a fault
When two crustal plates collide, they can form mountain ranges. The collision forces the crustal rocks to deform and buckle, leading to the creation of folded and uplifted mountain belts on the Earth's surface.
Crustal compression is the process where tectonic forces squeeze rock layers in the Earth's crust, causing them to deform and fold. This can lead to the formation of mountain ranges or fault lines as the rocks are pushed together and uplifted. Compression can occur at convergent plate boundaries where two tectonic plates collide.
They are geologic features because when the crustal plates move its makes cracks on earth the the mountains are one because everytime the crustal plates move it breaks the earths surface and the dirt and rocks start gathering together
dome
Fault
Well, mountains are formed mostly with folding and sometimes with volcanic eruptions. MOUNT EVERST was formed by the folding of the ocean. Folding is when the earth's crustal plates start to push together to form a mountain.
When the tectonic plates push together over a period of time, sometimes they jolt, like recently with Japan. However, most were far more violent than that, infact the Himalaya's are basically two plates that hit each other and went straight up.
Well, mountains are formed mostly with folding and sometimes with volcanic eruptions. MOUNT EVERST was formed by the folding of the ocean. Folding is when the earth's crustal plates start to push together to form a mountain.
They form volcanic mountains by heating magma that breaks through the crust. On the oceanic plates, these crustal hot spots can form chains of volcanic islands such as the Hawaiian Islands.
Three features along crustal plate boundaries are earthquakes, volcanoes, and mountain ranges. Earthquakes occur due to the movement of tectonic plates, volcanoes form at convergent boundaries where plates collide, and mountain ranges are often found at convergent boundaries where plates push against each other.
When crustal plates move toward each other, they can form convergent boundaries where one plate is forced beneath the other in a process called subduction. This can result in the formation of mountain ranges, deep ocean trenches, and volcanic activity in the area.
by two plates crashing together