Savanna food web, chain, ecosystem and its biome

Savanna food web

The Primary consumer in the Savanna food web is Zebras and elephants. The Secondary consumers are cheetahs, hyenas, etc. The Scavengers here are vultures, hyenas, and termites. The reason hyena is present in both Secondary and Scavenger is because it gets their food by hunting in groups and also Scavenging on dead animals.

In this biome, Tall grasses are dominant and are the primary producer. The tall grasses convert energy from the Sun and minerals, and nutrients from the soil into the biomass that forms the basis of this Food Web. One of the important examples savanna food web is the one that exists in Africa.

African savanna food web

In the African savanna food web, the savanna is essential and it is a treeless plain present in a tropical or subtropical area, which is grassland found in eastern Africa, and the Northern part of Southern America.

It generally consists of scattered trees and drought-resistant flora. Some of the famous savannas are the Serengeti Plains of Tanzania, the Acacia Plains of East Africa, the savannas of Venezuela, the Sahel, south of Sahara in East Africa, and the Australian Savanna.

These tropical grasslands are found between tropical forests and deserts. This biome is found between 10° to 20 ° N and S latitudes.

These are generally hot and dry and experience moderate to low rainfall. As a result of this climate, the grasses grow tall and sharp. The chief occupation of people living here is herding and basically, these are Nomadic.

The biggest threat to the Tropical savanna food web is human activities such as converting these biomes to Pastoral lands, Agricultural activities, over-grazing, livestock, logging, and the introduction of non-native plants, etc.

The types of savannas are Tropical and Subtropical Savannas, Temperate Savannas, Mediterranean Savannas, Flooded Savannas, and Montane Savannas.

It is referred to by different names around the world such as:

  • Pampas in South America
  • Pasture,
  • Prairie in Northern America,
  • Rangeland in the USA
  • Steppe in Eastern Europe and Central Asia
  • Veld in Africa.
  • Downs in Australia
Tropical savanna food web
Tropical savanna food web by Gossipguy, CC BY-SA 3.0 https://creativecommons.org/licenses/by-sa/3.0, via Wikimedia Commons


Food chains in the savanna

The Zebras and elephants graze on grasses. The Lion and cheetah eat Zebras. Mara eats pampas grass and Maned Wold hunts Mara. The Hyena hunts as well as scavenges.

There are Vultures, and termites, in Savanna that are also Scavengers. The decomposers or Detritivores are mushrooms, insects, and microorganisms.

To Summarise the Food chains in the savanna: Producers, Primary consumers, Secondary Consumers, and Scavengers.

Producers in the Savanna

The primary producers in a savanna represent a complex functional group consisting of species of different habitats, sizes, and physiological requirements. The subdivision of the primary producers into morphological types such as herbs and trees.

The herbs can be further separated into grasses and forbs, C3 and C4 photosynthetic types, nitrogen-fixing and non-fixing, deep and shallow-rooted, early and late growers and so on.

The functional group of plants is defined according to the habit and size. In Savanna ecosystems, it is vital to differentiate between Herbaceous and Ligneous plants. This is because there are plants related to different rates of organic matter production and accumulation.

The producers in the Savanna include Grass, Acacia Trees, baobab Trees etc. Here also people cultivate pearl millet, legumes, vegetable crops, fonio, African rice etc.

Primary consumers in the Savanna

Primary Consumers of the savanna or the Herbivores in Savannas comprise vertebrates and invertebrates. The vertebrates that are well known are the large native mammals – animals of browsers and grazers, which is a salient feature of many African Savannas.

Also, there are many smaller herbivorous animals in Savannas including Armadillos and porcupines. Although invertebrates such as grass-eating harvester termites are important features of savannas.

The termites, ants, and grasshoppers are neglected as components of the savanna yet these insect herbivores play an important role in the savanna process including consuming grass material and seed predation.

Primary consumers in the savanna are Ostrich, Zebra, Thomsons Gazelle, Grasshopper, Giraffes, Elephants, etc.

Secondary Consumers

Savanna’s secondary consumers are Lions, Cheetahs, Secretary Birds, Harrier Eagles, etc. Human is also part Savanna food chain and they compete with other organisms for food.

Scavengers

Scavengers in the savanna are Hyenas, vultures, detritivores or decomposers like Fungi, bacteria, other Microorganisms, termites, etc. Also, Black-backed Jackals are seen on the hunting grounds of a lion.

Sometimes the top predators like lions also scavenge food.

Decomposers

Like any other ecosystem, decomposers in the savanna play a very important role in the flow of energy. The decomposers such as Bacteria, Fungi, Earthworms, and Insects do the role of transferring the energy between producers and consumers.

Bacteria in Savanna

Bacteriareis great number colonize the savanna’s soil. The bacteria in the savannas sustain well where the temperature is above 25 degrees Celsius.

