becaouse we will be die
A group of mountain slopes in one area is called a mountain range.
The sides of a mountain are called slopes. These slopes can vary in steepness and play a role in determining the overall shape and characteristics of the mountain.
Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountains areas may feel warm afternoon quickly change into cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze. At nightfall, the air along the mountain slopes cools. This is cool air moves down the slopes into the valley, producing a mountain breeze.
Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountains areas may feel warm afternoon quickly change into cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze. At nightfall, the air along the mountain slopes cools. This is cool air moves down the slopes into the valley, producing a mountain breeze.
Mountain and valley breezes are other examples of local winds caused by an area's geography. Campers in mountains areas may feel warm afternoon quickly change into cold night soon after the sun sets. During the day, the sun warms the air along the mountain slopes. This warm air rises up the mountain slopes, creating a valley breeze. At nightfall, the air along the mountain slopes cools. This is cool air moves down the slopes into the valley, producing a mountain breeze.
The sun
During the day, warm air rises up the mountain slopes, creating anabatic winds blowing up the valley. At night, cold air descends down the slopes, creating katabatic winds blowing down the valley. This diurnal pattern of wind movement is typical in mountain-valley systems.
Most don't, but it's mainly because they have no choice, either because the growing conditions in the valleys are not suitable, or they don't know that they shouldn't be farming on mountain slopes to begin with.
The lower slopes of a mountain are typically referred to as the foothills. These are the more gradual, less steep areas at the base of the mountain before reaching the steeper and more rugged terrain higher up.
Curvaceous means having an attractively curvy figure. So this could be for a mountain, for a body, for hills or for slopes.
After sunset the sun is no longer warming the mountain side and there is cooling of the air along the slope. The air becomes more dense and sinks into to valley. Thus the wind blows from the mountain side down into the valley and is thus called a mountain breeze.
Farming on mountain slopes is possible through terrace farming, which involves carving flat platforms into the mountain to create level planting areas. These platforms help prevent erosion and allow for better water retention. Additionally, farmers may use irrigation systems to supply water to crops on mountain slopes.