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

From Wikipedia, the free encyclopedia

Mount Maude
North Face of Mount Maude seen from Seven Fingered Jack
Highest point
Elevation9040+ ft (2755+ m) NGVD 29[1]
Prominence882 ft (269 m)[1]
Coordinates48°08′14″N 120°48′14″W / 48.1373508°N 120.8039882°W / 48.1373508; -120.8039882[2]
Geography
Mount Maude is located in Washington (state)
Mount Maude
Mount Maude
Location in Washington
LocationChelan County, Washington, U.S.
Parent rangeNorth Cascades, Entiat Mountains
Topo mapUSGS Holden
Climbing
First ascentAugust 19, 1932 by Hermann F. Ulrichs and John Burnett.[3]
Easiest routeSouth slopes

Mount Maude is the 15th highest peak in Washington state. The peak is located in the Entiat Mountains, a subrange of the North Cascades. It is in the Glacier Peak Wilderness, at the headwaters of the Entiat River. The peak was given its name by Albert H. Sylvester in honor of Frederick Stanley Maude.[3]

The mountain from the south side consists of mostly talus with small rocky outcroppings, often compared with mountains in the Colorado Rockies. The northeast side is much different, with a steep rocky summit sheltering the small Entiat Glacier. Most climbers will climb Maude, Seven Fingered Jack, and sometimes Mount Fernow in the same trip.

YouTube Encyclopedic

  • 1/1
    Views:
    583
  • Native Report - Season 6 Episode 4

Transcription

Geology

The mountain is made of Cretaceous Orthogneiss, and Tonalite. The flank of the mountain on the southwest side are made of Triassic Orthogneiss and Triassic to Permian Heterogeneous Metamorphic rock. While the northeast side also consist of Eocene Quartz Diorite, and small marble deposits. Many normal faults are present as well as one small strike-slip fault near Spectacle Buttes.[4]

Routes

References

  1. ^ a b "Mount Maude, Washington". Peakbagger.com.
  2. ^ "Mount Maude". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2009-06-13.
  3. ^ a b Majors, Harry M. (1975). Exploring Washington. Van Winkle Publishing Co. p. 45. ISBN 978-0-918664-00-6.
  4. ^ https://web.archive.org/web/20150626142445/https://fortress.wa.gov/dnr/geology/?Theme=wigm. Archived from the original on June 26, 2015. Retrieved July 2, 2015. {{cite web}}: Missing or empty |title= (help)

Gallery

External links


This page was last edited on 15 April 2022, at 04:17
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.