The crust and the upper mantle together are referred to as the lithosphere. This rigid layer is characterized by its solid structure and extends from the Earth's surface down to about 100 kilometers (62 miles) deep. The lithosphere plays a crucial role in tectonic activity, as it is divided into tectonic plates that float on the more fluid asthenosphere beneath.
It is called the lithosphere.
The other name for crust is lithosphere, which refers to the solid outer layer of the Earth that includes the crust and the upper part of the mantle.
The boundary between the Earth's crust and the upper mantle is called the Mohorovičić discontinuity, commonly referred to as the "Moho." This boundary marks a transition from the relatively rigid and lighter materials of the crust to the denser, more ductile materials of the upper mantle. The Moho is significant in geophysics and geology, as it helps to understand the composition and behavior of the Earth's interior.
The crust and the upper part of the mantle are the solid part of the Earth called the lithosphere.
The area of Earth that forms the land is called the lithosphere. It includes the outermost layer of the Earth, which consists of the crust and the upper part of the mantle.
Lithosphere
It is called the lithosphere.
The other name for crust is lithosphere, which refers to the solid outer layer of the Earth that includes the crust and the upper part of the mantle.
The Earth's Crust
The rocky upper layer of the solid Earth is called the crust.
The Earth's crust is also known as the "lithosphere" but that term geologically includes the upper elastic part of the mantle.
The rocky upper layer of the solid earth is called the crust.
The upper rocky layer of Earth is called the lithosphere. It includes the Earth's crust and the uppermost part of the mantle.
The name of the topmost crust of the Earth is the "lithosphere." It includes the Earth's crust and part of the upper mantle and is divided into several large tectonic plates that float on the semi-fluid asthenosphere beneath them.
The crust is the outermost solid shell of the planet. It is chemically different from the underlying mantle. The scientific name for the crust is the lithosphere. It has an average thickness of 30-35 kilometers in continental areas and 5 kilometers in oceanic areas.
The lithosphere, it consists of two parts, a thin outside layer of solid rock called the crust and the rigid upper part of the mantle.
The crust and the upper part of the mantle are the solid part of the Earth called the lithosphere.