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レスコフ島

Leskov Island

成層火山 · United Kingdom · 190m

The 1-km-wide (maximum E-W direction) Leskov Island is shown in this 19 March 2021 PlanetScope satellite image (N is at the top). The island is the surface manifestation of a seamount chain that extends 60 km SW of Zavodovski in the South Sandwich Islands and is the smallest of the island group. The island coastline is entirely cliffs and it is constructed of eroded lava flows.
The 1-km-wide (maximum E-W direction) Leskov Island is shown in this 19 March 2021 PlanetScope satellite image (N is at the top). The island is the surface manifestation of a seamount chain that extends 60 km SW of Zavodovski in the South Sandwich Islands and is the smallest of the island group. The island coastline is entirely cliffs and it is constructed of eroded lava flows. · 写真: Satellite image courtesy of Planet Labs Inc., 2021 (https://www.planet.com/). · Wikimedia Commons
タイプ
成層火山
United Kingdom
地域
Antarctic-Scotia Volcanic Regions / South Sandwich Volcanic Arc
標高
190m
座標
-56.656, -28.140
最終噴火
不明
テクトニクス環境
Subduction zone / Oceanic crust (< 15 km)
火山地形
Composite
主要岩石
Andesite / Basaltic Andesite
地質学的概要

The small crescent-shaped Leskov Island lies about 50 km W of the main axis of the South Sandwich Islands, but appears to be comparable in age to volcanoes along the main arc. Only 900 m long and 400 m wide, it is bounded by steep cliffs and is the eroded remnant of a small andesitic stratovolcano. Its arcuate, NE-facing escarpment is concave toward Crater Bay, the site of the main eruptive center. A single Potassium-Argon determination gave an age of 0.5 million years, but fumarolic activity was recorded along the summit ridge in 1911 and 1964 (LeMasurier and Thomson, 1990).

Wikipedia の要約

レスコフ島 は、サウスサンドウィッチ諸島の島で、イギリス領サウスジョージア・サウスサンドウィッチ諸島のトラバーシー諸島に属している無人島である。ビソコイ島の56km西に位置する。

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