Chapter's Objectives

At the end of this chapter you will be able to;
 Identify major soil types of Ethiopia
 Understand soil degradation and conservation measures
 Describe the distribution of natural vegetations in Ethiopia
 Explain the significance of wildlife resources of Ethiopia

6.1 Introduction                                        

The past geological process and varied climatic events ensued Ethiopia to have varied soil and biological diversity. The formation and spatial variabilities of soils in Ethiopia is largely related to topographic and climatic factors, parent material (rocks) and land use. Different parts of Ethiopian regions experiences. Likewise, the distribution of wildlife and natural vegetation in Ethiopia and the Horn is controlled by many factors important among which are climate, soil types, drainage, etc. Natural vegetations are vital for human beings in many ways. Plants can provide shelter, food, source of fuel, pasture and grazing, raw material for industries. Ethiopia possesses unique and characteristic fauna and flora with a high level of endemicity. However, manmade as well as natural problems are threatening their availability and distribution.

6.2. Soil – Formation

Soil is a delicate but highly varied composition of mineral particles, organic matter and living organisms in dynamic equilibrium. This variability reflects primarily the parent material from which the soil was formed over very long periods of time and the environment in which the soil has developed. It consists of weathered mineral materials (45%), organic matter (5%), air (20-30%) and water (20-30%).

Soil formation is a long-term process. It could take several thousands of years to form a single stratum of soil. As it is a complex mixture of several constituents, its formation is also more complex. The formation of a particular type of soil depends on parent material, climate, topography, living organism and time.

Weathering disintegrates the inorganic substances (rocks) of soils. It is the breakdown of rocks at the Earth’s surface, by the action of rainwater, extremes of temperature, and biological activity. There are three types of weathering involving in soil formation. These are:

Physical disintegration causes decrease in size without appreciably altering composition. Differential stresses due to heating and cooling or expansion of ice break the rock. Abrasion (erosion by friction) due to water containing sediment or wind carrying debris is another type of physical weathering.

The process of biological weathering involves the weakening and subsequent disintegration of rock by plants, animals and microbes. Roots of plant can exert pressure on rock. Although the process is physical, the pressure is exerted by a biological process (i.e., growing roots). Microbial activity breaks down rock minerals by altering the rock’s chemical composition, thus making it more susceptible to weathering.

Chemical weathering involves the modification of the chemical and mineralogical composition of the weathered material. A number of different processes can result in chemical weathering. The most common chemical weathering processes are hydrolysis, oxidation, reduction, hydration, carbonation, and solution.

In most cases, the minerals in the parent materials are also found in the soils, which are formed from the disintegration and decomposition of the rock. However, this is not true of alluvial soils, which are transported from one place to the other by agents like running water.

Soils have two basic properties:

Physical properties

Soil physical properties are influenced by composition and proportion of major soil components. Properties such as texture, structure, porosity etc. are categorized under physical soil properties. These properties affect air and water movement in the soil, and thus the soil’s ability to function.

Chemical Properties

Soil chemistry is the interaction of various chemical constituents that takes place among soil particles and in the water retained by soil. Soil properties like availability of minerals, electrical conductivity, soil pH, etc. Soil chemical properties affect soil biological activity and indirectly the nutrient dynamics.

6.3. Major Soil Types in Ethiopia

Soils of Ethiopia are basically derived from crystalline, volcanic and Mesozoic sedimentary rocks. One can therefore, say that some of the soil divisions in the country are based on the geologic structure. However, it should be born in mind that, there are soils formed due to long waited deposition of sediments.

FAO has identified 18 soil associations in Ethiopia at scale of 1:2,000,000. Out of the major soils, 11 soil associations cover about 87.4 percent of the land area. The six major groups of soils in Ethiopia are discussed under the following points:

Nitosolsdevelop on gently sloping ground. Their parent materials include trap series volcanics, volcanic ash, and even metamorphic rocks. They are strongly weathered soils but far more productive than most other tropical soils. They are basically associated with highlands with high rainfall and they were, probably, formed on forest covered areas originally.

Due to the high rainfall, there is considerable soil leaching which makes the nitosolsto be poor in soluble minerals like potassium, calcium etc.; and rich in non-soluble minerals like iron and aluminum. The reddish-brown color of these soils is because of high concentration of iron (ferric) oxides due to leaching. But they are now widely found on cultivated areas and on mountain grasslands. Nitosolsare dominantly found in western highlands (Wellega), southwestern highlands (Kaffa, Illuababora), Southern highlands, Central highlands, and Eastern highlands.

Acrisolsare one of the most inherently infertile soils of the tropics, becoming degraded chemically and organically very quickly when utilized. In Ethiopia, it has lost most of the base nutrients and are characterized by low productive capacity. Acrisolsare found along with nitosolsmostly in some pockets of southwestern highlands of Ethiopia where there is high rainfall.

Vertisols are heavy clay soils with a high proportion of swelling clays when wet, and cracks when dry. These soils are extremely difficult to manage (hence easily degraded), but has very high natural chemical fertility. Vertisols mostly develop on volcanic plateau basalt, trachyte and pyroclastic materials, sedimentary rocks, colluvial slopes and alluvial plains. In Ethiopia, they are commonly found in parts of Northwestern, Central and Southeastern highlands (especially in Gojjam, Shewa, Arsi, Bale and central Hararghe).

These soils are mostly found in rugged topography and steep slopes. There is little evidence of pedogenic processes (soil forming processes). As a result, they are young, shallow and coarse textured and so have low water holding capacity. In addition, they are found in areas of low rainfall. So, most of the areas covered by these soils have limited agricultural use. They are, in most cases, left under the natural plant cover and used for grazing.

By and large, these soils are found in different parts of rugged and steep slopes of Central Highlands, on the Rift Valley Escarpments and highlands in of western Hararghe. Regosol and Lithosols are also found in the Danakil and eastern Ogaden.

These are soils of desert or dry steppe soils majorly available in arid and semiarid areas. Though the degree may vary, desert soils are characterized by high salt content and low organic content, because of the scanty vegetation. Generally speaking, these soils have poor humus content and nitrogen, but are rich in phosphorus and potash and can be very fertile if irrigated.

Xerosols are soils of the deserts, has low organic content. Yermosols are even drier and more problematic than Xerosols. Solanchaks are saline soils which develop in areas of high evaporation and capillary action. Badly managed irrigation schemes may turn soils into solonchaks.

In Ethiopia, Xerosols are found in Ogaden and northeastern escarpments, whereas the Yermosols and Solonchaks cover the Ogaden and Afar plains. The Solonchaks are majorly located in salty plains of Afar.

Fluvisols develop on flat or nearly flat ground, on recent alluvial deposits. These soils are associated with fluvial (river), marine (sea) and lacustine (lake) deposits.

These are soils formed due to deposition of eroded materials from highlands. The deposition takes place in depressions, lower valleys and lowlands. Lower regions of rivers like Omo, Awash, Abay and the plains of Akobo and Baro Rivers are home for fluvivsols. Lakes region (main Ethiopian rift) is also characterized by fluvisols.

Fluvisols are highly variable, but much prized for intensive agriculture because:

  • They develop on flat ground, deposition sites,
  • They are associated with rivers and ground water, making them important for large-scale irrigation and
  • They are fertile and their fertility is always renewed as a result of deposition of new soil materials.
  1. Luvisols

Luvisols develop mainly in areas where pronounced wet and dry seasons occur in alternation. Where leaching is not very high, they are found in association with nitosols. Luvisols have good chemical nutrients and they are among the best agricultural soils in the tropics. So, they are intensively cultivated. However, when luvisols are found on steep slopes (stony) and on flat areas (waterlogged) they are avoided and left for grazing. In Ethiopia, places with luvisols include Lake Tanaarea, parts of Northern, Central and Eastern Highlands and Southern lowlands.

