I was actually there. It was surprisingly soft...
View attachment 280600
Notice, on the right bank of the gully, the soft ash slumping into the (maybe 12-meter high) gulley. That's about the limit of vertical walls back when I took the shot. 120 film on a Voigtlander Perkeo, to give you some hint of when it was taken.
Never been there, um? You see, the "strata" are quite variable in hardness; the Cardenas Basalt is volcanic rock, about 6.0 on the Mohs scale which would be considered "hard." There is other, softer rock, but the river cut down through the basalt, just as it cut through other strata. And there is no way a sudden rush of water could cut entrenched meanders in basalt.
As Lyell pointed out, and I've shown you.
Which is quite normal. The decaying plant debris around the tree trunks form coal. You wouldn't see that in a huge flood. You have to have relatively still water to do that around the trees. That's no surprise, either.
Geologists have realized how coal forms for a long time. We have examples of all stages in the process still happening. Would you like to learn about that?
I'm not concerned about the current hardness....I'm more concerned about the hardness when th Grand Canyon formed after the flood and the amount of sapping.
The meanders were formed prior to the larger release of water and only provided a pathway for the rushing waters to follow. You still haven't presented any objections for a rapid formation of the Grand Canyon. SCIENCE cleary demonstrates it's possible and with the GC likely.
As to the polystratefossils in coal....the flood would have uprooted miles upon miles of forrest and vegetation and buried them in a similiar manner as the trees in Spirit Lake. There is much you can learn from this area if you would only believe the bible and what it has to say rather than mans misinterpretion of what really happened.
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