Mountains

The five types of mountains are fold mountains (e.g. the Rocky Mountains), fault-block mountains (e.g. the Sierra Nevada), volcanic mountains (e.g. Mount St. Helens), dome mountains (e.g. the Black Hills), and plateau mountains (e.g. the Colorado Plateau).

Plateau Mountains are actually not formed by the Earth's internal activity; instead, they're revealed by erosion. They're created when running water carves deep channels into a region, creating mountains. Over billions of years, the rivers can cut deep into a plateau and make tall mountains. Plateau Mountains are usually found near folded mountains. Plateau Mountains are flat areas that have been pushed above sea levels by forces from inside the earth. An example of a plateau mountain is mountains in New Zealand. Plateau Mountains form when large areas of flat-topped rocks are pushed above the crust by tectonic plates moving together. The dictionary describes these as large areas of 'high levels' of flat land.

Mountains are formed through tectonic processes such as the collision of continental plates, volcanic activity, and the folding and faulting of rock layers. Over millions of years, these processes push up the Earth's crust, creating the towering peaks we see today.

The movement of rock and soil down a hillside or mountain is called mass wasting or mass movement. This can occur due to the force of gravity acting on loose material, steep slopes, heavy rainfall, earthquakes, or human activities that disturb the natural stability of the land.

Trapdoor faulting is a geological phenomenon where faults occur beneath impermeable layers of rocks, causing fluids to accumulate and create high-pressure reservoirs. This can lead to sudden and catastrophic release of fluids, such as water or hydrocarbons, resulting in sinkholes, landslides, or other surface deformations. The term "trapdoor" refers to the abrupt and localized nature of the fault movement.

The rain shadow effect occurs when moist air is pushed up over a mountain range, causing it to cool and release precipitation on the windward side. As the air descends down the other side of the mountain, it warms up and becomes more dry, leading to a rain shadow area with much less precipitation on the leeward side of the mountains.

The process of plate tectonics constantly creates new mountains through collisions between tectonic plates, ensuring that mountain ranges are continuously being uplifted and formed. This ongoing geologic activity helps counterbalance the forces of erosion and ensures that mountains persist on Earth's surface.

The Tian Shan mountains are located on Asia. The word is also spelled "continent", not contient.

The Himalayas mountain chain was formed by the collision of the Indian tectonic plate with the Eurasian tectonic plate. This collision continues to push the two plates into each other, causing the Himalayas to still be one of the world's fastest-growing mountain ranges.

Mount Bromo last erupted in January 2011, with its activity continuing until November 2015. Since then, there have been no major eruptions reported.

Mount Shasta typically has andesitic magma, which is a type of intermediate magma that is common in subduction zone environments. This type of magma is rich in silica and forms from the partial melting of both oceanic and continental crust.

Because, elevation affects both temperature and precipitation, the type of biome found at a higher elevation can be different from one at a lower elevation.

For Example: Temperate forest, Boreal forest, Tundra, and Permanent ice.

(forest by mountain, higher up the mountain, go higher and you reach at tundra, top of mountain is cold and precipitation is very different, so it's permanent ice)

Hope this answers your question :)

Erosion by natural processes, such as wind, water, and ice, can eventually level mountains over millions of years. As these forces wear away at the rock and soil of a mountain, it can gradually reduce its height and size. Additionally, tectonic plate movements can also play a role in shaping and eroding mountains over long periods of time.

All depends on the size of the eruption. If it were a big eruption then it could bellow ash and smoke into the atmosphere and cause sunlight and heat to be blocked around the world making the earths temperature fall for a little while. Also it will send gasses like methane, carbon dioxide and sulpher into the atmosphere, adding to the greenhouse gas level and maybe contributing to global warming.

Mount Macedon was formed around 370 million years ago through volcanic activity, with lava flows and sedimentary deposits shaping its landscape. Over time, erosion and tectonic forces have further sculpted the mountain's distinctive features, including its slopes and valleys.

Mountains still exist because of ongoing tectonic activity, including the collision of tectonic plates and volcanic eruptions, which continue to uplift and create new mountain ranges. Erosion from natural processes such as weathering, rivers, and glaciers also plays a role in shaping and maintaining mountain landscapes.

Folding and Faulting usually work together to form mountains. Faulting works by one plate shifting up and one plate submerging. Folding however works by both plates pushing against each other slowly folding over and over.

Faulting and Folding and work together to make mountains by as one plate moves down the other up causes the plate going up to roll over or move on top of the other plate then as the bottom plate gets heat from the earths core it rises folding the plate on top again to bring it even higher.

Hoped it helped you

The Atlas Mountains were formed through a combination of tectonic plate movements and volcanic activity. The range primarily consists of folded and faulted rocks created by the collision of the African and Eurasian tectonic plates. Volcanic activity also played a role in shaping the landscape of the region.

The Rocky Mountains are on the North American plate.

The Rocky Mountains are a large mountain range that runs through western North America, spanning from Canada to the United States. They are known for their rugged peaks, diverse ecosystems, and outdoor recreational opportunities.

In the Himalayas, the Indian plate is colliding with the Eurasian plate, causing the Earth's crust to deform. This collision has formed the Himalayan mountain range through processes like thrusting and folding. The plates continue to move, leading to ongoing geological activity in the region.

The major forces that form folded mountains are tectonic plate movements, specifically convergent boundaries where two plates collide. The immense compressional forces generated during this collision cause the Earth's crust to buckle and fold, leading to the formation of mountain ranges. Over millions of years, continued plate movements can further deform and uplift these folded mountains.

At the Himalayan mountains, the Indian plate is colliding with the Eurasian plate. This collision is causing the plates to continue to converge, leading to the uplift of the Himalayas. The collision is also creating seismic activity, resulting in earthquakes in the region.

arid conditions in the Atacama Desert due to the blocking of moisture-bearing clouds by the Andes Mountains, leading to one of the driest places on Earth. Conversely, the windward side of the Andes receives heavy precipitation, supporting lush forests and vegetation in southern Chile. Overall, the rain shadow effect has contributed to stark contrasts in climate and landscapes across Chile.