Large segments of the crust and upper mantle known as the Lithospheric plates.
lithenosphere
The crust meets the mantle at the Mohorovičić discontinuity, also known as the Moho. This boundary represents the transition between the Earth's rigid outer layer (crust) and the underlying hotter, more plastic mantle layer.
The crust and the very top of the mantle make up the lithosphere, which is the outermost layer of the Earth. The lithosphere is divided into several tectonic plates that move and interact with each other at plate boundaries.
The crust and the mantle are separated by the Mohorovičić discontinuity, also known as the Moho. This is a boundary that marks the change in composition and density between the Earth's crust and mantle. Seismic waves help scientists study and understand this separation.
The Earth's crust is part of the outermost layer of the Earth, which is composed of the crust and the uppermost portion of the mantle. This layer is known as the lithosphere, which includes both the continental crust and the oceanic crust. Beneath the lithosphere lies the asthenosphere, which is a more ductile part of the upper mantle.
the mantle also known as the athenosphere the crust is also known as the lithosphere
Asthenosphere
lithenosphere
The crust and part of the upper mantle are known as the lithosphere. The lithosphere is the outermost solid shell of Earth that is broken into tectonic plates.
The boundary between the crust and upper mantle is known as the Mohorovičić discontinuity or Moho. It represents the change in seismic wave velocity and composition between the rigid outer layer (crust) and the more ductile layer beneath (mantle).
The Moho separates the crust and the mantle.
The crust meets the mantle at the Mohorovičić discontinuity, also known as the Moho. This boundary represents the transition between the Earth's rigid outer layer (crust) and the underlying hotter, more plastic mantle layer.
A large block of the crust and the rigid outermost part of the mantle is known as a tectonic plate. These plates float on the semi-fluid asthenosphere and interact with each other at plate boundaries, leading to geological phenomena like earthquakes and volcanic eruptions.
The layer of the Earth below the crust is called the mantle. The mantle is the thickest layer of the Earth with a depth of 2,890 kilometers.
The crust and uppermost hard rocky mantle, together, is known as the lithosphere, which is above the plastic-like upper mantle area known as the asthenosphere.
the crust + lithosphere earth's crust: crust crust continental crust lithosphere crust continental and oceanic crust mantle asthenosphere mantle lower mantle mantle outer core outer core inner core inner core
The predominant rock in the Earth's crust and upper mantle is called silicate rock, composed mainly of silicon and oxygen. This type of rock is known as "peridotite" in the mantle and "granite" in the crust.