ESAESA ScienceMars Express
   
Europe goes to Mars
About Mars Express
About Mars
Meet the team
Multimedia
VideoTalkMars Express imagesMars Express videosHRSC videosAnimation in 11 languagesDownload wallpapersDownload screensavers3D Flash 'model'Make a model
Services
Comments Bookmark and Share
 
 
 
 
News
 
printer friendly page
The Biblis Patera volcano
 
Colour nadir view of Biblis Patera
 
7 September 2005
These images, taken by the High Resolution Stereo Camera (HRSC) on board ESA’s Mars Express spacecraft, show the Biblis Patera volcano, located in the western part of the Tharsis rise on Mars.
 
 
Biblis Patera in context
The HRSC obtained these images during orbit 1034 with a ground resolution of approximately 10.8 metres per pixel. The scenes show the region of Biblis Patera, at approximately 2.0° North and 236.0° East.

Located between Olympus Mons and Tharsis Montes, the volcano Biblis Patera is 170 kilometres long, 100 kilometres wide and rises nearly three kilometres above its surroundings.
 
 
Black and white nadir view of Biblis Patera
The bowl-shaped depression (the ‘caldera’) may have been formed as the result of collapse of the magma chamber during eruptions of the volcano. The caldera has a diameter of 53 kilometres and extends to a maximum depth of roughly 4.5 kilometres.

The morphology of the caldera suggests that multiple collapse events have occurred.The radial depressions and faint concentric circles on the flanks of the volcano are most likely faults associated with the formation of Biblis Patera.
 
 
In the south-west (top left), the linear features extending north-west to south-east appear to be faults. Surrounding Biblis Patera there are more faults with a similar orientation and which may be related to the formation of the Tharsis Rise.

Biblis Patera is older than the surrounding plains, which consist of lava flows originating from Pavonis Mons (the middle one of the Tharsis Montes volcanoes). In the main colour image, clouds obscure the surface to the north-east of the caldera (bottom right), making it appear grey and less reddish-orange in colour.
 
 
3D anaglyph view of Biblis Patera
The stereo and colour capability and the high-resolution coverage of extended areas with the HRSC allow the improved study of the complex geological evolution of the Red Planet.

By supplying new image data for volcanoes like Biblis Patera, the HRSC provides scientists with the opportunity to better understand the morphology and volcanic history of Mars.

Data from the HRSC, coupled with information from other instruments on Mars Express and other missions, improves our understanding of this fascinating planet.
 
 
The colour images were processed using the HRSC nadir (vertical view) and three colour channels. The perspective view was calculated from the digital terrain model derived from the stereo channels.
 
 

Perspective view of Biblis Patera - looking west
 
The 3D anaglyph image was created from the nadir channel and one of the stereo channels. Stereoscopic glasses are needed to view the 3D image. Image resolution has been decreased for use on the internet.
 
 
For more information on Mars Express HRSC images, you might like to read our updated 'Frequently Asked Questions'.
 
 
 


Mars Express image browser
Recent images
Sulphate deposits in Juventae Chasma‘Butterfly’ impact crater in Hesperia PlanumFly over the Chasma Boreale at Martian north poleWater ice in crater at Martian north poleNicholson Crater on MarsCoprates Chasma and Coprates CatenaAncient floods on Mars: Iani Chaos and Ares VallisCrater Holden and Uzboi VallisTithonium Chasma up closeThe mesas of Aureum ChaosThe Medusa Fossae formation on Mars‘Hourglass’ shaped craters filled with traces of glacier
More information
High Resolution Stereo CameraBehind the lens...
 
 
 
   Copyright 2000 - 2010 © European Space Agency. All rights reserved.