|
The Pinnacles - Prominent Geological Features of Crater Lake National Park
|
These towering needle-like formations of
rock, called fossil fumaroles, projecting from the Sand Creek Canyon floor,
were formed under sheets of volcanic pumice that preceded Mazama's collapse.
As the surface of the hot pumice cooled over the years, steam and gases were
released by the hot rocks underneath through vents and tubes that were
welded into cement hardness by their passage. These ancient vents now stand
alone due to the erosion of the surrounding softer materials.
|

Plate 16. The Pinnacles, Sand Creek canyon,
showing pale pumice flow beneath smoke-gray scoria flow, above which lie 10 feet of fine ash. (Photograph by George Grant, National Park Service.) The Geology of Crater Lake
National Park, Oregon (1942) by Howell Williams |
|
Note: the numbers associated with each feature
name above correspond to their place on the Custom Google Map below
|
Related Materials
-
The Climax: Culminating Explosions of
Pumice and Scoria: The Sand Creek Flows, The Geology of Crater Lake National Park, Oregon (1942) by Howell Williams -
The Pinnacles, Nature Notes From Crater Lake, Vol.
4 No. 3, 1931, D. S. Libbey -
The Canyons of Crater Lake
National Park, Nature Notes From Crater Lake, Vol. 8 No. 2, 1935, Warren D. Smith
|
Crater Lake National Park
Prominent Geological Features Map
View Larger Map
|
|