Frosty Volcano
Encyclopedia
Frosty or Mt. Frosty is a stratovolcano
Stratovolcano
A stratovolcano, also known as a composite volcano, is a tall, conical volcano built up by many layers of hardened lava, tephra, pumice, and volcanic ash. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions...

 and the westernmost Holocene
Holocene
The Holocene is a geological epoch which began at the end of the Pleistocene and continues to the present. The Holocene is part of the Quaternary period. Its name comes from the Greek words and , meaning "entirely recent"...

 volcano of the Alaska Peninsula
Alaska Peninsula
The Alaska Peninsula is a peninsula extending about to the southwest from the mainland of Alaska and ending in the Aleutian Islands. The peninsula separates the Pacific Ocean from Bristol Bay, an arm of the Bering Sea....

 in Alaska, USA. Frosty is the youngest of the two large volcanic structures of the Cold Bay
Cold Bay Volcano
Cold Bay Volcano is a 6,299 ft stratovolcano at the southwest end of the Alaska Peninsula in the U.S. state of Alaska.-Sources:* *...

 volcanic complex. It has a summit elevation of 6601 feet (2,012 m). Frosty's last known eruption is unknown. The oldest products of the roughly 100 cu km Cold Bay complex, which lies southwest of the village of Cold Bay
Cold Bay, Alaska
Cold Bay is a city in Aleutians East Borough, Alaska, United States.Cold Bay is one of the main commercial centers of the Alaska Peninsula, and is home to Cold Bay Airport.-History:...

, form the glacially dissected late-Pliocene to early Pleistocene Morzhovoi Volcanics at the southern end of the complex.

Frosty Peak

North of Frosty Volcano is Frosty Peak, a symmetrical late-Pleistocene
Pleistocene
The Pleistocene is the epoch from 2,588,000 to 11,700 years BP that spans the world's recent period of repeated glaciations. The name pleistocene is derived from the Greek and ....

 to Recent stratovolcano constructed within the southernmost of two coalescing craters. The western wall of the ice-filled northern crater is breached by a large valley glacier
Glacier
A glacier is a large persistent body of ice that forms where the accumulation of snow exceeds its ablation over many years, often centuries. At least 0.1 km² in area and 50 m thick, but often much larger, a glacier slowly deforms and flows due to stresses induced by its weight...

. The symmetrical summit cone rises at 600 m (1,969 ft) above the floor of the southern crater.
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