A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological MonumentsLyell, Charles, Sir
Science
A Manual of Elementary Geology: or, The Ancient Changes of the Earth and its Inhabitants as Illustrated by Geological Monuments
Lyell, Charles, Sir
Geology
I described in 1839 the fossil shells collected by Captain Bayfield from
strata of drift at Beauport near Quebec, in lat. 47 deg., and drew from them
the inference that they indicated a more northern climate, the shells
agreeing in great part with those of Uddevalla in Sweden.[134-A] The shelly
beds attain at Beauport and the neighbourhood a height of 200, 300, and
sometimes 400 feet above the sea, and dispersed through some of them are
large boulders of granite, which could not have been propelled by a violent
current, because the accompanying fragile shells are almost all entire.
They seem, therefore, said Captain Bayfield, writing in 1838, to have been
dropped down from melting ice, like similar stones which are now annually
deposited in the St. Lawrence.[134-B] I visited this locality in 1842, and
made the annexed section, fig. 118., which will give an idea of the general
position of the drift in Canada and the United States. I imagine that the
whole of the valley B was once filled up with the beds _b_, _c_, _d_, _e_,
_f_, which were deposited during a period of subsidence, and that
subsequently the higher country (_h_) was submerged and overspread with
drift. The partial re-excavation of B took place when this region was again
uplifted above the sea to its present height. Among the twenty-three
species of fossil shells collected by me from these beds at Beauport, all
were of recent northern species, except one, which is unknown as living,
and may be extinct (see fig. 119.). I also examined the same formation
farther up the valley of the St. Lawrence, in the suburbs of Montreal,
where some of the beds of loam are filled with great numbers of the
_Mytilus edulis_, or our common European mussel, retaining both its valves
and purple colour. This shelly deposit, containing _Saxicava rugosa_ and
other characteristic marine shells, also occurs at an elevated point on
the mountain of Montreal, 450 feet above the level of the sea.[135-A]
[Illustration: Fig. 119. _Astarte Laurentiana._
_a._ Outside.
_b._ Inside of right valve.
_c._ Inside of left valve.]
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