{"id":8647,"date":"2024-04-22T18:03:21","date_gmt":"2024-04-22T18:03:21","guid":{"rendered":"http:\/\/versicolor.ca\/sandylakebedford\/?page_id=8647"},"modified":"2024-04-28T10:09:44","modified_gmt":"2024-04-28T10:09:44","slug":"e-pit-mound-topography-occurs-in-older-less-harvested-stands","status":"publish","type":"page","link":"https:\/\/versicolor.ca\/sandylakebedford\/recreation\/forest-walk-notes\/e-pit-mound-topography-occurs-in-older-less-harvested-stands\/","title":{"rendered":"E: Pit &#038; Mound topography occurs in older, less harvested stands"},"content":{"rendered":"<blockquote><p><em>&#8211; <strong>Mounds are formed<\/strong> by blowdown of Big Trees<\/em><br \/>\n<em>&#8211; <strong>Age<\/strong> = Oldest Tree on mounds +10-15 years<\/em><br \/>\n<em>&#8211; <strong>Pits and Mounds with similar orientation<\/strong> at Sandy Lake&#8212;&gt;Hurricanes<\/em><br \/>\n<em>hitting from SE; Sites 1,2,3 likely in 1869 (Saxby Gale, 155 yrs ago) or 1873<\/em><br \/>\n<em>(The Nova Scotia Storm, 151 yrs ago); Peninsula a storm 60-70 years<\/em><br \/>\n<em>earlier.<\/em><br \/>\n<em>&#8211; <strong>Ecological Significance<\/strong> &#8211; vernal pools in pits; mounds are preferred seedbeds; sites of the Wabanaki Forest Love Affair (Yellow Birch &amp; Hemlock); microbiota continuity.<\/em><\/p><\/blockquote>\n<p><strong>More Info<\/strong><\/p>\n<p><a href=\"https:\/\/en.wikipedia.org\/wiki\/Pit-and-mound_topography\"><strong>Pit-and-mound topography<\/strong><\/a><br \/>\nOn Wikipedia<\/p>\n<p><a href=\"http:\/\/versicolor.ca\/sandylakebedford\/forests\/acadian-forest-love-affair\/\"><strong>Wabanaki Forest Love Affair<\/strong><\/a><br \/>\nThe physical intimacy of yellow birch and hemlock often observed in old Wabanaki forest is more than a coincidence<\/p>\n<p><strong><a href=\"http:\/\/versicolor.ca\/sandylakebedford\/forests\/pit-mound-topography\/\">Pit &amp; Mound Topography<\/a><\/strong><br \/>\nPage on this website provides descriptive data on the pit and mound topography at Sandy Lake and Environs<\/p>\n<p>View the <strong><a href=\"http:\/\/versicolor.ca\/sandylakebedford\/forests\/mature-og-forest\/\">Mature\/OG Forest<\/a><\/strong> page for a discussion of their significance to the forest ecology of Sandy Lake and Environs.<\/p>\n<p>&nbsp;<\/p>\n<div id=\"attachment_8659\" style=\"width: 650px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM.png\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-8659\" class=\"size-large wp-image-8659\" src=\"http:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM-1024x766.png\" alt=\"\" width=\"640\" height=\"479\" srcset=\"https:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM-1024x766.png 1024w, https:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM-300x224.png 300w, https:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM-768x574.png 768w, https:\/\/versicolor.ca\/sandylakebedford\/wp-content\/uploads\/2024\/04\/Screen-Shot-2024-04-22-at-3.25.32-PM.png 1133w\" sizes=\"auto, (max-width: 640px) 100vw, 640px\" \/><\/a><p id=\"caption-attachment-8659\" class=\"wp-caption-text\"><strong>Pit and Mound topography at Sandy Lake<\/strong>.\u00a0 Growing evidence suggests Pit &amp; Mound Topography is a consistent feature of Old Growth in Nova Scotia.<br \/><em>Click on image for larger version<\/em><\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>&#8211; Mounds are formed by blowdown of Big Trees &#8211; Age = Oldest Tree on mounds +10-15 years &#8211; Pits and Mounds with similar orientation at Sandy Lake&#8212;&gt;Hurricanes hitting from SE; Sites 1,2,3 likely in 1869 (Saxby Gale, 155 yrs &hellip; <a href=\"https:\/\/versicolor.ca\/sandylakebedford\/recreation\/forest-walk-notes\/e-pit-mound-topography-occurs-in-older-less-harvested-stands\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":8563,"menu_order":50,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-8647","page","type-page","status-publish","hentry"],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/pages\/8647","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/comments?post=8647"}],"version-history":[{"count":12,"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/pages\/8647\/revisions"}],"predecessor-version":[{"id":8706,"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/pages\/8647\/revisions\/8706"}],"up":[{"embeddable":true,"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/pages\/8563"}],"wp:attachment":[{"href":"https:\/\/versicolor.ca\/sandylakebedford\/wp-json\/wp\/v2\/media?parent=8647"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}