Al Shouf Cedar Nature Reserve

Al Shouf Cedar Nature Reserve is a nature reserve in the Chouf and Aley districts of Lebanon. It is located on the slopes of Jebel Baruk mountain and has an area of 550 km2, nearly 5.3% of the Lebanese territory, making it the largest natural reserve in Lebanon.

The reserve contains the Lebanon cedar forests of Barouk, Maaser el Shouf and Ain Zhalta-Bmohray. It is an Important Bird Area (IBA) and Eco-tourism area. It hosts 32 species of wild mammals, 200 species of birds, and 500 species of plants.

Geodiversity
The Barouk mountain comprises rocks from the Pliocene which have undergone major tectonic movement that divided the mountains of Lebanon into two parallel parts; the eastern range is called the Anti-Lebanon, and the western range is called Mount Lebanon. The two mountain ranges are separated by the Beqaa Valley, which is composed of recent infill sediments. The main rocks are limestone. The whole of the Barouk Mountain is cavernous limestone, with many surface features such as dolines indicating the underlying cavernous forms of the mountain range. One particularly noteworthy cave, estimated to be 700 m long, is located near Niha village. Villagers report an abundance of stalactites and stalagmites and that there is an underground body of water.

The highest peak on the range at 1980 m. The trend from north to south is for the eastern slopes to change from very steep to less steep and for the western slopes to become increasingly steep. The top of the Barouk range becomes increasingly narrow towards the south.


 * Hydrology:

Precipitation in the watershed is the source of both surface streamflow and groundwater. The major portion of this occurs as rain. Snowfall often occurs at the upper elevations but snow seldom persists more than a few days and disappears before the end of the rainy season. Normally snow has little overall direct effect on stream-flow within the watershed. However, on rare occasions warm rains falling on the snow-pack may result in rapid melting and release of large quantities of water at a time when the soils are already fully saturated. These conditions result in rapid runoff and floods. A large proportion of the exposed surface rock in the Barouk region is cavernous, fissured and broken limestone, and its porous condition makes it very permeable. This results in much of the precipitation infiltrating with minimum surface runoff despite the often-shallow soils and sparse vegetative cover. Water percolates downward through the various formations and feeds the many large springs found on lower slopes in the area. Such springs help maintain stream-flow during the April to November dry season. Surface water flows originating on the range are mostly seasonal but some are perennial. Underground water generates outflow rivers such as: - Al Awali River, more commonly known as Al-Barouk river - Damour River, known as Al-Safa river The summit of the range is considered as a divide between two hydrological systems because of the difference between the two slopes of the mountain. The eastern slope is much steeper and favors surface stream flows, whereas the western slope is less steep and favors ground water aquifers. The rivers that flow in the valleys are the major source of agriculture irrigation and supply a dozen Shouf villages with domestic water and some of the western Bekaa villages. It is also the main source of water for the Aammiq Swamp in the Bekaa. From an erosion point of view these soils are in a state of equilibrium due to: The annual rainfall average is 1200 mm, and the mean annual temperature is 11.3 C. The mean daily maximum temperature is 23.4 C in August whereas the mean minimum temperature in January is -0.6 C. The absolute temperature ranges from -10.8 C in January to 32.3 C in August. The mean relative humidity lies around 65% but the eastern slopes are slightly drier. There are about 50 to 55 days of snow fall per year, depending on the information provided by the Ministry of Public Work and Transport.
 * Pedology:
 * Homogenous, belonging to the red brown Mediterranean soils formed on hard marl limestone.
 * derived from Jurassic, Balthonian, Callovian to Oxfordien - Portlandian marl limestone.
 * Stone contents ranges from 80 - 90%.
 * High permeability.
 * Mask of calcareous fragments.
 * Good vegetative cover.
 * Good drainage.
 * Climatology:

Biodiversity
The flora of the Al-Shouf Cedar area is partly covered by Mouterde's 1966, 1970 and 1983 flora of Lebanon. The most recent and extensive botanical researches on the official site were conducted, on behalf of the Ministry of Environment (Protected Areas Project), by (Georges Tohmé) the National Council for Scientific Research (NCSR) in 1999. Since then extremely few flora reports on the official site were published or known. Tohmé continued his field botanical studies at Al-Shouf Cedar Reserve during the last three years in order to obtain confirmation on the status of certain species. His recent new findings are published in Tohmé, G. & Tohmé, H. (2002). Few of them are incorporated here and the others will be added to the final report of the present study-project. The list of Al-Shouf Cedar Reserve species includes 500 identified species distributed over 61 families. Also the reserve is habitat to 25 internationally and nationally threatened species, 48 endemic to Lebanon or Lebanon and Syria or Lebanon and Turkey, and 14 rare species, whilst 214 species are restricted to the Eastern Mediterranean or Middle East area.
 * Flora

The reserve is also home to 24 tree species, of which some are found in Europe and the Mediterranean area as well as in Lebanon. The reserve is known for its official's efforts to save the cedar of Lebanon through continues management of the forests and planting new trees in previously logged and deforestated areas. The reserve form the last natural limits to the spread of Cedrus libani on the planet. The reserve is also known for the ability of the forests to regenerate by their own without any human interference. Other tree species in the reserve include : Cyprus oak (Quercus infectoria ), Brant’s oak (Quercus brantii), kermes oak (Quercus calliprinos), Calabrian pine (Pinus brutia), Aleppo pine (Pinus halepensis), stone pine (Pinus pinea), Greek juniper (Juniperus excelca), Syrian juniper (Arceuthos drupacea).

Cultural heritage
The cedar forests of Lebanon enjoy the unique distinction as the oldest documented forests in history. The cedars were important enough in the history of man to be traceable to the very earliest written records, that of the Sumerians in the third millennium BC. In the ancient Sumerian story, The Epic of Gilgamesh, one of the oldest pieces of literature in the world, the cedars feature prominently. Gilgamesh has since been recognized as King Gilgamesh of history and in probability visited Mount Lebanon. The setting of the Shouf is a nexus of many cultures, religions, and historical events, all of which have left an imprint which makes the area's cultural heritage as rich as its ecosystems. The following are some major landmarks: The cave castle of Tyron Niha relates to one of the closing episodes of Prince Fakhreddin II's epic history and are the only remaining vestiges of a once powerful fortress which was successively used by the Arabs, Crusaders, and a number of princes of Mount Lebanon. A feretory was built on the hill above the village of Niha to honor Job's memory and hold his relics. Ayoub is the Arabic name of the prophet Job. This once powerful Druze fortress served as a guardian outpost controlling the road that linked Beirut to Damascus, and a marching post for the Druze and Chehab rulers of the South Bekaa or Wadi al-Taym. El Sit Cha'wane is a famous figure in the Druze religion. Like Job in the Old Testament, she was held up as a model of virtue and devotion. A feretory was erected in her name.
 * The cedars:
 * Historic cultural sites:
 * Qalaat Niha:
 * El Nabi Ayoub:
 * Qab Elias Castle:
 * Mazar El Sit Cha'wane: