Tsunamis or tidal waves.
A seismograph is the graph that shows vibrations caused by an earthquake. It records the movement of the ground in a vertical direction as the seismic waves pass through the Earth's crust.
Sound energy is caused by vibrations in air or water. These vibrations create waves that travel through the medium and are picked up by our ears as sound.
Seismic waves are vibrations that travel through the Earth's layers during an earthquake, whereas a tsunami is a series of large ocean waves caused by displacement of water, often triggered by an undersea earthquake, volcanic eruption, or landslide. Seismic waves originate within the Earth, while tsunamis occur on the ocean's surface.
Vibrations in the Earth caused by sudden movements of rock are called earthquakes. These movements typically occur along geological faults, where stress builds up until it is released, resulting in seismic waves that propagate through the Earth. The intensity and duration of these vibrations can vary, depending on the magnitude of the earthquake and the geological conditions.
visable energy is light such as sunlight, but now sure what energy is both visable and caused by vibrations
Seismic waves: longitudinal compression waves.
Sound energy is the energy caused by objects' vibrations. Sound energy travels in waves through a medium such as air, water, or solids, carrying the vibrations produced by the object.
A seismometer is the instrument used to measure waves, such as seismic waves, within the Earth. This device detects and records the vibrations caused by seismic events like earthquakes. Seismometers are essential tools for studying the structure and properties of the Earth's interior.
The instrument that detects seismic waves is called a seismometer or seismograph. It measures the vibrations caused by seismic waves in the Earth's crust and can help to monitor and study earthquakes.
things that can cause seismic waves are earthquackes
Seismometers are instruments that measure Earth's vibrations, also known as seismic waves. These devices can detect and record ground movement caused by natural events like earthquakes or human activities such as explosions.
The vibrations caused by rocks breaking and moving due to a sudden release of energy are known as seismic waves. These waves are generated during events like earthquakes when accumulated stress along geological faults exceeds the strength of rocks, leading to their rupture. The primary types of seismic waves are P-waves (primary waves), which are compressional, and S-waves (secondary waves), which are shear waves. Together, they propagate through the Earth and can be detected by seismometers, helping scientists study the Earth's interior and assess seismic activity.