|Pinus contorta subsp. contorta in Anacortes Community Forest Lands, Washington|
|Subgenus:||P. subg. Pinus|
|Section:||P. sect. Trifoliae|
|Subsection:||P. subsect. Contortae|
Pinus contorta, with the common names lodgepole pine and shore pine, and also known as twisted pine,  and contorta pine,  is a common tree in western North America.  It is common near the ocean shore and in dry montane forests to the subalpine, but is rare in lowland rain forests.   Like all pines (member species of the genus Pinus), it is an evergreen conifer.
- Pinus contorta subsp. bolanderi:  Bolander's beach pine, Bolander pine; endemic to Mendocino County on the northwestern California coast;  near threatened by fires and development   
- Pinus contorta subsp. contorta: shore pine; Pacific Coast, southern Alaska to northwest California.   
- Pinus contorta subsp. murrayana: tamarack pine, or Sierra lodgepole pine; Cascade Range from Washington into northern California; the Sierra Nevada, the Transverse Ranges of southern California (including the San Bernardino Mountains, the Peninsular Ranges into northern Baja California, and the Spring Mountains of southern Nevada).   
- Pinus contorta subsp. latifolia: lodgepole pine; Rocky Mountains, Colorado to Yukon and Saskatchewan; aspen parkland and boreal forests.   
Depending on subspecies, Pinus contorta grows as an evergreen shrub or tree. The shrub form is krummholz and is approximately 1 to 3 m (3 to 10 ft) high. The thin and narrow-crowned tree is 40 to 50 m (130 to 160 ft) high and can achieve up to 2 m (7 ft) in diameter at chest height.  The murrayana subspecies is the tallest. The crown is rounded and the top of the tree is flattened. In dense forests, the tree has a slim, conical crown. The formation of twin trees is common in some populations in British Columbia. The elastic branches stand upright or overhang and are difficult to break. The branches are covered with short shoots that are easy to remove.   
The species name is contorta because of the twisted, bent pines found at coastal areas and the tree's twisted needles.    Pinus contorta is occasionally known under several English names: black pine, scrub pine, and coast pine.   P. contorta subsp. latifolia will hybridise with the closely related jack pine (Pinus banksiana).
The egg-shaped growth buds are reddish-brown and between 20 and 30 mm (3⁄4 and 1 1⁄4 in) long. They are short pointed, slightly rotated, and very resinous. Spring growth starts in beginning of April and the annual growth is completed by early July. The dark and mostly shiny needles are pointed and 4 to 8 cm (1 1⁄2 to 3 in) long and 0.9 to 2 mm (0.04 to 0.08 in) wide. The needle edge is weak to clearly serrated. The needles are in pairs on short shoots and rotated about the shoots' longitudinal axes. In Alberta above 2,000 m (6,600 ft), 1 to 5 needles occur per short shoot. A population with a high proportion of three-needled short shoots occurs in the Yukon. Needles live an average of four to six years, with a maximum of 13 years. 
The cones are 3–7 centimetres (1–3 in) long. The cones have prickles on the scales.
Many populations of the Rocky Mountain subspecies, P. contorta subsp. latifolia, have serotinous cones. This means that the cones are closed and must be exposed to high temperatures, such as from forest fires, in order to open and release their seeds.  The variation in their serotiny has been correlated with wildfires and mountain pine beetle attacks.  The cones of the coastal Pacific subspecies, P. contorta subsp. contorta, are typically non-serotinous,  and those of the inland Pacific subspecies, P. contorta subsp. murrayana, are completely non-serotinous. 
Pinus contorta is a fire-dependent species, requiring wildfires to maintain healthy populations of diverse ages. The bark of the lodgepole pine is fairly thin, minimizing the tree's defense to fire; however, the heat of fire opens the cones to release the seeds. This allows the species to regenerate and maintain its place in the forest habitat.  One plant community in which Pinus contorta is found is the closed-cone pine forest of coastal California.
Excessive wildfire prevention disrupts the fire ecology. The stands are usually so densely populated that the trees self-thin, or out-compete each other, leaving dead trees standing. These become a dry ladder fuel that can accelerate the fire to the crown of living trees. When the fire reaches the crowns of the trees, it can jump from tree to tree and becomes relatively unstoppable.
The natural fire regime for this species is primarily driven by climate. The fires occur most often after years of drought. Pinus contorta occurs from the upper montane to the subalpine region. These types of forests experience a lot of moisture in the form of snow in the winter due to their altitude. The density of the tree stand also prohibits the establishment of an understory. With all of that being said, the likelihood of a surface fire occurring is rare. Thus, infrequent but severe fires dominate this species. 
