volcanic activity and growing mountain ranges
Transform faults are strike-slip faults that occur at the boundary between two plates of the earth's crust and do not produce or destroy lithosphere. Divergent faults produce new sea floor, while convergent faults occur when two plates collide underneath and create underground mountains.
Earth does not produce water. The water currently on Earth is believed to have been here since shortly after Earth formed. Water on Earth goes through cycles between the atmosphere, the oceans, and glaciers.. Some water vapor is released by volcanoes, but this is balanced by water carried into the mantle at subduction zones.
Supercells can occur in most parts of the world. They usually form along some sort of a boundary such as a cold front or a dry line. You need strong wind shear to produce supercells in place of ordinary thunderstorms.
Regional metamorphism takes place in large areas around plate boundaries.
Divergent, since when the plates split, magma reaches the surface. Convergent, since it is where volcanoes are typically formed. Transform, since trough any crack magma can come out too.
Convergent boundaries that produce maintains are called subduction zones.
Hurricanes are produce by weather phenomena, though geologic features can influence them.
It depends
Often, a divergent boundary within a continent will produce rifts, which will produce rift valleys. A divergent boundary may also be referred to as an extensional boundary, a constructive boundary, or a divergent plate boundary.
normal reverse or strike slip
There are two basic types of convergent boundary. The first is a subduction zone, which occurs at a collision between two plates carry oceanic crust or one carrying continental and once carrying oceanic crust. In such a collision, one oceanic plate will subduct under the other and sink into the mantle. Such a collision produces volcanoes on the overriding plate and will produce mountain ranges on a continent. The other type of convergent boundary occurs when two continent collide. These collisions produce high mountains but not volcanoes. No subduction occurs as continental crust is not dense enough to sink into the mantle.
convergence plate boundary, where tectonic plates move towards each other and collide, leading to subduction zones which are highly constructive regions of volcanoes. Volcanoes also form at divergent plate boundaries. A good example being the numerous Icelandic volcanoes which have formed over he Mid Atlantic Ridge.
A slip zone is more likely to produce a sudden, shocking quake, while a subduction boundary is more likely to vent gases. The actual effects may not vary that much on the ground, but could make a big different if the epicenter is under the ocean floor. Because a slip zone quake doesn't displace a whole lot of water, it tends not to create tsunamis.
hot spots
The landforms that are formed at a transform boundary forms features such as fault lines and oceanic fracture zones. Fault lines are also known as strike slip faults. They produce powerful earthquakes.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
The huge sections are called tectonic plates. When they collide this is called a convergent boundary. Usually one plate is oceanic and one is continental, and the oceanic plate is forced down in a subduction zone. This forces the continental plate up, giving rise to mountains and often volcanoes.