There are two main factor that make ocean water more or less dense than about 1027 kg/m3:
<span>Areas immediately to the leeward of the mountains have a microclimate with sparse precipitation called a rain shadow.
It is described as "</span><span> a patch of land that has been forced to become a </span>desert because<span> mountain ranges blocked all plant-growing, rainy </span><span>weather" On one side of the mountain the weather is wet, rainy and snowy. And on the other side (the rain shadow) there are no precipitations. </span>
Answer:
The watershed simply restricts the movement of water toward one side, because the water can not move up but only down or on a flat area.
Explanation:
The watersheds represent physical boundaries that are separating the flow of water to rivers, seas, areas, or to put it simply, they direct the movement of water in different directions. The watersheds are marked by landforms that are at a higher elevation than their surroundings, and the separation of the movement of water occurs at the ridges.
Basically, the water moves downward on each side of the ridge. This means that the water on one side of the ridge belongs to one watershed as its waters go in one direction and area, while the water on the other side of the ridge belongs to another watershed because its waters move in another direction and area.
<span>Cirrus clouds are most common form of high-level clouds are thin and often wispy cirrus clouds. Typically found at heights greater than 20,000 feet (6,000 meters), cirrus clouds are composed of ice crystals that originate from the freezing of supercooled water droplets. Cirrus generally occur in fair weather and point in the direction of air movement at their elevation.
</span>Cumulus clouds are puffy clouds that sometimes look like pieces of floating cotton. The base of each cloud is often flat and may be only 1000 meters (3300 feet) above the ground. The top of the cloud has rounded towers. When the top of the cumulus resembles the head of a cauliflower, it is called cumulus congestus or towering cumulus. These clouds grow upward, and they can develop into a giant cumulonimbus, which is a thunderstorm cloud
Stratus clouds are uniform gray clouds that usually cover the entire sky. They can form when very weak, upward vertical air currents lift a thin layer of air high enough to initiate condensation<span>. Stratus clouds also form when a layer of air is cooled from below to its </span>dewpoint<span> temperature and </span>water vapor<span> condenses into liquid droplets. Stratus clouds look like a layer of fog that never reaches the ground. In fact, fog that "lifts" off the ground forms a layer of low stratus clouds. Precipitation rarely falls from true stratus clouds since the upward vertical motion needed for precipitation is very weak, but light mist and drizzle can sometimes accompany stratus clouds</span>
The biotite and/or amphibole will undergo hydrolysis to form clay, and oxidation to form iron oxides.
Chemical weathering of granite occurs when dilute carbonic acid, and other acids present in rain and soil waters, alter feldspar in a process called hydrolysis. Weathering is a time period which describes the overall procedure via way of means of which rocks are damaged down on the Earth’s floor into things like sediments, clays, soils and materials which might be dissolved in water.
The procedure of weathering usually starts off evolved while the earth’s crust is uplifted via way of means of tectonic forces. After the bodily breakup and chemical decay of uncovered rocks via way of means of weathering, the loosened rock fragments and changes merchandise are over excited via the procedure of erosion.
Erosion is based on transporting dealers consisting of wind, rivers, ice, snow and downward motion of substances to hold weathered merchandise far away from the supply area. As weathered merchandise are over excited, clean rocks are uncovered to in addition weathering. Over time, that mountain or hill is step by step worn down.
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