Arab Weather - Deep in the Zagros Mountains, south of the Iranian city of Qom, lies the Fordow nuclear facility. It's a site not only characterized by structural protection, but also by what can be described as "natural geological fortification," making it one of the most impervious to military threats. How did geography and geology contribute to containing and protecting the nuclear facility?
In detail, the Fordow facility is located within a rocky mountain within the Zagros Mountains, an area that represents the intersection of the Arabian and Iranian tectonic plates. This area is tectonically active, resulting in dense sedimentary layers such as limestone and dolomite.
These rocks are characterized by their hardness and high resistance to pressure. Their presence within a mountainous structure folded by ancient faults creates irregular layers that impede the transmission of shock waves and weaken their impact.
Limestone and dolomite are among the most prominent rocks with high energy absorption properties resulting from explosions and vibrations. This type of rock is sometimes used in military fortifications, but at Fordo, nature provided it in a ready-made and durable form.
Structural deformations resulting from tectonic movements over thousands of years have created networks of folds and faults that further complicate the mountain's structure and make targeting a specific point within the mountain's interior extremely difficult.
The nuclear facility is located between 80 and 110 meters below the earth's surface. While this depth is not very significant in military terms, it is sufficient to provide significant protection against most, even the most powerful, weapons. Studies indicate that pressure increases at a rate of approximately 1 megapascal per 100 meters, while temperatures rise by approximately 3 degrees Celsius per 100 meters. This provides a stable operating environment that reduces the risk of structural expansion and contraction of facilities and equipment.
What's striking about the Fordow facility is that the fortification process relied not only on concrete, but also on the use of the solid, winding mountainous structure as part of its natural defenses. The waves generated by any potential detonation would collide with heterogeneous layers, weakening their power and dissipating their energy before they could reach the core of the facility.
Satellite images and analytical reports show that the site was carefully chosen not only because it is hidden from view, but also because it is surrounded by layers of earth that give the facility near-complete "geographical immunity" against direct penetration.
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