Impact Cratering
NASA
NASA
NASA
Tycho
Euler
Rays
Tycho
Rays
Visual-wavelength imageVisual-wavelength image
VisualVisual
Visual
A meteorite
approaches the
lunar surface at high
velocity.
On impact, the
meteorite is
deformed, heated,
and vaporized.
The resulting
explosion blasts out
a round crater.
Slumping produces
terraces in crater walls,
and rebound can raise
a central peak.
1
1a
The craters that cover the moon and many other bodies in
the solar system were produced by the high-speed impact of
meteorites of all sizes. Meteorites striking the moon travel 10 to 70
km/s and can hit with the energy of many nuclear bombs.
A meteorite striking the moon’s surface can deliver tremendous
energy and can produce an impact crater 10 or more times larger in
diameter than the meteorite. The vertical scale is exaggerated at
right for clarity.
1b Rock ejected from distant impacts can fall back to the
surface and form smaller craters
calledsecondary craters. The
chain of craters here is a
45-km-long chain of secondary
craters produced by ejecta from
the large crater Copernicus 200
km out of the frame to the lower
right.
Bright ejecta blankets and rays
gradually darken as sunlight alters
minerals and small meteorites stir
the dusty surface. Bright rays are
signs of youth. Rays from the
crater Tycho, perhaps only 100
million years old, extend halfway
Rock ejected from distant
impacts can fall back to the
surface and form smaller craters
calledsecondary craters. The
chain of craters here is a
45-km-long chain of secondary
craters produced by ejecta from
the large crater Copernicus 200
km out of the frame to the lower
right.
Bright ejecta blankets and rays
gradually darken as sunlight alters
minerals and small meteorites stir
the dusty surface. Bright rays are
signs of youth. Rays from the
crater Tycho, perhaps only 100
million years old, extend halfway
around the moon.
Lunar craters such as Euler,
27 km (17 mi) in diameter, look
deep when you see them near the
terminator where shadows are long,
but a typical crater is only a fifth to a
tenth as deep as its diameter, and
large craters are even shallower.
Because craters are formed by
shock waves rushing outward, by the
rebound of the rock, and by the
expansion of hot vapors, craters are
almost always round, even when the
meteorite strikes at a steep angle.
Debris blasted out of a crater is
calledejecta, and it falls back to
blanket the surface around the crater.
Ejecta shot out along specific
directions can form bright rays.
Lunar craters such as Euler,
27 km (17 mi) in diameter, look
deep when you see them near the
terminator where shadows are long,
but a typical crater is only a fifth to a
tenth as deep as its diameter, and
large craters are even shallower.
Because craters are formed by
shock waves rushing outward, by the
rebound of the rock, and by the
expansion of hot vapors, craters are
almost always round, even when the
meteorite strikes at a steep angle.
Debris blasted out of a crater is
calledejecta, and it falls back to
blanket the surface around the crater.
Ejecta shot out along specific
directions can form bright rays.