Yardangs in Danielson Crater – indicators of climate changes on Mars?

07 June 2012

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  • Perspektivische Ansicht des Danielson%2dKraters

    Perspective view of Danielson Crater

    Realistic perspective views of the surface of Mars can be generated from data acquired by the stereo and colour channels of the High Resolution Stereo Camera (HRSC) on board ESA's Mars Express spacecraft, which are oriented at an oblique angle with respect to the planet's surface. This image shows a view of Danielson Crater, in the Arabia Terra region, with its characteristics yardangs. Yardangs are rocky protrusions with streamlined shapes, formed by the removal of the softer surrounding material through wind-driven abrasion. Since they are for the most part arranged parallel to one another, the prevailing wind direction during the erosion process can be determined.

  • Anaglyphenbild der beiden Krater Danielson und Kalocsa

    Anaglyph image of the two craters – Danielson and Kalocsa

    Anaglyph images can be created from the nadir channel of the High Resolution Stereo Camera (HRSC) camera system, which looks vertically down at Mars, and one of the four stereo channels, which are directed obliquely at the surface. Using red/blue (cyan) or red/green glasses gives a three-dimensional impression of the landscape. This image shows the two craters, Danielson (with a diameter of approximately 60 kilometres) and Kalocsa (with a diameter of approximately 33 kilometres) in the Arabia Terra region. The interior of Danielson Crater is characterised by what are known as yardangs (wind-eroded rock formations); this terrain feature is entirely absent from the smaller Kalocsa Crater. The floor of Kalocsa Crater is 1000 metres higher than that of Danielson Crater.

  • Topographische Übersichtskarte der Region Arabia Terra

    Topographic overview map of the Arabia Terra region

    Arabia Terra is the transition zone between the southern highlands of Mars and the low-lying plains of the planet's northern hemisphere. The region is characterised by numerous craters filled with stratified sediments. On 19 March 2012, the High Resolution Stereo Camera (HRSC) on board ESA's Mars Express spacecraft acquired images of two craters (Danielson and Kalocsa) during orbit 10,468, from an altitude of roughly 550 kilometres. The features depicted in the other images presented here are located in the small, inner rectangle.

  • Farbdraufsicht auf die beiden Krater Danielson und Kalocsa in der Region Arabia Terra

    Colour plan view of the Danielson and Kalocsa craters in the Arabia Terra region

    This colour plan view was created by combining data from the nadir channel of the High Resolution Stereo Camera (HRSC) on board ESA's Mars Express spacecraft, which is directed vertically down onto the planet’s surface, with data from the colour channels; north is to the right in the image. Arabia Terra is the transition zone between the southern highlands of Mars and the low-lying plains of the planet’s northern hemisphere. Similar to many craters in the Arabia Terra region, Danielson Crater is filled with stratified sediments, which, over time, have become heavily eroded. The terrain forms that result from this erosion are known as 'yardangs'. Wind effects can also be identified in an area of dunes extending over a length of 30 kilometres in Danielson Crater, although these dunes were only formed in the recent geological past. The dark discolouration is probably due to volcanic material. Other striking features are the massive lava flow in the lower section of the image (to the east of the craters) and a step that marks the transition to a lower-lying area of terrain in the top left-hand section of the image (south-west).

  • Topographische HRSC%2dBildkarte der Krater Danielson und Kalocsa

    Topographic HRSC colour map of the Danielson and Kalocsa craters

    Using the High Resolution Stereo Camera (HRSC), digital terrain models can be derived that illustrate the topography of the region using false colours. The altitudes can be read from the coloured scale at the top left of the image; north is to the right. In the absence of 'sea level', the elevation data are referenced to an areoid – a modelled equipotential surface on which everything experiences the same gravitational attraction towards the centre of the planet. The height differences between the bases of these two craters are easy to detect. The floor of Danielson Crater (blue, diameter approximately 60 kilometres) lies about 1000 metres lower than that of the smaller Kalocsa Crater (diameter approximately 33 kilometres).

On 19 March 2012, the High Resolution Stereo Camera (HRSC), operated by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) and on board ESA’s Mars Express spacecraft, acquired images of two adjacent craters with very different characteristics in the Arabia Terra region. The Danielson Crater (with a diameter of approximately 60 kilometres) is characterised by a variety of features referred to as 'Yardangs', while the smaller Kalocsa Crater (with a diameter of approximately 33 kilometres) entirely lacks this kind of formation. This crater's floor is 1000 metres higher in elevation than that of Danielson Crater.

