12 December 2013
Plan view of the Juventae Chasma basin
This view into the Juventae Chasma basin allows the different landscape forms found in this terrain to be seen. To the south (left), a relatively smooth, even surface, bearing sand and dust deposits is visible. Traces of large-scale tectonic movement, rock falls and the remnants of what were once highland plains, now relentlessly eroded, can be seen in the Maja Valles valley system (right) that stretches north from Juventae Chasma, with the intact highland areas located on the upper edge of the image. The two mountains, in places 3300 metres high, standing in the centre of the image and showing strong signs of wind erosion, are the most impressive features.
ESA/DLR/FU Berlin (G. Neukum).
Oblique view of 'Mound C' in Juventae Chasma
The stereo image data delivered by the DLR-operated HRSC camera system on board Mars Express enables to present the landscape from different perspectives. This image shows what scientists have named 'Mound C', a mountain in Juventae Chasma with a width of 53 kilometres and a height of 3300 metres, and whose dimensions naturally have more in common with an alpine mountain range than a heap of soil. Lighter layers are seen here on the eastern flank, close to the base, consisting of gypsum and similar sulphate minerals. Relatively soft material, stretching for several kilometres in line with the prevalent winds, has been eroded to form sharp ridges that look almost like a sand blaster has been at work.
The Juventae Chasma basin in the equatorial highlands of Mars
Covering an area of 150 by 250 kilometres, Juventae Chasma forms a huge basin on the Martian highlands between the plains of Lunae Planum in the northwest and Ophir Planum in the southeast. The depression, in places 5800 metres deep, opens out into the outflow channels of Maja Valles to the north. The two massifs, imaged during orbit 12,508 on 4 November 2013 by the HRSC stereo camera that DLR operates on board the Mars Express, are clearly visible in the topographical map.
NASA/JPL/MOLA; FU Berlin.
Anaglyph image of Juventae Chasma
The nadir channel of the DLR-operated HRSC camera system, the field of view of which is aligned perpendicular to the surface of Mars, and one of the four stereo channels can be used to produce anaglyph images. Viewed through red-blue (cyan) spectacles, they deliver a realistic, three-dimensional impression of the landscape, in which the two striking massifs in the basin of Juventae Chasma, found in the centre of the image, are particularly prominent. The impressive, precipitous cliff edge on the western reaches of the basin (parallel to the upper edge of the image) is equally imposing when seen in '3D'.
Topographical map of Juventae Chasma
The stereo image data acquired by the HRSC camera system, operated by DLR on board Mars Express, can be used to create digital terrain models. The large-scale formations of the Juventae Chasma basin, which is 5800 metres deep in places, are truly impressive in this colour-coded topographical image. From the high plains of Lunae Planum (upper edge of the image) the plateau abruptly plunges more than 4000 metres to the basin below. Two eye-catching massifs, shaped into their current form by the erosive force of the wind, stand in the centre of the depression; they consist largely of soft sulphate rock. A chaotically disordered landscape, marked by deep erosion, lies adjacent to the north in the outflow channel of Maja Valles.
The water that once flowed across Mars in its early days has left many traces. Among these, two terraced mountains located in the Juventae Chasma basin stand out; they appear to be composed of sediment layers. Spacecraft overflights have revealed that these are sulphate deposits containing minerals such as gypsum, alabaster or kieserite, which usually require water to form. One of the many passes of Mars Express, the European Space Agency (ESA) orbiter, was over Juventae Chasma just a few weeks ago. The spacecraft's High Resolution Stereo Camera (HRSC), operated by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR), acquired the images shown here on 4 November 2013.
The images have a resolution of approximately 16 metres per pixel, permitting detailed analysis of the structures found in the sulphate mountains. Juventae Chasma lies a few hundred kilometres to the northeast of the central part of Valles Marineris, the vast valley system that cuts up to 11 kilometres deep into the highlands and stretches for almost 4000 kilometres along the Martian equator.
The scale of Juventae Chasma is no less impressive; stretching 150 kilometres from east to west and 250 kilometres from north to south, the structure is approximately as large as the German state of Baden-Württemberg. To the north, Juventae Chasma passes into the Maja Valles, a system of large outflow channels that spreads 1600 kilometres across the highlands before opening into the lowlands of Chryse Planitia. This also is a clear indication that water must have been present here.
