Bale, also known as Bali, is a historical region situated in southeastern Ethiopia. Its history is intertwined with diverse cultures, religions, and ecological significance. The Bale Oromo are a subgroup of the numerous Oromo people residing in the Horn of Africa, specifically in the Bale region of Oromia, Ethiopia. This region has witnessed considerable unrest and violence in recent decades.
Even though the Oromo constitute over half of Ethiopia's population, they have historically held a secondary status relative to the Amharic and Tigrinya peoples, who live north of Oromia. Amharic is the official language of Ethiopia, although many more Ethiopians speak an Oromo language. The two main languages for the Bale Oromo are Oromo and Borana-Arsi-Guji. Many Oromo express discontent with the central Ethiopian government, which is predominantly composed of non-Oromo people. Religion is another significant factor shaping their identity and experiences.
This article delves into the historical, geographical, and cultural aspects of Bale Province, highlighting its significance in Ethiopian history and its unique natural environment.
Map of Ethiopia showing Bale Province.
Historical Overview
Bale was first mentioned during the rule of the Zagwe dynasty, described as a "mysterious province" bordering Islamic sultanates. Islam was present in the province, evidenced by 13th-century Arabic inscriptions. Oral traditions suggest that Islam was introduced to Bale by Sheikh Hussein, a Muslim scholar of Somali origin who migrated from Merca in the 12th or 13th century.
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In 1332, Bale was conquered by the Christian king of the Ethiopian Empire, Amde Seyon. Ethiopian rule of Bale provided an outpost to carry out attacks on neighboring states, such as Ifat and Adal. In the early 15th century, Adal conquered Bale for a brief period, but it was soon retaken by Christian Ethiopia under Emperor Zara Yaqob.
Bale was the first territory in Ethiopia that leader of Adal Ahmad ibn Ibrahim al-Ghazi had invaded during his conquest of Ethiopia. By 1531, Bale was still unconquered and its people were largely unconverted. This prompted the Imam to send an army largely consisting of recent converts to subjugate the defiant province.
Bale soon fell under intense pressure from the Oromo expansion. The Muslim governor of the province, Umar, moved to the northern parts of the province to avoid any confrontation with the Oromos, allowing them to occupy much of the southern and central parts of the province.
Islamization of the Oromo
The Islamization of the Oromo in Bale began in the 18th century. Sheikh Muhammad Tilma Tiamo, came from Harar to Bale after having a dream in which Sheikh Hussien called him to propagate Islam to the people of Bale and revive the shrine of Sheikh Hussien. The Islamification of Bale was intensified after Emperor Yohannes IV harsh policy towards of Muslim of Ethiopia, which prompted many of them to flee to Bale.
Bale was finally incorporated into Ethiopia during the conquests of Menelik II. The Arsi were defeated in 1886 at the Battle of Azule, but Darge did not move into Bale until 1891. Darge then established a new provincial headquarters at Goba and gave the governorship to his son, Ras Asfaw.
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Geographical Significance
Bale is a vast administrative region in southeastern Ethiopia. It is a highland massif dominated by Mount Batu (4,307m A.S.L.). The volcanic highlands of Bale are covered with forests and, at greater heights, by afroalpine grassland. The Bale national park endeavours to protect highland forests and fauna, which seriously suffered from widespread fires in spring 2000. The authorities make great efforts to attract tourists and to organize tours of the Sof Omar caves.
The Bale Mountains, covering an area of 2200 km2, include the Sanetti Plateau, which is the largest alpine ecosystem in Africa. The Plateau extends between ca. 3800 to 4100 m asl, surrounded by the peaks of Tullu Konteh (4050 m asl) and Tullu Dimtu (4377 m asl), the second-highest peak of the country. Erratic boulders, moraines, small lakes present on the plateau and in trough valleys are clear indicators of former glaciations.
