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During the past 150 million years LIPs have come in clusters with an average of one every ten million years. This clustering of LIPs is linked to the supercontinent cycle and has led to the proposal of superplumes or Large Low Shear Velocity Provinces (LLSVP). The HALIP, with its protracted lifespan, was part of several such clustering events at roughly 130, 120, and 90 Ma of which the last produced more than 18,000,000 km3 (4,300,000 cu mi) of igneous material alone. LIPs clustered with the HALIP are listed in the adjacent table. Bryan & Ferrari 2013, Large Igneous Province Clusters, pp. 1055-1057; fig. 2, p. 1056
Hi Fama Clamosa, thanks for your contributions! In the article you stated that a mantle plume was centered on the southern Alpha Ridge. Whereabouts is this mantle plume today? I'm assuming the HALIP is likely related to the Iceland hotspot. Volcanoguy16:32, 28 March 2016 (UTC)[reply]
'The Arctic Ocean is a few hundred million years old, making it the youngest ocean on Earth.'
I'm no geologist but a quick search reveals that the Atlantic Ocean is 'geologically the youngest' ocean. Other sources cite the Southern Ocean. The complexities of all this should be resolved here by someone more qualified than me. RobotBoy66 (talk) 09:56, 28 September 2023 (UTC)[reply]