• Large male brown bear at Brooks Falls

    Katmai

    National Park & Preserve Alaska

Geology of Katmai

Eroded bluff on the edge of the Valley of Ten Thousand Smokes
Ash in the Valley of Ten Thousand Smokes is now eroding into intricately carved badlands in many places.
NPS
 
Most people who visit Katmai fly to their destination. Above the land and water, people see a land pock marked with ponds and lakes, cut with deep valleys, and rippled with glacial moraines—all of which is set next to the rugged spine of active volcanoes. Katmai National Monument was established in 1918 because of its geology. The stories of the rocks, volcanoes, fossils, and glaciers of Katmai reveal the formation of this landscape.
 
Fossils: Katmai contains many fossil bearing rocks.
 
Geologic Formations: What rock is underneath your feet? How old is it? Find out here.
 
Glaciers and Glacial Features: Glaciers have been and continue to be Katmai’s sculptor.
 
Valley of Ten Thousand Smokes: Unique on the face of the earth, this 40 square-mile area so enthralled early explorers that they lobbied for the creation of Katmai National Monument.
 
Volcanoes: Over one dozen active, and many more dormant, volcanoes lie within Katmai’s boundaries.

Did You Know?

Did You Know?

Mt. Martin is just one of the many active volcanoes in Katmai National Park. Mt. Mageik, Trident Volcano, Mt. Griggs, Novarupta, and Mt. Katmai are four other active volcanoes in surrounding the Valley of Ten Thousand Smokes.