description Pilot Pinnacle Overview
Pilot Pinnacle is a prominent volcanic fumarole formation in Alaska's Valley of Ten Thousand Smokes that solidified from magma venting during the 1912 Novarupta eruption.
help Pilot Pinnacle FAQ
What is Pilot Pinnacle?
Pilot Pinnacle is a prominent volcanic fumarole formation in Alaska’s Valley of Ten Thousand Smokes. It solidified from material associated with magma venting.
Which eruption formed Pilot Pinnacle?
The formation is linked to the 1912 Novarupta eruption. Novarupta produced the Valley of Ten Thousand Smokes, one of Alaska’s major volcanic landscapes.
What is a fumarole?
A fumarole is a volcanic opening or formation associated with steam and gas released from hot ground. Pilot Pinnacle is a solidified example created by volcanic venting rather than a conventional mountain peak.
Where can Pilot Pinnacle be found?
It is in Alaska’s Valley of Ten Thousand Smokes, within the volcanic landscape shaped by the 1912 eruption. The site is part of the region associated with Katmai’s dramatic eruption history.
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