Also, bacteria such as Acidobacteria are immune to changes in the moisture of the soil. This Acidobacteria slows down when the soil has few nutrients left adaptation makes them survive in the Savannas.

The most prominent bacteria in the African Savannas are Proteobacteria, Actinobacteria, Acidobacteria, Bacteroidetes, Chloroflexi, Firmicutes, Gemmatimonadetes, Planctomycetes, and Verrucomicrobia.

Fungi

The soils in Savanna are poor in nutrients, have frequent droughts and are very acidic. Due to these harsh conditions, fungi are less distributed than bacteria.

The common fungi found in African savannas are Sarcoscypha dudleyi, Laetiporus sulphureus, and Trametes versicolor.

Conclusion

We have discussed the savanna food web such as its basis of the food chain, What eats what in this biome what this biome is its reasons for its dangerous future, and the names it is called around the world.

References

  1. What Are the Trophic Levels in the Savanna? (sciencing.com)

North east monsoon in India Upsc

North east monsoon in India

North east monsoon in India is also called as Post Monsoon or Retreating Monsoon. The southwest monsoon starts in North India by the end of the second half of September because of the southward shifting of pressure belts. This wind gets backs from the Indian peninsula and blows towards the Bay of Bengal.

The Coriolis forces deflect this wind and make this wind blow from the Northeast and it is known as North-East Monsoon or Post Monsoon season. The Northeast Monsoon in India is connected with the formation of the North-Easterly wind system over the Indian subcontinent.

From this season, the states such as Tamil Nadu, Andhra Pradesh, Kerala, and south interior Karnataka get good rainfall that almost 35% of its annual rainfall. The Retreating monsoon creates a large-scale loss of life during the storms that occur frequently in Tamil Nadu, Andra Pradesh, and some parts of Karnataka.

During these seasons, strong winds and storms hit the coastal regions, and the daytime temperature falls rapidly all over the country. The average temperature over North-west India shows a decreasing trend from 38 and falling to 28-degree celsius in November.

North east monsoon in india
North east monsoon winds in india map

Ncert Notes for Retreating Monsoon

The below notes from 11th book

Season of Retreating Monsoon

The months of October and November are known for retreating monsoons. By the end of September, the southwest monsoon becomes weak as the low pressure trough of the Ganga plain starts moving southward in response to the southward march of the sun. The monsoon retreats from the western Rajasthan by the first week of September.

It withdraws from Rajasthan, Gujarat, Western Ganga plain and the Central Highlands by the end of the month. By the beginning of October, the low pressure covers northern parts of the Bay of Bengal and by early November, it moves over Karnataka and Tamil Nadu. By the middle of December, the centre of low pressure is completely removed from the Peninsula.

The retreating southwest monsoon season is marked by clear skies and rise in temperature. The land is still moist. Owing to the conditions of high temperature and humidity, the weather becomes rather oppressive. This is commonly known as the ‘October heat’. In the second half of October, the mercury begins to fall rapidly, particularly in northern India. The weather in the retreating monsoon is dry in north India but it is associated with rain in the eastern part of the Peninsula. Here, October and November are the rainiest months of the year.

The widespread rain in this season is associated with the passage of cyclonic depressions which originate over the Andaman Sea and manage to cross the eastern coast of the southern Peninsula. These tropical cyclones are very destructive.

The thickly populated deltas of the Godavari, Krishna and Kaveri are their preferred targets. Every year cyclones bring disaster here. A few cyclonic storms also strike the coast of West Bengal, Bangladesh and Myanmar. A bulk of the rainfall of the Coromondal coast is derived from these depressions and cyclones. Such cyclonic storms are less frequent in the Arabian Sea.

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Below notes are from Ncert 10th book

Retreating/Post Monsoons (The Transition Season)

During October-November, with the apparent movement of the sun towards the south, the monsoon trough or the low-pressure trough over the northern plains becomes weaker. This is gradually replaced by a high-pressure system. The south-west monsoon winds weaken and start withdrawing gradually. By the beginning of October, the monsoon withdraws from the Northern Plains.

The months of October-November form a period of transition from hot rainy season to dry winter conditions. The retreat of the monsoon is marked by clear skies and rise in temperature. While day temperatures are
high, nights are cool and pleasant. The land is still moist. Owing to the conditions of high temperature and humidity, the weather becomes rather oppressive during the day.

This is commonly known as ‘October heat’. In the second half of October, the mercury begins to fall rapidly in northern India.

The low-pressure conditions, over north-western India, get transferred to the Bay of Bengal by early November. This shift is associated with the occurrence of cyclonic depressions, which originate over the Andaman Sea. These cyclones generally cross the eastern coasts of India cause heavy and widespread rain. These tropical cyclones are
often very destructive.

