Glaciers / Glacial Features

a huge snowy mountain with vast glacier flowing off it
Denali's Muldrow Glacier

The Muldrow is a surging glacier, with the most recent event occurring in 2021.


A Land Sculpted by Ice

In the high, frozen regions of the Alaska Range, snow and ice are the main forms of precipitation. In the past, most of the snow and ice remained behind; very little melting occurred. Snow and ice accumulated and got deeper and deeper, year after year, until the mass of ice that formed was so thick it compressed under its own weight. Gravity caused this ice to flow through stream valleys as glaciers. Glaciers are rivers of ice. The glaciers we see today in the park are increasingly small remnants of their former selves, but all around us we can see evidence of how they dominated the landscape. During past ice ages, most recently about 10,000 years ago, glaciers covered the Alaska Range and much of Alaska in ice. All of south-central Alaska has been buried in ice numerous times, and the shape of the land in this area comes from the carving forces of glaciers and the debris they leave behind.

Glaciers are often fed by more snow and ice precipitating and accumulating at higher elevations. If ice builds up at its source, a glacier may flow at rates ranging from several feet per year to several feet per day. As a glacier flows downhill, it grinds away at its beds with tremendous force. It picks up rocks from its bed, grinding some to a fine powder called silt and by plucking up larger chunks. When the glacial ice melts, the silt is carried along in the meltwater to be deposited downstream as outwash. Streams flowing from melting glaciers are often milky-colored. The silt in the water is called glacial flour, and the silty water is described as glacial milk. The larger chunks get left behind as erratics or in unsorted deposits forming ridges or hills called moraines. Erratics are rocks that are foreign to the surrounding terrain. They differ from the types of rock found where they are deposited.

The rocks embedded in glacial ice grind away at bedrock, forming the jagged ridges and deep U-shaped valleys found in the range. Large blocks of ice can be stranded in the moraines left behind by retreating glaciers. When they finally melt, a water-filled depression known as a kettle lake develops. The carving action of ice forms many of the elongated lakes in the upper Susitna Valley to the south of Denali, and examination of a map reveals that they are all oriented in the direction that the ice was moving.

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2 minutes, 7 seconds

A quick exploration of glaciers in Denali (no audio)


Life on Glaciers

All sorts of things are blown onto the glaciers by wind: small plants, seeds, pollen, tiny insects, sometimes even birds! Most of these things freeze and eventually die, but some things manage to survive on the snow and some even spend their entire lives on the glaciers. Glaciers in Denali are covered with algal cells, minute plants so small that they can’t be seen with the naked eye. These algal cells, or algae, provide food for other organisms. Food chains on the glacier are very simple when compared to food chains in other habitats, but they provide an elegant example of how energy flows through a system. The sun shines on the snow and the algae. The algae use the sun to produce food for themselves and are eaten by insects, such as springtails. The springtails may die, decompose and return their nutrients to the glacier, or they may become food for larger animals, such as beetles.

One thing all organisms living on the glaciers share in common is size. They are all tiny! This is because resources, such as nutrients, are in short supply. Larger animals could not survive on such meager rations. Temperatures on the ice and snow are always at or below freezing. This means that there is usually very little free water. All organisms need water to survive. But if ice forms inside an animal’s body it can cause tissue damage or death. Glacier organisms have many adaptations that help them to cope with freezing temperatures. When the temperature drops, some types of invertebrates can isolate water in their bodies and cause it to form ice crystals in non-critical areas of their system. This prevents their tissues from being damaged. They may also produce a type of glycerol that acts as an antifreeze in the cells, keeping them from freezing completely.

But that’s not all! When the sun shines on the glacier, the ultraviolet rays bounce on the ice crystals and subject organisms to heavy doses of radiation. To help prevent damage from the radiation, glacial organisms have developed different types of "sunscreen". For example, one type of algae is colored red (causing "watermelon snow"). The red pigmentation is a type of kerotene, a substance that acts as a sunscreen for the algae.

The Glaciers of Denali

Glaciers cover one million acres, or one-sixth of Denali National Park. Like the many arms of an octopus, glaciers flow away from the mountains transporting hundreds of thousand of tons of ice each year. This ice eventually melts in the lower reaches of the glaciers and rapidly fills rivers with turbulent muddy water that flows into the oceans. The iconic image of a glacier calving ice chunks into the ocean cannot be seen here - these glaciers are more distant and rougher, eking out an existence high in the Alaska Range.

The most massive glaciers in the park drain snow and ice from the flanks of Denali. Hundreds of unnamed glaciers and at least 40 named glaciers flow from heights as high as 19,000 feet and descend to elevations as low as 800 feet above sea level. The Peters Glacier flows from the north and northwest portion of the mountain, whereas the Kahiltna Glacier is situated on the southwestern side of Denali and shares the southern slopes with an arm of the Ruth Glacier. The Ruth Glacier primarily occupies the southeast side Denali.

From the very top of Denali, Harper Glacier dumps snow and ice into the upper reaches of Muldrow Glacier, which carries snow and ice off Denali's northeast slopes. Of these glacial systems, the Ruth, Kahiltna and Muldrow Glaciers are the longest glaciers in the park; each is more than 30 miles long. The Kahiltna Glacier, which is not only the longest glacier in the park but also in the entire Alaska Range, is 44 miles in length.


Learn More about Glaciers, Glaciology and Glacier Monitoring


Last updated: September 29, 2022

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