Today @ 03:54 PM post located here
dtyler:
A full discussion of these matters lies outside the scope of this note. However, sufficient has been said to show that Hutton's interpretation does not necessarily follow from the field evidences
No, insufficient has been said indeed. You have only dealt with the rocks
above the unconformity without discussing the rocks beneath it. Further, you have criticized Hutton's interpretations on a basis of age (no modern studies), whilst offering no alternative interpretation of your own for Siccar, but a bunch of generalized references of similar antiquity (and presumably thus in your view irrelevancy) to Hutton. More importantly, you have not even shown how an alternative interpretation might even be
possible, even though you cannot currently offer one.
I will give you a hand.
a) The rocks beneath the unconformity are bedded so each represents an event. How much time is recorded by the deposits and the bedding planes?
b) they are lithified/metamorphosed at low grade. This takes burial to a couple of kilometres. How quickly could they have been buried that far?
c) they are folded. This is plastic deformation which requires time at depth. How long were the rocks buried for?
d) they were uplifted. How quickly could they have been uplifted?
e) they were weathered down. How quickly could they have been weathered down?
As for the rocks above the unconformity;
a) They contain rounded pebbles from the underlying older rocks. How quickly can a pebble be rounded?
b) they contain microscopic particles of silt, sand and clay derived from the older rocks. How quickly could solid rock be broken down, not just to pebbles, but to
grains of sand?
c) they are bedded. Each bed represents an event. How much time does each event represent, and how much time do the bedding planes represent?
e) they are lithified. This requires deep burial and time. How deep were they buried, how long did it take to bury them, and how long were they buried for?
They are uplifted and being weathered again. How long did it take to uplift them?
Never mind a bit of calcrete!
What evidence is there for flash flooding? Or is it just assumed that because material is red and conglomeratic, it must be associated with flash flooding? (Sheet conglomerates are different from fan conglomerates, and it is the latter which should be associated with flash flooding. Other mechanisms of a more catastrophic nature may be better associated with sheet conglomerates)
A good question. Fan conglomerates develop in areas of high topographic gradient. They fan out towards areas of lower gradient, where they pass into sheets of conglomerate and interbedded sand, and then into sands and silts. In Glen's picture we seem to be looking at some very thinly bedded sands and ?possibly very thin, fine, gravelly conglomerates.
Do you think that is a fan? Remember, there are no modern descriptions of this outcrop, and Hutton, you say, tends to presuppose his descriptions- I wouldn't trust him if I were you. I can see a lot of planar bedding and cross-bedding in that picture. What does that tell you about the hydraulic regieme? Care to hazard a guess as to what the sedimentary system above the unconformity is, how it got there, and how long it took to get there?
Oh, and while we're on the problem of a lack of modern research at Siccar, one thing it does have going for it is that it is visited by hundreds of geologists every year. Like all of them, I've been there, and- like all of them- felt no need to tear my hair out at the way in which that charlatan Hutton misread the empirical data. Authoritative statements like:
Hutton's interpretation does not necessarily follow from the field evidences but it appears to have been imposed on them
Can only have come from someone who has also been to the outcrop. In that light, especially as you clearly have the inside track on thousands of geologists, might I ask why you've not published on the problem?
K
PS. So far my impression of your geological background is that a) you are using references often from near two centuries ago, interspersed with beginner's textbooks from 40 years ago, use quaint terms like 'greywacke' and 'old red', and do not understand more modern ones ('platform', for instance). It is therefore not suprising you believe that:
Students of geology are introduced early to the concept of uniformitarianism: present day slow rates of geologic activity are the basis for interpreting the rock record
As that is also a 19th-century view. I would be deeply interested to learn where- or when- you studied?