GEOGRAPHY OBJ
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31-40: BCBBABDADD
41-50: CACCCAACBD
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*WAEC GEOGRAPHY PRACTICAL*
*NUMBER SIX*
(6a)
A flood plain is a flat, low-lying area of land found along the sides of a river, which is periodically flooded when the river overflows its banks. It is formed mainly by deposition of sediments during flooding.
(6b)
[DRAW THE DIAGRAM]
=CHARACTERISTICS OF A FLOOD PLAIN=
(i) Flood plains are usually broad, flat areas adjacent to a river channel.
(ii) The soil is often very fertile due to the regular deposition of nutrient-rich sediments during floods.
(iii) Flood plains experience periodic flooding when the river overflows its banks.
(iv) They often have meanders (curves or bends) in the river channel.
(v) The area supports lush vegetation because of the availability of water and fertile soil.
(vi) The surface is composed of fine alluvial deposits like silt, clay, and sand.
(vii) Raised banks or levees may form along the edges of the river channel from sediment deposits.
=MODE OF FORMATION OF A FLOOD PLAIN=
(i) When a river exceeds its bank capacity, water spills onto the surrounding land, causing flooding.
(ii) As the floodwater spreads out over the flat land, it slows down and deposits sediments carried from upstream.
(iii) Over many floods, layers of silt, clay, and fine sand accumulate, building up the flood plain.
(iv) The river’s sideways erosion widens the valley floor, contributing to the flood plain’s flatness.
(v) Coarser sediments settle first near the river banks during floods, forming natural levees.
(vi) The flood plain gradually extends as more sediments are deposited with each flood event.
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*NUMBER SIX*
(6a)
A flood plain is a flat, low-lying area of land found along the sides of a river, which is periodically flooded when the river overflows its banks. It is formed mainly by deposition of sediments during flooding.
(6b)
[DRAW THE DIAGRAM]
=CHARACTERISTICS OF A FLOOD PLAIN=
(i) Flood plains are usually broad, flat areas adjacent to a river channel.
(ii) The soil is often very fertile due to the regular deposition of nutrient-rich sediments during floods.
(iii) Flood plains experience periodic flooding when the river overflows its banks.
(iv) They often have meanders (curves or bends) in the river channel.
(v) The area supports lush vegetation because of the availability of water and fertile soil.
(vi) The surface is composed of fine alluvial deposits like silt, clay, and sand.
(vii) Raised banks or levees may form along the edges of the river channel from sediment deposits.
=MODE OF FORMATION OF A FLOOD PLAIN=
(i) When a river exceeds its bank capacity, water spills onto the surrounding land, causing flooding.
(ii) As the floodwater spreads out over the flat land, it slows down and deposits sediments carried from upstream.
(iii) Over many floods, layers of silt, clay, and fine sand accumulate, building up the flood plain.
(iv) The river’s sideways erosion widens the valley floor, contributing to the flood plain’s flatness.
(v) Coarser sediments settle first near the river banks during floods, forming natural levees.
(vi) The flood plain gradually extends as more sediments are deposited with each flood event.
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*PRACTICAL GEOGRAPHY*
*NUMBER SEVEN*
(7a)
PICK ANY THREE
(I) Deflation: The removal of loose particles from the ground surface by wind action.
(ii) Abrasion: The wearing away of surfaces by wind-driven particles.
(iii) Saltation: The bouncing of particles on the ground surface due to wind impact.
(iv) Suspension: The carrying of fine particles in the air by wind.
(v) Creep: The slow downhill movement of larger particles on the ground surface due to wind action.
(7bi)
PICK ANY THREE
(i) Both are landforms created by wind erosion.
(ii) Both have a streamlined shape due to the erosive action of wind.
(iii) Both are found in arid and semi-arid regions.
(iv) Both are formed by the removal of sediments by wind erosion.
(v) Both have a desert-like landscape.
(7bii)
PICK ANY THREE
(I) A zeugen is a small, isolated, streamlined hill, while a yardang is a larger, elongated, streamlined hill.
(ii) A zeugen has a more rounded shape, while a yardang has a more pointed or sharp shape.
(iii) A zeugen is formed by the deposition of wind-blown sediments, while a yardang is formed by the removal of sediments by wind erosion.
(iv) A zeugen is typically found in areas with strong winds and limited vegetation, while a yardang is found in areas with strong winds and more vegetation.
(v) A zeugen is usually less than 100 meters high, while a yardang can be several hundred meters high.
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*NUMBER SEVEN*
(7a)
PICK ANY THREE
(I) Deflation: The removal of loose particles from the ground surface by wind action.
(ii) Abrasion: The wearing away of surfaces by wind-driven particles.
(iii) Saltation: The bouncing of particles on the ground surface due to wind impact.
(iv) Suspension: The carrying of fine particles in the air by wind.
