World Library  
Flag as Inappropriate
Email this Article

Hubbard Glacier

Article Id: WHEBN0000656879
Reproduction Date:

Title: Hubbard Glacier  
Author: World Heritage Encyclopedia
Language: English
Subject: Wrangell–St. Elias National Park and Preserve, Glacial lake outburst flood, Russell Fjord, Ice dam, Hubbard
Collection:
Publisher: World Heritage Encyclopedia
Publication
Date:
 

Hubbard Glacier

Hubbard Glacier
False color image of the Hubbard Glacier
Type Tidewater/Mountain glacier AKA Valley Glacier
Location Yakutat City and Borough, Alaska, U.S., Yukon, Canada
Coordinates
Length 122 kilometres (76 mi)
Terminus Sealevel
Status Advancing

Hubbard Glacier is a glacier, located in eastern Alaska and part of Yukon Canada, named after Gardiner Hubbard.

Map of Hubbard Glacier
Hubbard Glacier, Alaska squeezes towards Gilbert Point on May 20, 2002 The glacier is close to sealing off Russell Fjord at top from Disenchantment Bay at bottom.

The longest source for Hubbard Glacier originates 122 kilometres (76 mi) from its snout and is located at about , approximately 8 kilometres (5 mi) west of Mount Walsh with an altitude around 11,000 feet (3,400 m). A shorter tributary glacier begins at the easternmost summit on the Mount Logan ridge at about 18,300 feet (5,600 m) at about .

Before it reaches the sea, Hubbard is joined by the Valerie Glacier 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 25 metres (82 ft), and the decrease in salinity threatened its sea life.[1]

Around midnight on October 8 the dam began to give way. In the next 24 hours an estimated 5.3 cubic kilometres (1.3 cu mi) of water gushed through the gap, and the fjord was reconnected to the ocean at its previous level.[1] This was the second largest glacial lake outburst flood (GLOF) in recorded history, and had the equivalent flow of about 35 Niagara Falls.

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 18 m (59 ft) above sea level.[2] 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[3] 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.

Contents

  • Cited references 1
  • See also 2
  • Image gallery 3
  • External links 4

Cited references

  1. ^ a b "USGS Report: Hubbard Glacier, Alaska: Growing and Advancing in Spite of Global Climate Change and the 1986 and 2002 Russell Lake Outburst Floods". U.S. Geological Survey. Retrieved 2007-01-18. 
  2. ^ "2002 Russell Fjord Closure and Russell Lake Outburst". Water Resources of Alaska • Glacier and Snow Program. U.S. Geological Survey. January 3, 2007. Retrieved 2007-07-07. 
  3. ^ Ellin Beltz glossary of glacier terms Retrieved May 3, 2013.

See also

Image gallery

Panoramic view of the glacier

External links

  • Earthshots: Satellite Images of Environmental Change, U.S. Geological Survey
  • Google Maps: Interactive satellite view of where Hubbard Glacier meets the sea
  • U.S. Geological Survey: Sequence of photographs showing the 2002 ice blockage and breakthrough
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and USA.gov, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for USA.gov and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
 
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
 
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.
 


Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.