Cracker Creek Cone facts for kids

Cracker Creek Cone is a small cinder cone volcano located in the northwestern part of British Columbia, Canada. It's like a mini-mountain made from volcanic ash and rocks. This cone is part of a larger group of volcanoes in the area.

Scientists think a huge flow of hot, melted rock, called lava, might have come from Cracker Creek Cone. This lava flow partly filled a nearby area known as Ruby Creek.

What is Cracker Creek Cone?

Cracker Creek Cone is a type of volcano called a cinder cone. These volcanoes are usually small and have a cone shape. They are built up from bits of lava that explode from a single vent. These bits cool quickly in the air and fall around the vent, forming the cone.

How Old is This Volcano?

The lower western side of Cracker Creek Cone has a layer of glacial till covering it. Glacial till is a mix of rocks and dirt left behind by glaciers. This suggests that the cone is older than the most recent times when glaciers moved through Ruby Creek. This means it's been around for a while!

Where is Cracker Creek Cone Located?

Cracker Creek Cone is found in a large volcanic region called the Northern Cordilleran Volcanic Province. This area stretches across parts of Canada and the United States. It's known for having many different types of volcanoes.

Cracker Creek Cone is also one of three younger volcanoes in a smaller area called the Atlin Volcanic Field. This field is a specific spot within the larger volcanic province where more recent volcanic activity has happened.