Mountains

The two major mountain ranges in North America are the Rocky Mountains, which run from northern Canada to the southwestern United States, and the Appalachian Mountains, which stretch along the eastern United States.

No, not all mountains have snow caps. The presence of snow caps depends on factors such as elevation, latitude, and climate. Mountains in higher latitudes or with higher elevations are more likely to have snow caps year-round.

Mt. Baker is located in the North Cascades of Washington State in the United States. It is part of the North Cascade National Forest and is known for its picturesque beauty and excellent skiing and snowboarding opportunities.

How much of the earth's surface do mountains cover?

it is 99% of the earth

The Ring of Fire is a horseshoe-shaped area in the Pacific Ocean known for its high levels of seismic and volcanic activity. It is home to approximately 75% of the world's active and dormant volcanoes and experiences about 90% of the world's earthquakes. The area is characterized by subduction zones, where tectonic plates collide and one plate is forced beneath the other, leading to volcanic and seismic events.

Some of the Indian tribes that historically inhabited the Rocky Mountains region include the Shoshone, Ute, Blackfeet, and Cheyenne. They have a deep connection to the land and its resources, relying on hunting, gathering, and later trading as key aspects of their way of life.

They are on the western half of North America and stretch from northern Canada down into Mexico.

The point on the earth's surface farthest from the center of the globe is the summit of Mount Chimborazo in Ecuador. This is due to the bulging shape of the earth at the equator, which makes Mount Chimborazo's summit higher above the center of the earth compared to other mountains.

Mt. Everest, 29,281 feet. which is the tallest mountain in the world and yes it is

A linear mountain belt is a long and narrow region of elevated terrain that typically follows a linear or elongated trend. These mountain belts often form along tectonic plate boundaries where compressional forces lead to uplift and the formation of mountains. Examples include the Andes in South America and the Himalayas in Asia.

Mount Cotopaxi is located in Ecuador, within the Cotopaxi National Park. It is one of the highest active volcanoes in the world, standing at an elevation of 5,897 meters (19,347 feet) above sea level.

Two ways that volcanic eruption can benefit people include the creation of land mass and of energy. Volcanic steam and heat can be used to produce energy.

Mount Ararat stands at an elevation of 5,137 meters (16,854 feet) above sea level.

Fold moutains are actually formed by crust which have been uplifted and folded by compressional forces. This occurs along convergent plate boundaries where 2 plates move towards each other, between continental plates or between an oceanic and a continental plate. The crust and the rocks get bent and crumpled, and massive layers of Earth's crust gets uplifted as a result, forming spectacular fold mountains.

More well-know examples of fold mountains are the Himalayas in Asia and the Andes in South America.

Large anticlines form ridge-like mountains with a U or V-shaped profile. These mountains typically have an elongated shape due to the folding of rock layers, with the oldest rocks found in the center of the fold. Examples include the Appalachian Mountains in North America and the Zagros Mountains in the Middle East.

Mount Kosciuszko is a mountain, not a volcano. It is the highest peak in Australia, located in the Snowy Mountains in New South Wales. It is a popular destination for hikers and outdoor enthusiasts.

Complex mountains are formed when the crust is subjected to very large compressive forces. Under large compressive forces and moderately high temperatures and pressures, parts of the crust are bent into large folds and broken into slices that slide over underlying rocks. The slices of the rock slide away from the source of compression. GRADE 7 SCIENCE

Mount Rainier formed from volcanic activity during the last ice age, around 500,000 years ago. The mountain is a stratovolcano, built up by successive layers of lava and ash. The most recent major eruptive period occurred approximately 1,000 years ago, shaping the mountain into its current form.

Volcanic arcs and deep ocean trenches are formed along subduction zones. As one tectonic plate moves beneath another, the descending plate melts and creates magma that rises to the surface to form a volcanic arc. Deep ocean trenches are also created as the overriding plate bends and sinks into the Earth's mantle.

Ojos del Salado volcano in Chile contains primarily andesitic magma, which is a type of intermediate magma that has a silica content between that of basaltic and rhyolitic magmas. This type of magma often results in explosive eruptions due to its viscosity and gas content.

Fault-block mountains form from vertical fault movement. These mountains are created when blocks of the Earth's crust are pushed up and down along fault lines, resulting in steep, jagged peaks and valleys. An example of a fault-block mountain range is the Sierra Nevada in California.

The eruption of Mount St. Helens in 1980 was a significant event, but not the greatest explosive eruption in the last two hundred years. This title is often attributed to the eruption of Krakatoa in 1883, which had a larger impact on a global scale.

The Rocky Mountains,and Seirra Nevada in the USA

Mauna Loa is a mountain in Hawaii that is made of volcanic stone. The mountain continues to grow as lava is added to its lava fields.