description Valley of Ten Thousand Smokes fumaroles Overview
The Valley of Ten Thousand Smokes lies within Katmai National Park and Preserve on Alaska's Alaska Peninsula. Its defining deposits were laid down during the 1912 eruption of Novarupta, which buried a former river valley beneath deep accumulations of ash and pumice. Heat retained in those volcanic materials drove the steam vents, or fumaroles, that gave the valley its name. Thousands of vents were visible in the eruption's aftermath, making the valley an extraordinary example of heat escaping from freshly deposited volcanic material.
Most of that fumarolic activity diminished as the deposits cooled, so the historic name does not describe a valley still filled with thousands of steaming openings. The site suits an interest in volcanic history and the long aftermath of eruptions. Its significance lies in the relationship between the surviving deposits and the once extensive field of steam vents.
help Valley of Ten Thousand Smokes fumaroles FAQ
How was the Valley of Ten Thousand Smokes formed?
The Valley of Ten Thousand Smokes was formed during the massive 1912 eruption of the Novarupta volcano on the Alaska Peninsula. This eruption was the largest volcanic event of the 20th century and covered the former river valley in a deep layer of ash and pumice.
Where is the Valley of Ten Thousand Smokes located?
The valley is a volcanic landscape located within Katmai National Park and Preserve in Alaska. It sits near the base of the Alaska Peninsula, offering a barren, stark landscape that looks remarkably like a moonscape.
Why is it called the Valley of Ten Thousand Smokes?
In the immediate aftermath of the 1912 Novarupta eruption, thousands of fumaroles—vents emitting steam and volcanic gas—formed in the cooling ash. When explorers first surveyed the area, they saw tens of thousands of these smoking vents, leading them to name it the Valley of Ten Thousand Smokes.
Are there still thousands of fumaroles smoking in the valley today?
No, the vast majority of the smoking fumaroles have cooled and died out since the initial eruption over a century ago. Today, the valley is mostly a quiet, gray landscape of solidified ash, though a few isolated fumaroles still exist near the Novarupta dome.
explore Explore More
Similar to Valley of Ten Thousand Smokes fumaroles
compare_arrows Compare: Valley of Ten Thousand Smoke... See all arrow_forward
Reviews & Comments
Write a Review
Be the first to review
Share your thoughts with the community and help others make better decisions.
