This document discusses stratification in lakes. It describes how lakes are vertically divided into three layers - the epilimnion on top which is mixed by wind, the metalimnion in the middle where temperature drops rapidly, and the hypolimnion on the bottom which remains cool and unaffected by wind. It also explains how the stability of this stratification depends on the energy required to uniformly mix the layers, and discusses differences between eutrophic and oligotrophic lakes in terms of biomass, diversity, and water quality.