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Griggs volcano

Stratovolcano 2317 m / 7,602 ft
United States, Alaska Peninsula, 58.35°N / -155.09°W
Current status: dormant (1 out of 5)
Griggs volcano books
Typical eruption style: unspecified
Griggs volcano eruptions: 1790 BC ± 40 years
TimeMag. / DepthDistanceLocation
Sat, 6 Jan
Sat, 6 Jan 02:05 UTCM 1.7 / 4.7 km15 km- 118km NNW of Larsen Bay, Alaska
Wed, 3 Jan
Wed, 3 Jan 23:20 UTCM 1.8 / 0.3 km3 km- 91km SE of King Salmon, Alaska
Wed, 3 Jan 18:40 UTCM 1.5 / 0.7 km3 km- 91km SE of King Salmon, Alaska
Mon, 1 Jan
Mon, 1 Jan 16:21 UTCM 2.22 km- 93km SE of King Salmon, Alaska
Thu, 28 Dec
Thu, 28 Dec 05:10 UTCM 2.3 / 146.6 km32 km- 65km ESE of King Salmon, Alaska
View all recent quakes

Background:

The summit of Mount Griggs towers above Knife Creek on the NE side of the Valley of Ten Thousand Smokes. The volcano is uniquely offset west of the NE-trending alignment of volcanoes in the Katmai area. The broad, 2317-m-high stratovolcano, formerly known as Knife Peak, consists of a late-Pleistocene volcano with glacial valleys on the north that was truncated on its SW side by an early Holocene edifice collapse. A Holocene volcano was subsequently constructed within the 1.5-km-wide scarp left by the emplacement of a large SW-flank debris avalanche. Nested cones with three concentric craters mostly fill the scarp, and thick, blocky lava flows blanket the SW flanks of the volcano below the collapse scarp. In contrast to the more silicic centers of the Katmai area along the crest of the range, lava flows from Griggs are dominantly andesitic in composition, and dacitic lava flows are uncommon. No historical eruptions have occurred from Griggs, but noisy fumarolic jets near the summit can be heard from the valley floor, 1750 m below.
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Smithsonian / GVP volcano information


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