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Deception Island

Active volcanic island in the South Shetland archipelago

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  • 6 chapters

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Geography

Located within the Bransfield Strait, the island is roughly circular and horseshoe-shaped, with a maximum diameter around 15 km (9.3 mi). The highest peak, Mount Pond on the east side of the island, has an elevation of 539 m (1,768 ft), while Mount Kirkwood on the west has an elevation of 452 m (1,483 ft). Over half (57%) of the island is covered by glaciers up to 10 m thick, ice-cored moraines, or ice-covered pyroclasts. The sea has flooded the centre of the island to form a large bay, now called Port Foster, about 10 km (6.2 mi) long and 7 km (4.3 mi) wide. The bay has a narrow entrance, just 500 m (1,640 ft) wide, called Neptune's Bellows. The port is a basin with a flat floor up to 170 m (560 ft) deep with several small submarine cones and domes. The port is rimmed by a shallow coastal shelf with sandy-gravelly beaches. The outer coast of the island is characterised by 30–70 m (98–230 ft) cliffs of rock or ice.

Ravn Rock, a navigation hazard, lies 2.5 m (8.2 ft) below the water in the middle of the channel. Just inside Neptune's Bellows lies the cove Whalers Bay, which is bordered by a large black sand beach. Several maars line the inside rim of the caldera, with some containing crater lakes (including one named Crater Lake). Others form bays within the harbour, such as the 1 km (0.6 mi) wide Whalers Bay. Other features of the island include Mount Kirkwood, Fumarole Bay, Sewing-Machine Needles, Telefon Bay, and Telefon Ridge.

The linear Costa Recta spanning most of the east coast is hypothesised to be a scarp of a retreated submarine fault.

A 2016 study on Ardley Island, 120 km (75 mi) to the northeast, examined lake guano sediments and studied penguin population dynamics over 7,000 years. Three of five population growth phases were terminated by a sudden crash, due to volcanic eruptions from the active volcano of Deception Island. The history of volcanic eruptions is still under investigation, but several large eruptions have occurred in the last 10,000 years.

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