Tricouni Peak is a mountain located south of Cypress Peak on the Squamish-Cheakamus divide within the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada.

According to Tom Fyles himself,[3] "Tricouni Mountain was the name suggested for the peak, as from a distance it had the appearance of three cones".

[5] Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall.

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