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Jeita Grotto

Jeita Grotto
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Jeita Grotto Facts

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Jeita Grotto Physical Description

The stunning Jeita Grotto holds many surprises for its visitors. This begins with the fact that it’s actually a system of two caves. While these remain separate, the caves interconnect. Together, the amazing system possesses an overall length totaling about 5.6 mi (9 km).

Because of its size, it ranks as the longest cave system in its part of the world. The upper cave measures roughly 6,990 ft (2,130 m) in length. The lower section, meanwhile, measures about 20,300 ft (6,200 m) long. Heights also vary, but reach as high as 39 ft (12 m).

It musn’t be overlooked, though, that this marvelous location houses many individual wonders, as well. These include columns, ponds, curtains, stalactites and stalagmites. In fact, it also holds the largest known stalactite in the world, at 27 ft (8.2 m) long.

It also contains three huge, separate natural chambers, as well as a subterranean river. The largest of the chambers measures an impressive 390 ft (120 m) long. The river it holds further serves as the source of drinking water for 1.5 million local residents.

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Jeita Grotto Location, Geology, and Importance

The dazzling site now called the Jeita Grotto formed in an area of the world already renowned for its many remarkable natural features. That’s because the dazzling dual cave system formed in what mankind now knows as the country of Lebanon, in western Asia.

Within that region, the cave system sits about 11 mi (18 km) from the city of Beirut. That location makes its remaining unnotieced so long even more amazing. Its location places it on the western side of the Lebanon Mountains. More precisely, it’s in the Nahr al-Kalb valley.

Adding to its splendor is its proximity to the coast. Incredibly, the system sits only 3.1 mi (5 km) from coast of the Mediterranean Sea. This location places it in the Nahr al-Kalb valley. Its naturally formed opening lies approximately 330 ft (100 m) above sea level.

Not only the area around the Jeita Grotto, but the entire region has a largely limestone geology. This therefore allowed for the formation of the impressive limestone karst caves. The process further occurred over a currently undetermined span of millennia.

It now has rather varied usefulness in the region. Most notably, it remains one of the most important tourist sites in the region. But sadly, its use as a water source may soon come to an end. Pollution levels in the water due to agricultural runoff has begun to increase.

Features Sharing Its Region

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