A few things could happen, If both plates were both land, then they would buckle and fold and form high Mountains like with India and South western China forming Himalayas, But if one plate is a oceanic plate and the other is a land plate, then the oceanic plate is more dense and would slide under the lighter land plate and melt, then magma is formed from the oceanic plate and then rises to the top land plate the magma would come though and form volcanoes. Like the west coast of USA. copy and paste for a picture>
http://images.Google.com/imgres?imgurl=http://ase.tufts.edu/cosmos/pictures/Explore_figs_5/Chapter4/Fig4_14.jpg&imgrefurl=http://ase.tufts.edu/cosmos/print_images.asp%3Fid%3D4&usg=__Oyga2Y003IlkK3hqvr443noUqfM=&h=515&w=416&sz=37&hl=en&start=1&sig2=N1MEpwdc23QY6o0gLym7dg&um=1&itbs=1&tbnid=72xihO4NYhEA9M:&tbnh=131&tbnw=106&prev=/images%3Fq%3Dconverging%2Bplates%253F%26um%3D1%26hl%3Den%26tbs%3Disch:1&ei=chCZS9H0IMOWtgfwk5GwCQ
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
At divergent boundaries, mid-ocean ridges are formed as tectonic plates pull apart. At converging boundaries, various geologic features are formed such as trenches, mountains, and volcanic arcs, depending on the type of plates involved (oceanic vs. continental).
A convergent boundary is a tectonic plate boundary where two plates move towards each other and collide. This collision can result in the formation of mountain ranges, deep-sea trenches, and earthquakes due to the intense pressure and friction created by the converging plates. Subduction zones, where one plate is forced beneath the other, are common at convergent boundaries.
A mountain is an example of a possible result of converging plate boundaries. An actual example of a converging plate boundary would be the Indian-Eurasian Plate Boundarywhich is creating the Himalayan Mountain Range. Other convergent plates can create trenches such as the Mariana Trench, which is the lowest place on the surface of the Earth.
Mountains formed by continental plates colliding are known as fold mountains. These mountains are created when the intense pressure from the converging plates causes rocks to buckle and fold, resulting in uplifted and folded mountain ranges. Examples of fold mountains include the Himalayas and the Alps.
The type of tectonic forces that create mountains are called converging plates. As two continental plates push together, the stress forces them both upwards. Because of this the Himalayas are still growing.
The plates come together
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
it means that they are converging
Converging plates come together. They converge together. Diverging plates come apart.
Converging plates come together. They converge together. Diverging plates come apart.
No. Mount Mazama is associated with a subduction zone, which is formed by converging plates.
The energy spews out Lava
2 to 3 inches per year.
Many earthquakes are produced act converging plates. However a number of strong earthquakes also take place at transform boundaries where plates slide past one another, neither converging nor diverging. On rare occasions strong quakes will take place within a plate.
At a converging boundary, plates can collide and create subduction zones. This can lead to the formation of mountain ranges, deep ocean trenches, and earthquakes. The pressure and friction from the plates can also cause volcanic activity.
Around converging tectonic plates, you would find features such as mountain ranges, deep ocean trenches, and volcanic arcs. These features are a result of the intense forces created by the plates colliding and interacting with each other.