Stage 1 formation of spits
Longshore drift deposits material across the river mouth, leaving a bank of sand and shingle sticking out into the sea
Stage 2 formation of spits
Occasional changes to the dominant wind and wave direction lead to a spit having a curved end (recurved end)
Stage 3 formation of spits
Recurved ends are abandoned as the waves return to their original direction
Stage 4 formation of spits
Area behind the spit is sheltered from the waves and often develops into mudflats and salt marshes.