The S-wave.
The crust moves like globe, for example. you know how there is rings around it? that will be the crust and the ball will be the mantle. Spin the rings, not the globe. the crust moves AROUND the mantle
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
Seismic waves move outward from the source of an earthquake. These waves carry the energy released during the earthquake and can cause shaking and damage as they propagate through the Earth's crust.
The mantle is a layer of rock below the Earth's crust that moves due to convection currents caused by heat from the core. The core is the Earth's innermost layer made of iron and nickel. The mantle interacts with the crust through tectonic plate movements that can cause earthquakes, volcanic eruptions, and the formation of mountain ranges.
Convection currents in the mantle create plate tectonics.
The crust moves on a plastic like layer of the mantle.
The crust moves on a plastic like layer of the mantle.
An earthquake moves due to the plates under the Earth's crust moving
The crust moves like globe, for example. you know how there is rings around it? that will be the crust and the ball will be the mantle. Spin the rings, not the globe. the crust moves AROUND the mantle
In a sense, yes. The oceans lay on top of the crust. As the crust moves on top of the mantle at a speed roughly equivalent to the rate of fingernail growth, the ocean gets out of the way.
the lithosphere.
A sudden movement of the Earth's crust is called an earthquake.
The crust moves in 1 direction at a hotspot due to the convection currents of the mantle
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
The older oceanic crust moves away from the spreading center and is eventualy subducted back into the mantle.
Mantle plumes are in the mantle, BELOW the Earth's crust. The circulation of heat from the lower mantle to the upper mantle can cause "hot spots" in the overlying crust, heating the magma in the areas.
Moho barrier: Top of mantleOceanic crust: Thinnest layerUpper mantle: Moves the crustLower mantle: Borders liquid core