In February, NASA finished processing the mission's data and 
delivered it to the National Imagery and Mapping Agency 
(NIMA). More than eight terabytes of data recorded aboard the 
Space Shuttle Endeavour were refined into 200 billion 
research-quality measurements of Earth's landforms. The NIMA 
will perform additional data finishing and send it to the 
U.S. Geological Survey's Earth Resources Observation Systems 
Data Center, Sioux Falls, S.D., for final archiving and 
distribution. South America will be the next continental 
dataset.

The SRTM, flown Feb. 11 to 22, 2000, made 3-D measurements of 
the more than 80 percent of Earth's landmass located between 
60 degrees north and 56 degrees south of the equator; areas 
home to nearly 95 percent of the world's population. SRTM is 
a cooperative project of NASA, NIMA, the Department of 
Defense, the German and Italian space agencies. Fulfilling 
part of NASA's mission to understand and protect our home 
planet, it is managed by JPL for NASA's Earth Science 
Enterprise, Washington. The California Institute of 
Technology in Pasadena manages JPL for NASA.

For more information about SRTM on the Internet, visit:

http://www.jpl.nasa.gov/srtm/

-end-


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