25 January 2011
Following up from my post on rheomorphic flow in volcanic tuffs, it’s geology bake sale time! For my submission to this month’s Accretionary Wedge, hosted at Mountain Beltway, I’m trying to draw a few parallels between a confection more commonly known as “zebra cake” and deformation in pyroclastic deposits. To do a quick recap, rheomorphic flow occurs when parts of a pyroclastic deposit – either during or after deposition – become viscous enough to flow like a syrup. If there is flow banding in the deposit, it can become deformed and folded back on itself to form some visually striking patterns (such as in this piece of rhyolite from Mono-Inyo craters in California). So let’s bake a flow-banded pyroclastic deposit!
Zebra cake is similar in that it consists of alternating layers of vanilla and chocolate cake batter, poured in such a way that they form a “sideways” pattern in the cake pan rather than being layered vertically. In this cake, the alternating layers of vanilla and chocolate batter will represent flow banding that is compositionally different – the cocoa powder is ash that’s richer in some dark component (mafic minerals like pyroxene, hornblende or biotite), perhaps. In this particular version of the recipe in that link, I’ve substituted almond flour for some of the regular flour (think of it as throwing pumice pyroclasts in with the volcanic ash).
As I pour the cake, deformation is being introduced as different layers are being added to the deposit (since one flavor pushes the other out of the way, and so on. This could be an analogy for different pulses of a pyroclastic flow being deposited, or even different eruption pulses, which could vary the composition of a deposit. This is syn-depositional deformation.
However, if I tilt the cake pan a little bit and allow for some more flow, this could be considered post-depositional deformation.
The baking process is going to be an analog for welding, in which the heat retained in the pyroclastic material fuses it together into a dense rock. Since this is a high-grade (very hot) pyroclastic deposit, we’re not going to see any other features like gas-escape pipes – just the results of rheomorphic flow.
Beautiful! A nicely welded “deposit” with clear compositional variations – at least in map view. Let’s add a sugary co-ignimbrite ash fall deposit:
Then take a look at a cross-section:
Well, that didn’t turn out quite as beautiful as this. But if you think about it, this is a good analog for how things actually happen in natural systems – not neatly. This, then, is a pyroclastic deposit that has been very welded (and mixed a bit, post-deposition), to the point where it’s almost obliterated the flow banding that ideally would have shown up in cross-section. I’ve tried to annotate the remaining deposit to show the banding:
Of course, this is open to interpretation, but it looks like (in some places) the layers have overridden each other rather than pushing each other out of the way. (I suspect it had something to do with the almond flour; next time I’ll try it with just the regular kind.) Still, it’s the most delicious pyroclastic deposit I’ve ever tasted. (In geology, odds are you’ll get around to tasting a lot of rocks, even pyroclastic ones.)
And, as in any volcanic eruption, there’s usually a little cleanup afterward: