uneven
The movement of a uniform boundary is consistent and does not change in direction or speed. On the other hand, the movement of an uneven boundary can vary in its direction and speed as it interacts with different environments or obstacles.
At a transform boundary, plates slide past each other horizontally in opposite directions. This movement is called lateral sliding. It can create earthquakes as the plates become stuck and then suddenly release along the boundary.
The San Andreas Fault is associated with a transform plate boundary. It marks the boundary between the Pacific Plate and the North American Plate, where they are sliding past each other horizontally. This movement can cause earthquakes along the fault line.
When two tectonic plates slide past each other horizontally, the boundary between them is called a transform boundary. This type of boundary is characterized by lateral movement along fault lines, such as the San Andreas Fault in California.
A fault generally occurs along a transform boundary where tectonic plates slide past each other horizontally. The movement of these plates along the fault can cause earthquakes.
A transform plate boundary does not create or destroy crust. Instead, adjacent plates slide horizontally past each other. This movement can cause earthquakes along the boundary without significantly changing the amount of crust.
becease its cool
UnevenEach plate has several boundaries and exerts pressure in all directions, and the movement is rarely close to uniform.
UnevenEach plate has several boundaries and exerts pressure in all directions, and the movement is rarely close to uniform.
This condition is called an earthquake.
If there is movement of rock along this crack, then it is called a fault.
A transform boundary. This is where tectonic plates slide horizontally past each other in opposite directions. This movement can cause earthquakes along the boundary.
"Uneven cleavage"
A transform boundary occurs when two tectonic plates slide past each other horizontally. This movement causes earthquakes along the boundary due to the friction and pressure from the plates interacting.
When two boundaries move in opposite directions, it is called a transform boundary. The motion at this boundary is typically horizontal sliding or shearing, where the two plates slide past each other. This movement can result in earthquakes along the boundary.
This is a transform plate boundary. At transform boundaries, plates slide past each other horizontally. This movement can cause earthquakes due to the stress and friction along the boundary.
Haiti is located on a strike-slip plate boundary, specifically on the boundary between the North American Plate and the Caribbean Plate. This boundary is characterized by horizontal motion along a transform fault, where the plates slide past each other. The movement along this boundary has the potential to generate earthquakes, such as the devastating 2010 earthquake in Haiti.
No. it was along a convergent boundary.