Little Sitkin Island (; ) is a volcanic island in the Rat Islands archipelago of the Western Aleutian Islands, Alaska, about east of Davidof Island. Great Sitkin Island (which is essentially the same size as Little Sitkin) lies further east in the Andreanof Islands. Little Sitkin is roughly circular and about in diameter. The interior is extremely rugged and mountainous; only the lower slopes are grass covered. There are two prominent peaks, one high in the northeast part of the island and the other high in the southern part. Numerous streams are on the island but no lakes or ponds. The coast is generally bold, rocky, and precipitous, with a fringe of kelp wide. Small steam jets and hot springs are in the valley at the head of William Cove on the northwest of the island. Volcano Little Sitkin is a stratovolcano that erupted circa 1776, 1828 and 1900. The 1776 eruption shows signs of being explosive. The volcano has had three cone building episodes separated by the formation of two calderas. A summit crater caps the youngest cone, about in diameter at the base. The active stratovolcano on Little Sitkin Island occurs within the eroded remnants of a nested double caldera of probable late Pleistocene age. The older caldera (Caldera One) is about in diameter and is centered slightly northeast of the island's midpoint. The caldera formed at the site of a large stratovolcano, the remnants of which are the oldest rocks exposed on the island. A second stratovolcano was constructed almost entirely of lava flows within Caldera One and attained a height of about . A cataclysmic eruption, possibly in early post-glacial time, resulted in the formation of a second, smaller caldera (Caldera Two) that partially destroyed this cone. Caldera Two is elliptical in outline and measures ; the inferred eastern and southern margins are coincident with those of Caldera One. Field relations suggest that the northern boundary of Caldera Two is a hinge along which a large block, comprising most of the Caldera One stratovolcano, was tilted southward during the caldera eruption. The highest peak on the island is on the post-caldera remnant of the second cone. A deposit of partly welded tuff up to thick extends from the remnant cone northwest across the Caldera Two boundary fault, to slightly beyond the inferred location of the Caldera One boundary fault. The deposit is thought to have been