Chapter 30
Section 26. Description of A Glacier
I must now explain to you what a glacier is. You see before you thirty or forty mountain-peaks, and between these peaks what seem to you frozen rivers. The snow, from time to time melting and dripping down the sides of the mountain, and congealing in the elevated hollows between the peaks, forms a half-fluid mass, a river of ice, which is called (S. 4, N. 4) a glacier. As the whole mass lies upon a slanting surface, and is not entirely solid throughout, it is continually pushing, with a gradual but imperceptible motion, down into the valley below.—Mrs. Beecher Stowe.
Use the 2nd pers. sing.
Place the words ‘before you’ after the object.
glaubst du zu Eis erstarrte Flüsse zu erblicken.
which (App. § 16) from time to time melts, drips down on the mountain-sides (Bergabhänge), and congeals (gefrieren), etc., see S. 16, N. 4. Supply the adverb wieder before the verb ‘congeals’. The elevated hollow, die höher gelegene Felsspalte.
Eisstrom, m.
As = Since, da (App. § 16); to be entirely solid throughout, durch und durch fest sein.
it — pushing, so senkt sie sich fortwährend; with a ... but, mit einer zwar ... doch.
down — below, in das unten liegende Thal hinab.