White Chuck Cinder Cone facts for kids
Quick facts for kids White Chuck Cinder Cone |
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| Highest point | |
| Elevation | 6,020 ft (1,830 m) |
| Geography | |
 White Chuck Cinder Cone
Location in Washington (state)
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| Location | Snohomish County, Washington, U.S. |
| Parent range | Cascade Range |
| Topo map | USGS |
| Geology | |
| Mountain type | Cinder cone |
The White Chuck Cinder Cone is a special kind of volcano called a cinder cone. It's located near Glacier Peak in Snohomish County, Washington, in the U.S.. This cone sits close to where the White Chuck River begins.
People first learned about this cinder cone in 1934. It stands tall at about 6,020 feet (1,835 meters) above sea level.
How Old Is White Chuck Cinder Cone?
Scientists have studied the White Chuck Cinder Cone to figure out its age. They looked at how much glaciers have worn it down over time. Based on this, they believe the cinder cone is quite old. It probably formed sometime between 2,000 and 17,000 years ago. This makes it a relatively young feature in the long history of the Cascade Range volcanoes.
What is a Cinder Cone?
A cinder cone is the simplest type of volcano. It's built from small pieces of lava, called cinders, that are blown out of a single vent. As these cinders fall back to the ground, they pile up around the vent. This creates a cone-shaped hill with a bowl-shaped crater at the top. Cinder cones usually have steep sides and don't get as big as other types of volcanoes.
