The South American Plate and the Nazca Plate are the two plates that converge to form the Andes mountain range. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift of the Andes through volcanic activity and compression.
Compression is a stress state that acts to decrease the size / volume of an object. As such any force resulting in pressure or stress that acts to "squash" the crust is compression. This commonly occurs at convergent plate boundaries were one tectonic plate is colliding with another.
Mountains
A plateau can form on a convergent plate boundary where two plates collide, causing uplift and compression of the crust. It can also form on a divergent plate boundary where two plates move apart, leading to the stretching and thinning of the crust, creating a high, flat landform.
The Greater Antilles are located near a transform plate boundary between the North American Plate and the Caribbean Plate. These plates are silding past one another. In the area where these plates meet, stress builds up, which is released in the form of earthquakes.
because of the compression boundary. they form when the compression boundary is pushed together to the end. the fault is strike slip which helps because it helps move the plates together. the stress is the normal stress which helps bring the plates apart.
Folded mountains in the middle of a tectonic plate can form due to compressional forces within the plate, possibly caused by the collision of microplates or subduction of small tectonic plates beneath the larger plate. These folding events can create mountain ranges within the interior of a tectonic plate, such as the Urals in Russia or the Appalachian Mountains in the United States.
The South American Plate and the Nazca Plate are the two plates that converge to form the Andes mountain range. The Nazca Plate is subducting beneath the South American Plate, leading to the uplift of the Andes through volcanic activity and compression.
Compression is a stress state that acts to decrease the size / volume of an object. As such any force resulting in pressure or stress that acts to "squash" the crust is compression. This commonly occurs at convergent plate boundaries were one tectonic plate is colliding with another.
Mountains
No, rocks do not typically form folds under the influence of compressive stress. Folds in rocks are usually formed by tectonic forces such as compression, which causes the rocks to bend and fold. Compressive stress can lead to faulting and fracturing of rocks, rather than folding.
Tensional stress from divergent plate boundaries causes a normal fault to form. This stress pulls rocks apart along a fault line, causing the hanging wall to drop relative to the footwall.
Convergent plate boundaries, where two tectonic plates move towards each other, can cause mountains to form. The collision and compression of the plates can lead to the uplift of crustal rocks and the formation of mountain ranges.
Convergent plate boundaries can form both mountain ranges and subduction zones. Mountain ranges are typically formed when two continental plates collide, leading to compression and uplift of the crust. Subduction zones are formed when an oceanic plate is forced beneath another plate, usually resulting in the formation of deep ocean trenches and volcanic activity.
Plate tectonics cause earth tremors through the movement of tectonic plates. When these plates shift and grind against each other, it can create stress along faults in the Earth's crust. This stress is eventually released in the form of an earthquake, resulting in earth tremors.
Compression mostly. If you're exercising with proper form then the impact on the joints will be less regardless of the amount of loading used, so emphasize proper form if joint stress is a concern.
A convergent plate boundary would likely form a mountain chain of sedimentary rock. As tectonic plates collide, one plate may be forced beneath the other, leading to the uplift of sedimentary layers and their subsequent compression and deformation, forming mountain ranges.