They are floating on the outer core
Tectonic plates float on the asthenosphere, which is a semi-fluid layer of the Earth's mantle. This allows the plates to move and interact with each other, causing geological phenomena such as earthquakes and volcanic activity.
Lithosphere
Plates float on the semi-fluid asthenosphere layer, which is part of the upper mantle. This layer is under the lithosphere and allows the movement of the tectonic plates.
The outer layer of the earth where the land masses are is called the crust
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 tectonic plates float on the lithosphere. This overlies the asthenosphere.
The tectonic plates, part of the lithosphere, move around and float on the top of the asthenosphere.
They don't. Tectonic plates float on the asthenosphere, as they are a bit less dense.
There called tectonic plates, and they do not float on anything.
There called tectonic plates, and they do not float on anything.
Tectonic plates float on the mantle because they are less dense
There called tectonic plates, and they do not float on anything.
Tectonic plates float on the mantle because they are less dense
Tectonic plates float on an underlying molten layer.
Tectonic plates are segments of the lithosphere. They float on top of the asthenosphere.
Tectonic plates float on the asthenosphere, which is a semi-fluid layer of the Earth's mantle. This allows the plates to move and interact with each other, causing geological phenomena such as earthquakes and volcanic activity.
The continental plates float on asthenosphere, molten rock (lava).