We run on the Tacoma and Eastern rail line. Beginning in 1906, that's what people used to take to get to the entrance of the national park at Ashford, Washington. From there, they'd take stagecoaches up to Paradise Inn.
The constant seismic rumblings were spotted by the Pacific Northwest Seismic Network (PNSN), where seismometers on Mount Rainier recorded three straight days of nearly nonstop, high-energy seismic signals across the west flank of the volcano. Unlike the seismic activity tied to major earthquakes, the patterns being seen in Washington look more like a volcanic tremor, a type of nonstop hum or roar that begins when magma, hot water, and gas moves around inside a volcano.
