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Drainage systems and Water
Resource of Ethiopia and the Horn
Introduction
• About 71% of the earth's surface is
covered by water bodies majorly
occupied by seas and oceans.
• Of the Earth’s total water surface,
oNearly 97.5% is alkaline accumulated in seas
and oceans.
oThe remaining 2.5% is fresh water,
• 68.7% is deposited in glaciers,
• 30.1% in ground water,
• 0.8% in permafrost and
• 0.4% in surface waters
Introduction
• In Ethiopia
oThe diverse topographical setup
orelatively higher rainfall and
oits nearness to equator made the country to have larger volume of ground and
surface water.
• Around 0.7 % of the total land mass of Ethiopia is covered by water
bodies.
• The country’s surface water potential as studied in different
integrated river basin master plans is estimated to be 124.4 billion
cubic meters (BCM).
• Consequently, many call Ethiopia, the water tower of “Eastern
Africa”.
Activity
Form a group of three to four students and
Define the following terms
• Drainage
• Drainage system
• Drainage pattern
• Catchment area/ basin
• Watershed
Answer for the Activity
• Drainage
o is flow of water through well-defined channel.
• Drainage system
o is branched network of stream channels together with the adjacent
land slopes they drain.
• Drainage basin (Catchment area)
o is the topographic region from which a river and its tributaries collect
both the surface runoff and subsurface flow.
• Drainage pattern:
o is the arrangement and shapes of rivers with their tributaries
• Watershed
o is the highland that separates two basins.
Drainage System of Ethiopia
The general patterns of major river
basins in Ethiopia are determined
by
• The topography of the outward sloping of
the Western and South eastern plateaus
• The structural formation of the Rift Valley
with its in-ward-sloping escarpments
resulting mainly in an inland drainage
system.
• Faults and joints that structurally influence
part of the courses of many rivers.
The Major Drainage
Systems of Ethiopia
The Southeastern
Drainage Systems
The Western
Drainage Systems
The Rift Valley
Drainage System
Drainage System of Ethiopia
• The Western Drainage Systems are the largest of
all drainage systems draining 40 percent of the
total area of the country and carry 60 percent of
the annual water flow.
• This drainage system comprises four major river
basins:
• Tekeze (major tributers are (Angereb and Goang)
(12%),
• Abay (65%), Baro-Akobo (17%), Ghibe (Omo)
(6%).
• Omo /Ghibe/ - flows to south (exceptional)
• Tekeze, Abay, Baro-Akobo= Join the Nile and finally
to Mediterranean Sea
• The name of some rivers be changed after crossing
international boundary.
Western Drainage System
Drainage System of Ethiopia
• The basin which is mainly drained by Wabi-
shebelle and Ghenale, slopes south-eastwards
across large water deficient plains.
• Major highlands of this basin include plateaus
of Arsi, Bale, Sidama and Harerghe.
• Wabshebelle and Ghenale rivers cross the
border into Somalia, carrying 25 percent of the
annual water flow of Ethiopia.
• Ghenalle has fewer tributaries but carries more
water than Wabi-shebelle, reaches the Indian
Ocean.
• In Somalia, Ghenalle is named the Juba River.
The Southeastern Drainage Systems
Drainage System of Ethiopia
• is an area of small amount of rainfall, high
evaporation and small catchment area.
• The size of the drainage area is restricted
by the outward sloping highlands, which
starts right from the edge of the
escarpment.
• The Rift Valley drainage system is therefore
left with the slopes of the escarpment and
the Rift Valley floor itself as the catchment
area.
• The only major river basin is that of the
Awash.
The Rift Valley Drainage System
The Ethiopian Rivers
• Ethiopia is endowed with
many rivers.
• Majority of the rivers
originate from highland
areas and cross the
Ethiopian boundary.
• Altogether, Ethiopian rivers
form 12 major watersheds
separating the
Mediterranean Sea from the
Indian Ocean drainage
systems.
The Ethiopian Rivers
Rivers
Catchm
entAre
a (km2)
Length of Rivers (km)
Major tributaries
Total Inside Outside
Abay
198508 1360 800 560
Dabus, Dedessa, Fincha,
Guder, Muger, Jema, Beshilo
Wabi
shebelle
205407 2000 1340 660
Ramis Erer, Daketa, Fafan
Ghenale 168141 1050 480 370 Dawa, Weyb, Welmel, Mena
Awash 113709 1200 1200 0 Akaki, Kesem, Borena, Mile
Tekeze 87733 1168 608 560 Tirari (Atbara, Angereb)
Ghibe (Omo) 77205 760 760 0 Gojeb
Baro 75718 507 227 280 Akobo
The Ethiopian Rivers
General Characteristics of Ethiopian Rivers
• Major rivers originate from
the highlands elevating more
than 1500 meters above
sea level,
• Majority of Ethiopian rivers
are trans-boundary.
• Due to the marked
seasonality of rainfall, they
show seasonal
fluctuation
• Due to surface ruggedness
they have rapids and
waterfalls along their
course
General Characteristics of Ethiopian Rivers
• They have cuts, steep-
sided river valleys and
deep gorges along their
courses,
• Rivers in Ethiopia flow on
steep slopes having
steep profiles.
