The Salish and Kootenai Tribes of the Flathead Nation lived in what is now Montana on the eastern slopes of the Rockies
Today, Cahuilla families live in modern houses and apartment buildings.In the past, most Cahuilla people lived in brush houses called kish. Kish are small round or cone-shaped houses made of a wooden frame covered with reeds and brush. These are very simple houses and Cahuilla people really only used them to sleep in. When they were resting, socializing, or working on crafts, Cahuilla people sat outside-- it was rarely cold or rainy in the climate where they lived.
method 1 : Artificial rain is produced by spraying clouds with substances like Silver Iodide (costly) or cheaper ones like solid carbon dioxide (dry ice) or even finely powdered Sodium Chloride. The process is called seeding. method 2 : The process involved in artificial rain-making involves three easy-to-understand stages. The first stage is agitation. That is using chemicals to stimulate the air mass upwind of the target area to rise and form rain clouds. The chemicals used during this stage are calcium chloride calcium carbide, calcium oxide, a compound of salt and urea, or a compound of urea and ammonium nitrate. These compounds are capable of absorbing water vapour from the air mass, thus stimulating the condensation process. The second stage is called building-up stage. Here the cloud mass is built up using chemicals such as kitchen salt, the T.1 formula, urea, ammonium nitrate, dry ice, and occasionally also calcium chloride to increase nuclei which also increase the density of the clouds. In the third stage of bombardment chemicals such as super-cool agents: silver iodide and dry ice are used to reach the most unbalanced status which builds up large beads of water (Nuclei) and makes them fall down as raindrops. In planning every stage a high degree of expertise and experience is required, in selecting the types and amounts of chemicals to be used, while taking into consideration weather conditions, topographical conditions, wind direction and velocity as well as the location or delimitation of the area for chemical seeding. Several other ideas are also involved in rain making. Rockets containing rain-making chemicals can be fired into the clouds either from the ground or from aircraft. A jet of rain-making chemicals is shot from a highly pressurised cannister directly into the cloud base, so as to coerce clouds which normally hang above mountain tops to cluster up and rain on the mountain or their slopes. Rain-making chemicals are added to super-cooled clouds, i.e., those at altitudes above 18,000 metres, to stimulate the formation of ice crystals in the cloud or cloud cluster.
Sometimes they are called the foothills, or the piedmont, (French for foothills).
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.
The sun
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.
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.
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.
cold,dry mountain slopes