The concept of plate tectonics has revolutionized the explanation about how earthquakes occur in Earth Sciences. Plate tectonics tells us that the Earth's rigid outer shell (lithosphere) is broken into a mosaic of oceanic and continental plates which can slide over the plastic aesthenosphere, which is the uppermost layer of the mantle. The plates are in constant motion. Where they interact, along their margins, important geological processes take place, such as the formation of mountain belts, earthquakes, and volcanoes.
the lithoseshere
Chitin
No, the rocks in the earth at that depth are too rigid and plastic-like to store the amount of stress needed for an earthquake to occur.
rotating a given rigid point about x or y axis is called a rotaion in CG.
Earth's plastic-like layer is called the lithosphere. It is the rigid outer layer of the Earth, consisting of the crust and the upper part of the mantle. It is broken into pieces called tectonic plates that float on the semi-fluid asthenosphere underneath.
The outermost rigid layer of the Earth is called the lithosphere. It includes the crust and uppermost part of the mantle and is divided into tectonic plates that float on the semi-fluid asthenosphere below.
The uppermost part of the mantle with liquid and plastic properties is called the asthenosphere. It is a semi-fluid layer located beneath the rigid lithosphere that allows for the movement of tectonic plates.
It is called the asthenosphere, the layer of hot, ductile rock directly below the lithosphere.
The rocky rigid layer of the Earth is called the lithosphere. It consists of the crust and the uppermost part of the mantle and is divided into several tectonic plates that float on the semi-fluid asthenosphere beneath.
Earth's plastic-like layer is referred to as the lithosphere, which is the rigid outer layer of the Earth that includes the crust and the upper part of the mantle.
The rigid layer of the Earth surrounding the asthenosphere is called the lithosphere. It is composed of the crust and the uppermost part of the mantle, and it is broken into tectonic plates that float on the semi-fluid asthenosphere below.
The rigid layer of rock in the Earth's crust is called the lithosphere. It is made up of the crust and the outermost part of the mantle, and it is divided into tectonic plates that float on the semi-fluid asthenosphere beneath them.
The rigid upper layer of the Earth is called the lithosphere. It is composed of the crust and the uppermost part of the mantle, and it is broken into tectonic plates that float on the semi-fluid asthenosphere below.
The rigid layer that includes the upper part of the mantle and the crust of the Earth is called the lithosphere. This layer is divided into several tectonic plates that float on top of the partially molten asthenosphere below. The lithosphere is responsible for the movement of tectonic plates and the formation of geological features on Earth.
The crust and the upper mantle together are called the lithosphere. The lithosphere is a rigid outer layer of the Earth that is broken into tectonic plates.
The rigid outer layer of Earth is called the lithosphere. It is composed of the crust and the uppermost part of the mantle, and it is broken up into tectonic plates that float on the semi-fluid asthenosphere below.