| The Cambridge Encyclopedia of Meteorites
by O. Richard Norton
Cambridge University Press, Cambridge, England, 2002, Hardcover, 11" x 8-3/4",
354 pages, $50.00.
Reviewed by June Culp Zeitner
Almost
everyone is entranced by these fiery visitors from the sky. Where do they originate?
How do you know if you have found one? How many fall to Earth? What kind is the
rarest? What is the largest? Are they dangerous? At last, here is a book that
will not only answer all of your questions, but take you on a journey through
the skies of the centuries and the landing fields of celestial rocks.
Noted astronomer and meteoriticist Dr. Norton, author of Rocks from Space,
has been director of leading planetariums and has designed optical telescopes
and the hemispheric projection system which is the forerunner of Imax. He founded
Science Graphics company, producing science teaching aides used by over 3,000
universities. Norton is also a Contributing Editor of the journal Meteorite.
The smallest meteorites are interplanetary dust. The largest are over 200 kilometers
in diameter. There are 20 classes of meteorites. The most common minerals in them
are iron, nickel, olivine, and hyperthene. (For gem enthusiasts, some of the olivine
is facetable. Diamonds have been present in others.) Several times reports have
hinted at fossils in a meteorite, but this has never been proven.
Chondrites are of particular interest to me, since I mistook one that my father-in-law
found for a terrestrial rock. Chondrites alone have five classes, and one of these,
carbonaceous, has numerous subdivisions with various textures and inclusions.
Many meteorite falls have been witnessed, some inflicting damage on vehicles
or buildings, but the scientific study of meteorites is quite recent. People are
alert to the chance of finding a space visitor, so tens of thousands of meteorites
have been found since the mid-1900s, when only 2,000 were known. Irons are the
easiest to recognize, but there are also stones and stony irons. Some meteorites
are found strewn in fields. Since the serious study of meteorites began, many
craters have been identified, including the gigantic Chicxulub crater, believed
by some to be responsible for the K-T extinction during which so many species
disappeared.
There are so many questions about meteorites that Norton discusses in his book,
readers gain a new appreciation of the complexity of this great science. There
are sections about the age of the universe, asteroids, Martian meteorites, and
lunar meteorites.
The book covers this new science thoroughly. It is well-written and understandable,
with exceptional illustrations and graphics. The six appendices and the glossary
provide an additional education in this fascinating field. It is time for a complete
encyclopedia on meteorites and anyone interested in the universe or Earth will
find it indispensable.
June Culp Zeitner, who has been writing for the Lapidary Journal since 1956 and
joined the editorial staff in 1967, is the author of nine gem and mineral books,
and helped start the National Rockhound and Lapidary Hall of Fame.
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