The Mars we see today has a thin, cold and dry atmosphere. Across its surface lie vast dune seas of wind blown sediment. Yet Mars was once an dynamic world with active volcanoes, a denser atmosphere, and possibly liquid water on its surface. Meteorites blasted off of the Red Planet suggest to some that Mars may once have supported microbial life.
The primary task of the missions to Mars is to help us to understand the current climate of Mars and how it has evolved over time.
Mars mission hotline (800) 391-6654 or (818) 354-2410 (Select 4 from voice menu)
NASA to launch two Mars Moble Landers for 2003!
A Movie of the mission can be found Here
This photomicrograph shows one of the bacteria like structures found within the Martian
meteorite.
This elliptical crater is located on the slope of the giant Martian volcano known as Ceraunius Tholus. The volcano has been eroded and probably consists of ash deposits. Ceraunius Tholus is about the size of the Big Island of Hawaii. The elliptical impact crater, just above Ceraunius Tholus formed after the volcano. Such craters are formed from the impact of asteroids or comets that have a very shallow angle of approach. In the process of crater formation some material is ejected to the side and some may also be hurled outward and into space. Remember that this crater is thought to have been the source of some of the Martian meteorites (such as Zagami), but not the meteorite with the evidence of life.
Here is an image of
the Martian meteorite (ALH84001) which was
found in Antarctica in 1984. The actual crater from which ALH84001
came from may have been found.
Read this!
Here are two images of other Martian meteorites
image 1 and
image 2
WWW references on Mars and Martian Meteorites (a.k.a. SNC Meteorites):
MARS (SNC) Meteorites from JPL
Mars from Solar Views
Mars
PDS Mars Explorer for the Armchair Astronaut
updated 09-11-2002
This page was created by the Lake Afton Public
Observatory