6.4. Soil Degradation & Control Measures

Soil degradation

Soil degradation is defined as a change in any or all of the soil status resulting in a diminished capacity of the ecosystem to provide goods and services. It could also be the deterioration of the physical, chemical and biological properties of soil.

There are three major types of soil degradation. These are:

Physical Degradation refers to the deterioration of the physical properties of soil. This includes:

Compaction: densification of soil is caused by the elimination or reduction of structural pores. Soils prone to compaction are susceptible to accelerated runoff and erosion.

  • Soil erosion: is a three-phase process consisting of the detachment of individual soil particles, transportation and deposition.

Reduction in soil organic matter content, decline in biomass carbon, and decrease in activity and diversity of soil fauna are ramifications of biological degradation.

Nutrient depletion is a major cause of chemical degradation. In addition, excessive leaching of cat-ions in soils with low-activity clays causes a decline in soil pH and a reduction in base saturation.

Causes of soil degradation

Soil degradation may result from natural and human-induced causes. Topographic and climatic factors such as steep slopes, frequent floods and tornadoes, storms and high-velocity wind, high-intensity rains and drought in dry regions are among the natural causes. Deforestation and overexploitation of vegetation, overgrazing, indiscriminate use of agrochemicals and lack of soil conservation practices, and over extraction of ground water are some anthropogenic causes of soil degradation.

Soil Erosion Control Measures

The aim of soil conservation is to reduce erosion to a level at which the maximum sustainable level of agricultural production, grazing or recreational activity can be obtained from an area of land without unacceptable environmental damage. Since erosion is a natural process, it cannot be prevented. But it can be reduced to a maximum acceptable level or soil loss tolerance.

We have two major soil erosion control mechanisms. These are:

These types of soil erosion control mechanisms include vegetative strips, plantation, and reforestation. Biological controls can prevent splash erosion, reduces the velocity of surface runoff, increases surface roughness which reduces runoff and increases infiltration, and etc.

Physical measures are used to control the movement of water and wind over the soil surface. The major types of physical erosion control measures commonly applied in Ethiopia includes terracing, check dams, gabion, trenches, contour ploughing, soil bunds etc

6.5. Natural Vegetation of Ethiopia

6.5.1. Introduction

Natural vegetation refers to a plant cover that develops with little or no human interference. It can also be seen as any original plant cover grown in an area. Its distribution on the surface of the earth is uneven majorly controlled by factors such as climate, soil types, drainage, etc. However, to a large extent, temperature and precipitation affect the spatial distribution and the original plant cover of a region. That is why, more than any other single element, the natural vegetation of an area becomes a very good indicator of the climatic conditions.

Natural vegetations are vital for human beings in many ways. Plants can provide shelter, food, source of fuel, pasture and grazing, raw material for industries, source of timber and non-timber products. The other uses include moderating effect on local climate, as home of wild life, medicinal values, minimizing soil erosion etc.

The characteristics of Ethiopia’s natural vegetation are to a large extent determined by elevation (and temperature) and rainfall. In Ethiopia, since temperature is mostly controlled by elevation, the spatial distribution of natural vegetation in the country is strongly correlated to it. Lowlands due to their low rainfall and high temperature have harsh environment and are characterized by xeromorphic plants (plants which are adapted to drought and high temperatures). Highlands (up to about 3000 m) are cooler than the lowlands and where there is adequate moisture a variety of forests can be seen. Plants whose growth is limited by the low temperature characterize high altitude areas (mostly above 3000 m). Ethiopia possesses an estimated number of 6000 species of higher plants of which 10% are endemic.

6.5.2. Major Natural Vegetation Types of Ethiopia

Taking altitude into consideration it is possible to broadly classify the vegetation belts of Ethiopia into the following five groups.

