mountain range
Mountain ranges are typically found near convergent plate boundaries, where tectonic plates collide and push up the Earth's crust. Oceanic ridges, on the other hand, are located at divergent plate boundaries where tectonic plates move apart and create new oceanic crust. Mountain ranges are not usually found directly on top of oceanic ridges.
Parallel mountain ranges are called "ranges" or "ridges." Examples include the Sierra Nevada and the Rocky Mountains in North America.
The Andes is a fold mountain range, formed by the collision of tectonic plates. It is characterized by long linear ridges that result from the folding and uplifting of the Earth's crust.
A compact group of mountains is called a mountain range. Mountain ranges are a series of peaks and ridges that are geologically related and usually form a continuous chain. Examples include the Rocky Mountains and the Andes.
A region of parallel mountain chains is known as a mountain range or a mountain belt. Examples include the Rocky Mountains in North America, the Andes in South America, and the Himalayas in Asia. These mountain ranges are formed by tectonic plate movements and are characterized by a series of parallel peaks and ridges.
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are where the lithosphere is moving apart and new oceanic crust is being formed.
It is true that mid-ocean ridges are underwater mountain ranges. These ridges are long, seismically active submarine ridges associated with seafloor spreading.
Soil erosion is a special concern for deserts and mountain ridges because these areas have limited vegetation to hold the soil in place. The sparse vegetation in deserts and mountain ridges increases the likelihood of erosion by wind or water. Additionally, the steep slopes in mountain ridges can lead to rapid movement of soil during erosion events.
Submarine mountain ranges at the bottom of the ocean are called oceanic ridges or mid-ocean ridges. These are underwater mountain ranges that form along plate boundaries where tectonic plates are diverging or moving apart.
Mid-ocean ridges
ridges
mountain ridges above geological plates
Mountain chains at ocean ridges
Mount Everest
the mid-ocean ridges
Because the mountain is connected to the stream and the river which leads to the edge of a water shed.