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A tree approximately 20 m tall on Cave Mountain, Nevada (C.J. Earle, 2001.09.27).

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Foliage with first-year cone and weathered wood on a tree in the Ruby Mountains of Nevada (C.J. Earle, 2001.09.23).

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Bark on a tree in the Ruby Mountains of Nevada (C.J. Earle, 2001.09.23).

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Cone of a tree on Cusick Mountain, Oregon, about 8 cm long (C.J. Earle, 2008.07.20).

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Cone of a tree on Mt. San Jacinto, California, about 10 cm long (C.J. Earle, 2004.04.10).

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Cones of var. reflexa, 16 to 20 cm long, collected in a stand on the W ridge of Signal Pk in the Pinal Mtns. of Arizona (C.J. Earle, 2012.12.27).

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The official largest limber pine, near Snowbird, UT. "Big Tree" Bob Van Pelt for scale [C.J. Earle, 1995.08.03].

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Closed-canopy forest of Pinus flexilis, Pinus longaeva, and Picea engelmannii on Cave Mountain, Nevada. These two pines very rarely form a closed-canopy stand [C.J. Earle, 2001.09.27].

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A large, old tree near the summit of Mt. San Jacinto, California [C.J. Earle, 2004.04.10].

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The Dielman Monarch, a large, old tree on the slopes of Cusick Mountain, Oregon [C.J. Earle, 2008.07.20] (aside: Cusick Mountain was named for pioneering Oregon botanist William Cusick). In early 2010 this tree was featured in an Oregon Public Broadcasting episode.

 

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Conservation status

Pinus flexilis

E. James 1823

Common names

Limber pine, limbertwig, Rocky Mountain pine (Peattie 1950), pino [Spanish] (Perry 1991), pin blanc de l'ouest [French] (Kral 1993).

Taxonomic notes

Section Strobus. Syn: Apinus flexilis (E. James) Rydberg (Kral 1993). One variety, Pinus flexilis var. reflexa Engelmann 1879 (syn: P. reflexa (Engelmann) Engelmann 1882; P. ayacahuite var. strobiformis Lemmon 1892; P. ayacahuite var. reflexa (Engelmann) Voss 1907; P. flexilis subsp. reflexa (Engelmann) Murray 1982 (Farjon and Styles 1997). P. flexilis and P. strobformis form a cline, showing continuous variation in ecological, morphological and molecular characters, a subject detailed in the "Taxonomic notes" section of P. strobiformis. Briefly, intermediate populations occur from southern Colorado to the northern Sierra Madre, and trees in this transitional area can reasonably be called Pinus reflexa (Engelmann) Engelmann, or may be referred to a variety or subspecies of P. flexilis or P. strobiformis. The cline becomes more complex in Mexico, with distinctions between populations of the Sierra Madre Occidental and Oriental, as well as of the Transverse Volcanic Plateau.

This cline has been the subject of much debate since the days of Engelmann and Lemmon. Among the more recent authorities, Farjon and Styles (1997) describe P. flexilis and P. strobiformis as forming a polymorphic cline, while Perry (1991) describes them as distinct taxa with introgression in their shared range. My own interpretation, after review of the relevant literature (cited above, plus Frankis [2008], Moreno-Letelier and Piñero [2009], and Bisbee [in litt.]) is that these taxa likely arose in the New World, probably from a subtropical Mexican progenitor, and that the cline has been subject to frequent migrations and mixing associated with glacial-interglacial transitions throughout the Pleistocene. Substantial further paleontological and molecular study is likely to be needed before anyone can confirm or deny that hypothesis.

Three photographs presented here show cones of limber pine in northeast Oregon, in extreme southern California, and in southern Arizona. All cones appeared representative of their local populations.

