THE MAJOR FEATURES OF THE EARTH’S SURFACE
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THE MAJOR FEATURES OF THE EARTH’S SURFACE
The
surface of the earth is made up of two main features: 1. Land and 2. Water bodies.
The land surface is estimated at 29.2% of the total area of the
earth’s surface while water covers the remaining 70.2%. The most of the land exists in large block
called continents; likewise, the most of the water is contained in
large water bodies called seas and oceans.
Definitions
of Some Terms:
Canal is the
small mass of land joining two continents. (e.g. sues canal). Gulf is the water inlet to the land (e.g.
gulf of guinea, Mexico and Banguela). Strait is the narrow water path that
separates one land mass from another (e.g. Gibraltar in morocco, Makasan in
Indonesia). Peninsula is a part
of land entering in a body of water (e.g. Msasani in Tanzania and Indian
peninsula). Cape is piece of land
getting in the sea (e.g. Cape of Good Hope in South Africa, Cape Verde, and
Palmas).
A.
CONTINENTS
By
definition, continent refers to a major landmass rising from the ocean
floor.
Continent is surrounded by water bodies. Continents rise from ocean
floors. There are seven continents on the earth’s surface. These are:
1)
Africa
2)
Asia
3)
Australia
4)
Europe
5)
Antarctica
6)
South America
7)
North America
Most
of the continents are joined together by small mass of land, like Suez Canal,
that connects Africa and Asia, Panama Isthmus join North America and South
America. The Northern hemisphere is
covered by more land surface whereas southern hemisphere occupies small part of
it.
All
continents originated from the drifting apart of one Sialic known as Pangaea
over million years ago. See the figure below:
Asia
Asia
is the largest continent in the world covering more than one third of the
earth’s surface. The continent has total areas of 43.6 million kilometer square
and lies from 00 to 670N and 300E about 1800E.
Africa
Africa
is the second largest continent in the world, covers 30.3 million km2.
It Lies from 350N and 370N to 1600W.
North America
It
is the third largest continent, which covers 25.3 Million Km2. It
extends from 100N to 650N and from 600W to 1600W.
South America:
It
is the fourth largest continent that covers about 17.6 million kilometer square
extending from 100N and 500S and between 350W
and 800W.
Antarctica
It
lies within latitude 660S covering the area of about 13.3 million km2.
Antarctica is the fifth largest continent in size and therefore it is the only
the uninhibited continent.
Europe
Europe
is the sixth largest continent in size that separated from Asia by Ural
Mountain to East side. Its total area is about 10.5 million kilometer square.
Australia
It
is the smallest continent in size. Its total area is about 7.7 million
kilometer square. The following table
shows the size of continents:
Continent
|
Area (Km2)
|
Asia
|
43, 608, 000
|
Africa
|
30, 335, 000
|
North America
|
25, 349, 000
|
South America
|
17, 611, 000
|
Antarctica
|
13, 340, 000
|
Europe
|
10, 498, 000
|
Australia
|
7, 682, 000
|
The
Major Feature of the Continents:
The
surface of any continent is not smooth due to the agents of denudation and
deposition. Features (relief features) are hills, mountains, rift valley,
plains, plateaus and basins. Mountains, plains and plateaus forms the major
relief features of the continents.
1.
Plains
Plain
is an undulating land usually near to the sea level. Plains are large and
nearly flat stretch of land that usually has no great change in its height.
Plains are characterized by very gentle slopes and wide valleys. Such plain are
described as rolling or undulating plains and Serengeti Plain is
an example of such plain that found in Tanzania. Many plains are found in
coastal areas of the continents, which are called coastal plains. Many of plains are caused by down warping of the
earth’s crust. North Europe plain, Siberia plain, and the great central pain of
America are example of the plain.
2.
Plateaus
Plateaus
are extensive high altitude areas with more or less uniform summit levels.
Plateaus are described as table-lands.
Most of plateaus are resulted due to the warping of the earth‘s crust that
caused by uplifting of some areas. Plateaus that are covered by thick layers of
volcanic lava are called lava-plateaus.
Brasilia highland, central plateau of Africa, Colombia plateau, Decan plateau
of India and Ethiopian plateau are examples of the plateaus.
3.
