Tikhonravov (Martian crater)
Planet | Mars |
---|---|
Coordinates | 13°30′S 324°12′W / 13.5°S 324.2°WCoordinates: 13°30′S 324°12′W / 13.5°S 324.2°W |
Diameter | 386 km |
Eponym | Mikhail Tikhonravov |
Tikhonravov is a large, eroded crater in the Arabia quadrangle of Mars. It is 386.0 kilometres (240 mi) in diameter and was named after Mikhail Tikhonravov, a Russian rocket scientist.[1] Tikonravov is believed to have once held a giant lake that drained into the 4500 km long Naktong-Scamander-Mamers lake-chain system. An inflow and outflow channel has been identified.[2] Many craters once contained lakes.[3] [4] [5]
Pedestal craters
Some craters in Tikhonravov are classified as pedestal craters. A pedestal crater is a crater with its ejecta sitting above the surrounding terrain. They form when an impact crater ejects material which forms an erosion resistant layer, thus causing the immediate area to erode more slowly than the rest of the region. The result is that both the crater and its ejecta blanket stand above the surroundings.[6]
- Map of Arabia quadrangle with major craters.
- Tikhonravov crater floor, as seen by Mars Global Surveyor. Click on image to see dark slope streaks and layers.
- Streaks on side of pedestal crater in Tikhonravov, as seen by HiRISE. Scale bar is 500 meters long. Click on image to see close-up of the crater edge.
- Close-up of layers in Tikhonravov in Arabia, as seen by Mars Global Surveyor, under the MOC Public Targeting Program. Layers may form from volcanoes, the wind, or by deposition under water. The craters on the left are pedestal craters.
- Layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program. Pedestal crater is within the much larger Tikhonravov Crater.
- Layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program. Pedestal crater is within the much larger Tikhonravov.
- Close-up of some layers under cap rock of a pedestal crater, as seen by HiRISE under HiWish program.
- Close-up of some layers under cap rock of a pedestal crater and a dark slope streak, as seen by HiRISE under HiWish program.
References
- ↑ Gazetteer of Planetary Nomenclature: Tikhonravov
- ↑ Fassett, C. and J. Head III. 2008. Valley network-fed, open-basin lakes on Mars: Distribution and implications for Noachian surface and subsurface hydrology. Icarus: 198. 39-56.
- ↑ Cabrol, N. and E. Grin. 2001. The Evolution of Lacustrine Environments on Mars: Is Mars Only Hydrologically Dormant? Icarus: 149, 291-328.
- ↑ Fassett, C. and J. Head. 2008. Open-basin lakes on Mars: Distribution and implications for Noachian surface and subsurface hydrology. Icarus: 198, 37-56.
- ↑ Fassett, C. and J. Head. 2008. Open-basin lakes on Mars: Implications of valley network lakes for the nature of Noachian hydrology.
- ↑ http://hirise.lpl.arizona.edu/PSP_008508_1870
See also
- HiWish program
- Impact crater
- Impact event
- Groundwater on Mars
- List of craters on Mars
- Ore resources on Mars
- Planetary nomenclature
- Pedestal crater
- MOC Public Targeting Program
- Water on Mars