The underlying rock of the Central Coast Range are the igneous rocks from the Siletz River Volcanics of the Paleocene age. These formations consist mainly of pillow basalt, large lava flows, tuff-breccia, and sills. The entire Oregon Coast Range overlies a convergent tectonic margin that interacts with the Juan de Fuca Plate that is being sub-ducted beneath the North America tectonic plate.... Read More