• Some of the rivers serve
as boundaries, both
international and domestic
administrative units.
The Ethiopian Lakes
• Relatively Ethiopia is rich in lakes.
• Almost all Ethiopian lakes are result
of tectonic process that took place
during Quaternary period of
Cenozoic era.
• Except few Ethiopian lakes, majority
of lakes are located within the Rift
Valley System.
• The lakes in the drainage are mainly
formed on faulted depressions and
are clustered along the system
forming linear pattern.
The Ethiopian Lakes
Lake Area(sq.
km)
Max Depth
(m)
Remark
Tana 3600 9 Largest lake
Abaya 1150 13 Second largest and the largest of all RV lakes
Chamo 551 10 The third largest and the second largest of all RV
lakes
Ziway 434 4 The fourth largest and shallowest lake in Ethiopia
Shala 409 266 The deepest lake in Ethiopia
Koka 205 9 Artificial Lake on Awash river
Kabgabi 230 46
Abiyata 205 14
Hawasa 229 10
Ashenge 20 25
Hayk 5 23
Subsurface (Ground) Water Resource of Ethiopia
• As compared to surface water resources, Ethiopia has lower
ground water potential.
• However, there exists higher total exploitable groundwater potential.
• Climatic and geophysical conditions determine the availability of
groundwater resource.
• Based on existing scanty knowledge, the groundwater potential of
Ethiopia is estimated to be 2.6 - 6.5 BMC.
• However, this estimate is now considered underestimated.
• Considering various separate studies, Ethiopian potential of
groundwater is believed to range between 12-30 BMC.
Importance of Ethiopian rivers and Lakes
Hydroelectric power potential
• Ethiopian rivers have a very high potential for generating electricity.
Irrigation and transportation
• The terrain in Ethiopia is so rugged that it limits the uses of Ethiopian rivers
both for irrigation and transportation.
• In the highlands, steep slopes, rapids, waterfalls, narrow and deep valleys and
gorges are important obstacles.
• But on the lowlands, their demand for irrigation is high.
• The Baro at its lower course is the only navigable river.
• Comparatively, Ethiopian lakes are much suitable for transportation than rivers.
• Lake Tana and Abaya are relatively the most used for transportation
Importance of Ethiopian rivers and Lakes
Fishing and Recreation
• Ethiopian lakes are rich in fish. Currently the
annual production of fish is estimated to be 31.5
thousand tons
• More than 60% of fish supplies are coming from
Ethiopian main Rift Valley lakes
• scenic beauty of the lakes, the hot springs
around them, the spectacular river gorges and
the most impressive waterfalls make Ethiopian
rivers and lakes important recreational and
tourist attractions

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geography chapter 4.pdf

  • 1. Drainage systems and Water Resource of Ethiopia and the Horn
  • 2. Introduction • About 71% of the earth's surface is covered by water bodies majorly occupied by seas and oceans. • Of the Earth’s total water surface, oNearly 97.5% is alkaline accumulated in seas and oceans. oThe remaining 2.5% is fresh water, • 68.7% is deposited in glaciers, • 30.1% in ground water, • 0.8% in permafrost and • 0.4% in surface waters
  • 3. Introduction • In Ethiopia oThe diverse topographical setup orelatively higher rainfall and oits nearness to equator made the country to have larger volume of ground and surface water. • Around 0.7 % of the total land mass of Ethiopia is covered by water bodies. • The country’s surface water potential as studied in different integrated river basin master plans is estimated to be 124.4 billion cubic meters (BCM). • Consequently, many call Ethiopia, the water tower of “Eastern Africa”.
  • 4. Activity Form a group of three to four students and Define the following terms • Drainage • Drainage system • Drainage pattern • Catchment area/ basin • Watershed
  • 5. Answer for the Activity • Drainage o is flow of water through well-defined channel. • Drainage system o is branched network of stream channels together with the adjacent land slopes they drain. • Drainage basin (Catchment area) o is the topographic region from which a river and its tributaries collect both the surface runoff and subsurface flow. • Drainage pattern: o is the arrangement and shapes of rivers with their tributaries • Watershed o is the highland that separates two basins.
  • 6. Drainage System of Ethiopia The general patterns of major river basins in Ethiopia are determined by • The topography of the outward sloping of the Western and South eastern plateaus • The structural formation of the Rift Valley with its in-ward-sloping escarpments resulting mainly in an inland drainage system. • Faults and joints that structurally influence part of the courses of many rivers. The Major Drainage Systems of Ethiopia The Southeastern Drainage Systems The Western Drainage Systems The Rift Valley Drainage System
  • 7. Drainage System of Ethiopia • The Western Drainage Systems are the largest of all drainage systems draining 40 percent of the total area of the country and carry 60 percent of the annual water flow. • This drainage system comprises four major river basins: • Tekeze (major tributers are (Angereb and Goang) (12%), • Abay (65%), Baro-Akobo (17%), Ghibe (Omo) (6%). • Omo /Ghibe/ - flows to south (exceptional) • Tekeze, Abay, Baro-Akobo= Join the Nile and finally to Mediterranean Sea • The name of some rivers be changed after crossing international boundary. Western Drainage System
  • 8.
