To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Languages
Recent
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Marble Canyon (British Columbia)

From Wikipedia, the free encyclopedia

Marble Canyon
Marble Canyon is located in British Columbia
Marble Canyon
Marble Canyon
Geography
CountryCanada
ProvinceBritish Columbia
Regional district
Coordinates50°50′00″N 121°41′00″W / 50.8333°N 121.6833°W / 50.8333; -121.6833

Marble Canyon is in the south-central Interior of British Columbia, a few kilometres east of the Fraser River and the community of Pavilion,[1] midway between the towns of Lillooet and Cache Creek. The canyon stems from a collapsed karst formation.

YouTube Encyclopedic

  • 1/3
    Views:
    2 586
    3 465
    319
  • Marble Canyon Kootenay National Park | British Columbia Canada | StepHenzVlogs
  • Marble Canyon, Kootenay National Park in Canadian Rockies, British Columbia, Canada Travel 4K
  • MARBLE CANYON Provincial Park BC

Transcription

Nomenclature

The canyon's name comes from the brilliant limestone of its walls. The bedrock is microcrystalline limestone (sedimentary rock) rather than marble (metamorphic rock).

The native name of the canyon in the Shuswap language is, when referring to the whole, sxmeltám, possibly referring to "Indian doctors",[2] while the name for the area of Crown and Turquoise Lakes and the provincial campground and adjoining south wall is getsgátsp, of unknown meaning. In addition to the steep walls rising from the lake's southeastern end, there is an eroded pinnacle known as Chimney Rock, or in a translation of K'lpalekw, the Secwepemc (Shuswap) name for it, Coyote's Penis.[3]

Geography

The north wall is over 965 metres (3,166 ft) high above Pavilion Lake and is the southernmost extent of the Marble Range; the south wall is c. 515 m (1500 ft) and is the northern extremity of the Clear Range. Higher peaks lie in behind the walls, increasing the depth if measured from their summits.

Stromatolites

Within the canyon are a series of lakes draining towards the Fraser River via Pavilion Creek. The largest of these is Pavilion Lake, which is home to a colony of microbialites (also known as stromatolites), unusual carbonate structures built by bacteria which resemble freshwater "coral" and which are the largest freshwater stromatolites in the world.[4][5]

Rock and ice climbing

Waterfall near Crown Lake

Marble Canyon is popular with climbers, both for its clean rock walls and also for its ice climbs, including one waterfall that freezes solid in midwinter (officially Crown Lake Falls but to climbers, "Icy BC"), and which is immediately opposite the provincial park campground adjacent to Highway 99 from Lillooet to Cache Creek, British Columbia.[6][7]

Cultural rights

These areas and Pavilion Lake, in addition to being provincial park, are also governed by special cultural rights and have important spiritual significance of the Pavilion Band.[8]

See also

References

  1. ^ "Marble Canyon (canyon)". BC Geographical Names.
  2. ^ Canadian Mountain Encyclopedia, "Native names for Marble Canyon", citing an essay by R. Tyhurst's in A Complex Culture of the British Columbia Plateau, Brian Hayden's, SFU Press
  3. ^ "Chimney Rock", Canadian Mountain Encyclopedia
  4. ^ BC Parks Marble Canyon Provincial Park webpage
  5. ^ Pavilion Lake Research Project
  6. ^ BC Parks Marble Canyon Provincial Park webpage
  7. ^ Canadian Mountain Encyclopedia entry
  8. ^ BC Parks Marble Canyon Provincial Park webpage
This page was last edited on 4 April 2024, at 15:20
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.