Griend is always named in one breath with Terschelling. However the island was formed in a very different manner.
In the early Middle Ages, extensive salt marshes lay south of Terschelling, Ameland and Schiermonnikoog. The first pioneers probably departed for Terschelling via these salt marshes. Griend, a village or small city in those days, is on the highest part of such a marsh. During the St. Lucia flood on 14 December 1287, the village Griend was washed away. The area is a kind of 'hallig': an island built from remnants of salt marshes (halligs are still found in the German Wadden Sea). Erosion from the waves creates cliff coasts, which slowly but surely disappear into the sea. The surface area of Griend at the end of the 14th century was only 165 hectare.
At one point, the current called the Vlie transported a large amount of sand, probably due to erosion of a coast somewhere else. Some of this sand was deposited on Griend, which lies exactly in line with the channel. Sand on the marsh dried and was blown by the wind. A low beach ridge several meters high was formed, in the shape of a sickle.
There has been no question any more of a salt marsh since hundreds of years. Griend is now the highest part of the so-called Grienderwaard, an extensive tidal bank with old clay and sand layers not far under the surface. The northwest side of the island in particular lies open to the strong Vlie current. This current regularly attacks the low beach ridge and dunes during storms.
The Vlie current runs westward of the Grienderwaard, the Meep is to the north and the Blauwe Slenk is to the south. Therefore, the island is surrounded by three deep channels on three sides. The east side is a transition to the tidal flats under the Frisian coast.
Under influence of water and wind, the overgrown sickle-shaped island of Griend slowly moves sometimes more, sometimes less in an easterly direction. It moved around 350 meters between 1850 and 1910. According to calculations, it must had moved a total of several kilometers since the 13th century. The total surface area at the end of the 19th century was around 25 hectare.
Up till 1932, there was a constant balance between erosion and growth; washed away sand on the west side settled again on the east side of the island. Fine particles settled on the east and new salt marshes formed between the arms of the beach ridge.
The Vlie current reaches Griend during high tide due to a shallow channel in the Grienderwaard, more like a depression in the bottom. This channel then splits and flows in a northerly and southerly direction: the so-called 'zwin' (tideway). This shallow channel is only visible during low tide and stretches in a sickle form in front of the sickle-shaped ridge.