Mountains
Mountain
is the highland areas rising above mean sea level. There are various types of
mountains formed depending to their mode of formation. There are major four types
of mountains that named according to their mode of formation:
a)
Fold Mountains
b)
Block Mountains
c)
Volcanic Mountains
d)
Residual Mountains
(a) Volcanic
Mountains
Volcanic
mountains are mountains formed from the pilling up and cooling of molten lava
and ashes that are thrown out from the earth’s interior after volcanic
eruption. Most of the volcanic mountains contains craters at their peaks and
are conical in shape. Crater can be filled with water to form lake like
Ngorongoro in Arusha. There are major three classifications of volcanic
mountains:
1.
Active volcanoes: are volcanic
mountains which still experiencing periodic eruptions and erupted in the recent
periods. Mount Vesuvius and Stromboli in Italy, mount Mauna Loa in Hawaii,
Krakatau in Indonesia, Mufumbiro in Uganda, Oldonyolengai in Tanzania are
examples of active volcanoes.
2.
Dormant volcanoes: are those mountains which have erupted
once in the past but have remained inactive for fairly long period. These are
called sleeping volcanoes which
become active once again. Examples of dormant volcanoes are Kilimanjaro
Mountain and Meru Mountain in Tanzania.
3.
Extinct (dead) volcanoes: are those mountains which were active
but not erupted for a very long time and have not shown any sign of erupting
again. Elgon, Ngorongoro, Kenya and Rungwe in East Africa are examples of dead
volcanoes.
(b) Fold
Mountains
Fold
Mountains are formed by wrinkling of the earth’s crust caused by compressional
forces. In them, they occur when sedimentary rocks are laid in horizontal
layers which were later folded by compressional forces. Most of the ranges in the world are formed by
fold Mountains, like cape ranges in South Africa, Mount Everest of Himalaya,
Atlas, Alps, Appalachians in U.S.A and the great divided ranges of Australia.
The anticline is the up fold and syncline is the down fold
of the fold mountain.
(c)
Block Mountains (Horst)
Block
Mountain is an upland bordered by faults on one or more sides. Block Mountain
formed due to being raised or tilted up by the earth movement along faults
bounded block. Block Mountain does not cover large area like fold mountain.
Examples of Block Mountain are mountain Sinai in Asia, Ruwenzori in Tanzania.
Block Mountains are associated with rift valleys.
(d) Residual
Mountains
Residual
mountains are formed by prolonged denudations. Sekenke hills in Singida
Tanzania, Mesas and Buttes in US and Adamawa in Nigeria.
4 Rift Valleys (Grabens)
Rift
valley is an elongated trough or depression formed when two sets of faults sink
down. The Great East African rift valley is an example. Sometimes trenches are
filled with water to form lakes. The bottom of a valley is called is called floor and valley’s side are called valley-walls or valley-slopes.
5 Basins
Basin
is the natural or artificial depression varying in size on the Earth’s surface.
If basins are filled with or occupied by water, tend to form rivers or lakes
and ocean basin. Examples of basins are Lake Victoria, Congo basin, Kalahari
basin, Chad and Sudan basin.
6 Drainages
Drainage
refers to the situation by which, water are removed from an area. Streams and
rivers are responsible for draining the land surfaces. The processes of water
to flow on the ground are known as overland flow, and if water percolates into
the ground are called underground water. Surface
flow of water from rainfall or snow-melt over the ground is known as water runoff.
The
surface water from rainfall or snow-melt flows in small channels, which finally
join to form large trenches of rivers are called tributaries. Small streams that branches off before they enter the
sea or lake are known as distributaries.
The area from which a river system collects its rain water is called river/basin/catchment area/drainage basin.
The boundary between one catchment area and the next is formed by crest line of
the surrounding highland called watershed/water
divide/basin perimeter and the main river and its tributaries together
forms river system.
B.
WATER BODIES
Water
body is any significant accumulation of water such as ocean, lake, river and
other alike. Some water bodies are manmade (artificial). Navigable water bodies
are called water ways. There are more
water bodies in the southern hemisphere than the northern hemisphere.
1. Oceans
Ocean
is a large body of water that surrounds the landmasses of the earth. Ocean
covers almost 360 million kilometer square which is equal to 71%. The Pacific
Ocean is the ocean while Arctic Ocean is the smallest ocean.
Salinity
of ocean water depends on the temperature, amount of fresh water entering in
the ocean, nature of the rock of the ocean floor and additional of organic
materials. The following is the table that shows the five large oceans in the
world:
Ocean
|
Area (Km2)
|
Average Depth (M)
|
Pacific
|
155, 557, 000
|
4, 028
|
Atlantic
|
76, 762, 000
|
3, 926
|
Indian
|
68, 556, 000
|
3, 936
|
Southern
|
20, 327, 000
|
4, 000 to 5, 000
|
Arctic
|
14, 056, 000
|
1, 205
|
Types
of Water Movement In oceans
Water
moves in the oceans is into two main ways:
a) Horizontal movement: e.g.
tides and currents.
b) Vertical movement: e.g. Sinking and rising of water.
