It is cause by the Mojo Discontinuity.
It is a zone that differs in density.
A crack in the Earth's crust that can lead to an earthquake is called a fault.
the focus of an earthquake is beneath the surface of the earth in the crust.
Seismic, or earthquake waves travel through the earth. They may travel through our crust, which is rocky, or through the more fluid parts, like the mantle, but the medium is the earth.
An earthquake
Earth's crust shift into each other causing an earthquake
earthquake waves travel through the earths crust.
The plate within the crust where an earthquake occurs is often along a fault line, where two tectonic plates are in contact. When stress builds up along the fault line and is released suddenly, it causes the plates to move, resulting in an earthquake.
Earthquake is a noun. It refers to a sudden and violent shaking of the ground caused by movements within the earth's crust.
An earthquake is a sudden and violent shaking of the ground, it is caused by movements within the earth's crust or volcanic action.
The Earth's crust is where earthquakes typically occur. When tectonic plates, which make up the crust, slide against each other, it can build up stress that is eventually released as an earthquake. The crust's composition and structure play a significant role in how seismic waves travel during an earthquake.
When an earthquake occurs, seismic waves travel outward from the focus (the point where the earthquake originates) through the Earth's crust and mantle. These waves can be detected by seismometers and help scientists study the characteristics of the earthquake and the structure of the Earth's interior.
The point within the earth where the earthquake occurs is known as the focus or hypocentre. The point directly above this on the earth's surface is known as the epicentre.
An Anticline is formed when the crust bends and curves upward.
The starting point of an earthquake is called the focus or hypocenter, which is located beneath the Earth's surface where the earthquake originates. It is typically several kilometers deep within the Earth's crust.
An earthquake typically involves the lithosphere, which includes the outermost layer of the Earth's crust and the top part of the mantle. The interaction and movement of tectonic plates within the lithosphere are mainly responsible for causing earthquakes.
Earthquake waves travel fastest in the interior of the Earth, as speed of waves increases as we go inside the Earth. The speed of a wave depends on the properties of the medium it travels in. The wave propagates faster in the denser and heavier core.
A crack in the Earth's crust that can lead to an earthquake is called a fault.