During summer, hot wind form the sufrace of the land move towards the higher toward the hill areas and as a result the cold wind form the hill blow downwards to occupy those empty areas which bring cold wind, thus making it cooler during summer.w
it is due to the increasing altitude of the mountain slopes that the temperature is less and thus it is cooler than compared to the plains
A scree slope is caused by weather erosion breaking off pieces of rock from the cliff and mountain-side.
The character -James Bond- has never visited Canada in the movies or in the books. However during filming of some ski chases the MGM may have used Canadian slopes as ideal slopes for filming Bond, but usually it still means Bond is in another country when he is not.
The mountain supports a great diversity of plant and animal life at various elevations of its slopes. Melting snow provides pure water for the fertile soil and for the human and animal populations.
There are a couple of popular ski slopes in Canada. Some of those ski slopes are located at the following resorts: Kicking Horse Resort, Fernie Alpine Resort, and Red Resort.
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South facing mountain slopes in the northern hemisphere receive more sunlight compared to north facing slopes, leading to higher temperatures and drier conditions. This creates a microclimate that can support different vegetation and wildlife compared to the cooler and more shaded north facing slopes.
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A group of mountain slopes in one area is called a mountain range.
Temperate rainforests are found in moist and cooler climates and distinct seasons, away from the equator.
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.
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High mountain ranges have short summers due to their high elevation, which results in colder temperatures. The high altitude causes the air to be less dense, leading to cooler temperatures even during the summer months. Additionally, the steep slopes of mountain ranges can block sunlight, further limiting the length and intensity of the summer season.
People farm on mountain slopes because these areas can have fertile soil, good drainage, and exposure to sunlight. Additionally, mountain slopes allow for better water management through natural irrigation and terracing, making them suitable for cultivating crops. Farming on mountain slopes also allows for diversified agriculture and can help prevent soil erosion.