In this video we see how friction at the base of moving thrust sheets can influence the way an orogenic wedge develops. Combined with erosion we create a landscape of … Continue reading A Window into the World of Klippen
Philip S. Prince, Virginia Division of Geology and Mineral Resources The explanation for Cove Mountain’s shape lies in the fold structures within the fault-bounded Cove Mountain block. The ages of … Continue reading Cove Mountain looks like a “2”…Part 2!
An iconic southwest Virginia hiking destination only gets more interesting if you zoom out a bit… by Philip S. Prince, Virginia Division of Geology and Mineral Resources The Appalachian Trail … Continue reading Cove Mountain looks like a “2,” even to a structural geologist…but why?
Model: Phil Prince
Words: Lisa Whalen
Most of the time in this blog we discuss collision which makes us thing about compressional forces. This time we’re going the opposite direction and investigating what we can replicate with sandbox models in terms of extension, or when the continents are under tensional forces. This gets me thinking about pull-apart bread as geologists love food analogies.
In this video Phil shows the formation of normal listric faults occur as two continents pull away from each other much like what is occurring in the Basin and Range in the Western United States (or in the bread above).
Normal faults form as the hanging wall moves downward relative to the foot wall. In a listric normal fault the fault plane or where the hanging wall and foot wall touch isn’t plane so much as it’s scoop shaped.
Images: nps.gov and geologylearn.blogspot.com
Model by Phil Prince
Words by Lisa Whalen
Last time we looked at a model replicating a translational landslide. Continuing with our landslide theme, this time Phil has built a model comparing translational slides with rotational or slump landslides. These are characterized by a more curved plane of weakness that allows the slide to move. The curvature leads to the moving material becoming deformed, first through extension or tensional forces as it initially pulls away to compression as the sliding mass piles up on top of itself.
Words by Lisa Whalen
Model by Phillip Prince
Images credit: British Geological Survey
Sandbox models aren’t just for mountain building. In this video Phillip Prince replicates landslides.
A translational landslide is when rock or soil moves down-slope along a plane of weakness like a joint, fault or bedding surface. Best illustrated with chocolate and a weaker layer of caramel:
A rotational landslide on the other hand has a curved surface of weakness and moves large blocks of material that tend to rotate backwards as they move.
Here in southwest Virginia are some of the largest known landslides in the world, with one slide reaching almost 3 miles long. You can learn more about “The Mountain that Moved” on the USGS site about Sinking Creek Mountain. The landslides occurred in the Pleistocene, but weren’t discovered until the 1980’s because the enormous size of the landslides obscured their presence. Today they can be identified partly through different vegetation and the presence of springs and pare visible from many of my favorite hiking areas. They may have been caused by erosion or even by earthquakes.
As an aspiring mountaineer another way to think about translational landslides is to think of slab avalanches. In this case you have layers of snow separated by a weaker layer. Weather, more snow, or people (such as in the video below) can tip the scales of the forces that are keeping the layers of snow coherent and trigger an avalanche.
Words by L. Whalen
Model by P. Prince
Nothing stays the same very long – and tectonic environments are no exception. Structures from a later event can overprint a previous event. Sorting this all out is both fun and hard work. In this video, Phil recreates two stages of the geologic history of Triton Bay, West Papua (northwest New Guinea).
First, we see convergence forming parallel anticlines. Subsequent extension creates a characteristic rectangular pattern, that when filled in with water matches the local structure.
Words by Lisa Whalen
Video/Model: by Phil Prince
The Ouachita orogeny occurred ~300 million years ago when part of South American collided with the southern part of North America.
In this model Phil Prince takes us to the Ouachita Mountains of Arkansas and Oklahoma. Here you will see how the strength of different rock layers coupled with deep erosion can produced the characteristic shape of this range. Sinuous ridges formed from chert snake around valleys scooped out of shale abutting a broad sandstone plateau.