Monday, 7 September 2026

KERALA PSC / INDIAN GEOGRAPHY / THE ISLANDS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

 KERALA PSC / INDIAN GEOGRAPHY / THE ISLANDS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE



 KERALA PSC / INDIAN GEOGRAPHY / THE ISLANDS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE


·      India has in all 247 islands of which 204 lie in the Bay of Bengal and the rest in the Arabian Sea and the Gulf of Mannar.

·      India has two groups of islands namely the Andaman and Nicobar Islands in the Bay of Bengal and the Lakshadweep Islands in the Arabian Sea

·      Andaman’s consists of a northern cluster of 204 small islands and Nicobar Islands consists of a southern cluster of 19 Islands

·      Ten degree channel separates Andaman from Nicobar

·      Port Blair is the capital of Andaman & Nicobar Islands

·      The southernmost tip of India, Indira Point (now submerged after 2004 Tsunami) is in Great Nicobar islands which is the biggest island in Nicobar group.

·      The Barren Island which became active in 1991 after being (inactive) for over two centuries is in Andaman

·      The Lakshadweep in the Arabian Sea comprises of a group of 36 Islands, about 300km to the west of Kerala coast. Only 11 of the islands are inhabited.

·      Kavarathi is the capital of Lakshadweep

·      Minicoy islands is separated from Maldives by 8º channel.

·      New Moore Island lies in Bay of Bengal near West Bengal also belongs to India.

·      Coco Islands North of Andaman belong to Myanmar.

·      The Andaman and Nicobar Islands are close to the Indo-Australian Plate Boundary

·      Androth is the largest island, 4.8sq.km and is nearest to Kerala.


 KERALA PSC / INDIAN GEOGRAPHY / THE ISLANDS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

KERALA PSC / INDIAN GEOGRAPHY / PLAINS OF INDIA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

 KERALA PSC / INDIAN GEOGRAPHY / PLAINS OF INDIA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE



 KERALA PSC / INDIAN GEOGRAPHY / PLAINS OF INDIA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE


·      The vast plains of north India are alluvial in nature and the western most portion is occupied by the Thar Desert.

·      The plains of south India, ie, coastal plains are also alluvial to a large extent.

·      The northern plain is known as the Ganga-Brahmaputra plain and is divided into smaller units like the western plain, eastern plain, Bihar plain, Bengal plain and Brahmaputra plain.

 

NORTHERN PLAIN

·      This plain lies to the South of the northern mountain wall and stretches in the shape of an are from the western most part of the country to the Brahmaputra valley in the east.

·      The Indo-Gangetic Plains also known as the Northern Plains

·      Indo-Gangetic plain is one of the most extensive stretches of the alluvium in the world

·      It is brought down by the rivers from the Himalayas in the north and the Peninsular plateau in the south.

·      The northern plains contain two river system, viz, the Indus and its tributaries in the west and the Ganga-Brahmaputra in the east.

·      The slit and alluvium that these rivers have been depositing have made the plains fertile.

·      These are gently sloping plains below 300m in elevation. The general slope is from West to East.

 

WESTERN PLAIN

·      The Western part of the northern plain is called the Indus plain or Punjab plain.

·      It slopes gently towards West and extends into Pakistan through Punjab

·      The plain is drained by the Indus and its tributaries. That part of the plain that extends in India is drained into the Arabian Sea by the rivers –Sutlej, Beas and Ravi, tributaries of the Indus that join the main stream after entering Pakistan. The Indian part of the plain is also called the Punjab and Haryana Plain.

·      Streams carrying water only during the rainy season and with their beds choked with boulders are called chos in Punjab

·      The water becoming sub-surface in this zone emerges on the surface in lower areas downstream and produces marshy conditions. Such marsh areas in Punjab are called mand.

·      The only river that remains perennial in its upper course in Haryana is Ghaggar. This stream is lost in the dry area in Rajasthan.

 

EASTERN PLAIN

·      It comprises the flood plain and the delta plains of the Ganga and the Brahmaputra

·      It is customary to divide this part into the Ganga plain and the Brahmaputra plain.

·      Ganga enters the Northern plains at Hardwar. The Yamuna joins it at Allahabad. The big Himalayan rivers joining the Ganga downstream of Allahabad from west to east are the Gomati, Ghaghara, Gandak and Kosi.

·      The Brahmaputra is known as Dihang in Arunachal Pradesh. After the meeting of the Lohit, Dihang and Dibang is called the Brahmaputra. After meeting with Ganga it is called Padma.

·      An important division of the plain is made in terms of the khaddar and the bangar zones. The term khaddar refers to the new alluvium and the bangar to the old alluvium.

