The chain of undersea mountains is called a mid-ocean ridge. It is formed by the movement of tectonic plates and is characterized by volcanic activity and the creation of new oceanic crust.
A chain of undersea mountains that circles the earth is called a mid-ocean ridge. These ridges form where tectonic plates pull apart, allowing magma to well up and create new oceanic crust. The most well-known mid-ocean ridge is the Mid-Atlantic Ridge.
A long undersea mountain chain is called a mid-ocean ridge. These ridges are formed by tectonic plates spreading apart, allowing magma to rise and create new oceanic crust. The Mid-Atlantic Ridge is one well-known example of a mid-ocean ridge.
An undersea volcanic formation that does not rise at least 1000 meters above the surrounding sea floor is called a seamount. These underwater mountains are formed by volcanic activity and can vary in size and shape.
A chain of mountains is often referred to as a mountain range.
A mid-ocean ridge is an undersea mountain chain where new ocean floor is produced through volcanic activity. Here, magma rises up from the Earth's mantle and solidifies as it cools, leading to the formation of new crust.
A chain of undersea mountains that circles the earth is called a mid-ocean ridge. These ridges form where tectonic plates pull apart, allowing magma to well up and create new oceanic crust. The most well-known mid-ocean ridge is the Mid-Atlantic Ridge.
ocean ridge
Seamounts are undersea mountains that rise 1,000 meters above the sea floor.
A string of mountains is called a mountain chain.
A row or chain of mountains ranged in a line is called a mountain range. A narrow gap through a mountain range is a mountain pass.
A string of mountains is called a mountain chain.
A Mountain Range
Mount Everest is in a chain of mountains called the Himalayas.
Yes, a string of mountains is commonly referred to as a mountain range or a mountain chain. These terms are used to describe a series of mountains that are connected together along a continuous line.
undersea mountains
The islands of southern Europe, such as Sicily, Sardinia, and the Balearic Islands, are primarily formed by a combination of undersea mountains and volcanic activity. These landforms are geologically diverse, with some areas experiencing volcanic eruptions that have contributed to their formation over millions of years.
A long undersea mountain chain is called a mid-ocean ridge. These ridges are formed by tectonic plates spreading apart, allowing magma to rise and create new oceanic crust. The Mid-Atlantic Ridge is one well-known example of a mid-ocean ridge.