shinbits said:
I believe you about plates pushing up on lakes and mountains. But this would falsify geologic rock ages, because the layer that first existed on the bottom rises to the top, with younger layers at the bottom.
Make sense?
Absolutely not, it just proves that you can't even grasp this simple concept. The whole area is uplifted with the oldest rocks at the bottom and th eyoungest at the top, this is a simple, pancake ( analagous to a stack of pancakes ) geology case, the easiest to grasp. To push a bit further:
Think of it in terms of a telephone directory, bend it into an arch - mimicing plate collision, then slice off the top to a flat plane - mimicing erosion. The center of the plane now has the first pages of the telephone directory - analogous to the oldest rocks, the outside of this plane has the back pages of the directory - nalagous to the youngest rocks.
A similar pattern can be seen in southern England except in reverse the yougest rocks are at the center - around London, and the oldest rocks are reveal ed further away in sequence.
The difference is because in th efirst case we were creating an
anticline - bowing the rocks up, whereas in the real case around London we are looking at a
syncline .
Now I know these concepts are difficult without pictures, but google anticline and syncline and then see if you can find other pictures in the resources. Until you can grasp these very easy fundamental points you are arguing from a point of zero knowledge and your points are therefore quite worthless
http://www.arc.losrios.edu/~borougt/GeologicStructuresDiagrams.htm
This is the best I could come up with at short notice, and there must be better diagram resources out there but there are pictures showing the above cases.
There are even pictures showing cases where you can get older rocks above younger rocks ( recumbant folding ) so I am reluctant to postthe site for fear that you will grasp this special ( rare ) case like a drowning man grasps a straw, and try and make it a general case.
But we have to start somewhere.