Earthquakes are caused when energy is released as the lithosphere (crust and upper mantle) of the Earth moves. Energy is emitted in the form of waves. There are different types of waves, some move faster, slower, sideways, or up and down. A seismograph records these waves on a seismogram.
The seismic waves that cause the majority of damage in earthquakes are the surface waves of which there are two types.
Mostly wind. Earthquakes can also cause waves.
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
The height of the wave in the earthquakes depends with the earthquake in question.
Seismic waves Types: Primary waves Secondary waves Surface waves
The four types of plate movements that can cause earthquakes are convergent boundaries, divergent boundaries, transform boundaries, and subduction zones. These movements can result in the buildup of stress within the Earth's crust, which may eventually be released in the form of an earthquake.
Earthquakes can cause several types of damage. Some of the major damage they can cause are collapsed building, sinkholes, tsunamis, and loss of life.
Earthquakes and volcanoes! Also earthquakes can in turn cause tsunami.
They are both can cause damage and they are both types of earthquakes.
A seismic wave known as the Love wave typically has the largest amplitude. These are surface waves that travel through the Earth's crust and have a horizontal motion that can cause significant shaking during earthquakes.
Yes
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.