(v) Creep: The slow downhill movement of larger particles on the ground surface due to wind action.
(7bi)
PICK ANY THREE
(i) Both are landforms created by wind erosion.
(ii) Both have a streamlined shape due to the erosive action of wind.
(iii) Both are found in arid and semi-arid regions.
(iv) Both are formed by the removal of sediments by wind erosion.
(v) Both have a desert-like landscape.
(7bii)
PICK ANY THREE
(I) A zeugen is a small, isolated, streamlined hill, while a yardang is a larger, elongated, streamlined hill.
(ii) A zeugen has a more rounded shape, while a yardang has a more pointed or sharp shape.
(iii) A zeugen is formed by the deposition of wind-blown sediments, while a yardang is formed by the removal of sediments by wind erosion.
(iv) A zeugen is typically found in areas with strong winds and limited vegetation, while a yardang is found in areas with strong winds and more vegetation.
(v) A zeugen is usually less than 100 meters high, while a yardang can be several hundred meters high.
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WAEC PRACTICAL GEOGRAPHY ANSWER
*NUMBER FOUR*
(4a) An artesian well is a well drilled into a confined aquifer where water rises to the surface naturally due to pressure without the need for pumping.
(4b)
(PICK ANY FOUR)
(i) Presence of a confined aquifer: This is a water-bearing layer of permeable rock or sediment that is sandwiched between two layers of impermeable rock, which traps the water under pressure.
(ii) Inclined aquifer structure: The aquifer must be tilted so that water can enter at a higher elevation and flow down to where the well is drilled, creating the necessary pressure.
(iii) Recharge area at a higher elevation: Water must be able to enter the aquifer at a location above the point where the well is drilled, increasing pressure due to gravity.
(iv) Impermeable layers above and below the aquifer: These layers prevent water from escaping, allowing pressure to build up within the confined aquifer.
(v) Adequate water supply: There must be consistent rainfall or surface water sources feeding into the recharge area to maintain pressure in the aquifer.
(vi) Proper drilling into the confined aquifer: The well must penetrate the pressurized aquifer correctly to allow the water to rise naturally to the surface without the need for pumping.
(4c)
(PICK ANY TWO)
(i) Provides a reliable water supply: Artesian wells offer a consistent source of clean groundwater, especially in areas where surface water is scarce or unreliable.
(ii) Requires no pumping in some cases: Because of the natural pressure in the confined aquifer, water can flow to the surface without the need for mechanical pumps, saving energy and maintenance costs.
(iii) Supplies water for irrigation: Farmers can use artesian wells to irrigate crops, especially in dry regions where rainfall is insufficient.
(iv) Supports domestic and industrial use: The water from artesian wells can be used for drinking, cooking, cleaning, and even for industries that need large quantities of water.
(v) Less prone to contamination: Since the aquifer is confined between impermeable layers, the water is better protected from surface pollutants, making it safer for human use.
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*NUMBER FOUR*
(4a) An artesian well is a well drilled into a confined aquifer where water rises to the surface naturally due to pressure without the need for pumping.
(4b)
(PICK ANY FOUR)
(i) Presence of a confined aquifer: This is a water-bearing layer of permeable rock or sediment that is sandwiched between two layers of impermeable rock, which traps the water under pressure.
(ii) Inclined aquifer structure: The aquifer must be tilted so that water can enter at a higher elevation and flow down to where the well is drilled, creating the necessary pressure.
(iii) Recharge area at a higher elevation: Water must be able to enter the aquifer at a location above the point where the well is drilled, increasing pressure due to gravity.
(iv) Impermeable layers above and below the aquifer: These layers prevent water from escaping, allowing pressure to build up within the confined aquifer.
(v) Adequate water supply: There must be consistent rainfall or surface water sources feeding into the recharge area to maintain pressure in the aquifer.
(vi) Proper drilling into the confined aquifer: The well must penetrate the pressurized aquifer correctly to allow the water to rise naturally to the surface without the need for pumping.
(4c)
(PICK ANY TWO)
(i) Provides a reliable water supply: Artesian wells offer a consistent source of clean groundwater, especially in areas where surface water is scarce or unreliable.
(ii) Requires no pumping in some cases: Because of the natural pressure in the confined aquifer, water can flow to the surface without the need for mechanical pumps, saving energy and maintenance costs.
(iii) Supplies water for irrigation: Farmers can use artesian wells to irrigate crops, especially in dry regions where rainfall is insufficient.
(iv) Supports domestic and industrial use: The water from artesian wells can be used for drinking, cooking, cleaning, and even for industries that need large quantities of water.
(v) Less prone to contamination: Since the aquifer is confined between impermeable layers, the water is better protected from surface pollutants, making it safer for human use.
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(3a)
A lithosphere is the solid outer layer of the Earth, consisting of the crust and the uppermost part of the mantle. It is rigid and forms the Earth's landforms, such as mountains, valleys, and ocean basins.
