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Majlis Al Jinn Cave, Oman

August 28, 2012 by staff 

Majlis Al Jinn Cave, Oman, Majlis al Jinn also Majlis al-Jinn (meeting/gathering place of the Jinn), local name: Khoshilat Maqandeli is the ninth largest cave chamber in the world, as measured by the surface area of the floor. It ranks higher when measured by volume. The cave is located in a remote area of the Selma Plateau at 1,380 metres above sea level in the Sultanate of Oman, 100 km south-east from Muscat.

The Selma Plateau is a shallow syncline on the north-eastern limb of the Jabal Bani Jabir anticline. The cave was formed in fossiliferous carbonate rocks of the Middle Eocene Hadhramaut Group, Dammam Formation. It is one of several caves on the Selma Plateau.

Majlis al Jinn is a single chamber measuring about 310 metres by 225 metres, with a domed ceiling 120 metres high and three entrances in the roof. The totally free-standing roof is only about 40 metres thick over most of the cave. The deepest part of the cave is 178 metres below the top of the highest entrance. The volume of the chamber is approximately 4,000,000 cubic metres, and the floor area is 58,000 square metres.

When it was surveyed in 1985, Majlis al Jinn was the second largest known cave chamber in the world by volume. However, more than 15 chambers larger than Majlis al Jinn have been surveyed since that time.

There are no visible lower exits or passages leading from the chamber-these passages most likely have been blocked by debris on cave floor. Water entering the cave collects along the lowest part of the floor, then slowly infiltrates into the fine-grained, mud-cracked sediment or evaporates. The entrances receive surface runoff from only a small drainage area, so water never reaches most parts of the cave. While surface temperatures can exceed 40 °C, air temperatures in the chamber are a constant 17-18 °C.

Access to the cavern is only through a free descent of one of three vertical entrances in the ceiling, formed by water seeping through the weakened marly limestone in the zones of fracturing. The two largest entrances are called Asterisk (Khoshilat Beya Al Hiyool) and First Drop (Khoshilat Maqandeli), the smallest is Cheryl’s Drop (Khoshilat Minqod) . Entrance depths:Cheryl’s Drop – 158.2 meters. Asterisk – 139.6 meters. First Drop – 118.0 meters.

Below the two larger entrances are high piles of rocks (“breakdown.”) The remains of goats, birds, and snakes have been found on the floor of the chamber. The entrance openings in the ceiling provide ambient light in the chamber most of the day. There are only a few stalactites and draperies on the ceiling and walls, but moderate and fragile speleothems are common on the floor. Growth only occurs during times of seepage and drips following heavy rains.

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