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What Are These Holes?


fossils4fun

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Hi fossil friends, I walk by this big rock every time I go fossil hunting and I am always wondering, what are these holes?

The rock is about 2 feet tall and 2 or 3 feet wide. The holes are about 4 or 5 inches across.

If anyone knows I would really appreciate it, it's driving me crazy, thanks so much and have a great new year. :)

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It would help if you could post some larger, more detailed photos and also tell us something about the locality and the geological formation and age where it is lying. Was it transported there or did it derive from the local layers?

Edited by Ludwigia

 

Greetings from the Lake of Constance. Roger

http://www.steinkern.de/

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Let me try again with the pictures, I'm new at this so it may take a little while, thanks. :)

It was not transported here, a natural formation to the area, the place is Northwest Arkansas and I have a lot of sandstone with impressions in them, I hope that helps a little.

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They could be gas bubbles that were entrained in the sediment.

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"There has been an alarming increase in the number of things I know nothing about." - Ashleigh Ellwood Brilliant

“Try to learn something about everything and everything about something.” - Thomas Henry Huxley

>Paleontology is an evolving science.

>May your wonders never cease!

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It may just be from dripping water? That would be my guess. That or there may once have been some type of bivalve that has long since dissolved into nothing.

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Dang that is neat looking. Is it a sandstone???

I'm guessing without hearing more that it looks like the weathering phenomena of a limestone/carbonate rock. Rain water dissolving the rock and maybe that process is enhanced mechanically by some freeze/thaw during the winter over the years..

Regards, Chris

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I'm just guessing, since it's still difficult to recognize any details, but it may be that the "holes" were created by concretions within the sediment which have since fallen out due to weathering.

 

Greetings from the Lake of Constance. Roger

http://www.steinkern.de/

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Most likely, it is differential weathering. If there is any variation of resistance in the strength of the rock, the weaker spots will erode out first. This can be cause by a variety of reasons.

Context is critical.

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Most likely, it is differential weathering. If there is any variation of resistance in the strength of the rock, the weaker spots will erode out first. This can be cause by a variety of reasons.

Missourian, I agree. Not sure what might be holding the sand grains together--could be limey or maybe not.

Saw this neat picture of a section of similar strange stuff somewhere in the state while I was out looking...

https://arkansasgeological.files.wordpress.com/2013/11/2013-11-19-033.jpg

I should find and have a piece of this outcrop--how I'd get it back here and where I'd put it is an entirely different matter..... :)

Regards, Chris

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Very nice picture, I've never seen anything quite like it before. I do have a bluff with perfectly half round basketball size holes in it. I never knew what they were but I thought it might be a place where water once slapped the side. Just a thought, I may be all wrong.

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...Not sure what might be holding the sand grains together...

I think iron is implicated; there are similar constructs to be seen in such disparate places as Calvert Cliffs and transgressive Pennsylvanian coal-zone deposits.

"There has been an alarming increase in the number of things I know nothing about." - Ashleigh Ellwood Brilliant

“Try to learn something about everything and everything about something.” - Thomas Henry Huxley

>Paleontology is an evolving science.

>May your wonders never cease!

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Could be stromatolites, which were softer and weathered out. Particularly with the one specimen with the wavy texture. Looks very algal matish to me.

Brent Ashcraft

ashcraft, brent allen

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