Here I've highlighted a couple of the beds that cut across other beds. The principle of superposition tells us that younger beds are on top of older beds, and the principle of cutting tells us the feature doing the cutting-- whether that's bed forms, as here, a fault or a dike-- is younger than the rocks it cuts. The highlighted horizons are cutting the other beds nearby, so those horizons are younger. Since they're younger, we can infer they're on top. Thus stratigraphic "up" is the opposite of the orientation in these two photos. Which is to say (at the risk of being confusing) that "up" is down.
Back to today's photo, just a quick comment: who says rocks aren't pretty? There are some interesting details, but take a moment to enjoy to appreciate the esthetic quality of the exposure.
Here's a crop from above ("below") the cobble:
I'm guessing that the round clast on the upper left was able to roll into place, then draped with subsequent sediment. The bump (keep in mind, stratgraphically, that's a divot) in the right middle looks like a burrow of some sort. And toward the upper right, the tent-like form *may* be a very small
Another structure, which puzzles me a little, is visible in both yesterday's and today's shots. (The crop is from yesterday's.)
I *think* that's a dewatering structure; as saturated sediment compacts, the interstitial water can escape along a channel and disrupt the sediments it's passing through. However, I think it's also possible that it might be a burrow instead.
Photo unmodified. July 21, 2016. FlashEarth location.
1 comment:
thanks! yes, beautiful
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