Chambers's Edinburgh Journal, No. 309: New Series, Saturday, December 8, 1849Various
General
Chambers's Edinburgh Journal, No. 309: New Series, Saturday, December 8, 1849
Various
Periodicals
The first two or three stages being across certain intermediate
valleys, we have much up-hill and down-hill work along roads by no
means good. It was pitiable to see the little heavy-laden carts of
the peasantry toiling up the steep ascents, each with its forked pike
trailing behind it, on which to rest the vehicle, while the horse
should stop a few minutes at a time to recover breath and strength.
Many were conducted by women; and I could not but admire the hardy,
independent air of these females, as they sat, whip in hand, urging
their steeds along, though, as might be expected from such a rough
out-of-door life, their figures exhibit little of the attractions
of their sex. At many places I found rock-surfaces with dressings
generally in a north and south direction, being that of the valleys.
It is not unworthy of remark that two of the rivers are crossed by
modern wooden bridges, where a pontage is paid; and these were the only
charges approaching to the character of a toll to which I was subjected
throughout the whole of my travels in Scandinavia. Of the valleys,
one is full of sandy, a second of clay terraces, marking some decided
difference in the former submerged condition of the two districts. On
passing into a third at Trygstad, we find a vast plateau composed of
clay below and pure sand above, bearing magnificent pine-forests, and
which extends, without any intermission, to the foot of the Miösen
Lake. It would be a curious study to any native geologist to examine
this formation, and to trace its source, and the circumstances under
which it was deposited. There are remarkable generalities about
such things. Instructed by what I had seen in Scotland, as soon as
I observed the valley filled with sand up to a certain height a few
miles below where I knew a lake to be, I mentally predicted that this
formation would terminate at the foot of the lake, and that there would
be no terraces on the hill-sides above that sheet of water. Such proved
to be the case.
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