Chikoida Mountain facts for kids
Quick facts for kids Chikoida Mountain |
|
|---|---|
| Highest point | |
| Elevation | 1,927 m (6,322 ft) |
| Prominence | 975 m (3,199 ft) |
| Geography | |
| Location | British Columbia, Canada |
| Parent range | Taku Plateau |
| Geology | |
| Age of rock | Cenozoic |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Last eruption | Cenozoic |
Chikoida Mountain is a mountain located in the northwestern part of British Columbia, Canada. It stands on a high, flat area known as the Taku Plateau. This mountain is about 52 kilometers (32 miles) southeast of a town called Atlin. You can find it on the east side of the Silver Salmon River.
What is Chikoida Mountain?
Chikoida Mountain is not just any mountain; it's a special kind of mountain called a volcanic feature. This means it was formed by volcanic activity a very long time ago. It's part of a larger area known as the Northern Cordilleran Volcanic Province. This province is a huge region in western North America where many volcanoes have formed over millions of years.
How Old is Chikoida Mountain?
Chikoida Mountain formed during the Cenozoic era. This era began about 66 million years ago and continues to this day. So, Chikoida Mountain is many millions of years old! It's a reminder of Earth's powerful geological past.
Where is the Taku Plateau?
The Taku Plateau is a large, elevated area of land in British Columbia. A plateau is like a big, flat tableland that is higher than the land around it. The Taku Plateau is known for its rugged beauty and is home to many natural features, including mountains like Chikoida.
