Gabrielse Cone facts for kids

Gabrielse Cone is a young cinder cone volcano located in the Tuya Volcanic Field in British Columbia, Canada. It's a special kind of volcano that usually erupts only once. This cone is about 400 meters (1,312 feet) wide and has a central crater that is about 30 meters (98 feet) deep. It formed very recently in Earth's history, during the Holocene epoch, after the last big ice age. On its northeast side, it looks like it's broken open, with old lava flows spreading out from it. The cone is found near the start of Iverson Creek.

What is Gabrielse Cone?

Gabrielse Cone is a type of volcano called a cinder cone. These volcanoes are usually small and cone-shaped. They are built from bits of hardened lava, called cinders, that erupt from a single vent.

Where is Gabrielse Cone Located?

This volcano is found in a region called the Tuya Volcanic Field. This area is in British Columbia, Canada. It's part of a larger chain of volcanoes known as the Northern Cordilleran Volcanic Province.

How Did Gabrielse Cone Form?

Gabrielse Cone formed during the Holocene epoch. This is the most recent geological time period, which started about 11,700 years ago. The cone is considered "postglacial," meaning it formed after the last major ice age ended. This suggests it's quite young in geological terms. When it erupted, it created a central crater and sent out lava flows.

Who is Gabrielse Cone Named After?

Gabrielse Cone is named after a Canadian geologist named Hu Gabrielse. He was the first person to identify and study this unique volcano.