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The whole island is extensively penetrated at sea level by natural cave formations that provide unique habitats for many marine creatures, notably sea anemones, some of which are only safely accessible at low tide.Sark is made up mainly of amphibolite and granite gneiss rocks, intruded by igneous magma sheets called quartz diorite.

It is a royal fief, which forms part of the Bailiwick of Guernsey, with its own set of laws based on Norman law and its own parliament. Sark (including the nearby island of Brecqhou) has an area of 2.10 square miles (5.44 km Protective railings were erected in 1900; before then, children would crawl across on their hands and knees to avoid being blown over the edge.Recent (1990–2000) geological studies and rock age dating by geologists from Oxford Brookes University shows that the gneisses probably formed around 620–600 million years ago during the Late Pre-Cambrian Age Cadomian Orogeny.The quartz diorite sheets were intruded during this Cadomian deformation and metamorphic event.A subsequent attempt by the families to endow a constitution under a bailiff, as in Jersey, was stopped by the Guernsey authorities who resented any attempt to wrest Sark from their bailiwick.In 1844, desperate for funds to continue the operation of the silver mine on the island, the incumbent Seigneur, Ernest le Pelley, obtained Crown permission to mortgage Sark's fief to local privateer John Allaire.

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