So here it is: the answer to
the riddle of the cake. This image shows the t-shirt cake labelled with a few key geologic units to help make my explanation a bit more coherent.

The main problem here is that central package of strata that are tilted at an angle: the sandstone, limestone, and marl (plus the little
brown layer in there that was too thin to label). If they're tilted at an angle, why aren't the layers underneath? The principles of superposition, lateral continuity, and original horizontality suggest that if these layers are tilted up at a crazy angle, then
so should the underlying layers (
i.e., basalt, siltstone, and shale #1). Instead, this drawing depicts what amounts to an
upside-down angular unconformity bounding the tilted layers below, in addition to the regular, perfectly-acceptable angular unconformity bounding the tilted layers above. This is what I referred to earlier as a geologic "impossibility."
But
Ron Schott, wily geologist that he is, pointed out another possibility: that this isn't necessarily an impossible situation, just an
improbable one. As I suspect is usual, Ron is right. One way that you could get the t-shirt cake situation is with that "lower upside-down unconformity" surface being a low-angle thrust fault, like the Lewis Thrust beneath Glacier National Park in Montana. That way, a package of rocks including tilted layers gets slid laterally (sideways) along such a fault, bringing them to rest on top of some other flat-lying sedimentary layers. The upper unconformity could form either before or after faulting in this scenario.
Another improbable situation: the marl, limestone, and sandstone are the oldest layers, and they were tilted at angle, eroded, and younger layers were deposited on top: shale #1, siltstone, basalt. Then everything got folded in a
really big overturned fold (like a nappe), putting them upside-down in this location. Then erosion attacked that, from the top down, and etched away the older rocks, leaving the younger sedimentary strata upside-down. Then deposition resumed with the shale #2, producing the upper angular unconformity. In this scenario,
both angular unconformities are real, but superposition is pretty much thrown out the window.
OK -- new contest: can you come up with any other geologically coherent possibilities to produce a central series of tilted strata bounded above and below by horizontal strata in the manner shown? Same prize.
Many thanks to students Will and Hannah, who asked me questions about this one all day today.
Labels: geology, humor