faulting causes large blocks of the Earth's crust to drop down relative to other blocks
The tectonic plates that collide vertical to one opposit end of the other so that the can crash making an earthquake this is done to global warming but really it is earthquake causing global warming
Tectonic shear stress.
Compressional stress is the stress produced by two tectonic plates moving towards each other.
Earthquakes are primarily caused by tectonic stress, which occurs when the Earth's tectonic plates interact. This stress can result from three main types of tension: compressional stress, where plates push together; tensional stress, where plates pull apart; and shear stress, where plates slide past one another. When the accumulated stress exceeds the strength of the rocks, it releases energy in the form of seismic waves, causing an earthquake.
The force that occurs when tectonic plates are pushed together is called "compression." This type of stress can lead to the formation of mountains, earthquakes, and other geological phenomena as the plates collide and interact with each other.
Compressional tectonic stress causes folded mountains. This stress occurs when tectonic plates collide, leading to the deformation and folding of the Earth's crust. Over time, the accumulated pressure and movement result in the creation of folded mountain ranges.
Compressive stress causes folding mountains to form. This stress occurs when tectonic plates collide or converge, leading to the deformation and folding of rock layers, ultimately creating mountain ranges.
The type of tectonic stress that forms fault-block mountains is known as extensional stress. This stress occurs when the Earth's lithosphere is being pulled apart, causing blocks of crust to move vertically. As the blocks are uplifted and tilted along fault lines, fault-block mountains are created.
Tectonic stress, caused by the movement of Earth's tectonic plates, produces the most significant crustal deformation. This stress results in the formation of features like mountains, faults, and earthquakes as the Earth's crust responds to the forces generated by tectonic plate interactions.
Tensional stress, which results from the pulling apart of the Earth's crust, causes fault block mountains to form. This stress leads to the extension and fracturing of the crust, resulting in the blocks of crust moving up or down along faults to create a mountain range.
Compressional Stress
Tectonic stress causes most earthquakes. This stress is generated as tectonic plates move and collide with each other, building up pressure that is eventually released as an earthquake. Other types of stress, such as volcanic or anthropogenic activities, can also trigger earthquakes in specific circumstances.
Verticle stress causes monocline. Verticle stress causes monocline.
When two tectonic plates collide, compressional stress occurs. This stress causes the rocks to fold and deform, leading to the formation of mountain ranges, such as the Himalayas. The intense pressure and friction between the plates can also result in earthquakes and volcanic activity.
The dominant type of stress associated with folded mountains is compressional stress caused by tectonic plate collision. As plates converge, the rocks are squeezed and folded, leading to the formation of folded mountain ranges such as the Himalayas and the Appalachians.
Fault-block mountains are formed primarily by tectonic forces associated with extensional stress, which causes the Earth's crust to stretch and fracture. This leads to the formation of faults, where blocks of crust are lifted or tilted. As these blocks are elevated relative to their surroundings, they create the rugged terrain characteristic of fault-block mountain ranges. An example of this process can be seen in the Sierra Nevada mountains in California.
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.