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Tectonic plates are segments of the lithosphere. They float on top of the asthenosphere.
The tectonic plates float on the lithosphere. This overlies the asthenosphere.
Asthenosphere
The plates of lithosphere float on top of the semi-fluid asthenosphere, which is located beneath the lithosphere in the Earth's upper mantle. The asthenosphere allows the plates to move and interact with each other due to its partially molten and more ductile nature compared to the lithosphere above it.
The large sections of lithosphere that float on the asthenosphere are called tectonic plates. These plates are rigid sections of Earth's lithosphere that move and interact with each other at plate boundaries, causing geological phenomena like earthquakes and volcanic eruptions.
The tectonic plates, part of the lithosphere, move around and float on the top of the asthenosphere.
Plates of the lithosphere float on the semi-fluid asthenosphere beneath them. The movement of these plates is driven by the heat and convection currents within the Earth's mantle. This movement is responsible for phenomena like earthquakes, volcanic activity, and the formation of mountains.
Plates of the lithosphere do not float on the core. They float on the asthenosphere (plastic mantle). Due to convection currents and the earths rotation, plates glide over the asthenosphere. This theory is the theory of Plate Tectonics.
Plates of the lithosphere float on the semi-fluid asthenosphere, which is the upper portion of the mantle beneath the Earth's crust. The movement of these plates is driven by the heat generated from the Earth's core, causing them to drift and interact with one another at plate boundaries.
The asthenosphere lies beneath the lithosphere, which is where the tectonic plates lie. Because of the high temperature, the asthenosphere has the property to flow (plasticity); the tectonic plates "float" on this flow.
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.
Because of something called Isostacy-the gravitational equilibrium between lithosphere and asthenosphere, such that plates "float" at an elevation that dependes on the thickness and density. EX. Think floating ice cubes