The western side near the Pacific Ocean is sliding north relative to the eastern side inland, with no significant vertical movement.
The boundary of an earthquake refers to the area where two tectonic plates meet and release built-up stress in the form of seismic activity. This boundary can be a subduction zone, a transform fault, or a collision zone, depending on the type of plate interaction. Earthquakes often occur along these boundaries due to the movement and interaction of the tectonic plates.
California sits on the boundary of the Pacific Plate and the North American Plate, making it part of the San Andreas Fault system. The movement of these tectonic plates along the fault lines can lead to large, destructive earthquakes. Additionally, the state has a high population density and many critical infrastructure systems, increasing the potential impact of an earthquake.
Poo. :) Joking, just google it, Yahoo Answers has good answers about it Example: San Andreas is a transform fault with two plates sliding past each other. There is also a large bend in the fault (around the LA area). Basically, since these are large rocky plates and not water or something else slippery, they get stuck and tension builds up. When that tension is released as the plates slip, you get an earthquake. The bend makes it more difficult for the plates to slide past each other, which creates more tension, which is why there is such potential for the "big one."
St Andreas fault makes up the boundary between North American plates and the Pacific Ocean. It is 850 miles (1370 km) long, along the western coast of California from Cape Mendocino in the north to just south of the Salton Sea near the US-Mexico border.
A transform boundary occurs when tectonic plates slide past each other horizontally, causing earthquakes. On the other hand, a convergent boundary forms when two tectonic plates collide, leading to the formation of mountains, trenches, and volcanic activity.
The San Andreas fault is a transform boundary, where two tectonic plates slide past each other horizontally. In this case, the Pacific Plate and the North American Plate are moving in opposite directions, causing frequent earthquakes along the fault line.
a transform boundary.
it makes a fault, i think that's what it's called too Nope, it's a transform boundary. yup transform boundary
It is called transform boundaries.An earthquake
The San Andreas fault
Transform fault
The boundary of an earthquake refers to the area where two tectonic plates meet and release built-up stress in the form of seismic activity. This boundary can be a subduction zone, a transform fault, or a collision zone, depending on the type of plate interaction. Earthquakes often occur along these boundaries due to the movement and interaction of the tectonic plates.
California sits on the boundary of the Pacific Plate and the North American Plate, making it part of the San Andreas Fault system. The movement of these tectonic plates along the fault lines can lead to large, destructive earthquakes. Additionally, the state has a high population density and many critical infrastructure systems, increasing the potential impact of an earthquake.
Poo. :) Joking, just google it, Yahoo Answers has good answers about it Example: San Andreas is a transform fault with two plates sliding past each other. There is also a large bend in the fault (around the LA area). Basically, since these are large rocky plates and not water or something else slippery, they get stuck and tension builds up. When that tension is released as the plates slip, you get an earthquake. The bend makes it more difficult for the plates to slide past each other, which creates more tension, which is why there is such potential for the "big one."
St Andreas fault makes up the boundary between North American plates and the Pacific Ocean. It is 850 miles (1370 km) long, along the western coast of California from Cape Mendocino in the north to just south of the Salton Sea near the US-Mexico border.
Tectonic plates shifting around while bumping into another tectonic plate. When the plates slide pass each other, it creates a transform boundary which makes earthquakes.
Tectonic plates shifting around while bumping into another tectonic plate. When the plates slide pass each other, it creates a transform boundary which makes earthquakes.