An example of the climate that plays a huge role in the fire regime of Pinus contorta is quite complex. There are three different oscillations that play a major role in droughts. These are the Pacific Decadal Oscillation (PDO), Atlantic Multi-decadal Oscillation (AMO) and El Nino (ENSO). A combination of these oscillations being in effect (+) or not in effect (-) have a global effect on the water available to these forests. So when the AMO +, ENSO – and PDO –, there is going to be a drought and likely a severe subalpine fire. 
Suillus tomentosus, a fungus, produces specialized structures called tuberculate ectomycorrhizae with the roots of lodgepole pine (Pinus contorta var. latifolia). These structures have been shown to be the location of concentrations of nitrogen-fixing bacteria which contribute a significant amount of nitrogen to tree growth and allow the pines to colonize nutrient-poor sites.  
This species is attacked by blue stain fungus (Grosmannia clavigera), distributed by the mountain pine beetle from its mouth.
Lodgepole pine is named for its common use as structural poles for the Native American tipi shelter. A typical tipi is constructed using 15 to 18 pines. The long, straight, and lightweight characteristics of the species made it ideal for horse transport in nomadic Plains buffalo hunting cultures. Tribes made long journeys across the Great Plains to secure lodgepole pines that only grew in mountainous areas. In Minnesota, other species such as red pine would be used in tipis, though they were generally thicker, heavier, and more cumbersome to transport than Pinus contorta.
Pinus contorta is still used by many today for erecting tipis on American Indian reservations, at powwows, and at private homes. The trees may be harvested for tipi poles in U.S. National Forests, provided the harvester secured a permit to cut living trees for ceremonial or traditional purposes. The Bighorn Mountains, the Black Hills, and the Medicine Bow Mountains are popular tipi pole harvesting areas for Native Americans living on Plains Indians reservations in North and South Dakota, and immigrant tipi enthusiasts.
Pinus contorta is cultivated as an ornamental tree by the horticulture industry. Plant nurseries grow Pinus contorta subsp. contorta and Pinus contorta subsp. murrayana for use in traditional and wildlife gardens, and as smaller selections of the native plant for natural landscaping. The Shore pine's (ssp. contorta) smaller varieties and cultivars are also used in container gardening, including as large bonsai specimens.
Cultivars of this species include:
- ‘Chief Joseph’, a dwarf variety of Pinus contorta var. latifolia grown for its yellow winter needles
- ‘Spaan's Dwarf’, a dwarf variety of Pinus contorta var. contorta that grows wider than it grows tall
Lodgepole pine is the Provincial tree of Alberta, Canada.
Pinus contorta is a serious invasive species of wilding conifer in New Zealand, along with several other western North American pine species. It is listed on the National Pest Plant Accord and is prohibited from sale, commercial propagation, and distribution.
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- "Pinus contorta var. bolanderi". Germplasm Resources Information Network (GRIN). Agricultural Research Service (ARS), United States Department of Agriculture (USDA).
- Also treated as Pinus contorta subsp. contorta var. bolanderi, in which case what is treated here as Pinus contorta subsp. contorta is the variety Pinus contorta subsp. contorta var. contorta.
- "Pinus contorta ssp. bolanderi". Calflora: Information on California plants for education, research and conservation, with data contributed by public and private institutions and individuals, including the Consortium of California Herbaria. Berkeley, California: The Calflora Database – via www.calflora.org.
- Farjon, Aljos (2010). A Handbook of the World's Conifers. 2. Leiden, Netherlands: Koninklijke Brill NV. pp. 654–655. ISBN 978-90-04-17718-5.
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- "Pinus contorta var. contorta". Germplasm Resources Information Network (GRIN). Agricultural Research Service (ARS), United States Department of Agriculture (USDA).
- "Pinus contorta var. murrayana". Germplasm Resources Information Network (GRIN). Agricultural Research Service (ARS), United States Department of Agriculture (USDA).
- "Pinus contorta ssp. murrayana". Calflora: Information on California plants for education, research and conservation, with data contributed by public and private institutions and individuals, including the Consortium of California Herbaria. Berkeley, California: The Calflora Database – via www.calflora.org.
- "Pinus contorta var. latifolia". Germplasm Resources Information Network (GRIN). Agricultural Research Service (ARS), United States Department of Agriculture (USDA).
- "Pinus contorta". Natural Resources Conservation Service PLANTS Database. USDA. Retrieved 2015-01-24.
- Johnson, Kershaw; MacKinnon, Pojar (1995). Plants of the Western Boreal Forest and Aspen Parkland. Edmonton AB: Lonepine Publishing. p. 27. ISBN 1-55105-058-7.
