A transform boundary.
The San Andreas Fault is a transform plate boundary between the Pacific and North American Plates.
The San Andreas fault is part of the transform boundary that marks the point where the North American and Pacific tectonic plates meet.
The San Andreas fault is part of a destructive plate boundary. The fault itself is undergoing transverse movement.
TRANSFORM
Transform
Haiti is an example of a transform boundary, because the left side of Haiti (where Port Au Prince is located) is the boundary of a tectonic plate that is sliding past another tectonic plate going in the other direction (Transform boundary). Because of this, a lot of tension builds up between the two plates, until an earthquake occurs when they slide past each other. (Keep in mind that tectonic plates move very little, and it took Pangea 250 million years to become what we see the world as now).Think, today (this is recent news as of January 20, 2010) when you turn on the news you hear of the devastating effects of a 7.0 earthquake in Haiti. This was because of the tectonic plates going in opposite directions against each other, i.e. the transform boundary!The most famous example is the San Andreas Fault in California.Transform boundaries -- where crust is neither produced nor .... one of the most visible and spectacular consequences of plate tectonics. ... However, a few occur on land, for example the San Andreas fault zone in California.
when two plates are slide past one another an example is the san Andreas fault California which is the boundary between the north America and pacific plates
Earthquakes occur along the San Andreas Fault because of the tectonic plates. When the plates slip or shift, an earthquake happens.
earthquakes along the San Andreas fault in California
There are 3 main types of faults 1. Normal 2. Strike slip 3. Reverse(Thrust) In a normal fault the foot wall stays in place while the hanging wall moves DOWNWARDS In a strike slip the tectonic plate(s) slide past each other horizontally In a reverse fault, the hanging wall gets pushed UPWARDS over the foot wall (The pictures are in the reverse order)
The San Andreas Fault is a transform plate boundary.
Yes, for example the San Andreas Fault is a plate boundary.
It is on the San Andreas fault.
A transform boundary.
It is on a transform fault boundary.
The San Andreas fault is a transform plate boundary.
The San Andreas fault is not connected to the North American or Pacific Plates but is merely the boundary between the two where they make contact. As such, it is a fault as well as a plate boundary.
San Francisco is located on the boundary between the Pacific Plate and the North American Plate, known as the San Andreas Fault. This is a transform plate boundary, where the two plates are sliding past each other horizontally.
The San Andreas fault is a right-lateral (dextral) strike-slip fault which marks a transform (or sliding) boundary between the Pacific Plate and the North American Plate. In essence the plate boundary is destructive rather than constructive but at present the energy is directed at moving the Pacific Plate in a generally northerly direction, parallel with the coastline.
The name of the transform boundary that separates the Pacific Plate and the North American Plate is known as the San Andreas Fault. It is the site of many of the earthquakes that plague Southern California.
The San Andreas Fault is part of a transform plate boundary.
Divergent plate boundary: Mid-Atlantic Ridge. Transform plate boundary: San Andreas Fault.