Thread: Picture I took this norning

Summer stratification: In warm months, lakes form three layers—

1. Epilimnion – Warm surface layer with lots of oxygen.
   
2. Thermocline – Middle layer where temperature drops rapidly (sometimes 1–3°F per foot).
   
3. Hypolimnion – Cold, deep water with little oxygen.

The “break”: The thermocline break is the point where this temperature change meets the lake bottom—often along a slope or drop-off.
Fish, especially in summer, stack along this zone because it offers:

• Comfortable, cooler temperatures.
  
• Enough oxygen.
  
• Access to food drifting down from above.

Fishing advantage: If you can locate that break—using electronics or a temperature probe—you can target suspended fish or those holding right where the thermocline touches structure. Drop shots, jigs, or live bait presentations right in that layer can be deadly, especially for walleye, bass, or big panfish.