Enhanced 3D model of Mars crater edge shows ups and downs

A dramatic 3D Mars view based on terrain modeling from NASA's Mars Reconnaissance Orbiter data shows "highs and lows" of Mojave Crater.

The vertical dimension is exaggerated three-fold compared with horizontal dimensions in the synthesized images of a portion of the crater's wall. The resulting images look like the view from a low-altitude aircraft. They reflect one use of digital modeling derived from two observations by the orbiter's High Resolution Imaging Science Experiment camera.

This enhanced view shows material that has ponded and is backed up behind massive blocks of bedrock in the crater's terrace walls. Hundreds of Martian impact craters have similar ponding with pitted surfaces. Scientists believe these "pitted ponds" are created when material melted by the crater-causing impacts is captured behind the wall terraces.

Mojave Crater, one of the freshest large craters on Mars, is about 60 kilometers (37 miles) in diameter. In a sense, it is like the Rosetta Stone of Martian craters, because it is so fresh. Other craters of this size generally have already been affected by erosion, sediment and other geologic process. Fresh craters like Mohave reveal information about the impact process, including ejecta, melting and deposits.


High resolution image

Mojave's fans and channels, as seen in the image above are most intriguing. They hint that impacts such as Mojave's may have unleashed water or water-ice from the subsurface to flow across the surface and, perhaps, condense as rain or snow for a brief period of Martian time. This further suggests that early climate on Mars could have been heavily influenced by the intense bombardment about 3.9 billion years ago when impacts creating craters Mojave's size and far larger were more common.

The digital terrain model yielding this view combines data from a pair of images taken by the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter. The model provides detailed topographical information for an area covering portions of the crater's northwestern wall terraces, rim and ejecta blanket. Such digital terrain models are superior to standard stereo images viewed with blue-red glasses, which show only relative changes in elevation instead of absolute numerical data. Digital terrain models can be used for rendering perspective views from any angle or even fly-by movies. More importantly, they can be used for detailed quantitative analysis, such as profiles, slopes, morphometry, numeric modeling, etc.

Credit: NASA/JPL-Caltech/University of Arizona

 

Source: Jet Propulsion Laboratory
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