Notes-Class 10-Geography-Chapter-3-Physiography & Drainage-Maharashtra Board

Physiography & Drainage

Class 10-Geography-Chapter-3 Maharashtra Board

Notes

Topics to be learn :

  • Comparative study of physiography of India and Brazil:
India Brazil
1- Himalayas

2- North Indian Plains

3- Peninsula

4- Coastal Plains

5- Island groups

1- Highlands

2- Great Escarpment

3- Coastal region

4- Plains

5- Island groups

  • Comparative study of drainage of India and Brazil:
India Brazil
1- Himalayan drainage

2- Peninsular rivers.

1-Amazon river

2-Paraguay- Parana rivers

3-Sao Francisco river

4-Coastal rivers.


Physiographic Divisions of India :

Himalayas : Himalayas is one of the young fold mountains in the world. It extends from Pamir Knot in Tajikistan in the west to the east. Himalayas is one of the major mountain systems of the continent of Asia.

Himalayan ranges :

(ii) Himalayan ranges in south-north direction :

  • Shivalik (the southernmost range.)
  • Lesser Himalayas.
  • Greater Himalayas.

Many Trans Himalayan ranges are also located to the north of Himalayan Range.

(iii) Himalayan ranges in west-east direction :

  • Western Himalayas (Kashmir Himalaya).
  • Central Himalaya (Kumaun Himalayas)
  • Eastern Himalaya (Assam Himalayas).

[collapse]

The North Indian Plains :

  • Division lies between Himalaya Mountains in the north and the Peninsula in the south.
  • Extends from Rajasthan and Punjab in the west to Assam in the east.
  • Mostly a flat low lying area.
  • The North Indian Plains are divided into two parts.

The part lying to the east of the Aravalis is the basin of the river Ganga and is therefore known as the Ganga Plains. It slopes eastward.

North Indian Plains :

The information of the North Indian Plains is as follows :

(i) Division :

  • Ganga Plains
  • Thar Desert
  • Punjab - Haryana Plains.

(ii) Features of Ganga Plain :

  • The delta of Ganga-Brahmaputra rivers (Sundarbans) extends in the state of West Bengal in India and Bangladesh.
  • Sundarbans is the largest delta region in the world.

(iii) Features of Thar Desert :

  • The western part of the North Indian Plains is occupied by the Thar Desert (Marusthali).
  • The state of Rajasthan is occupied by the Thar Desert.

(iv) Features of Punjab-Haryana Plain:

  • The Plains of Punjab lies to the north of Thar Desert.
  • It has very fertile soil.
  • Agriculture is highly developed in this region.

[collapse]

The Peninsula :The Indian peninsula lies to the south of North Indian Plains. This region tapers towards the Indian Ocean.

Many plateaus and hill ranges are included in the Indian peninsula.

The information of the Peninsula is as follows :

Mountains & Plateaus :

(i) Mountains :

  • The Aravalis Mountain range is located in the northern part.
  • Vindhya and Satpuda ranges are located in the central part.
  • Western Ghats (mountainous region) is located in the western part and
  • Eastern Ghat (mountainous region) is located in the eastern part.

(ii) Plateaus : The Indian peninsula also includes a series of plateaus bordering the Plains.

  • Maharashtra Plateau, Karnataka-Telangana Plateau, Chhota Nagpur Plateau, etc. are the main plateaus in this region.

[collapse]

The Coastal regions of India :

Western Coast : Barring the Gujarat coast, the western coast is mostly a narrow strip of land between the Arabian Sea and the Western Ghats. It does not have any vast extending plain lands.

The Gujarat coast is relatively broader, but it, too, has small and narrow coastal plains.

The Konkan Coast is full of spurs extending from the Western Ghats right up to the western coastline. It is rocky, having no vast plains.

The Malabar Coast is characterised by sand dunes, lagoons and backwaters. It, too, does not have any fast plain.

Features of the western coastal region of India :

Features of the western coastal region of India :

  • Borders the Arabian Sea.
  • Rocky and comparatively narrower.
  • Short and westward flowing rivers flow to the western coast and meet the Arabian Sea.
  • Rivers form estuaries in the western coastal region.

[collapse]

Eastern coast : The eastern coast of India is formed due to the depositional work of eastward flowing rivers meeting the Bay of Bengal.

Eastern coast of India is a coast of emergence and not a submergence like western coast. As its effect, the sea is not much deeper on the eastern coast than in the western coast.

Long and eastward flowing rivers meeting the Bay of Bengal form deltas at many places on the eastern coast. As its effect, it becomes difficult for ships to reach the east coast covered with sediments.

Therefore, there are fewer natural ports on the eastern coast of India.

