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There are three main types of mountains. block mountains formed by sections of the earth's crust that have been tilted or lifted up by the movement of two close fault lines, large cracks in the earth's surface. These are usually smaller than other types of mountains and are often separated by valleys. Volcanic mountains are formed by magma that is pushed out of the earth through a crack or weak place in the earth's crust. Fold mountains are formed when rock is "squeezed" together. When plates collide, the rock along the edges crumples, creating a huge zig-zag pattern in layers of the earth's crust. Upwarped mountains are formed when magma pushes up the earth's crust without breaking the surface. This creates a rounded mountain that gently slopes toward the surrounding land.
This depends upon the viscosity (i.e. how runny the lava is ) and the composition (i.e. the percentage composition of silicon which determines the properties of the lava and how much gas is retained within the lava) of the magma greatly. In Iceland, Hekla is an example of a mountain/volcano and is classed as a shield volcano as it had long, gently inclined sides. However, in Peru where the Nazca plate is being subducted beneath the South American plate rhyolitic eruptions produce steeply sided mountains with thrust faults. The type of the tectonic plate margin determines the type of mountains produced as well as the viscosity and composition.
It depends on the specific application or use. Sedimentary rocks are formed from the accumulation of sediments and can be more easily broken down and compacted. They often contain fossils and organic matter. Volcanic rocks are formed from volcanic activity and can be more resistant to weathering and erosion. They often have a more uniform composition and can be more durable. Ultimately, the better choice will depend on factors such as strength, density, and aesthetic preference.
No, most mountains are formed from rocks squashed up as the continents move round the Earth furthermore, not every volcano is a mountain - for instance Yellowstone park is a volcano and it is not a mountain.
The island-arc volcanoes are formed from the subduction of an oceanic tectonic plate under another tectonic plate, and often parallel an oceanic trench.
Mountains formed from the buildup of volcanic lava often take this shape
Mountains formed from the buildup of volcanic lava often take this shape
Shield
There are two areas where volcanic mountains often form. They are subduction zones and hot spots.
There are three main types of mountains. block mountains formed by sections of the earth's crust that have been tilted or lifted up by the movement of two close fault lines, large cracks in the earth's surface. These are usually smaller than other types of mountains and are often separated by valleys. Volcanic mountains are formed by magma that is pushed out of the earth through a crack or weak place in the earth's crust. Fold mountains are formed when rock is "squeezed" together. When plates collide, the rock along the edges crumples, creating a huge zig-zag pattern in layers of the earth's crust. Upwarped mountains are formed when magma pushes up the earth's crust without breaking the surface. This creates a rounded mountain that gently slopes toward the surrounding land.
Volcanic rocks are often more resistant to erosion than surrounding rock
Mountains typically have steep slopes, elevated peaks, and are formed due to tectonic plate movements or volcanic activity. They are often characterized by diverse ecosystems and are important sources of freshwater. Mountains also impact weather patterns and climate in surrounding regions.
Mountains are large landforms that rise significantly above their surrounding areas, typically with steep slopes and high peaks. They are formed through tectonic plate movements, volcanic activity, or erosion processes. Mountains are often characterized by diverse ecosystems due to variations in altitude, climate, and vegetation.
A chain of mountains is a series of connected mountain peaks or ranges that have a similar geological origin. They are formed through tectonic processes such as the collision of continental plates or volcanic activity. These mountain chains can span long distances and are often associated with diverse ecosystems and climate patterns.
This depends upon the viscosity (i.e. how runny the lava is ) and the composition (i.e. the percentage composition of silicon which determines the properties of the lava and how much gas is retained within the lava) of the magma greatly. In Iceland, Hekla is an example of a mountain/volcano and is classed as a shield volcano as it had long, gently inclined sides. However, in Peru where the Nazca plate is being subducted beneath the South American plate rhyolitic eruptions produce steeply sided mountains with thrust faults. The type of the tectonic plate margin determines the type of mountains produced as well as the viscosity and composition.
They create a convergent boundary and can often create mountains, over a period of years.
There are three main types of mountains. block mountains formed by sections of the earth's crust that have been tilted or lifted up by the movement of two close fault lines, large cracks in the earth's surface. These are usually smaller than other types of mountains and are often separated by valleys. Volcanic mountains are formed by magma that is pushed out of the earth through a crack or weak place in the earth's crust. Fold mountains are formed when rock is "squeezed" together. When plates collide, the rock along the edges crumples, creating a huge zig-zag pattern in layers of the earth's crust. Upwarped mountains are formed when magma pushes up the earth's crust without breaking the surface. This creates a rounded mountain that gently slopes toward the surrounding land.