To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Frosty Peak Volcano

From Wikipedia, the free encyclopedia

Frosty Peak Volcano
Frosty Peak Volcano, a stratovolcano at the southwest end of the Alaska Peninsula
Highest point
Elevation6,299 ft (1,920 m)
Prominence6,772 ft (2,064 m)
ListingMountain peaks of Alaska
Coordinates55°04′02″N 162°50′07″W / 55.0673°N 162.8354°W / 55.0673; -162.8354
Geography
LocationAlaska Peninsula, Alaska, U.S.
Parent rangeAleutian Range
Topo mapUSGS McCarthy B-2
Geology
Mountain typeStratovolcano
Volcanic arcAleutian Arc
Last eruptionUnknown - Pleistocene or later

Frosty Peak Volcano, also known as Mt. Frosty, Frosty Volcano, or Cold Bay Volcano, is a 6,299 ft (1,920 m) stratovolcano at the southwest end of the Alaska Peninsula in the U.S. state of Alaska.[1][2]

Map showing volcanoes of Alaska. The mark is set at the location of Cold Bay Volcano.

History

Frosty Peak is the tallest and most recently formed peak of the volcanic complex.[3] Its exact age is unknown, but it was probably formed in the middle to late Pleistocene, and possibly erupted even more recently. Frosty Peak is the southern cone of the double-coned Frosty Volcano, which formed in the middle Pleistocene some time before the Wisconsin Glaciation.[4]

Frosty Volcano itself is located on the northern flank of an even older volcano, the Morzhovoi Volcano.[5] Morzhovoi Volcano was probably formed in the early to middle Pleistocene, and collapsed into a caldera. The highest points that remain from the caldera are called North and South Walrus Peak.[6]

Frosty Peak

See also

References

  1. ^ "Frosty - Introduction". www.avo.alaska.edu. Retrieved 2018-06-10.
  2. ^ "Frosty Peak | Volcano World | Oregon State University". volcano.oregonstate.edu. Retrieved 2018-06-10.
  3. ^ "Frosty". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-27.
  4. ^ Waldron, Harold (1961). "USGS Bulletin 1028-T - Geologic Reconnaissance of Frosty Peak Volcano and Vicinity, Alaska" (PDF).
  5. ^ "Morzhovoi - Introduction". www.avo.alaska.edu. Retrieved 2018-06-10.
  6. ^ Geological Survey Bulletin. U.S. Department of the Interior, Geological Survey; Washington, D.C. 1961.

External links

This page was last edited on 13 May 2024, at 16:05
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.