Augustine Volcano during its 2005-2006 eruption. Cyrus Read, Alaska Volcano Observatory/USGS.
In Nanwalek, a village on the southern flank of the Kenai Peninsula and 50 miles east of Augustine Volcano, Maharrey found small pieces of wood and other tsunami debris in an eroded face of peat, 21 feet above high-tide level today. He also discovered more than one dozen ash layers that came from Augustine and mounts Katmai and Spurr.
Maharrey’s dating of tsunami deposits from more than 4,000 years ago extends the Augustine tsunami record by about 2,000 years. Maharrey’s academic advisor Jim Beget had found evidence of Augustine splashes into the sea from 1,400, 1,700 and 2,100 years ago.
Maharrey became interested in looking at Augustine’s history after Beget showed him the following account from the logbook of the Alaska Commercial Company. Someone wrote on Oct. 6, 1883:
“This morning at 8:15 o’clock, 4 tidal waves flowed with a westerly current, one following the other . . . the sea rising 20 feet above the usual level. At the same time the air became black . . . and it began to thunder.”
That writer indicated something happened in 1883 that didn’t in 2006: part of Augustine crumbled. Because the mountain is surrounded by wide apron, it takes a tremendous landslide to send a wave in the direction of Nanwalek, now home to 177 people.
During field expeditions to the western shore of Cook Inlet, Beget found debris from the 1883 tsunami near Mount Iliamna, Nanwalek and Homer.
The newfound tsunami date at Nanwalek shows that Augustine is a repeat offender at piling lava above the tipping point.
“Augustine didn’t just start having debris avalanches 2,100 years ago,” Maharrey said.
In 1883, the extreme tides of Cook Inlet saved the village from being swamped. Because the Augustine-induced tsunami happened at low tide, the 20-foot rise of the sea had the same effect as a random high tide. Researchers think perhaps a few kayaks were lifted away and a few shelters were destroyed, but no one was killed.
Most of the village of Nanwalek is built on a high terrace above the beach, Maharrey said, but an Augustine-generated tsunami today at high tide could inundate the airstrip and low-lying areas along the beach. As the tsunami wave progressed, it would flood coastal areas all around southern Cook Inlet to several feet above the tideline. Or, if it happened at dead low tide, another Augustine tsunami might not wet anything.
Since the late 1970s, the director of the Geophysical Institute at the University of Alaska Fairbanks has supported the writing and free distribution of this column to news media outlets. This is Ned Rozell’s 20th year as a science writer for the Geophysical Institute.