|
Entry
| Breakup
| Impact
| Composition
| History
| Time
of Day to Watch | Shower
Dates |
Imagine a
baseball zipping along at 30,000 miles per hour. That's how big and fast
many meteors are. And though some are bigger than baseballs, most are more
like grains of sand. The larger meteors are sometimes broken bits off
asteroids or other planets. The small stuff is often dust left by a
passing comet.
Entry
into the atmosphere

When they hit
the atmosphere, meteors rub against air particles and create friction,
heating them to more than 3000 degrees Fahrenheit. The intense heat
vaporizes most meteors, creating what we call shooting stars. (Most become
visible at around 60 miles up.) Some large meteors splatter, causing a
brighter flash called a fireball, and an explosion, which can often
be heard up to 30 miles away. When meteors hit the ground, they're called meteorites.
Some meteors are bits broken off asteroids, others -- mere cosmic dust --
are cast off by comets. (And one more term: A meteoroid is an
object in space that may, if it enters our atmosphere, become a meteor.)
Meteor
breakup

Whether an
object breaks apart depends on its composition, speed and angle of entry.
A faster meteor at an oblique angle suffers greater stress. Meteors
composed of iron withstand the stress better than those made of stone.
Even an iron meteor will usually break up as the atmosphere becomes denser
-- around 5 to 7 miles up.
A meteor
sometimes explodes above the surface, causing widespread damage from the
blast and ensuing fire. This happened in 1908 over Siberia.
Impact
with Earth

Extraterrestrial
objects that hit the ground, their speed roughly half what it was upon
entry, blast out craters 12 to 20 times their size. Craters on Earth form
much as they would on the moon or any rocky planet. Smaller objects create
simple, bowl-shaped craters. Larger impacts cause a rebound that creates a
central peak; slipping along the rim forms terraces. The largest impacts
form basins in which multiple rebounds form several inner peaks.
Typical
composition
|
Iron
meteorite
|
Stony
meteorite
|
Earth's
crust
|
|
Iron
91%
Nickel 8.5%
Cobalt 0.6%
Source:
Encyclopaedia Britannica
|
Oxygen
36%
Iron 26%
Silicon 18%
Magnesium 14%
Aluminum 1.5%
Nickel 1.4%
Calcium 1.3%
|
Oxygen
49%
Silicon 26%
Aluminum 7.5%
Iron 4.7%
Calcium 3.4%
Sodium 2.6%
Potassium 2.4%
Magnesium 1.9%
|
History
In ancient
times, objects in the night sky conjured superstition and were associated
with gods and religion. But misunderstandings about meteors lasted longer
than they did about most other celestial objects.
Meteorites (the
pieces that make it to Earth) were long ago thought to be cast down as
gifts from angels. Others thought the gods were displaying their anger. As
late as the 17th century, many believed they fell from thunderstorms (they
were nicknamed "thunderstones"). Many scientists were skeptical
that stones could fall from the clouds or the heavens, and often
they simply didn't believe the accounts of people who claimed to have seen
such things.
In 1807, a
fireball exploded over Connecticut, and several meteorites rained down. By
then the first handful of asteroids had been discovered, and a new theory
emerged suggesting meteorites were broken bits off asteroids or other
planets. (A theory that still holds.)
One
of the most significant meteorite events in recent history destroyed
hundreds of square miles of forest in Siberia on June 30, 1908. Across
hundreds of miles, witnesses of the Tunguska event saw a ball of fire
streak through the sky, suggesting the meteor entered the atmosphere at an
oblique angle. It exploded, sending out hot winds and loud noises and
shook the ground enough to break windows in nearby villages. Small
particles blown into the atmosphere lit the night sky for several days. No
meteorite was ever found, and for years many scientists thought the
devastation was caused by a comet. Now, the prevailing theory holds that a
meteor exploded just above the surface.
The largest
meteorite recovered in the United States fell in a wheat field in southern
Nebraska in 1948. Witnesses saw a giant fireball in the afternoon that
some said was brighter than the sun. The meteorite was found buried 10
feet deep in the ground. It weighed 2,360 pounds.
The most famous
meteorite crater in the United States is misnamed Meteor Crater. It's in
Arizona, and it's huge. The rim rises 150 feet from the surrounding plain,
and the hole is 600 feet deep and nearly a mile wide. It was the first
crater that was proved to be caused by a meteorite impact, which occurred
between 20,000 and 50,000 years ago.
Meteor
showers

When a comet
nears the sun, a trail of dust and other debris burns off and remains in
solar orbit. As Earth orbits the sun, it passes through this debris field
spread across its path. Small bits burn up in the atmosphere, creating
meteors. Meteors come from other sources, too, but comet debris streams
are the source of sometimes dramatic meteor showers.
When to watch

The part of
Earth where dawn is breaking is always at the leading edge of our planet's
plunge along its orbital path around the Sun. This part of the planet
tends to "catch" oncoming meteors left by a comet, whereas the
other side of Earth, where it is dusk or late evening, outruns the debris.
For that reason, the hours between midnight and dawn are typically the
best time to watch a meteor shower.
Some
of the primary meteor showers
|
Name
|
Peak
|
Duration
|
|
Quadrantids
|
Jan. 4
|
2 days
|
|
Perseids
|
Aug. 11
|
4-5 days
|
|
Orionids
|
Oct. 21
|
4 days
|
|
Leonids
|
Nov. 17
|
not
known
|
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