Mountains

an oceanic ridge

May be rays like on our Moon. In smaller meteor impacts. a crater like the one shown, forms. ... For example, the growth of a new mountain range will ..... 17 State the agent of erosion that is most likely responsible for shaping the Catskill Plateau so that it physically resembles a mountainous region. @ Raj Bista

Air has a certain amount of moisture in it, called humidity. Fog or precipitation result when the air accumulates too much moisture to hold ... the amount of moisture air can hold varies based on air pressure which itself varies. Storms can lower air pressure, but are a bit dynamic and chaotic ... air pressure is naturally lower the higher in altitude you are, though; air is thickest at lower elevations. The air becomes too thin at altitude to hold onto the moisture, so it 'piles up' against mountain ranges and tends to dump whilst the wind continues across the mountains. Then devoid of the moisture it dumped, it tends to create a "rain shadow" on the far side of the mountain range as the air re-thickens when it lowers in altitude on the far side of the mountain range without the moisture it lost on the windward side of the mountains. Thus, you often have a lush, green side of mountains as the mountains cause the atmosphere to dump its moisture, and a desert on the far side as the air regains pressure but is devoid of moisture.

Mountains are worn down through a process called weathering and erosion. Weathering breaks down rocks into smaller pieces, while erosion carries these pieces away, gradually shaping the mountain over time. Factors such as wind, water, ice, and biological activity all contribute to this natural process of mountain erosion.

Two processes that could cause high mountains with rounded peaks are erosion and glaciation. Erosion from wind, water, or ice can wear down sharp peaks over time, creating a more rounded appearance. Glaciation, where glaciers move over the landscape, can also smooth out mountain peaks as the ice grinds and shapes the rock.

A volcanic mountain is formed by geothermal pressure and material discharge, specifically a stratovolcano, which is characterized by its steep sides and periodic explosive eruptions. Examples of stratovolcanoes include Mount Fuji in Japan and Mount Vesuvius in Italy.

when rain or snow falls the windward side of a mountain the side that faces wind direction gets most of the rain or snow and the leeward side of a mountain the side that faces away from the wind gets less rain it is said to be in a rain shadow .

Mount Everest is made of sedimentary rocks such as shale limestone etc

High mountainous areas typically have a colder climate with temperatures decreasing as elevation increases. Precipitation levels can vary, but snowfall is common in these areas. Strong winds and low oxygen levels are also characteristic of high mountain environments.

Mountain ranges are formed slowly over years due to tectonic plate movements. When two plates collide, one can be pushed above the other, creating uplift and forming mountain ranges. The process of erosion further shapes and exposes the mountains over time.

The rain shadow effect occurs when moist air is forced to rise over a mountain range, causing it to cool and release precipitation on the windward side of the mountain. As the air descends on the leeward side, it becomes warmer and drier, creating a rain shadow where little precipitation falls. This results in a contrast in vegetation and climate on either side of the mountain range.

When an oceanic plate subducts beneath a continental plate (convergent boundary) it can create enormous mountains due to the intense compression and uplift of the continental crust. An example of this is the Andes Mountains in South America, formed by the subduction of the Nazca Plate beneath the South American Plate.

Yes.

This is because metals are found within the earth's crust, and mountains are simply upheavals of said crust. You can view a mountain as a exposed part of the crust that would otherwise be underground - therefore one can assume that metals would be found in larger quantities in mountainous areas as opposed to plains.

Mountains are considered abiotic because they are non-living physical features of the Earth's surface. Biotic elements such as plants and animals can live in or on mountains, but the mountains themselves are not living organisms.

Technically, a volcano is a type of mountain.

Mountains are formed by two continental tectonic plates colliding. The compressing plates forms folds in the crust, and if no or a small amount of erosion has occurred to wear down these folds, they continue to rise and break to form a mountain, which build on top of each other and form mountain ranges. (Lots of mountains)

Volcanoes are formed by a continental plate and an oceanic plate colliding, where the denser oceanic plate undergoes 'subduction' and slips under the less dense continental plate. The heat and pressure from the oceanic plate causes uplifting of magma from the earth's mantle, which rises to the surface, therefore creating a volcano.

There has to be a crack in the crust so a volcano can form and for the magma to rise through, while mountains are the crumpling of two landmasses. However, volcanoes may also later become mountains if they become completely dormant and no more lava (magma ).

Mountains can become shorter over time due to processes like erosion, weathering, and tectonic activity. Erosion from factors such as water, wind, and ice can wear down the surface of mountains, while weathering breaks down the rocks that make up the mountains. Tectonic processes like plate movement can also cause mountains to slowly erode and decrease in height.

No, the tallest mountains on Earth are found on land. The highest mountain range, the Himalayas, boasts the tallest peak, Mount Everest. In comparison, the ocean's mountains, such as undersea volcanic peaks or seamounts, are not as high as the tallest land-based mountains.

Mt.Vesuvius isn't in a mountain range because it's not technically a mountain its a volcano

The weight of a mountain can vary greatly depending on its size, composition, and elevation. However, mountains can weigh billions or even trillions of tons due to the massive amount of rock and sediment they are made of.

As mountains are worn down through erosion, the material that makes up the mountains is broken down into smaller pieces and transported away. This erosion helps to reduce the height and volume of the mountains over time, eventually reshaping the crust.

Glaciation in the Western Cordillera has influenced the landscape by creating steep valleys, sharp peaks, and U-shaped valleys. Glacial erosion and deposition have shaped the region's topography, leaving behind moraines, cirques, and other glacial landforms. The presence of glaciers also impacts the local climate, hydrology, and biodiversity in the region.

Mountains change due to forces such as erosion, tectonic plate movement, and volcanic activity. Weathering and erosion wear down mountain peaks, while tectonic plate movement can push mountains upwards or cause them to fold and fault. Volcanic activity can also build new mountains or alter existing ones.

Scientists can determine the approximate age of mountains by studying the rock layers within them. By analyzing the composition, structure, and fossil evidence in the rocks, as well as using techniques like radiometric dating, scientists can estimate the age of the mountain and when it was formed. Additionally, studying the erosion patterns and surrounding geological features can provide clues about the age of a mountain.

Fold mountains are formed when two tectonic plates collide, exerting immense pressure on the earth's crust. This pressure causes the crust to buckle and fold, creating large mountain ranges. Over time, erosion can further shape and expose these folded rock layers, creating the characteristic ridges and peaks of fold mountains.

Mount Lhotse is part of the Himalayas and has an alpine climate that is cold and harsh, with temperatures dropping significantly as altitude increases. The summit is covered in snow and ice year-round, with strong winds and low temperatures making it a challenging environment for climbers.