The Forms of Water in Clouds and Rivers, Ice and Glaciers — John Shaqi
The Forms of Water in Clouds and Rivers, Ice and GlaciersTyndall, John
Science
The Forms of Water in Clouds and Rivers, Ice and Glaciers
Tyndall, John
Clouds; Glaciers; Ice; Rivers; Water
161. Thus we shall proceed to work, first making clear to our minds
what is to be done, and then making sure that it shall be accurately
done. To give our work reality, I will here record the actual
measurements executed, and the actual thoughts suggested, on the
Mer de Glace in 1857. The only unreality that I would ask you to
allow, is that you and I are supposed to be making the observations
together. The labour of measuring was undertaken for the most part
by Mr. Hirst.
§ 22. _Motion of the Mer de Glace._
162. On July 14, then, we find ourselves at the end of the Glacier
des Bois, not far from the source of the Arveiron. We direct our
telescope across the glacier, and fix the intersection of its
spider's threads accurately upon the edge of a pinnacle of ice. We
leave the instrument untouched, looking through it from hour to
hour. The edge of ice moves slowly, but plainly, past the fibres,
and at the end of three hours we assure ourselves that the motion
has amounted to several inches. While standing near the vault of the
Arveiron, and talking about going into it, its roof gives way, and
falls with the sound of thunder. It is not, therefore, without reason
that I warned you against entering these vaults in summer.
163. We ascend to the Montanvert Inn, fix on it as a residence, and
then descend to the lateral moraine of the glacier a little below the
inn. Here we erect our theodolite, and mark its exact position by
a plummet. We must first make sure that our line is perpendicular,
or nearly so, to the axis or middle line of the glacier. Our
instructed assistant lays down a long staff in the direction of
the axis, assuring himself, by looking up and down, that it is the
true direction. With another staff in his hand, pointed towards
our theodolite, he shifts his position until the second staff is
perpendicular to the first. Here he gives us a signal. We direct our
telescope upon him, and then gradually raising its end in a vertical
plane we find, and note by sketching, a standard point at the other
side of the glacier. This point known, and our plummet mark known, we
can on any future day find our line. (To render the measurements more
intelligible, I append on the next page an outline diagram of the Mer
de Glace, and of its tributaries.)
164. Along the line just described ten stakes were set on July 17,
1857. Their displacements were measured on the following day. Two of
them had fallen, but here are the distances passed over by the eight
remaining ones in twenty-four hours.
DAILY MOTION OF THE MER DE GLACE.
First Line: A A' upon the Sketch.
East West
Stake 1 2 3 4 5 7 9 10
Inches 12 17 23 26 25 26 27 33
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