I dont understand what your point is. Remember the point was can sediment layers be eroded from the tops of mountains. The grand Canyon is not a mountain to start with. I was using that as an example of how thick sediment layers can be. The canyon is about 1800 meters deep and parts do go down to the igneous rocks below the sediments. But with mountains the erosion is stronger/quicker as it is elevated. The link states that a mountains worth of erosion can happen over millions of years. But when the mountain is growing (being pushed up through plate movements) it will continue to be high as it replaces the lost rocks through erosion. So mountains lose more than the sediment thickness through erosion over time if they can lose a mountains worth of rocks. In other words mountains lose way more sediments than the depth of the grand canyon. They will erode beyond the depth of the canyons sediments through to the igneous rocks and then some more to completely erode the mountain away. If it wasn't fro the fact that Mountains are growing then they would completely erode off the face of the earth. Mountains have eroded off the face of the earth in the past.
What I find, in favor of a massive flood, is that places like the grand Canyon even exist.
What I would expect is that lower layers would be much more compacted and resistant to erosion.
As layers, from whatever source, are laid down, I'd expect the lowest layers to be harder
and resistant to erosion. But what I see, when I have been to the canyon, is all the layers
of pretty much equal "toughness."
Here and there you will find a "tough" layer that holds out better than layers under it.
Niagara falls is an example of the lower layers being weaker than the top. But over time,
I'd expect the lowest layers to be the hardest rock, as least there should be many clear
examples of broad flat rivers hitting an impenetrable layer.
Instead, there are deep fissures with more vertical walls, which suggest all the layers
were laid down "at one time" and all having equal resistance to erosion.
I've never heard an explanation for the lower layers not being harder.