Escalante (Martian crater)
Escalante Crater is an impact crater in the Amenthes quadrangle of Mars. It is located at 0.2° N and 244.7° W. It is 79.3 km (49.3 mi) in diameter, and was named after Mexican astronomer (c. 1930) Francisco Javier Escalante Plancarte.[1]
- Map of Amenthes quadrangle. The northwest part is the large impact basin Isidis. The crater Escalante sits right on the equator.
- CTX camera (on Mars Reconnaissance Orbiter) image of Escalante Crater. Dunes are visible near the bottom of the image.
- Enlargement of dunes in Escalante Crater from previous photo. Image taken with CTX camera (on Mars Reconnaissance Orbiter).
Planet | Mars |
---|---|
Coordinates | 0.2°N 244.7°W |
Quadrangle | Amenthes |
Eponym | Mexican astronomer F. Escalante |
Impact craters generally have a rim with ejecta around them, in contrast volcanic craters usually do not have a rim or ejecta deposits. As craters get larger (greater than 10 km in diameter) they usually have a central peak.[2] The peak is caused by a rebound of the crater floor following the impact.[3] If one measures the diameter of a crater, the original depth can be estimated with various ratios. Because of this relationship, researchers have found that many Martian craters contain a great deal of material; much of it is believed to be ice deposited when the climate was different.[4] Sometimes craters expose layers that were buried. Rocks from deep underground are tossed onto the surface. Hence, craters can show us what lies deep under the surface.
See also
References
- "Gazetteer of Planetary Nomenclature". planetarynames.wr.usgs.gov. Feature 1841. USGS. 17 November 2010. Retrieved 2022-04-15.
- "Stones, Wind, and Ice: A Guide to Martian Impact Craters".
- Hugh H. Kieffer (1992). Mars. University of Arizona Press. ISBN 978-0-8165-1257-7. Retrieved 7 March 2011.
- Garvin, J., et al. 2002. Global geometric properities of martian impact craters. Lunar Planet Sci. 33. Abstract @1255.