The proces is called convection
The proces is called convection
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.
Convection
The circulation within Earth's mantle is called mantle convection. This process involves the movement of hot material rising and cool material sinking in the mantle, creating convection currents that drive plate tectonics.
No, the asthenosphere is located beneath the lithosphere in the Earth's mantle. It is a semi-fluid layer that allows for the movement of tectonic plates.
The proces is called convection
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.
The scientific name for the Earth's upper mantle is "asthenosphere." It is a layer of the Earth located beneath the lithosphere and is characterized by its partially molten state, which allows for the movement of tectonic plates.
Convection
Convection
One special feature of Earth's crust is that it is divided into tectonic plates that float and move on the semi-fluid upper mantle. This movement causes earthquakes, volcanoes, and the formation of mountain ranges.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
QuestionThe term for the circular movement of material inside earth's mantle is convection current. This current causes the movement of the tectonic plates.
The mantle viscosity, or thickness of the Earth's mantle, affects the movement of tectonic plates. A more viscous mantle slows down plate movement, while a less viscous mantle allows for faster plate movement. This relationship influences the speed and direction of tectonic plate motion.
Plasticity means that there is enough movement in the asthenosphere to allow thelithospheric plates to move.