The thickly populated deltas of the Godavari, the Krishna and the Kaveri are frequently struck by cyclones, which
cause great damage to life and property. Sometimes, these cyclones arrive at the coasts of Odisha, West Bengal and Bangladesh. The bulk of the rainfall of the Coromandel Coast is derived from depressions and cyclones.

north east monsoon winds in india map
North east monsoon winds in India map

Distribution of Rainfall

Parts of western coast and northeastern India receive over about 400 cm of rainfall annually. However, it is less than 60 cm in western Rajasthan and adjoining parts of Gujarat, Haryana and Punjab. Rainfall is equally low
in the interior of the Deccan plateau, and east of the Sahyadris. Why do these regions receive low rainfall? A third area of low precipitation is around Leh in Jammu and Kashmir. The rest of the country receives moderate rainfall.
Snowfall is restricted to the Himalayan region.

Owing to the nature of monsoons, the annual rainfall is highly variable from year to year. Variability is high in the regions of low rainfall, such as parts of Rajasthan, Gujarat and the leeward side of the Western Ghats. As such, while areas of high rainfall are liable to be affected by floods, areas of low rainfall are drought-prone.

Conclusion

The North East Monsoon is a crucial aspect of India’s climate system, bringing much-needed rainfall to southern peninsular India. Understanding its dynamics and impact is essential for various sectors like agriculture, water resource management, and disaster preparedness. For UPSC aspirants, a thorough grasp of the North East Monsoon is vital, as it is frequently tested in the geography and general studies papers.

Downloads

1.North East Monsoon in India Upsc 10th Ncert Notes Pdf

2.North East Monsoon in India 11th Ncert Notes for Upsc Pdf

The direction of South west monsoon in India

Direction of South West monsoon in India

The Bay of Bengal wind moves to northeast India, Myanmar and this wind is trapped by mountain groups such as Khasi, Garo, and Jaintia. This results in the heaviest rainfall in the world, that is Mawsynram located in Meghalaya.

Then it moves to the west, which results in a rainfall decrease from east to west. The southwest monsoon winds in India are responsible for 75% of the Indian rainfall. Tamil Nadu that is located on the leeward side receives less rainfall from this wind.

South west monsoon in India

There occurs a rapid increase of temperature in May over the North-Western plains. This intensifies the low-pressure condition over there.

By early June, this low pressure is enough to attract the trade winds of the Southern Hemisphere, which come from the Indian Ocean.

These Southeast trade winds cross the equator and enter the Bay of Bengal and Arabian sea and catch up in the air circulation over India.

These pass over the equatorial warm currents and bring a lot of moisture. This wind after crossing the equator follows a southwesterly direction. That is the reason it is called Southwest Monsoons.

Rain of Southwest Monsoon starts abruptly. The first result of this rain is it brings down the temperature quickly. This sudden onset of moisture-laden winds is associated with violent thunder and lightning. This is termed as ‘break’ or ‘burst’ of the monsoon.

The burst of monsoon starts in the first week of June in the coastal areas of Kerala, Karnataka, Goa, and Maharashtra. In the internal part of the country, the burst of monsoon gets delayed to the first week of July.

There would be a decline in day temperature from 5°C to 8°C between mid-June and mid-July.

When these winds approach the land, its southwesterly direction is changed by the relief and thermal low pressure over Northwest India. The southwestern monsoon approaches India by two branches:

  1. Arabian Sea Branch
  2. Bay of Bengal Branch

Monsoon Winds of the Arabian Sea

The Monsoon winds the starts over the Arabian sea further split into three branches:

First Branch

The first branch is obstructed by the Western Ghats. These winds get on to slopes of western ghats from 900-1200. Then they quickly become cool and as a result, the windward side of Sahyadris and Western Coastal plain gets heavy rainfall between 250 cm and 400 cm.

After crossing the western Ghats, these winds descend and get heated up and as a result humidity of these winds gets decreases. Due to this, the winds cause little rainfall in the east of the Western Ghats.

This region is called the Rain-Shadow region. This is because it receives less rainfall.

Second Branch

Another branch of Arabian sea monsoon winds hits the coast north of Mumbai. This moves along the Narmada and Tapi river valleys.

Then these winds cause rainfall in an extensive area of central India. As a result, the Chotanagpur plateau gets 15 cm of rainfall from this part of the branch.

At last, these winds enter the Ganga Plain and mingle with the branch of the Bay of Bengal.

Third Branch

The third branch of wind hits the Saurashtra Peninsula and Kachchh. Then it passes over Rajasthan and Aravalis and causes only a little rainfall.

In Punjab and Haryana, it joins the Bay of Bengal branch. These two branches reinforced and cause rains in the Western Himalayas.

Monsoon Winds of the Bay of Bengal

The Bay of Bengal branch strikes the coast the Myanmar and southeast parts of Bangladesh. The Arakan Hills on the coast of Myanmar deflect a big portion of the Bengal branch towards the Indian subcontinent.

