#78 MARTIAN TERRAIN
Boulder Tracks on the Slopes of Noctis Labyrinthus.
This image spans the floor and two walls of a pit in Noctis Labyrinthus, a system of deep, steep-walled valleys on the western edge of Valles Marineris.
The valleys themselves are tectonic features known as graben - trench-like features that form in response to extension (or stretching) of the crust. In the case of Noctis Labyrinthus, volcanic activity in the Tharsis region may have formed a bulge, which then stretched and fractured the crust above it.
The subimage focuses on one of the pit walls, where numerous boulder tracks criss-cross each other in a large patch of smooth, dust-covered terrain. Boulders leave linear patterns in the dust as they tumble down the steep slopes.
Written by: Nicole Baugh
The valleys themselves are tectonic features known as graben - trench-like features that form in response to extension (or stretching) of the crust. In the case of Noctis Labyrinthus, volcanic activity in the Tharsis region may have formed a bulge, which then stretched and fractured the crust above it.
The subimage focuses on one of the pit walls, where numerous boulder tracks criss-cross each other in a large patch of smooth, dust-covered terrain. Boulders leave linear patterns in the dust as they tumble down the steep slopes.
Written by: Nicole Baugh