Neither production nor consumption of lithosphere occurs at these boundaries.
YES. A Strike-slip fault is usually a transform boundary.
The transform boundary is also known as the transform fault. This type of boundary is commonly found in deep ocean floors and are typically involved in movement which aids in relieving tension in the layers of the earth.
The Alpine Fault is a geological right-lateral strike-slip fault. It forms a transform boundary, so yes.
It is a transform plate boundary.
Transform boundary / conservative boundary.
A transform fault boundary is a conservative plate boundary. This is what gets rid of lithosphere.
YES. A Strike-slip fault is usually a transform boundary.
A strike-slip or transform fault.
It is a right-lateral strike-slip fault
It's a transform boundary between two plates. The resultant fault of a transform boundary.
It's a transform boundary between two plates. The resultant fault of a transform boundary.
A transform boundary.
A transform fault boundary is a type of tectonic plate boundary characterized by horizontal sliding of plates past each other. This movement can cause earthquakes as the plates grind against each other. An example of a transform fault boundary is the San Andreas Fault in California.
It's a transform boundary between two plates. The resultant fault of a transform boundary.
It's a transform boundary between two plates. The resultant fault of a transform boundary.
The San Andreas fault in California is a major transform boundary or fault, as is New Zealand's Alpine fault and North America's Queen Charlotte fault.
the san Andreas fault