Therefore the Monsoon enters West Bengal and Bangladesh from the south and southeast direction instead of the south-westerly direction.

From here, this branch splits into two under the influence of the Himalayas and the thermal low is northwest India. It’s one branch moves westward along the Ganga plains reaching up to Punjab plains.

Another branch moves up to Brahmaputra valley in the north and the northeast causing heavy rains.

Its subbranch strikes the Garo, Khasi hill of Meghalaya, Mawsynram that is located on the crest of Khasi Hills. This region receives the highest average annual rainfall in the world.

But during this season, the Tamil Nadu coast remains dry. This is due to two factors:

a. Tamil Nadu coast is situated parallel to the Bay of Bengal of southwest monsoon.

b. Also it lies in the rainshadow area of the Arabian sea branch of the southwest monsoon.

For Tnpsc

The southwest monsoon is the most important feature of the Indian climate. It takes place in the Southern Tip of India Peninsula normally by the first week of June.

South-West monsoon advances along the Konkan coast during starting of June and it covers the whole country by July 15.

The global phenomenon El Nino influences the South West Monsoon. In North India, the temperature reaches almost 46-degree Celsius before the southwest monsoon or rainy season.

There occurs a “Burst of Monsoon”, which is termed as Break, which is a sudden approach of monsoon wind over southern India with Thunder Showers.

This show reduces the temperature of the country.

south west monsoon in india
direction of southwest monsoon in india in map

South West Monsoon Winds

The monsoon wind that is the southern tip of India’s landmass gets separated into two branches.

One branch starts from the Arabian Sea and Another Branch starts from the Bay of Bengal. The one from the Arabian sea provides heavy showers to the west coast of India and is located on the west ghats windward side.

The other part towards the north hits the Himalayan Mountains and brings heavy rainfall in the North.

Rajasthan and western parts get rain from these winds as the direction of the wind is parallel to the Aravali mountains and there is nothing to hold or intrude the wind.

Theory of plate tectonics Upsc

Theory of plate tectonics

The theory of plate tectonics is a scientific theory that explains the formation of major landforms due to the Earth’s underlying movements. The Earth is often described as a living planet, which reshapes itself constantly through the forces that operate deep beneath the surface. Among these, the theory of plate tectonics is perhaps the most fundamental in explaining the Earth’s dynamic nature.

Plate Tectonics refers to the movement of large plates that make up Earth’s outer shell, and it is responsible for shaping continents, forming mountains, which fuels volcanic activity, and triggers earthquakes, etc.

What is the theory of plate tectonics?

The interest in the distribution of oceans and continents came to life after the introduction of the concept of seafloor spreading.

After that, it was McKenzie and Parker and also Morgan 1967 came out with another theory. This theory is based on a Lithospheric plate also called a Tectonic plate.

The tectonic plate is a massive, irregularly shaped block of solid rock and it is generally made of both continental and oceanic plates.

Their theory is collectively called Plate Tectonic theory.

Plate Tectonic theory

According to the theory of plate tectonics, the plates move horizontally over the Asthenosphere as solid units.

Plate Classification

The lithosphere consists of the crust and top mantle with a thickness of 5 to 100 km in oceanic parts and 200 km in continental areas.

Depending on the occupied area of the plate, the lithosphere is classified as an oceanic or continental plate.

  • If a large portion of the plate occupies the ocean it is called an Oceanic plate
  • If a large portion of the plate occupies the continent it is called a continental plate.
Plate tectonic theory
Plate tectonic theory – Position of continents through geological past Source:Ncert

An example of an Oceanic plate is the Pacific plate and the Continental plate is the Eurasian plate. According to this theory, the earth’s lithosphere is divided into seven major and some minor plates.

These plates are surrounded by Young fold mountain ridges, trenches, and faults. The major leaves are as follows:

Major and minor plates of the world

7 Major plates

The seven major plates of earth are:

  1. Antarctica and surrounding oceanic plates,
  2. North American Plate(with the western Atlantic floor separated from the South American Plate along with the Caribbean Islands),
  3. South American Plate (With the western Atlantic floor separated from the North American Plant along with the Caribbean islands),
  4. Pacific Plate,
  5. India-Australia-New Zealand Plate,
  6. Africa with the eastern Atlantic floor plate,
  7. Eurasia and the adjacent oceanic plate.

Above is the list of major plates. Now let us see the list of some important minor plates below:

  • Cocos Plate – It is found Between Central America and the Pacific plate
  • Nazca plate – It is found between South America and the Pacific plate
  • Arabian Plate – It is found in the Saudi Arabian landmass
  • Philippine Plate – It is found between the Asiatic and Pacific plate
  • Caroline Plate – It is found between the Philippine and Indian Plate that is North of Guinea
  • Fuji Plate – It is found in the North-East of Australia
Tectonic Plates across the World in World map
Tectonic Plates across the World by Source: Ncert

These tectonic plates are dynamic, they keep moving on.

