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Monitors get weird vibes from Antarctic. (Oceanography).


In August 2000, seismometers on islands in the South Pacific began picking up unusual signals coming from regions even farther south. During the next 5 months, 13 separate groups of pressure waves traveled through the ocean depths for thousands of miles before they smacked into the islands and were converted into detectable ground motions.

In most cases, the energy received by the instruments was concentrated at a few frequencies, says Emile A. Okal, a seismologist seis·mol·o·gy  
n.
The geophysical science of earthquakes and the mechanical properties of the earth.



seis
 at Northwestern University Northwestern University, mainly at Evanston, Ill.; coeducational; chartered 1851, opened 1855 by Methodists. In 1873 it absorbed Evanston College for Ladies.  in Evanston, Ill. That suggests the source of the vibrations had a distinct shape. Sometimes the islands' shaking lasted no more than 2 minutes, but on other occasions it went on for hours. Scientists previously had detected similar vibrations from undersea volcanic activity, but these events displayed a puzzling characteristic: Unlike any volcano, the source of the pressure waves seemed to move across Antarctica's Ross Sea Ross Sea, arm of the Pacific Ocean, Antarctica, between Victoria Land and Marie Byrd Land. It was discovered in 1841 by Sir James Clark Ross, a British explorer. Ross Island with Mt. , heading northwest at a rate of several kilometers per day.

Satellite observations of the Ross Sea during that time solved the puzzle handily hand·i·ly  
adv.
1. In an easy manner.

2. In a convenient manner.

Adv. 1. handily - in a convenient manner; "the switch was conveniently located"
conveniently

2.
. The data enabled researchers to precisely pin the source of most of the events to a large, drifting iceberg dubbed B-15B. The space images show that this 135-kilometer-by-40-km chunk, a piece of a megaberg that calved from the Ross Ice Shelf Ross Ice Shelf

World's largest body of floating ice. It lies at the head of the Ross Sea, which forms an enormous indentation in Antarctica. Its area is estimated to be about the size of France.
 a few months earlier (SN: 5/12/01, p. 298), had been intermittently colliding with other large bergs as winds and currents propelled it across the ocean.

Exactly what caused the vibrations--which took place only occasionally during the ice bergs drift--isn't known, says Okal. Maybe bumping against other large bergs caused the pressure waves. Perhaps they resulted from the oscillation of water in a large crack or fissure fissure /fis·sure/ (fish´er)
1. any cleft or groove, normal or otherwise, especially a deep fold in the cerebral cortex involving its entire thickness.

2. a fault in the enamel surface of a tooth.
 in the iceberg, or maybe B-15B scraped along the ocean bottom or against an undersea mountain as it drifted northwest. The ocean floor in this area isn't well mapped, Okal notes.

Whatever the phenomenon's cause, he says, scientists should now recognize that icebergs can be a source of noise for seismometers and underwater acoustic sensors. A worldwide network of such instruments plays an important role in monitoring the Comprehensive Nuclear Test-Ban Treaty nuclear test-ban treaty: see disarmament, nuclear.
Nuclear Test-Ban Treaty
 officially Treaty Banning Nuclear Weapons Tests in the Atmosphere, in Outer Space and Under Water
 (SN: 7/14/01, p. 25). --S.P.
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Article Details
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Publication:Science News
Article Type:Brief Article
Geographic Code:1USA
Date:May 4, 2002
Words:356
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