The evidence of the theory of continental drift can be found on the edges of the tectonic plates. For example, the boundary of the African Plate and the Eurasian plate is in the Mediterranean Sea, just south of the island of Crete. At this boundary, scientists have observed that the Eurasian Plate is sliding under the African Plate at a rate of three to four centimeters per year as the African Plate drifts north
The most studied <span>transform fault in the world
is "San Andrea's fault".
The point where two plates slide with one another i called Transform Plate Boundaries. The
fracture zone which makes a transform plate boundary is known
as a <span>transform fault.</span>
<span>"San Andrea's fault" runs for around 1200 km
through California (A rough estimate). </span></span>