Wegner believed that the continents move by his Continental Drift Theory.

Alfred Wegner

But it is not, Actually, the continents reside over, the tectonic plates. It is the tectonic plates that actually move. And the fact is all the plates have moved in the past and will continue to move in future as well.

In the continental drift theory, Wegner believed that all the continents were once together as a single landmass called Pangaea. But later research revealed that these plates are wandering throughout geological history and Pangea was the result of the converging of different continental masses, which once were present somewhere else.

By using Palaeomagnetic data, the position of the current continental landmass is founded.

As per the data, the Indian subcontinent is traced with the help of rocks found in the Nagpur area.

The plate boundaries are of three types:

  1. Divergent Boundaries
  2. Convergent Boundaries
  3. Transform Boundaries

Divergent Boundaries

Whenever the plates move from each other, a new crust is generated. The spreading sites are sites where the plates move away from each other.

Example: the Mid-Atlantic Ridge divergent boundaries, as a result of the American plate, separated the front of the Eurasian and African Plates.

Convergent Boundaries

One plate dives under another where the crust is destroyed, Subduction zone is the location where the sinking of a plate occurs.

The convergence can occur in three ways, these are 1. Between an oceanic and continental plate; 2. between two oceanic plates; 3. between two continental plates

Transform Boundaries

Plates horizontally slide over each other, the crust is neither created nor destroyed. Transform faults are the planes of separation generally perpendicular to the mid-oceanic ridges.

“The eruption does not take all along the entire crest at the same time, there is a differential movement of a portion of the plate away from the axis of the earth and also the earth rotation has effects on the separated block of the plate“.

Plate Movement Rate

The rate of the plate movement is determined by the strips of the normal and reverse magnetic fields that are parallel to the mid-oceanic ridges. Accordingly, the slowest plate movement rate is found in Arctic Ridge at less than 2.5cm/yr.

The fastest plate movement rate is found in the East Pacific rise near Easter Island in the south pacific about, west of Chile about 3400 km.

Plate Movement Force

When Alred Wegner proposed the Continental Drift Theory, most scientists believed that the earth was static and motion solid object but after various studies such as seafloor spreading, Plate Techtonic, etc, scientists found earth was continuously moving and dynamic. Now plate movement is accepted by everyone.

Below the Rigid plate, the mobile rock is believed to moving in a circular manner. The heated material is rise above, spreads, gets cooled and sinks to greater depths and this cycle is repeated continuously and called convection cell or convection flow.

The two main sources of heat within the earth are Radioactive decay and residual heat. This idea is first proposed by Arthur Holmes’s 1930s, later Harry Hess went about Seafloor Spreading.

The slow movement of the hot, softened mantle is responsible for the force behind the plate movement.

Also, Check the Indian Plate Movement

Conclusion

We have discussed Plate tectonic theory, Its types and the evidence that supports it. Also, we have discussed the Tectonic plates boundaries.

References

https://www.google.co.in/books/edition/Did_Plate_Tectonics_Give_Rise_to_Life_Un/KzMxEQAAQBAJ?hl=en&gbpv=1&dq=Theory+of+plate+tectonics&pg=PT11&printsec=frontcover

Continental drift theory Upsc

Continental drift theory

It is a Hypothesis, theory regarding the formation of the continents. When we look at the shape coastline of the Atlantic Ocean, the symmetry of the coastlines on either side of the ocean creates a curiosity in us.

This made many scientists think that the Two American continents, Europe and Africa were once together. This idea was first proposed by Abraham Ortelius, a Dutch mapmaker in 1596.

Continental drift theory was proposed by?

Continental drift theory was proposed by Alfred Wegener.

Also, A guy named Antonio Pellegrini drew a map, illustrating that the three continents were once together. But the comprehensive argument to support this theory was put by a German Scientist, Alfred Wegener. This theory was known as the Continental Drift theory. This theory was proposed in the year 1912.

Continental Drift Theory
Continental Drift Theory by nationalgeographic.org/encyclopedia/continental-drift/

According to Wegener, all the continents were once together as a single continental mass and it is surrounded by a mega ocean. He called this Mega continent ‘PANGAEA‘ and this mega ocean ‘PANTHA-LASSA‘.

Wegner argued that Pangaea began to split around 200 million years ago. Also that the super continental split into two large continental masses, one is Laurasia and another one is Gondwanaland.

Laurasia formed the northern component and Gondwanaland formed the southern part. Subsequently, these two continental masses broke into many pieces that we see today.

The best evidence for continental drift theory

The following is the evidence that supports the Continental drift theory by Alfred Wegener.

  • Jig-Saw-Fit
  • Rocks of Same Time across the continent
    • Tillite
    • Placer Deposits
    • Distribution of Fossils
  • Placer Deposits
  • Distribution of Fossils
  • Force for Drifting
  • Post-Drift Studies

Jig Saw Fit

Africa and South America’s shorelines have a great and unmistakable match. In 1964, Bullard produced the best fit for Atlantic margin using computer drawings, and it proved to be a great match. The match was tried at 1000 Fathom, deep in the sea.

Fathom

a unit of Fathom is equal to six feet (1.8 metres), mainly used in reference to the depth of sea, lakes etc.

Rocks of the Same Age across the continent

The Age of rocks is determined by radiometric dating methods across the continents and oceans. By this method belt of ancient rocks from the Brazil coast which is of age 2000 million years match those from Western Africa.

And the rocks from the Jurassic age, are found along the coastline of South America and Africa. These were the earliest marine deposits. This also suggests that the ocean did not exist prior to this age.

Tillite

Gondawana sediments from India has its counterparts in 6 different places in southern Hemisphere
Tillite (Gondawana) found in India and Parts of Southern Hemisphere – CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=1320706

Tillite were the sedimentary rocks that are formed out of deposits of glaciers. A sedimentary rock that consists of consolidated masses of unweathered blocks such as large, angular, detached rock bodies and glacial till which are unsorted and unstratified rock material deposited by glacial ice in a rock flour.

Gondawana sediments from India and has their counterparts in six different landmasses of the Southern Hemisphere. At the base, the system has thick tillite indicating prolonged glaciation.

The Gondawana system of sediments from India was found in Africa, Falkland Island, Madagascar, Antarctica, and Australia.

The Glacial Tillite provides strong evidence of palaeoclimates and the drifting of continents.

Placer Deposits

Placer Deposits
Placer Deposits By © Hans Hillewaert, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=11750393

The presence of rich placer deposits of gold on the Ghana coast and the absolute absence of source rock in the region is an amazing thing.

The gold-bearing veins are in Brazil and are gold deposits of Ghana are derived from the Brazil plateau.

Distribution of Fossils

The same animal and plant fossils were found on different continents separated by thousands of Kilometres and the ocean between them is great evidence that the continents were once together.

Examples are Lemurs found in India, Madagascar and Africa linked to Lemuria landmass. These were separated by thousands of Kilometre and the ocean between them.

Also, Mesosaurus, an extinct marine reptile that has adapted to Brackish water, skeletons were found only in two places, are southern Cape province of South Africa and Iraver formation of brazil. The distance between these two locations is 4800 km and the ocean is in between them.

Force for Drifting

Alfred Wegners suggested that the movement of continents is due to tidal forces and polar-fleeing forces. Polar fleeing forces are forces created due to the rotation of the earth.

But the many scientists rejected this as these forces were very few.

Post-drift Studies

The post-World-II period and evolution of technology added new information to the studies. This includes information collected from the ocean floor mapping provided a new dimension for the study of the distribution of oceans and continents.

Conclusion

We discussed the Continental drift theory by Alfred Wegner and the evidence that supports this theory. This is useful for Upsc and other public service commission exams.

Types of forest in Tamilnadu Tnpsc

Forest in Tamil Nadu

In Tamilnadu, the forest into divided into three major groups as per the temperature. They are Tropical Forest, Montane Subtropical forest, and Montane Temperate Forest.

These are further divided based on moisture and physio-gnomic variations.

Tropical Evergreen Forest

Tropical Evergreen Forest at Kolli Malai
Tropical Evergreen Forest at Kolli Malai By Chinchu.c – Own work, CC BY 4.0, https://commons.wikimedia.org/w/index.php?curid=83680255

The tropical evergreen forest is found in the regions which receive heavy rainfall. It is found in the upper slopes of Western Ghats of Tirunelveli, Kanyakumari, Nilgiris, and Coimbatore districts.

The major tree species of this forest are cinnamon, Malabar ironwood, panasa, java plum/Jamun, jack, kindal, ayani, and crape myrtle.

The semi-evergreen type of forest is found over the regions of sub-tropical climate over the Eastern Ghats.

The famous regions are Servarayan, Kollimalai, and Pachaimalai. Species of Indian mahogany, monkey teak, woolly cassia, jack, and mango trees are common in this region.

Montane Temperate Forest

 Montane Temperate Forest - Nilgiris
Montane Temperate Forest – Nilgiris By Ranveig – Own work, Public Domain, https://commons.wikimedia.org/w/index.php?curid=2838568

Montane Temperate Forest is found in the sheltered valleys of Anaimalai, Nilgiris, and Palani Hills over a 1000 metres altitude.

These are known as ‘Sholas‘. The tree in these forests are evergreen and are usually short. Nilgiri Champa, wights litsea, and rose apple are the common trees found in this forest.

Tropical Deciduous Forest

 Tropical Deciduous Forest - Agasthya Malai
Tropical Deciduous Forest – Agasthya Malai By Rakesh – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=242144

This type of forest lies in the margin of semi-evergreen and evergreen forests. The trees in this forest shed their leaves during the dry season.

The trees reach up to a height of 30 metres. Some trees of this forest are silk cotton, kapok, kadamba, dog teak, woman’s tounge, axlewood, and siris.

Bamboos are also common in this type of forest. Some trees of this forest are economically important.

Mangroves

Mangroves forest in Tamil Nadu - Pichavaram
Mangroves forest in Tamil Nadu – Pichavaram By Karthik Easvur – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=33271265

This type of forest is found in the coastal areas, river deltas, tails of islands, and overseas faces where accretion is in progress. The vegetation is typically evergreen, moderate in height, and has leathery leaves.

The vegetation of this forest is adapted to survive in tidal mud and saltwater. Asiatic mangrove, white mangrove, wild jasmine/Indian pivot, etc. are some of the notable trees of this forest.

Pichavaram, Vedaranyam, Muthupet, Chatram, and Thoothukudi are the places in Tamil Nadu where the mangrove forest is found to a considerable extent.

Role of Mangroves in Coastal Zone Management

Mangroves help in the prevention of coastal erosion from waves and storms. It also protects coral reefs and seagrass meadows from being smothered in sediments.

Pichavaram mangrove forest is located near Chidambaram, Cuddalore district. This is the second-largest mangrove forest in the world covering about 1,100 hectares (11 sq. km) of area.

It is separated from the Bay of Bengal by a sandbar and consists of species like Avicennia and Rhizophora.

It also supports the existence of rare varieties of shell and finishes.

Tropical Thorn Forest

Thorn forest in Tamil Nadu is found where there is little rainfall. These forests are found from plains up to 400 meters altitude.

The common trees of this forest are rusty acacia, wheel, neem, and palm. Shrubs are common vegetation in this type of forest.

This type of forest is found in the districts of Dharmapuri, Ramanathapuram, Virudhunagar, and some parts of the interior districts.

Conclusion

Tamil Nadu has a wide variety of wild animals, birds, and reptiles. Its hills hold an ideal place for elephants, bison, tigers, deers, and monkeys.

Types of soil found in Tamil Nadu and its district wise Distribution Tnpsc

Types of soil found in Tamil Nadu

Tamil Nadu state is located in the southernmost part of the Indian subcontinent. It consists of several hills, plateaus, rivers,s and several types of soils. Types of soil are based on their physiography, such as hills, plateaus, coastal lines, rivers, etc.

Also, the soil of a place depends on factors like climate, parent rocks, and vegetative cover of the respective places.

As Tamil Nadu heavily depends on agriculture and its allied industry, it is important to study the soils, their nature, and distribution for better administration.

Types of soil found in Tamilnadu
Types of soil in Tamil Nadu Map

Types of Soil in Tamil Nadu

Alluvial, Black, Red, Laterite, and Saline Soil

The Tamilnadu Agriculture University classifies primarily 4 Types of soil present in Tamilnadu, they are

  1. Red soils (62 per cent)
  2. Black soils (12 per cent)
  3. Laterite soils (3 per cent) and
  4. Coastal soils (7 per cent)

Alluvial Soil

Alluvial Soil in Tamil Nadu
Alluvial Soil in Tamil Nadu By Ramesh Thadani – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=18350182

Alluvial soils are formed by the deposition of silt by the rivers. It is most fertile as it is rich in minerals such as lime, potassium, magnesium, nitrogen, and phosphoric acid, but it is deficient in nitrogen and phosphoric acid.

It is porous and loamy. The supported crops are Paddy, sugarcane, banana, and turmeric. Basically, it is found along the river valleys and coastal plains of Tamil Nadu.

It is found in the districts of Thanjavur, Tiruvarur, Nagapattinam, Villupuram, Cuddalore, Tirunelveli, and Kanyakumari, and along the river valleys in a few interior districts.

The Tamil Nadu Agriculture University site did not mention the alluvial soil percentage, but it should be somewhere around 3 to 6%.

Black Soil

Black Soil By Ganesh Dhamodkar, CC BY 3.0, https://commons.wikimedia.org/w/index.php?curid=54754371

Black soil is formed by the weathering of igneous rocks. It is also called Regur Soil. This is developed over the Deccan lava granite region under semiarid conditions.

It is fine-textured and clayey in nature; it is poor in phosphoric acid, nitrogen, and organic matter. The main minerals found in this soil are calcium, magnesium, carbonates, potash, and lime.

As cotton grows well in it, it is also called black cotton soil. The major crops cultivated in it are Cotton, sorghum, cumbu, and fodder crops.

