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(2010) argued that kimberlite eruptions, and thus diamond deposits, occur preferentially within 15° of the edge of the African LLSVP, defined as the –1% ΔVS contour in the deep mantle. They claim that ~80% (1112 out of 1395) kimberlites and related volcanics erupted since ca. 320 Ma lie within this zone, and therefore propose that, in addition to causing hotspots and LIPs, deep-mantle plumes cause this distinctive style of volcanic activity, comprising clusters of pipes, dikes, and sills.
I’m forever whitewashing after them, whitewashing off the scandalosities they do be scrabbling on the privy walls.
[…] semen is a gift, and the relation between the one who is fellated and the one who fellates is a relation between one who gives and one who receives.
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