Features of the eastern coastal region of India :

Features of the eastern coastal region of India :

  • Borders the Bay of Bengal.
  • Comparatively broader.
  • Long and eastward flowing rivers flow to the eastern coast and meet the Bay of Bengal.
  • Rivers form deltas in the eastern coastal regions.

[collapse]

Islands groups :

1) Lakshadweep Islands : Lakshadweep Islands is a group of islands of India located in the Arabian Sea.

Lakshadweep Islands group :

Features of islands in Lakshadweep Islands group :

  • Located in the Arabian Sea.
  • To the southwest of the mainland of India.
  • Far away from the western coastline of India.
  • Atoll islands, comparatively small in extent and are short in height.

[collapse]

Andaman-Nicobar Islands group :

2) Andaman and Nicobar Islands : Andaman and Nicobar islands are group of islands of India located in the Bay of Bengal.

Features of islands in Andaman-Nicobar Islands group :

1) Located in the Bay of Bengal.

2) To the southeast of mainland of India.

3) Far away from the eastern coastline of India.

4) Islands in Andaman group :

  • Only active volcanic islands in India, comparatively large in extent and have hilly regions in their interior parts. (Barren Island has the only active volcano in India.)
  • Nicobar group : Most of the islands are atoll islands.

[collapse]

Physiographic divisions of Brazil :

The Highlands : Most of the region of Brazil is covered by highlands. The highlands of Brazil and Guyana highlands together form the core of the continent of South America.

The information of these highlands is as follows :

(i) Highlands :

  • Guyana Highlands
  • Brazilian Highlands / Plateau.

(ii) Guyana Highlands :

(ii) Guyana Highlands :

  • Located in the northern part
  • Pico de Neblina peak is the highest peak (3014 m) lying on the border between Brazil and Venezuela.

[collapse]

(iii) Brazilian Highlands :

(iii) Brazilian Highlands :

  • Located in the southern and eastern part
  • Northern slope : (a) Amazon and its tributaries flow from the northern slope. (b) Many rapids and waterfalls are formed by these rivers. (c) Rivers originating from the northern slopes meet the Atlantic Ocean.
  • Southern slope : (a) Major rivers like Uruguay, Paraguay and Parana originate from the southern slope. (b) These rivers flow from Brazil and enter Argentina.
  • Eastern Slope : Very steep forming the Great Escarpment.

[collapse]

The Great Escarpment :

The Great Escarpment : The Great Escarpment border the eastern side of the

Brazilian Highlands. The information of the Great Escarpment is as follows :

(i) The nature and the altitude of the Great Escarpment :

  • From Sao Paulo to Porto Alegre, the height of Brazilian Highlands/ Plateau decreases remarkably leading to the formation of the Great Escarpment.
  • The altitude of the Great Escarpment/ eastern side of the Brazilian Highland is approximately 790 m.

(ii) The effect of the Great Escarpment on climate :

  • It acts as a barrier to the southeast Trade winds.
  • It leads to heavy rains in the Brazilian coastal areas and it also gives rise to the rain shadow area/ ‘Drought Quadrilateral' to the northeast of the Brazilian Highlands.

[collapse]

The Coasts : The coastline of Brazil extends for approximately 7400 km. It is divided into the northern coast and the eastern coast. The information of these coasts is as follows :

(i) Northern coast :

(i) Features of the northern coast :

  • Extends from Amapa province in the north to Rio Grande do Norte.
  • Northern coast is a low-lying region as Amazon and its many tributaries flow to the northern coast and meet North Atlantic Ocean
  • Marajo island, Marajo and Sao Marcos Bays lie on this coast.

[collapse]

(ii) Eastern coast :

(ii) Features of the eastern coast :

  • Extends from Rio Grande do Norte to the south.
  • Many small rivers flow to the eastern coast and meet South Atlantic Ocean.
  • Sao Francisco is the only major river meeting the South Atlantic Ocean in this region.
  • Many beaches and sand dune complexes lie on the eastern coast of Brazil.
  • In some areas, the eastern coast of Brazil is protected by coral reefs and atoll islands.

[collapse]

The Plains : The plains in Brazil is divided into Amazon basin in the north and Paraguay-Parana source region in the southwest.

The information of the plains in Brazil is as follows :

(i) Amazon Plains :

(i) Amazon Plains :

  • Largest plain land of Brazil.
  • Lies between Guyana Highlands and Brazilian Highlands in the northern parts of Brazil.
  • Width is the maximum, i.e. nearly 1300 km in the west.
  • The width is the minimum, i.e. 240 km where the Guyana Highlands and Brazilian
  • Highlands come closer.
  • Most of the area is inaccessible.

