Type of Boundary Description/Features of Plate Boundary Example Diverging Boundary Notes Lithosphere is lifted and spread apart by convection currents Magma flows into crack and solidifies New crust being made at boundary Process repeats Effects Sea Floor Spreading Submarine mountain ranges Earthquakes, volcanic activity Widening of ocean basins Mid – ocean ridge Notes continental plate arches upward from convection current and pulls apart to form a rift with faulting (cracks) the blocks slide downward streams and rivers fill in to make a linear lake, this may eventually lead to a new ocean basin East Africa Rift, The Red Sea Oceanic Diverging Boundary Continental Effects-a rift valley occupied by a linear lake or shallow arm of the ocean, earthquakes occur along the faults, volcanic activity sometimes occurs within the rift valley Sliding (Transform)Boundary Two plates slide against each other in a sideways motion. As two plates slide past one another, in a transform boundary, neither plate is added to at the boundary, nor destroyed. The fracture formed between the two plates is referred to as a fault line The result of two massive plates pushing against one another is that massive amounts of energy build up. Occasionally this energy is released suddenly in the form of large earthquakes. California's San Andreas Conversion Boundary Continent – Continent Notes powerful collision occurs deformed rock, folding and faulting of plates 100’s of miles into the plate Himalaya Mountains; Ural Mountains Effects-intense folding, broad folded mountain range, earthquake activity, shortening and thickening of the plates in the collision zone 1. Conversion Boundary Ocean – Continent Notes thinner, more dense oceanic plate is overridden by the thicker, less dense continental plate (subduction). Ocean trenches occur at the zone of subduction at depths of 100 miles, partial melting begins, magma chambers form and may rise and break through the crust to form volcanoes Volcanic arc chains onshore (EXAMPLE: Andes, Cascades) Effects- earthquakes along the continental margin, ocean trench offshore, volcanic eruptions inland Conversion Boundary Ocean – Ocean Notes one oceanic plate will subduct, remelt at depths near 100 miles; magma chambers that are produced may start to rise and break through the surface to form a volcano; the cone will be below sea level but may eventually grow higher; produces an island chain and in time the islands grow larger and an elongated landmass is created Effects- earthquakes, oceanic trench, volcanic islands Japanese Islands, Aleutian Islands