Geologic formation
The geologic formations of New River Gorge & Preserve highlight millions of years of Earth's history, showcasing the power of erosion and the unique characteristics of the region.
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Geologic formation Details
The geologic formations of the park highlight millions of years of Earth's history, showcasing the power of erosion and the unique characteristics of the region. The New River Gorge, a steep V-shaped canyon in West Virginia, exposes rock layers that reveal ancient geological processes. The gorge cuts through the Appalachian Plateau, exposing rock formations that are up to 320 million years old. The most prominent formations include sandstone and shale, which are especially visible along the canyon walls and cliffs. Nuttall Sandstone, found in the lower gorge, is a defining feature of the area. This erosion-resistant rock, composed of 98% quartz, has played a significant role in shaping the steepness of the gorge. The durability of Nuttall Sandstone has made the cliffs particularly enticing to rock climbers. Around Batoff Mountain, some of the oldest and most pristine examples of this sandstone can be observed. The New River itself is an ancient waterway with origins tied to the prehistoric Teays River, which once flowed into an inland sea that covered central North America. As the Appalachian Mountains rose, the New River maintained its ancient course, cutting through ridges rather than flowing around them. This unique geological history allowed the river to carve into coal-rich rock layers, exposing seams of high-quality coal that spurred industrial development in the region.
Difficulty
Open
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Estimated time
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Region
Conservation & Climate
Nearby Parks Around Geologic formation
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