Ethiopia's historical geological processes and climatic variations have resulted in varied soil and biological diversity.
Distribution of wildlife and natural vegetation is influenced by:
Climate
Soil types
Drainage
Ethiopia is home to many unique endemic fauna and flora resources.
Composition of soil includes:
Weathered Mineral Materials (45%)
Organic Matter (5%)
Air (20-30%)
Water (20-30%)
Soil Formation:
A long-term process, taking thousands of years.
Influenced by:
Climate and topography
Parent material (rocks)
Living organisms
Vegetation cover
Time
Weathering: Breakdown of rocks into smaller soil pieces through:
Frost action
Rainwater action
Extreme temperature variations
Biological activity
Types of weathering:
Mechanical (Physical) Weathering:
Physical disintegration of rock without changing composition.
Involves:
Differential stresses
Frost action
Abrasion (erosion by friction)
Biological Weathering:
Weakening and disintegration from biological agents:
Plant roots
Burrowing animals
Microbes (bacteria and fungi)
Chemical Weathering:
Disintegration through chemical reactions, altering composition.
Major reactions include:
Carbonation
Dissolution
Oxidation
Hydrolysis
Physical Properties:
Texture, structure, porosity affecting air and water movement.
Chemical Properties:
Availability of minerals, electrical conductivity, soil pH.
Ethiopian soils derived from:
Crystalline, volcanic, and Mesozoic sedimentary rocks.
Soil Types (FAO classification): 18 soil types, major ones cover 87.4% of land area.
Develop on gently sloping ground in highlands with high rainfall.
Strongly weathered, high leaching, reddish-brown color due to iron oxides.
More productive than most tropical soils.
Found in:
Western Highlands (Wellega)
Southern/Central/Eastern Highlands
Associated with high rainfall highland areas.
Low productive capacity, known for nutrient loss.
Found alongside nitosols in SW highlands.
Found in highlands and moderate climates.
Heavy clay soils, prone to swelling and cracking.
Develop from volcanic basalt and sedimentary rocks.
Found in NW, Central, and SE Highlands.
Desert soils in arid areas, characterized by high salt content and low organic matter.
Fertility improved by irrigation.
Definition: Deterioration of soil properties (physical, chemical, biological).
Types:
Physical Degradation: Includes compaction and soil erosion.
Biological Degradation: Loss of organic matter, carbon, and soil fauna.
Chemical Degradation: Nutrient depletion, toxic chemical buildup.
Aim: Reduce erosion for sustainable agricultural production without environmental damage.
Major control mechanisms:
Biological Control:
Vegetative strips
Afforestation and reforestation
Physical Control:
Terracing, check dams, contour ploughing.
Natural Vegetation (NV): Plant cover with minimal human interference.
Controlled by: altitude, climate, and drainage.
Estimated 6000 species of plants, with 10% endemic.
Afro-alpine and sub-afro-alpine Region
Forest Region
Woodland Savanna Region
Steppe Vegetation Region
Semi-Desert Vegetation Region
Afro-Alpine: Found between 3,200-4,620 m; characterized by tussock grasslands and lichens.
Forests: Vary from humid to arid; characterized by distinct flora.
Woodland Savanna: Xeromorphic characteristics; trees shed leaves in dry season.
Major causes:
Forest clearing for agriculture
Timber exploitation
Overgrazing and urban expansion.
Birds: 860 species (16 endemic).
Mammals: 279 species (31 endemic).
Includes Walia Ibex, Gelada Baboon, and Ethiopian Wolf.
Ecological, economic, and recreational values.
Used for scientific research and promoting tourism.
Protected areas established:
National parks and sanctuaries where legal hunting is regulated.
Challenges faced in protected areas:
Human expansion, overgrazing, illegal wildlife trade.