Meromictic lakes are rare natural lakes in which the layers of water never fully mix, leaving deep bottom waters isolated from seasonal circulation. The best local examples are Green Lake and Round Lake in Green Lakes State Park near Syracuse, NY — two meromictic glacial lakes with turquoise water and stratified layers that provide valuable scientific insights into ancient sediments and aquatic ecosystems.
A Natural Wonder in Upstate New York. Meromictic lakes are a fascinating type of lake characterized by permanent stratification, where the water layers do not fully mix.
Unlike holomictic lakes, which experience complete mixing at least once a year due to seasonal temperature changes or wind, meromictic
lakes maintain distinct layers year-round. This term was coined in 1935 by Austrian limnologist Ingo Findenegg to describe lakes with
incomplete mixing.
How Stratification Works
In a typical lake, water circulates vertically, allowing oxygen and nutrients to distribute evenly. However, in meromictic lakes,
the upper layer (mixolimnion) may mix seasonally, while the deeper layer (monimolimnion) remains isolated and stagnant.
This separation is often due to differences in density caused by higher salinity, minerals, or organic matter in the bottom waters,
preventing overturn. These lakes are usually deep with a small surface area, sheltered from strong winds that could disrupt the layers.
At Green Lakes State Park near Syracuse, both Green Lake and Round Lake are meromictic. Their deeper waters remain permanently stratified, creating unique ecological conditions and striking blue-green water that attracts visitors year-round.
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