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Revision as of 14:46, 15 May 2009 by KennethNg (talk | contribs) (New page: {{Coord|55.354736000000003|-131.691317 |display=title}} == Misty Fjords National Monument == * '''Location & Contact Information''' ** Address: 3031 Tongass Ave Ketchikan AK USA ** Telep...)
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Coordinates: 55°21′17″N 131°41′29″W 55.354736000000003, -131.691317

Misty Fjords National Monument

  • Location & Contact Information
    • Address: 3031 Tongass Ave Ketchikan AK USA
    • Telephone Number: +
    • Official Website: []
  • Overview

Misty Fjords National Monument was created December 1, 1978, and covers 2,294,343acres (9,246km²) of Tongass National Forest in the Panhandle of southeast Alaska. All but 151,832acres (614km²) is designated wilderness; Congress reserved the non-wilderness area for the Quartz Hill molybdenum deposit, possibly the largest such mineral deposit in the world. The monument is administered by the U.S. Forest Service, an agency within the U.S. Department of Agriculture.The area is called "The Yosemite of the North" for its similar geology. Light-colored granite, about 50 to 70 million years old (Eocene Epoch to Cretaceous Period) has been sculpted by glaciers that gouged deep U-shaped troughs throughout the monument. Many of the glacial valleys are filled with sea water and are called "canals", but they are not man-made in any way; the walls of these valleys are near-vertical and often rise 2,000 to 3,000feet (600 to 900m) above sea level, and drop 1,000feet (300m) below it. Because of the remoteness of the area, most visitors arrive by cruise ship or fly over the monument in tourist aircraft from Ketchikan or Juneau, Alaska.The region was first visited by Europeans in 1793 when George Vancouver sailed through Behm Canal, the prominent sea-filled glacial trough along the western margin of the monument and separating it from Revillagigedo Island. Vancouver discovered New Eddystone Rock, a 237foot (72m) tall column of basalt in the middle of Behm Canal. It was formed within the past 5 million years by volcanic activity, evidence for which is scattered sparsely through the monument, including a lava flow high above Punchbowl Cove, and at Blue River in the far northern part of the monument near the Canadian border.Across from the Salmon River and Portland Canal and the settlement of Hyder, Alaska, small glaciers occupy high areas of the northeast part of the monument. Soule and Through Glaciers cover high plateaus and valleys in the Lincoln and Seward Mountains, where one peak rises to 6,250feet (1,900m) above sea level. Most mountain tops in the monument are in the 4,000 to 5,000foot (1,200 to 1,500m) elevation range. Tree line is usually around 2,700feet (800m). Western Hemlock, Sitka Spruce and Western Redcedar dominate the prolific rainforest vegetation; wildlife in abundance includes both Grizzly and Black Bears, many species of salmon, whales, mountain goats, and deer.[1]

Gallery

References

  1. Misty Fjords National Monument Wikipedia.ORG. Accessed May 2009.