Answer:
brackets?
Explanation:
Respuesta: El viento, la vegetación, el agua y el ser humano.
Answer:
The inner core is not liquid or even molten
Explanation:
So, false.
Answer: False
Explanation: Â I learned this in College Class! The reason it is False is that the Earth's inner core is the innermost geologic layer of the planet Earth.
The type of hard stabilization which increases beach erosion are - Groin and Jetty.
Beach erosion, often referred to as coastal erosion, is a process wherein local sea level rise, powerful wave action, and coastal flooding wear down or carry away rocks, soils, or sands along the coast.
Strong storms and sea level rise can degrade beaches, but human activities like coastal development and the building of inlets and navigation channels have made the problem worse and altered how water and sand move naturally. One of the most obvious signs of coastal erosion is the formation of sea cliffs. Sea cliffs are the precipitous faces of rock and earth created by wrathful waves. The shoreline is eroded by waves pounding against it until a notch is created.
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Once an air parcel reaches the hurricane's eyewall, it turns upward and rises due to a process called convection.
The inward drop in air pressure in a hurricane allows inward flowing air to cool below the sea-surface temperature, which in turn allows more heat to flow in from the sea.
Due to low pressure at its center, twists stream toward the focal point of the tempest and air is constrained vertical. High in the climate, winds stream away from the tempest, which permits additional air from underneath to rise. The air that ascents should be warm and wet so it frames the billows of the tempest.
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The answer is B. Layers of soil get rockier as they get deeper.
Soil is in essence mature while it accomplishes a dampness stage that licenses it to hinder into bunches estimating 1-10 mm. (With a superior dampness content, the dirt adheres to the culturing carry out; with a diminishing dampness content, the dirt breaks into large bunches and blocks.)
A soil can not be more experienced than the most seasoned hedges creating in it. It can not be more seasoned than the substances wherein it desk work or the display on which it's far found. Soil researchers compositions with geologists to conclude how one of a kind the display is, and the manner in which extensive the figure substances had been there.
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A prolonged period of freezing weather with sizable glaciers covering the majority of the planet is known as an ice age, and when these glaciers melt, they can have a significant impact on the environment.
The effects of ice age glaciers include altered air currents and weather patterns, the conversion of once dry regions into wet ones, the formation of lakes, and isostatic depression.
Weather and air movement: Air flows counterclockwise around low pressure areas, such as the warm air around the equator, as a result of the earth's rotation. This causes air to move from left to right or from west to east. Imagine the jet stream as a river of air that carries weather throughout the world by transferring air masses from west to east.
Dry regions: A dry environment is one where alcohol consumption is prohibited. A dry area is intended to reduce alcohol-related issues and anti-social behaviour in public places like reserves and major commercial districts.
Lake formation: Landslides or mudslides that send dirt, rock, or mud tumbling down mountains and hillsides can also produce lakes. Natural dams formed by the accumulation of debris can stop a stream from flowing and cause a lake to form. Beavers can block rivers or streams and create vast ponds or marshes by creating dams out of tree branches.
Idiopathic depression: Large portions of the Earth's crust descend into the asthenosphere as a result of isostatic depression, which is frequently brought on by glacial ice during continental glaciation. Centimeters per year are lost to isostatic depression and rebound.
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A change in wind direction is a weather phenomenon that will always occur when flying across a front.
Wind direction is contingent upon the course from what or to which place it originates. For example, a boreal wind blows from northward to the west side when facing north. The wind is the flow of air that happens as it is fiery for one sun and so rises. Wind direction is calculated concerning valid northward (not compass point) and is reported from what or to which place the wind is tumbling.
On Earth, ordinary weather phenomenon involve wind, clouds, rain, snowstorm, fog, and dust storms. Less common occurrences contain everyday troubles to a degree whirlwinds, hurricanes, typhoons, and ice storms. Almost all knowledgeable weather phenomenon happen in the air (the lower contained the air).
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