Eruptions are not the only hazard created by volcanoes. They can create havoc millions of years after their fires have grown cold because with time, their deposits can weaken to produce landslides. This happens because volcanic deposits are commonly rich
Eruptions are not the only hazard created by volcanoes. They can create havoc millions of years after their fires have grown cold because with time, their deposits can weaken to produce landslides. This happens because volcanic deposits are commonly rich in volcanic glass, a non-crystalline form of silica. In wet climates, this glass can readily transform into soft, weak minerals (primarily clay) through chemical weathering.
Volcanoes and landslides are important for landscape evolution in Hawaii and worldwide. In Washington state, an old legend makes the connection between them.
In one version of a legend of the Klickitat people, the chief of all gods (Tyhee Saghalie) and his sons (Pahto and Wy’east) came to the land along the Columbia River and decided to stay, but the sons quarreled about which area each would get. To settle the dispute, the chief sent Pahto to the north side of the river and Wy’east to the south. He then built a great bridge across the river, the Bridge of the Gods, so that the family could continue to meet.
But the brothers renewed their quarrel, this time about a beautiful maiden, Loowit. The quarrel escalated. Massive rocks were hurled; the ground shook. Villages were buried, forests were destroyed and the great bridge collapsed into the river. As punishment, the father turned the angry sons and the maiden into volcanoes — Pahto became Mount Adams, Wy’east became Mount Hood and Loowit became Mount St. Helens.
Geology tells the same story. Northwest Native Americans really could walk across the Columbia River atop the massive Bonneville landslide, which slid across and dammed the river almost 600 years ago. When the landslide-dammed lake overtopped the blockage, the bridge “collapsed” to form a great rapids — the Cascades of the Columbia. This landslide is part of a legacy left by ancient Cascade volcanoes. Until recently, the extent of this legacy had not been fully appreciated.
A recently completed USGS study (https://pubs.er.usgs.gov/publication/sim3358) mapped and dated many landslides not previously recognized in a rainy corner of the Pacific Northwest — the Columbia River Gorge in Skamania County, Wash. These landslides, formerly hidden by dense forest, occurred at least tens of thousands of years ago, and about a dozen are still moving. Their slip planes (sliding surfaces) occur entirely within volcanic deposits laid down by eruptions that occurred about 25 million years ago in the ancestral Cascade Range — deposits from volcanoes that have long since eroded away.
Tectonic forces operating throughout the past few million years tilted the beds of volcanic deposits southward toward the downcutting Columbia River, which facilitates sliding along weak zones within the weathered, clay-rich sediment beds. The discovery of so many previously unknown landslides was made possible by the availability of three new technologies — LiDAR, GPS and InSAR, which were essential for this project.
The discovery of these landslides has implications for hazards today.
The Bonneville landslide has a volume of about 1 cubic kilometer (think of a box a half a mile wide, long, and high) and runout distance of about 6 km (3.7 mi). Another such large landslide rapidly sliding into the Columbia River today could have a catastrophic impact on downstream communities and on the transportation and energy-distribution infrastructure of the Pacific Northwest.
Hawaiian volcanoes have their own landslide stories. In fact, during the past several million years, 17 distinct landslides occurred throughout the Hawaiian Islands. These landslides were the subject of a Volcano Watch article on Jan. 23, 2014 (https://volcanoes.usgs.gov/hvo/hvo_volcano_watch.html?vwid=212).
Volcano
activity updates
This past week, Kilauea Volcano’s summit lava lake fluctuated in concert with summit inflation and deflation, with levels ranging about 17-35 m (56-115 ft) below the vent rim. On the East Rift Zone, the 61g flow remained active, with lava entering the ocean near Kamokuna and surface breakouts downslope of Pu‘u ‘O‘o. These flows do not pose an immediate threat to nearby communities.
Mauna Loa is not erupting. During the past week, small-magnitude earthquakes were recorded, mostly from beneath the volcano’s summit caldera and upper Southwest Rift Zone at depths up to 5 km (3 mi). Microearthquakes also occurred on the east flank at depths of 5-13 km (3-8 mi). GPS measurements continue to show deformation consistent with inflation of a magma reservoir beneath the summit and upper Southwest Rift Zone. No significant changes in volcanic gas emissions were measured.
Two earthquakes were reported felt on the Big Island during the past week. At 7:28 a.m. May 22, a magnitude-3.3 earthquake occurred 12.4 km (7.7 mi) north of Na‘alehu at a depth of 10.7 km (6.6 mi). At 11:15 a.m. May 18, a magnitude-3.2 earthquake occurred 10.7 km (6.6 mi) west of Kalapana at a depth of 7.2 km (4.5 mi).
Visit the HVO website (https://volcanoes.usgs.gov/hvo) for past Volcano Watch articles, Kilauea daily eruption updates, Mauna Loa weekly updates, volcano photos, recent earthquakes info, and more. Call for summary updates at 808-967-8862 (Kilauea) or 808-967-8866 (Mauna Loa). Email questions to askHVO@usgs.gov.
Volcano Watch (https://volcanoes.usgs.gov/hvo/hvo_volcano_watch.html) is a weekly article and activity update written by U.S. Geological Survey scientists. Today’s article is from the Cascades Volcano Observatory.