[collapse]

(ii) The plain of Paraguay and Parana rivers :

(ii) The plain of Paraguay and Parana rivers :

  • Located to the southwest of the Brazilian Highlands.
  • It is near the source region of Paraguay and Parana rivers.

[collapse]

(iii) Pantanal region :

(iii) Features of Pantanal region :

(1) One of the largest wetlands in the world.

(2) Characterized by swamps and marshes.

(3) Located towards the southwest of the Brazilian Highlands extending in the state of Mato Grosso do Sul.

Reasons behind the formation of swamps in the extensive continental location of Pantanal :

  • Paraguay river and its tributaries flow from the Pantanal region.
  • Pantanal receives runoff from the Brazilian Highlands.
  • The sediments brought by Paraguay river and its tributaries get deposited in the low lying Pantanal region.
  • The sediments and erosion residues as well as water remains filled throughout the years in Pantanal region leading to formation of swamps.

[collapse]

 Islands : Besides mainland, some islands are also included in Brazil. The information of these islands is as follows :

(i) Classification :

  • Coastal islands
  • Marine islands.

(ii) Coastal islands. :

(ii) Features of coastal islands :

  • Formed due to depositional work of Amazon river and its tributaries.
  • They are near the eastern coast of Brazil in South Atlantic Ocean and are coral islands/ atolls.

[collapse]

(iii) Marine islands. :

(iii) Features of marine islands :

  • Were a part of the mainland of Brazil.
  • Located in the Atlantic Ocean and nearly 300 km away from the mainland of Brazil.
  • Rocky
  • They are the tops of the submerged mountains.

[collapse]

Difference between the physiography of India and Brazil. :

Difference between the physiography of India and Brazil.

India Brazil
Physiography divided into the Himalayas, the North Indian Plains, the Peninsula, the Coastal Plains and the Island groups. Physiography divided into the Highlands, the Great Escarpment, the Coastal region, the Plains and the Island groups.
Many high and long extending mountains in India. There are no high and long extending mountains in Brazil.
The highest range of altitude is 6000 metres to 8000 metres. The highest range of altitude is 500 metres to 1000 metres.
The western part of the North Indian plains is occupied by desert. No such hot desert area lies in Brazil.
Many wide plains are located in the north and in the coastal areas in India. There are no wide plains in Brazil.
At many places, there are regions of backwaters in India. There are no such regions of backwaters in Brazil.
No any escarpments are located in India. The Great Escarpment is located in the northeast part of Brazil. This Great Escarpment demarcates the eastern side of the Brazilian Highland.

[collapse]

Drainage in India :

Himalayan drainage : Most of the Himalayan rivers originate in the snow covered southern heights of the Himalayan range. These rivers are well fed by rains during the rainy season through the southwesterly monsoon winds. These rivers are also fed by the melting of snow during summer. Therefore, most of the Himalayan rivers are perennial in nature.

The information of these rivers is as follows :

(i) Classification :

  • Sindhu river system
  • Ganga river system.

(iii) Characteristics of Sindhu river and its tributaries :

(ii) The features of Sindhu river and its tributaries :

  • Main river : Sindhu
  • Tributaries : Jhelum, Chenab, Ravi, Beas, etc. All these rivers flow from the state of Jammu and Kashmir.
  • Satluj originates near Man Sarovar.
  • The deposition of sediments brought by Satluj and its tributaries has formed the Punjab-Haryana Plain.

[collapse]

(iii) Characteristics of Ganga river and its tributaries :

(iii) The features of Ganga river and its tributaries :

  • The main river Ganga originates from Gangotri glacier.
  • Yamuna is a major tributary of Ganga and it originates at Yamunotri.
  • Dihang, Brahmaputra are the tributaries of Ganga flowing in northeast region of India.
  • Chambal, Ken, Betawa, Shon, Damodar, etc. are the peninsular tributary rivers of Ganga.

[collapse]

Peninsular rivers : The information of these peninsular rivers is as follows :

(i) Classification :

  • Westward flowing
  • Eastward flowing.

(ii) Features of westward flowing rivers in India :

(ii) Features of westward flowing rivers in India :

  • Many westward flowing rivers flowing from Kerala, Karnataka, Maharashtra and Southern Gujarat have similar features.
  • Tapi, Narmada, Mahi and Sabarmati flow into the Gulf of Khambhat.
  • Mahi river flows from the northeast to the southwest.
  • Sabarmati river originates from the southern slopes of Aravalis.
  • Luni river originates from the western slopes of Aravali and flows into the Gulf of Kutchchh.

