Tensional stress
Tensional stress
divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.
Divergent plate boundaries typically produce smaller earthquakes compared to convergent plate boundaries, where tectonic plates collide. At divergent boundaries, tectonic plates move apart, creating new crust, which generally results in less intense seismic activity. In contrast, convergent boundaries often involve subduction, leading to significant stress accumulation and larger earthquakes. Therefore, the largest earthquakes are generally associated with convergent, rather than divergent, plate boundaries.
A compressional bounday is plate boundarys that are being compressed
Stress at a divergent plate boundary is called tensional stress. This stress creates pulling forces that lead to the plates moving away from each other, resulting in the formation of new oceanic crust.
Convergent on the western perimeter, divergent on the Easter perimeter.
Divergent
divergent boundary
Cool
It forms a convergent boundary with the South American Plate, divergent.
Convergent,Divergent, and Transform Boundaries
It forms a convergent boundary with the South American Plate, divergent.