One plate is usually subducted under the other forming a trench. The Marianas Trench, for instance, is over 30,000 feet deep. Underwater volcanoes may also be formed from the subduction, and they may continue to grow in height until they jut from the surface of the water.
Continent to Continent CollisionsWhen two continents converge, their point of contact will be uplifted due to the compression forces exerted on the rock. A series of fold mountains may result. As an example of mountain ranges that were formed like this look to the Alps.
Almost like they look now. Plate movement is extremely slow, about the rate of fingernail growth.
Its surface would look like that of the Moon, Mars or Mercury all of which do not have tectonic plates and a fixed crust.
The oceanic crust is made out of mostly basalt.
A place where two plates slip past each other, moving in opposite directions
Ridge
When plates move towards each other it is called a convergent boundary. The two types of plates converging depends on what happens. When it is oceanic/oceanic, both plates subduct (go downward), leading to the creating of trenches found at the depths of the ocean. When an oceanic plate converges with a continental plate, the more dense oceanic plate subducts under the continental plate, again creating trenches, and also leading to the destruction of the ocean floor. When continental plates converge, they tend to smash up and rise, creating mountains. When plates move apart, it is called a divergent boundary. When oceanic plates move apart, magma rises, cools, and solidifies to create new ocean floor. This, along with continental/oceanic convergence, accounts for seafloor spreading. When two continental plates diverge, the area left between them slowly turns into an ocean. For an example of this type of ocean, look at the Red Sea.
well that's easy just look up on divergent boundaries and it states the main features,which are two tectonic plates,ocean plates and mid-oceanic ridges.
they are the giant plates underneath all the continents
Continent to Continent CollisionsWhen two continents converge, their point of contact will be uplifted due to the compression forces exerted on the rock. A series of fold mountains may result. As an example of mountain ranges that were formed like this look to the Alps.
Actually I have found dinner plates that are square. They look really cool. Anyway maybe when they were first designed they wanted it to look like a never ending circle of food. Answer I like square plates, but suspect that food stays on round plates better.
its just like a cracked hard boiled egg the shell are the plates and the egg while is the mantle. the tectonic plates move on top of magma which is the mantle. they move due to convection currents which occur within the mantle the oceanic plates sub duct in to the mantle while the continental plates don't as they are not as dense. they basicly freeze and move sideways and then descend back in to the mantle again just very slowly. just like a massive jigsaw puzzle. if you get a hard boiled egg and crack it and wiggle it around it might become clear!!!
You look fat when seated because your mass tends to converge in one small area.
An Omega necklace is made to look like a chain. It is however, constructed out of plates and not chain links. The plates are worked together in such a way that it gives the appearance of a chain.
Almost like they look now. Plate movement is extremely slow, about the rate of fingernail growth.
A tectonic plate is a piece of lithosphere. The lithosphere is the outer, rigid "shell" of the earth. A plate moves along the asthenosphere (layer below the lithosphere) and can be either continental or oceanic lithosphere. Volcanic activity and earthquakes are common at boundaries of individual plates.
well this is what I do look at licence plates and look where they are from..... 1 advise is only do this if you like the states or know them all :)