Window to a watery past on Mars

This 70 km-wide crater shows interesting internal features, including a smaller crater (foreground), exposed light-toned deposits (foreground/centre), and chaotic terrain (background), as well as slumped crater walls.
Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO


This 70 km-wide crater and its surrounds offer a window into the watery past of the Red Planet.



The scene, captured by ESA's Mars Express, is a composite of two images taken in March 2007 and February 2017.

It focuses on a large crater in the Margaritifer Terra region in the southern hemisphere of Mars, and includes a portion of Erythraeum Chaos to the north (right in the main colour image below).

The region is located at the northern edge of Noachis Terra, which at 3.7–4 billion years old, represents some of the oldest and most heavily cratered terrain on Mars.

Remnants of valley networks across the scene indicate that water once flowed through this region, shaping the features seen today. Indeed, as shown by the context image, Parana Valles lies to the east, while Loire Valles lies to the northwest.

There are a number of distinctive features inside the 70 km crater, such as the striking light-toned material that is interpreted as exposed bedrock.  'Chaotic terrain' is visible both inside and outside the crater, marked by randomly oriented blocks separated by troughs.  

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The scene, captured by ESA's Mars Express, is a composite of two images taken in March 2007 and February 2017.  It focuses on a large crater in the Margaritifer Terra region in the southern hemisphere of Mars, and includes a portion of Erythraeum Chaos to the north (right in the main colour image below).  The region is located at the northern edge of Noachis Terra, which at 3.7–4 billion years old, represents some of the oldest and most heavily cratered terrain on Mars.  Remnants of valley networks across the scene indicate that water once flowed through this region, shaping the features seen today. Indeed, as shown by the context image, Parana Valles lies to the east, while Loire Valles lies to the northwest.  There are a number of distinctive features inside the 70 km crater, such as the striking light-toned material that is interpreted as exposed bedrock.  'Chaotic terrain' is visible both inside and outside the crater, marked by randomly oriented blocks separated by troughs.   he scene, captured by ESA's Mars Express, is a composite of two images taken in March 2007 and February 2017.
It focuses on a large in the Margaritifer Terra in the southern hemisphere of Mars, and includes a portion of Erythraeum Chaos to the north (right in the main colour image below).
The region is located at the northern edge of Noachis Terra, which at 3.7–4 billion years old, represents some of the oldest and most heavily cratered terrain on Mars.
Remnants of valley networks across the scene indicate that water once flowed through this region, shaping the features seen today. Indeed, as shown by the context image, Parana Valles lies to the east, while Loire Valles lies to the northwest.
There are a number of distinctive features inside the 70 km crater, such as the striking light-toned material that is interpreted as exposed bedrock.
'Chaotic terrain' is visible both inside and outside the crater, marked by randomly oriented blocks separated by troughs.


Read more at: https://phys.org/news/2017-06-window-watery-mars.html#jCp

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