{"id":35596,"date":"2015-01-02T22:47:24","date_gmt":"2015-01-03T05:47:24","guid":{"rendered":"http:\/\/trgg.ca\/?post_type=dt_portfolio&#038;p=35596"},"modified":"2019-10-12T13:15:02","modified_gmt":"2019-10-12T20:15:02","slug":"pinnacle-peak","status":"publish","type":"dt_portfolio","link":"https:\/\/www.tumblerridgegeopark.ca\/index.php\/project\/pinnacle-peak\/","title":{"rendered":"Pinnacle Peak"},"content":{"rendered":"<div class=\"wpb-content-wrapper\" id=\"wpb-content-root\"><p>[vc_row][vc_column][vc_column_text]<strong>PINNACLE PEAK HIKING ROUTE<\/strong><\/p>\n<ul>\n<li>4-6 Hours<\/li>\n<li>7km Return Distance<\/li>\n<li>690m (2260 ft) Elevation Change<\/li>\n<\/ul>\n<p>The 670 metre ascent to the top of Pinnacle Peak leads through an old cut-block, a thick forest of fir and spruce, an avalanche chute, and along an alpine ridge. The rewards for this hard work are great: spectacular mountain views with intriguing geological features and fossils, and a summit climb which looks challenging from a distance but turns out to be a simple scramble. There are fine views of the Windfall Lake area, Sentinel Peak with a glacier on its eastern flank, and Mt Crum with its distinctive anticline.[\/vc_column_text]<div class=\"ult-spacer spacer-6acbe62bc1648\" data-id=\"6acbe62bc1648\" data-height=\"10\" data-height-mobile=\"10\" data-height-tab=\"10\" data-height-tab-portrait=\"\" data-height-mobile-landscape=\"\" style=\"clear:both;display:block;\"><\/div>[\/vc_column][\/vc_row][vc_row][vc_column]<div class=\"dt-fancy-separator title-left h3-size\" style=\"width: 100%;\"><div class=\"dt-fancy-title\" style=\"color: #000000;\"><span class=\"separator-holder separator-left\"><\/span>More Information<span class=\"separator-holder separator-right\"><\/span><\/div><\/div>[vc_tta_accordion color=&#8221;black&#8221; c_icon=&#8221;chevron&#8221; c_position=&#8221;right&#8221; active_section=&#8221;1&#8243;][vc_tta_section title=&#8221;Fossils in Limestone&#8221; tab_id=&#8221;1496029193940-8f1725b8-4679&#8243;][vc_column_text]The limestone rocks preserve the remains of creatures that inhabited this offshore sea. We find <a href=\"https:\/\/en.wikipedia.org\/wiki\/Trilobite\" target=\"_blank\" rel=\"noopener noreferrer\">trilobites<\/a>, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Brachiopod\" target=\"_blank\" rel=\"noopener noreferrer\">brachiopods<\/a>, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Crinoid\" target=\"_blank\" rel=\"noopener noreferrer\">crinoids<\/a>, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Blastoid\" target=\"_blank\" rel=\"noopener noreferrer\">blastoids<\/a>, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Ammonoidea\" target=\"_blank\" rel=\"noopener noreferrer\">ammonoids<\/a>, clams, <a href=\"https:\/\/en.wikipedia.org\/wiki\/Bryozoa\" target=\"_blank\" rel=\"noopener noreferrer\">bryozoans<\/a>, and a variety of <a href=\"https:\/\/en.wikipedia.org\/wiki\/Burrow#Invertebrate_burrows\" target=\"_blank\" rel=\"noopener noreferrer\">invertebrate burrows<\/a>. The easiest fossils to recognize are the corals, both the solitary (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Rugosa\" target=\"_blank\" rel=\"noopener noreferrer\">rugose<\/a>) and colonial (<a href=\"https:\/\/en.wikipedia.org\/wiki\/Tabulata\" target=\"_blank\" rel=\"noopener noreferrer\">tabulate<\/a>) forms. These types of corals went extinct at the end of the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Permian\" target=\"_blank\" rel=\"noopener noreferrer\">Permian Period<\/a>. Just below the summit of Pinnacle Peak the route passes an impressive bedding plane exposure which contains numerous coral fossils.[\/vc_column_text][\/vc_tta_section][vc_tta_section title=&#8221;Mississippian Period Geology&#8221; tab_id=&#8221;1496029194061-a9e52b91-6f0c&#8221;][vc_column_text]The rocks encountered along the route are from the Mississippian Period (359-323 million years ago). In some other parts of the world rocks of this age contain the remains of ancient forests, and have yielded abundant coal resources. By contrast, rocks of this age in the Tumbler Ridge area were formed from sediments deposited on the floor of a balmy, shallow sea, about 20\u02da north of the equator, off the shore of the continent of Laurentia. Near the summit the parallel bedding planes have been steeply titled by the mountain-formation process, and lie at an angle of 60\u02da to the horizontal. These limestone rocks are from the Rundle Group \u2013 initially described on Mt Rundle near Banff, Alberta.