Most of the large asteroids in the Asteroid Belt are already known, so this means that either the meteorite originated on an asteroid that has been eroded, or there is another large asteroid out there.
Not exact matches
These facilities,
most notably the
Large Synoptic Survey Telescope (LSST) set to debut in 2020, promise to revolutionize the field
of «transient» astronomy — the study not
of steady - shining stars and galaxies, but
of the things that rapidly move and change: exploding stars, whirling
asteroids and comets, and anything else that goes «bump!»
These core samples contain bits
of the original granite bedrock that was the unlucky target
of cosmic wrath 66 million years ago, when a
large asteroid struck Earth, blasted open the 180 - kilometer - wide Chicxulub crater, and led to the extinction
of most life on the planet.
New images indicate that
most of the cavities are secondary impacts from rocks kicked up when
large asteroids hit.
That feature — in which the crust thickness drops from 30 to about 10 miles (50 to 20 kilometers) over a
large area that is the
most visible feature on Mars — has been known to astronomers for more than 30 years and was long suspected to be due to an
asteroid impact that flung
most of the crust out the area.
But in spite
of this,
most civilian astronomers believe that tackling the catastrophically
large but very rare impacts should be the first priority («How to destroy the doomsday
asteroid», New Scientist, 6 June).