Tutsingale Mountain facts for kids
Quick facts for kids Tutsingale Mountain |
|
|---|---|
| Highest point | |
| Elevation | 1,722 m (5,650 ft) |
| Prominence | 272 m (892 ft) |
| Listing | List of volcanoes in Canada |
| Geography | |
| Location | Cassiar Country, British Columbia, Canada |
| Parent range | Kawdy Plateau (northern Stikine Plateau) |
| Topo map | NTS 104J/15 |
| Geology | |
| Mountain type | Subglacial mound |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Last eruption | Pleistocene |
Tutsingale Mountain is a special kind of mountain located in northern British Columbia, Canada. You can find it on the Stikine Plateau, east of Nuthinaw Mountain. It's also northwest of Dease Lake and near the Tachilta Lakes.
This mountain is unique because of how it formed. It's actually a type of subglacial volcano. This means it grew under a thick layer of ice!
Contents
How Tutsingale Mountain Formed
Tutsingale Mountain was created during a time called the Pleistocene period. This was a very long time ago, when huge sheets of ice covered much of the Earth. The area where Tutsingale Mountain now stands was completely covered by a thick glacier.
Volcanic Eruptions Under Ice
Imagine a volcano erupting, but not into the air. Instead, the hot lava came out under a massive ice sheet! When the lava met the cold ice, it cooled down very quickly. This process built up the mountain from the bottom, under the ice.
What is a Subglacial Mound?
Tutsingale Mountain is known as a subglacial mound. This is a specific type of subglacial volcano. It means the volcano never managed to break through the thick ice above it. The lava just piled up underneath the ice, forming a mound shape.
This is different from volcanoes that erupt into the open air. The ice acted like a mold, shaping the mountain as it grew.
Where is Tutsingale Mountain?
This interesting mountain is part of the Kawdy Plateau. This plateau is a northern section of the larger Stikine Plateau. It's located in an area known as Cassiar Country in British Columbia.
Part of a Volcanic Belt
Tutsingale Mountain is also part of a bigger group of volcanoes. This group is called the Northern Cordilleran Volcanic Province. This area has many volcanoes that have been active over millions of years.
Key Facts About Tutsingale Mountain
- Height: Tutsingale Mountain stands at 1,722 meters (about 5,650 feet) tall.
- Type: It is a subglacial mound, formed under ice.
- Last Eruption: Its last known activity was during the Pleistocene period.
This mountain is a cool example of how powerful natural forces like volcanoes and glaciers can shape our Earth!
