The ground over which we rode in a SW. direction, parallel to
the base of the escarpment, was very irregular in form, rising in
places into mounds sloping inwards towards the cliffs as well as
outwards towards the plain; and, although in great part covered
with vegetation, it appeared pretty certain that the whole was
composed of irregular masses of sandstone intermixed to some
extent with fragments of the rocks forming the barrier beside
us. To those who did not admit the probability of the boulders
before seen being deposited by glacial action, the phenomena here
presented offered strong confirmation. A glacier descending from
a main valley necessarily flows down the slope towards the plain,
and could not turn aside at right angles to its previous course,
and to the line of maximum inclination, unless there had been a
barrier of solid rock stopping the way, of which there was here not
the slightest indication. Whether or not materials that are borne
down a steep incline by sub-aërial denudation form a talus with a
diminishing slope resting against the face of the escarpment, or form
mounds at a greater or less distance from the base, is a question
depending upon the momentum with which they descend; and this again
depends on three elements—the weight of the blocks, the steepness,
and the length of the slope. If the greater portion of the materials
consist of large blocks launched down a steep and long incline, these
will travel to a considerable distance from the base of the cliff,
and gradually form a barrier that will stop the course of other
similar masses, until these accumulate into considerable mounds, as
may be seen in many instances of berg-falls in the Alps. Whatever be
the origin of these accumulations in this part of the Great Atlas,
it would appear that the conditions that gave rise to them have now
ceased, as we saw no instance of any large block that appeared to
have been recently borne to its present position.
As it was important to reach our night quarters by daylight, we
collected few plants during the afternoon ride; a fine _Asperula_,
with numerous flowers varying from white to pink, seemingly not
different from the Spanish _A. hirsuta_, was a great ornament here,
and in several other places on the skirts of the Atlas.
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