Only in extremely rare instances. Most tsunamis; those triggered by earthquakes, landslides, and volcanic eruptions cannot reach cloud base. However, the tsunamis triggered by large asteroid impacts can be thousands of feet high and could reach up to cloud level.
Rarely. Most tsunamis, which are triggered by earthquakes, do not exceed 50 feet in height, but even a 10 foot tsunami wave can be very destructive.
In deep ocean water, the speed of a tsunami can exceed 500 mph but the wave height may be only a few feet. As the tsunami approaches shallow water and the sea floor rises, the speed decreases while the wave height increases significantly. This is why tsunamis can cause devastating flooding and destruction when they reach the coastline.
A tsunami gains its height primarily through the energy released by underwater disturbances, such as earthquakes, volcanic eruptions, or landslides. When these events displace a large volume of water, they create waves that travel outward at high speeds. As the tsunami approaches shallow coastal waters, the wave slows down and compresses, causing its height to increase dramatically. This phenomenon, known as wave shoaling, can lead to towering waves when they reach the shore.
A tsunami can travel uphill depending on the slope, height, and force of the incoming wave. In some cases, tsunamis have been recorded to reach elevations of several hundred feet as they move inland.
When a wave is traveling in deep water, its bottom is at a set depth. As it comes ashore, the wave tries to stay the same wave height. since the land is denser than the water, the water is forced upward. That upward movement is the height of the tsunami.
A tsunami wave can reach heights of over 100 feet (30 meters) when it hits land.
Tsunami waves can reach heights of over 100 feet. The maximum height of a tsunami is influenced by factors such as the magnitude of the earthquake or underwater volcanic eruption that triggers it, the shape of the seafloor, and the distance the wave travels before reaching land.
Rarely. Most tsunamis, which are triggered by earthquakes, do not exceed 50 feet in height, but even a 10 foot tsunami wave can be very destructive.
In deep ocean water, the speed of a tsunami can exceed 500 mph but the wave height may be only a few feet. As the tsunami approaches shallow water and the sea floor rises, the speed decreases while the wave height increases significantly. This is why tsunamis can cause devastating flooding and destruction when they reach the coastline.
it gets higher
As a tsunami wave approaches the shore, its speed decreases due to the wave energy being compressed into a smaller space. This leads to an increase in wave height and impact force when the tsunami hits the coastline.
A tsunami gains its height primarily through the energy released by underwater disturbances, such as earthquakes, volcanic eruptions, or landslides. When these events displace a large volume of water, they create waves that travel outward at high speeds. As the tsunami approaches shallow coastal waters, the wave slows down and compresses, causing its height to increase dramatically. This phenomenon, known as wave shoaling, can lead to towering waves when they reach the shore.
A tsunami increases in height near the coast due to a phenomenon called wave shoaling. As the tsunami approaches shallower waters, the energy of the wave is compressed into a smaller water column, causing the wave to slow down and grow taller. Additionally, the ocean floor's topography can further amplify the wave's height, resulting in the towering waves often seen when tsunamis reach land.
A tsunami can travel uphill depending on the slope, height, and force of the incoming wave. In some cases, tsunamis have been recorded to reach elevations of several hundred feet as they move inland.
a tsunami is a tidal wave caused by an underwater earthquake :]
When a tsunami reaches shallow water, its wave height increases significantly due to the reduction in water depth. As the tsunami approaches the shore, the energy of the wave is compressed into a smaller water column, causing the wave to rise dramatically. Additionally, the wave's speed decreases, contributing to the growing height and potential destructive power as it impacts coastal areas.
As a tsunami travels across the ocean, it is in deeper water where its energy is spread out over a larger area, causing the wave height to be lower. As the tsunami approaches shallower waters near the shoreline, the wave slows down and the energy becomes concentrated, leading to an increase in wave height.