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The mantle of the Earth, composed of semi-solid rock, would respond to gentle, continuous pressure by undergoing a process called plastic deformation. This means that over time, the mantle material would slowly flow and change shape without breaking, allowing it to accommodate the pressure. The rate of this deformation depends on factors such as temperature and the amount of pressure applied. Ultimately, the mantle's ability to respond to this pressure contributes to geological processes like plate tectonics and volcanic activity.
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How would the earth's mantle react under gentle continuous pressure and why?
Under gentle continuous pressure, the Earth's mantle would gradually deform and flow due to its semi-solid, ductile nature. This process, known as mantle convection, occurs because the high temperatures and pressures in the mantle allow for the slow movement of solid rock over geological timescales. As pressure increases, the mantle materials become denser, promoting a slow, viscous flow rather than fracturing. This behavior is essential for the dynamics of plate tectonics and the overall geodynamic processes of the Earth.
Why is the pressure in the center of the earth greater than the pressure in the mantle?
Because towards the center of the earth, there is more mass on top of it, so there is more pressure. All of the other layers, and the stuff on top of the earth is pushing down on it from all sides. For the mantle, its only the stuff on the top of the earth that is putting pressure on it.
What causes the pressure that allows diamonds form in the mantle?
Diamonds are believed to be formed about 90 miles below the surface of the Earth, in the mantle. So, the weight of the Earth above them creates the pressure to form diamonds.
How is the temperature and pressure in the Earth's mantle related to the depth of the mantle?
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
The pressure at the interface between the Mantle and the outer core earth is infertile be approximately what?
The pressure at the interface between the Earth's mantle and the outer core is estimated to be around 1.3 million times atmospheric pressure, or approximately 130 gigapascals (GPa). This extreme pressure results from the weight of the overlying mantle material and the intense conditions found at such depths. This region, known as the core-mantle boundary, plays a crucial role in the dynamics of Earth's geophysical processes.
How would the earth's mantle react under gentle continuous pressure?
it will steady as liquid form and hot
How would the earth's mantle react under gentle continuous pressure and why?
Under gentle continuous pressure, the Earth's mantle would gradually deform and flow due to its semi-solid, ductile nature. This process, known as mantle convection, occurs because the high temperatures and pressures in the mantle allow for the slow movement of solid rock over geological timescales. As pressure increases, the mantle materials become denser, promoting a slow, viscous flow rather than fracturing. This behavior is essential for the dynamics of plate tectonics and the overall geodynamic processes of the Earth.
How would the mantle behave when there is a gentle continious pressure?
Under gentle continuous pressure, the mantle would slowly deform and flow over long periods of time. This gradual movement of the mantle is known as mantle convection, where warmer, less dense rock rises and cooler, denser rock sinks, driving the slow movements of tectonic plates on Earth's surface.
Why is the pressure in the center of the earth greater than the pressure in the mantle?
Because towards the center of the earth, there is more mass on top of it, so there is more pressure. All of the other layers, and the stuff on top of the earth is pushing down on it from all sides. For the mantle, its only the stuff on the top of the earth that is putting pressure on it.
How does the mantle interacts with earth crust?
something about pressure i guess lol :)
What causes the pressure that allows diamonds form in the mantle?
Diamonds are believed to be formed about 90 miles below the surface of the Earth, in the mantle. So, the weight of the Earth above them creates the pressure to form diamonds.
What is a n example of convection in earth system?
An example of convection in the Earth system is the movement of mantle material in the Earth's interior through the process of mantle convection. This movement of hot rock material creates the slow, continuous flow of mantle material that drives tectonic plate movements on the Earth's surface.
How is the temperature and pressure in the Earth's mantle related to the depth of the mantle?
The degree of temperature and exertion of pressure by the molten materials (magma) within the mantle is directly proportional to its depth. This means that, the deeper you go down the mantle the higher the degree of temperature and pressure exerted.
The pressure at the interface between the Mantle and the outer core earth is infertile be approximately what?
The pressure at the interface between the Earth's mantle and the outer core is estimated to be around 1.3 million times atmospheric pressure, or approximately 130 gigapascals (GPa). This extreme pressure results from the weight of the overlying mantle material and the intense conditions found at such depths. This region, known as the core-mantle boundary, plays a crucial role in the dynamics of Earth's geophysical processes.
How was the planets mantle formed?
The earth's mantle would have formed initially in the same way as the crust, by the cooling of the earth but as for the metamorphic rock that defines the earth's mantle, that would have taken millions of years of extreme heat and pressure for it to form.
What pressure is the mantle?
23 g/cookies 5
Which graph shows the best inferred density of earth from the upper mantle to the lower mantle?
To determine the best inferred density of Earth from the upper mantle to the lower mantle, one would typically look for a graph that displays density values increasing with depth. This trend is due to the increasing pressure and temperature conditions as you move deeper into the Earth. A graph that shows a smooth, continuous increase in density, consistent with geophysical models, would be most indicative of the mantle's density profile. Look for key markers indicating the transition zones between the upper and lower mantle, where density changes more significantly.
