The soft, weak upper portion of the mantle is known as the asthenosphere. It lies beneath the lithosphere and is composed of partially molten rock that allows the rigid lithospheric plates to float and move over it. This movement is a key driver of plate tectonics, leading to geological phenomena such as earthquakes and volcanic activity.
The plates are part of the crust, the upper layer of the Earth. The plates are moved by currents in the upper mantle. The plates and flexible upper mantle are referred to collectively as the lithosphere and sit atop the mantle layer called the aesthenosphere.
The lithosphere, which includes the uppermost portion of the mantle, forms the solid tectonic plates along with the crust. This layer is divided into massive plates that float on the semi-fluid asthenosphere beneath them.
The lithospheric plates are made up of the crust and the uppermost part of the mantle. These plates float on the semi-fluid asthenosphere beneath them.
The lithosphere, which includes the rigid outermost layer of the Earth's mantle, is responsible for the movement and formation of tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with each other at plate boundaries, leading to processes like subduction and spreading.
the plates float on top of the upper mantle
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 solid portion of the upper mantle which behaves as a brittle solid is known as the lithospheric mantle. This part of the upper mantle along with the crust forms tectonic plates.
The crust is the layer at the surface that forms the upper part of the plates. The plates also include a portion of the upper mantle just beneath the crust. Together, the crust and this upper portion of the mantle form the lithosphere.
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.
Sections of Earth's crust that "float" over the upper mantle.
The plates are part of the crust, the upper layer of the Earth. The plates are moved by currents in the upper mantle. The plates and flexible upper mantle are referred to collectively as the lithosphere and sit atop the mantle layer called the aesthenosphere.
The lithosphere, which includes the uppermost portion of the mantle, forms the solid tectonic plates along with the crust. This layer is divided into massive plates that float on the semi-fluid asthenosphere beneath them.
The crustal plates float on the asthenosphere, which is a semi-solid layer of the upper mantle beneath the Earth's crust. This layer allows the crustal plates to move over time due to convection currents in the mantle.
The lithospheric plates are made up of the crust and the uppermost part of the mantle. These plates float on the semi-fluid asthenosphere beneath them.
The lithosphere, which includes the rigid outermost layer of the Earth's mantle, is responsible for the movement and formation of tectonic plates. These plates float on the semi-fluid asthenosphere below and interact with each other at plate boundaries, leading to processes like subduction and spreading.
The moving portion of Earth's crust and upper mantle is known as the lithosphere. It is broken into tectonic plates that float on the semi-fluid asthenosphere below, causing them to move and interact with each other, which leads to processes like earthquakes, volcanic eruptions, and mountain building.