Jizan, February 28, 2024, Recent discoveries on the summits of Al-Qahar Mountains, situated northeast of the Jazan region approximately 130 kilometers from Jizan, indicate a fascinating geological history suggesting that these mountains, part of the Al-Reeth Governorate, might have once been submerged underwater for hundreds of millions of years, constituting the ancient seabed.
Dr. Zaraq bin Issa Al-Faifi, a professor at Jazan University's Department of Biology and College of Science, spearheaded research in the region, revealing compelling evidence of the mountains' aquatic past. Fossils and remnants of marine organisms such as stone corals were among the findings supporting this theory. Dr. Al-Faifi highlighted the presence of sand and limestone formations, distinctive sedimentary layers of varying hues, easily crumbled by hand, as further indications of the area's submerged history. These observations were complemented by numerous signs and markers observed on the mountain peaks.
Emphasizing the importance of further investigation into the historical context of this period, the state of Al-Qahar Mountains during its underwater phase, and the marine landscape of that era, Dr. Al-Faifi urged geologists and experts to delve deeper into this intriguing facet of the Sarawat Mountains.
At elevations exceeding 2,000 meters above sea level, Al-Qahar Mountains boast a plethora of geological marvels, including unique conical formations, distinct sedimentary and limestone rocks, deep canyons, and steep inclines. The mountains also host several inhabited towns and cities, adding to their allure for history enthusiasts and mountaineers. Renowned as Mount Zahwan, the rugged terrain and steep slopes of Al-Qahar Mountains lend credence to their imposing name.
The Saudi Geological Survey (SGS) affirmed the presence of fossils in Al-Qahar Mountains and other ancient environments through the examination of sedimentary rocks and contained fossils. They noted that geological mapping and earlier studies in the region provided insights into these ancient environments. According to the SGS, sedimentation occurred in low-lying areas during deep geological epochs, eventually leading to the region's elevation through various geological processes to its current altitude.
