Canyon
The area behind a mountain that receives little rain is known as a rain shadow. This phenomenon occurs when moist air rises over the mountain, cools, and loses moisture as precipitation on the windward side. As the air descends on the leeward side, it becomes drier and warmer, leading to significantly reduced rainfall in the rain shadow region. This can create arid or semi-arid conditions, often resulting in distinct vegetation and ecosystems.
The term is Rain Shadow.
is that mountain are only little but not that little and escarpment are just between the mid range of a mountain
A large piece of flat land is called a plain. A desert is a dry, barren area with little vegetation. A mountain is a raised landform with a peak or summit.
Surprisingly, the summit Mount Everest receives very little precipitation, being above the level at which precipitation occurs. On average, the whole of the mountain receives about 18 inches of snow.
A plain
A rain shadow.
The area behind a mountain with little rain is called a rain shadow.
rain shadow
That area is called a rain shadow. It occurs when moist air rises over a mountain, releases moisture on the windward side, and descends down the other side, resulting in a drier climate on the leeward side.
rain shadow
A desert.
Most of Patagonia receives little rainfall so qualifies as a desert.
Mesopelagic
The leeward side of a mountain, also known as the rain shadow side, typically receives less precipitation because as air descends down the mountain, it warms and is not able to hold as much moisture. This results in decreased cloud formation and precipitation on the leeward side compared to the windward side.
The term is Rain Shadow.
This phenomenon is called a "rain shadow effect." When moist air is forced to rise over a mountain range, it cools and loses its moisture as precipitation on the windward side. As the air descends on the leeward side, it warms and becomes drier, creating arid conditions and little precipitation, known as a rain shadow.