View of an almost 6000-metre-deep basin with gypsum mountains
Like the Grand Canyon in the United States, with its carved paths in the plains of the Colorado plateau, the highlands around Juventae Chasma suddenly plummet into the vast expanse of the deep valley. An astronaut standing on this precipitous ledge would be looking down 5800 metres to the valley floor. Numerous traces of landslides and rock falls can be seen along the flanks. The ground to the south of this depression (to the left in the plan view) reveals a fairly nondescript topography, remaining flat over larger expanses and covered by sandy deposits. In contrast, though, the northern reaches (to the right in the images) are distinctly haphazard, displaying huge massifs formed by landslides that rolled down from the upper edge of the high plateau and are now isolated fragments, exposed to the weather.
The light layers of the two largest, isolated massifs in Juventae Chasma make them easy to spot in the Mars Express images. These two mountains were initially named 'Mound B' and 'Mound C' by US researchers, where 'Mound C' is the larger of the two – although geologists usually use the term 'mound' to describe no more than a heap of soil. But Mound C is almost 53 kilometres long, 20 kilometres wide and, at its highest elevation, rises 3300 metres above its surroundings – so its actual dimensions are more equivalent to a mountain chain such as the Zillertal Alps in the Tyrol. The summit ridges of both 'mounds' bear clear traces of wind erosion – kilometre upon kilometre of elongated, streamlined 'yardangs', produced by the wind blasting sand and dust against the flanks. It would seem, therefore, that the rock is soft and not particularly resistant to erosion.
Volcanoes, lakes, river deltas, springs – or did the sulphate 'fall from the sky'?
The most striking and geologically interesting feature of Mound B and Mound C is the horizontal stratification arranged like terraces along the mountainsides. The layered sulphate minerals were identified using the OMEGA spectrometer on board Mars Express and also CRISM on NASA's Mars Reconnaissance Orbiter, which both measure the radiation reflected from the surface in visible and near infrared light. Mineralogists use the term 'polyhydrated sulphates', meaning that two or more water molecules are incorporated into the crystalline lattice of these sulphuric acid salts, themselves readily soluble in water. This is also true of gypsum, the best-known calcium sulphate and the mineral of this type most commonly found on Earth.
As yet, there is no clear understanding of the processes that led to the emergence of these sulphate layers on Mars, and hypotheses remain controversial. One theory suggests that the formation of sulphates may have a connection with volcanic eruptions in ice-covered mountains – exposed to the heat released during the eruption, the ice melts, freeing the water to form sulphate minerals. Another idea suggests sedimentation in stagnant water supersaturated with calcium sulphate. Discussions also address the precipitation of sulphates at the end of water courses, in the deltas where the suspended materials carried in the currents form deposits and the dissolved substances form salts as the water evaporates. Another theory suggests that the sulphates formed directly at the sources of the surface water.
Another, somewhat exotic, possibility is that the sulphate layers may, in a sense, have 'fallen from the sky'. For this to happen, extremely fine granules of dust and ash must have descended from the atmosphere and landed on the surface of Mars, coming into contact with ice. Alternatively, tiny ice crystals may have bonded with dust to form this kind of precipitation. A similar phenomenon is observed on both Martian poles, where layers not unlike those found in Juventae Chasma are deposited as the seasons shift. However, the layered mounds of these sulphate mountains are substantially older than the geologically speaking very young strata found at the North and South Poles, dating back around three billion years.
Image processing and the HRSC experiment on Mars Express
These images were created using data acquired on 4 November 2013 during Mars Express orbit 12,508 using the High Resolution Stereo Camera (HRSC). The image resolution is approximately 16 metres per pixel. The images show a section of the planet located at about four degrees south and 298 degrees east.
The colour plan view (image 1) was created using data from the nadir channel, the field of view of which is aligned perpendicular to the surface of Mars, and the colour channels of the HRSC. The oblique perspective view (image 2) was generated using data from the HRSC stereo channels. The anaglyph (image 4), 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 one stereo channel. The colour-coded topographic view (image 5) is based on a digital terrain model of the region, from which the topography of the landscape can be derived.
The High Resolution Stereo Camera was developed at 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 over 40 co-investigators from 33 institutions and ten countries. The camera is operated by the DLR Institute of Planetary Research in Berlin-Adlershof. The images shown here were generated by the Institute of Geological Sciences at FU Berlin in conjunction with the DLR Institute of Planetary Research in Berlin.
Last modified:03/02/2014 11:53:49