Thermal stratification is generally observed in
(A)
Temperate lakes
(B)
Tropical lakes
(C)
Tropical ponds
(D)
Temperate ponds
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Thermal stratification occurs when two types of steam with different temperatures come into contact. Their temperature difference causes the colder and heavier water to settle at the bottom of the pipe while allowing the warmer and lighter water to float over the colder water.
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