Hubbard Glacier
Template:Short description Template:About Template:Infobox glacier
Hubbard Glacier (Lingít: Sít' Tlein) is a glacier located in Wrangell–St. Elias National Park and Preserve in eastern Alaska and Kluane National Park and Reserve in Yukon, Canada, and named after Gardiner Hubbard.
Geography
The longest source for Hubbard Glacier originates Template:Convert from its snout and is located at about Template:Coord, approximately Template:Convert west of Mount Walsh with an elevation around Template:Convert. A shorter tributary glacier begins at the easternmost summit on the Mount Logan ridge at about Template:Convert at about Template:Coord.
Before it reaches the sea, Hubbard is joined by the Valerie Glacier<ref>Way: Valerie Glacier (48749131) OpenStreetMap</ref> to the west, which, through forward surges of its own ice, has contributed to the advance of the ice flow that experts believe will eventually dam the Russell Fjord from Disenchantment Bay waters.
The Hubbard Glacier ice margin has continued to advance for about a century. In May 1986, the Hubbard Glacier surged forward, blocking the outlet of Russell Fjord and creating Russell Lake. All that summer, the new lake filled with runoff; its water level rose Template:Convert, and the decrease in salinity threatened its sea life.<ref name="USGS">Template:Cite web</ref>
Around midnight on October 8, the dam began to give way. In the next 24 hours, an estimated Template:Convert of water gushed through the gap, and the fjord was reconnected to the ocean at its previous level. This was the largest glacial lake outburst flood (GLOF) in recorded history.<ref name="USGS"/>
In spring 2002, the glacier again approached Bert Point. It pushed a terminal moraine ahead of its face and closed the opening again in July. On August 14, the terminal moraine was washed away after rains had raised the water level behind the dam it formed to Template:Convert above sea level.<ref name="USGS2">Template:Cite web</ref> The fjord could become dammed again, and perhaps permanently. If this happens, the fjord could overflow its southern banks and drain through the Situk River instead, threatening trout habitat and a local airport.
It takes about 400 years for ice to traverse the length of the glacier, meaning that the ice at the foot of the glacier is about 400 years old. The glacier routinely calves<ref>Ellin Beltz glossary of glacier terms Retrieved May 3, 2013.</ref> off icebergs the size of a ten-story building. Where the glacier meets the bay, most of the ice is below the waterline, and newly calved icebergs can shoot up quite dramatically, so that ships must keep their distance from the edge of the glacier in Disenchantment Bay.
Collision
On June 25, 2022, the cruise ship Norwegian Sun collided into a growler (a chunk of ice smaller than an iceberg) in foggy conditions as it approached the Hubbard Glacier for sightseeing. The ship was damaged but it was considered safe. It cut its cruise itinerary short and sailed back to Juneau for assessment, and then Seattle for repairs without further incident.<ref>Template:Cite web</ref>
MV Hubbard
The Alaska Marine Highway System ferry MV Hubbard is named after Hubbard Glacier.<ref>Template:Cite web</ref> This name was chosen by local student Taylor Thompson, whose essay won Alaska's name-the-new-ferry contest.<ref>Template:Cite web</ref>
See also
References
Gallery
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The glacier from a distance
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Hubbard Glacier and icebergs formed by calving
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Closeup of Hubbard Glacier
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The glacier relatively close
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Panoramic view