Along Whistler’s Valley Trail near Rainbow Park you come across some impressively unusual trees. Unlike most other Whistler trees with straight trunks and slender branches, these lodgepole pines have wide gnarled trunks and magnificently huge, muscular branches. The branches of are of various sizes, ranging from very thick and long to enormous and long enough to disappear into the forest canopy. The more impressive branches emerge from the trunk nearly horizontal, then abruptly bend skyward.
Alexander Falls 
Ancient Cedars 
Black Tusk 
Blackcomb Mountain Brandywine Falls Brandywine Meadows Brew Lake Callaghan Lake Cheakamus Lake 
Cheakamus River 
Cirque Lake Flank Trail Garibaldi Lake Garibaldi Park Helm Creek Jane Lakes Joffre Lakes Keyhole Hot Springs Logger’s Lake Madeley Lake Meager Hot Springs Nairn Falls Newt Lake Panorama Ridge Parkhurst Ghost Town Rainbow Falls Rainbow Lake Ring Lake Russet Lake Sea to Sky Trail Skookumchuck Hot Springs Sloquet Hot Springs Mount Sproatt Taylor Meadows Train Wreck 
Wedgemount Lake Whistler Mountain
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Just looking at the top half of one of the lodgepole pines near Rainbow Park, it would appear as several trees growing close together, instead of one tree with parallel, upward growing branches. In fact, some of the largest, skyward growing branches are similarly thick as the trunk, which nearer the top of the tree split into four closely packed trunk-sized branches. This chaotic frenzy of gigantic branches gives these trees a marvelously striving and powerful appearance, like supersized bodybuilders in the midst of normal sized people. The base of these bizarrely beautiful trees follows a similar pattern to the branches. Where the trunk meets the hard, cement-like ground is a tangled row of startlingly enormous roots emerging horizontal and plunging down into the ground. It is easy to think that decades have worn the forest floor away revealing the roots, but it appears that these trees grow this way on purpose. Maybe as a way to better stabilize the enormous girth above, or maybe to avoid unseen rocky ground below. Whatever the reason, none of their neighbouring big trees replicate this sprawling, exposed root pattern these big lodgepole pines exhibit. This chaotic array of powerful roots, like the similarly thick branches above, set these old pines apart from their more conventional tree neighbours. With their thick trunks, enormous branches, and grey, old and scaly bark, these grizzled old lodgepole pines look ancient, however they are probably just a couple hundred years old. Not that two centuries isn’t old for a tree, but nearby, similarly aged western redcedars, western hemlocks and Whistler spruce trees look comparatively youthful.
The arrestingly hardy appearance of these lodgepole pines is a clue to their remarkable adaptability to difficult environments. You are just as likely to find lodgepole pines growing in dry, sandy soil as you are to find them in swampy terrain. Though not readily noticeable on a hot July day, but the big, gnarled lodgepole pines near Rainbow Park reside in fairly swampy ground much of the year. If you were to look across the nearby train tracks you would see an expanse of wetland extending to the forest beyond. The much smaller, though no less hardy lodgepole pines that grow on the rock plateau near the Whistler Bungee Bridge in Brandywine Falls Provincial Park, exist in a considerably drier environment.
An interesting feature of lodgepole pines is that they largely rely on forest fires to propagate. The seeds in lodgepole pine cones is protected by a layer of pitch which keeps them safe until the heat from a forest fire releases them. After a forest fire sweeps through a valley, lodgepole pines are one of the first trees to appear in fantastic numbers. The lodgepole name originated from the frequent use of these trees by indigenous people as support poles for teepees and lodges. Lodgepole pine is the common name of one of four subspecies of Pinus contorta. Its full scientific name is Pinus contorta subsp. latifolia. The other, naturally growing subspecies of Pinus contorta you may encounter in the vicinity of Whistler is the shore pine, or Pinus contorta subsp. contorta. These grow all along the Pacific coast from Alaska to California, whereas lodgepole pines grow more in the interior of BC, in the Rocky Mountains from Colorado to the Yukon and as far as Saskatchewan. The other two subspecies, bolanderi (Bolander’s beach pine) and murrayana (tamarack pine, or Sierra lodgepole pine), range only in the southwest United States. The Pinus contorta species gets their descriptive name contorta for two reasons. First, weather battered, coastal lodgepole pines often have a battered and contorted form. Second, their needles have a contorted, or slightly twisted shape to them.
