Space Nomads: Meteorites in Sky, Field, and LaboratoryLaPaz, Lincoln
Science
Space Nomads: Meteorites in Sky, Field, and Laboratory
LaPaz, Lincoln
Meteorites
Many weathered pebbles and fragments of obsidian somewhat resemble the
tektites superficially. There is a very simple test by which you can
distinguish true tektites from obsidian. If you hold a thin splinter of
tektite glass in a blowpipe flame, the glass melts quietly but only with
the greatest difficulty. On the contrary, when you test in the same
flame the terrestrial glass, obsidian, it froths up much more easily,
into a bubbly, whitish mass.
Although the question of where the tektites came from is still not
entirely settled, most scientists agree that all tektites did have a
_common_ origin. For example, tektites from widely scattered localities
on the earth’s surface show not only similar queer shapes and surface
markings (technically known as “sculpturing”), but also have very much
the same chemical composition and, in particular, the same content of
radioactive elements.
Because the tektites chemically resemble certain terrestrial rocks,
scientists at first believed that some kind of earth process must have
created them. One suggestion was that lightning had fused dust particles
suspended in the air to form them; another, that they had come from
volcanoes; still another, that the tektites were simply inclusions that
had weathered out of terrestrial rocks. A few scientists once took
seriously the possibility that tektites were refuse from primitive glass
factories!
[Illustration: Tektite vs. obsidian, after blowpipe test.]
While such theories have not yet been completely discarded, most
scientists now feel that the tektites had their origin somewhere outside
the earth. There are several reasons for this belief. First, the shape
of such unusually symmetrical forms as are found, for example, among the
australites, indicates that these small bodies at one time were members
of a swarm of freely-spinning liquid masses. Again, flow features
observed on the surfaces of certain tektites (and the fusion crust
definitely identified on one specimen) show that these bodies at some
time must have traveled through the earth’s atmosphere at high velocity.
If, then, the tektites were not produced by earth processes, where did
they come from? According to primitive legends, they were “rocks” or
“pebbles” from the moon. Indeed, one of the earliest scientific theories
as to their origin (proposed by the Dutch authority Verbeek in 1897)
likewise attributes them to debris jetted out from the moon. Another
holds that tektites are fragments of the outermost glassy layers of some
so-called “meteorite-planet,” or planets.[8] Still another idea is that
tektites are what is left of a comet when it passes so close to the
blazing-hot sun that the “ices” which make up most of the cometary
nucleus (head) are all distilled away.
Public-domain text, read in full here on John Shaqi.
Space Nomads: Meteorites in Sky, Field, and Laboratory — John Shaqi
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