Now you see a vertical slice through the Earth along the red line on the previous web page and which crosses the plate boundary in this region.
We can see that the earthquake locations in the Earth, as shown by the colored dots, provide evidence of a convergent plate boundary with oceanic lithosphere of the Pacific Plate subducting (sinking) below the North American Plate. The shallow earthquakes in the upper right corner are located near the Aleutian Trench, which marks the boundary between the North American and Pacific plates along the sea floor. The dipping region of earthquakes shown here is called the Wadati-Benioff Zone or just Benioff Zone. The thick white lines outline the pieces of lithosphere in this region.
So even the deep earthquakes, in this particular
case down to 200 kilometers, are in the lithosphere -- lithosphere
sinking back into the Earth along a convergent plate boundary.
We can also see earthquakes
below the volcanic arc caused by the movement of molten rock or by
the sinking of the crust in this region.
On the expedition worksheet, make a drawing of the earthquake distribution with an outline of the subducting Pacific Plate and the overriding North American plate.