The Mid-Atlantic Ridge is a mid-ocean ridge, a divergent tectonic plate or constructive plate boundary located along the floor of the Atlantic Ocean. The mid-Atlantic ridge splits nearly the entire Atlantic Ocean north to south - it's a divergent plate boundary. 10,000 km long.
Yes, the Mid-Atlantic Ridge is a divergent boundary, not a transform fault.
The Mid-Atlantic Ridge is a divergent tectonic plate boundary that extends down the center of the Atlantic Ocean. It is characterized by a long, narrow mountain range with a symmetrical V-shaped profile.
In a million years, the Mid-Atlantic Ridge may continue to grow as tectonic plates move apart, leading to new seafloor spreading and volcanic activity. This could result in the ridge becoming more pronounced and longer over time.
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.
Coast of Iceland
The Mid-Atlantic Ridge is approximately 10,000 kms (6,213.5 miles) long.
The mid-Atlantic ridge splits nearly the entire Atlantic Ocean north to south - it's a divergent plate boundary. 10,000 km long
its long
The Mid-Atlantic Ridge, or MAR.
A long continuous chain of mountains under water. New oceanic crust is formed at the Mid-Atlantic Ridge.
the mid-atlantic ridge is in the process of creating iceland.
The Mid-Atlantic ridge.
The mid Atlantic ridge.
Mid-Atlantic Ridge.
The Mid-Atlantic ridge.
Mid-Atlantic Ridge
The Mid-Atlantic ridge.