They are both transverse waves, albeit having different wavelength and frequency. I think that velocity of the waves will also be different as x-rays travel at the speed of light.
S waves, or Secondary waves, are earthquake waves during an earthquake. They crash after P waves ( Primary waves) and are less stronger than surface waves
p waves
s waves
P or Primary waves are the fastest earthquake or seismic waves.
Siesmic
Earthquake waves, like other waves, transfer energy through a medium. They travel in a wave-like pattern, with characteristics such as amplitude, frequency, and wavelength. Additionally, earthquake waves can be reflected, refracted, and diffracted similar to other types of waves.
chelsea say head
Seismic waves are the vibration generated by an earthquake, explosion, or similar phenomenon and propagated within the Earth or along its surface.
Earthquake waves are called seismic waves.
Source earthquake waves are seismic waves produced directly from the earthquake's source, such as the initial rupture of rocks along a fault. These waves include P-waves and S-waves that travel through the Earth and are used to locate and study earthquakes. Source earthquake waves provide valuable information about the earthquake's characteristics and help in assessing its impact.
Electromagnetic waves have x-rays as a subset of their range.
An earthquake generates seismic waves that propagate through the Earth's interior in a similar way that waves move through water. These waves are characterized by their amplitude, frequency, and wavelength, similar to how ocean waves are described. The different types of seismic waves (P-waves, S-waves, and surface waves) behave distinctively due to their differing characteristics and how they interact with the Earth's materials.
it is a wave of Devansh Earthquakes move through the ground in waves, much like how thunder does through air.
Examples of electromagnetic energy are radio waves, Xrays, optical light waves, infrared waves, sunlight and lightening.
the bigger the waves the bigger the earthquake
Earthquake waves are vibrations that travel through the Earth's crust when an earthquake occurs. There are three main types of earthquake waves: primary (P) waves, secondary (S) waves, and surface waves. These waves can cause the ground to shake and can be detected by seismographs.
Earth is the medium for earthquake waves.