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Some sandy layers on the left Bank of the river Tovey, which sir R.
Murchison (based probably on their mineral properties)
classified in his Silurian System under karadagskogo Sandstone
be now his own judgment, based on coming across them
fossils, belong to the Llandeilo formation. Meanwhile still
then, continue to do and make conclusions based on mineral
signs. Despite the fact that Siluria, like many other geological
works, proves with numerous examples, often in the space of
the few miles to meet the rocks of the same antiquity, sharply
differing from one another in their composition, while rocks, very
various degrees of antiquity, are often similar in their composition,
despite the fact that he sir R. Murchison as, for example, in the above
the case shows us how in the previous activities, it was introduced in
a misleading confidence in the lithological evidence - despite all of this,
in all "Siluria," reasoning it shows that he considers absolutely
natural to expect formations of the same ancient chemical identities
composition, no matter what distance they were from each other.
For example, referring to the Silurian rocks of South Scotland, he says:
"When I in 1850, drove road between Domini and Moffat, it occurred to
mind that monotonous reddish or purple Sandstone and shale,
occurring in the North from first town, and so strongly reminiscent of the lower
rocks Longmynd, Llanberis and S. David, needs to be the same
the antiquity of these last." Then he again insists on the fact that
these layers are "absolutely identical in composition with the lower mountain
rocks of the Silurian region." On the basis of this identity of mineral
signs and concluded that this Scottish formation of modern
the lower formations of the Wallis because the number available there
paleontological data is too low to use it
was to confirm or refute this kind of situation. If between
The Wallis and Scotland ran continuously such layers, located in
the same order, then, of course, it is unlikely that it would be possible to object to
similar output. But the fact that he sir R. Murchison admits that in
Westmorland and Cumberland some members of the system "accept
lithological appearance, quite different from that which they have in
Silurian and Valleskey areas", therefore, there is no reason
to expect mineralogical continuity in Scotland. So the obvious way
the assumption that these Scottish formations are of the same antiquity with
commandsim Shropshire in, involves a secret belief that the well-known
mineral characteristics typical of known ages.
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