Dana Glacier (Washington) facts for kids
Quick facts for kids Dana Glacier |
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 Dana Glacier
Location in Washington (state)
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| Type | Alpine glacier |
| Location | Chelan County, Washington, U.S. |
| Coordinates | 48°19′09″N 121°03′05″W / 48.31917°N 121.05139°W |
| Length | 1 mi (1.6 km) |
| Terminus | Icefall/Barren rock |
| Status | Retreating |
The Dana Glacier is a cool natural feature found in the Wenatchee National Forest in Washington, U.S. It's like a very slow-moving river made of ice! This glacier is located about half a mile west of a mountain called Dome Peak.
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What is Dana Glacier?
Dana Glacier is an Alpine glacier. This means it's a type of glacier that forms in mountain valleys. It flows generally towards the north. The glacier stretches for about 1 mile (1.6 km).
How Does It Look?
A special ridge of rock, called an arête, splits the Dana Glacier into two parts. Imagine a sharp, knife-like ridge sticking up through the ice! Other arêtes also separate Dana Glacier from its neighbors, Chickamin Glacier and Dome Glacier. These other glaciers are to its east and south.
Its Journey Downhill
The Dana Glacier moves downhill from very high up. It starts at nearly 8,000 feet (2,400 meters) and flows down to about 6,000 feet (1,800 meters). This downward movement is what makes it a glacier.
Is It Changing?
Like many glaciers around the world, Dana Glacier is currently "retreating." This means it is getting smaller. The ice is melting faster than new snow can build up. Scientists study glaciers like Dana Glacier to understand more about our planet's climate.
Why Are Glaciers Important?
Glaciers are super important for a few reasons. They store a lot of fresh water. When they melt slowly, they provide water for rivers and streams. This water is used by people, animals, and plants. Glaciers also help shape the land. As they move, they carve out valleys and mountains. They are like giant natural bulldozers!
