|Incidence angle 75.3
NACs M193289571LE and M193289571RE
|Incidence angle 36.2
NACs M183861185LE and M183861185RE
An even wider view places the feature north west of Marius R crater in an area where the outer rays from Aristarchus, Kepler and several craters to the west overlap on the eastern edge of the Marius hills. This particularly rugged terrain is also marked by lava flows, sinuous rilles and mare ridges. About half of the Moon’s volcanic domes are in this region. Lunar domes are much smaller than shield volcanoes on Earth. The Marius hills range from 200-500m in height whereas the Mauna Loa volcano in Hawaii (the largest shield volcano on Earth) is 17,170m tall. Here is a wide field image with the featured region indicated showing its proximity to the Marius domes:
image from Global Morphologic Map
Photographed from a more oblique angle by the LRO’s Wide Angle Camera the domes are more impressive:
So what is going on in kodemunkey’s image? Rotating the image so that north is up and using the topography graph from the ACT-REACT Quick Map shows a steep drop from west to east. Lava flows appear to have created a complex knot of ridges and valleys. The pale tracks at top left are very bouldery and connect to 2 small craters suggesting that they are more recent landslides and flow from higher ground towards the lower rugged region.
Kodemunkey found his image from the latest LRO data release 11.
ACT-REACT Quick Map link
Paper: Compositional variability of the Marius Hills volcanic complex from the Moon Mineralogy Mapper (M3)
NAC Strip: M170877942RE Latitude: 9.4 Longitude: -48.3 (close to Marius V crater)
After finding the fresh white crater on the NAC strip I did a bit more exploring and found a crater with a good example of “black stuff” – see the TLP Project – Black Stuff for more information.
“Black Stuff” – same NAC strip as above.
The Marius Hills region of the Moon is full of interesting formations and contains many volcanic domes, cones and rilles, and is well worth exploring.
I looked at a wider view of the area using the ACT-REACT tool and discovered the Rima Suess rille which runs for about 200 km across this region. There is a strange elongated “craterlet” to the north-west of the rille which appears to be connected to it in some way. I can’t find much information about this craterlet and it would be interesting to know how it formed and if it is related to the Rima Suess at all.
from ACT-REACT tool. Craterlet is at Latitude: 8.65 Longitude: -48.66