Ethiopia has the largest extent of Afro-alpine and sub afro-alpine habitats in Africa. This vegetation type, also known as high mountain vegetation is similar to the Alpine vegetation in temperate regions. These ecosystems are found on mountains having an elevation ranging between 3,200 and 4,620 meters above sea level. The Afro-alpine habitat covers nearly 1.3% of the total landmass of Ethiopia.

The Afro-alpine region is found at very high altitudes (4,000 – 4,620 m). Like any other landform in Ethiopian, the climate of Afro-alpine ecosystems is controlled by latitude and altitude. The annul precipitation which ranges between 800 and 1,500 mm, is mostly in the form of sleet or snow. Temperature records of 0oC and below are widely experienced in these ecosystems. Soils in this ecosystem are mostly shallow and eroded. The Bale and Semein mountains are typical examples of afro-alpine vegetations.

Compared to the Afro-alpine, the Sub-afro-alpine region is found at a lower elevation, roughly between 3,300 and 4,000 meters. As a result, the plants in this region are adapted to somewhat less extreme environment than the Afro-alpine.

Vegetation in the Afro-alpine region consists of tussock grasslands, scrub, scattered mosses and lichens while the Sub-afro alpine region is dominated by woodland, often degraded to scrub stages and also wet grasslands. Lobelia rhynchopetalum(giberra) and Erica arborea(Asta) are some of the dominant species in the Afro-alpine and Sub-afro alpine regions respectively.

Forest is a complex ecosystem consisting predominantly of trees that shield earth and support numerous life forms. Not all forests are similar in terms of species composition, structure and physiognomy. In any geographical region, environmental factors such as climate, soil types, topography and elevation determine the types of forests.

In Ethiopia, forests are found at different elevations, 450 to 3,500m in humid parts and 2,300 to 3,300 m in most arid parts. Moreover, forests are characterized by variation in mean annual rainfall that range between 200 and 2,200mm. These wide variations in rainfall and altitude result in two broad classification of forests: Highlands and Lowland forests. Highland forests include Hagenia Abyssinia (Kosso), Juniper procera (tid), ArundinariaAlpina(kerkha), Podocarpusfalcatus (zigba), Aningeriaadolfi-friedericii (keraro) and Oleaafricana (Weyra) forests; while Baphia are classified as lowland forests. Moreover, there are also Gallery (Riverine) Forests. These are forests that stretch along the banks of the lower courses of rivers. Riverine forests are classified as lowland forests and are found in some places such as the banks of Awash, Wabishebelle, Ghenale etc. Dominant species include Ficussur (sholla) and different kinds of acacia trees.

Like the forests, the woodland savannahs are also found in areas of wide altitudinal ranges (250 to 2,300 m). Although the mean annual rainfall ranges between 200 and 1,400 mm, the large part of this region is found at a lower elevation and in a drier environment. The plants in the woodland savannah are known for their xeromorphic characteristics like shading of leaves during the dry season. Vegetation types with intermediate characteristics between savannahs and woodlands are shrublands and bushlands. Woodland savannah region can be broadly classified into three divisions:

  • Juniper procera(tid) is dominant species for both the Junipers Forests and Junipers Woodlands. The difference is in height: 3 – 45 meters tall in the forests and 10 -15 meters in the woodlands.
  • Acacia woodlands are dominated by both trees and shrubs, which belong to the same genus ‘Acacia’. E.g. Acacia etbaica(grar), Acacia mellifera(Konter).
  • Mixed deciduous woodlands: As the name implies, most of the trees in mixed deciduous woodlands shed their leaves during the dry season.

