the earths crust
Tectonic Plates
The lithosphere is broken up into sections called tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with one another at plate boundaries, where most earthquakes and volcanic activity occur.
No, the Earth's crust is broken into sections called tectonic plates, not bowls. These plates float on the semi-fluid asthenosphere below and interact with each other at their boundaries, which can lead to geological activity like earthquakes and volcanoes.
it's a lithosphere
The lithosphere, which is the outermost layer of the Earth, is responsible for making up the tectonic plates. It includes the crust and upper part of the mantle and is broken up into various plates that are in constant motion due to the underlying mantle convection currents.
Tectonic plates.
Tectonic Plates
Tectonic Plates
The lithosphere is broken up into sections called tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with one another at plate boundaries, where most earthquakes and volcanic activity occur.
Earth Quake
The Earth's lithosphere is broken up into tectonic plates. The lithosphere is the outermost rigid layer of the Earth, and it includes the crust and the uppermost part of the mantle.
No, the Earth's crust is broken into sections called tectonic plates, not bowls. These plates float on the semi-fluid asthenosphere below and interact with each other at their boundaries, which can lead to geological activity like earthquakes and volcanoes.
The lithosphere is the layer that moves with the tectonic plates. The lithosphere is made up of the crust and the upper part of the mantle, and it is broken into tectonic plates that move and interact with each other.
It is broken up into pieces called tectonic plates
The lithosphere is the layer of the Earth that is broken up into tectonic plates. These plates are like puzzle pieces that move and interact with each other, causing geological phenomena like earthquakes and volcanic activity.
it's a lithosphere
Earth's rigid outer layers are broken up into tectonic plates, which float on the semi-fluid asthenosphere below. These plates move relative to each other, causing phenomena like earthquakes, volcanic activity, and mountain-building.