Mars crater shows evidence for climate evolution

Jun 07, 2012
High-Resolution Stereo Camera (HRSC) nadir and colour channel data taken on 19 June 2011 by ESA’s Mars Express have been combined to form a natural-colour view of the Danielson and Kalocsa craters and their environment in the Arabia Terra region. Centred at around 7°N and 353°E, this image has a ground resolution of about 26 m per pixel. The image shows the yardangs bisected by the darker dune field in Danielson crater. Credits: ESA/DLR/FU Berlin (G. Neukum)

(Phys.org) -- ESA’s Mars Express has provided images of a remarkable crater on Mars that may show evidence that the planet underwent significant periodic fluctuations in its climate due to changes in its rotation axis.

On 19 June 2011, Mars Express pointed its high-resolution stereo camera at the Arabia Terra region of Mars, imaging the Danielson and Kalocsa craters.

Danielson crater is named after the late George E Danielson, who was instrumental in the development of many spacecraft cameras flown to Mars. Seen to the right (north) in the image, it is the larger crater, roughly 60 km across.

This computer-generated perspective view was created using data obtained from the High- Resolution Stereo Camera (HRSC) on ESA’s Mars Express. Centred at around 7°N and 353°E, this image has a ground resolution of about 26 m per pixel. A part of Danielson crater dominates this view with the detailed relief of the yardangs being interrupted by the 30 km-long field of dark dunes. The uniform thickness in the alternating sedimentary layers provides evidence for the theory that periodic changes in the climate of Mars occurred, possibly due to changes in the planet’s rotation axis. Credits: ESA/DLR/FU Berlin (G. Neukum)

Kalocsa crater lies in the centre of the image and is smaller, about 33 km in diameter and a kilometre shallower than Danielson. It is named after a town in Hungary famed for its astronomical observatory.  

Danielson crater, like many in the Arabia Terra region, is filled with layered sediments, which in this instance have been heavily eroded over time. Within the crater are peculiarly layered buttes, known as yardangs.

Yardangs are streamlined hills carved from bedrock or any consolidated or semi-consolidated material by abrasive dust and sand particles carried in the wind.

They are seen on Earth in desert regions, with notable examples in North Africa, Central Asia and Arizona in the United States.

In the case of Danielson crater, it is believed that sediments were cemented by water, possibly from an ancient deep groundwater reservoir, before being eroded by the wind.

The orientation of the yardangs leads scientists to theorise that strong north–northeasterly winds (from the lower right in the image) both deposited the original sediments and then caused their subsequent erosion in a later drier period of martian history.

This colour-coded plan view is based on a digital terrain model of the region, from which the topography of the landscape can be derived. Note the strong view in colour relief of the ejecta blanket surrounding Kalocsa crater, and the marked change in depth where the darker dune region bisects the centre of Danielson crater. Centred at around 7°N and 353°E, this image has a ground resolution of about 26 m per pixel. Credits: ESA/DLR/FU Berlin (G. Neukum)

A 30 km-long field of darker dunes can be seen bisecting the yardangs and is thought to have formed at a later epoch.

The crater floor of Danielson shows evidence for a series of alternating sedimentary layers with roughly uniform thickness and separation.

Some scientists believe that this indicates periodic fluctuations in the climate of , triggered by regular changes in the planet’s axis of rotation. The different layers would have been laid down during different epochs.

By marked contrast, Kalocsa crater shows a completely different topography.

Here, no layered sediments are seen. This is thought to be due to the higher altitude of its floor, with the crater not tapping in to the suspected underlying ancient water reservoir.

Another hypothesis is that this is younger than its neighbour, created when water was not present anymore.

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