San Francisco, Sacramento and the Sierra Nevada are on the North American Plate. However, earthquakes are very common. They can also move in the same direction, just at different speeds.Earthquakes can occur here due to the plates becoming stuck every so often, hence generating earthquakes. Destructive. Here, the 2 plates slide past each other in opposite directions, generating friction as they do. A conservative plate boundary, which is sometimes called a ‘transform plate margin’, occurs when plates move alongside each other, in the opposite direction or in the same direction at different speeds. Conservative plate boundaries occur in few places. San Andreas Fault (Pacific + …

What is the San Andreas Fault? Conservative plate boundary. Most transform faults are underwater, but the San Andreas Fault is one of the few that is exposed on land. What is a conservative plate boundary and what's an example?

San Diego, Los Angeles and Big Sur are on the Pacific Plate. Transform fault boundaries consist of two plates sliding against each other in a horizontal motion. Transform faults are found here. In a conservative plate boundary, no plate materials are constructed or destroyed. Following an earthquake along a conservative plate boundary, there are often aftershocks as the additional stress on other areas along the fault are relieved. Destructive plate boundaries also know as convergent or tensional boundaries. Vulcanicity is rare as less magma rises along lines of weakness to the earth's surface. The friction between these two plates as they slide past one another is the cause of the earthquakes in the San Francisco Bay area. San Francisco is located on the San Andreas Fault, which is the boundary of the Pacific and North American plates. Earthquakes at conservative plate boundaries can be very destructive as they occur close to the Earth’s surface. The San Andreas Fault exemplifies a transform fault plate boundary. 10 Facts about San Andreas Fault The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through California. It slices California in two from Cape Mendocino to the Mexican border. Figure 6- Diagram of collision plate boundary The San Andreas Fault is the sliding boundary between the Pacific Plate and the North American Plate. One famous conservative boundary is the San Andreas Fault in San Francisco, North America. When plates slip past each other creating sudden movement the …

A destructive boundary happens when an oceanic and a continental plate meet, and the oceanic plate is forced under the lighter continental plate. The San Andreas Fault is an example of a conservative plate boundary. Plate Boundaries (Fault Lines) Types Of Boundaries. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal).