This document provides a comprehensive overview of rivers, including their definitions, sources, courses, and various components such as tributaries and deltas. It explains the processes of erosion, transportation, and deposition, detailing the features formed by rivers and their significance to humans, including both positive and negative effects. The document concludes with practice questions to assess understanding of the material.

1. UNIT.4. RIVERS AND TECTONIC PLATES
4.1. Definition of Rivers
River is a natural stream of flowing water in definite channel. Sometimes, it
is referred to large mass of water flowing in a specific valley.
The valley that river water flows from upstream toward the downstream is
also called river channel or River course.
The term River System is referred to the combination of main river with its
tributaries, its delta and its distributaries. River discharge is the volume of
water flowing through a river channel; measured at any given point in cubic
metres per second.

2. Rivers may begin from the following areas:
 Springs
 Lakes
 Glaciers and Snow
 Highlands areas which receive heavy and evenly distributed rainfalls.
Once a river forms, it will typically flow downhill. The movement the river
makes is its current, or its flow. The flow among rivers varies; the shortest (Roe
River) is 210 feet long, while the longest (Nile River) is over 4,000 miles long.
The point where a river starts its flow is known as river source while its
ending point is called river mouth. the land that surrounds the channel is the
riverbank. The flow of river from source to mouth is known as River Course.
The smaller river that joins into the main river is called Tributary.Tributary flows
into the bigger river at the river confluence. The smaller channels that split
from the big river are called Distributaries. The areas where distributaries
scattered as fingers at the fan shaped mouth or ending area is called River
Delta.

3. Source: the starting point of a river, the place from which a river flows.
Mouth: the ending point of a river, usually where it enters a sea or lake
Tributary: a small river that flows into the main river.
Confluence: the location where a tributary meets the main river.
Distributary: a small river that flows away from the main river.
Estuary: the section of the river near the mouth that is influenced by tides
Drainage basin: the area of land from which water will flow into a river system
Watershed: the imaginary line that separates two drainage basins.

4. 4.2. River Profile
A long profile is a line representing the river from its source (where it starts)
to its mouth (where it meets the sea). It shows how the river changes over its
course.

5. Upper course - in the upper course, where the river starts, there is often an
upland area. The river's load is large in the upper course, as it more erosive
area.
• middle course - The section of the river which comes between the upper
and lower course. It is usually wider than the upper course and the water flows
slowly. Tributary is a stream or river that flows into another stream or river
instead of flowing into the sea.
• Lower course - in the lower course, the land is a lot flatter. The river's load is
fine sediment, as erosion has broken down the rocks.

6. The upper course is marked by a V-shaped valley, with steep sides and a
shallow channel. The middle course is marked by gently sloping valley sides
and a wider and deeper channel. The lower course is a very wide, nearly flat
valley and usually has a wide, deep channel.
A. as the river flows downhill there is an increase in vertical erosion. The
channel is shallow and narrow because there is not a lot of water in the
channel.
B. As the river flows into the middle course, there is some vertical erosion but
more lateral erosion. The channel is wider and deeper as a result.
C. In the lower course there is a lot less erosion, with only some lateral
erosion. The channel is at its widest and deepest.

7. 4.2.1. Erosional processes
 Hydraulic action – Air trapped in the cracks of the river bed by the water
exerts pressure on the rock wall, causing it to break.
 Abrasion – Eroded rocks wear off the river channel.
 Attrition – Eroded rocks collide and rub together.
 Solution – Soluble components of the rocks are dissolved in the water (eg.
limestone, chalk)

8. 4.2.2.Transport processes
The river picks up sediment and carries it downstream in different ways. Light
loads are carried longer distance than heavy materials transferred from eroded
areas to the accumulation zone.
• Traction – Heavy boulders are rolled along the river bed
• Saltation – Small rocks are bounced along the river bed
• Suspension – Light particles (eg. sand grains) are transported in the water
• Solution – Dissolved particles are carried along by the river.
• Flotation – Light objects, eg. wood, float on the river surface

9. 4.2.3. Deposition
Deposition occurs when the river does not have enough speed to carry the load (eg.
delta, inner bends of meander or during dry spells). The velocity of a stream may slow
down due to a reduction in rainfall, increased evaporation and more friction with the river
bed.
4.3. Erosional and Depositional Features (Landforms)
Waterfalls, gorges and plunge pools
1. form in the upper course where hard rock is layered horizontally above soft rock
2. soft rock is less resistant to erosion and is worn away.
3. hard rock forms an overhang, creating a Knick point.
4. plunge pool develops at base of Knick point as force of water erodes soft rock.

10. 5) hard rock eventually unsupported by soft rock below,
causing the overhang to collapse.
6) plunge pool enlarges as hard rock erodes it.
7) waterfall retreats upstream and gorge may form

11. V-shaped valleys
V-shaped valleys typically form in the upper course of a river, where water
flows at high velocity and forcefully cuts into the surrounding mountains and
hills.
Potholes. Potholes are smooth, rounded hollows in the bedrock of the river.

12. 1. in the upper course
2. when flowing water encounters bedload (stones are trapped in hollows on the
river bed).
3. forced over bedload and down cuts behind it (eddie currents).
4. currents cause differential erosion (hydraulic action and abrasion).
5. small holes are formed and widened by currents.
6. deep vertical erosion lowers river bed
Rapids
1. form in the upper course
2. hard rock and soft rock layered diagonally (no obvious breaks of slope).
3. soft rock is less resistant, so it is eroded faster than hard rock.
4. hard rock remains, resulting in bumps along the river bed.

13. Meanders and oxbow lakes
Meanders are large bends common in the middle and lower courses of a river.
Deltas, Levees and Flood plains
Deltas form in the lower course, where the velocity decreases, resulting in the deposition of
sediment.

14. How floodplains form:
• river overflows at times of high discharge and spreads over surrounding flat land
• river velocity decreases, resulting in deposition
• flood plains build up with success floods over the years.
How levees form:
Levees may form in course material is deposited at the edge of the river channel and forms and
natural embankment.
4.4. Significance of Rivers to Man
Positive Effects of Rivers:
1. Rivers are both local and international boundaries demarcating between independent
countries or regions within the same state.
2. Some rivers are navigable which can be used for transporting loads, livestock and even
people from one location to another using small vessels.

15. 3. Rivers aid international trade facilitating movement and flow of supply of goods
from suppliers to their consumers who are in different locations.
4. The organic matters brought down by river waters provide valuable food for
fish and spawning purposes and even for industrial purposes.
5. Rivers provide natural ground or sites for the generation of hydroelectric
power.
6. Rivers provide building materials because deposited loads like clay and
gravels are used for construction purposes.
7. Rivers are sources of water used for irrigation, domestic use and even
industrial purpose.
8. Rivers are site provides us for recreational and entertainment centers like
swimming.
9. Rivers have some attractive scenes/ features like waterfalls and ox-bow lakes
which are tourists’ attractions.
10.Rivers are fishing grounds were many fishers caught species of fish for both
consumption or for sale.

16. Negative Effects of Rivers:
1. Soil erosion. River water leads soil erosion.
2. Rivers are hostages of snails and mosquitoes which can cause water
borne diseases like bilharzia and malaria respectively.
3. Rivers are habitats of dangerous wild animals like crocodiles and snakes.
4. Rivers can cause flooding which leads loss of life and properties.
Practice questions
1. List the three types of river erosion.
2. Define the terms: river, basin, Source, Mouth.
3. List and define the four processes of erosion.
4. What is the deposition?
5. State four processes of river transportation.