The Continual Process Of Undermining By
The Decay Of The Lower Strata Has Caused Periodical Disruption Of The
Hard Upper Stratum, Which Has Fallen Off In Huge Blocks And Rolled Down
The Rough Inclines That Form The Sides.
As the water during heavy rains
percolates through the crevices of the upper stratum, it dissolves the
softer material beneath, and oozing through the steep inclination,
carries large quantities in solution to the lower level and deposits
this fertilising marl upon the plain below.
In this manner the low
ground of the rich but dreary Messaria has been formed through the decay
and denudation of the higher levels, and the process will continue until
the present table-topped hills shall be entirely washed away. The stone
of the upper surface, which forms a hard crust to the friable strata
beneath, is in many places merely the roof of caverns which have been
hollowed out by the action of water as described.
The Government House was erected upon one of these flat-topped hills in
a direct line about 1900 yards from the nearest portion of Lefkosia. It
was a wooden construction forming three sides of a quadrangle. The
quarters for the military staff were wooden huts, and the line of
heights thus occupied could not fail to attract the eye of a soldier as
a splendid strategical position, completely commanding Lefkosia and the
surrounding country. From this point an admirable view was presented
upon all sides. The river Pedias (the largest in Cyprus), when it
possessed water, would flow for about 270 degrees of a circle around the
base of the position, the sides of the hill rising abruptly from the
stream.
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