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Hells Canyon

Canyon in the western United States

  • 6 min read
  • 4 chapters
Hells Canyon
Unknown author · Public domain

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Through Canyon, Sedimentary rock and North America

The canyon was carved by the waters of the Snake River, which flows more than one mile (1.6 km) below the canyon's west rim on the Oregon side and 7,400 feet (2,260 m) below the peaks of Idaho's Seven Devils Mountains to the east. This area includes 214,000 acres (334 sq mi; 870 km2) of wilderness; most of the area is inaccessible by road.

Geology

The geologic history of the rocks of Hells Canyon began 300 million years ago with an arc of volcanoes that emerged from the waters of the Pacific Ocean. Over millions of years, the volcanoes subsided and limestone built up on the underwater platforms. The basins between them were filled with sedimentary rock. Between 130 and 17 million years ago, the ocean plate carrying the volcanoes collided with and became part of the North American continent. A period of volcanic activity followed, and much of the area was covered with floods of basalt lava, which smoothed the topography into a high plateau.

Area rivers began carving Hells Canyon out of the plateau about 6 million years ago. Water from Lake Idaho overtopped a natural divide between it and the Salmon River around 3 million years ago, allowing the Snake River to flow through the plateau and further carve the canyon. A 2025 study concludes that the canyon is younger than previously thought, beginning only 1.6 million years ago. Significant canyon-shaping events occurred as recently as 15,000 years ago during a massive outburst flood from Lake Bonneville in Utah. The canyon rim contains dense forests, scenic overlooks and mountain peaks. At the bottom of the canyon, the area is a dry, desert environment.

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