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
153. These determinations were made by means of a theodolite, of
which I will give you some notion immediately. The same instrument
was employed the same year by the late Professor Forbes upon the
Mer de Glace. He established independently the greater central
motion. He showed, moreover, that it is not necessary to wait a
year, or even a week to determine the motion of a glacier; with a
correctly-adjusted theodolite he was able to determine the motion
of various points of the Mer de Glace from day to day. He affirmed,
and with truth, that the motion of the glacier might be determined
from hour to hour. We shall prove this farther on (162). Professor
Forbes also triangulated the Mer de Glace, and laid down an excellent
map of it. His first observations and his survey are recorded in a
celebrated book published in 1843, and entitled "Travels in the Alps."
154. These observations were also followed up in subsequent years,
the results being recorded in a series of detached letters and essays
of great interest. These were subsequently collected in a volume
entitled "Occasional Papers on the Theory of Glaciers," published in
1859. The labours of Agassiz and Forbes are the two chief sources of
our knowledge of glacier phenomena.
§ 21. _The Theodolite and its Use. Our own Measurements._
155. My object thus far is attained. I have given you proofs of
glacier motion, and a historic account of its measurement. And
now we must try to add a little to the knowledge of glaciers by
our own labours on the ice. Resolution must not be wanting at
the commencement of our work, nor steadfast patience during its
prosecution. Look then at this theodolite; it consists mainly of a
telescope and a graduated circle, the telescope capable of motion
up and down, and the circle, carrying the telescope along with it,
capable of motion right and left. When desired to make the motion
exceedingly fine and minute, suitable screws, called tangent screws,
are employed. The instrument is supported by three legs, movable, but
firm when properly planted.
156. Two spirit-levels are fixed at right angles to each other on
the circle just referred to. Practice enables one to take hold of
the legs of the instrument, and so to fix them that the circle shall
be nearly horizontal. By means of four levelling screws we render it
_accurately_ horizontal. Exactly under the centre of the instrument
is a small hook from which a plummet is suspended; the point of the
bob just touches a rock on which we make a mark; or if the earth be
soft underneath, we drive a stake into it exactly under the plummet.
By re-suspending the plummet at any future time we can find to a
hairbreadth the position occupied by the instrument to-day.
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