Conrad Glacier facts for kids
Quick facts for kids Conrad Glacier |
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 Conrad Glacier
Location in Washington (state)
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| Type | Mountain glacier |
| Coordinates | 46°29′37″N 121°24′23″W / 46.49361°N 121.40639°W |
| Length | .25 mi (0.40 km) |
| Terminus | Barren rocks |
| Status | Retreating |
The Conrad Glacier is a mountain glacier found in the Goat Rocks area of Washington, a state in the USA. This glacier is located on the north side of Gilbert Peak, which stands at 8,184-foot (2,494 m) tall.
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What is Conrad Glacier?
Conrad Glacier is a body of ice that slowly moves down a mountain. It flows towards the north-northeast. The glacier starts at a high elevation of about 7,500 ft (2,300 m). As it moves, it reaches areas of bare rocks and loose rock fragments called talus.
Where is it Located?
The glacier is part of the beautiful Goat Rocks wilderness. This area is known for its rugged mountains and stunning natural scenery. The Goat Rocks are located within the Gifford Pinchot National Forest in Washington state.
How Has it Changed Over Time?
Like many glaciers around the world, Conrad Glacier has been shrinking. Scientists have observed significant changes over the years. Between 1970 and 2004, parts of the glacier lost more than 29 ft (8.8 m) of their thickness. This is like losing the height of a three-story building!
Glacier Retreat and Proglacial Lakes
Because of this shrinking, the Conrad Glacier has split into several smaller pieces of ice. This process is called "glacier retreat." It means the glacier is melting faster than new snow and ice can form.
Where the glacier used to end, there is now a proglacial lake. This lake formed at an elevation of 6,416 ft (1,956 m). A proglacial lake is a body of water that forms in front of a melting glacier. It's a clear sign that the glacier has moved back from its original position.
