Sound is a form of energy that is created by vibrations and is transmitted through a medium, such as air, water, or solids. These vibrations cause particles in the medium to compress and expand, creating a series of high and low pressure areas known as compressions and rarefactions.
Properties of Sound
Frequency: The number of vibrations per second, measured in Hertz (Hz). Higher frequency sounds are perceived as higher pitch, while lower frequency sounds are perceived as lower pitch.
Amplitude: The maximum displacement of particles from their rest position. Greater amplitude corresponds to a louder sound.
Wavelength: The distance between successive compressions or rarefactions in a sound wave.
Speed: The speed of sound varies depending on the medium. In dry air at 20°C, the speed of sound is approximately 343 meters per second.
Be familiar with the anatomy of the human ear and the process of hearing.
By mastering these concepts, you will gain a solid understanding of the principles of sound and its significance in the natural world and human experience.
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.
Earth Science
History of Earth
Develop a model to illustrate how Earth’s internal and surface processes operate at different spatial and temporal scales to form continental and ocean-floor features.