Geography
Pelican Butte is located in Klamath County, Oregon. It is disconnected from the main axis of the Cascade Range, having formed above a network of Fault_(geology)#Dip-slip_faults, normal faults that mark the eastern border of the Cascades. The volcano reaches an elevation of . Pelican Butte has steep sides and despite erosion from glaciers, its original shape is mostly preserved. During the Pleistocene epoch, glaciers formed a canyon and a cirque on the northeastern side of the volcano; they also reduced the summit elevation several tens of meters and carved out an intrusive rock, intrusive conduit in the volcano. Pelican Butte is large, with a volume of , making it one of the larger Quaternary volcanoes in the region of Crater Lake (Oregon), Crater Lake and Mount Shasta. It is about 33 percent larger than Mount McLoughlin, which lies to its west. Pelican Butte is the most prominent shield volcano in the southern Oregon Cascades.Ecology
On the volcano, at about elevation, Douglas fir and Pinus ponderosa, Pondersora pine trees dominate. At an elevation of , the Abies magnifica, Shasta red fir dominates certain areas; at elevations of , the red fir as well as Abies concolor, white fir become predominant. In a study of relationships between the northern spotted owl and its prey species, scientists identified animals including the Northern flying squirrel, Bushy-tailed woodrat, and voles as living at Pelican Butte. Less common animals that served as prey included Peromyscus, Deer mice and Townsend's chipmunk as well as insects.Geology
Pelican Butte is a shield volcano. It sits on basaltic andesite erupted during the Pliocene and early Pleistocene epochs. Samples from the volcano have 58 to 60 percent silicon dioxide, silica, and the volcano is made up of calc-alkaline basaltic andesite and andesite lava with normal Magnet#Polarity, polarity. For the lower volcano, thick lava flows followed existing channels forming volcanic glass, glassy deposits with phenocrysts including plagioclase, augite, hypersthene, and olivine. These phenocrysts are relatively sparse among the lava flows. A second type of andesitic lava created thinner flows with Lava#Block_lava_flows, blocks and scoria closer to the summit of the volcano. With a finer grain and Vesicular texture, vesicular texture, the lava has phenocrysts of white plagioclase with sodic labradorite as well as olivine, augite, and hypersthene. It is believed that the volcano is made up of breccia based on eroded areas with breccia between lava flows, though breccia is not well-exposed elsewhere on the mountain. The summit of Pelican Butte has a cinder cone. Eruptive material at the volcano includes basalt and andesite, with minerals including plagioclase feldspar, olivine, clinopyroxene, and orthopyroxene. Along the southwestern flank of the volcano, pyroxene basaltic andesite deposits form outcrops that have been weathering, weathered into spheres. These outcrops typically range from in length, rarely exceeding , forming ridges that range from in width. One deposit with block lava has a vesicular texture with zeolite. In general, basaltic andesite deposits are 75–80% plagioclase, 8–10% clinopyroxene, and 8–10% orthopyroxene, with olivine ranging from 2–5%, typically in an altered form as iddingsite. There is one distinct geochemical sample with a higher nickel and chromium content than other lava erupted by the volcano, which may reflect heterogeneity in the source for the erupted material. A fault (geology), fault fault scarp, scarp sits adjacent to lava flows on the western flank of the volcano, though the fault did not move the deposits, suggesting this lava was erupted 1.17 million years ago.Eruptive history
Pelican Butte last erupted within the past 700,000 years. Dating for its last eruptive activity is unclear; it has clearly not erupted since it was covered by glaciers about 12,000 years ago, though it probably has not erupted for 60,000 years. According to Wood and Kienle (1990), most eruptions took place less than 200,000 years ago. However, Gorman (1994) reports that K–Ar dating of the summit places the volcano at 540,000 years old. According to the Global Volcanism Program, Pelican Butte has not erupted since the Pleistocene. Eruptions at Pelican Butte built a summit cone with tuff breccia and lapilli during pyroclastic eruptive activity, which was mostly covered by lava flows before it was eroded over time by glaciation, which lowered the cone's elevation significantly. Eruptive activity at Pelican Butte was mildly explosive eruption, explosive, later switching to thinner flows with Lava#.CA.BBA.CA.BB.C4.81, ʻaʻā and block lava.Human history
Pelican Butte is named after nearby Pelican Bay. It was also known by American Indians as Mongina; the U.S. Coast and Geodetic Survey previously listed it under the name Lost Peak.Recreation
A gravel road runs all the way to the summit of the mountain, branching north off Oregon Route 140. The road is only open during snow-free months during the summer. The last few miles of the road are steep and narrow, but they are accessible by vehicles with high Ride height, ground clearance. The peak of Pelican Butte offers a 180 degree view of the Cascades stretching from south of Crater Lake to Mount McLoughlin. A winter use trail for the volcano is operated by the Klamath Basin Snowdrifters Snowmobile Club.Notes
* [a] The U.S. National Geodetic Survey lists the elevation of Pelican Butte as . However, the Geographic Names Information System lists its elevation as , and the Global Volcanism Program of the Smithsonian Institution lists the Twin Buttes summit elevation as .References
Sources
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* {{Volcanoes of Oregon , state=collapsed Buttes of Oregon Shield volcanoes of the United States Subduction volcanoes Cascade Volcanoes Volcanoes of Oregon Mountains of Oregon Landmarks in Oregon Cascade Range Fire lookout towers in Oregon Dormant volcanoes Mountains of Klamath County, Oregon Fremont–Winema National Forest Volcanoes of Klamath County, Oregon Pleistocene shield volcanoes Volcanoes of the United States