Eos Chasma, Part of Valles Marineris 30 August 2004

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Eos Chasma, part of Valles Marineris 30 August 2004 The northern part of Eos Chasma’s valley floor is a rough area with angular hills reaching almost 1000 metres. In contrast, the southern part reveals a These images, taken by the High Resolution smooth topography with distinct flow structures. Stereo Camera (HRSC) on board ESA's Mars Express spacecraft, show the southern part of In some areas of the southern slope, at least two Valles Marineris, called Eos Chasma. terrace levels can be observed. Some haze in the valley hints at the presence of aerosols (airborne The images were taken during orbit 533 in June microscopic dust or liquid droplets). 2004, and are centred at Mars longitude 322° East and latitude 11° South. The image resolution is The colour image was created from the HRSC’s approximately 80 metres per pixel. nadir (vertical view) and three colour channels. The 3D anaglyph image was created using the nadir Between surrounding plains and the smooth valley and one of the stereo channels. floor, a height difference of about 5000 metres has been measured. The perspective views, with height exaggerated by The plain to the south, above Eos Chasma, is a factor of four, were calculated from the digital covered by several impact craters with diameters terrain model derived from the stereo channels. of around 20 kilometres and drainage channels. Image resolution was reduced for use on the internet. To the east on this plain, isolated regions with cracked surfaces become more prominent. The Source: ESA direction of flow of the drainage channels in this area of the plain is ambiguous, as the channels to the north-east drain towards the south-east, and those in the south-west normally flow to the north- west. 1 / 2 APA citation: Eos Chasma, part of Valles Marineris (2004, August 30) retrieved 29 September 2021 from https://phys.org/news/2004-08-eos-chasma-valles-marineris.html This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only. 2 / 2 Powered by TCPDF (www.tcpdf.org).

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