  • 9. Drainage System of Ethiopia • The basin which is mainly drained by Wabi- shebelle and Ghenale, slopes south-eastwards across large water deficient plains. • Major highlands of this basin include plateaus of Arsi, Bale, Sidama and Harerghe. • Wabshebelle and Ghenale rivers cross the border into Somalia, carrying 25 percent of the annual water flow of Ethiopia. • Ghenalle has fewer tributaries but carries more water than Wabi-shebelle, reaches the Indian Ocean. • In Somalia, Ghenalle is named the Juba River. The Southeastern Drainage Systems
  • 10.
  • 11. Drainage System of Ethiopia • is an area of small amount of rainfall, high evaporation and small catchment area. • The size of the drainage area is restricted by the outward sloping highlands, which starts right from the edge of the escarpment. • The Rift Valley drainage system is therefore left with the slopes of the escarpment and the Rift Valley floor itself as the catchment area. • The only major river basin is that of the Awash. The Rift Valley Drainage System
  • 12. The Ethiopian Rivers • Ethiopia is endowed with many rivers. • Majority of the rivers originate from highland areas and cross the Ethiopian boundary. • Altogether, Ethiopian rivers form 12 major watersheds separating the Mediterranean Sea from the Indian Ocean drainage systems.
  • 13. The Ethiopian Rivers Rivers Catchm entAre a (km2) Length of Rivers (km) Major tributaries Total Inside Outside Abay 198508 1360 800 560 Dabus, Dedessa, Fincha, Guder, Muger, Jema, Beshilo Wabi shebelle 205407 2000 1340 660 Ramis Erer, Daketa, Fafan Ghenale 168141 1050 480 370 Dawa, Weyb, Welmel, Mena Awash 113709 1200 1200 0 Akaki, Kesem, Borena, Mile Tekeze 87733 1168 608 560 Tirari (Atbara, Angereb) Ghibe (Omo) 77205 760 760 0 Gojeb Baro 75718 507 227 280 Akobo
  • 15. General Characteristics of Ethiopian Rivers • Major rivers originate from the highlands elevating more than 1500 meters above sea level, • Majority of Ethiopian rivers are trans-boundary. • Due to the marked seasonality of rainfall, they show seasonal fluctuation • Due to surface ruggedness they have rapids and waterfalls along their course
  • 16. General Characteristics of Ethiopian Rivers • They have cuts, steep- sided river valleys and deep gorges along their courses, • Rivers in Ethiopia flow on steep slopes having steep profiles. • Some of the rivers serve as boundaries, both international and domestic administrative units.
  • 17. The Ethiopian Lakes • Relatively Ethiopia is rich in lakes. • Almost all Ethiopian lakes are result of tectonic process that took place during Quaternary period of Cenozoic era. • Except few Ethiopian lakes, majority of lakes are located within the Rift Valley System. • The lakes in the drainage are mainly formed on faulted depressions and are clustered along the system forming linear pattern.
  • 18. The Ethiopian Lakes Lake Area(sq. km) Max Depth (m) Remark Tana 3600 9 Largest lake Abaya 1150 13 Second largest and the largest of all RV lakes Chamo 551 10 The third largest and the second largest of all RV lakes Ziway 434 4 The fourth largest and shallowest lake in Ethiopia Shala 409 266 The deepest lake in Ethiopia Koka 205 9 Artificial Lake on Awash river Kabgabi 230 46 Abiyata 205 14 Hawasa 229 10 Ashenge 20 25 Hayk 5 23
  • 19. Subsurface (Ground) Water Resource of Ethiopia • As compared to surface water resources, Ethiopia has lower ground water potential. • However, there exists higher total exploitable groundwater potential. • Climatic and geophysical conditions determine the availability of groundwater resource. • Based on existing scanty knowledge, the groundwater potential of Ethiopia is estimated to be 2.6 - 6.5 BMC. • However, this estimate is now considered underestimated. • Considering various separate studies, Ethiopian potential of groundwater is believed to range between 12-30 BMC.
  • 20. Importance of Ethiopian rivers and Lakes Hydroelectric power potential • Ethiopian rivers have a very high potential for generating electricity. Irrigation and transportation • The terrain in Ethiopia is so rugged that it limits the uses of Ethiopian rivers both for irrigation and transportation. • In the highlands, steep slopes, rapids, waterfalls, narrow and deep valleys and gorges are important obstacles. • But on the lowlands, their demand for irrigation is high. • The Baro at its lower course is the only navigable river. • Comparatively, Ethiopian lakes are much suitable for transportation than rivers. • Lake Tana and Abaya are relatively the most used for transportation
  • 21. Importance of Ethiopian rivers and Lakes Fishing and Recreation • Ethiopian lakes are rich in fish. Currently the annual production of fish is estimated to be 31.5 thousand tons • More than 60% of fish supplies are coming from Ethiopian main Rift Valley lakes • scenic beauty of the lakes, the hot springs around them, the spectacular river gorges and the most impressive waterfalls make Ethiopian rivers and lakes important recreational and tourist attractions