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Mercury
Winter 2008 Table of Contents


In
this scanning electron microscope image of spherule SP37-3,
the plagioclase feldspar grain is labeled "Pg."
Image courtesy of Jeremy Delaney et al, 2004 LPSC poster
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by
Linda M.V Martel
Micrometeorite
bombardment accounts for almost 30,000 tons of material entering
Earth's atmosphere each year. Though most of the material
evaporates during entry or is lost at sea or falls on the land unnoticed,
thousands of micrometeorites have been collected successfully from
deep-sea sediments, from the snow and ice of the polar caps, and
now from a water well at the South Pole.
If
you think it's cold where you live, consider this cool little story
about ice...Antarctic ice...studded with minuscule grains from the
cosmos. Researchers are studying extraterrestrial materials that
are particles and spherules less than a millimeter in size but whose
combined mass accounts for about 1,000 tons of new stuff added to
Earth yearly. A micrometeorite is generally defined as a tiny meteorite
larger than 50 micrometers but smaller than a millimeter. Micrometeorites
that have either partially or completely melted when plunging through
Earth's atmosphere are called cosmic spherules.
Just
as the Antarctic blue ice serves as an ideal collector of meteorites,
it also preserves micrometeorites and cosmic spherules that land
on the surface and are subsequently incorporated into ice layers.
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