Malham Cove is a limestone pavement formed after the last ice age by meltwater, largely from Malham Tarn. The meltwater carved out the cove as it fell over the edge as a waterfall and the resulting limestone pavement on the surface of the cove is characterised by limestone blocks (called clints and fissures called grykes). The grykes are rich in plant life including wood sorrel, wood garlic, and anemone.