The geography and geology of south-eastern EgyptBall, John
Science
The geography and geology of south-eastern Egypt
Ball, John
Geology -- Egypt; Physical geography -- Egypt
It was generally necessary to remain for at least a week on the
mountain summits which formed the main triangulation stations,
for only on about one day in seven was the air clear enough for
sighting the beacons on the longer lines. Occasionally the entire
landscape was blotted out for ten or more consecutive days by clouds
surrounding the summit, while at other times it was possible to see
only for a limited distance round the station owing to haze. Such
times were made use of to map all visible detail within a moderate
range (say within a radius of twelve kilometres) round the station.
In this work the first stage was to find a small base, one end
of which was the station itself. Usually a minor peak of the same
range, 500 to 1,000 metres away from the station, was fairly easily
accessible, and was chosen for the other end of the base. The six-inch
theodolite being at the main station, the five-inch tacheometer was
set up at the auxiliary station, and all noteworthy hill tops, as well
as a few points along each main line of drainage, were triangulated
off this small base. The length of the base was found by including
one or two main triangulation points in the round of angles. These
minor triangles were conveniently reduced by the slide rule, and the
points plotted at once on the plane-table by means of the alidade
and the calculated distances. The base being short, it was necessary
to observe to fine marks; cracks in the rocks, and the droppings
of birds on the peaks, and the centres of selected tree trunks in
the wadis, were usually chosen. The levels of these minor points
were determined by vertical angulation in the ordinary way. Usually
about thirty points were thus fixed round each high station. Once a
number of points were fixed in the wadis, the levels of these gave
the slope, and the difference of height between any other parts of
the wadis and the station could be estimated to within a few metres by
means of the knowledge thus obtained. A sketch being now made of the
wadis, which appeared spread out almost like a map below the station,
a hundred or more points along them were selected, and their depths
below the station being very approximately known from the wadi slope,
their distances were found by observing depression angles to them
and reducing the vertical triangle by means of the slide rule on
the spot. In all, therefore, measurements were usually made of the
distances of from 100 to 200 conspicuous points in the area round
the station, and when these were plotted with the alidade on the
plane-table sheet it was not difficult to sketch in all the detail
with considerable accuracy. Usually it was not possible to see all
round the mountain from the station itself, so that subsidiary
plane-table stations near the main one were necessary. In other
cases more than one small base was measured in order to get good
angles to various points by the minor triangulation.
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