<span>Igneous RockBelow the hard, solid lithosphere, Earth’s interior contains hot, melted rocks in liquid form. When liquid rock cools, it solidifies to become igneous rock. The lava that flows from a volcano can cool to form the igneous rock basalt. Molten material deep within Earth can form the igneous rock granite.
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The answer is The Great Basin. For the most part, its eastern limit is the Wasatch Mountains of Utah and the western edge is framed by the Sierra Nevada and Cascade Mountains that make a rain shadow over a great part of the Great Basin, keeping numerous Pacific tempests from achieving the district.
The Great Basin Desert, the biggest U. S. leave, covers a dry span of around 190,000 square miles and is circumscribed by the Sierra Nevada Range on the west and the Rocky Mountains on the east, the Columbia Plateau toward the north and the Mojave and Sonoran betrays toward the south.
After looking at the map/picture you have given above. There are several reasons why location D has a cooler climate than location E. Some of the reasons are a higher altitude, father north of the equator, location E is closer to the equator.
The three zones to be to be classified of a river system are as following:-
- Zone of sediment production (Streams in the mountain)
- Zone of sediment transportation (River in between the mountain and shore)
- Zone of sediment deposition (Streams that end at the shore)
<h3><u>Explanation:-</u></h3>
Production of sediment will fall under initial zones. Sediment may be created in a variety of ways, such as when igneous and metamorphic rocks are exposed to wind and water and weather. decay of the wildlife and plants. However, the majority of sediments are produced when rocks are broken down by streams, rivers, and other moving bodies of water. Rocks may also be weathered extensively by wind. sediment formed by the weathering of rocks is found in the first zone.
The second zone will cover sediment transport. The slope (which may be caused by any type of landform) allows the produced sediment to flow and travel downhill, according to the diagram.
Under the third zone, sediment deposition occurs. Because the flow of the streams ceases at the bottom, all carried silt will be deposited there.
To know more about the zones of a river system, click the links.
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