- Schütt, Weisgerber; Schuck, Lang; Stimm, Roloff (2008). Lexikon der Nadelbäume. Hamburg, Germany: Nikol. pp. 365–367. ISBN 3-933203-80-5.
- "Plants and Trees: lodgepole pine". U.S. Forest Service. Retrieved 12 August 2014.
- "Pinus contorta var. contorta : Shore Pine". Oregon State University. Retrieved 12 August 2014.
- "Forests of Crater Lake National Park: Lodgepole Pine (Pinus Contorta)". Crater Lake Institute. Retrieved 12 August 2014.
- Cope, Amy B. (1993). "Pinus contorta var. contorta". Fire Effects Information System (FEIS). US Department of Agriculture (USDA), Forest Service (USFS), Rocky Mountain Research Station, Fire Sciences Laboratory – via https://www.feis-crs.org/feis/.
- Anderson, Michelle D. (2003). "Pinus contorta var. latifolia". Fire Effects Information System (FEIS). US Department of Agriculture (USDA), Forest Service (USFS), Rocky Mountain Research Station, Fire Sciences Laboratory – via https://www.feis-crs.org/feis/.
- Feduck, Mike. "The genetic basis of cone serotiny in Pinus contorta as a function of mixed-severity and stand-replacement fire regimes". bioRxiv 023267.
- Cope, Amy B. (1993). "Pinus contorta var. murrayana". Fire Effects Information System (FEIS). US Department of Agriculture (USDA), Forest Service (USFS), Rocky Mountain Research Station, Fire Sciences Laboratory – via https://www.feis-crs.org/feis/.
- Schoennagel, Tania; Thomas Veblen (2004). "The Interaction of Fire, Fuels and Climate across Rocky Mountain Forests". BioScience. 54 (7): 661–76. doi: 10.1641/0006-3568(2004)054[0661:TIOFFA]2.0.CO;2. ISSN 0006-3568.
- Kauffman, J. Boone (August 2004). "Death Rides the Forest: Perceptions of Fire, Land Use and Ecological Restoration of Western Forests" (PDF). Conservation Biology. 18 (4): 878–82. doi: 10.1111/j.1523-1739.2004.545_1.x. Retrieved 24 February 2010.
- Paul, L.R.; Chapman, B.K.; Chanway, C.P. (2007). "Nitrogen Fixation Associated with Suillus tomentosus Tuberculate Ectomycorrhizae on Pinus contorta var. latifolia". Annals of Botany. 99 (6): 1101–1109. doi: 10.1093/aob/mcm061. PMC 3243579. PMID 17468111.
- Chapman, W.K.; Paul, L.R. (2012). "Evidence that Northern Pioneering Pines with Tuberculate Mycorrhizae are Unaffected by Varying Soil Nitrogen Levels" (PDF). Microbial Ecology. 64 (4): Open Access. doi: 10.1007/s00248-012-0076-0.
- Coops, Nicholas C.; Waring, Richard H. (March 2011). "A process-based approach to estimate lodgepole pine (Pinus contorta Dougl.) distribution in the Pacific Northwest under climate change". Climatic Change. 105 (1–2): 313–328. doi: 10.1007/s10584-010-9861-2.
- Rudolf, John Collins (28 February 2011). "Climate Change Takes Toll on the Lodgepole Pine". Green: A Blog About Energy and the Environment. Retrieved 1 March 2011.
- "results of search". umich.edu.
- "RHS Plantfinder - Pinus contorta 'Chief Joseph'". Retrieved 2 May 2018.
- "AGM Plants - Ornamental" (PDF). Royal Horticultural Society. July 2017. p. 78. Retrieved 2 April 2018.
- Lotan, James E.; Critchfield, William B. (1990). "Pinus contorta". In Burns, Russell M.; Honkala, Barbara H. Conifers. Silvics of North America. Washington, D.C.: United States Forest Service (USFS), United States Department of Agriculture (USDA). 1 – via Southern Research Station (www.srs.fs.fed.us).
|Wikimedia Commons has media related to:|
|Wikispecies has information related to Pinus contorta|
- Jepson eFlora, The Jepson Herbarium, University of California, Berkeley
- University of Wisconsin: Lodgepole forest webpage
- Virginia Tech dendrology website: Pinus contorta
- Guardian (U.K.) article: "Plague of beetles raises climate change fears for American beauty"
- Pinus contorta in the CalPhotos Photo Database, University of California, Berkeley
- Picea sitchensis - information, genetic conservation units and related resources. European Forest Genetic Resources Programme (EUFORGEN)