In a stratified lake, the warmer and less dense layer is called the

Name: In a stratified lake, the warmer and less dense layer is called the
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The epilimnion is the warmer and less dense layer in a stratified lake, located near the surface. It is separated from the colder and denser hypolimnion by the thermocline, which is a zone of rapid temperature change. The hyperlimnion is not a recognized layer in a stratified lake.

In a Stratified Lake, the Warmer and Less Dense Layer