Features of Newberry caldera
The present 6.5 by 8 km (4 by 5 mi) caldera at Newberry Volcano's summit formed about 75,000 years ago by a major explosive eruption and collapse event. This was the most recent of at least three caldera- forming eruptions that lofted pumice and ash (tephra) high into the air and spread pyroclastic flows across the volcano's surface. Subsequent lava flows have partly buried the deposits from this eruption, but one exposure can be seen at Paulina Creek Falls, where a deposit of pyroclastic flow and fall material was so hot that ash and pumice particles were welded together and then cooled into solidified rock.
Before formation of the caldera, Newberryâ€™s summit was 150 to as much as 400 m (500 to 1,000 ft) higher than present-day 2,434-m (7,986-ft) Paulina Peak. Once the caldera was formed, more eruptions began to fill it with lava flows, and lava also erupted at numerous sites outside the caldera, covering much of the volcanoâ€™s north and south flanks.
Today, Newberry caldera holds two beautiful lakes, Paulina Lake and East Lake, popular for fishing, boating, swimming, and camping. Both caldera lakes have hot springs with temperatures as high as 135 degrees Fahrenheit. In 1987, temperatures higher than 500 degrees Fahrenheit at a depth of 900 m (approximately 3,000 ft) were found in a U.S. Geological Survey drill hole in the center of the caldera. These temperature measurements indicate that an active magma system lies beneath Newberry Volcano.