·      The lower part of the plain adjacent to the rivers that is prone to frequent floods is called khaddar.

·      Bangar soils frequently have beds of Kanker or hard pans

·      The western part of the plain, from Haridwar to Aligarh is called Upper Doab and from Aligarh to Allahabad is called the Middle Doab.

·      The northern part of Ganga-Yamuna Doab and Uttar Pradesh is covered by Ruhelkhand Plain. This part is drained by Ghaghra, Rapti and Gomti rivers

·      The plain is characterized by streams that flow as sub-surface channels in dry season. This area is called the bhabhar or the bhabar zone.

·      The marshy region at the foot of the Himalayas is called the terai zone. Much of this zone has been drained out and reclaimed fro agriculture.

·      The foot hill zones of the eastern plain in the northern parts of West Bengal and still eastward are occupied by the Bengal Duars and Assam Duars.

 

COASTAL PLAINS

·      The coastal plains separate the peninsular plateau from the sea

·      The coast of India is divided into western coast and eastern coastal plains

·      The western coastal plain lies between the western Ghats and the Arabian Sea

·      It stretches from the Gulf of Kachch in the north upto Kanyakumari in the south, with a length of about 1500km

·      It is divided into Malabar Coast, Karnataka Coast, Konkan Coast, Gujarat Coast and Kachch and Kathiwad Peninsular

·      The coast is straight and is affected by the South-West Monsoon winds over a period of six months

·      Mumbai, Marmagoa, Cochin, Mangalore, Karwar, Nhava-Sheva and Kandla are the important parts on the west coast.

·      The eastern coastal plain extends from Kanyakumari to the Gangetic delta and between the Eastern Ghats and the Bay of Bengal.

·      This part of the plain south of the Krishna river mouth is known as the Coromandel Coast and in the north it is known as Utkal Coast

·      It consists of the deltas of rivers Mahanadi, Godavari, Krishna and Kaveri. It is a broad and flat land.

·      There are some saltwater lakes or lagoons. Chilka lake of Orissa and Pulicat Lake of Tamil Nadu are the best examples.


 KERALA PSC / INDIAN GEOGRAPHY / PLAINS OF INDIA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

KERALA PSC / INDIAN GEOGRAPHY / PENINSULAR PLATEAU / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

 

KERALA PSC / INDIAN GEOGRAPHY / PENINSULAR PLATEAU / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE



KERALA PSC / INDIAN GEOGRAPHY / PENINSULAR PLATEAU / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE


·      It is the largest of India’s physical divisions. It is the oldest and is formed of hard rocks

·      The Eastern Ghats and the Western Ghats constitute its eastern and western boundaries respectively

·      The river Narmada, which flows through a rift valley, divides the region into two parts: the Malwa Plateau in the north and the Deccan Plateau in the South.

·      The northwest part of the Malwa plateau is occupied by the Aravalli Ranges, Malwa region in the center, the Chotta Nagpur Plateau in the east and Vindhya mountains in the south.

·      The Deccan Plateau is composed of very old and hard rocks. This region is made up of crystalline rocks

·      The plateau region includes a number of other minor mountains besides the Aravalli and the Eastern and Western Ghats. They include the Vindhyas and Satpuras in Central India

·      The Satpuras, which lie between the rivers Narmada and Tapti, have several hills including the Rajpipla Hills in Maharashtra, and the Maikal Range and Pachmarhi Hills in Madhya Pradesh.

·      The Western Ghats separate the Deccan Trap region from the Western Coastal Plain while the Eastern Ghats lie between the Eastern Coastal Plain and the Deccan Trap.

·      The rocks of the Deccan Trap are rich in deposits of a variety of minerals. Granite, basalt, gneiss and quartzite are the major rocks besides some limestone and sandstone.

·      The Western Ghats form a continuous range from south to north and the highest range of this region is often called the Sahyadri

·      There are mountains passes across the western ghat linking the plateau with the western coastal plain. The Thal Ghat, the Bhor Ghat and the Palakkad gap are the three important passes. Anamudi is the highest peak in the western ghats.

·      The Western Ghats are blessed with the fine hill stations such as Mahabaleshwar, Udhagamandalam and Munnar.

·      The eastern Ghats do not constitute continuous chain of hills like the western Ghats. This chain is broken into small hills.

·      The Western Ghats are connected to the Eastern Ghats by the Nilgiri Hills (blue Mountains)

·      Two branches of the Annamalai Hills are known as the Palani Hills and the Yelagiri (Cardamom) Hills.

·      The Western Ghats are known by different local names. In Maharashtra and Karnataka they are called Sahyadri. Further south, they are called the Nilgiris in Tamil Nadu. Still further south, along the Kerala and Tamil Nadu border, they are known as Anaimala and Cardamom Hills.

