description Valley of Ten Thousand Smokes fumaroles Overview
The Valley of Ten Thousand Smokes is a volcanic landscape located within Katmai National Park and Preserve on the Alaska Peninsula. It was formed during the 1912 eruption of Novarupta, which covered the former river valley in a deep layer of ash and pumice. In the immediate aftermath, thousands of fumaroles—vents emitting steam from cooling volcanic deposits—appeared across the valley floor, giving the area its distinctive name.
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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.
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