Mahogany Mountain

This article is about a mountain in the Owyhee Mountains. For the mountain in the Wasatch Range, see Mahogany Mountain (Utah).

Mahogany Mountain
Leslie Gulch rock spire, Mahogany Mountain, Oregon. Photo: BLM (2008).
Highest point
Elevation	6,526 ft (1,989 m) NAVD 88[1]
Prominence	1,892 ft (577 m)[2]
Coordinates	43°14′06″N 117°15′21″W[1]
Geography
Mahogany Mountain Location in Oregon Show map of Oregon Mahogany Mountain Mahogany Mountain (the United States) Show map of the United States
Location	Malheur County, Oregon, U.S.
Parent range	Owyhee Mountains
Topo map	USGS McCain Creek
Geology
Last eruption	15.5 million years ago

Map showing location of Mahogany Mountain and the caldera.

Aerial photograph of Mahogany Mountain airport (1JY2), Oregon

Mahogany Mountain is an ancient caldera volcano on the border of Oregon and Idaho, in Malheur County and Owyhee County, respectively. While its early history is largely unknown, its last eruption was probably 15.5 million years ago. This eruption ejected layers of rhyolite and produced tuff, creating formations of rock in the Leslie Gulch.

Nearby features include the Owyhee River, historically used as a fishing and camping ground for early Native Americans. The climate of the area tends to be extreme; that is, it is cold in the winter and hot in summer. Sparse vegetation is present, including shrubs and patches of juniper.

Geography and geology

A part of the Basin and Range Province, the volcano's most recent eruptive activity dates to approximately 15 million years ago (the Miocene), forming during a period of active volcanism including eruptions of ignimbrite and ash. It formed around the same time as Three Fingers, Castle Peak, and three other volcanoes. Today the volcano appears gnarled due to erosion and is topped by pine forests.[3]^[verification needed] The caldera is narrow and shaped like a ridge, with precipitous slopes and an escarpment on the northwest flank. It consists of rhyolite tuff and sedimentary layers.[4]

Leslie Gulch lies within the depression of the volcano. Layers of ash and tuff are evident in the formation, and leftover volcanic rocks sit in it as well.[5] The gulch features an array of rock formations and ash erupted from the volcano approximately 15.5 million years ago.[6]

History

The nearby Owyhee River was utilized by Native Americans as early as 5,000 years before European habitation of the area. It served as a source of food, both for fishing and hunting, and the natives often camped along its banks.[6]

Climate and vegetation

The area by the volcano features cold winters and hot summers, with only 25 centimeters (10 in) of rainfall each year. Steppe-like shrubs make up the majority of the vegetation, though juniper is present in patches. There are 64 known mammalian species in the area.[7]

References

1. "Mahogany Mountain". NGS Data Sheet. National Geodetic Survey, National Oceanic and Atmospheric Administration, United States Department of Commerce.
2. "Mahogany Mountain, Oregon". peakbagger.com. Retrieved 2021-12-03.
3. Bishop, p. 158. (incomplete ref)
4. Warman, Philip Creveling (1903). Catalogue and Index of the Publications of the United States Geological Survey 1901 to 1903. United States Government Printing Office. p. 14.
5. Barnes, Christine (2004). Only in Oregon: Natural and Manmade Landmarks and Oddities. Farcounty Press. ISBN 978-1560372929. p. 67.
6. "Leslie Gulch" (PDF). Bureau of Land Management. 2010-05-06. Retrieved 2010-05-09.
7. Verts, B.J.; Carraway, Leslie N. (1998). Land Mammals of Oregon. University of California Press. ISBN 978-0520211995. p. 33.

External links

• "Mahogany Mountain". Geographic Names Information System. United States Geological Survey, United States Department of the Interior.