Identifying a lodgepole pine in Whistler is easy if you find the ones on the Valley Trail from Lorimer Road to Rainbow Park mentioned above. Less obvious ones in Whistler might require a closer look. The bark on lodgepole pines is noticeably scaly looking like cornflakes. The colour is greyish brown and sometimes with orange highlights in the furrows. The bark is very similar to Whistler spruce trees, so you then have to check out the needles. Lodgepole pine needles are about 5cm long and grow in bundles of two. Overall, the needles are arrayed around the twig. The pine cones are fairly distinct when compared to other Whistler trees. Less than 5cm long, lodgepole pine cones are small compared to other pines. Each cone scale has a tiny prickle on it. The cones sometimes grow in pairs and occasionally point back towards the trunk.
Lodgepole pine bark grayish brown and cornflake like in appearance. You may see a slight orange colouring between the flakes. Whistler spruce trees have similar scaly, cornflake like bark, though the scales are much larger on Whistler spruce trees.
Lodgepole pine needles are possibly the easiest, distinguishing feature. They will be arrayed in bundles of two, a feature you don’t see in other Whistler tree needles.
Lodgepole pine cones are fairly easy to distinguish from other Whistler area tree cones. They are fairly small, less than 5cm long, egg-shaped, and each scale has a very noticeable prickle at the tip. Young cones are light green in colour and turn brown as they age. Lodgepole pine cones are attached directly to the branch without a stalk and it is not unusual to see an old cone attached for years.
Lodgepole pines require a lot of sun and in Whistler you often find them in sunny plateaus on various hiking trails. The Brew Lake trail has several rocky, sunny and very dry plateaus with several hardy lodgepole pines growing as krummholz. Near the Whistler Bungee Bridge alongside Cheakamus River you will find similarly hardy trees growing on the hard, rocky plateau. Certainly the best examples of mature lodgepole pines in Whistler are the terrifically gnarled, old pines along the Valley Trail near Rainbow Park.
Pictured below is a nice grove of very hardy lodgepole pine trees alone the Brew Lake trail. Trees that are stunted and brutalized by their hardy environment are known as krummholz which literally translates from German as bent, crooked, twisted wood.
P
lants of the Whistler Region is an excellent book that includes great pictures and descriptions of most trees you will find in Whistler. Small enough to fit in your pocket and comprehensive enough to identify most things you will encounter growing in the forests of Whistler. Along with conifer trees and broadleaf trees the book has chapters on flowers, berries, ferns and shrubs. You can find Plants of the Whistler Region on Amazon, the Whistler Library and at Armchair Books in Whistler Village. The author Collin Varner has a wonderful series of Plants of.. books on various regions beyond Whistler. Plants of Vancouver and the Lower Mainland, Plants of the Gulf and San Juan Islands and Southern Vancouver Island, and Plants of the West Coast Trail. In the last couple years he has started a new series of books. The Flora and Fauna of Coastal British Columbia and the Pacific Northwest and Edible and Medicinal Flora of the West Coast: British Columbia and the Pacific Northwest.
Ablation Zone Accumulation Zone Adit Lakes Aiguille Alpine Zone Arborlith Arête ARRTI Armchair Glacier The Barrier Battleship Islands Bears Bench Bergschrund Bivouac Bungee Bridge Bushwhack Cairn Carter, Neal Chimney Cirque Cloudraker Coast Douglas-fir Coast Mountains Col Columnar Jointing Cordilleran Cornice Corrie Lake Crevasse Dalgleish, Alec Deadfall Emerald Forest Erratic The Fissile Fitzsimmons Creek Fitzsimmons Range Fyles, Tom Garibaldi Ranges Garibaldi Volcanic Belt Gemel Glacier Window Green Lake Green Lake Loop Hoary Marmot Krummholz Lodgepole Pine Moraine Mt Garibaldi Mt James Turner Mountain Hemlock Northair Mine North Arm Farm Nunatuk Nurse Stump Overlord Pacific Yew Paper Birch Parkhurst Cat Parkhurst RD8 Parkhurst Cletrac Parkhurst Plow Tree Parkhurst Ridge Parkhurst Sawmill Parkhurst Wye Peak 2 Peak Rainbow Lodge Roundhouse Rubble Creek Scree Spearhead Range Tarn The Table Townsend, Charles Usnea Waterbar Western Hemlock Western Redcedar Whistler Spruce Winram, Mills
Alexander Falls Ancient Cedars Black Tusk Blackcomb Mountain Brandywine Falls Brandywine Meadows Brew Lake Callaghan Lake Cheakamus Lake Cheakamus River Cirque Lake Flank Trail Garibaldi Lake Garibaldi Park Helm Creek Jane Lakes Joffre Lakes Keyhole Hot Springs Logger’s Lake Madeley Lake Meager Hot Springs Nairn Falls Newt Lake Panorama Ridge Parkhurst Ghost Town Rainbow Falls Rainbow Lake Ring Lake Russet Lake Sea to Sky Trail Skookumchuck Hot Springs Sloquet Hot Springs Mount Sproatt Taylor Meadows Train Wreck Wedgemount Lake Whistler Mountain
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