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Will present day glacier retreat increase volcanic activity? Stress induced by recent glacier retreat and its effect on magmatism at the Vatnajokull ice cap, Iceland

机译:当今的冰川退缩会增加火山活动吗?冰岛瓦特纳冰原冰盖近期冰川退缩引起的应力及其对岩浆作用的影响

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摘要

Global warming causes retreat of ice caps and ice sheets. Can melting glaciers trigger increased volcanic activity? Since 1890 the largest ice cap of Iceland, Vatnajokull, with an area of similar to 8000 km(2), has been continuously retreating losing about 10% of its mass during last century. Present-day uplift around the ice cap is as high as 25 mm/yr. We evaluate interactions between ongoing glacio-isostasy and current changes to mantle melting and crustal stresses at volcanoes underneath Vatnajokull. The modeling indicates that a substantial volume of new magma, similar to 0.014 km(3)/yr, is produced under Vatnajokull in response to current ice thinning. Ice retreat also induces significant stress changes in the elastic crust that may contribute to high seismicity, unusual focal mechanisms, and unusual magma movements in NW-Vatnajokull.
机译:全球变暖导致冰盖和冰盖退缩。冰川融化会触发火山活动吗?自1890年以来,冰岛最大的冰盖瓦特纳冰原(Vatnajokull)面积约8000 km(2),在上个世纪以来一直不断退缩,损失了约10%的质量。如今,冰盖周围的隆升高达每年25毫米。我们评估正在进行的冰川等静与当前变化之间的相互作用,以改变瓦特纳冰原下方的火山的地幔融化和地壳应力。该模型表明,响应当前的冰层稀疏,在瓦特纳冰原下产生了大量的新岩浆,类似于0.014 km(3)/年。退冰还会在弹性地壳中引起明显的应力变化,这可能导致西北瓦特纳冰原的高地震活动,异常的震源机制和异常的岩浆运动。

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