Krakatoa last erupted in 1883, resulting in one of the most powerful volcanic events in recorded history. The eruption caused tsunamis up to 131 feet high, destroyed over two-thirds of the island, and resulted in tens of thousands of deaths.
Seismic activity generates seismic waves. These waves can be classified into two main types: body waves that travel through the Earth's interior (P-waves and S-waves) and surface waves that travel along the Earth's surface (Love waves and Rayleigh waves).
The energy source of tsunami waves is much greater The energy source of Tsunami waves is much greater
Yes. Krakatoa is a volcano prone to violent eruptions and it probably will erupt violently again. While it periodically has small eruptions,we might not see another one on the scale of the 1883 eruption for a few thousand years.
Red (low end) & Violet (high end).
The effect of two or more waves interacting that caused them to cancel out is
Krakatoa last erupted in 1883, resulting in one of the most powerful volcanic events in recorded history. The eruption caused tsunamis up to 131 feet high, destroyed over two-thirds of the island, and resulted in tens of thousands of deaths.
Body waves Body waves and surface waves are the two types of seismic waves formed during great earthquakes. P waves and S waves are called body waves because they travel through the body of the Earth. Surface waves Love waves and Rayleigh waves travel only on the surface of the Earth and cause the most destruction.
The two types of waves in radio waves are AM (amplitude modulation) and FM (frequency modulation). In gamma rays, there are no different types of waves as they are all high-energy electromagnetic waves.
Sound waves and water waves are similar in that they are both caused by vibrations and carry energy. They are different in that a sound waves are three dimensional, while water waves are just two dimensional.
Earthquake waves are called seismic waves. There are two main types of seismic waves: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface. These waves are responsible for the shaking and damage caused by earthquakes.
Gravitational waves are caused by the acceleration of massive objects, such as when two black holes merge or when two neutron stars collide. As these objects move in spacetime, they create ripples that propagate outward at the speed of light, carrying energy away from the system. These ripples are what we observe as gravitational waves.
The waves from an earthquake that travel through the Earth's interior are known as body waves. There are two types of body waves: P-waves (primary waves) and S-waves (secondary waves). These waves contribute to the shaking and damage caused by an earthquake.
When two sound waves that are close in pitch interact, it creates a phenomenon called beating. This is heard as a pulsating increase and decrease in loudness, caused by the periodic reinforcement and cancellation of the waves.
Seismic activity generates seismic waves. These waves can be classified into two main types: body waves that travel through the Earth's interior (P-waves and S-waves) and surface waves that travel along the Earth's surface (Love waves and Rayleigh waves).
There are two general factors that are needed to produce very high waves. These are geographical location and seafloor topography. Wind is what creates the energy that creates waves.
The energy source of tsunami waves is much greater The energy source of Tsunami waves is much greater