South Sister
South Sister
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Geology and History Summary for Three Sisters
The cluster of glaciated stratovolcanoes called the Three Sisters extends for 20 km (12 mi) along the crest of the Cascade Range in Oregon, 35 km (20 mi) west of the city of Bend and 100 km (60 mi) east of Eugene.
Pyroclastic Flow Hazards at Three Sisters
Pyroclastic flows can form in two ways: from the collapse of a tephra plume during an explosive eruption or from the collapse of the front of a steep lava flow or dome on a volcano's slope.
Debris Avalanche Hazards at Three Sisters
South, Middle, and North Sister, as well as Broken Top are high, steep-sided peaks that could produce debris avalanches.
Eruption History for South Sister
South Sister is the southernmost and tallest of the Three Sisters. Early eruptions began between 50 to 45 ka, when South Sister produced numerous rhyolite lava flows and domes. Between 37 and 30 ka, the broad cone was built of rhyolite to andesite domes and flows, and construction of the cone ended with an explosive eruption that left pyroclastic deposi
Future Eruptions Around Three Sisters
The Three Sisters region has hosted volcanic eruptions for hundreds of thousands of years, and future eruptions are a certainty.
Modern Deformation and Uplift in the Sisters Region
In 2001, scientists discovered a broad area of uplift west of South Sister that had been rising a few cm (inches) per year since the 1990s. Uplift rates have varied, with a new pulse starting in 2020–2021. Geochemistry data indicate that magmatic activity in the region predates the past few decades.
Glaciers and Related Features of Three Sisters
The high stratovolcanoes support only about one dozen small glaciers, chiefly in cirques, and numerous patches of perennial snow and ice.