The correct answer is...
Convection and the release of heat from the Earth's core drives further convection in the mantle. Convection in the mantle drives plate tectonic motion of the sea floor and continents.
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Because the Earth's magnetic field arises in the unstable patterns of fluid flow in the core, it changes direction an irregular intervals. In recent geologic history it may have switched direction about every 200,000 years. Any kind of geologic deposit put down over time will thus have different layers magnetized in opposing directions, recording the magnetic field as it was when the layer solidified.
No, earthquakes can occur anywhere in the crust, oceanic crust or continental crust. An earthquake occurs when the hard brittle solid material of the crust fractures under stress. Earthquakes cannot occur deeper than the crust (the mantle is plastic and flows slowly under stress instead of fracturing, the outer core is liquid and flows even easier than the mantle).
Convection occurs mainly in the mantle, which is the layer beneath the Earth's crust. The heat generated by the core causes convection currents in the mantle, leading to the movement of tectonic plates.
Convection currents occur in the Earth's mantle, which is the layer beneath the Earth's crust. These currents are responsible for driving the movement of tectonic plates on the Earth's surface, leading to phenomena like earthquakes and volcanic activity.
35 - 60 Kms would be the uppermost mantle, which along with the crust forms the hard, brittle lithosphere. The Mantle is a semi-molten layer.
Heat transfer in the Earth's mantle drives the movement of the Earth's crust through the process of convection. As mantle material heats up, it becomes less dense and rises, causing the overlying crust to move. At the same time, cooler mantle material sinks back down, completing the cycle of heat transfer and driving the continuous motion of tectonic plates.
The proces is called convection
Crust and Mantle.
The convective currents in the mantle, driven by heat from the Earth's core, allow for the movement of the Earth's crust. This movement results in phenomena like plate tectonics, where tectonic plates interact at their boundaries, leading to earthquakes, volcanoes, and the creation of mountains.
mantle
No, earthquakes can occur anywhere in the crust, oceanic crust or continental crust. An earthquake occurs when the hard brittle solid material of the crust fractures under stress. Earthquakes cannot occur deeper than the crust (the mantle is plastic and flows slowly under stress instead of fracturing, the outer core is liquid and flows even easier than the mantle).
No. Convection currents which could lead to volcanism in the crust occur in the mantle. The crust is too cold and brittle for convection currents to occur.
Convection occurs mainly in the mantle, which is the layer beneath the Earth's crust. The heat generated by the core causes convection currents in the mantle, leading to the movement of tectonic plates.
The crust is compressed into mountains (if it is continental crust) or subducted back into the mantle if it is oceanic crust.
Convection currents occur in the Earth's mantle, which is the layer beneath the Earth's crust. These currents are responsible for driving the movement of tectonic plates on the Earth's surface, leading to phenomena like earthquakes and volcanic activity.
the mantle
The crust moves in 1 direction at a hotspot due to the convection currents of the mantle
Heat transfer from the mantle creates convection currents that drive the movement of Earth's crustal plates. As hotter mantle material rises, it pushes the crust apart at mid-ocean ridges, while cooler material sinks, pulling the crust down in subduction zones. This movement of the crust is known as plate tectonics.