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Mar 21 2007, 12:33 PM EDT
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Change: sedimentary structures thatsediment, createcreating the characteristic featuresdeposits and structures of the Coastal Mountains. TheThis following pages willsite examineexamines major concentrations of glacial activity in the South Coastal Mountains of BC, including: Garibaldi Provincial Park, the Waddington Region, and the Lillooet Icefield. ENJOY!Click
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Mar 21 2007, 10:04 AM EDT
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Change: activity continuously for the several thousand years. Glaciers flow from the Coastal and Rocky Mountains, where they originate in large ice fields. Coastal British Columbia, specifically the southern portion,portion (from Vancouver to Prince Rupert)Rupert), is home to thousands of glaciersmanyglaciers many of themwhich are
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Mar 21 2007, 9:27 AM EDT
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Change: activity throughout recent earth history (the Holocene).activity. Glaciers flow from the Coastal and Rocky Mountains, where they originate in large ice fields. Coastal British Columbia, specifically the southern portion, (from Vancouver to Prince Rupert) is home to thousands of glaciersmany of them are valley glaciers. Each of
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Mar 20 2007, 11:09 PM EDT
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Change: through-outthroughout recent earth history (the Holocene). Glaciers flow from the Coastal and Rocky Mountains, where they originate in large ice fields. Coastal British Columbia, specifically
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Mar 20 2007, 1:50 PM EDT
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Change: The Northwestern coast of North America is host to a large number of glaciers, and ice fields. These features are dependant on their location, altitude,
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Mar 18 2007, 3:50 PM EDT
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Change: Mountains. The following pages will examine two major concentrations of glacial activity: Garibaldi National Park, and the Lillooet Ice Field. ENJOY!Click Picturepicture to Enterenter Sitesite
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Mar 18 2007, 3:48 PM EDT
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Change: the Coastal Mountains. The following pages will examine two major concentrations of glacial activity: Garibaldi National Park, and the Lillooet Ice Field. ENJOY! Click Picture to Enter Site
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Mar 13 2007, 4:15 PM EDT
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Change: till characteristic of the Coastal Mountains. The following pages will examine two major concentrations of glacial activity: Garibaldi National Park, and the ComptonLillooet Ice Field. ENJOY!
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Feb 2 2007, 12:05 PM EST
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Change: Renamed from Welcome to BC Coast South! by Feb 2 2007, 12:05 PM EST for: Rename
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Feb 2 2007, 12:04 PM EST
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Change: Renamed from British Columbia and Yukon- B.C. Coast South by Feb 2 2007, 12:04 PM EST for: Rename
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Feb 2 2007, 12:01 PM EST
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Change: of the Coastal Mountains. The following pages will examine two major concentrations of glacial activity: Garibaldi National Park, and the Compton Ice Field. ENJOY! ~Team BC South
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Feb 2 2007, 12:01 PM EST
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Change: setting/setting, countrysubstrait, rock, annual climate conditions and many more important factors. Glacial Ice on the West Coast of Canada behaves differently than the Glaciers in the
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Feb 2 2007, 12:00 PM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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Feb 2 2007, 11:56 AM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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Feb 2 2007, 11:51 AM EST
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Change: EDITORS NOTE: The Northwestern coast of North America is host to a large number of glaciers, and ice fields. These features are dependant on their
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Jan 24 2007, 1:30 PM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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Jan 24 2007, 1:29 PM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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Jan 24 2007, 1:29 PM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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Jan 24 2007, 1:10 PM EST
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Change: Glacier Terrarosa Glacier Tremor Glacier Trorey Glacier Turner Glacier Tyee Glacier Ubyssey Glacier Warren Glacier Wedgemount Glacier Whert Glacier Whistler Glacier *Not an Exhaustive List, Team BC South reserves the right to change the content of this page Icefields of Southern British Columbia:Manquam Icefield Misty IcefieldSnowcap Icefield
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Jan 24 2007, 11:20 AM EST
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Change: There were only format changes (bold, italics, etc.) in this version. See this version for details.
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