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Three Fingers Rock

From Oregon Hikers Field Guide

Looking to Three Fingers Rock from the north on McIntyre Spring Road (bobcat)
Summit register on East Finger (bobcat)

Description

Along with Mahogany Mountain, the Three Fingers caldera (15 1/2 million years before the present), of which this rocky prominence is merely a component, is responsible for the rhyolite formations in nearby Leslie Gulch and the Honeycombs. These rhyolite flows came in association with the Columbia River Basalts, which flooded this area of southeastern Oregon and southwestern Idaho.

The East Finger of Three Fingers Rock is the easiest scramble, suitable for kids with a bent for adventure. The Middle Finger is more of a short technical ascent, with exposure and loose rock. The West Finger is a steeper scramble. If you’ve brought binoculars, scan the surrounding countryside for mustangs and bighorn sheep. Golden eagles have also been known to nest on Three Fingers Rock.


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Oregon Hikers Field Guide is built as a collaborative effort by its user community. While we make every effort to fact-check, information found here should be considered anecdotal. You should cross-check against other references before planning a hike. Trail routing and conditions are subject to change. Please contact us if you notice errors on this page.

Hiking is a potentially risky activity, and the entire risk for users of this field guide is assumed by the user, and in no event shall Trailkeepers of Oregon be liable for any injury or damages suffered as a result of relying on content in this field guide. All content posted on the field guide becomes the property of Trailkeepers of Oregon, and may not be used without permission.