(3b)
(PICK ANY THREE)
(i) It is the outermost solid layer of the Earth.
(ii) It includes both the crust and the upper part of the mantle.
(iii) It is rigid and brittle in nature.
(iv) It is broken into tectonic plates that move over the asthenosphere.
(v) It contains both continental and oceanic crust.
(vi) It plays a role in the formation of landforms through geological processes like folding and faulting.
(3c)
(PICK ANY FIVE)
(i) Source of minerals: The lithosphere contains valuable minerals like gold, iron, and copper used in industries.
(ii) Supports agriculture: It provides soil which is essential for growing crops and feeding livestock.
(iii) Habitat for living things: Humans, animals, and plants live on the land provided by the lithosphere.
(iv) Foundation for infrastructure: Buildings, roads, bridges, and other structures are built on the lithosphere.
(v) Source of fossil fuels: Resources like coal, oil, and natural gas used for energy come from the lithosphere.
(vi) Controls geological activities: Processes like earthquakes and volcanic eruptions originate in the lithosphere.
(vii) Supplies raw materials: Materials like clay, sand, and limestone used for making cement and glass come from it.
(viii) Supports scientific study: Rocks and fossils found in the lithosphere help scientists understand Earth's history.
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A lithosphere is the solid outer layer of the Earth, consisting of the crust and the uppermost part of the mantle. It is rigid and forms the Earth's landforms, such as mountains, valleys, and ocean basins.
(3b)
(PICK ANY THREE)
(i) It is the outermost solid layer of the Earth.
(ii) It includes both the crust and the upper part of the mantle.
(iii) It is rigid and brittle in nature.
(iv) It is broken into tectonic plates that move over the asthenosphere.
(v) It contains both continental and oceanic crust.
(vi) It plays a role in the formation of landforms through geological processes like folding and faulting.
(3c)
(PICK ANY FIVE)
(i) Source of minerals: The lithosphere contains valuable minerals like gold, iron, and copper used in industries.
(ii) Supports agriculture: It provides soil which is essential for growing crops and feeding livestock.
(iii) Habitat for living things: Humans, animals, and plants live on the land provided by the lithosphere.
(iv) Foundation for infrastructure: Buildings, roads, bridges, and other structures are built on the lithosphere.
(v) Source of fossil fuels: Resources like coal, oil, and natural gas used for energy come from the lithosphere.
(vi) Controls geological activities: Processes like earthquakes and volcanic eruptions originate in the lithosphere.
(vii) Supplies raw materials: Materials like clay, sand, and limestone used for making cement and glass come from it.
(viii) Supports scientific study: Rocks and fossils found in the lithosphere help scientists understand Earth's history.
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The GEOGRAPHY practical is 2pm
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*WAEC GEOGRAPHY PRACTICAL*
*NUMBER SIX*
(6b)
=CHARACTERISTICS OF A FLOOD PLAIN=
(i) Flood plains are usually broad, flat areas adjacent to a river channel.
(ii) The soil is often very fertile due to the regular deposition of nutrient-rich sediments during floods.
(iii) Flood plains experience periodic flooding when the river overflows its banks.
(iv) They often have meanders (curves or bends) in the river channel.
(v) The area supports lush vegetation because of the availability of water and fertile soil.
(vi) The surface is composed of fine alluvial deposits like silt, clay, and sand.
(vii) Raised banks or levees may form along the edges of the river channel from sediment deposits.
=MODE OF FORMATION OF A FLOOD PLAIN=
(i) When a river exceeds its bank capacity, water spills onto the surrounding land, causing flooding.
(ii) As the floodwater spreads out over the flat land, it slows down and deposits sediments carried from upstream.
(iii) Over many floods, layers of silt, clay, and fine sand accumulate
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*NUMBER SIX*
(6b)
=CHARACTERISTICS OF A FLOOD PLAIN=
(i) Flood plains are usually broad, flat areas adjacent to a river channel.
(ii) The soil is often very fertile due to the regular deposition of nutrient-rich sediments during floods.
(iii) Flood plains experience periodic flooding when the river overflows its banks.
(iv) They often have meanders (curves or bends) in the river channel.
(v) The area supports lush vegetation because of the availability of water and fertile soil.
(vi) The surface is composed of fine alluvial deposits like silt, clay, and sand.
(vii) Raised banks or levees may form along the edges of the river channel from sediment deposits.
=MODE OF FORMATION OF A FLOOD PLAIN=
(i) When a river exceeds its bank capacity, water spills onto the surrounding land, causing flooding.
(ii) As the floodwater spreads out over the flat land, it slows down and deposits sediments carried from upstream.
(iii) Over many floods, layers of silt, clay, and fine sand accumulate
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The GEOGRAPHY practical is 2pm
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MATHEMATICS #1500
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MATHEMATICS #1500
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