 

Table 6.1: Woodland Savanna Region

Woodland savanna type

Altitude(m)

MeanAnnual RF (mm)

Growing season(No. of months)

Dominant species

Junipers woodland

1,350-2,200

500-900

4-8

Junipers procera

Acacia woodland

250-2,300

200-1,000

1-9

Acaciaetabica(Grar)

Mixed deciduous woodland

300-1,300

800-1.400

5-12

Mixed trees

These are regions in the arid and semiarid parts of the country where the temperature is very high and the rainfall very low. Both are found at low elevations, the steppe at elevations of 100 to 1,400 m above sea level and the semi-deserts at 130 meters below sea level to 600 meters above sea level.

The steppe gets a mean annual rainfall of 100 to 550 mm as compared to 50 to 300 mm for the semi desert areas. Growing period lasts up to 2 months for the steppe and a maximum of one month for the semi-deserts. Even though there is a variation in the degree of alkalinity and salinity; soils in both regions are generally alkaline and saline.

In these regions xerophytic (i.e. drought-resisting plants) are the dominant vegetations. Xerophytic plants such as short shrubs, scattered tufts of grass species and a variety of acacias are some of the examples. Where there are moist soils, rich vegetation of acacia and palm trees may be observed. Trees are normally restricted to fringes along watercourses.

6.5.3. Natural vegetation Degradation & Conservation

Natural vegetation Degradation

Over the past century, a rapid growth of the already dense Ethiopian population has led to overexploitation of the land. In areas with settled agriculture, new land has been cleared at the expense of forests. Ethiopia’s forest resources have been disappearing at an alarming rate. A century ago, forests covered about 40 percent of the total land area. For the last few decades, forests have been cleared for different reasons. Major causes for the gradual disappearance of the natural vegetation in Ethiopia are:

Clearing of forests for cultivation

  • Timber exploitation practices
  • Charcoal burning and cutting for fuel
  • Extensions of coffee and tea production areas
  • Overgrazing
  • Expansion of settlements both rural and urban, and clearing for construction.

 

Natural Vegetation Conservation

Conservation of biodiversity is protection and management of biodiversity so as to maintain at least its current status and derive sustainable benefits for the present and future generation. There is an urgent need of conservation of the ever-degrading biodiversity. There are three main approaches of biodiversity conservation:

Protection: through designation and management of some form of protected area. Protected areas include sanctuaries, national parks, and community conservation areas.

Sustainable forest management: involving sustainable harvesting of forest products to provide a source of financial income

Restoration or rehabilitation: is the process of assisting the recovery of a forest ecosystem that has been degraded, damaged, or destroyed. This may involve the re-establishment of the characteristics of a forest ecosystem, such as composition, structure, and function, which were prevalent before its degradation.

6.6. Wild Life/Animals in Ethiopia

6.6.1. Wildlife in Ethiopia

Ethiopia is one of the few countries in the world, which possess unique and characteristic fauna with a high level of endemicity. Existence of wide range of ecosystems endowed Ethiopia with great varieties of habitats contributing for the occurrence of high faunal diversity. However, data on faunal resource of the country is as a whole is limited to mammals, birds, reptiles, amphibians and a few groups of arthropods.

Ethiopia has about 860 avian species (16 endemic species and two endemic genera), 279 species of mammals (31 endemic species and six endemic genera), 201 species of reptiles (14 endemic species), 23 species of amphibians (23 endemic species), and 150 freshwater fish (6 endemic species).

A total of 279 mammalian species of which 31 are endemic are known to occur in Ethiopia including those that require urgent conservation action i.e. Walia Ibex (Capra walie), Gelada Baboon (Theropithecus gelada), Mountain Nyala (Tragelaphusbuxtoni), Ethiopian Wolf (Canissimensis), Starck‟s Hare (Lepusstarcki).

Generally speaking, the main wild life concentrations in the country occur in the southern and western parts. The wild animals in Ethiopia can be classified into five major groups:

  1. Common wild animals (those animals that are found in many parts of the country (e.g. hyenas, jackals)
  2. Game (lowland) animal, (which include many herbivores like giraffes, wild asses, zebras etc. and carnivores like lions, leopards, and cheetahs)
  3. Tree animals or arboreals (which include monkeys, baboons)
  4. A variety of birds in the Rift Valley lakes
  5. Rare animals (gelada baboon and Semien fox) scattered in highlands; walia- ibex in the Semien Massifs, Nyala in the Arsi Bale massifs).

