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Earth as egg: hard-boiled or raw?


Earth as egg: Hard-boiled or raw?

Most cooks know that a hard-boiled egg spins much faster than a raw or partially cooked egg. This difference often serves as a test for doneness. On a more global level, it may also illustrate one reason why Earth's magnetic field Earth's magnetic field (and the surface magnetic field) is approximately a magnetic dipole, with one pole near the north pole (see Magnetic North Pole) and the other near the geographic south pole (see Magnetic South Pole).  has sporadically switched direction in the past, according to according to
prep.
1. As stated or indicated by; on the authority of: according to historians.

2. In keeping with: according to instructions.

3.
 a controversial theory proposed by Richard Muller and Donald Morris at the Lawrence Berkeley Laboratory in Berkeley, Calif.

Most geophysicists think the geomagnetic field geomagnetic field

Magnetic field associated with the Earth. It is essentially dipolar (i.e., it has two poles, the northern and southern magnetic poles) on the Earth's surface. Away from the surface, the field becomes distorted.
 arises from currents of liquid iron flowing in the planet's outer core. But this is only a general theory. Scientists disagree over many details, including why the magnetic field sometimes weakens and then switches direction. Some have suggested that meteorites Meteorites
See also astronomy.

aerolithology

the science of aerolites, whether meteoric stones or meteorites. Also called aerolitics.

astrolithology

the study of meteorites. Also called meteoritics.
 hitting the Earth might turn the field around, but this theory has gained little support in recent years.

Now Muller and Morris are reviving it. They suggest that impacts or volcanic eruptions volcanic eruptions

discharging of fumes, dust and lava from volcanoes. They have damaging potential in addition to those of being physically overpowering by the lava flow or the ash or dust fallout.
 could loft dust into the atmosphere and suddenly cool the Earth to a point where great ice caps would develop over the polar regions polar regions: see Antarctica; Arctic, the. . Like an ice-skater accelerating a spin by pulling her arms toward her body, the movement of water toward the poles would speed the Earth's rotation.

At this point, the difference between hard-boiled and raw eggs becomes important. Like the contents of a raw egg, the liquid portions of the inner Earth are not firmly attached to the solid parts, so the entire core will not accelerate at the same time. As the crust and mantle speed up, friction and electromagnetic forces accelerate the outermost out·er·most  
adj.
Most distant from the center or inside; outmost.


outermost
Adjective

furthest from the centre or middle

Adj. 1.
 portions of the liquid core, but deeper regions of the core should lag behind for several hundred years, says Muller.

It is this shearing between regions in the outer core that causes the reversals, he proposes. Spin-up "scrambles" the flow patterns and weakens the geomagnetic field. When the entire core finally reaches speed, the field rejuvenates itself. But starting from a weak state, the field has an equal chance of pointing north or south. Not all reversals would occur in this way, but sudden cooling could explain some, Muller says.

So far, the physicists have few data or calculations to prove their ideas, although they say the theory offers several predictions that scientists can test. Other researchers remain extremely skeptical. In particular, some say it will take the entire core only a few years to reach speed.
COPYRIGHT 1989 Science Service, Inc.
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 1989, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Title Annotation:Earth Sciences; geomagnetic field variations
Author:Monastersky, Richard
Publication:Science News
Date:May 20, 1989
Words:397
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