Stage 1
Convections in asthenosphere cause 2 plates to slide past one another; plates can move in opposite directions or in same direction at different speeds
Stage 2
San Andres Fault in California marks conservative plate boundary between Pacific Plate and North American plate
Both are moving NW at different speeds
Stage 3
Huge plates slide past one another and can become stuck (tension builds up)
Stress relieved as seismic waves during an earthquake event
Stage 4
Conservative Plate boundary has no volcanic activity only earthquake
1906 7.8 magnitude earthquake in San Francisco
Draw a conservative plate boundary
Yes