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August 5, 2019
Somewhere on the AGU Landslide blog, I came across a reference to another type of rock strength-controlled, intact landslide I had never heard of–the Toreva Block. Like the Appalachian Valley and Ridge giant landslides, it is possible to replicate Toreva-style movement with contrasting model materials that represent failure-prone shale and much stronger topography-supporting lithologies, like sandstone or basalt.
July 10, 2019
Geologic maps can be very visually engaging, but non-geologists may find it difficult to extract the information that a map is supposed to communicate…. Cross sections included with a map can help, but it can still be tough to pull it all together if you don’t look at this sort of material all the time.
June 20, 2019
If you Google the word “landslide”…the first search result you get is the Fleetwood Mac song. I suppose this says something about the place of Earth Science in the 2019 world, but whatever (more on this at the end of the post!). Clicking the “Images” tab improves things, assuming you are indeed seeking information about the geologic feature.
May 14, 2019
This post steps back to the Rocky Mountain Front Range models from a few weeks back in which I used a model that took a large-scale perspective on the Front Range for comparison to some published work.
April 29, 2019
The southeast slope of Sinking Creek Mountain in Craig County, Virginia hosts what is certainly one of the largest landslide complexes in eastern North America–and possibly the least noticeable. Despite extending for 15 miles (25 km) along the mountainside…this group of translational blockslides was not documented until 1986 by Art Schultz of the USGS.
March 25, 2019
A sandbox model perspective on the tilted sedimentary layers of the eastern Rocky Mountain Front Range
One of my earliest recollections as a geology student was a discussion of the upturned sedimentary rocks in The Garden of the Gods at the eastern foot of the Rocky Mountain Front Range in Colorado. I distinctly remember hearing about the vertical movement of a large block of crust, which would ultimately produce the high mountains, tilting the overlying sedimentary layers out of its way as it rose.
March 7, 2019
By Philip S. Prince, Virginia Division of Geology and Mineral Resources (Scroll down for summary video link) The Breaks rock slide, a large slide feature at the western edge of the Appalachian fold-thrust belt, was first described 30 years ago in Schultz and Southworth (1989). In an impressive display of imagery analysis and general geologic know-how, the authors successfully identified several large but topographically subtle ancient landslide features without the …
February 26, 2019
The topographic features of the Powell Valley Anticline (PVA) played a significant role in the lives of both indigenous and Euro-American peoples on the American frontier in the late 18th century… Here I focus on two subjects inextricably connected to PVA topography: The Wilderness Road and Robert Benge, also known as Chief Benge, Captain Benge, Bob Benge, or simply “The Bench.” Benge and Wilderness Road users had two very opposite goals, leading to numerous clashes and Benge’s ultimate demise in the mountains of the PVA.
February 15, 2019
…how much existing geologic maps, particularly those produced without any digital topography or remote sensing, could be enhanced by checking them against LiDAR hillshade. The answer varies, and to continue the Powell Valley Anticline discussion, I draped a 1965, hand-drafted geologic map over the new LiDAR hillshade background.
February 12, 2019
The Mississippian-aged sedimentary section in the northeastern portion of Virginia’s Powell Valley Anticline (PVA) offers up stunning hillshade imagery on the flanks of the aptly-named Cliff Mountain.