Mount Gordon is a

cinder cone A cinder cone (or scoria cone) is a steep conical hill of loose pyroclastic fragments, such as volcanic clinkers, volcanic ash, or scoria that has been built around a volcanic vent. The pyroclastic fragments are formed by explosive eruptions o ...

in the Wrangell Mountains of eastern Alaska, United States, located between Nabesna Glacier and the

stratovolcano A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and per ...

Mount Drum. It is the most prominent of a group of Pleistocene and Holocene cinder cones, most of which are less than high. The exact age of Mount Gordon remains unknown.

References

Mountains of Alaska Landforms of Copper River Census Area, Alaska Volcanoes of Alaska Cinder cones of the United States Mountains of Unorganized Borough, Alaska Volcanoes of Unorganized Borough, Alaska Pleistocene volcanoes {{CopperRiverAK-geo-stub