Lifted by the collision of the Indian tectonic plate with the Eurasian Plate, the Himalayan range runs northwest to southeast in a 2,400-kilometre (1,500 mi)-long arc. The range varies in width from 400 kilometres (250 mi) in the west to 150 kilometres (93 mi) in the east. Besides the Greater Himalayas, there are several parallel lower ranges. The southernmost, along the northern edge of the Indian plains and reaching 1000 m in altitude, is the Sivalik Hills. Further north is a higher range, reaching 2000-3000 m, known as the Lower Himalayan Range.
The collision of plates can also result in the formation of mountain ranges, volcanic activity, earthquakes, and the creation of new landmasses. These geological processes can have significant impacts on the Earth's surface and can influence the distribution of habitats and ecosystems.
Aleutians: Two oceanic plates Appalachians: Two continental plates Andes: One continental plate, one oceanic plate North American Cordillera: One island plateau, one continental plate Aleutian mountains are those that form when two oceanic plates collide. The Appalachians formed when two continents collided. Andean-type mountains form when oceanic crust is subducted under continental crust. The North American Cordillera is an example of arc-continent collision, which is when island plateaus join a continent.
Those would be the Himalayas.
no those plates match that car you will get in more trouble for switching plates than not haning any at all
Convergent boundary where two tectonic plates collide can create mountains. One plate is usually forced beneath the other in a process called subduction, leading to the formation of mountain ranges like the Andes or Himalayas.
Plate tectonics explain the formation of mountains by mountain chains may form where plates move together. As plates move apart, magma may rise to the surface, forming a volcano.
The regions of greatest relief are often those near the active junction of two tectonic plates. This junction may be a subduction zone, such as in the major oceanic trenches such as the Marina Trench; or a collision zonesuch as near the Andes and the Himalayas.
Yes, it is made of tectonic plates and those plates have names e.g. Indo Australian plate, Eurasion plate
The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere. The lithosphere displaces the asthenoshpere. Thick tectonic plates, such as those made of continental crust, displace more asthenosphere than do thin plates, such as those made of oceanic lithosphere.
If you have plates on it, and you intend to keep those plates, then yes.
Although they aren't common, yes, transform faults can give rise to mountains. Most transform faults take place between oceanic crust, but an easy-to-see example is that of the San Andreas Fault giving rise to the San Gabriel Mountains.
Collision, shaking, shock, and bump are words. Those mean concussion.