Slwal Zone

In oceanography and freshwater biology, the shallow zone (often referred to as the or Neritic Zone ) extends from the shoreline to the depth where sunlight can no longer reach the bottom effectively for plant growth.

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Water masses in the shallow zone are distinct from the deep ocean due to their interaction with the atmosphere and seafloor. In oceanography and freshwater biology, the shallow zone

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The shallow zone is characterized by a sharp velocity contrast. Seismic waves traveling through bedrock (high velocity) encounter soil and soft sediment (low velocity) in the shallow zone. According to the conservation of energy, as wave velocity decreases, amplitude must increase to conserve energy flux. This phenomenon, known as , means that ground motion is often significantly more intense at the surface than at depth.

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