Juan De Fuca Plate. Here the san andreas merges. Your left hand represents an oceanic plate called juan de fuca, ninety thousand square miles in size.
The place where they meet is the cascadia subduction zone. The juan de fuca plate, lying east of the ridge system, forms an actively convergent margin with the north american plate.
The Juan De Fuca Plate, East Of This Spreading Centre, Is Subducting Under The North.
Evolution and hydration of the juan de fuca crust and uppermost mantle:
For Example The Juan De Fuca Plate Is Actually Three Separate Plates (Gorda, Juan De Fuca, And Explorer) That All Move In The Same General Direction But At Slightly Different Rates.
The cascadia subduction zone (csz) megathrust fault is a 1,000 km long dipping fault that stretches from northern vancouver island to cape mendocino california.
The Juan De Fuca Plate Between Its Northern And Southern Ends Has Few Earthquakes, Indicating That Internal Deformation Is Less Important There.
Images References :
The Juan De Fuca Microplates Are Believed To Be The Last Remaining Fractured Portions Of The Farallon Plate In The Continental U.
19.1, the juan de fuca and gorda segments.the third, the explorer.
Now Slide Your Left Hand Under Your.
It separates the juan de fuca and north america.
Evolution And Hydration Of The Juan De Fuca Crust And Uppermost Mantle:
