Sealed bottom lakes are formed in a number of ways, but the most common is through the deposition of fine-grained sediments in the bottom of a lake basin. These sediments, which are often derived from glaciers, rivers, or windblown dust, can form a layer that is impermeable to water. In some cases, a sealed bottom lake may also be formed by the movement of tectonic plates, which can cause the rocks at the bottom of the lake to become fractured and sealed.