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Gusev is a crater on the planet Mars and is located at 175.4°E 14.6°S. The crater is about 170 kilometers in diameter and formed approximately three to four billion years ago. It was named after Russianmarker astronomer Matvei Gusev (1826–1866) in 1876.

A channel system named Ma'adim Vallis drains into it that probably carried liquid water, or water and ice, at some point in Mars' past. The crater appears to be an old crater lake bed, filled with sediments up to 3000 feet thick. Some exposed outcrops appear to show faint layering, and some researchers also believe that landforms visible in images of the mouth of Ma'adim Vallis where it enters Gusev resemble landforms seen in some terrestrial river deltas. Deltas of this nature can take tens or hundreds of thousands of years to form on Earth, suggesting that the water flows may have lasted for long periods. Orbital images indicate that there may once have been a very large lake near the source of Ma'adim Vallis that could have provided the source of this water. It is not known whether this flow was slow and continuous, punctuated by sporadic large outbursts, or some combination of these patterns.
Panoramic photo taken by Spirit Rover on January 1, 2006 from the crater Gusev, looking up a slope and across rippled sand deposits in a dark field dubbed "El Dorado".


More recently, satellite images showed the trails of dust devils on Gusev's floor. The Spirit rover later photographed dust devils from the ground, and likely owes much of its longevity to dust devils cleaning its solar panels.

On January 3, 2004, Gusev was the landing site of the first rover in NASAmarker's two Mars Exploration Rovers, named Spirit. It is hoped that the numerous smaller and more recent craters in this region will have exposed sedimentary material from early eras, although at first the region proved disappointing in its lack of available bedrock for study on the flat lava plains of the crater, Spirit's landing site. She eventually arrived at the Columbia Hills, however, and rocks examined in that region show that the Columbia Hills did have small amounts of briny (salty) water interacting with them in ancient times, though nowhere near as much as Meridiani Planum, the landing area for Spirit's twin, Opportunity.

Features within Gusev

Hills

  • The Columbia Hills is a range of low hills 3 km from Spirit's original landing site; Spirit is currently exploring them
  • The Apollo 1 Hills are three widely-spaced hills 7–14 km away from Spirit's landing site


Craters

  • Bonnevillemarker is a 200-metre crater visited by Spirit
  • Crivitz is a smaller crater located within Gusev
  • Thira is a crater located within Gusev, and could be seen from the summit of Husband Hill


Other

  • Sleepy Hollow is a shallow depression near Spirit's landing site
  • Adirondackmarker is the name of the first rock visited by Spirit
  • Home Platemarker is a layered geological feature recently studied by Spirit


See also



References

  1. Aqueous processes at Gusev crater inferred from physical properties of rocks and soils along the Spirit traverse


External links




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