The movement of magma through the Earth's crust is known as intrusion.
This is known as a fault. A fault is a fracture in the Earth's crust along which movement has occurred. Movement along faults can result in earthquakes.
the mantle also known as the athenosphere the crust is also known as the lithosphere
The "crust" or biosphere
A crack in the rocks of the earth's crust where no movement has occurred is known as a joint. Joints are fractures in the rocks that do not show any displacement and are caused by stress or pressure within the earth's crust. They often provide pathways for fluids to move through the rocks.
Heat transfer from the mantle creates convection currents that drive the movement of Earth's crustal plates. As hotter mantle material rises, it pushes the crust apart at mid-ocean ridges, while cooler material sinks, pulling the crust down in subduction zones. This movement of the crust is known as plate tectonics.
It is known as a 'fault'.
The sphere that extends from Earth's core to Earth's crust is known as the mantle. It is the layer of the Earth located between the core and the crust and consists of solid rock that is capable of flowing over long periods of time. The mantle plays a crucial role in the movement of tectonic plates and the convection currents that drive the Earth's geological processes.
The movement of the Earth's plates is known as plate tectonics. Geologists think the plates move due to a build up of extreme heat in the Earth's crust.
The result is commonly known as an earthquake.
A fractured surface on Earth's crust when a mass of rocks is in motion is known as a fault. It occurs due to the movement of tectonic plates along a fracture line. This movement can result in earthquakes as energy is released when the rocks slide past each other along the fault.
A crack in the earth's crust is known as a fault. Faults form when tectonic plates shift and release stress, causing the rock to break and create fractures. These fractures can vary in size and can lead to earthquakes if there is sudden movement along the fault line.
A crack in the Earth's crust caused by tectonic plate movement is known as a fault. Faults occur when stress from the movement of tectonic plates exceeds the strength of rocks, leading to a fracture. The movement along these faults can result in earthquakes, as the rocks on either side slip past each other. The study of faults is crucial for understanding seismic activity and assessing earthquake risks.