Questions, answers about Hawaii lava flowAssociated Press
By JENNIFER SINCO KELLEHER 27 minutes ago
After weeks of slow, stop-and-go movement, a river of asphalt-black lava was less than the length of a football field from homes in a Big Island community Tuesday. (Oct. 28)HONOLULU (AP) — Lava that has entered a rural Hawaii town has been described as a disaster in slow motion. After months of creeping through uninhabited areas of the Big Island, it reached Pahoa this week, crossing a residential street, burning down a garden shed and inching toward homes and a main road that goes through downtown.
The lava is from Kilauea, one of the most active volcanos in the world. It has been actively erupting since 1983.
HOW PREDICTABLE IS ITS PATH?
Scientists from the U.S. Geological Survey's Hawaiian Volcano Observatory have the tools to monitor active volcanos to determine if an eruption is imminent and forecast the path of a lava flow.
But lava is still a natural phenomenon, and much like a hurricane, some uncertainty remains.
The Big Island's topography contributes to deviations in the lava's route, said volcanologist Loyc Vanderkluysen, as assistant professor at Drexel University in Philadelphia who earned a doctorate degree from the University of Hawaii.
Lava surged through the village of Pahoa on Hawaii's Big Island, as residents were forced to evacuate their homes. The molten stream picked up speed last week after weeks of slow, stop-and-go movement. (Oct. 29)The lava emerged from a vent in June. It started moving through thick vegetation that made it difficult at times to see deviations in topography, he said.
But it's looking like the lava is headed to Pahoa Village Road, which runs through downtown.
"Laterally it might be a little to the right or left, but it will head to the road" — unless it suddenly stops moving, Vanderkluysen said.
What's less predictable is where a new branch will sprout from the miles-long flow and spread in other directions.
"We don't have a good grasp of where breakouts are going to happen," he said.
This Tuesday, Oct. 28, 2014 photo provided by the U.S. Geological Survey shows lava that has pushed through a fence marking a property boundary above the town of Pahoa on the Big Island of Hawaii. After weeks of slow, stop-and-go movement, a river of asphalt-black lava was less than the length of a football field from homes in the Big Island community Tuesday. The lava flow easily burned down an empty shed at about 7:30 a.m., several hours after entering a residential property in Pahoa Village, said Hawaii County Civil Defense Director Darryl Oliveira. A branch of the molten stream was less than 100 yards (90 meters) from a two-story house. It could hit the home later Tuesday if it continues on its current path, Oliveira estimated. Residents of Pahoa Village, the commercial center of the island's rural Puna district south of Hilo, have had weeks to prepare for what's been described as a slow-motion disaster. Most have either already left or are prepared to go. (AP Photo/U.S. Geological Survey)HOW HOT IS THE LAVA?
About 2,100 degrees Fahrenheit, according to Janet Babb, spokeswoman for the Hawaiian Volcano Observatory. "Ten times hotter than boiling water."
But the temperature starts to drop after the lava is exposed to air.
"The crust cools down, and you can walk on it after a few days," Vanderkluysen said.
CAN ANYTHING BE DONE TO STOP IT?
"Lava diversion is a very complex issue," Babb said. "It's a complex legal, political, technical and cultural issue."
Residents have expressed anger at suggestions to divert the Kilauea flow, saying it's culturally insensitive to interfere with the will of Pele, the Hawaiian volcano goddess.
Attempts were made to stop flows from Italy's Mount Etna by building trenches and concrete walls. But that was only partially successful.
Such efforts also are extremely expensive, noted Vanderkluysen.
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