The crust
tectonic plates
Earthquakes occur in the crust (solid rock) layer.
The Earth's outermost layer of hard brittle rock is called the crust. The crust is typically about 23 miles thick beneath continents, and about 6.5 miles thick beneath oceans. The crust is relatively light and brittle compared to other Earth layers. Most earthquakes occur within the crust.
Most earthquakes occur where the edges of Earth's plates are.
the crust- most outer layer of earth
The crust is the upper layer of the earth. It is where the movement of plates occur due to which earthquakes occur. The Earth's crust is a thin layer of rock, like skin on an apple.
This is known as the Lithosphere.
This is known as the Lithosphere.
tectonic plates
Earthquakes occur in the crust (solid rock) layer.
The Earth's outermost layer of hard brittle rock is called the crust. The crust is typically about 23 miles thick beneath continents, and about 6.5 miles thick beneath oceans. The crust is relatively light and brittle compared to other Earth layers. Most earthquakes occur within the crust.
Yes that is generally where most earthquakes occur
Most earthquakes occur where the edges of Earth's plates are.
Most earthquakes occur at or near the boundaries between tectonic plates.
Earthquakes occur due to brittle failures in the Earth's lithosphere. Brittle failures occur where fractures propagate through the material. So an earthquake is literally the consequence of fracturing or shattering a part of the brittle outer layer of the earth. It could also be argued that they "shatter" the lives of the people affected by them.
The asthenosphere is too plastic, so it cannot build up stress like the lithosphere can.
Isostasy refers to the balance between the Earth's lithosphere (outermost layer) and asthenosphere (plastic layer below). When the lithosphere undergoes stress, such as due to tectonic forces, it can become imbalanced and adjust to achieve equilibrium. During this adjustment process, known as isostatic readjustment, earthquakes can occur as the rocks rupture and release built-up energy. Hence, isostasy can be a contributing factor to the occurrence of earthquakes.