Akutan Broad Bight Valley Lahars

Start: 1611 yBP [1]

Event Type: Not an eruption

Event Characteristics:
  • Lahar, debris-flow, or mudflow [1]

Description: From Waythomas (1999): "Broad Bight valley is a wide glacial valley on the south side of Akutan Island, southeast of the caldera (Fig. 1 [in original text])."
"Lahar deposits in the middle part of Broad Bight valley (sections 58, 70, 71, Fig. 12 [in original text]) form a downstream thinning fan that covers the valley floor to a depth of at least 2 m. These lahar-runout deposits are distinctly finer grained (largest clasts are pebble size) and contain a greater percentage of fines (silt+clay) than their upstream counterparts. At section 87 (Fig. 12 [in original text]) lahar runout deposits overlie the Akutan tephra. Indicating that most, if not all, of the lahar deposits in Broad Bight valley are younger than the tephra."

References Cited

[1] Stratigraphic framework of Holocene volcaniclastic deposits, Akutan Volcano, east-central Aleutian Islands, Alaska, 1999

Waythomas, C. F., 1999, Stratigraphic framework of Holocene volcaniclastic deposits, Akutan Volcano, east-central Aleutian Islands, Alaska: Bulletin of Volcanology, v. 61, n. 3, p. 141-161.

Complete Eruption References

Stratigraphic framework of Holocene volcaniclastic deposits, Akutan Volcano, east-central Aleutian Islands, Alaska, 1999

Waythomas, C. F., 1999, Stratigraphic framework of Holocene volcaniclastic deposits, Akutan Volcano, east-central Aleutian Islands, Alaska: Bulletin of Volcanology, v. 61, n. 3, p. 141-161.
Hard Copy held by AVO at FBKS - CEC file cabinet
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