On Caribbean islands with mountains, the windward slopes facing the trade winds force air upward, causing rainfall. As a result, areas immediately to the leeward of the mountains have a microclimate with sparse precipitation. This is termed as the rain shadow. It is the dry area located at the lee side of the mountain. The air in the mountains that is being left with little to no moisture, moves behind the mountain and bringing back a drier side which is popularly called as the “rain shadow”.
1. cloud form together
2. wind
3. starts turning into a cone shape.
4. becomes it a hurricane
sorry if some wrong
The landform that is much of northern and eastern Europe would be plains.
Basically physical and chemical weathering (do not confuse with erosion, which involves movement) contribute to the destruction of mineral forms. In this case it breaks down the rocks, minerals and soils, creating slopes and hills. It may be caused by (any form of) water, wind, gravity, waves or sunlight.
<span>When wind and running water gradually decrease in velocity, the transported sediments are deposited over a period of time, and are sorted by size and density. This is because as the velocity decreases, sediments or rocks will accumulate resulting to variety of sizes and a change in density.</span>