Ocean
currents: Ocean current is the movement of surface water. There are
two types of ocean currents: Warm ocean
currents: these are ocean currents formed by masses of warm water e.g.
Mozambique, Brazilia ocean currents. And the second is cold or cool ocean currents:
these are ocean currents that formed by masses of cold water e.g. California,
Benguela, and West Australia ocean currents.
Tides:
Tides are periodic rise and fall in the level of water in
the oceans and sea. Tides occur twice a day (in 24 hours). Tides are caused by
the sun and to a greater exert the moon exerts a gravitational attraction on
the earth’s surface.
Waves:
Waves are the up and down movements of the surface water.
There are two parts of lakes, sea and ocean waves: Trough: is the lowest part of the wave and Crest: is the highest part of the wave.
The distance between one crest to another is called wavelength. Waves are caused by winds which drive them to the
shore. Wave travel in a defined direction, whereas water moves up and down.
2. Lakes
Lake
is a hollow in the earth earth’s surface in which water are collected in them.
Lakes which are in great size are called seas
like
Caspian Sea, Dead Sea and Aral Sea. Most of lakes are permanent, but
some are for temporary.
3. Seas
Sea
is an expense of salt water that covers most of the earth’s surface. Examples
of seas are North Sea, Mediterranean Sea, China Sea, red sea etc.
4. River
River
is anybody of fresh water flowing from an upland sources to a large lake or sea
fed by springs and tributary streams. River starts on hillsides as a small
channels or rills. Some examples of rivers are river Nile, river Amazon, yellow
river, and Rufiji River. Rivers have the
following parts: channel is in which water flows and flat region or food plain of valley on either sides of the channel.
Nature
of the Ocean Floor
Ocean
floor is not smooth in nature but it contains varied reliefs. The relief of the
ocean floor is as varied as that of the land surface; it is irregular in shape.
There are features on the ocean floor that we do not see because they covered
by water. The following are the main
features of the ocean floor:
1.
Continental shelf: Continental shelf is the gentle sloping
margin of a continent. The continental shelf is occupied by shallow water that
extends from the coast to a depth about 180 to 200m towards the ocean basin. It
is excellent for growth of plankton because shallow water allows sun rays to
reach its floor.
2.
Continental slope: Continental slope is the steep slope
that extends from the edge of the shelf to the deep sea plain. The continental
slope marks the edge of the continent at the beginning of the ocean basin.
3.
Ocean ridge: Ocean
ridge is the raised part of the ocean floor. It takes a form of ridge or
plateau on the ocean floor as a sea bed. Mid Atlantic ridge and the Abaltros
plateau are examples of ocean ridge which rise above the surface to form
oceanic island.
4.
Ocean trenches: Ocean trenches are long, narrow
depressions found on the ocean floors. The deepest known ocean trench is the
Marianas Trench near the island of Guam in the Pacific Ocean. It is deepest
part is 11911m below sea level.
5.
Deep sea plains: Ocean deep sea plain is wide gently
sloping surface with a depth of about 300m and 5500m. Deep sea plain is also
called abyssal plain.
6.
Continental islands: Island is a piece of land that is
completely surrounded by water. Very small islands are called islets or keys. The following are three types of islands: Oceanic islands: formed due to volcanic activities, Continental islands: lies on
continental shelf and Coral islands: formed
from coral rocks.
TRIAL
QUESTIONS
1. List down three sources of rivers.
2. Outline two movement of water in the large water bodies.
3. Giving example from each, mention two types of ocean
currents.
4. Describe major two relief features of the earth.
5. With the aid of sketch map of East Africa, indicate the
largest lakes.
6. Give the meaning of the following terminologies:
a)
Water divide
b)
Catchment area
c)
Underground flow
d)
Drainage
e)
Ocean deep
7. Differentiate between the following:
a)
Fold and block mountain
b)
Tributaries and distributaries
c)
Continental shelf and deep sea plain
d)
Tides and ocean currents
8. Write short notes about:
a)
Tides
b)
Waves
c)
Volcanic Mountain
d)
Valleys
e)
Islands.
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