·      The Sivasamudram Fall, the Gokak Fall and the Mahatma Gandhi Fall are important waterfalls in this area.

·      The most important waterfall formed by the Narmada is the Dhuandhar Falls near Jabalpur. The river flows through marble rocks in this region and hence the Dhuandhar Fall is also called the Marble Falls.

·      The Aravallis are one of the oldest fold mountains in the world. The highest peak of Aravalli range is Guru Shikhar near Mt. Abu (1158m) in Rajasthan.

·      The Aravallis due to erosion over a long period of time their height has been reduced and they can be considered relict mountains

·      River Chambal is the most important river originating from the eastern slopes of the Aravallis

·      The Luni and the Sabarmati are the most important rivers rising from the Aravallis and flowing in a westerly direction.

·      East of Aravalli range, the area is less dry and there are lower hills like Bundi Hills. Chambal and its tributaries flow through this part draining southeastern part of Rajasthan.


KERALA PSC / INDIAN GEOGRAPHY / PENINSULAR PLATEAU / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

KERALA PSC / INDIAN GEOGRAPHY / TRANS HIMALAYA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

 KERALA PSC / INDIAN GEOGRAPHY / TRANS HIMALAYA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE



KERALA PSC / INDIAN GEOGRAPHY / TRANS HIMALAYA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE


·      The Trans-Himalaya is a region of lofty mountains and vast glaciers. It comprises the Karakoram Ladakh and Zaskar ranges that originate from the Pamir Knot

·      The highest peak in India, Mount K2 (Mt. Godwin Austin 8611m) is in the Karakoram Range

·      The Trans Himalaya, in which there are several gorges and mountain passes, has an average height of above 6000m

·       Karakoram range is about 500km in length and is the most heavily glaciated part of the world outside the polar regions

·      The world’s second and third longest glaciers outside the polar regions are the Siachen Glacier (70km) and the Biafo Glacier (63km)

·      Ladakh range extends southeastward for 370km from the mouth of the Shyok River in the Ladakh region to the Tibetan border

·      The Ladakh range has no major peaks. Its average height is a little less than 6000 meters and few of its passes are less than 5000m.

·      Purvachal also called Eastern Highlands lies along the Eastern border of India with Myanmar

·      Some of the prominent features of the range include steep slopes, conical peaks and deep valleys

·      There are three hill ranges that come under the Patkai or the Purvachal. They are the Pataki-Burn, the Garo-Khasi-Jaintia, and the Lushai Hills

·      The climate ranges from temperate to alphine due to altitude.


KERALA PSC / INDIAN GEOGRAPHY / TRANS HIMALAYA / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

KERALA PSC / INDIAN GEOGRAPHY / IMPORTANT PASSES OF HIMALAYAS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE

 KERALA PSC / INDIAN GEOGRAPHY / IMPORTANT PASSES OF HIMALAYAS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE



 KERALA PSC / INDIAN GEOGRAPHY / IMPORTANT PASSES OF HIMALAYAS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE


·      Kashmir: Burzil and Zoji-la

·      Himachal Pradesh: Bara Lacha-la, Shipki-la.

·      Uttaranchal: Thanga-la, Niti-la, Lipu-Lekhla

·      Sikkim: Nathula, Jelepla mand Darki

·      Khybar pass is the most famous pass which leads from Peshwar to Kabul

·      South of Khybar pass is the Gomal Pass (it is in Pakistan)

·      The Bolan Pass leads from Kandahar to Quetta

·      In the Lesser Himalayas, slate, limestones and quartzites are the dominant rocks

·      This range holds some of India’s famous hill stations like Dalhousie, Nainital, Simla, Mussorie and Darjeeling

·      The southernmost range of the Himalayan system is called outer or sub-Himalayas or Siwaliks

·      This range is clearly distinguished only in the western part of the Himalayas. It is not a continuous range like the other ranges

·      Unlike the other ranges this mountain range is made up of mud and soft rocks. The Siwalik is prone to landslides and earth quakes.

·      There are broad longitudinal valley’s known as ‘Duns’

·      The Himalayas are known for some of the beautiful valleys of the world. The Kashmir valley is a classical example. It is rightly described as ‘paradise on the earth’.

·      The other important valleys are Kulu and Kangra in Himachal Pradesh

·      The doons in the Kumayun Himalaya of Uttar Pradesh are also well known


 KERALA PSC / INDIAN GEOGRAPHY / IMPORTANT PASSES OF HIMALAYAS / NOTES / OBJECTIVE QUESTIONS / STUDY MATERIALS / GENERAL KNOWLEDGE