20/04/2026
The Limestone Pavements of Lough Corrib
A limestone pavement is formed when glaciers scrape away the soil and loose material on top of limestone and leave a smooth limestone slab. Limestone tends to fault in straight lines. Slightly acidic rainfall then finds all the faults and cracks and is drawn in by capillary action. As the cracks widen they channel more water and these faults and cracks deepen and dissolve away.
What you see in the sonar picture is the result of thousands of years of rainfall on a sheet of rock which is now 5m underwater, and this process occurred at some time since the end of the last Ice-Age, around 12000 years ago
These photos are of Clydagh Point limestone pavement and the Long Shallow submerged limestone pavement.
The Long Shallow pavement itself is evidence of the changing nature of Corrib - the now submerged pavement was above the shoreline of the lake for long enough for the rain to dissolve away the limestone in the cracks. The lake then rose dramatically and submerged the pavement under 5m of water.
Other indicators that we have point to the possibility that this happened sometime between 4000 and 6000 years ago.
The submerged pavements provide a hunting ground for predators, and a hiding place for others, as well as being beautiful and fascinating dive sites.