The outer layer of the earth where the land masses are is called the crust
Lithosphere
The pieces of the Earth's crust are called tectonic plates. These plates float on the semi-fluid layer of the Earth's mantle and interact with each other, causing movements such as earthquakes and volcanic activity.
The Earth's outer layer, or lithosphere, is broken into sections called tectonic plates. These plates float on top of the semi-fluid asthenosphere beneath them and interact with each other at plate boundaries, causing movements such as earthquakes and volcanic activity.
The plates that make up the Earth's crust are called tectonic plates. These plates float on the semi-fluid asthenosphere underneath and interact with each other at plate boundaries, causing various geological phenomena such as earthquakes and volcanic activity.
They are floating on the outer core
There called tectonic plates, and they do not float on anything.
There called tectonic plates, and they do not float on anything.
Lithosphere
The tectonic plates, part of the lithosphere, move around and float on the top of the asthenosphere.
There called tectonic plates, and they do not float on anything.
The pieces of the Earth's crust are called tectonic plates. These plates float on the semi-fluid layer of the Earth's mantle and interact with each other, causing movements such as earthquakes and volcanic activity.
The earth's tectonic plates are said to "float" on layers of magma, which is molten, or very hot liquid rock deep under the surface of theearth.
plates of the earth's crust that float on top of the molted mantle layer.
Magma is lava underneath the earth. The tectonic plates of the earth float on it.
The Earth's outer layer, or lithosphere, is broken into sections called tectonic plates. These plates float on top of the semi-fluid asthenosphere beneath them and interact with each other at plate boundaries, causing movements such as earthquakes and volcanic activity.
plates
The tectonic plates float on the lithosphere. This overlies the asthenosphere.