11/03/2026
Can you name this peak? Here’s a clue: Little _ Peak**.
Built by lava between 160,000 and 40,000 years ago, this peak took shape as Mount Rainier’s eruptions slowed. Meanwhile, erosion wore away the mountain’s upper slopes and lowered its summit.
But the shaping of this peak was not as gradual. After thousands of years of slow erosion, a sudden collapse transformed it in seconds.
On December 14, 1963, 12-14 million cubic yards of rock broke loose from this peak and thundered onto Emmons Glacier below changing the landscape in moments. No one witnessed the collapse, but its roar was certainly heard.
The rock debris covered the glacier as an insulating blanket. Two or three years later, scientists observed that Emmons Glacier had advanced significantly—a reminder that rock, ice, and volcanic activity are connected in a landscape that is always changing.
What geologic changes come to mind when you think of Mount Rainier?
**This is Little Tahoma Peak, elevation 11,138 feet (3,395 meters). Located east of Mount Rainier’s summit, it is the third-highest peak in Washington.
NPS/RBall photo