Step 1: Recall what a leaky aquifer means.
A leaky, or semi-confined, aquifer is not fully sealed off the way a strictly confined aquifer is.
Step 2: Identify the bounding layers.
It sits between aquitards, layers that are not fully impermeable but still let a limited, slow amount of water leak through vertically, which is why some water can seep in or out.
Step 3: Rule out the stricter descriptions.
Fully impermeable layers, plain clay, or generic rock layers would either stop all leakage or are too vague to describe the semi-permeable behaviour that defines a leaky aquifer.
\[ \boxed{\text{Semi-permeable layers}} \]