29. October 2020
Mars Express mission

Blurred craters on Mars – traces of for­mer glacia­tion in the south­ern high­lands

View of a crater triplet in the Noachis Terra region on Mars
View of a crater triplet in the Noachis Ter­ra re­gion on Mars
Image 1/5, Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO

View of a crater triplet in the Noachis Terra region on Mars

The im­age shows three su­per­im­posed im­pact craters. The largest of them mea­sures 45 kilo­me­tres across, the mid­dle one ap­prox­i­mate­ly 34 and the small­est 28. One sce­nario for the for­ma­tion of the crater triplet be that a me­te­oroid broke in­to at least three pieces on en­ter­ing the Mar­tian at­mo­sphere be­fore all three bod­ies suc­ces­sive­ly hit the sur­face. How­ev­er, it could al­so be a co­in­ci­dence that three im­pactors hit Mars in­de­pen­dent­ly at al­most the same po­si­tion and over a some­what greater time in­ter­val.
Signs of glacial activity in a crater triplet on the southern highlands of Mars
Signs of glacial ac­tiv­i­ty in a crater triplet on the south­ern high­lands of Mars
Image 2/5, Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO

Signs of glacial activity in a crater triplet on the southern highlands of Mars

The oblique per­spec­tive view in­to the crater triplet, lo­cat­ed in the Noachis Ter­ra re­gion, clear­ly shows the flow traces of rock glaciers at the bot­tom of the crater. The dark patch in the largest crater rep­re­sents a small ac­cu­mu­la­tion of dark sands, which else­where on Mars form nu­mer­ous im­pres­sive dune fields. Es­pe­cial­ly in the two craters on the right-hand side of the im­age, deeply in­cised gul­lies tes­ti­fy to the ero­sive ac­tiv­i­ty of flow­ing wa­ter.
Topographic map of a crater triplet in Noachis Terra
To­po­graph­ic map of a crater triplet in Noachis Ter­ra
Image 3/5, Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO

Topographic map of a crater triplet in Noachis Terra

Sci­en­tists from DLR and Freie Uni­ver­sität Berlin com­pute dig­i­tal ter­rain mod­els from im­age strips of the sur­face on Mars, ac­quired from dif­fer­ent an­gles by the High Res­o­lu­tion Stereo Cam­era (HRSC) on board Mars Ex­press. In this pro­cess, height in­for­ma­tion is as­signed to ev­ery pix­el. The colour cod­ing of the dig­i­tal ter­rain mod­el (see key at top right) pro­vides in­for­ma­tion about height dif­fer­ences in this crater triplet, which lies to the east of the Le Ver­ri­er crater. North is to the right of the im­age. This shows that the three craters rep­re­sent de­pres­sions in the Mar­tian high­lands that are more than 1500 me­tres deep, de­spite clear signs of ad­vanced ero­sion – ev­i­denced by the crater rims ris­ing on­ly slight­ly above the sur­round­ing plain. Sed­i­ments have filled all three craters – orig­i­nal­ly, they had a depth of three to four thou­sand me­tres from the crater rim to the cen­tre of the crater de­pres­sion.
3D view of a crater triplet in Noachis Terra
3D view of a crater triplet in Noachis Ter­ra
Image 4/5, Credit: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO

3D view of a crater triplet in Noachis Terra

Anaglyph im­ages can be cre­at­ed us­ing da­ta ac­quired by the nadir chan­nel of the High Res­o­lu­tion Stereo Cam­era (HRSC) op­er­at­ed by DLR on board ESA’s Mars Ex­press space­craft (the field of view of which is aligned per­pen­dic­u­lar to the sur­face of Mars) and one of the four oblique-view­ing stereo chan­nels. When viewed with red-blue or red-green glass­es, these im­ages give a three-di­men­sion­al view of the land­scape. North is to the right of the im­age. The high im­age res­o­lu­tion clear­ly cap­tures the di­verse to­pog­ra­phy of this re­gion in­clud­ing the dis­tinc­tive lin­ear struc­tures in the north­ern­most crater, which trace the plas­tic flow of rock glaciers with de­bris on the sur­face.
Topographic overview map of the surroundings of a crater triplet in Noachis Terra
To­po­graph­ic overview map of the sur­round­ings of a crater triplet in Noachis Ter­ra
Image 5/5, Credit: NASA/JPL (MOLA); FU Berlin

