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The san Andreas fault is a transform boundary between two plates. The resultant fault of a transform boundary is a strike-slip fault. The North American plate and the Pacific â¦plate are both moving vertically in different directions.
For example, the San Andreas Fault in California is a continental transform boundary. Along this boundary, frequent, shallow earthquakes occur (like the famous 1906 and 1989 San Francisco earthquakes), but there is little associated volcanic activity or topographic relief (see Figure 7).