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Eruption! A survivor's tale.


Struggling to stay alive, Stanley Williams This article is about Stanley Tookie Williams III. For the dance instructor, see Stanley Williams (ballet).

Stanley Tookie Williams III (December 29, 1953 – December 13, 2005), born in Monroe, Louisiana, was a convicted murderer and an early leader
 lifted himself out of the exploding volcano. Unable to use his broken legs, he crawled down the mountain slope and hid behind a large rock to find shelter from falling, fiery debris.

Moments earlier, Williams and six fellow volcanologists (volcano scientists) had been wrapping up measurements inside the Galeras volcano in Colombia, South America South America, fourth largest continent (1991 est. pop. 299,150,000), c.6,880,000 sq mi (17,819,000 sq km), the southern of the two continents of the Western Hemisphere. , when it suddenly erupted. Boulders and hot gas from the exploding inferno crushed Williams's legs, fractured his skull, and burned his body extensively. But Williams was the lucky one. His six colleagues and three nearby tourists died in the blast.

Ironically, Williams and his colleagues were part of an international team trying to save people's lives from deadly volcanoes. The measurements they were taking that January 1993 day were part of a decade-long effort to identify the signs of impending im·pend  
intr.v. im·pend·ed, im·pend·ing, im·pends
1. To be about to occur: Her retirement is impending.

2.
 eruptions at the world's most dangerous volcanoes. As it turns out, says Williams, data from the tragic, unexpected explosion may finally give scientists the clues they have been searching for.

PREDICTING DISASTER

Approximately 50 volcanoes erupt every year, endangering people's lives. The 1991 eruption of Mount Pinatubo Noun 1. Mount Pinatubo - a volcano on Luzon to the northwest of Manila; erupted in 1991 after 600 years of dormancy
Pinatubo
 in the Philippines killed 300 people by spreading tons of heavy ash that crushed roofs on houses for kilometers around. The 1985 explosion of Mt. Nevado del Ruiz Nevado del Ruiz is an Andean stratovolcano in Caldas Department, Colombia. It is the northernmost volcano of the Andean Volcanic Belt and lies about 15 miles southeast of Manizales, with the town of Armero in the valley below.  in Colombia melted glaciers atop the mountain and created massive mudflows; 23,000 people died. And while the January 1993 eruption at Galeras was deadly only to those at close range, a stronger explosion could have wiped out more than 400,000 people who live nearby.

That's why Williams, a professor of volcanology volcanology
 or vulcanology

Scientific discipline concerned with all aspects of volcanic phenomena. Volcanology deals with the formation, distribution, and classification of volcanoes, as well as their structure and the kinds of materials ejected during an
 at Arizona State University Arizona State University, at Tempe; coeducational; opened 1886 as a normal school, became 1925 Tempe State Teachers College, renamed 1945 Arizona State College at Tempe. Its present name was adopted in 1958. , traveled to Colombia in the first place - to see if he and his colleagues could figure out what makes the volcano tick.

But Galeras fooled everyone. It didn't provide the usual warning signs of an imminent eruption.

Normally, before an eruption, large amounts of gas (mostly water vapor mixed with carbon dioxide carbon dioxide, chemical compound, CO2, a colorless, odorless, tasteless gas that is about one and one-half times as dense as air under ordinary conditions of temperature and pressure. , sulfur dioxide sulfur dioxide, chemical compound, SO2, a colorless gas with a pungent, suffocating odor. It is readily soluble in cold water, sparingly soluble in hot water, and soluble in alcohol, acetic acid, and sulfuric acid. , and other gases) escape from a volcano's vent. That's the volcano's opening, which leads from a chamber filled with molten (semi-melted) rock, called magma, kilometers below the ground (see diagram, p. 17). In this magma chamber A magma chamber is a large underground pool of molten rock lying under the surface of the earth's crust. The molten rock in such a chamber is under great pressure, and given enough time and pressure can gradually fracture the rock around it creating outlets for the magma. , says Williams, the molten rock churns and pushes against the "roof" as if trying to get out. The movement forces gases up through tiny cracks in the rocks and shakes the ground with periodic tremors.

EERIE SILENCE

Williams and his colleagues did detect gases escaping from Galeras and rumbling tremors in the surrounding area several weeks before the January 1993 eruption. And the tremors did grow more frequent and intense.

But by the time Williams and his colleagues were conducting studies inside the volcano, the tremors had died down. The volcano was spewing only tiny levels of gas and appeared to be asleep, says Williams. The scientists mistakenly - and tragically - assumed that any budding danger had passed.

What they found out was that the volcano had been "tricking us spectacularly," Williams says. He and one of his students, Tobias Fischer, now suspect that the volcano had bottled itself up. As the magma flowed, they hypothesize hy·poth·e·size  
v. hy·poth·e·sized, hy·poth·e·siz·ing, hy·poth·e·siz·es

v.tr.
To assert as a hypothesis.

v.intr.
To form a hypothesis.
, cracks in the rocks above the magma chamber somehow started to seal up. That increased the pressure - and the strength and frequency of the tremors.

But then, Williams now theorizes, the cracks sealed up completely. When that happened, the tremors stopped, because the magma could no longer move around, Williams says. Gases could no longer escape. But the pressure continued to build. "We were sitting on a bomb that was [silently] ticking away," Williams says.

Suddenly, "the ground began to shake, and 10 seconds later, everybody was dead - that's how little warning we had," he says.

FUTURE FORECAST

This pattern of an eerie stillness just before eruption repeated itself two months after the deadly blast. Williams and Fischer have now translated the pattern into a model they say may help predict eruptions.

The model went on to correctly forecast a June 1993 eruption at Galeras. But the volcano proved to be more complicated than Williams and Fischer had originally thought. In November 1993 and March 1994, the "pre-eruption" pattern seemed to be occurring again - but the volcano didn't blow. The scientists later realized that the tremors they detected in those months were slightly different from the ones that had preceded the earlier, true eruptions.

Were they deterred from pursuing an eruption-forecasting model? Not at all. Now fully recovered from his injuries, Williams continues to climb into the bellies of volcanoes to collect the data he needs. His ultimate goal is to be able to forecast eruptions the way meteorologists Atmospheric scientists
  • Cleveland Abbe
  • Ernest Agee ...smells
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  • Gary M. Barnes
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  • Tor Bergeron
  • Jacob Bjerknes
  • Vilhelm Bjerknes
  • Howard B.
 forecast the weather. That will require setting up more volcano-observing stations and collecting a lot more data, he says.

"I can't claim I'm going to prevent a volcano from erupting e·rupt  
v. e·rupt·ed, e·rupt·ing, e·rupts

v.intr.
1. To emerge violently from restraint or limits; explode: My neighbor erupted in anger over the noise.

2.
," he adds, "but I may be able to help people minimize the disaster."
COPYRIGHT 1995 Scholastic, Inc.
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 1995, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Title Annotation:includes related article; volcanologist Stanley Williams
Author:Stein, Ben P.
Publication:Science World
Date:Feb 10, 1995
Words:809
Previous Article:Under alien control. (short story)
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