The highlands of the West Bank are primarily underlain
by sedimentary limestone, dolomite and dolomitic
limestone. The stone quarried for building purposes,
ranging in color from white to pink, yellow and
tawny, is known collectively as Jerusalem stone.
Soft
Senonian limestone is found to the east of Jerusalem,
and has long been used as an inexpensive building
material.
Stone
of the Cenomanian layers, known in Arabic as
mizzi ahmar and mizzi yahudz, is far more durable
than Senonian limestone, but is very hard and
was expensive to quarry using pre-modern methods.
Turonian
layers yield mizze helu and meleke, the most
prized building stones. The thin layered mizze
helu is easily quarried and worked. Meleke is
soft and easy to chisel, yet hardens with exposure
to the atmosphere and becomes highly durable.
It was used for the great public buildings of
antiquity, and for the construction of the Islamic
period city walls and buildings.
The remains of ancient quarries can be seen
near Yemin Moshe, in the Sanhedria neighborhood,
and elsewhere.
Monday through Thursday 9 AM to 6 PM
Friday 9 AM to 2 PM
Sunday 9 AM to 4 PM
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