is a chunk of rock or iron that has landed on the ground after surviving a fiery passage through the atmosphere. Meteorites are believed to be pieces of asteroids most likely originating in the asteroid belt between the planets of Mars and Jupiter. After wandering the solar system for countless ages, enduring collisions, and the effects of gravitational forces, they fall to Earth.
When the path of these space rocks intersects with Earth's orbit, the meteoroid enters the atmosphere at high velocity causing the luminous phenomena we call a meteor or shooting star. These meteors should not be confused with a meteor shower
. Meteor showers involve the Earth passing through a comets orbit.
A very bright meteor is called a fireball and may be called a bolide if associated with a smoke train and detonations (which often produces meteorites). These events can also be tremendous force of nature. The recent Russian meteor sonic boom and shock wave
on February 15, 2013 caused considerable property damage and injury to people.
Sometimes the forces on these objects are too great and fragmentation will occur resulting in a few to even many thousands of individual pieces. The area on the ground surface meteorites cover is a distribution ellipse also know as a strewnfield.
As the meteoroid passes through the atmosphere, ablation occurs where melting and vaporization removes material from the surface. This ablation can also produce regmaglyphs
which are flight marks produced during the passage of a meteoroid through the atmosphere and often look like thumbprints pushed into the surface. This melting of the exterior surface from heating due to it's high velocity through Earth's atmosphere is also what causes the fusion crust
seen on the exterior of meteorites.
An oriented meteorite
is formed when it's passage through the atmosphere is in a stable orientation. It receives the characteristic ablation features from being melted mostly on one surface. Among these features are a rounded front surface or a cone shape and often radial lines of melting
in the front surface, and a rolled over lip of melted material which has cooled around the circumference of the back side.
On very rare occasions large meteoroids will reach the ground with enough velocity and mass to form an impact crater. The best preserved impact crater today is Meteor Crater in Arizona
. Associated with impact structures and craters is a type of rock called an impactite
. This glassy rock, also called crater glass
, is formed from the melting of native rocks during the impact of asteroids. A second glassy object associated with impact events but much less understood are tektites. A tektite
is a natural glass object formed by the melting of native rocks during some asteroid impacts. Some tektites, the Australites, receive aerodynamic shapes as the still plastic but cooling glass falls back to the surface from very high altitude. Muong Nong
tektite glass may be from a melt sheet formed near the impact site.
There is much incorrect information on the internet but you can double check your meteorite facts
with some of the following sites. The Meteoritical Society
is the International Society for Meteoritics and Planetary Science. A great source for information and articles is our Meteorite Times Magazine
which is a free online bi-monthly publication. A great source of meteorite pictures
and information is the Encyclopedia of Meteorites
website. The Meteoritical Bulletin Database
site is a great bookmark to have and you'll use it often. Here's some good advice for people who think they may have found a meteorite
. The best social forum, Club Space Rock
is a friendly, informative, interactive meteorite community.
Meteorite Information & Articles
There are three basic types of meteorites
. Iron Meteorites which consist of mostly iron with varying amounts of nickel. The second and most abundant group is the Stone Meteorites made up of silicate minerals with a small amount of metal grains. The third group is the Stony-Iron Meteorites which contain roughly half mineral and half nickel iron metal. Most are believed to originate from the asteroid belt but there are also meteorites proven to be from the Moon and Mars.
Iron meteorites are made of solid metal and sometimes inclusions of minerals and silicate but the majority of the mass will be nickel-iron metal. Iron meteorites with very little nickel are called Hexahedrites and have no distinctive pattern when etched. The very high nickel content meteorites are called Ataxites and the third is a large group of iron meteorites called the Octahedrites which have a crystal structure formed by a mixture of both Taenite and Kamacite.
The largest group of meteorites by far is the stony meteorites. Made of minerals that for the most part are the same as minerals that are found on Earth. However,they have structures and textures not found here. The stony meteorite group is divided into two major subgroups; the chondrites and the achondrites. The chondrites get their name because of the spherical mineral structures they contain called chondrules. In space the molten droplets of rock material cooled in the very low gravity into tiny round spheres that crystallized into minerals. Achondrites are stony meteorites without chondrules. These meteorites have an igneous mineral structure with crystals that indicate they formed in an environment with some gravity. In most stony meteorites there is metallic nickel-iron. The metal is in the form of grains scattered throughout the matrix of the rock.
The Stony-Iron meteorites are made of both nickel iron metal and stone and this group includes two large sub groups, the pallasites and the mesosiderites. The Pallasites are characterized by having a large portion of their mass in the form of olivine crystals with these crystals being surrounded by nickel-iron. Mesosiderites have silicate minerals found commonly in many iron meteorites but the amount of silicates gets quite high resulting in these meteorites classified as mesosiderites.
Meteorites from the Moon & Mars
Lunar meteorites are mostly volcanic rocks called basalts. Over time the impacts on the Moon have broken the rocks into fragments that have been melted and reformed into rocks called breccias. Lunar meteorites will often show small individual areas of different colors that make up these breccias and are called clasts. Moon rocks are very old. Volcanic activity is believed to have stopped early in the Moon's history.
Mars meteorites can be broken down into three distinct groups. They are Shergotty, Nakhla, and Chassigny which form a grouplet of planetary meteorites know as the SNC group. Scientists have proven that these meteorites came from Mars by comparing the trapped Martian atmosphere in the meteorites compared with the measurements of the Martan atmosphere by the NASA Viking spacecraft that landed on Mars in 1976.
Author: James Tobin [Google