Description

Trees 12–15(–26) m tall; 60–90(–200) cm diameter, straight to contorted; crown conic, becoming rounded; growth form may be substantially altered near timberline (krummholz form occurs) or on very dry sites. Bark light grey, nearly smooth, becoming dark brown and cross-checked in age into scaly plates and ridges. Branches spreading to ascending, often persistent to trunk base; twigs pale red-brown, puberulous (rarely glabrous), slightly resinous, aging gray, tough and flexible, smooth. Buds ovoid, light red-brown, 0.9–1 cm, resinous; lower scales ciliolate along margins. Needles 5 per fascicle, spreading to upcurved and ascending, persisting 5–6 years, 3–7 cm × 1–1.5 mm, pliant, dark green, abaxial surface with less conspicuous stomatal bands than adaxial surfaces, adaxial surfaces with strong, pale stomatal bands, margins finely serrulate, apex conic-acute to acuminate; sheath 1–1.5(–2) cm, shed early. Staminate cones broadly ellipsoid-cylindric, ca. 15 mm, pale red or yellow. Ovulate cones maturing in 2 years, shedding seeds and falling soon thereafter, spreading, symmetric, lance-ovoid before opening, cylindro-ovoid when open, 7–15 cm long, yellow-brown, resinous, sessile to short-stalked, apophyses much thickened, strongly cross-keeled, umbo terminal, depressed. Seeds irregularly obovoid; body 10–15 mm, brown, sometimes mottled darker, wingless or nearly so. 2n=24 (Little 1980, Kral 1993).

In the absence of cones, it strongly resembles P. albicaulis. However, limber pine branches become roughened at a smaller size, usually <10 cm diameter, vs. >10 cm diameter in P. albicaulis. On older trees (>30 cm dbh), limber pine bark is usually composed of longitudinal reddish-brown plates with intervening fissures, while whitebark pine bark becomes light brown and thinly platy without conspicuous fissures. When in flower, whitebark pollen cones are a striking red color, while limber pine pollen cones are reddish or yellow. Saplings are very difficult to distinguish; Kral (1993) contends that bud scale margins are entire in whitebark pine, whereas lower bud scales have ciliate margins in limber pine. I have not tested this assertion in the field.

Distribution and Ecology

The type variety occurs in the Rocky Mountains and Intermountain Ranges from Canada: SE British Columbia and SW Alberta, S through USA: Oregon, Idaho, Montana, North Dakota, South Dakota, Nebraska, Wyoming, Colorado, Utah and Nevada to N New Mexico and W through N Arizona to S California at (1000)1500-3700 m, preferring dry, rocky slopes and ridges of high mountains up to timberline, often occurring in pure stands (Little 1980, Kral 1993). See also Thompson et al. (1999). Hardy to Zone 3 (cold hardiness limit between -39.9°C and -34.4°C) (Bannister and Neuner 2001).

Var. reflexa occurs in USA: Colorado, Arizona, New Mexico and W Texas (possibly Utah), and in Mexico: Chihuahua, Coahuila, Nuevo León (Frankis 2008, Bisbee in litt.).

Distribution data from USGS (1999).

The hardest land that supports a pinyon-juniper forest is the high plains of eastern Montana, where you can find a Pinus flexilis–Juniperus scopulorum forest clinging to the sandstone cliffs and washes of the Missouri breaks. West of there, all down the spine of the high Rocky Mountains from Alberta to New Mexico, this species comes into its own as a tree of the high mountains. On exposed and rocky sites it will sometimes descend to the lower treeline, but usually it is a tree of the passes and summits, sharing its habitat with other subalpine species such as Abies lasiocarpa var. bifolia and Picea engelmannii. It occupies similar sites in the Wallowa Mountains of Oregon, where it thrives best on limestone substrates (much like its southern cousin P. longaeva); and also west across the high plateaux of Utah and the high mountains of the Basin and Range province, where it occupies picturesque sites that receive most of their precipitation with the winter snows. It even holds to this niche in the highly diverse subalpine forests of the Sierra Nevada, where it reigns east of the range crest and on high summits of the Inyo, Panamint, White and other desert ranges, often mingling there with P. monophylla.

