Geologists examine a section of the Orangeburg
Scarp along the James River in Virginia.
Not exact matches
The authors use LiDAR and field data to identify linear
scarps, sags, and swales that cut across both bedrock and Quaternary deposits
along the Leech River fault.
Such a
scarp runs vertically
along the right edge of the image (bottom), which encompasses a horizontal extent of about 200 kilometers.
But one of these old beaches, the Pliocene - era Orangeburg
Scarp, warps and bends
along its course from Florida to North Carolina.
The large
scarps were formed as Mercury's interior cooled, causing the planet to contract and the crust to break and thrust upward
along faults making cliffs up to hundreds of miles long and some more than a mile (over one - and - a-half kilometers) high.