mountain ranges and trenches
Compressional stress.
Convergent Plate Boundaries
Subduction, is when one plate is pushed down into the magma, by the other plate sliding over the top.
The lithosphere is broken up into what are called tectonic plates - in the case of Earth, there are seven major and many minor plates. The lithospheric plates ride on the asthenosphere. These plates move in relation to one another at one of three types of plate boundaries: convergent or collision boundaries, divergent or spreading boundaries, and transform boundaries. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates is typically at speeds of 50-100 mm/a.
Both involve tectonic plate moving relative to one another and help recycle oceanic crust. At divergent boundaries plates move away from each other and new crust is created. At most convergent boundaries oceanic crust is destroyed.Both of these boundary types produce volcanoes.
Compressional stress.
Convergent Plate Boundaries
They are divided by divergent, convergent AND transform boundaries.
Plate boundaries are places where two tectonic plates meet. There are three major types of plate boundaries. These are divergent, convergent, and transform plate boundaries.
Fault lines.
Convergent boundaries (plates moving toward each other, also called destructive boundaries), divergent boundaries (plates moving away from each other (sometimes called constructive boundaries), fault lines (sideways movement).
Convergent (or destructive): Where two plates are moving toward each other. Collisions between oceanic plates results in subduction of the more dense plate. Collisions between an oceanic plate and a continental plate may result in the subduction of the oceanic plate because oceanic plates are more dense than continental plates. Collisions between two continental plates results in uplift and mountain formation where neither plate subducts.Divergent (or constructive): Where two plates are moving away from each other. Divergent plate boundaries are the site of new crust formation, particularly at the mid-ocean ridges, where spreading plates are infilled with basaltic magma from the asthenosphere.Transform (or conservative): Where two plates slide (actually 'grind') alongside each other and neither plate subducts. Earthquakes are common at transform faults due to the grinding and snapping movements of the plates as they move.
Subduction, is when one plate is pushed down into the magma, by the other plate sliding over the top.
The lithosphere is broken up into what are called tectonic plates - in the case of Earth, there are seven major and many minor plates. The lithospheric plates ride on the asthenosphere. These plates move in relation to one another at one of three types of plate boundaries: convergent or collision boundaries, divergent or spreading boundaries, and transform boundaries. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates is typically at speeds of 50-100 mm/a.
Both involve tectonic plate moving relative to one another and help recycle oceanic crust. At divergent boundaries plates move away from each other and new crust is created. At most convergent boundaries oceanic crust is destroyed.Both of these boundary types produce volcanoes.
Volcanoes can form at three places-1. Divergent boundaries2. Convergent boundaries (oceanic-oceanic and oceanic-continental)2. Above hot spots
Intrafaith Boundaries are Boundaries within a single major faith..