Saturday, August 27, 2011

LROC: Atlas

The interior of a crater-floor fracture within landmark nearside crater Atlas. LROC Narrow Angle Camera (NAC) observation M157303976L, LRO orbit 8316, April 13, 2011; incidence angle 47°, resolution 0.5 meters per pixel. View the full size LROC Featured Image HERE [NASA/GSFC/Arizona State University].

Sarah Braden
LROC News System

Floor-fractured Atlas crater (46.7°N, 44.4°E) is 87 km in diameter. The cause of the fractures that cut the crater's floor is not well understood. It is thought that the fractures have wide, flat floors, like a trough (or graben) and that they record a period of uplift of the crater floor. The question is, what caused the uplift? Floor-fractured craters have been a known lunar feature since the days of the Lunar Orbiters, but with LROC images, geologists are working to better understand how they formed. LROC NAC frames allow for a look at the interiors of the fractures, and with stereo images we can measure their shapes.

A roughly 2 by 4 kilometer section of LROC NAC frame M157303976L, from which the field of view (red box) within the LROC Featured Image released August 26, 2011 can be found [NASA/GSFC/Arizona State University].

And, in turn, the field of view within the image above is seen in this small section of a much larger LROC Wide Angle Camera (WAC) 643 nm band mosaic gathered during LRO orbits 2750 through 2757, January 31, 2010. The field of view is roughly 50 x 100 kilometers [NASA/GSFC/Arizona State University].

After the impact that created Atlas, the floor of the crater was molten. As it cooled, the solid floor formed. In the case of Atlas, eventually uplift caused the floor to break and pull apart, forming the graben, or fractures. There are two theories for the cause of the uplift. One possibility is the slow readjustment of the crust after the crater-forming impact. During an impact, the energy released compresses the crust. However, over time the crust can rebound to its original, pre-impact position. This rebound would supply the uplift that forms the fractures on the floor of Atlas crater. A second possibility is that the fractures may be due to an intrusion of magma into the crust below the crater, which uplifted and disrupted the crater floor as it rose. When investigating floor-fractured craters, geologists often look for signs of volcanic activity related to an intrusion of magma. Unraveling the origin of lunar features like this one is a primary focus of LROC science.

One hundred meter per pixel WAC context view of Atlas, showing the field of view of the entire LROC NAC frame M157303976L View the full size LROC WAC context image HERE[NASA/GSFC/Arizona State University].

Explore the entire NAC frame!

Related Images:
Mapping the Moon with Wide Angle Camera
The fractured floor of Compton
Gassendi's Fractures
Alphonsus crater mantled floor fracture

From an Earth-bound perspective Atlas (upper right) is the constant companion of it's neighbor to its west, 71 km-wide Hercules, seen in this oblique view captured when the Moon was Full, January 10, 2009, by Mario Weigand [LPOD/].

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