What Are Meromictic Lakes? – Explained with Green Lakes State Park Examples

   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.

Meromictic Lakes Explained

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. 

meromictic lakes



Causes and Types
Meromixis can arise from various factors. Biogenic meromixis occurs when organic decomposition in the depths produces gases or increases salinity.  Crenogenic meromixis results from subsurface saltwater inflows, while ectogenic meromixis is triggered by external events like landslides introducing dense materials.  The bottom layer often becomes anoxic (oxygen-deprived), supporting unique microbial communities and preserving ancient sediments.

 

meromictic lakes



Examples and Significance
Notable meromictic lakes include Green Lake and Round Lake in New York, known for their turquoise waters and glacial origins.  Others are Lake Tanganyika in Africa, the deepest meromictic lake, and Soap Lake in Washington, with high mineral content.  These lakes are scientifically valuable for studying climate history through undisturbed varves (annual sediment layers) and extremophile life forms.  They also pose ecological challenges, as the anoxic depths can release toxic gases if disturbed. 

meromictic lakes



Meromictic lakes represent only about 1% of the world’s lakes, making them rare natural laboratories for understanding aquatic ecosystems and Earth’s past. 

Meromictic Lakes at Green Lakes State Park

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.

Back to Green Lakes State Park

Related Resources

What Are Meromictic Lakes? – Green Lakes State Park Geology & Rare Lakes Near Syracuse NY