The crust
Plates beneath the Earth's crust are located in the upper part of the mantle, known as the lithosphere. These plates are constantly moving and interacting with each other, causing geological phenomena like earthquakes, volcanic eruptions, and mountain building.
Beneath Africa, and beneath Europe and Asia
The plates (continental and ocean plates) ride atop the asthenosphere, a layer of viscous rock in the upper mantle beneath the crust.
The pacific oceanic plate is sinking beneath conential plate
The asthenosphere, located in the upper mantle, is easily deformed due to its semi-molten state. This layer allows tectonic plates to move on the ductile rock beneath them.
The lithosphere is the part of the Earth that contains tectonic plates. These plates are divided pieces of the lithosphere that float on the semi-fluid asthenosphere beneath them.
In the center/middle of the plate.
Tectonic plates are located within the Earth's lithosphere, which is the outermost layer of the Earth. These plates float on top of the semi-fluid asthenosphere beneath them. The movement of these plates is responsible for various geological phenomena like earthquakes, volcanic activity, and mountain building.
The lithospheric plates vary in thickness but generally range from 5 to 200 kilometers (3 to 124 miles). Thicker plates are found beneath continents, while thinner plates are located beneath oceans.
The scientific name for the Earth's upper mantle is "asthenosphere." It is a layer of the Earth located beneath the lithosphere and is characterized by its partially molten state, which allows for the movement of tectonic plates.
The Earth's surface is broken into large pieces called tectonic plates. These plates float on the semi-fluid asthenosphere layer beneath them and interact at plate boundaries, where geological phenomena such as earthquakes and volcanic eruptions occur.
there mostly found at earths plates come together and one plate sinks beneath the other