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Roads End Point

From Oregon Hikers Field Guide

Revision as of 01:16, 5 July 2016 by Bobcat (Talk | contribs)

Roads End Point from the beach (bobcat)

Description

The convoluted headland between Roads End and the mouth of the Salmon River consists of two late Eocene (45 million years ago or so) formations. The Nestucca Formation, layers of sandstone and volcanic tuff, was overlaid by basalt flows. These flows once formed a barrier, which the onslaught of the ocean has breached to forms small caves and crater-like coves. Roads End Point is a basalt promontory with softer sandstone on either side that will continue to be eroded by the sea. In time, Roads End Point will become a sea stack.

The tide pools at the base of Roads End Point are some of the best on the Oregon Coast.

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Contributors

bobcat (creator)

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.

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