Jabal Hafeet (, "Mount Hafeet"; variously transcribed Jabal, Jabel or Jebal and Hafit or Hafeet – literally "empty mountain") is a mountain in the region of Tawam, on the border of the United Arab Emirates and Oman, which may be considered an outlier of Al Hajar Mountains in Eastern Arabia. Due to its proximity to the main Hajar range, the mountain may be considered as being part of the Hajar range. To the north is the UAE city of Al Ain, in the Eastern Region of the Emirate of Abu Dhabi, and the adjacent Omani town of Al-Buraimi. The sole mountain in the Emirate of Abu Dhabi, and one of the highest mountains in the country, it has given its name to a period in UAE history, the Bronze Age (3200 to 2600 BCE) Hafit Period, because of the discovery of a cluster of important Bronze Age beehive tombs at its foothills. As of 2017, the mountain is recognised as being part of a national park, and was incorporated into the Sheikh Zayed Network of Protected Areas in 2018. Climate Jebel Hafeet has a hot desert climate (BWh) according to the Köppen climate classification. On average, of rain falls annually. The temperature is relatively cool from October to March, usually remaining below . The average overall temperature is . Orography and geology Geology The Jabal Hafit mountain trends NNW–SSE over about and is wide. It protrudes above the surrounding plains. The mountain consists of shallow marine sedimentary rocks, which includes limestone, marl, and evaporites. These layers contain many fossils which includes corals, foraminifera, and bryozoa. Fossils indicate that the sedimentary rocks exposed at the surface range from early Eocene to early Miocene in age, younging from the mountains core to its flanks. This structure is an anticline, or more specifically an east-verging pericline. The west limb has a dip of around 30° and the east limb has overturned bedding at 70° in the central area. This results in an inclined axial plane, creating an asymmetric fold. This is unexpected because the structure is folding towards the Hajar Mountains in the east. If the structure is related to the formation of the Hajar Mountains, the anticline would typically be west verging. This indicates that the Jabal Hafit anticline formed due to a backthrust (antithetic fault), and is a fault-propagation fold. Within the eroded core of the anticline, at the Green Mubazzarah