a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
Transform boundaries create strike-slip faults, where tectonic plates slide past each other horizontally in opposite directions. These faults are characterized by lateral motion rather than vertical displacement.
Most transform faults occur in the oceanic crust, particularly in between tectonic plates in areas such as mid-ocean ridges. These faults are characterized by horizontal movement along the fault line, accommodating the lateral displacement of the plates. An example of a well-known transform fault is the San Andreas Fault in California.
Transform boundaries create earthquakes as tectonic plates slide past each other. These boundaries also form faults where rocks are broken and displaced. Additionally, transform boundaries can lead to the formation of linear features such as ridges or valleys on the Earth's surface.
Crust is neither formed nor destroyed at transform plate boundaries. At these boundaries, tectonic plates slide past each other horizontally, resulting in earthquakes and faults but no new crust is created or destroyed.
near subduction zones
Strike-slip faults are common at transform boundaries because the plates are sliding past each other horizontally in opposite directions. This movement creates shear stress along the faults, leading to the formation of strike-slip faults. The San Andreas Fault in California is a well-known example of a transform boundary with a prominent strike-slip fault.
Transform Boundaries
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
Transform boundaries produce strike-slip faults. These faults occur when two tectonic plates slide past each other horizontally. Examples of transform boundaries include the San Andreas Fault in California.
Transform faults I believe.
Boundaries, or faults, are locations on the edges of plates, crustal masses that are very slowly moving atop the convective outer mantle (asthenosphere).At convergent boundaries, two crustal masses (plates) are pushing into each other. This can result in subduction, so may be a destructive boundary.At divergent boundaries, two masses of rock are pulling away from each other. This can be a constructive boundary when it produces rifting and seafloor spreading.At transform boundaries, or transform faults, rock masses move past one another. These are known as conservativeboundaries because crust is neither destroyed or created.(these can cause earthquakes when accumulated strain is released)
At transform boundaries, tectonic plates slide past each other horizontally. This movement can cause earthquakes due to the release of built-up stress along the boundary. Additionally, features such as strike-slip faults and transform faults are common at transform boundaries.
Transform boundaries create strike-slip faults, where tectonic plates slide past each other horizontally in opposite directions. These faults are characterized by lateral motion rather than vertical displacement.