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The answer is mountain ranges
This will form a convergent boundary.
At a convergent plate boundary one of the features is mountains. Volcanoes are also typical.
Fault Lines. A transform boundary connects two diverging boundaries, creating a fault line. ... Trenches. Trenches are geological features formed by convergent boundaries. ... Volcanoes. ... Mountain Ranges. ... Ridges. ... Rift Valleys.
It's homoplasy.
The Himalayas, a mountain range at the northern edge of the India plate
The answer is mountain ranges
This will form a convergent boundary.
The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.
The Himalayan mountains.
They are where mid-ocean ridges occur. Island arcs are common features of convergent boundaries where two ocean plates meet. The boundary where two plates slide past each other, is a transform boundary. The density of the plates, is important at subduction zones, where the denser plate sinks below the less-dense plate, which is also a feature of convergent plates. Tectonic plates are part of the lithosphere, which floats on the asthenosphere.
If you're looking at a convection zone along coastal areas you'll look for subduction zones, trenches, accretionary wedges, volcanic activity, seismic activity, mountain building activity, island creation (think Japan), and possibly exotic terrains to name a few. If you're looking at convergent boundaries on continental land you'll generally find mountain building (think Himalayas), faulting, and seismic activity; not as much volcanism here since the crust is even think to support the mountain zone. There isn't specifically one feature to be found because you have three options for convergent boundaries: continental-oceanic, continental-continental, and oceanic-oceanic.
At a convergent plate boundary one of the features is mountains. Volcanoes are also typical.
If you're looking at a convection zone along coastal areas you'll look for subduction zones, trenches, accretionary wedges, volcanic activity, seismic activity, mountain building activity, island creation (think Japan), and possibly exotic terrains to name a few. If you're looking at convergent boundaries on continental land you'll generally find mountain building (think Himalayas), faulting, and seismic activity; not as much volcanism here since the crust is even think to support the mountain zone. There isn't specifically one feature to be found because you have three options for convergent boundaries: continental-oceanic, continental-continental, and oceanic-oceanic.
Converging plates come together. They converge together. Diverging plates come apart.
Fault Lines. A transform boundary connects two diverging boundaries, creating a fault line. ... Trenches. Trenches are geological features formed by convergent boundaries. ... Volcanoes. ... Mountain Ranges. ... Ridges. ... Rift Valleys.
In plate tectonics, a Divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other. These areas can form on the end of continents but eventually form ocean basins. Divergent boundaries within continents initially produce rifts which produce rift valleys. Therefore, most active divergent plate boundaries are between oceanic platesand are often called mid-oceanic ridges. Divergent boundaries also form volcanic islands which occur when the plates move apart to produce gaps which molten lava rises to fill. Thus creating a shield volcano which would eventually build up to become a volcanic island.