General Awareness Landforms

Landforms

1. One – fourth of the earth’s surface is covered by land and the portion which forms land on earth’s surface is not the same everywhere. At some places the land may be too high, at some places very low, some areas would be lush green and certain areas are dry and barren.

2. Our planet earth is a beautiful collaboration of various physical features. These different physical features are called the various landforms on the surface of the earth.

3. These are geographical features that control the ecosystem, climate, weather and the essence of life on earth. In simple terms, we say that any shape on the earth’s surface is known as a landform.

4. The various landforms that we have, came into existence due to natural processes such as erosion, wind, rain, weather conditions such as ice, frost and chemical actions.

5. Natural events and disasters such as earthquakes (the tectonic plates) and eruption of volcanoes created the various shapes of the land that we see.

6. The different major landforms are mountains, hills, valleys, plateaus, plains and deserts.

Mountains

1. A mountain is the highest landform on the surface of the earth.

2. It is usually found to be conical in shape with steep sides and a pointed tip called a peak.

3. As compared to their surroundings, mountains are high points on the surface of the earth.

4. Mountain range is a series of mountains which could be steep and snow covered or they could be gently sloping having rounded tops.

5. The highest mountain range in the world is the Himalayas.

6. Some mountains are found under the sea and could be taller than the Mount Everest, which is the highest mountain peak in the world.

7. There are three types of Mountains:

i) Volcanic mountains
ii) Fold mountains
iii) Block mountains

Fold Mountains

1. It is formed due to the compressive forces generated by endogenetic forces like earthquake, landslide etc.
e.g. of fold mountains - Himalayas, Alps, Andes, Rockies, Atlas etc.

2. On the basis of age, fold mountains are grouped into the following:

(a) Young/New Fold Mountains- They came into existence after the continent drift.
e.g. Himalayas, Andes, Rockies, Alps. Himalayas are regarded as the youngest mountains in the world.

(b) Old Mountains - They belong to pre-drift era, then subject to denudation and uplift.
e.g. Pen-nines (Europe), Appalachians (US), Aravalis (India) etc.

3. Examples of fold mountains include:

i) Himalayan Mountains in Asia
ii) the Alps in Europe
iii) the Andes in South America
iv) the Rockies in North America
v) the Urals in Russia

Block Mountains

1. It is formed when great block of Earth's crust may be raised or lowered due to tectonic activities.

2. The land between the two parallel faults either rises forming block mountains or horsts or subsides into a depression termed as Rift Valley or Graben.

3. Block mountains are created when large areas or blocks of earth are broken and displaced vertically.

4. The uplifted blocks are termed as horsts and the lowered blocks are called graben.

5. The Great African Rift Valley (valley floor is graben), The Rhine Valley and the Vosges mountain in Europe are examples.

6. Block mountains are also called fault block mountains since they are formed due to faulting as a result of tensile and compressive forces.

7. Block mountains are surrounded by faults on either side of rift valleys or grabens.

8. Examples-Vindhya and Satpura in Madhya Pradesh, Vosges in France and Black forest in Germany.

9. There are two basic types of Block Mountains:

i) Tilted block mountains have one steep side contrasted by a gentle slope on the other side.


ii) Lifted block mountains have a flat top and extremely steep slopes.

Volcanic Mountains

1. As the name suggests, volcanic mountains are formed by volcanoes.

2. Volcanic Mountains are formed when molten rock (magma) deep within the earth, erupts, and piles upon the surface.

3. Magma is called lava when it breaks through the earth's crust. When the ash and lava cools, it builds a cone of rock.

4. Rock and lava pile up, layer on top of layer.They are formed due to the accumulation of volcanic material, also known as mountains of accumulation.

5. Examples-mount Fuji (Japan), Cotopaxi in Andes, Vesuvius and Etna in Italy, Mount Mayon (Philippines) etc.

Residual or Dissected Mountains

1. Residual mountains are remnants of old mountains which have been worn down by agents of denudation.

2. They are formed as a result of erosion of plateaus and high planes by various agents of erosion.

3.. They are known as residual mountains or dissected mountains.

4. They owe their present form to erosion by different agencies.

5.They are usually hard resistant rocks that are let standing after the surrounding areas have been reduced by agents of denudation.
Mode of Formation of Residual Mountains

6. Residual mountains are formed from old fold, block or volcanic mountains by agents of denteation.

7. They may also emerge from plateaux as hills and valleys that have been dissected by rivers.

8. e.g. Nilgiris, Girnar and Rajmahal.Examples Catskill mountains of New York, Sierras of Spain, Highlands of Scotland and Nilgiri, Parasnath, Girnar, Rajmahal of India.

Major Mountain Ranges

The list depicts the major mountain ranges:

Plains

1. A relatively low-lying and flat land surface with least difference between its highest and lowest points is called a Plain.

