description Cayley Massif Overview
The Cayley Massif is a volcanic mountain complex located in the southern Coast Mountains of British Columbia, Canada. It forms part of the Garibaldi Volcanic Belt, which represents the northern extension of the Cascade Volcanic Arc. The massif is dominated by Mount Cayley, a highly dissected and potentially active stratovolcano. Featuring rugged, heavily glaciated terrain, the area is composed of volcanic rocks that originated during periods of eruptive activity in the Miocene and Pliocene epochs.
help Cayley Massif FAQ
Where is the Cayley Massif?
The Cayley Massif is in the southern Coast Mountains of British Columbia, Canada. It lies within the Garibaldi Volcanic Belt between the Squamish and Cheakamus river valleys.
Is the Cayley Massif an active volcano?
It is a volcanic complex rather than a single simple cone, with Mount Cayley as its dominant summit. Geological evidence in the wider Cayley volcanic field includes lava domes, stratovolcanic rocks, and eruptions that occurred after the last glacial period.
What is the highest peak in the Cayley Massif?
Mount Cayley is the highest and best-known summit in the massif, rising to roughly 2,400 meters. The complex also includes several other major volcanic peaks and ridges.
How old is the Cayley volcanic complex?
The broader Mount Cayley complex records volcanic activity over roughly 2.2 million years. It includes rock types ranging from basaltic andesite to rhyodacite.
explore Explore More
Reviews & Comments
Write a Review
Be the first to review
Share your thoughts with the community and help others make better decisions.
