Answer:
- prolonged exposure to high pressure zones
- mountain ranges
- cold oceanic currents
Explanation:
All deserts form because of prolonged period of lack of precipitation. That happens because of multiple reasons, with some of them being high pressure zones, mountain ranges, and cold oceanic currents. The high pressure zones are basically consisted of denser, lower air masses which do not allow the low pressure air masses to come in, thus stopping the rainfall. The mountain ranges are a natural barrier, and they manage to stop the wet air masses, so there's lot of rainfall on the windward side, but the leeward side will be very dry. The cold oceanic currents bring in colder and dry weather, with the air masses also being very dense, and while they manage to produce some moisture close to the ground, the rainfall is extremely rare.
1.China
2.India
3.United States
and the 4th if you want it is Indonesia
The answer is D. When carbon-based fuels are burned, they emit carbon dioxide into the atmosphere. Carbon dioxide is a greenhouse gas that causes a greenhouse effect that increases global temperatures hence global warming. However, it is important to note that carbon dioxide is not the only carbon-based greenhouse gas. Methane too is a greenhouse gas, several times more potent than carbon dioxide. Reducing the emission of these greenhouse gases, therefore, mitigates the risk of global warming.
Answer:
They took some gold and slaves from Taino
I hope this helps : )
The cone-shaped structure, or edifice, of the volcano is formed by the symmetrical buildup of lava and/or pyroclastic substance around the central vent system. The central vent is deep connected to a magma chamber, which serves as the primary storage area for eruptive material.
The third type of volcano, shield volcanoes, are almost entirely composed of fluid lava flows. Stream after stream spills out in all ways from a central summit exhaust, or group of vents, forming a broad, gently sloping cone with a profile similar to that of a warrior's shield.
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