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Boring Lava Field

The Boring Lava Field (also known as the Boring Volcanic Field)[3] is a Plio-Pleistocene volcanic field with cinder cones, small shield volcanoes, and lava flows in the northern Willamette Valley of the U.S. state of Oregon and adjacent southwest Washington. The field got its name from the town of Boring, Oregon, located 12 miles (20 km) southeast of downtown Portland. Boring lies southeast of the densest cluster of lava vents. The zone became volcanically active about 2.7 million years ago, with long periods of eruptive activity interspersed with quiescence. Its last eruptions took place about 57,000 years ago at the Beacon Rock cinder cone volcano; the individual volcanic vents of the field are considered extinct, but the field itself is not.

Boring Lava Field

4,061 feet (1,238 m)

57,000 years ago[3][4]

The Boring Lava Field covers an area of about 1,500 square miles (4,000 km2), and has a total volume of 2.4 cubic miles (10 km3). This region sustains diverse flora and fauna within its habitat areas, which are subject to Portland's moderate climate with variable temperatures and mild precipitation. The highest elevation of the field is at Larch Mountain, which reaches a height of 4,055 feet (1,236 m).


The Portland metropolitan area, including suburbs, is one of the few places in the continental United States to have extinct volcanoes within a city's limits, and the Boring Lava Field plays an important role in local affairs, including the development of the Robertson Tunnel, recreation, and nature parks. Because of the field's proximity to densely populated areas, eruptive activity would be a threat to human life and property, but the probability for future eruptions affecting the region is very low. The field may also influence future earthquakes in the area, as intrusive rock from its historic eruptions may affect ground movement.

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Recreation[edit]

Trails in the city of Gresham travel over parts of the Boring Lava Field and its cones. Mount Tabor and Powell Butte are better known for their recreational uses than other cones;[103] Powell Butte Nature Park has 9 miles (14 km) of trails.[40] The Mt. Tabor Park is open to bicyclists and pedestrians from 5 a.m. through midnight and to motorized vehicles from 5 a.m. through 10 p.m. each day, except for Wednesdays when the park roads are not open to automobiles.[43] The Hogan Butte Nature Park offers views of Mount Adams, Mount Hood, Mount Rainier, and Mount St. Helens,[104] as well as running trails and sites for picnicking.[44]


In addition to the nature park on Hogan Butte, a number of smaller cinder cones are also publicly accessible. The Gresham Saddle Trail traverses Gresham Butte and Gabbert Butte, running for 3.3 to 3.7 miles (5.3 to 6.0 km). The trail is considered to be of moderate difficulty, and it offers no amenities. It includes the Gabbert Loop Trail, which extends for 1 mile (1.6 km) through forests of maples, alders, ferns, and firs.[103]

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[a] Evarts et al. (2009) list only 80 centers but acknowledge there are likely more buried vents;[80] Le Corvec et al. (2013) list 88 volcanic centers at Boring Lava Field.[105]

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[b] Low-K is a geological term used to describe lava with low amounts of potassium, while high-K describes lava enriched in potassium.

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[c] Refractory refers to any material that does not easily convert from liquid to gas via the process of vaporization, which includes elements and compounds made from metals.

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USGS Map of Boring Lava Field

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