
A repeated signal caused by reflection between barriers.An echo is a sound or other signal that returns to the listener after being reflected off a surface or barrier. In physics, the term extends beyond acoustics to any wave phenomenon—electromagnetic, seismic, or even quantum—where a delayed copy of the original signal arrives due to reflection. The delay and intensity of the echo carry information about the distance and nature of the reflecting object, making it a fundamental tool for probing environments that are otherwise inaccessible.
The study of echoes dates back to antiquity, with early explanations by Greek philosophers. The first systematic scientific investigation was conducted by the German physicist August Toepler in the 19th century, who used the schlieren method to visualize sound waves and their reflections.
When a wave encounters a boundary between two media with different properties, part of its energy is reflected back. The reflected wave travels back to the source, arriving after a time equal to twice the distance to the barrier divided by the wave's speed. In acoustics, this is why you hear a distinct repetition of your voice in a canyon or a large hall; in radar and sonar, the same principle is used to locate objects by measuring the round-trip time of pulses.
Echo principles are used in sonar for underwater navigation and fishing, in medical ultrasound imaging, and in radar systems for aircraft and weather detection.
In bats, echolocation is so precise that they can detect objects as thin as a human hair, using echoes to navigate and hunt in complete darkness.



