horse isle answer - plate tectonics
Mountains formed by magma that reaches the Earth's surface are called volcanoes.
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.
Residual mountains are also called mountains of denudation because they are formed by the erosion and removal of surrounding material, leaving behind a more resistant core. Over time, the processes of weathering and erosion wear away the softer rocks, exposing the harder rocks as peaks or ridges. This denudation process results in the formation of residual mountains.
Mountains formed by magma that reach the Earth's surface are called volcanoes. These volcanic mountains are created through the eruption of lava, ash, and gases from the Earth's mantle and crust. Over time, repeated eruptions build up the volcano, forming a distinct peak.
Geologists classify mountains based on their formation process, height, and steepness of slopes. Some features called mountains may not meet the specific criteria set by geologists, such as being formed by tectonic processes like folding and faulting. Therefore, they may be referred to as hills or other landforms instead.
Mountains are formed by the process of orogeny.
Plate Tectonics.
Mountains formed by magma that reaches the Earth's surface are called volcanoes.
False. Dome mountains are formed by the uplifting and folding of rock layers, not by normal faults. Mountains formed by blocks of rock uplifted by normal faults are called fault-block mountains.
Uplift and subsequent erosion
Horse isle 2 answer: Plate TectonicsMoonWishes or MoonWind
Plate tectonics
That process is called Speciation!
Mountains are classified based on their elevation above sea level. They can be categorized as major mountains (over 6,560 feet), minor mountains (1,000-6,560 feet), and hills (under 1,000 feet). Additionally, mountains can also be classified by their formation process, such as volcanic, fault-block, or fold mountains.
When an earthquake happens the tectonic plates slide up rubbing on each other. Then they slide up and form huge rocks that are eroded in time. These formations are called mountains
Convergent boundary mountains are formed where two tectonic plates collide, causing one plate to be forced beneath the other in a process called subduction. This collision can lead to the formation of mountain ranges due to the intense pressure and folding of the Earth's crust. The Himalayas are a notable example of convergent boundary mountains, formed by the collision of the Indian Plate with the Eurasian Plate.
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.