Due to the annual migration of the ITCZ between 10° North and South, the climate of the Bale Mountains is characterized by a pronounced rainfall seasonality with a short dry (November to February) and a long rainy season (March to October). The rain-bearing air masses derive from the Indian Ocean and the Atlantic Ocean via the Congo Basin, whereas northerly winds dominate during the dry season.
The south to north rainfall gradient and the altitudinal temperature gradient stratify the vegetation into the Afromontane forest, the Ericaceous belt, and Afroalpine zone. The Afromontane forest spans from ~ 1450 to 3200 m asl in southern exposition, and from ~ 2800 to 3300 m asl along northern slopes. The Ericaceous belt covers ~ 90,000 ha between ca. 3200 and 3800 m asl and is dominated by Erica arborea L. and Erica trimera (Engl.). The Afroalpine vegetation above 3800 m asl is open and rich in Tussock grasses and mainly dominated by Helichrysum splendidum-Alchemilla haumannii dwarf-scrubs and Giant Lobelia (L. rhynchopetalum), accompanied by patches of Erica, growing between big boulders along steep slopes.
4K African Animals: Bale Mountains National Park - Scenic Wildlife Film With Real Sounds
Bale Mountains National Park (BMNP)
The Bale Mountains National Park (BMNP) boasts a spectacularly diverse landscape mosaic comprised of distinct ecosystems and habitats and associated biodiversity. The property covers an area of 215,000 hectares in the heart of the Bale-Arsi Massif in the south-eastern Ethiopian Highlands in Oromia National Regional State. The National Park has been legally protected and demarcated since 2014.
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The property includes the Africa’s largest area of afro-alpine habitat above 3,000 m above sea level (a.s.l.) with numerous glacial lakes, wetlands and moorlands. Volcanic ridges and peaks tower above the plateau, most prominently Tullu Dimtu, Ethiopia’s second highest peak at 4,377 m a.s.l. Elsewhere in the park, extensive grasslands thrive next to various types of forests including tree heath, bamboo and juniper forests. As the origin of several important rivers, the ecosystems and habitats within BMNP and its surroundings regulate the supply of water for millions of people in and beyond Ethiopia.
The park and its surroundings are home to an extraordinary fauna and flora with an exceptional degree of endemism and in several cases the only remaining populations of globally threatened species across numerous taxonomic groups. For example, Mountain Nyala and Bale Monkey are both endemic to this area, along with numerous endemic rodents and amphibians, as well as the most important remaining population of Ethiopian Wolf.
Landscape of Bale Mountains National Park.
Outstanding Universal Value
The property protects a landscape mosaic of extraordinary beauty that is shaped by the combined forces of ancient lava outpourings, glaciation and the dissection by the Great Rift Valley. It features volcanic peaks and ridges, dramatic escarpments, sweeping valleys, glacial lakes, lush forests, deep gorges and numerous waterfalls, creating an exceptional natural beauty. The altitudinal gradient of the park spans almost 2,900 metres from the highest peak standing at 4,377 m a.s.l. (Tullu Dimtu) down to approximately 1,500 m a.s.l. in the Harenna Forest.
The property harbours diverse and unique biodiversity at ecosystem, species and genetic levels. The Sanetti Plateau and the slopes of the Bale Mountains National Park above 3,500 m a.s.l. encompass the largest intact and contiguous expanse of afro-alpine habitat in the world further adding to the importance of the property as a rare large-scale remnant of this habitat. The forests of the Bale Mountains serve as a genetic reservoir for Wild Forest Coffee and countless medicinal plant species.
Integrity and Management
Covering 215,000 hectares, the property serves as a meaningful and viable representation of afro-alpine and associated forests. The afro-alpine Sanetti Plateau is situated within the property in its entirety. At the foot of the southern escarpment lies the tropical moist Harenna Forest, one of Ethiopia’s largest natural forests, granted protection in the national law with about 100,000 hectares within BMNP and the adjacent areas.
The property has a recognized buffer zone comprising all 29 neighbouring kebeles (the smallest administrative unit in Ethiopia) surrounding the legally gazetted and demarcated park boundary as a key investment in the future integrity of the property. The buffer zone itself harbours very important conservation values, as well as securing landscape connectivity beyond the property.
