458
December 2006
Horological Journal
to be oriented vertically
downwards.
Concentric with the main
plate is another, smaller,
disc, pivoted upon a
pierced rivet. The disc is
marked 1–12 twice along
its edge. On Cole’s
instrument, the numbers
run anti-clockwise, so the
time can be read directly
off it, but the diagram
above shows the figures
running the other way
round, meaning the time
has to be derived by
subtracting the indication
from 12. The hours, and
often the half-hours, are
marked with prominent
teeth, so that the operator
could feel the time at night.
A further vital feature is the index, marked in this case by a
smiling sun, and in the drawing by fleurs-de-lis. On more
complex instruments, more indices are provided, inscribed with
the names of the stars they are designed to measure.
Also pivoted at the centre is a movable straight index, the
alidade, the key edge of which lines up with the centre of the
instrument. The alidade must, of course, protrude well beyond
the edge of the main disc. In use, the observer chooses which
star he wishes to sight, and sets the appropriate index on the
inner disc to correspond with the current date (in the case of
Cole’s nocturnal there is only one, as has been stated before,
for Kochab ß). The instrument is held up by the handle, and,
while sighting the Pole Star through its centre, the alidade is
swung round to intersect with the chosen star. The time is then
read off the smaller disc.
Such an instrument can be used in any latitude, and remains
operationally accurate for many years, as the variation in direct
ascension varies very little over the centuries.
About the tide computer
The reverse of Cole’s nocturnal is a device used to determine
the time of high tide, based on the age of the moon.
The main plate has three zones. The outer is divided into 360º
in 1° intervals, the middle into twice 12 hours, and the inner into
32 compass directions. Within this is a volvelle, or rotating ring,
with a small pointer, and divided into 30 days. This is meant to
represent the age of the moon, but as the lunar cycle is
markedly different to this, the limited usefulness of the
instrument becomes apparent. When considered in conjunction
with a timekeeper that displays the time in ‘quantum leaps’ of
about half an hour, we can begin to appreciate the problems
facing navigators in the late middle ages. The centre of the
device has a lunar volvelle, with an aperture to visually
represent the moon’s age, and a large pointer, and is engraved
with symbols representing the four quarters of the age of the
moon.
The tides, with their constantly changing levels, greatly affect
navigation due to the energy generated by the immense
quantity of water in motion, and its effect on submarine
currents. Moon and Sun both exert gravitational attraction over
water on Earth, the Moon’s effect being more obvious because
of its proximity to the Earth. The change of the water level is
produced about every 6 hours, so that in one day the water
level will rise twice and fall twice. Although, astronomically, the
high and low tides are related to the position of the Moon, there
is in fact a difference between the time that the Moon passes
over a given place on the Earth and the rise or fall of the water
level at that place; this difference in time is called the
‘establishment of the port’ and is defined as the interval
between the passage of the Moon and the high tide over the
local meridian.
Spring tides, happening at the full moon and new moon,
produce the greatest range in height between high and low
water; this is because of the syzygy, where the Moon, Sun, and
Earth are aligned in space.
At neap tides, in the first quarter and last quarter of the Moon,
the Moon and Sun form a right angle with the Earth, the
attraction of the Moon is partly counteracted by that of the Sun,
and the difference between high and low tide is at its least. It is
therefore clear that a knowledge of the moon’s age is vital to
mariners, especially those active in Humphrey Cole’s era.
A critical point with the use of a tide predictor such as this is that
it can only determine the time of the passage of the moon over
a certain point. In order to discover the actual time of high tide,
a separate chart recording the ‘establishment of the port’ must
be consulted, in much the same way that the equation of time
must be known before a sundial can be put to good use.
The production of a replica scientific instrument
The primary technical consideration is, of course, to make the
instruments work as they were originally intended. Once it has
been decided which instrument is likely to be of commercial
interest, and to capture the
imagination, the engineering
process
can
begin.
Engineers, mathematicians
and astronomers have all
been employed to perform
the required calculations, in
order, for example, to ensure
that a given instrument will
work at a certain new
latitude. The skills of graphic
designers, illustrators and
modelmakers
are also
harnessed to ensure that the
final moulds we make
represent
the
piece
accurately.
Sometimes an item is
available to be examined, in
which case photos or
drawings can be obtained. In
the case of the Humphery
Cole instrument described
here, plans were based on
pictures from a book.
Missing or unclear parts
require further research and
comparison with similar
items, extrapolating the information where necessary, so that a
working instrument can be made.
In nearly every case it is impossible to effectively make the
reproduction instrument in the original material. These early
devices were made of brass, copper, and bronze, and would be
prohibitively expensive to cast today: zinc and aluminium alloys
are used instead, with gold plating to improve the appearance.
Such a reproduction takes considerable time, especially the
research and the correction of errors after the prototypes are
made. About six months mathematical and historical research
is required, including finding and making drawings. Once all the
technical aspects are resolved, master plans are drawn in 3D