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・ Little pied bat
・ Little pied cormorant
・ Little pied flycatcher
・ Little Pigeon Creek Community
・ Little Pigeon River
・ Little Pigeon River (Cheboygan County)
・ Little Pigeon River (Indiana)
・ Little Pigeon River (Michigan)
・ Little Pigeon River (Mullett Lake)
・ Little Pigeon River (Tennessee)
・ Little Pike Bay
・ Little Pilgrim
・ Little Pine
・ Little Pine Creek
・ Little Pine Creek (Luzerne and Columbia Counties, Pennsylvania)
Little Pine Mountain
・ Little Pine River
・ Little Pine State Park
・ Little Pine Township, Crow Wing County, Minnesota
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・ Little Piney River
・ Little Pioneer
・ Little Pipe Creek bridge and viaduct
・ Little Piute Mountains
・ Little Placentia Sound
・ Little Plain Historic District
・ Little Plains River
・ Little planet
・ Little Plastic Castle
・ Little Plastic Remixes


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Little Pine Mountain : ウィキペディア英語版
Little Pine Mountain

Little Pine Mountain is a mountain in Santa Barbara County, California, in the Los Padres National Forest at the southern edge of the San Rafael Mountains. It separates the drainages of Oso Creek, which flows into the upper Santa Ynez River, from the drainage of Santa Cruz Creek, which flows into the middle section of the river via Lake Cachuma. The mountain is named for a thin grove of Coulter pines located on the summit.
The mountain is reached by the Santa Cruz National Recreation Trail, and is a popular day hike and mountain biking route for residents of Santa Barbara during the winter months. There is a camp at Happy Hollow Spring near the summit.〔
The rocks of the lower slopes of the mountain comes from the Franciscan Assemblage, which creates serpentine soils that support a unique chaparral ecosystem. Large deposits of dark-red cinnabar are exposed above ground. The middle slopes of the mountain are dominated by the Espada Formation. The summit largely consists of Matilija Sandstone. There is a small band of Temblor Formation, a Great Valley Sequence unit usually found much farther north, encircling the high ridge of the mountain. North slope outcrops consist largely of Espada Formation rocks, with a band of serpentinite splitting the Espada section in half.〔Dibblee, T.W., and Ehrenspeck, H.E., ed., 1987, Geologic map of the San Marcos Pass quadrangle, Santa Barbara County, California: Dibblee Geological Foundation, Dibblee Foundation Map DF-08, scale 1:24,000〕
==References==


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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