Mountains

piedmont, from the French pied (foot) mont (mountain)

The name of the mountain system made up of parallel ranges is the "Cordillera." This term is often used to describe mountain ranges that run parallel to each other, such as the Andes in South America or the Rocky Mountains in North America.

A continental plate is colliding with another continental plate, causing upward motion. A lithospheric plate is colliding with another lithospheric plate of similar bouyancy, causing upward motion.

Mountains change over time due to geological processes such as tectonic plate movements, erosion, and volcanic activity. These processes can lead to the uplifting of mountains, wearing down of rock through weathering and erosion, and the formation of new mountain ranges. Over millions of years, mountains can undergo significant changes in their size, shape, and elevation.

The Cascade Mountains were formed by the subduction of the Juan de Fuca tectonic plate beneath the North American plate. This process began around 40 million years ago and continues to shape the range today through volcanic activity and uplifting. The result is a long chain of volcanic peaks and rugged terrain stretching from British Columbia in Canada to California in the United States.

57 people died in the May 17, 1980 eruption.

the highest point on earth is mount Everest.but the highest mountain includind below sea level height is tall er but i cant remember the name.

Unwarped mountains are high landforms that have not been significantly altered by tectonic activity, such as folding or faulting. They retain their original shape and structure, often providing insights into the geologic history of a region. Unwarped mountains are typically found in regions with low levels of tectonic activity.

No, Stone Mountain in Georgia is a large granite dome formed underground millions of years ago and exposed through uplift and weathering. It is not an example of erosion in the traditional sense. Erosion refers to the wearing away of rock and soil by natural processes like water, wind, and ice.

Mount Tarawera in New Zealand erupted in 1886, resulting in a series of explosive blasts and destroying several villages.

An example of an eroded mountain is the Appalachian Mountains in the eastern United States. Over millions of years, the forces of weathering and erosion have worn down these once towering mountains into rolling hills and valleys.

The Earth's highest mountain range is the Himalayas, located in Asia. This mountain range stretches across five countries: India, Nepal, Bhutan, China, and Pakistan. The tallest peak in the Himalayas is Mount Everest.

Dome mountains are created through the process of uplift and folding of the Earth's crust, typically in response to tectonic forces. They form when rocks are uplifted in a broad arch or dome shape due to underlying geologic processes, such as magma intrusion or regional compression. Over time, erosion can expose the dome structure at the surface.

Dome mountains are formed by the uplift of rock layers in a broad region, creating a dome-shaped structure, while volcanic mountains are formed by the accumulation of lava and volcanic ash erupting from a volcano. Dome mountains do not have volcanic activity associated with them, whereas volcanic mountains are typically associated with magma and eruptions.

Upwarped mountains are created by the uplifting and folding of the Earth's crust. They are typically broad and gently sloping, with a wide base and a rounded summit. These mountains often form in regions of tectonic activity, such as at the boundaries of continental plates.

The primary effects of the Grímsvötn eruption include the release of ash and volcanic gases into the atmosphere, disrupting air travel and potentially affecting local air quality. The eruption can also lead to the formation of volcanic lightning, lahars (mudflows), and pyroclastic flows which pose risks to nearby communities and infrastructure.

K-2 is the second-highest mountain in the world, with an elevation of 28,251 feet (8,611 meters) above sea level. It is located in the Karakoram Range on the China-Pakistan border.

They provide evidence Pangea existed because mountain belts along the margins of North America, Africa and Europe line up as well and have similar rock types, indication that the continents at one time were joined as Pangea. Also that indicate that there were once contiental drift.

The Himalayas stretch for about 1,500 miles (2,400 kilometers) across five countries in South Asia: India, Nepal, Bhutan, China, and Pakistan.

Folding is usually the result of compressional stress, where rocks are squeezed together and deform due to tectonic forces. This can lead to the bending or curving of rock layers.

Less rain falls on the eastern slopes of western mountains because as moist air moves inland from the ocean, it is forced to rise over the mountains. As the air rises, it cools and condenses, leading to precipitation on the windward side (western slopes). By the time the air descends on the leeward side (eastern slopes), it has lost much of its moisture, resulting in drier conditions.

Lhotse is the fourth tallest mountain on Earth, with a height of 8,516 meters (27,940 feet). It is located in the Himalayas on the border between Tibet and the Khumbu region of Nepal, next to Mount Everest.

The Himalayas formed when the Indian tectonic plate collided with the Eurasian plate around 50 million years ago. This collision caused the Earth's crust to crumple and uplift, creating the tallest mountain range in the world.