HR: 1340h
AN: V23A-0618 [Abstracts]
TI: Life on the Edge: Holocene Tephra Stratigraphy of Tanginak Anchorage, Sitkalidak Island, Kodiak
Archipelago, Alaska
AU: * Mahrt, E
EM: bmahrt@u.washington.edu
AF: University of Washington Department of Earth and Space Sciences, PO Box 351310, Seattle, WA 98195
United States
AU: Bourgeois, J
EM: jbourgeo@u.washington.edu
AF: University of Washington Department of Earth and Space Sciences, PO Box 351310, Seattle, WA 98195
United States
AU: Fitzhugh, J B
EM: fitzhugh@u.washington.edu
AF: University of Washington Department of Anthropology, Box 353100, Seattle, WA 98195
United States
AB:
Geologic hazards associated with volcanism in the North Pacific have profound if usually temporary effects on the environment
and human populations. Ash falls associated with these events are often preserved across large areas providing time specific
markers. In the past century, volcanic activity and its effects in the North Pacific have been recorded, but much of the
Holocene volcanic record in the Alaskan region is still being investigated. The Kodiak Archipelago, while not volcanic
itself, is located near both Aleutian and Alaskan peninsula volcanoes. However, little has been published about the Holocene
tephrochronology of the Kodiak region.
This study focuses on the area around Tanginak Spring Site (KOD481). Located on Sitkalidak Island it is the earliest
known human occupation in the Kodiak archipelago. We are documenting Holocene environmental changes on Sitkalidak Island and
relating these changes to the archaeological record. As part of this work, we will establish a local tephrochronology using
stratigraphy and geochemistry which will allow us to better correlate sedimentary changes across large areas as well as study
human interaction with ashfall events. Herein we report a preliminary tephrochronology in peat excavations on Sitkalidak
Island dating back to the earliest Holocene. Dates are radiocarbon years BP on peat directly below tephra. Marker tephra
present in our reference sections are Katmai 1912, light gray (historic?), medium gray (3370), medium gray (3720), beige 1
(4340), apricot (5390), beige 3 (6790), black (9280), and white (11,520). Geochemical and petrographic analysis will help to
determine with which volcanic events these tephra are associated. Establishing a local tephrochronology is important not
only for local correlation but also to ascertain the tephra stratigraphy of the Kodiak Archipelago and beyond. The frequency
of tephra in Tanginak Anchorage sections suggests that tephra will be a very useful stratigraphic tool in this region.
DE: 8404 Ash deposits
SC: Volcanology, Geochemistry, Petrology [V]
MN: 2004 AGU Fall Meeting