X-Nico

unusual facts about meteorites



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3103 Eger

4 Vesta is the parent body for Howardite, Eucrite, and Diogenite meteorites, while 3103 Eger is the parent body for Aubrite meteorites.

8 Flora

Flora, and the whole Flora family generally, are good candidates for being the parent bodies of the L chondrite meteorites.

Cassidy Glacier

The glacier was named by the Advisory Committee on Antarctic Names in 1992 after William A. Cassidy, Department of Geology and Planetary Science, University of Pittsburgh, who in 13 field seasons, 1976–90, led United States Antarctic Research Program teams in the investigation and collection of Antarctic meteorites from diverse sites through Victoria Land and southward to Lewis Cliff, adjacent to the Queen Alexandra Range.

Flora family

The Flora family members are considered good candidates for being the parent bodies of the L chondrite meteorites (Nesvorny 2002), which contribute about 38% of all meteorites impacting the Earth.

Fort Rock

They resemble impact craters formed by meteorites, but lack the heavy metal signature residues of space objects.

Hypoxanthine

In August 2011, a report, based on NASA studies with meteorites found on Earth, was published suggesting hypoxanthine and related organic molecules, including the DNA and RNA components adenine and guanine, may have been formed extraterrestrially in outer space.

Mbozi meteorite

The Germanium-Gallium ratio is larger than 10, which can also be seen in meteorites of the IIF iron meteorite group and the Eagle station pallasites.

Meteoric iron

When meteorites make their descent through the atmosphere outer parts are ablated.

Michael D. Reynolds

He worked with Meade Instruments in 2005 to develop and create Meade’s MeteoriteKit, a special set of meteorites, tektites, and impactites.

Micrometeorite

Carbonaceous chondrite, a class of chondritic meteorites comprising at least seven known groups and many ungrouped

Walter Flight

The later papers were chiefly upon meteorites, dealing in detail with the recorded circumstances of their fall, and with their mineralogical and chemical constituents; several, written in conjunction with Professor Story-Maskelyne, give accounts, published in the 'Philosophical Transactions,' of the meteorites which fell at Rowton in Shropshire, at Middlesbrough, England, and at Cranbourne, Australia.


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