in fact, include species closely allied to them
("cud-weeds" of the genus _Gnaphalium_).
The huge cliffs of rocks on either side (in some parts over a thousand
feet in sheer height from the torrent) come closer to one another in
the part where we now are than in most Alpine valleys, so as almost to
give it the character of a "gorge." At some points the highest part of
the precipice actually overhangs the perpendicular face by many feet.
A refreshing cold air comes up from the icy torrent, whilst the heat
of the sun diffuses the delicious resinous scent of the pine trees.
Above the naked rock we see steep hill-sides covered with forest, and
away above these again bare grass-slopes topped by cloud. But as the
clouds slowly lift and break we become suddenly aware of something
impending far above and beyond all this, something more dazzling in
its white brightness than the sun-lit clouds, a form sharply cut in
outline and firm, yet rounded by a shadow of an exquisite purple tint
which no cloud can assume. The steely blue Alpine sky fits around this
marvel of pure whiteness as it towers through the opening cloud, and
soars out of earth's range. What is this glory so remote yet impending
over us? It is the Jungfrau, the incomparable virgin of the ice-world,
who bares her snowy breast. She slowly parts her filmy veil, and, as
we gaze, uncovers all her loveliness.
The rock walls of the Lauterbruennen valley show at one place a
thickness of many hundred feet of strongly marked, perfectly
horizontal "strata"--the layers deposited immense ages ago at the
bottom of a deep sea. Not only have they been raised to this position,
and then cut into, so as to make the profound furrow or valley in the
sides of which we see them, but they have been bent and contorted in
places to an extent which is, at first sight, incredible. Close to one
great precipice of orderly horizontal layers you see the whole series
suddenly turned up at right angles, and the same strata which were
horizontal have become perpendicular. But that is not the limit, for
the upturned strata are seen actually to turn right over, and again
become horizontal in a reversed order, the strata which were the
lowest becoming highest, and the highest lowest. The rock is rolled up
just as a flat disc of Genoese pastry--consisting of alternate layers
of jam and sponge-cake--is folded on itself to form a double
thickness. The forces at work capable of treating the solid rocks, t
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