10/29/93:  NASA-RUSSIAN MISSION EXPLORES KAMCHATKAN VOLCANOES

Brian Dunbar
Headquarters, Washington, D.C.                      October 29, 1993

Myron Webb
Stennis Space Center, Miss.

RELEASE:  93-198

     Preliminary results from an historic U.S.-Russian scientific expedition
are shedding new light on the geology of Eastern Russia.

     The data was obtained in August and September by NASA and Russian
scientists using NASA's Learjet Model 23 based at the John C. Stennis Space
Center, Miss.

     The expedition, on which a Russian served as co-pilot and translator,
studied a variety of sites on the Kamchatkan peninsula to provide
remote-sensing imagery and field data.  These data will be used to study the
geologic evolution of the volcanoes, the impact of large volcanic eruptions on
the atmosphere and its chemistry.

     The data also will be used to model thermal and dynamical aspects of
volcanoes.  Carrying NASA's Thermal Infrared Multispectral Scanner (TIMS) and a
Zeiss camera, the plane flew the first civilian research mission over Russian
territory.

     "The Kamchatka area is geologically significant because three of the
plates of the Earth's crust are converging in that area," said Dr. Miriam
Baltuck, Chief of the Solid Earth Branch of NASA's Office of Mission to Planet
Earth. "The Pacific plate, which contains most of the Pacific Ocean, is sliding
beneath the Eurasian and North American plates.  When one plate descends, or
subducts beneath another, it heats up and partially melts.  The molten material
generated from this process rises to the surface through the overriding plates
and erupts through volcanoes."

     In the Western Pacific, this process has formed the arcs of islands that
rim the Pacific and also is responsible for deadly earthquakes.  The
Kliuchevskoi volcano, one of the larger volcanoes on the peninsula, has been
mildly active since April with small summit eruptions and emissions of sulfur
dioxide and ash plumes.

     Kamchatkan volcanoes also are capable of more energetic eruptions, similar
to the 1991 eruption of Mount Pinatubo in the Philippines. Such eruptions can
inject ash, sulfur dioxide and aerosols-small solid or liquid particles that
become suspended in the atmosphere-high into the atmosphere where they can
affect global temperatures and ozone levels.

     The program resulted from 4 years of negotiations between NASA and the
Russian Academy of Sciences, under the auspices of the Volcanology
Implementation Team of the U.S.-Russian Earth Science Joint Working Group. With
the support of numerous U.S. and Russian agencies a new, direct air corridor
was approved between Shemya Air Force Base, Alaska, and Elisovo, Russia. This
new air corridor, which avoided an exhaustive northern ferry route, should
appear on future aeronautical charts.

     As part of the agreement, Oleg Gusev, a Russian citizen, served as
co-pilot and translator aboard the Learjet. He is the first Russian to serve as
a crew member on a NASA aircraft and only the second Russian to co-pilot a U.S.
government aircraft -- the first was in 1943 during World War II.

     "This is the first time, to our knowledge, that a U.S. civilian research
aircraft has flown over the territory of the former Soviet Union," said Dr. Jim
Hunning, Manager of the Airborne Science Office in NASA's Office of Mission to
Planet Earth. "It has opened up a new avenue of research and air transportation
for science and commerce."

     The expedition data have clarified the structure of the volcanic areas and
found evidence of the processes that created them.  An image of Tolbachik
Volcano, for example, showed solidified lava flows from eruptions in 1975 and
1976.  The younger flow proved richer in silicon and aluminum, with the older
flow richer in magnesium and calcium.  The texture of the flows appears to
belie the chemical analyses which shows that the older flow has the steep
margins and ridges associated with a more viscous lava while the younger flow
appears to have been more fluid.

     Another site, Bezymianny Volcano, showed many similarities to Mount St.
Helens in Washington state.  Bezymianny's eruption on March 30, 1956, like
Mount St. Helens' in 1980, was directed largely to the side instead of upward.
The Bezymianny eruption reduced the elevation of the volcano by approximately
660 feet (201 meters).  The explosion is believed to have raised an ash column
to altitude of more than 22 miles (35 kilometers).

     Inside the Bezymianny crater, a lava dome has grown to a height of 1,650
feet (500 meters).  A similar dome exists on Mount St. Helens, and the
temperature data on Bezymianny will be compared to that from the Mount St.
Helens dome, which has been the subject of TIMS surveys over the past 4 years.
The comparison data can be used to develop models describing the thermal and
physical evolution of volcanoes.

     The floor of the Uzon Caldera, which was formed approximately 100,000
years ago, is the site of vigorous geothermal activity, including geysers and
hot springs.  A temperature map developed from the TIMS data will allow
scientists to estimate the geothermal input to the groundwater system.

     Spectral data from the Gorely Volcano will allow scientists to study the
structure of more than 8,000 years of volcanic flows.  With this historical
record, geologists can better understand how the continuing subduction of the
Earth's crust manifests itself on the surface through volcanoes.

     Overall, the data will help scientists understand volcanic eruptions,
frequency and magnitude and the effects of those eruptions on the atmosphere.
The science team also will evaluate the data for development of a Volcano
Global Impact Index which would link geological and weather data and evaluate
their combined global impact.
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  Via FTL BBS (404-292-8761) and NASA Spacelink (205-895-0028)
