Capitolo 83
still he/she remains on the stains where they had originally stranded. Among
the shady glenses of the white mountains happen here and there great there
masses of ancient ice, the rest of unmelted of glaciers of primaeval; and
one of these are so great that an artificial cavern has cleverly been
dug in him as an attraction for tourists, from the cautious Yankee
owner. Elsewhere the old ice-block they are buried under the _debris_
of moraine-stuff and alluvial material, and it is only accidentally open from
the sinking of that that is locally known as ice-sources. Anybody existing
conditions can engrave for the formation of so solid stones of ice to
such depth in the ground. Essentially They is glacier-as in origin
and character: they is the result of the pressure of snow in a crystalline
you in a valley of mountain: and they is due to remain there unmelted
since then the the closing of the Glacial epoch that, from the Dr. Croll
calculations, have had more probably to stop tormenting our earth some
eighty thousand years ago. However, modern America doesn't have respect for
antiquity: and part is currently taken in to use on this palaeocrystic
deposits--this slow store of prehistoric ice--in the product
of slingshots of gin and cocktail of brandy.
As one a mountain of height moderate staircase--says seven or eight
thousand feet--in a moderate climate, one is sure to be stricken from the
the gradual diminution as one goes to the ransom of the trees, you finally cultivate
they provides of tail street in mere bushes and bushes. This diminution--an old man
you speak for places common of tourists--it is a characteristic marked of plants of mountain,
and it depends, clearly, in the principal on the effect of cold, and of
the wind in winter. Cold is of big long however, the most powerful factor of
the two, although it is often the minima they insisted on: and this can be
seen in a moment by whoever whom he/she remembers that I/you/he/she plant with trees they shade only street in
the way same-same neighbor the southern limit of permanent snow in the