Cross-bedding in Archean komatiitic ash deposits

When I was learning about the Archean from the perspective of Barberton Mountain Land in South Africa, I was expecting to see komatiite lava flows. Early on in Earth history, the planet was hotter: (1) it was closer to the many thermokinetic impacts that built the planet from stone-cold meteorites, and (2) there were many more unstable radionuclides around, decaying and releasing their energy into the young planet. As a result, some minerals that don’t melt readily at modern volcanoes were able then to turn to liquid and ooze out of volcanoes at temperatures much higher than modern eruptions. As they crystallized, these lava flows grew “chandeliers” of spinifex textured olivine and pyroxene crystals.

However, I was not expecting to see primary sedimentary structures in these ash deposits. Some of the ultramafic volcanoes blew up, sending ash into the Archean atmosphere, from where it rained down as itty-bitty particles. In addition to accretionary lapilli and tsunamites (with accretionary lapilli!), the komatiite ash deposits show current flow indicators such as cross-beds, indicating they were moved around by currents of either air or water prior to final deposition:

These cross-beds are concave-up (like smiley faces), and if you’re astute, you’ll be able to find a few instances here where the top of the cross-beds are truncated by an overlying bed. Here’s a GIGAmacro example of that, with cross-bedding annotated in blue, and the bottom of the overlying bed in gray:

[gigamacro id=1CQ1BjpfARZSAZmF width=100% height=550]

Note also the rusty patina of these ultramafic volcanic/sedimentary rocks – the olivine therein is ready to rust, even in the arid climate of South Africa.

0 thoughts on “Cross-bedding in Archean komatiitic ash deposits”

  1. Dear Callan:
    After posting your interesting blog about Cross-bedding in Archean komatiitic ash deposits, I received the following inquiries regarding their origin.
    Can this deposit be the product of eroded komatiitic volcanic rocks instead of an ash deposit? If it is an ash deposit, do the fine layers represent episodic volcanic events or is the ash reworked in a marine environment that then produced the fine layering?

    Reply
    • This is a great question. It’s my understanding that it’s the latter – that these are reworked by water.

      Reply
  2. These ashes may not have been deposited in the water… I think we have to see if the rock has hyalo character; if it does, it means that an aerial has been deposited… The Mg content is also important.

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