Topographic overview map of the surroundings of a crater triplet in Noachis Terra

The High Res­o­lu­tion Stereo Cam­era (HRSC) op­er­at­ed by the Ger­man Aerospace Cen­ter (Deutsches Zen­trum für Luft- und Raum­fahrt; DLR) im­aged a crater triplet in the south­ern high­land re­gion of Noachis Ter­ra on 6 Au­gust 2020 dur­ing Mars Ex­press or­bit 20,982. The south­ern hemi­sphere has a sig­nif­i­cant­ly high­er num­ber of im­pact craters than the north­ern hemi­sphere, tes­ti­mo­ny to its greater age.
  • These images of Mars, acquired by the DLR-operated HRSC instrument, show a crater triplet in the Noachis Terra region in the southern highlands of Mars.
  • The southern hemisphere has a significantly higher number of impact craters than the northern hemisphere, testimony to its greater age.
  • Some of the impact craters in this region appear to have ‘melted’ and almost become flattened, which can be explained by flow movements of ice beneath the surface.
  • HRSC has been mapping the Red Planet in unprecedented resolution, in three dimensions and in colour, since 2004 – as part of ESA’s Mars Express mission.
  • Focus: Space, planetary research, Mars

These High Resolution Stereo Camera (HRSC) images show a rare crater triplet, located in the Noachis Terra region in the southern highlands of Mars. HRSC has been mapping the Red Planet in unprecedented resolution, in three dimensions and in colour, since 2004 as part of ESA's Mars Express mission. It was developed at the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) and built in cooperation with German industry. It is operated by the DLR Institute of Planetary Research. In addition to global topography, Mars Express provides new data on the geology, mineralogy and atmosphere of Mars, in order to gain insights into the climate history of our neighbouring planet and to clarify the role of water and the location of the water that is still present.

Age, formation and geology

The highland regions of the southern hemisphere of Mars are covered with impact craters. The craters are much more numerous than in the northern hemisphere, which proves that these regions are among the oldest on the planet. One of these regions is called Noachis Terra and gave its name to the Noachian Period, an epoch that lasted from approximately 4.1 to 3.7 billion years ago and was marked by a strong bombardment by meteorites and asteroids. In this early phase of the planet, large regions were topographically shaped, hence the name Noah, after the ark builder in the Old Testament. The images show three superimposed impact craters. The largest of them measures 45 kilometres across, the middle one approximately 34 and the smallest 28. One scenario for the formation of the craters could be that a meteoroid broke into at least three pieces before all three bodies hit the surface of Mars in succession.

However, it could also be a coincidence that three impactors hit Mars independently at almost the same location over a somewhat longer time interval. Due to the fact that there are still residues of its ejecta blanket around the smallest crater, it is obvious that this smaller crater was formed after the two larger ones. Their ejecta blankets have long since been eroded and blurred. At the northern rim of the crater triplet (top right in images 1, 3, 4) another small, circular structure is visible, possibly representing a fourth, now filled impact crater.

Craters filled with sediment and ice

Like many other impact craters in the southern highlands, these three craters show typical rims that have already been smoothed out by erosion, as well as shallow and fairly flat crater floors, indicating that they are filled with sediment. Parts of the crater walls seem to have 'melted' and sunk into the centre of the crater depression, and numerous wide gullies cut through the slopes. Particularly striking are the linear structures in the northernmost crater (lower right in images 1, 3, 4). Its surface morphology resembles that of terrestrial block or debris glaciers, which are common in alpine and polar regions.

This typical flow structure was formed when a mixture of debris and ice from a glacier in the crater flowed downhill to the centre of the crater triplet at a breakthrough in the inner crater rim. The debris traces the movements of the plastic ice flow in the subsurface. This is particularly visible on the colour-coded elevation model (image 3). The dark patch in the largest crater represents a small accumulation of dark sands, which form numerous and quite impressive dune fields elsewhere on Mars.

