description Upheaval Dome Overview
The Upheaval Dome is a prominent impact crater located within Canyonlands National Park in Utah. Formed approximately 26 million years ago, it’s recognized for its distinctive circular ridge—a syncline—resulting from the force of the initial impact. Scientists continue to study this geological feature to understand meteorite impacts and their effects on Earth's crust. The site is of interest to geologists, paleontologists, and those studying planetary science.
help Upheaval Dome FAQ
How was Upheaval Dome formed?
Upheaval Dome is highly unusual because scientists have long debated its origins, with theories ranging from a meteorite impact to a collapsed salt diapir. Currently, the meteorite impact theory is the most widely accepted explanation.
Where is Upheaval Dome located?
It is located within Canyonlands National Park in Utah. Visitors can reach it by hiking the Upheaval Dome Trail, which provides stunning views of the crater's center.
How big is Upheaval Dome?
The unique geological structure features a prominent ring syncline that spans roughly 5 kilometers in diameter. The central crater itself is significantly smaller but incredibly deep.
Can you hike to the bottom of Upheaval Dome?
While most visitors hike to the two main overlooks along the crater's rim, there is a steep, strenuous trail that leads into the center. The Syncline Loop is a challenging 8.3-mile hike that circles the entire formation.
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