After the arrival in Juneau airport, visitors can take the route leading south-east to the nearby Juneau City. But there is also another route – to the north – and after some seven kilometers, the road stops at the Mendenhall Lake. Here visitors finally have an unhindered view on a beautiful natural landmark – Mendenhall Glacier or, in local Tlingit language – Sitaantaagu or “The Glacier Behind the Town”. This glacier ends in the lake and numerous icebergs with the characteristic blue color of glacial ice are floating around the lake. Mighty, noisy Nugget Falls are visible to the right. Mountains are covered with thick, deep green forests but their summits are covered with ice and snow. Beautiful!
But there is a note of sadness in this landscape: consequences of global warming. Like almost any other glacier in the world, Mendenhall Glacier is melting and receding.
Mendenhall Glacier got its European-American name in 1891 or 1892 from Thomas Corwin Mendenhall (1841-1924): this outstanding scientist defined the border between Alaska and Canada. Back then the glacier extended further south, in the site of the present-day Mendenhall Lake. Now it has receded per some 3 kilometers and continues to melt. The glacier is 21.9 km long.
Currently, the glacier ends in the lake – but soon it will recede further and pull out from the lake. Then there will be no more floating icebergs in the Mendenhall lake.
The retreating glacier has uncovered also remnants of some 1,400 – 2,350 years old forest. This means that the glacier has advanced since then: most likely due to increased precipitation in the Juneau Icefield above the glacier.
Walk to the ice caves
Visitors can admire the beauty of the glacier and surrounding landscape from diverse vantage points. There is East Glacier Loop – a trail that lets to walk higher in the hills and look on the glacier from above. Nugget Falls Trail leads along the eastern shore of the lake towards the Nugget Falls, without crossing them.
But, if a visitor wants to reach the glacier (and caves in it!), he needs to take the West Glacier Trail. It starts on the western shore of the lake and after hefty walking over the hills for some 5 – 6 kilometers and diverse wonderful views the visitor finally is at the glacier. Don’t walk there alone: the trail is long and, if the rain starts, the cliffs become slippery. Or a bear might come… Or you can get lost when the darkness comes.
Caves in the blue ice
Ice caves in the Mendenhall Glacier are not unique. Ice is a fine material for cave formation: it is hard, tough but at the same time easily formed by the water. And there is a lot of water on the contact between the glacier ice and the ground. Each mountain glacier has got countless smaller and larger streams under it. Each of these streams gradually creates a cave near its exit from the glacier.
Glacial caves in mountain glaciers are rather short-lived and fast-changing. In the late summer, the stream becomes more powerful, ice melts and crumbles, the entrance of the cave collapses but deeper inside new passages are formed by the stream. During the winter it is calmer: the stream is frozen or silently flows under the ice. But the glacier moves anyway and the ice groans and cracks. Thus: winter could be the best time to see the caves if the visitor dares to climb across the hills during the short hours of the winter day.
Caves are not very long: some tens of meters or, sometimes – hundreds of meters. But this is more than enough: the eerie beauty of the glacial ice cave overwhelms immediately, after the first few meters.
The most unusual feature is the blue color. Everything is blue: initially in lighter shades but further inside – deep blue and finally – just black darkness. The physics behind this effect is the same as in deepwater: as the Sunlight goes through the extremely lucid glacial ice, the molecular structure of the water (ice) filters out the longer lightwaves one after another. The shortest waves of the blue color go much deeper into the ice than any other color.
Seeking the Mendenhall Glacier Ice Caves
After the walk on West Glacier Trail, the visitor reaches the glacier. Now he needs to find the ice caves (if he is not together with a guide). The walk along with the contact of the steep glacial moraine (mix of soft gravel and clay) and the ice is not simple. Everything is wet, there are numerous small ponds and streams with ice-cold water. Caves could be found when walking along the streams towards the glacier. Sometimes the caves are further on the glacier, not on its rim. And sometimes there are no accessible caves at all.
If the visitor is lucky, he finds a suitable entrance in one or another ice cave. The incredible blue color, the sounds of the moving glacier inside the cave… Gorgeous! Something to remember for the whole life!
But, if he has spent more time than initially planned, a thought sits in the mind: “Will I manage to go back across the hills before the darkness?”
Walk on the glacier and in the caves is dangerous and at any time (especially in warm days) the collapse of the ice can happen. Thus, if possible, better ask for the assistance of special tour agencies.
Mendenhall Glacier Ice Caves on the map
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|Location, GPS coordinates:||58.44197 N 134.55568 W|
|Rating:||(3.5 / 5)|
|Where is located?||North America, United States, Alaska, Juneau, north from the city airport, at the western side of Mendenhall Glacier near its end|
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