Arabia Terra is the transition zone between the southern Martian highlands and the low-lying plains of the planet's northern hemisphere. Similar to many craters in the Arabia Terra region, Danielson Crater is filled with stratified sediments that, over time, have become heavily eroded. The terrain features resulting from this erosion are known as 'yardangs'. Yardangs are rocky protrusions with streamlined shapes that formed as a result of the removal of the softer surrounding material by wind-driven abrasion. The prevailing wind direction during the erosion process can be determined since they are, for the most part, arranged parallel to one another.

Yardangs are 'milled' out of the rock by the grains of sand carried by the wind, which have a sandblasting effect. When winds blow in the same direction for an extended period of time, nozzle-like shapes can be formed – wind-blown channels – which accelerate the process. The unusual name originates from the language of the Uigurs and roughly translates as 'steep sand wall'. The Swedish researcher Sven Hedin coined the term in 1903 after observing rock formations of this kind in the Central Asian Lop Nor desert.

The yardangs in the Danielson Crater indicate that the wind must have blown primarily from the north-northeast. Researchers suspect that the sediments were initially transported into the crater by the action of the wind; there, they came into contact with water, which caused them to solidify. Later, during a dry period in the history of Mars, these formations were eroded away again. Some researchers have suggested that the changes to the sediments could be an indication of changes in the climate that were triggered by periodic shifts in Mars' rotational axis.

The effect of the wind can also be identified in an area of dunes extending over a length of 30 kilometres in Danielson Crater, although these dunes were only formed in the planet's recent geological past. The dark discolouration is probably due to volcanic material – volcanic ash or dark volcanic rock weathered down by sand and dust. This is a stark contrast to the typical ochre-coloured surface of Mars.

Impact craters as an indicator of the depth of groundwater reserves?

The smaller Kalocsa Crater presents a quite different picture; no stratified sediment deposits can be seen here. This is possibly due to the fact that this crater is not as deep. Danielson Crater is about 1000 metres deeper than Kalocsa Crater and might therefore have reached a reserve of ground water located at a greater depth, which could have caused the sediments to solidify.

Other striking features are the massive lava flow in the lower section of the image (east of the craters) and a step that marks the transition to a lower-lying area of terrain in the top left-hand section of the image (south-west). Here, part of the ejecta from the smaller Kalocsa Crater extends like a promontory into the lower-lying surroundings. At the edge of these ejecta, a crater about five kilometres across – which is almost entirely filled – is visible. This suggests that the ejecta blanket once stretched further into the surrounding area. In addition, a number of small, bump-shaped elevations can be identified. These are likely remnants of a terrain that once reached a much higher altitude.

Image processing and the HRSC experiment on Mars Express

These HRSC images were acquired during Mars Express orbit 10,468. The image resolution is approximately 26 metres per pixel. The data was acquired at approximately 7 degrees north and 353 degrees east.

The plan-view colour image was created from the nadir channel, the field of view of which is aligned perpendicular to the surface of Mars, and the colour channels; the oblique perspective view was generated from HRSC stereo channel data. The anaglyph, which creates a three-dimensional impression of the landscape when viewed with red/blue or red/green glasses, was derived from the nadir channel and one stereo channel. The colour-coded plan view is based on a digital terrain model of the region, from which the topography of the landscape can be derived.

The HRSC camera experiment on the European Space Agency's Mars Express mission is headed by Principal Investigator (PI) Professor Gerhard Neukum (Freie Universität Berlin), who was also responsible for the technical design of the camera. The science team consists of 40 co-investigators from 33 institutions in ten nations. The camera was developed at DLR under the leadership of the PI and it was built in cooperation with industrial partners EADS Astrium, Lewicki Microelectronic GmbH and Jena-Optronik GmbH. The instrument is operated by the DLR Institute of Planetary Research in Berlin-Adlershof. The systematic processing of the HRSC image data is carried out at DLR. The images shown here were created by the Institute of Geological Sciences at Freie Universität Berlin.

Last modified:
07/06/2012 10:24:49

Contacts

 

Elke Heinemann
Deutsches Zentrum für Luft- und Raumfahrt (DLR) - German Aerospace Center

Tel.: +49 2203 601-2867

Fax: +49 2203 601-3249
Prof.Dr. Ralf Jaumann
German Aerospace Center (DLR)

Institute of Planetary Research, Planetary Geology

Tel.: +49 30 67055-400

Fax: +49 30 67055-402
Ulrich Köhler
Deutsches Zentrum für Luft- und Raumfahrt (DLR) - German Aerospace Center

Tel.: +49 30 67055-215

Fax: +49 30 67055-402