[\/vc_column_text][\/vc_tta_section][vc_tta_section title=&#8221;Small Caves&#8221; tab_id=&#8221;1496029248529-b41ff2f2-fb08&#8243;][vc_column_text]One of the distinguishing features of limestone rocks is their soluble capacity in water containing dissolved carbon dioxide, resulting in\u00a0caves and tunnels. Explorers may find small limestone caves in the rock layers below the alpine ridge section of the route. Sometimes animals fall into such caves and cannot escape. The alkaline environment is\u00a0excellent for preservation of their remains, yielding information on animal life in the <a href=\"https:\/\/en.wikipedia.org\/wiki\/Pleistocene\" target=\"_blank\" rel=\"noopener noreferrer\">Pleistocene Era<\/a>.[\/vc_column_text][\/vc_tta_section][vc_tta_section i_icon_fontawesome=&#8221;fa fa-map-marker&#8221; add_icon=&#8221;true&#8221; title=&#8221;Map&#8221; tab_id=&#8221;1496029249690-f90fba83-95b1&#8243;][vc_column_text]<\/p>\n<div data-canvas-width=\"328.7898619607843\">From Tumbler Ridge, drive north towards\u00a0Chetwynd on Highway 29 for 25 km to the turnoff\u00a0for the former Bullmoose Mine. \u00a0Follow the\u00a0Bullmoose\u00a0mine road for 17 km and turn left onto\u00a0the Windfall Creek Forest Service Road. \u00a0This\u00a0turnoff is just before an electrical substation.<\/div>\n<div data-canvas-width=\"328.7898619607843\">Follow the\u00a0Windfall Creek road for 23 km. \u00a0This\u00a0road climbs over a pass at km 14 and goes by\u00a0very scenic alpine areas. \u00a0Turn left at\u00a0km 23 and<\/div>\n<div data-canvas-width=\"99.77766117647059\">follow this side-road for 1.8 km until it ends at a\u00a0crossing of Windfall Creek, where the bridge has\u00a0been removed.<\/div>\n<p>[\/vc_column_text]<div class=\"ult-spacer spacer-6acbe62bc1686\" data-id=\"6acbe62bc1686\" data-height=\"10\" data-height-mobile=\"10\" data-height-tab=\"10\" data-height-tab-portrait=\"\" data-height-mobile-landscape=\"\" style=\"clear:both;display:block;\"><\/div>[vc_gmaps 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css_animation=&#8221;bounce&#8221;]<\/p>\n<p style=\"text-align: center;\"><a href=\"https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2019\/10\/pinnaclejuly2019.pdf\" target=\"_blank\" rel=\"noopener noreferrer\">Download PDF<\/a><\/p>\n<p><a href=\"https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2019\/10\/pinnaclejuly2019.pdf\" target=\"_blank\" rel=\"noopener noreferrer\"><img data-srcset=\"https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2015\/06\/pdf-282x300.png 282w, https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2015\/06\/pdf.png 350w\" decoding=\"async\" data-src=\"http:\/\/trgg.ca\/wp-content\/uploads\/2015\/06\/pdf-282x300.png\" class=\"alignnone wp-image-35522 aligncenter lazyload\" src=\"data:image\/gif;base64,R0lGODlhAQABAIAAAAAAAP\/\/\/yH5BAEAAAAALAAAAAABAAEAAAIBRAA7\" alt=\"pdf\"    sizes=\"(max-width: 47px) 100vw, 47px\" \/><noscript><img decoding=\"async\" class=\"alignnone wp-image-35522 aligncenter\" src=\"http:\/\/trgg.ca\/wp-content\/uploads\/2015\/06\/pdf-282x300.png\" alt=\"pdf\" width=\"47\" height=\"50\" srcset=\"https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2015\/06\/pdf-282x300.png 282w, https:\/\/www.tumblerridgegeopark.ca\/wp-content\/uploads\/2015\/06\/pdf.png 350w\" sizes=\"(max-width: 47px) 100vw, 47px\" \/><\/noscript><\/a>[\/vc_column_text]<div class=\"ult-spacer spacer-6acbe62bc1691\" data-id=\"6acbe62bc1691\" data-height=\"10\" data-height-mobile=\"10\" data-height-tab=\"10\" data-height-tab-portrait=\"\" data-height-mobile-landscape=\"\" style=\"clear:both;display:block;\"><\/div>[vc_gmaps 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fossils.<\/p>\n","protected":false},"author":2,"featured_media":35610,"comment_status":"open","ping_status":"closed","template":"","dt_portfolio_category":[80,75,76,81],"dt_portfolio_tags":[],"class_list":["post-35596","dt_portfolio","type-dt_portfolio","status-publish","has-post-thumbnail","hentry","dt_portfolio_category-alpine-hiking","dt_portfolio_category-hiking-destinations","dt_portfolio_category-paleontological-sites","dt_portfolio_category-strenuous","dt_portfolio_category-80","dt_portfolio_category-75","dt_portfolio_category-76","dt_portfolio_category-81","description-off"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Pinnacle Peak - Tumbler Ridge Global Geopark<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" 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