[{"@context":"http:\/\/schema.org\/","@type":"BlogPosting","@id":"https:\/\/wiki.edu.vn\/en\/wiki19\/overlord-mountain-wikipedia\/#BlogPosting","mainEntityOfPage":"https:\/\/wiki.edu.vn\/en\/wiki19\/overlord-mountain-wikipedia\/","headline":"Overlord Mountain – Wikipedia","name":"Overlord Mountain – Wikipedia","description":"From Wikipedia, the free encyclopedia Overlord Mountain is a 2,625-metre (8,612-foot) glacier-clad peak located in the Garibaldi Ranges of the","datePublished":"2018-07-27","dateModified":"2018-07-27","author":{"@type":"Person","@id":"https:\/\/wiki.edu.vn\/en\/wiki19\/author\/lordneo\/#Person","name":"lordneo","url":"https:\/\/wiki.edu.vn\/en\/wiki19\/author\/lordneo\/","image":{"@type":"ImageObject","@id":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","url":"https:\/\/secure.gravatar.com\/avatar\/c9645c498c9701c88b89b8537773dd7c?s=96&d=mm&r=g","height":96,"width":96}},"publisher":{"@type":"Organization","name":"Enzyklop\u00e4die","logo":{"@type":"ImageObject","@id":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","url":"https:\/\/wiki.edu.vn\/wiki4\/wp-content\/uploads\/2023\/08\/download.jpg","width":600,"height":60}},"image":{"@type":"ImageObject","@id":"https:\/\/www.wikimedia.org\/static\/images\/wmf-logo.png","url":"https:\/\/www.wikimedia.org\/static\/images\/wmf-logo.png","height":"101","width":"135"},"url":"https:\/\/wiki.edu.vn\/en\/wiki19\/overlord-mountain-wikipedia\/","wordCount":2434,"articleBody":"From Wikipedia, the free encyclopediaOverlord Mountain is a 2,625-metre (8,612-foot) glacier-clad peak located in the Garibaldi Ranges of the Coast Mountains, in Garibaldi Provincial Park of southwestern British Columbia, Canada. It is the highest point of the Fitzsimmons Range, which is a subset of the Garibaldi Ranges, and can be readily seen from the Whistler Blackcomb ski area.[3] It is situated 15\u00a0km (9\u00a0mi) southeast of Whistler, and its nearest higher peak is Mount Macbeth, 3\u00a0km (2\u00a0mi) to the north-northeast.[3] The Benvolio Glacier rests below the south aspect of the summit, the Fitzsimmons Glacier on the east aspect, and the expansive Overlord Glacier spans the northern and western aspects of the mountain. Precipitation runoff from the peak and meltwater from its glaciers drains into tributaries of the Cheakamus River. The first ascent of the mountain was made in 1923 by Phyllis Munday and Don Munday via the Benvolio Glacier.[1] The mountain’s descriptive name was recommended by the \u00a0Garibaldi Park Board and officially adopted on September 2, 1930, by the Geographical Names Board of Canada.[2][4]Table of ContentsClimate[edit]Climbing Routes[edit]Gallery[edit]See also[edit]References[edit]External links[edit]Climate[edit]Based on the K\u00f6ppen climate classification, Overlord Mountain is located in the marine west coast climate zone of western North America.[5] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below \u221220\u00a0\u00b0C with wind chill factors below \u221230\u00a0\u00b0C. The months July through September offer the most favorable weather for climbing Overlord Mountain.Climbing Routes[edit]Established climbing routes on Overlord Mountain:[1]\u00a0 \u00a0Benvolio Glacier – class\u00a02 First Ascent 1923West Ridge – class\u00a04East RidgeNorth RidgeGallery[edit]See also[edit]References[edit]^ a b c d e f “Overlord Mountain”. Bivouac.com. Retrieved 2019-11-15.^ a b c “Overlord Mountain”. Geographical Names Data Base. Natural Resources Canada. Retrieved 2019-11-15.^ a b “Overlord Mountain, British Columbia”. Peakbagger.com. Retrieved 2019-11-12.^ “Overlord Mountain”. BC Geographical Names. Retrieved 2019-11-12.^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). “Updated world map of the K\u00f6ppen\u2212Geiger climate classification”. Hydrol. Earth Syst. Sci. 11. ISSN\u00a01027-5606.External links[edit]li{counter-increment:listitem}.mw-parser-output .hlist ol>li::before{content:\" \"counter(listitem)\"a0 \"}.mw-parser-output .hlist dd ol>li:first-child::before,.mw-parser-output .hlist dt ol>li:first-child::before,.mw-parser-output .hlist li ol>li:first-child::before{content:\" (\"counter(listitem)\"a0 \"}]]>.navbox-abovebelow,.mw-parser-output tr+tr>.navbox-group,.mw-parser-output tr+tr>.navbox-image,.mw-parser-output tr+tr>.navbox-list{border-top:2px solid #fdfdfd}.mw-parser-output .navbox-title{background-color:#ccf}.mw-parser-output .navbox-abovebelow,.mw-parser-output .navbox-group,.mw-parser-output .navbox-subgroup .navbox-title{background-color:#ddf}.mw-parser-output .navbox-subgroup .navbox-group,.mw-parser-output .navbox-subgroup .navbox-abovebelow{background-color:#e6e6ff}.mw-parser-output .navbox-even{background-color:#f7f7f7}.mw-parser-output .navbox-odd{background-color:transparent}.mw-parser-output .navbox .hlist td dl,.mw-parser-output .navbox .hlist td ol,.mw-parser-output .navbox .hlist td ul,.mw-parser-output .navbox td.hlist dl,.mw-parser-output .navbox td.hlist ol,.mw-parser-output .navbox td.hlist ul{padding:0.125em 0}.mw-parser-output .navbox .navbar{display:block;font-size:100%}.mw-parser-output .navbox-title .navbar{float:left;text-align:left;margin-right:0.5em}]]>Wikimedia ErrorOur servers are currently under maintenance or experiencing a technical problem.Please try again in a few\u00a0minutes.See the error message at the bottom of this page for more\u00a0information. 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