Big tree

Height 18 m, dbh 222 cm, crown spread 14 m. Locality: On a ridge S of Snowbird, Utah (American Forests 1996). There is also a very large specimen in Oregon, the Dielman Monarch (photo at left), measuring 205 cm DBH, 9.34 m tall, and with a crown spread of 8.2 m (Dielman 2009). Some very large trees reportedly occur in Nevada and Colorado as well, but I don't have the numbers.

Oldest

Crossdated ages of 1,670 years from site ERE in New Mexico, collected by Swetnam and Harlan; and 1659 years for specimen KET3996 from Ketchum, Idaho collected by Schulman in 1956 (Brown 1996). Given that crossdated tree ages are always underestimates because of the near-impossibility of sampling the tree's seedling growth years, either of these trees could have been the older, particularly since KET3996 was sampled about 30 years before the ERE tree. During a 1994 visit to Craters of the Moon National Monument, I believe I located KET3996; it was dead, and had been for many years.

Dendrochronology

Limber pine is an important species due to its longevity and widespread occurrence in the arid U.S.

Ethnobotany

There is some evidence that the seeds were used as a food source by certain Great Basin tribes, such as the Northern Shoshone. Numerous grinding stones at Alta Toquima Village, a high elevation prehistoric site in central Nevada, also suggest use of pine nuts as food, with limber pine the likely source (Lanner 1996).

I have observed that miners, sheepherders, and other rural residents in its range (ca. 1850-1950) used it for cabins, fencing, mine timbers, and doubtless, firewood. Muir (1894) wrote that "Throughout Utah and Nevada it is one of the principal timber-trees, great quantities being cut every year for the mines. The famous White Pine Mining District, White Pine City, and the White Pine Mountains have derived their names from it." However, the wood is too contorted and resinous, and the trees generally too small (though one wonders what stands were exterminated in the historical period) to warrant commercial exploitation in the modern age.

Observations

The most memorable stands I have seen have been:

Remarks

Both the epithet flexilis and the common name "limber" refer to the tough, flexible twigs. The seeds are an important food source for rodents and certain birds (Little 1980).

The fresh-cut wood has the odor of turpentine (Kral 1993).

White pine blister rust (Cronartium ribicola), an introduced fungal disease, has afflicted this and certain other white pines (Elias 1987).

This species is one of the primary hosts for the dwarf mistletoe Arceuthobium cyanocarpum (Hawksworth and Wiens 1996).

Stop a moment and listen to the whistle of the mountain wind it its short, stubby, thick needles. They are lifting their voices in a tale of their life that is all fierce endurance. The sort of winter wind that would get into the headlines of newspapers if it blew down below, blows here for days and weeks, raising the voices of the Pines to a high sustained keening note. Snows that would stop all traffic on our roads and streets weigh down its branches. But they do not break, for this a Limber Pine whose long boughs and twigs can bend and bend without snapping. A tree better adapted to endure timberline conditions does not exist.Donald Culross Peattie

Citations

Bisbee, Jeff. in litt.. Cone morpholoy of the Pinus flexilis-strobiformis complex and related species of the western United States and Mexico. Bulletin of the Cupressus Conservation Project 3:xxx-xxx.

Dielman, Gary. 2009. Ascending the Giants - Chronicles Of Measuring Champion Trees. ascendingthegiants.org/news/15/52/Limber-Pine.html, accessed 2010.02.14.

James, Edwin. 1823. Account of an Expedition from Pittsburgh to the Rocky Mountains, Performed in the Years 1819, 1820., V.2, pp. 224-225. Available http://content.wisconsinhistory.org/u?/aj,17167, accessed 2011.05.20.

See also

Burns and Honkala (1990).

Kendall, Katherine C. 1995. Limber pine. In Status and Trends of the Nation's Biological Resources. U.S. Geological Survey.

Lanner (1983).

Schoettle, A.W. and S.G. Rochelle. 2000. Morphological variation of Pinus flexilis (Pinaceae), a bird-dispersed pine, across a range of elevations. American Journal of Botany 87:1797-1806. Available: http://www.amjbot.org/cgi/content/full/87/12/1797, accessed 2008.01.07.

Last Modified 2014-12-12