Ketoy
Ketoy is an uninhabited volcanic island located in the centre of the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. Its name is derived from the Ainu language for "skeleton" or "bad".
Geography
The shape of the island is almost circular: approximately 10 km in length by approximately 9 km in width, with an area of The length of the coastline is 38.3 kilometers. Despite its relatively small area, the island has much landscape diversity, which is explained by its complex geomorphology, in which there are stratovolcanic cones, calderas, lava flows, volcanic plateaus, various valleys, high and steep coastal ledges, sea terraces, and rocky beaches. The steep cliffs ranging from 30 metres to 60 metres on the east and south sides with the west and north being taller. The beaches on the island consist of boulders and stones. The rivers and streams are numerous: mostly flowing to the south and east. The terrain is undulating and steep with numerous hills, rising to two main peaks:The highest point is Mount Ketoy - with a height of 1,172 meters to the east of the 1.5 km wide freshwater crater lake. The lake is 110 meters deep, and is the source of the Stochny Creek, which flows into the Pacific Ocean; the surface of the lake is at an altitude of 667 meters. The waters of thermal springs at the lake contain strontium, which makes them potentially interesting for the metallurgical industry.
The second peak is Pallas - with a height of 993 meters in the center of the island, which is still an active volcano. A major eruption occurred from 1846 to 1847, with the last known eruption in 1960. Eruptions of uncertainty occurred in 2013 and 2018. Pallas also has a crater lake, Lake Glazok, about 300 meters wide and 40 meters deep, with acidic water.