This 60 million year old meteor crater is a perfect model of an impact
basin, something any lunar observer familiar with basins like
Orientale or Nectaris should recognize.
It has a central peak, terracing in the walls, and concentric rings
around it.
The inner crater (the smooth red wall across the chasm) is about
two miles away. The outer shock rings are much bigger.
More photos from Upheaval:
For years it was believed to be a collapsed salt dome (hence the name), but later research, starting with Eugene Shoemaker, shows that nearly all the evidence points to an impact origin, which will be no surprise to the lunar observer since it looks remarkably like a terrestrial version of the Orientale Basin, which we see in profile on the southwestern limb of the moon, or like the Nectaris basin which is more subtle than Orientale, but has the advantage of being visible face-on from earth.
Compare this face-on satellite shot of Orientale side by side with this aerial photo of Upheaval Dome. See the similarity?
We attempted to hike the trail that winds downhill just inside the
first shock ring to the bottom, where a spur trail heads inside
the crater. Unfortunately, we
ran out of water by the time we got 2/3 of the way to the bottom.
The trail continues down toward this canyon (carved by a tributary
of the Green River) then bends around the bottom part of the outer
shock ring -- the big red rocks looming just right of center --
and the trail to the center would be just on the other side of those
rocks.
Looking up from different vantage points at various parts of
the outside of part of Upheaval Dome's first shock ring.
Left, another view of the outer shock ring, and the way the terrain
beyond it drops off into the canyon; right, concentric shock rings.
Other links on Upheaval Dome, including some great aerial shots showing the double-ringed basin structure: