Mount Gordon
Upper Nile
Mount Gordon is a notable cinder cone situated in the Wrangell Mountains of eastern Alaska, United States. Positioned between the Nabesna Glacier and the stratovolcano Mount Drum, it stands out as the most prominent among a group of Pleistocene and Holocene cinder cones. These cones are generally less than 100 meters (330 feet) in height. Despite its prominence, the precise age of Mount Gordon remains undetermined. The mountain was named after a local prospector who explored the area in 1899, linking it to the region's history of exploration and prospecting. Its volcanic nature and location amidst glaciers and other volcanic features make it a unique natural landmark within the rugged Alaskan wilderness.
Plan your trip to Central Equatoria with AI
Create a detailed itinerary in minutes. AI suggests the best places, restaurants, and an optimized route.
Interesting facts
- •Mount Gordon is the most prominent cinder cone among a group in the Wrangell Mountains.
- •It lies between the Nabesna Glacier and Mount Drum, a stratovolcano.
- •Most of the cinder cones in this group are less than 100 meters (330 feet) high.
History
Mount Gordon was named after a local prospector active in the area in 1899.
It is part of a group of cinder cones formed during the Pleistocene and Holocene epochs.
The exact age of Mount Gordon itself is unknown, but it shares geological origins with nearby volcanic features such as Mount Drum.