hey i kno this ha ha ha ha ha the two waves are p waves and s waves
The electromagnetic spectrum organizes different types of electromagnetic waves according to their wavelength or frequency.
The sound of a bass drum primarily comes from two types of energy: kinetic energy and sound energy. Kinetic energy is generated when the drumstick strikes the drumhead, causing it to vibrate. This vibration transfers energy to the air, producing sound waves, which is the sound energy we hear.
The energy of infrared waves is greater than the energy of radio waves. This is because infrared waves has a smaller wavelength compared to radio waves. The smaller the wavelength, the higher the energy.
The areas under the Earth where earthquake waves bounce off are known as seismic wave reflection zones. These zones occur at boundaries between different geological layers, such as the crust and mantle or between different rock types. When seismic waves encounter these boundaries, some waves reflect back, while others may refract or transmit through the layers. This behavior helps seismologists understand the Earth's internal structure and the properties of various geological formations.
Radio waves are made by different types of transmitter. They are also given off by stars and lightning, this is why there is interference on your radio in a thunderstorm.
seismic
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.
Earthquake generated waves are called seismic waves. These are waves of energy that travel through the Earth's layers. Their velocity depends on the elasticity and density of the medium that they travel through.
The waves of energy that an earthquake produces are called seismic waves. There are two main types: body waves, which travel through the Earth's interior, and surface waves, which travel along the Earth's surface.
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
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.
Seismic waves are energy waves produced by an earthquake as it generates stress and releases energy along fault lines. These waves travel through the Earth and can be recorded by seismographs, helping scientists study the size, location, and characteristics of the earthquake. By analyzing seismic waves, geologists can understand the underlying causes of an earthquake and assess potential risks for future seismic activity.
Earthquake waves, like other types of waves, carry energy and propagate through a medium. They can be described in terms of wavelength, frequency, and amplitude. Additionally, earthquake waves can undergo reflection, refraction, and diffraction just like other waves.
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
P waves (primary waves) and S waves (secondary waves).
Potential energy is transformed into seismic waves during an earthquake :)
These are known as seismic waves - of which there are 4 types; P-waves, S-waves and Love and Rayleigh waves.