 

6.6.2. Wildlife Conservation

What are the challenges of wildlife conservation in Ethiopia?

Wildlife plays an important role in several ways. The importance of wildlife can be categorized as ecological importance, economic importance, investigatory importance, conservation of biological diversities etc. Wild animals can be used for:

 Scientific and educational researches (valuable information for medical purposes and environmental studies)

 Physical and mental recreation (aesthetic value)

 Promotion of tourism (economic value)

 It’s potential for domestication

 Maintaining ecological balance

To prevent the destruction of wildlife a total area of nearly 100,000 square kilometers of national parks, sanctuaries, community conservation areas, botanical gardens, wildlife reserves etc. have been established in different part of the country. Hence in Ethiopia there are:

 21 major national parks

 2 major wildlife sanctuaries,

 3 wildlife reserves,

 6 community conservation areas,

 2 wildlife rescue centers,

 22 controlled hunting areas,

 2 botanical gardens and 3 biosphere reserves

Even though the number and the predominant animals may vary, many of the national parks in Ethiopia have different turnovers of animals. These include buffaloes, zebras, lions, elephants, ostriches, giraffes, oryx, African wild asses, etc.

Table 6.2: National Parks of Ethiopia

S.N

Name

Region

Year est.

Area in sq.km

1

KafetaShiraro

Tigray

1999

5000

2

Semien Mountains

Amhara

1959

412

3

Alatish

Amhara

  

4

Bahir Dar Blue Nile River Millennium

Amhara

2008

4729

5

BorenaSaynt

Amhara

2008

4325

6

Yangudi-Rassa

Afar

1969

4731

7

Awash

Oromiya and Afar

1958

756

8

DatiWolel

Oromiya

2010

1031

9

Bale Mountains

Oromiya

1962

2200

10

Yabello

Oromiya

1978

1500

11

AbijataShala

Oromiya

1963

887

12

Arsi Mountains

Oromiya

2012

 

13

Geralle

Somali

1998

3558

14

Gambella

Gambella

1966

4650

15

Nechsar

SNNPR

1966

514

16

Omo

SNNPR

1959

3566

17

Mago

SNNPR

1974

1947

18

Maze

SNNPR

1997

202

19

Gibe Sheleko

SNNPR

2001

248

20

Loka Abaya

SNNPR

2001

500

21

ChabraChurchura

SNNPR

1997

1190

Some of the national parks are unique in their wild animals they have. E.g.

  1. Abiyatta-Shalla lakes National Park is predominantly bird sanctuary. Important bird species include the flamingos and pelicans.
  2. Omo, Mago, and GambelaNational Parks have hippopotamus and crocodiles in rivers and lakes.
  3. Semienand Bale Mountains National Parks have rare animals like Walia ibex, Semien fox, gelada baboon and Nyala.

Challenges of wildlife conservation in Ethiopia

Do you know that if you leave nature to its own system, it has notable system of taking care of itself!

Conservation of Ethiopia‟s biodiversity and ecosystems is vital to ensure sustainable development, to mitigate and adapt to the effects of climate change and to prevent the collapse of life-supporting ecosystem services. Protected areas were created to protect the major biodiversity. However, it is a sad fact that these ecologically fundamental resources are usually undervalued and are under threat from various dimensions. Here are some of the major challenges that Ethiopian protected areas are facing;

 Limited awareness on the importance of wild life

 Expansion of human settlement in protected areas.

 Conflict over resource

 Overgrazing (fodder and wood)

 Illegal wildlife trade

 Excessive hunting

 Tourism and recreational pressure

 Mining and construction material extraction

 Forest fire

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