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
157. Look through the telescope; you see it crossed by two fibres
of the finest spider's thread. In actual work we first direct the
telescope across the glacier, until the intersection of the two
fibres accurately covers some well-defined point of rock or tree at
the other side of the valley. This, our fixed standard, we sketch
with its surroundings in a note-book, so as to be able immediately
to recognise it on our return to this place. Imagine a straight line
drawn from the centre of the telescope to this point, and that this
line is permitted to drop straight down upon the glacier, every point
of it falling as a stone would fall; along such a line we have now to
fix a series of stakes.
158. A trained assistant is already upon the glacier. He erects
his staff and stands behind it; the telescope is lowered without
swerving to the right or to the left; in mathematical language it
remains _in the same vertical plane_. The crossed fibres of the
telescope probably strike the ice a little away from the staff of the
assistant; by a wave of the arm he moves right or left; he may move
too much, so we wave him back again. After a trial or two he knows
whether he is near the proper point, and if so makes his motions
small. He soon exactly strikes the point covered by the intersection
of the fibres. A signal is made which tells him that he is right; he
pierces the ice with an auger and drives in a stake. He then goes
forward, and in precisely the same manner takes up another point.
After one or two stakes have been driven in, the assistant is able to
take up the other points very rapidly. Any requisite number of stakes
may thus be fixed in a straight line across the glacier.
159. Next morning we measure the motion of all the stakes. The
theodolite is mounted in its former position and carefully levelled.
The telescope is directed first upon the standard point at the
opposite side of the valley, being moved by a tangent screw until the
intersection of the spider's threads accurately covers the point.
The telescope is then lowered to the first stake, beside which our
trained assistant is already standing. He is provided with a staff
with feet and inches marked on it. A glance shows us the stake has
moved down. By our signals the assistant recovers the point from
which we started yesterday, and then determines the distance from
this point to the stake. It is, say, 6 inches; through this distance,
therefore, the stake has moved.
160. We are careful to note the hour and minute at which each stake
is driven in, and the hour and the minute when its distance from its
first position is measured; this enables us to calculate the accurate
_daily motion_ of the point in question. The distances through which
all the other points have moved are determined in precisely the same
way.
Public-domain text, read in full here on John Shaqi.
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