Friday, March 30, 2007
Kilauea volcano compared to Mount St.Helens
Mount St. Helens may be following the example of Kilauea in Hawaii with magma being replaced from a reservoir beneath the volcano as fast as it emerges as lava at the surface, scientists say.
While the two volcanoes are different in many respects, St. Helens appears to have become an "open system" as its domebuilding eruption that began in the fall of 2004 continues at a pace that has been unchanged for the past year, said Daniel Dzurisin, a geologist at the U.S. Geological Survey's Cascades Volcano Observatory.
This pair of Jan. 23, 2007 photos released by the U.S. Geological Survey's Cascades Volcano Observatory, shows Mount St. Helens' dome as seen from the north, top, with a matching thermal-imaging infrared image, bottom. Scientists say Mount St. Helens may be following the example of the Kilauea volcano in Hawaii, with magma being replaced from a reservoir beneath the volcano as fast as it emerges as lava at the surface. (AP Photo/Courtesy U.S. Geological Survey's Cascades Volcano Observatory, Julie Griswold and Matt Logan)
Analyzing of digital elevation models made from high-resolution aerial photographs, scientists have kept close tabs on the rate at which lava has been pushing into the crater. At first it was about a dumptruck load, roughly 8 cubic yards, per second.
A year later it was down to slightly more than 1 cubic yard per second and since last April it has been fairly constant about 0.6 of a cubic yard per second _ still the equivalent of about nine truckloads every two minutes.
The longer the eruption continues at that rate, the more likely it is that a direct pathway has developed for molten rock to emerge from deep within the planet's crust, Dzurisin said, adding that it will take another year of data to reach a more definite conclusion.
"That situation could go on for a long time," Dzurisin said. "The ongoing eruption (at Kilauea) in Hawaii, for example, started in 1983."
Other evidence indicating the development of an open system at St. Helens is the slowing of deformation around the flanks of the volcano, indicating the magma chamber beneath the surface is being refilled rather than deflating, which would cause sagging.
At Johnston Ridge Observatory, five miles north of the crater, a global positioning system monitor has moved toward the volcano by about an inch since the eruption began, with most of the movement coming in the first year and a half.
Since then the rate of deformation has subsided considerably while lava continues to emerge, indicating the magma is being replenished.
It took about four centuries to build the symmetrical, cone-shaped peak that led St. Helens to be compared with Mount Fujiyama in Japan before a massive blast on May 18, 1980, removed the top 1,314 feet, flattened miles of southwest Washington forests and left 57 people dead.
"We know that St. Helens is capable of dome eruptions lasting decades," Dzurisin said.
While the two volcanoes are different in many respects, St. Helens appears to have become an "open system" as its domebuilding eruption that began in the fall of 2004 continues at a pace that has been unchanged for the past year, said Daniel Dzurisin, a geologist at the U.S. Geological Survey's Cascades Volcano Observatory.
This pair of Jan. 23, 2007 photos released by the U.S. Geological Survey's Cascades Volcano Observatory, shows Mount St. Helens' dome as seen from the north, top, with a matching thermal-imaging infrared image, bottom. Scientists say Mount St. Helens may be following the example of the Kilauea volcano in Hawaii, with magma being replaced from a reservoir beneath the volcano as fast as it emerges as lava at the surface. (AP Photo/Courtesy U.S. Geological Survey's Cascades Volcano Observatory, Julie Griswold and Matt Logan)
Analyzing of digital elevation models made from high-resolution aerial photographs, scientists have kept close tabs on the rate at which lava has been pushing into the crater. At first it was about a dumptruck load, roughly 8 cubic yards, per second.
A year later it was down to slightly more than 1 cubic yard per second and since last April it has been fairly constant about 0.6 of a cubic yard per second _ still the equivalent of about nine truckloads every two minutes.
The longer the eruption continues at that rate, the more likely it is that a direct pathway has developed for molten rock to emerge from deep within the planet's crust, Dzurisin said, adding that it will take another year of data to reach a more definite conclusion.
"That situation could go on for a long time," Dzurisin said. "The ongoing eruption (at Kilauea) in Hawaii, for example, started in 1983."
Other evidence indicating the development of an open system at St. Helens is the slowing of deformation around the flanks of the volcano, indicating the magma chamber beneath the surface is being refilled rather than deflating, which would cause sagging.
At Johnston Ridge Observatory, five miles north of the crater, a global positioning system monitor has moved toward the volcano by about an inch since the eruption began, with most of the movement coming in the first year and a half.
Since then the rate of deformation has subsided considerably while lava continues to emerge, indicating the magma is being replenished.
It took about four centuries to build the symmetrical, cone-shaped peak that led St. Helens to be compared with Mount Fujiyama in Japan before a massive blast on May 18, 1980, removed the top 1,314 feet, flattened miles of southwest Washington forests and left 57 people dead.
"We know that St. Helens is capable of dome eruptions lasting decades," Dzurisin said.
# posted by kevin : 8:29 AM
