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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.

All the Sark rocks (and those of the nearby Channel Islands of Guernsey and Alderney) formed during geological activity in the continental crust above an ancient subduction zone.

The location is also the highest point in the Bailiwick of Guernsey.

Little Sark had a number of mines accessing a source of galena. Off the south end of Little Sark are the Venus Pool and the Adonis Pool, both natural swimming pools whose waters are refreshed at high tide.

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.There is a narrow concrete road covering the entirety of the isthmus that was built in 1945 by German prisoners of war under the direction of the Royal Engineers.Due to its isolation, the inhabitants of Little Sark had their own distinct form of Sercquiais, the native Norman dialect of the island.A windmill, dated 1571, is found there, the sails of which were removed during World War I.This high point is named Le Moulin, after the windmill.

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