Bale Mountains National Park is managed by the Ethiopian Wildlife Conservation Authority (EWCA). The entire surface area of the property of 215,000 hectares enjoys a high level of legal protection in line with IUCN Protected Area Category II. The national park is surrounded by an officially recognized buffer zone of 235,121 hectares, ranging between approximately 5 to 20 km from the boundaries of the park.
The property’s strategic and operational management is guided by a 10-year General Management Plans (GMP), which includes management programmes on Park Operations; Tourism Management; Interim Settlement & Grazing Management; Outreach and Ecological Management. Threats to the property are actively being addressed through the General Management Plan’s Interim Settlement Grazing Management Programme, a Grazing Pressure Reduction Strategy and a linked Livelihood Improvement Strategy, which include measures to reduce livestock to sustainable levels and gradually expand no-grazing zones through a participatory process with relevant communities.
The Bale Oromo People
The Bale Oromo face significant challenges, including limited access to electricity, education, and modern medicine. They are primarily farmers and pastoralists, cultivating crops such as cotton, maize, wheat, peanuts, coffee, and various fruits and vegetables. The region's susceptibility to drought often leads to famine, compounding their hardships. Their main form of transportation is the horse. Most Bale Oromo are unable to read and write.
Marriage to one wife is the norm for most Bale Oromo men. A wealthier man may have up to four wives. A man's wealth is frequently measured by how many cattle he owns. Bale Oromo marry within their Oromo people. Families arrange marriages. The new wife goes to live with her husband's family. Families live in round huts made from juniper and eucalyptus wood with a thatched roof. Couples have many children but many do not live past the age of five due to the lack of modern medicine. The average life span of the Bale Oromo adult is only 54 years.
The vast majority of the Bale Oromo are Sunni Muslims, and their practice of Islam is often intertwined with traditional folk beliefs.
The Bale Oromo require peace, access to education, modern medicine, and, above all, the opportunity to hear and understand the message of Jesus Christ.
Late Quaternary Paleoenvironmental Fluctuations
The highlands of the Bale Mountains in southeastern Ethiopia are promising sites for studying paleoenvironmental fluctuations. Their unique exposition to main atmospheric circulation systems contribute to their climate sensitivity. In addition, the special geomorphological features, characterized by high altitudes up to 4377 m above sea level (asl), by moraines and small glacial depressions, support the reconstruction of the landscape evolution. During MIS 3, the Bale Mountains were one of the most extensively glaciated mountains in Ethiopia. This caused a temperature decrease and a downward shift of Afroalpine vegetation.
Based on biogeochemical and palynological analyses of laminated lacustrine sediments, after deglaciation at about 18 cal kyr BP, a steppe-like herb-rich grassland with maximum Chenopodiaceae/Amaranthaceae and Plantago existed. Between 16.6 and 15.7 cal kyr BP, conditions were dry with a desiccation layer at ~ 16.3 cal kyr BP, documenting a temporary phase of maximum aridity on the plateau.
At ~ 15.7 cal kyr BP, the record shows an abrupt onset of the African Humid Period, almost 1000 years before the onset of the Bølling-Allerød warming in the North-Atlantic region, and about 300 years earlier than in the Lake Tana region. Erica pollen increased significantly between 14.4 and 13.6 cal kyr BP in agreement with periodically wet and regionally warm conditions. Similarly, intense fire events, documented by increased black carbon, correlate with wet and warm environmental conditions that promote the growth of Erica shrubs.
Conclusion
Bale Province, Ethiopia, represents a region of significant historical, geographical, and cultural importance. From its ancient Muslim roots and the conflicts of the medieval period to the stunning landscapes of the Bale Mountains National Park, Bale offers a rich tapestry of stories and natural wonders. The challenges faced by the Bale Oromo people underscore the need for continued efforts to promote peace, education, and sustainable development in the region.
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