The Nabesna is a big river of ice. It is in Alaska. It comes from high mountains. Many small ice paths feed it. It is very, very long. It makes a river when it melts. Can you imagine walking on ice?
The Nabesna is a big river of ice. It is in Alaska. It sits in the Wrangell Mountains. Deep snow feeds the ice. Many small ice paths feed it too. The ice flows past tall peaks. It turns and heads north. The ice melts at the end. This melt makes the Nabesna River. The river flows into another river. People use the ice to climb. Small planes can land on it. The ice is getting shorter now. It was once much longer.
The Nabesna Glacier is a giant river of ice. It sits in Alaska. It is part of the Wrangell Mountains. This glacier is very long. It is 53 miles long. It is the longest valley glacier in North America. It is also the longest interior valley glacier in the world. Deep snow feeds the ice. About 40 smaller ice paths, called tributary glaciers, also feed it. The ice flows from a large icefield. This icefield covers the north side of Mount Wrangell. Mount Wrangell is a large volcano. The glacier flows past Mount Blackburn and Atna Peaks. Then it turns north. At the end, the ice melts. This melt forms the Nabesna River. The river flows into the Tanana River. People use the glacier to climb or ski. Small bush planes can even land on the ice. They land when snow covers the cracks. The glacier is slowly shrinking. It has been shrinking since the early 1900s. It may have been even longer before that. It may have once been over 200 miles long.
The Nabesna Glacier is a massive river of ice in Alaska. It is a very special kind of glacier. It is a valley glacier. This glacier is 53 miles long. It is the longest valley glacier in North America. It is also the longest interior valley glacier in the whole world.
This huge ice feature sits in the Wrangell Mountains. It is a very important part of the landscape there.
Deep snow feeds the glacier to keep it growing. It gets snow from an icefield on Mount Wrangell. Mount Wrangell is a large shield volcano. About 40 smaller glaciers also feed the Nabesna. These are called tributary glaciers.
The ice flows past Mount Blackburn and the Atna Peaks. It starts by moving east. Then the glacier turns north. It ends at an elevation of about 3,000 feet.
People first gave this glacier its name in 1902. A man named F. C. Schrader named it. He worked for the U.S. Geological Survey. He named it after the Nabesna River.
The glacier is a main path for many people. Ski mountaineers and climbers use it to reach the mountains. Scientists also travel there to study the ice. It is a gateway to the heart of the mountains.
There are many interesting facts about this place. The glacier ends near an old mining town called Nabesna. You can reach this area by the Nabesna Road.
Some small bush planes can land on the ice. They land between 6,000 and 7,000 feet high. They can land when winter snow covers the deep cracks. These cracks in the ice are called crevasses. This makes the surface safer for landing.
As the years go by, the glacier is changing. It has been slowly shrinking since the early 1900s. This is called a retreat.
It might have been shrinking for even longer than that. Some ice marks show it was once much bigger. It may have been over 200 miles long. When the ice melts at the end, it forms the Nabesna River. This river flows into the Tanana River through a wildlife refuge.
The Nabesna Glacier is a massive river of ice located in Alaska. It is a significant geographic feature within the Wrangell Mountains. This glacier is classified as a valley glacier. A valley glacier is a large mass of ice that moves through a mountain valley. The Nabesna is a record-breaking glacier. It is the longest valley glacier in North America. It also holds the title of the longest interior valley glacier in the world.
The glacier forms through a complex process of accumulation and flow. It is fed by deep snowfall in the Wrangell Mountains. This snow comes from an extensive icefield. This icefield covers the northern flanks of Mount Wrangell. Mount Wrangell is a large shield volcano. The glacier also receives ice from approximately 40 tributary glaciers. Tributary glaciers are smaller glaciers that flow into a larger main glacier. These many sources help maintain the vast expanse of the Nabesna.
Gravity pulls the ice along a specific path through the mountains. Initially, the glacier flows in an easterly direction. It moves past several prominent volcanic peaks. These include Mount Blackburn and the Atna Peaks. After this initial path, the glacier changes direction. It turns toward the north. The glacier eventually reaches its terminus, which is its end point. This terminus sits at an elevation of about 3,000 feet.
History helps us understand how the glacier was named and discovered. F. C. Schrader named the glacier in 1902. He was a member of the U.S. Geological Survey. He chose the name based on the Nabesna River. The glacier serves as a vital route for many people today. It provides the normal access into the heart of the eastern Wrangell Mountains. Ski mountaineers and climbers use the ice to travel. Scientists also visit the glacier to conduct research.
The glacier is a unique place for transportation and travel. Small bush planes can actually land on the central portion of the ice. This usually happens at elevations between 6,000 and 7,000 feet. Pilots must wait for specific conditions to land safely. The winter snow must cover the crevasses. Crevasses are deep cracks that form in the moving ice. When the snow covers these cracks, the surface becomes more stable for landing.
Scientists have observed that the Nabesna Glacier is changing over time. The glacier has been undergoing a slow, near-continuous retreat. A retreat means the glacier is shrinking. This process has been happening since at least the early 1900s. There is evidence that the retreat may have started even earlier. Glacial deposits found much further down the valley suggest a massive past size. The glacier may have once been over 200 miles long.
Finally, the glacier plays a major role in the local water system. As the ice melts at its terminus, it creates the Nabesna River. This river flows in a northward direction. It travels through the Tetlin National Wildlife Refuge. Eventually, the Nabesna River flows into the Tanana River. This connection shows how the glacier supports the broader environment of Alaska. The movement of ice and water links the mountains to the river systems below.
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