
The Arabic word Shadah comes from singing. The medieval geographer Yaqut al-Hamawi recorded it in his 13th-century Mu'jam al-Buldan as a pair of mountains, Shadah al-Asfal and Shadah al-Ala, lower and upper, rising together above the low plains of Tihamah. Shadah al-Asfal is the southern one, reaching more than 1,500 meters above sea level, its massif a jumble of Precambrian granite spires that locals call Nadba, some of them standing like upended ships, nearly 200 meters tall, worn into shape by a billion years of weather.
The Shadah massif lies in Al-Bahah region near the towns of Makhwah and Qilwah, in the southwestern corner of Saudi Arabia where the Sarawat Mountains rise sharply from the Red Sea coastal plain. Shadah al-Asfal belongs to the Zahran tribe. Shadah al-Ala, just to the north, belongs to the Ghamd tribe. Both tribes have held their respective mountains for centuries and continue to hold them, with villages spread across the ridges and foothills. The mountain is bordered on the east by Makhwah Governorate, on the west by the Qarama Mountains, on the south by Al Khuraig and Bani Shorafa, and on the north by Shadah al-Ala and Nira Valley. The larger range sits among mountains that are among the highest in the Kingdom.
The archaeology researcher Ahmed Qashash has described the geology directly. The two Shadah mountains are composed of granite igneous rocks that were uplifted and exposed long ago, during Precambrian mountain-building events, the earliest geologic age of Earth's formation. Over the intervening billion-plus years, the rocks have been carved by water, wind, and heat into caves and caverns. Some of the caves formed through millions of years of erosion. Others are the frozen ghosts of gas bubbles, cavities left inside the magma when it crystallized, revealed as the rock wore down. Still others are the spaces left when huge boulders fell on top of each other, creating chambers underneath. These caves are especially abundant on Shadah al-Asfal. For the people who live on this mountain, they are more than geological features.
People have lived in the caves of Shadah al-Asfal since early human habitation of the peninsula, and the caves remain inhabited. They are fortified natural dwellings, cool in summer heat, sheltered from the brief but heavy rains that come in winter storms, defensible in centuries when that mattered. Qashash calls them ideal homes for the people of these mountains. Around 4,000 people live across Shadah al-Asfal today, distributed among villages on the summit, the flanks, and the foothills. Alro'os sits at the very top. Once it was an agricultural capital with coffee trees, pomegranates, bananas, fruits and vegetables. Most of those crops have perished because the rains have grown unreliable and there are no dams to store what does fall. The terraces survive. So do the orchards of the villages that sit lower down, catching what water they can from the valleys.
The villages of Shadah al-Asfal sound like a tribal genealogy recited aloud. Alro'os at the top. Alfarea, the second largest, below it. Alashraaf on the summit. Rahban to the west, Alnemra west of Rahban, Altwaref south of Alnemra. Aldahna southwest of Alro'os. Tha'lab to the north of Alro'os, Alasaha west of Tha'lab, Altaraf in the north near the foothill. Hazah, tucked in a deep chasm southeast of Altaraf, inhabited by the Bani Umar tribe. Adad at the southern foothill. Alshefa at the top looking out over Tihamah. Alaradia on the east of Alashraaf, on the road to Alshefa. The valleys have their own names: Dhi Hada, Tajma, Nat'a, Kharas, Nawan, Helfa. The place is lived-in down to the smallest ridge, and every name here belongs to someone whose great-grandparents lived in the same houses.
Across the mountain, in caves and on cliff faces, Nabataean inscriptions remain. At Rahwat al-Dahnah, ancient paintings depict the lives of sultans with crowns on their heads. Other inscriptions appear in a cave in Alashraaf, in the village of Alaradia, and in the cave of Al-Adah in Alfarea, in front of the old school. Nabataean writings and symbols are carved in and around Alashraaf, especially at Al-Harir and Shafa Al-Sakhra. The Nabataean civilization, the one that carved Petra from the cliffs of Jordan, ranged south through northwestern Arabia and into the Tihamah highlands. On Shadah al-Asfal, their carvings speak to a trade network that crossed these mountains, caravans and their merchants leaving marks on the walls of the caves where they sheltered. Archaeological surveys in 2023 reported further discoveries of ancient granite walls and chambers at Al-Mamalah in Al-Baha, some of the Shadah caves dating back more than 3,000 years.
The first primary school for boys on Shadah al-Asfal opened in 1388 AH (roughly 1968 CE), with 45 students in the first year. By 1393 AH, ten graduates ranked in the top ten of the Al-Qunfudhah educational district. An elementary school for boys opened in Tha'lab in 1403 AH, an intermediate school in Alfarea in 1407 AH. The first girls' elementary school opened in 1403 AH in Alfarea, followed by a second in Tha'lab in 1404 AH. The first intermediate school for girls opened in 1412 AH in Alfarea. It is a short list of dates for a mountain that has been inhabited for thousands of years, but it represents a real transformation. Children who once would have learned only what their parents taught them can now study in a language that reaches beyond the valleys. The mountain is still mostly the same. What happens on it, for some of its residents, has changed.
Shadah Al-asfal is located at 19.73 degrees north, 41.38 degrees east, in Al-Bahah Province in southwestern Saudi Arabia. Nearest major airport is Al-Baha Domestic Airport (OEBA), roughly 90 km east. The Red Sea coast lies 50 km to the west. From altitude, the Sarawat range appears as a sharp escarpment between the coastal Tihamah plain and the higher inland plateau. Summit elevations exceed 1,500 meters. Hot desert climate below; cooler temperatures at altitude. Visibility is typically good but dust and haze can reduce it, especially in summer. Mountain weather can change quickly.