the thin mountain ridge is called an arête.
The low point on a mountain ridge is called a col or a saddle. It is the area between two higher points along the ridge line.
A mountain ridge that separates the heads of opposing glacial valleys is called an arete. It is a narrow and sharp ridge formed by the erosive action of glaciers on both sides.
The low point of a mountain ridge is called a col or a saddle. It is the point where two slopes converge and is often a pass or a corridor between two peaks.
The mountain range at the bottom of the Atlantic Ocean is called the Mid-Atlantic Ridge. It is an underwater mountain system that runs down the center of the Atlantic Ocean from the Arctic Ocean to the southern tip of Africa.
A pass in a mountain range is commonly referred to as a mountain pass. It is a route through a mountain range or over a ridge that allows for easier travel between two regions separated by mountains.
The low point on a mountain ridge is called a col or a saddle. It is the area between two higher points along the ridge line.
ocean ridge
A mountain ridge that separates the heads of opposing glacial valleys is called an arete. It is a narrow and sharp ridge formed by the erosive action of glaciers on both sides.
ridge
arete
Continental ridge
The low point of a mountain ridge is called a col or a saddle. It is the point where two slopes converge and is often a pass or a corridor between two peaks.
A mountain ridge.
The term for the natural gap in a mountain ridge is called a "pass" or a "col." These are low points that allow for easier travel between two adjacent valleys or mountain peaks.
A mountain ridge that separates river systems is called a watershed or a drainage divide. This geographic feature determines the direction in which water flows, dividing the flow of water into different river basins.
The large mountain range found on the floor of the Atlantic Ocean is called the Mid-Atlantic Ridge. The Mid-Atlantic Ridge reaches a maximum width of about 860 nautical miles.
Mid-Ocean Ridge.