Convection currents rese and sink through the mantle and the liquid outer core. In Earth's mantle, large amounts of heat are transferred by convection currents. Heat from the core and the mantle itself causes convection currents in the mantle.
The lower part of the Mantle is liquid.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
The liquid core of Earth is surrounded by the solid mantle and crust. This liquid outer core is mostly composed of iron and nickel, and it is responsible for generating Earth's magnetic field through convection currents.
Convection in Earth's mantle drives the motion of tectonic plates. As the mantle heats up and rises, it moves the plates above it in a process known as plate tectonics. This convection helps create features like mountains, volcanoes, and earthquakes.
Convection movements; currents in Earth's interior. Note that a significant part of Earth's interior is liquid.
Convection currents rese and sink through the mantle and the liquid outer core. In Earth's mantle, large amounts of heat are transferred by convection currents. Heat from the core and the mantle itself causes convection currents in the mantle.
convection occurs in the asthenosphere, which is located under the lithosphere. the inner core heats the liquid mantle and it circles and produces plate tectonic activity.
The lower part of the Mantle is liquid.
If Earth's interior cools to a non liquid state, the convection currents will stop.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core
Moho barrier=where crust meets the mantle Oceanic crust=Thinnest layer
The liquid core of Earth is surrounded by the solid mantle and crust. This liquid outer core is mostly composed of iron and nickel, and it is responsible for generating Earth's magnetic field through convection currents.
The mantle layer with more convection is the upper mantle, which has a higher temperature and undergoes vigorous convection currents. In contrast, the lower mantle has less convection due to its higher pressure and lower temperature, leading to slower convective movement.
hotspots
Convection in Earth's mantle drives the motion of tectonic plates. As the mantle heats up and rises, it moves the plates above it in a process known as plate tectonics. This convection helps create features like mountains, volcanoes, and earthquakes.
hotspots