Very large corals in the tidal range. They get hard to imagine this as entirely rubble. They could be early Holocene. Again, no clear in situ corals. Took a few photos of the organisms sort of on the surface of the probably vermated constructional terrace but the flat low low tide mark.

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Photographs of Jacky standing above some upward cupping forms that maybe growth position corals hard to tell but certainly something interesting about the way the rock is weather.

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A bunch of photographs of the green algae, how they made a type and a finer one. Some circular organisms that I think are probably some kind of an enemy, they're just in the closed up state. And then out towards where the waves crashed, sort of orange, brown color is some kind of plant or algae. The utility had brought a piece from a topocu landing. We looked at before it and this seems to be the organism that lives in the edge of the foreground here in the Mississippi.

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A conspicuous upward branch in coral is that one of our suggests of a big insub.

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photograph of an encrusting coral exposed at low tide today which probably isn't even lowest tide of the year. It's sort of remarkable that these organisms can sustain themselves in these varieties.

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Photograph of water draining off of the? Anyways, I took some photos of the. Water running off as waves, similar to what we've seen in India. So, it makes me wonder that. If this was a stormier environment which you have essentially deeper channels here?

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A few more photographs of corals that I have decided to make their home here in this sometimes exposed and never buried the environment.

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There's a boulder perched on this flat. I wonder what kind of storm I brought back.

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It really seems like there's just too many upward branching corals in this unit for it not to be some kind of in-situ reef slash reef hardground system.

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A bunch of photographs of worm tubes, sort of at the bottom of the tidal launch. Likely some kind of vermitude.

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I can't quite make out exactly what I'm looking at, but when you step back from the tidal notch, there's this sort of light and dark banding. Makes these scalloped or circular shapes. The white up close is clearly some kind of cement or fine calcium carbonate. The dark, you can sort of see the grain texture of the underlying rock. Maybe these are some kind of feeding traces or something else that I should have with the organos that live here in the tidal zone. I don't see it any higher.

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Photographs show some large brain corals. Unsure if they're in growth position or in situ. Associated with the coral sort of around the outcrop here there are a lot of these. I don't know like tabular and a flat maybe four or five centimeters thick plates. It's not exactly clear what they are. The carbonate doesn't weather very nicely and I don't have the hammer but they are at least reminiscent of some of the encrusters. The things that we've been calling encrusters in other locations.

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Close-up photograph of one of these tabular blocks does show that there are corallites.

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Roger Creel stands on the title bench looking at potential MIS-5E outcrop here on the road.

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Hard to tell without a hammer and looking really closely with a hamlands, but it really doesn't seem like this outcrop has much sand suggesting that we're likely closer to the wave break. The corals are small enough that it doesn't feel like something we'd be seeing off the edge of the shelf, like the lower parts on Etchu, where we have really large corals, which is probably deeper water. This feels like a really shallow outcrop in encrusters and sparse corals that are probably in the position that they grew in. It's too high to be early-holicing. It really feels like it has to be a 5-e.

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been looking pretty hard for coral and algae or other sort of delicate coral organisms and I just don't see it maybe broken up bits of it but nothing that seems in situ.

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Upward branching corals seemingly in gross position are abundant throughout the outgrow.

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There's definitely some sand in the system. Just took a photograph of clear crossbedding up above the title zone. Roger points out that this is quite reminiscent of Cook's Landing and I agree with that. The paleo environment. Sand here and there, a few crossbeds, but probably at any point in time this was a pretty hard surface. You could walk on without sand moving around. The corals and the acrusters are just doing whatever they can with the tiny bit of accommodation space they have.

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