The Principles of Stratigraphical GeologyMarr, J. E. (John Edward)
Science
The Principles of Stratigraphical Geology
Marr, J. E. (John Edward)
Geology, Stratigraphic
{ Lower Devonian
Lower Devonian { Hangman Grits { Slates
(Coblenzian) { Lynton Slates { Lincombe and Warberry
{ Foreland Grits { Grits and
{ Meadfoot Sands
[Footnote 83: An account of the South Devon rocks by Mr Ussher will be
found in the _Quart. Journ. Geol. Soc._, vol. XLVI. p. 487; from it
the above classification of the rocks of S. Devon is taken.]
The division into Lower Middle and Upper Devonian is generally
adopted, though the alternative titles given to these divisions are
not always used with the same signification, and the distribution of
the different local stages given in the above classifications is
usually adopted in the main, though a detailed comparison of the
Devonian beds of North and South Devon is still attended with
difficulty.
More than once an attempt has been made to prove that the apparent
succession of the North Devon rocks, which is that given in the above
table, is not the true one, and of recent years Dr Hicks has obtained
a number of fossils from the Morte Slates which had hitherto yielded
none, and he believes that these fossils indicate that the Morte
Slates are on a lower horizon than the beds on which they rest.
Whatever be the ultimate verdict, we can, at any rate, say that the
"Devonian Question," as it is termed, is not settled[84].
[Footnote 84: See Hicks, H., "On the Morte Slates and Associated Beds
in North Devon and West Somerset," _Quart. Journ. Geol. Soc._, vols.
LII. p. 254, LIII. p. 438.]
_Description of the Strata._ The general variations in the
lithological characters of the deposits of Devonian age will be seen
from the accompanying figure which represents the deposits of Britain
as they occurred from north to south before they had been affected by
subsequent earth-movements (Fig. 19). The conventional signs which are
used are similar to those which have been used in other parts of this
work, and will save description of the section.
[Illustration: Fig. 19.
A. Lower Palæozoic and Precambrian Rocks.
N.S. North of Scotland }
C.V. Central valley of ditto } Old Red Sandstone Type.
W. Wales }
N.D. North Devon } Devon Type.
S.D. South Devon }
]
The ridges separate different deposits of Devonian rocks, which were
possibly deposited in isolated areas, though there was probably
connexion between them at any rate at times.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account