[collapse]

(iii) Features of eastward flowing rivers in India :

(iii) Features of eastward flowing rivers in India :

  • Ganga, Godavari, Krishna, Kaveri are major eastward flowing rivers.
  • Godavari, Krishna and Kaveri originate in the eastern slopes of the Western Ghats.
  • Godavari is the second largest river system in India in terms of the catchment area.
  • Krishna river basin is located to the south of Godavari. Bhima and Tungabhadra are the major tributaries of river Krishna.
  • River Kaveri flows through the states of Karnataka and Tamil Nadu. It is used for irrigation since a long time.

[collapse]

 The major water divides of India :

Himalayas, Aravali range, Vindhya range, Satpuda range, Western Ghats are the major water divides of India.

  • Western Ghats separates the west flowing rivers meeting the Arabian Sea from the east flowing rivers meeting the Bay of Bengal
  • Vindhya range separates the Ganga drainage basin and Narmada drainage basin
  • Himalayas separates the rivers flowing in Himalayan system from the rivers flowing in Trans Himalayan range.

Measures are being taken to control pollution in the rivers of India :

Measures are being taken to control pollution in the rivers of India :

The following measures are being taken to control pollution in the rivers of India :

  • Controlling the discharge of human sewage into rivers.
  • Applying sufficient and appropriate pre-treatment to the industrial effluent/waste before being discharged to the sewers.
  • Displaying hoardings informing tourists not to pollute water of rivers and highlighting the importance of cleanliness.
  • Removing solid waste from rivers and applying other river cleaning processes.

[collapse]

Drainage in Brazil : In Brazil there are three major river Basins.

  • Amazon Basin
  • Paraguay-Parana system in the southwest
  • Sao Francisco in the eastern part of highland and other rivers at the coasts

(i) Features of Amazon basin :

 (i) Features of Amazon basin :

  • Amazon collects its headwaters from the eastern slopes of Andes Mountains in Peru.
  • Amazon river basin forms the largest plains in Brazil.
  • It is located in the northern parts of Brazil.
  • Amazon river has a huge discharge, leading to formation of islands near its mouth.
  • The width of the mouth of Amazon river is nearly 150 km. Most of the course and the mouth of Amazon river is used for navigation.

[collapse]

(ii) Features of Paraguay — Parana system :

(ii) Features of Paraguay — Parana system :

  • Located in the southwest region of Brazil.
  • Paraguay and Parana flow in southwest direction in Brazil and meet River Plata in Argentina.
  • Receives their headwaters from the southern slopes of Brazilian Highlands.

[collapse]

(iii) Features of Sao Francisco :

(iii) Features of Sao Francisco :

  • Sao Francisco’s entire basin is within Brazil.
  • It originates from the eastern slopes of Brazilian Highlands.
  • From its origin, for a distance of about 1000 km it flows towards the north over the Brazilian Plateau and then takes a sharp eastward turn and enters the coastal strip along the South Atlantic Ocean.
  • The downstream of Sao Francisco is used for navigation for nearly a distance of about 250 km.

[collapse]

(iv) Coastal rivers of Brazil :

(iv) Coastal rivers of Brazil :

  • These rivers are of short length.
  • Significant due to densely populated coastal area.
  • River Paraniba and River Itapecuru flows to the north and meet the North Atlantic Ocean.
  • River Jequitinhonha and River Pusguvach and some other rivers meet the South Atlantic Ocean.
  • River Puraguaco flows to the east and enters the Atlantic Ocean near Salvador town.

[collapse]

Distinguish between Ganga River Basin and Amazon River Basin :

Distinguish between Ganga River Basin and Amazon River Basin :

Ganga River Basin Amazon River Basin
1) Ganga originates from the Gangotri glacier in the Himalayas.

2) The length of Ganga is 2525 km

3) The water discharge of Ganga is 16,648 cu.m per sec.

4) The tributaries of Ganga are Yamuna, Betawa, Ken, Shon, etc.

1) Amazon originates from the eastern slopes of Andes mountain in Peru.

2) The length of Amazon is 6400 km.

3) The water discharge of Amazon is 2,09,000 cu.m. per sec.

4) The tributaries of Amazon are Negro, Japura, Zingu, Purus, etc.

[collapse]



Useful links :


Main Page : - Maharashtra Board Class 10 -Geography  - All chapters notes, solutions, videos, test, pdf.

Books :  MSBSHSE -Class 10th Geography Text Books – Chapter wise  PDF for download 

Previous Chapter : Chapter-2-Location & Extent - Online Notes

Next Chapter : Chapter 4 -Climate - Online Notes

3 Comments

Add a Comment
  1. It was helpful for me thank you

  2. I love this website can i get all lesson notes and all subject pls i request you to send me required thing

    1. all subjects are not ready we are working on it

Leave a Reply

Leave you Replay.... Your email address will not be published. Required fields are marked *