2. Plains are broad, nearly level stretches of land that have no great changes in elevation.

3. They are generally lower than the land around them; they may be found along a coast or inland.

4. Coastal plains generally rise from sea level until they meet higher landforms such as mountains or plateaus.

5. Inland plains may be found at high altitudes.


Forms of Plain

Structural Plain : Formed due to the uplift of a part of the sea floor. e.g. the Great Plain of USA. Erosion Plain Formed when the elevated tract of land is worn down to a plain by the process of erosion. e.g. Plain of North Canada.

Depositional Plain : Formed by filling up of sediments into depressions along the foothills, lakes and seas. e.g. Indo Ganga Plain.

DESERT

• A desert is a barren area of land where little precipitation occurs and consequently living conditions are hostile for plant and animal life. About to one-third of land surface of the Earth is arid or semi-arid.
• Deserts are formed by weathering processes as large variations in temperature between day and night put strains on the rocks which consequently break in pieces.
• The major hot deserts of world are located on the western coasts of the continents between latitudes 15° and 30°N and South (S) because the effects of off-shore trade wind. Some of the examples arc Sahara, Arabian, Great Australian Desert, etc.
• The cold deserts are located in the interior of the continents such as Gobi, Talda Makan etc and some are found at some distance from the sea, such as Atacama. This deserts are dry due to the effect of orographic barrier.


ISLANDS

An island is any piece of land that is surrounded by water. A grouping of geographically or geologically related islands is called an
archipelago. The various types of islands are named according to the way they were formed.

Types of Island

They are as follows :

Continental Island : t is simply an island that rests on the continental shelf. Because of this, these islands are always quite close to a given continent. Also, the water level around a continental island is very shallow, typically less than 600 feet. Canadian island of new found land is a continental island, as is Greenland. Great Britain is the largest continental island in Europe.

Volcanic Islands : They are formed when volcanoes deep in the ocean rise above the water's surface.

Coral Island : It is an island that forms a ring and partially or totally encloses a shallow body of water or lagoon. Coral islands, which are large collections of coral a top rock (usually volcanic) in the ocean. Lakshadweep island in Indian ocean is best example of coral islands.

Alluvial Islands : They are formed by the outward flow of water depositing silt and gravel at the mouth of a river. New Moore island at the mouth of Ganga river in West Bengal is an alluvial island.

Barrier Islands : They are formed by waves depositing sand on the shallow ocean bottom as they crash on the shoreline.

Tectonic Island : They are formed by the result of tectonic activity. By the tectonic movement long island arcs (archipelagoes) are formed. Indonesia, Philippines, Japan groups cf island arc best example of it.



LAKES

A lake is a body of water surrounded by land from all the sides. A lake ca.n be fed and drained by rivers and streams.

Types of Lakes

Lakes can be classified as Tarn Tarn lakes (also often classified as Alpine lakes) are usually associated with glacial regions areas that have
been glaciated in the past. These follows form as the ice scours out the side of a hill, creating what is called a cirque.

Tarn Lake : Tarn lakes from the last ice ages are evident along some slopes of the Adirondack Mountains and from more recent glaciation in the European Alps.

Rift Valley : Lake Rift valley lakes occur in areas where rock is pulling apart. As a narrow wedge of land drops from the movement, a long, narrow lake often forms. The Rift valley, which cuts through Africa and Asia, contains the largest group of such lakes, including lake
Nyasa.

Crater Lake : Crater lakes form at a volcanic peak. When an extinct volcano collapses, it often leaves a somewhat
circular depression; water from rain and runoff eventually fills the lake. Crater lake in Oregon is a good example of such a lake.

Deflation Lake : Deflation lakes usually occur in deserts as the wind blows out depressions in the sand. If the hole reaches the local groundwater table, it can create an oasis. Such features dot the Sahara desert in Africa which are locally called Oasis.

Oxbow Lake : Oxbow lakes are created by a curved river meander that was cut off by sediment or other means, creating a bowed shaped lake. The Mississippi River shows evidence of past Oxbow lakes.

Artificial Lake : Artificial lakes are those usually formed by the damming of a river. These lakes are usually created to regulate the flow of a seasonal flooding river and many times offer a constant supply of potable (drinkable; water or generated electricity).

Classification of Plains

The image showcases the classification of plains:

Plateau

1. A plateau is a portion of land that is more or less flat and level, elevated above the surrounding area. It may have steep slopes or vertical cliffs on one or more sides. Tabular upland having relief of more than 500 feet may be defined as plateau.

2. Plateaus can be formed by the erosion of surrounding areas by rivers, flooding and glacier activity. An uplift of land can occur from the pressure of a large magma chamber under layers of rock.

3. Repeated lava flows can also form a plateau over a period of time. The collision of tectonic plates of the Earth’s crust can elevate a portion of land to create a plateau.

4. Tibetan plateau (5000 m) is the highest plateau in the world.

5. Famous Plateaus
• Auyantepui, Venezuela
• Columbian Plateau, northwestern USA
• Colorado Plateau, southwestern USA
• Deoasai Plains, Deosai National Park, Pakistan
• Tibetan Plateau, central Asia.

Important Plateaus of the World

Following are the important plateaus of the world:

 
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