The crust and the lithosphere.
Studies of earthquake waves passing through Earth support the conclusion that the Earth has distinct layers with varying densities and composition. This is because seismic waves travel at different speeds and paths as they move through different layers, providing information about the internal structure of the Earth.
Intense vibrations felt throughout Earth's crust during an earthquake are called seismic waves. These waves are responsible for shaking and transmitting energy through the Earth's layers, leading to the ground motion experienced during an earthquake.
A seismic wave travels through the Earth's layers, after a volcano, explosion, or earthquake. Transverse, compressional, longitude, and shear waves are all types of seismic waves after earthquakes.
The Earth's crust is cracked during an earthquake. The crust is the outer layer of the Earth and is made up of several large and small tectonic plates that shift and slide against each other, causing the release of seismic energy. These cracks, known as faults, are responsible for the formation of earthquakes.
An Earthquake
Earthquake waves travel through the Earth at different speeds depending on the type of material they pass through. By studying how these waves travel and are reflected at boundaries between layers, scientists can determine the different properties and boundaries of the Earth's layers, such as the crust, mantle, outer core, and inner core.
Oceanic crust
Studies of earthquake waves passing through Earth support the conclusion that the Earth has distinct layers with varying densities and composition. This is because seismic waves travel at different speeds and paths as they move through different layers, providing information about the internal structure of the Earth.
These vibrations change speeds and directions when they go into different layers of the Earth.
Intense vibrations felt throughout Earth's crust during an earthquake are called seismic waves. These waves are responsible for shaking and transmitting energy through the Earth's layers, leading to the ground motion experienced during an earthquake.
A seismic wave travels through the Earth's layers, after a volcano, explosion, or earthquake. Transverse, compressional, longitude, and shear waves are all types of seismic waves after earthquakes.
A seismic wave is a wave of energy that travels through the Earth's layers away from an earthquake in all directions. There are two main types of seismic waves: P-waves (primary waves) and S-waves (secondary waves), with P-waves being faster and able to travel through both solid and liquid layers of the Earth.
The two layers of the Earth involved in earthquakes are the crust and the lithosphere. Earthquakes are commonly caused by the movement of tectonic plates within the lithosphere, which is the rigid outer layer of the Earth that includes the crust.
The Earth's crust is cracked during an earthquake. The crust is the outer layer of the Earth and is made up of several large and small tectonic plates that shift and slide against each other, causing the release of seismic energy. These cracks, known as faults, are responsible for the formation of earthquakes.
Energy released during an earthquake creates seismic waves that travel through the Earth's crust, causing the ground to shake. This energy can also lead to the displacement of rock layers, fractures in the Earth's surface, and the generation of secondary hazards such as landslides and tsunamis.
no...the earthquake did not cause a hole in the earth
It is Napier and Hastings who were involved of course