Smooth terrain

The plain around the impact craters, which also has a smooth, flat surface, shows interesting landscape features. It is not covered by countless small and medium-sized impact craters, as one would expect for a surface of this age on Mars. Secondary craters, which are formed when ejected material hits the area around a newly formed crater, are not visible either. Only a handful of bowl-shaped, lightly eroded and therefore young craters can be found there. It appears that craters older than a certain age have been subject to 'melting' and that many of the smaller and medium-sized impact craters that were even older have disappeared as a result. Ice in the Marian subsurface seems to have played the key role in this levelling process.

Given enough time, smaller surface structures formed on an ice-rich surface may also 'melt' again due to the flow of the ice, breaking down to a certain extent and smoothing the surface again. The process, which is typical of glacial activity on Mars, is referred to as 'terrain softening'. This observation shows that there were once large quantities of water on Mars. They created glacier-like flow structures with very large ice masses, especially during the Noachian Period. Today, most of the glacier ice has long since sublimed and left the debris masses it carried with it as witnesses of its flow processes, similar to glacial moraines on Earth. However, ground ice is still abundant on Mars today. It was first detected in 2008 by NASA’s Phoenix lander in the high latitudes of the northern lowlands.

All images can be found in high resolution together with other images from HRSC in the Mars Express image gallery on flickr.

  • Image processing

    These images were acquired by the High Resolution Stereo Camera (HRSC) on 6 August 2020 during Mars Express orbit 20,982. The image resolution is approximately 15 metres per pixel. The centre of the images is located at about 19 degrees east and 37 degrees south. The perpendicular colour view was generated using data acquired by the nadir channel, the field of view which is aligned perpendicular to the surface of Mars, and the colour channels of HRSC. The oblique perspective view was computed using a Digital Terrain Model (DTM) and data acquired by the nadir and colour channels of HRSC. The anaglyph, which provides a three-dimensional view of the landscape when viewed using red-green or red-blue glasses, was derived from data acquired by the nadir channel and the stereo channels. The colour-coded topographic view is based on a DTM of the region, from which the topography of the landscape can be derived. The reference body for the HRSC DTM is a Mars equipotential surface (Areoid).

    HRSC was developed and is operated by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR). The systematic processing of the camera data was performed at the DLR Institute of Planetary Research in Berlin-Adlershof. Personnel at the Department of Planetary Sciences and Remote Sensing at Freie Universität Berlin used these data to create the image products shown here.

  • The HRSC experiment on Mars Express

    The High Resolution Stereo Camera (HRSC) was developed by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) and built in collaboration with partners in industry (EADS Astrium, Lewicki Microelectronic GmbH and Jena-Optronik GmbH). The science team, which is headed by Principal Investigator (PI) Ralf Jaumann, consists of 52 co-investigators from 34 institutions in 11 countries. The camera is operated by the DLR Institute of Planetary Research in Berlin-Adlershof.

Contact
  • Elke Heinemann
    Ger­man Aerospace Cen­ter (DLR)
    Pub­lic Af­fairs and Com­mu­ni­ca­tions
    Telephone: +49 2203 601-2867
    Fax: +49 2203 601-3249

    Contact
  • Daniela Tirsch
    Ger­man Aerospace Cen­ter (DLR)

    In­sti­tute of Plan­e­tary Re­search
    Telephone: +49 30 67055-488
    Fax: +49 30 67055-402
    Linder Höhe
    51147 Köln
    Contact
  • Ulrich Köhler
    Pub­lic re­la­tions co­or­di­na­tor
    Ger­man Aerospace Cen­ter (DLR)
    In­sti­tute of Plan­e­tary Re­search
    Telephone: +49 30 67055-215
    Fax: +49 30 67055-402
    Rutherfordstraße 2
    12489 Berlin
    Contact
  • Prof.Dr. Ralf Jaumann
    Freie Uni­ver­sität Berlin
    In­sti­tute of Ge­o­log­i­cal Sci­ences
    Plan­e­tary Sci­ences and Re­mote Sens­ing
    Telephone: +49-172-2355864
    Malteserstr. 74-100
    12249 Berlin
    Contact

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