I can’t comment on the thread itself, so I thought to open a side thread.
Thank you for publishing these three articles. As a (retired) Earth Scientist I find them excellent, not just because they engage decisively with many of the YEC misconceptions, but in their own right as a good illustration of what sound geological analysis can tell us about the past.
I’m a European and haven’t (yet) had the opportunity to visit the Grand Canyon myself, but very recently I was on a brief excursion to a classic geological site here in England to the famous (at least among geologists!) De La Beche unconformity in Somerset:
This is an abandoned quarry face where steeply bedded Carboniferous Limestone is truncated and overlain by the horizontal Jurassic Inferior Oolite. The interface between the two rock formations (with 3 persons standing on it) is a flat lying angular unconformity representing about 175 million years of time.
The grey Carboniferous Limestone was deposited when this part of the world was situated at tropical latitude, some 350 - 320 million years ago. It is thick bedded, and after deposition and lithification the entire formation was deformed and tilted, the beds are now dipping around 50 degrees. This happened during the Variscan orogeny, an extensive mountain building episode caused by the collision of the North American and ‘European’ continents. This collision formed the supercontinent of Pangaea and created a huge mountain chain extending for thousands of kilometers along the collision zone, much like the Himalayans of today.
Erosion immediately attacked the exposed land surface, and over time the mountains were worn down grain by grain. The erosion products were deposited as vast continental redbeds around remnants of the old mountain roots. Later still, the sea re-entered the now low lying landscape and deposited new rock formations, in this case the yellow Inferior Oolite limestone of Mid Jurassic age, 174 - 176 million years ago, that overlies the unconformity surface. These beds are virtually undeformed and still nearly horizontal, as they were when deposited. The reason we see them now on land is the relatively low global sea level of the present time.
These two rock formations contain entirely different fossil assemblages, because of evolution and also because of the intervening Late Permian Extinction, the biggest mass extinction event in the history of the planet that wiped out an estimated 81% of marine species. The unconformity surface itself contains worm borings and oysters that were living on the (then) sea floor.
I can’t even imagine the mental contortions one would have to go through to explain this outcrop as the result of processes operating in just one single year. That makes no sense whatsoever.