No, destructive waves typically have crests close together, with a short wavelength. These waves can carry a lot of energy and have the potential to cause significant damage to Coastlines and structures due to their intensity and frequency.
Yes. Constructive interference happens when waves add up to a more powerful wave than either were before, destructive interference happens when waves add up to a less powerful wave than either were before.
Short wavelength waves bend less than long wavelength waves when they pass through a medium because they have higher frequencies and shorter distances between wave crests. This phenomenon is known as refraction.
A long narrow depression between waves is known as a trough. It is the lowest point of a wave where the water level is at its lowest. Troughs are followed by wave crests, the highest points in a wave.
Longer wavelength waves have lower frequency because frequency is inversely proportional to wavelength in a wave. This means that the longer the wavelength, the fewer wave crests pass a given point per unit time, resulting in a lower frequency.
Long waves due to lightning has lowest frequecy. Apart from light produced an electrical disturbance in the form of electromagnetic waves are also accompanied with the lightning.
has a long wavelength hope that helped :) :)
Everything from long radio waves up to gamma radiation
Yes. Constructive interference happens when waves add up to a more powerful wave than either were before, destructive interference happens when waves add up to a less powerful wave than either were before.
Short wavelength waves bend less than long wavelength waves when they pass through a medium because they have higher frequencies and shorter distances between wave crests. This phenomenon is known as refraction.
A long narrow depression between waves is known as a trough. It is the lowest point of a wave where the water level is at its lowest. Troughs are followed by wave crests, the highest points in a wave.
Tsunamis are the most destructive waves in the ocean, typically caused by underwater earthquakes, volcanic eruptions, or landslides. Their long wavelengths and high speeds make them capable of causing widespread devastation when they reach coastlines.
Longer wavelength waves have lower frequency because frequency is inversely proportional to wavelength in a wave. This means that the longer the wavelength, the fewer wave crests pass a given point per unit time, resulting in a lower frequency.
Surface waves stem from body waves(P and S waves) that reach the surface. Because of their low frequency, long duration, and large amplitude, the Surface waves can be the most destructive type of seismic wave.
The energy from an earthquake travels in the form of seismic waves through the Earth's layers. When these waves reach the surface, they cause the ground to shake, creating the tremors that are felt during an earthquake.
Long waves due to lightning has lowest frequecy. Apart from light produced an electrical disturbance in the form of electromagnetic waves are also accompanied with the lightning.
Longshore drift is evidence of constructive waves. Constructive waves carry and deposit sediment along the coastline, resulting in the movement of sand and material parallel to the shore. This process helps build up beaches and create landforms such as spits and barrier islands.
L waves, also known as Love waves, are a type of surface wave that move in a horizontal, side-to-side motion. They travel along the Earth's outer layer and can cause significant shaking and damage during earthquakes due to their long wavelengths and high amplitudes. L waves move slower than P and S waves but are responsible for the most long-lasting and destructive effects of an earthquake.