Frosted Gullies in a Central Pit
NASA/JPL/University of Arizona
Frosted Gullies in a Central Pit
ESP_038903_1115  Science Theme: Mass Wasting Processes
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The frosted gullies in this observation are located along an irregularly shaped pit approximately 15 kilometers wide. The pit lies within an impact crater in Sisyphi Planum that is about 35 kilometers in diameter and is located northwards of the Southern polar layered deposits.

Carbon dioxide frost covers much of the region and helps to reveal subtle textures in the landscape. The layered sediment visible in the walls of the pit and in which these gullies formed likely originally filled much of the impact crater.

Evidence for a variety of processes abound in this region. The dark, low albedo spots along some of the gullies and on the frosted debris aprons, especially along the base of the layered terrain are likely areas of defrosting, where carbon dioxide frost sublimates during southern spring. Periglacial terrain forming polygonal patterns suggests that the region is rich in near surface ground ice and volatiles.

Ice-rich landslide-like forms and sinuous ridges running along the base of the pit wall are also common, owing to the unstableness of the layered sediment that comprises the pit walls.



Written by: Ginny Gulick  (10 December 2014)
 
Acquisition date
13 November 2014

Local Mars time
16:00

Latitude (centered)
-68.458°

Longitude (East)
1.289°

Spacecraft altitude
249.2 km (154.9 miles)

Original image scale range
25.0 cm/pixel (with 1 x 1 binning) so objects ~75 cm across are resolved

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25 cm/pixel

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Polarstereographic

Emission angle
0.8°

Phase angle
60.2°

Solar incidence angle
61°, with the Sun about 29° above the horizon

Solar longitude
233.0°, Northern Autumn

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North azimuth:  99°
Sub-solar azimuth:  28.8°
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POSTSCRIPT
NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, Calif., manages the Mars Reconnaissance Orbiter for NASA’s Science Mission Directorate, Washington. The HiRISE camera was built by Ball Aerospace and Technology Corporation and is operated by the University of Arizona.