A Dynamic Water Body
![Illustriative graph showing the different temperature zones in the water column of Hyde’s Quarry. Starting at the top warmest zone, the Epilimnion averages 70 degrees fahrenheit, it has a depth of 15 feet. The zone below that is the Metalimnion, ranging 50-70 degrees fahrenheit, and has a depth of 15 to 45 feet. Within this zone is the Thermocline, which varies it's depth regularly. The deepest zone is the Hypolimnion zone, which ranges in depth from 45 to 60 feet, and has a temperature of 45 to 50 degrees.](../assets/images/main3-extra1.jpg)
Epilimnion
This top layer receives the most sunlight, warmth, and oxygen. Zebra mussels are common in this area, because their shell shape and byssal thread production let them attach firmly to hard surfaces and endure the motion of wind and waves.
Metalimnion
In this middle layer, cooler water mixes upward, and warmer water mixes downward. The thermocline—the point delineating the greatest temperature and density difference—resides here, moving up and down as the seasons and water temperatures change. In Hyde’s Quarry, the contractor injected potassium chloride directly into the lower layers after the thermocline initially blocked it from diffusing through the water column.
Hypolimnion
This bottom layer holds the coldest, darkest, most dense water. With low dissolved oxygen, it can become anoxic when the water body stratifies strongly in summer. Unlike zebra mussels, which prefer to attach to hard substrate, quaggas can settle in soft sediment here.