12 April 2018
This overhead view of the Ismenia Patera depression clearly reveals its varied features, such as flow traces, meteorite impacts and the fissuring of the deposits inside the crater. There are various opinions regarding the formation of Ismenia Patera – this circular structure is either an impact crater or a supervolcano. This coloured view was produced using data from the nadir channel, which is oriented perpendicular to the Martian surface, and the colour channels of the High Resolution Stereo Camera (HRSC) operated by DLR.
ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO.
This perspective oblique view was computed from data acquired by the stereo channels of the High Resolution Stereo Camera (HRSC) operated by DLR. Digital terrain models are derived from this image data, which allow the computation of perspective views of the Martian landscape. In this view, the numerous gullies on the crater rim and the rugged crater floor can be seen clearly.
The Ismenia Patera depression is located in the Arabia Terra region, at the transition between the southern highlands and northern lowlands on Mars. The images described in the article are taken from the smaller rectangle inside the larger, marked image strip of the High Resolution Stereo Camera (HRSC) operated by DLR.
NASA/JPL/MOLA, FU Berlin.
Data from the nadir channel, oriented perpendicular to the Martian surface, and one of the four oblique-view stereo channels of the DLR-operated HRSC camera system on the ESA Mars Express spacecraft can be used to generate anaglyph images. These provide a realistic, three-dimensional view of the landscape, when wearing red and blue or red and green glasses. This spatial view clearly reveals the morphology of the 75-kilometre-diameter crater with its interior hills and boulders.
The nadir channel, oriented perpendicular to the Martian surface, and the stereo channels of the HRSC camera allow digital terrain models of the Martian surface to be derived with an accuracy of up to 10 metres per pixel. These colour-coded representations clearly portray the absolute altitudes above a reference level, the areoid (the equivalent of sea level on Mars; derived from the Greek word for Mars, Ares). These altitude values can be determined using the colour scale in the top right-hand corner of the image.
Images from the High Resolution Stereo Camera (HRSC) operated by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR) on board ESA's Mars Express spacecraft show the collapsed depression Ismenia Patera. There are two hypotheses regarding the formation of this geological structure – it is either an impact crater or the caldera of a Martian supervolcano.
Ismenia Patera (Latin: patera – shallow bowl) is located in the Arabia Terra region, at the transition between the Martian southern highlands and northern lowlands. Inside the 75-kilometre-wide crater, hills and several hundred-metre-high mesas are arranged in a circle around the centre (Images 1, 4 and 5). On closer inspection, small gullies running into the crater are visible in some places on the rim of Ismenia Patera, which have been formed by water or ice flowing into the crater (Image 2). The floor of the crater is covered by deposits, the surfaces of which display traces of previous ice flow. These patterns were probably produced by rock glaciers – ice flows whose surfaces transport large quantities of boulders and debris. Similar phenomena are present on Earth in the Alpine and Polar regions, where glacial ice is completely covered by debris that has slid onto the ice from the surrounding mountain slopes. This ice-debris mass moves slowly downslope, leaving behind such flow structures.
Conspicuous groups of small impact craters, for example in the centre of Ismenia Patera, were probably caused by another meteorite impact in the immediate vicinity, which ejected large boulders towards the centre of the crater, producing small craters.
There are various opinions regarding the formation of the crater. According to one hypothesis, it was formed by a meteorite impact and subsequently filled with material deposits and, at times, with ice. Eventually, the crater surface collapsed as the underground ice melted and the water evaporated, leaving behind a rugged, hilly landscape. Another hypothesis suggests that Ismenia Patera is a volcanic caldera – a volcanic crater created by the emptying of the magma chamber following a large eruption. Volcanoes that produce a large amount of material during a single eruption are called supervolcanoes. Apart from Ismenia Patera, there are two other supervolcano candidates in Arabia Terra, namely Siloe Patera and Eden Patera. On Earth, volcanic structures such as the Phlegraean Fields near Naples, the Yellowstone area and Lake Taupo in New Zealand are considered to be supervolcanoes. On Mars, however, volcanic eruptions are no longer expected.
The theory of supervolcanoes in the ancient volcanic province in Arabia Terra is still a controversial topic for Mars researchers. In favour of the volcanic crater theory is the fact that the 'paterae' are irregularly-shaped collapse features with low topographic relief – partly without ejecta deposits elevated crater rim – which would be typical of impact craters. On the other hand, such an irregular shape may also be created by superimposed and subsequently altered impact craters. Future measurement methods for examining the Martian subsoil, to provide evidence for the existence of magma chambers below the paterae, for example, could shed light on this matter. These include seismic experiments, such as those on board NASA's InSight lander scheduled for launch on 5 May 2018, as well as orbiting radar experiments.
The image data was acquired by HRSC on 1 January 2018, during Mars Express orbit 17,723. The image resolution is 17 metres per pixel. The centre of the imaged area is at approximately two degrees east and 39 degrees north. The colour overhead view (Image 1) was created using data acquired by the nadir channel, which is directed perpendicular to the Martian surface, and the colour channels. The oblique perspective view (Image 2) was computed from data acquired by the stereo channels of HRSC. The anaglyph (Figure 4), which creates a three-dimensional impression of the landscape when viewed through red-blue or red-green glasses, was derived from data supplied by the nadir channel and one stereo channel. The colour-coded topographic view (Image 5) is based on a digital terrain model (DTM) of the region, from which the topography of the landscape can be derived. The reference body for the HRSC DTM is an equipotential surface for Mars (areoid). Staff at the Department of Planetary Science and Remote Sensing at the Free University of Berlin produced the image products shown here. The systematic processing of the data takes place at the DLR Institute of Planetary Research in Berlin-Adlershof.
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 51 co-investigators from 35 institutions and 11 countries. The camera is operated by the DLR Institute of Planetary Research in Berlin-Adlershof.
Last modified:12/04/2018 11:19:10