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
The observed azimuths, unlike the observed latitudes, were more
accurate than the results of triangulation, repetition having shown
them to be reliable within 2″ or 3″, an error of which magnitude
would soon be surpassed in the process of continuing a chain of
azimuths with the unadjusted values of the angles of the triangles,
which were the only values possible to be used in the field. On
arriving at an azimuth station, therefore, a fresh chain of azimuths
was begun from the results of the observation, and continued to the
next station where astronomical observations were undertaken. The
accumulated azimuth error was, however, never found to exceed 10″
in any chain, a quantity which could not sensibly affect the computed
positions of points for plotting on the maps.
=Connexion with the Sudan Surveys.=—At the south end of the
area, connexion was made to a number of points triangulated by
the Sudan Surveys, but as the Sudan triangulation was commenced
as an independent piece of work from an observed latitude and a
telegraphically determined longitude, the connexion affords no
check on the accuracy of the triangulations. The difference found
between my positions and those of the Sudan Surveys was practically
constant for all the Sudan points connected, and amounted to 3″·5
in latitude and 26″ in longitude[70]; these figures represent the
errors in the assumed latitude and longitude of the starting point
of the Sudan Surveys, and will be employed as corrections to the
Sudan positions now that a complete chain of triangulation connects
Berber with the Mediterranean.
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