Also, it is one of the important types of soil found in Tamil Nadu as it occupies 12% of the total soil. It is distributed across the districts of Coimbatore, Madurai, Virudhunagar, Tirunelveli, and Thoothukudi.

Red Soil

Red Soil in Tamil Nadu
Red Soil in Tamil Nadu

Red soils cover over two-thirds of the total area of Tamil Nadu. It is found mostly in the central districts of the state. It is sandy and loamy in texture. However, the characteristics of red soils change based on their formation and the climatic conditions under which it is formed.

It is porous, friable, and non-retentive to moisture. It is red in colour due to the presence of a high concentration of Iron oxides.

It is poor in nitrogen, phosphorus, acidic and humus. Almost all the crops can be cultivated in it with the application of manure and irrigation facilities.

It is the most important type of soil found in Tamil Nadu, as it is present in 62% of Tamil Nadu. It is distributed in the districts of Sivagangai, Ramanathapuram, etc.

The crops grown in it are Paddy, Ragi, Tobacco, and Vegetables.

Laterite Soil

Laterite soils in tamil nadu
Laterite soils in Tamil Nadu

Laterite is derived from the Latin word ‘Later’, which means brick. This develops in areas where the temperature is high and there is high rainfall. It is formed by the process of intense leaching.

As the rain washes away the lime and silica, it is left with Iron oxide and aluminium compounds.

Also, its humus content is removed quickly by bacteria that thrive well in high temperatures. As a result, these are poor in organic matter, nitrogen, phosphate, and calcium.

But it has excess Iron oxide and potash. Hence, it is not suitable for agriculture. But by using manure and fertilisers, cultivation can be made.

It supports paddy, ginger, pepper, cashew nuts, and plantains. Also, it is suitable for the cultivation of tea and coffee plants. Also, it is widely used to cut bricks for construction.

It is found in some parts of the Kancheepuram, Tiruvallur, and Thanjavur districts. Also in the mountainous region of the Nilgiris.

Saline Soil

It contains a large proportion of sodium, potassium, and magnesium; as a result, they are infertile and do not support vegetative growth. Also, it lacks nitrogen and calcium.

Because of poor drainage and a dry climate, they have more salt. Its nature ranges from sandy to loamy.

Seawater intrusion in deltas promotes saline soils. Also, in the area that promotes intensive agriculture using intensive irrigation, saline soil is formed due to capillary action that brings salts to the top.

To solve the problem of salinity, the farmer is advised to use Gypsum in the soil.

These are confined to the Coromandel coast. Saline soils in Tamil Nadu are confined to the Coromandel coast. Vedaranyam has a pocket of saline soil.

However, the tsunami waves on December 26, 2004, brought a lot of sand and deposited it all along the east coast of Tamil Nadu. The tsunami made the coastal areas unsuitable for cultivation to a considerable extent.

Soil Erosion

It is a non-renewable resource, and it is very difficult to replace the soil once it is degraded or washed away.

The factors responsible for erosion are deforestation, overgrazing, urbanisation, and heavy rains and floods.

The problem with soil erosion is affecting the natural vegetation, the rate of ecological succession, and agricultural productivity.

As of now, the Desertification of Tamil Nadu is a major problem. According to the desertification atlas prepared by the ISRO, about 12% of the total geographical area is under desertification and land degradation.

Theni, the Nilgiris, and Kanyakumari are the worst-affected districts where about 12,000 hectares (120 Sq.km) were affected by sand deposition in Theni and Rajapalayam.

Reference

  1. https://agritech.tnau.ac.in/agriculture/agri_soilgroups.html

Seasons in Tamil Nadu with Months (Including Autumn Season in Tamil Nadu)

Autumn season in Tamil is called “இலையுதிர் காலம்”. It occurs between September and October and is one of the six traditional seasons observed in Tamil Nadu.

Tamil Nadu lies to the south of the Tropic of Cancer, which is near the Equator. It receives vertical Sun rays, and the temperature is relatively high throughout the year. The east coast of Tamil Nadu enjoys a tropical maritime climate, and the Bay of Bengal and Indian Ocean influence the climate of the coastal regions.

Tamil Nadu’s climate is relatively hot, and its annual temperature ranges from 18 to 43 degrees Celsius, and its annual rainfall is about 958.5 mm.

Tamil Nadu climate
Tamil Nadu Climate

The East Coast experiences a tropical maritime climate, and the western region has a mountainous climate. The mountainous climate prevails over the Blue Mountains, Anaimalai, and Kodaikanal Hills. These areas have cool and pleasant climates due to thick forests and high altitudes.

“Please check the seasonal fruits in Tamil Nadu with the months“

In the central part of Tamil Nadu, the high temperature is due to the low altitude and distance from the sea. This is the region of climatic variation that exhibits the influence of the coastal and the interior location.

The migration of vertical sun’s rays leads to the formation of different seasons in Tamil Nadu as follows.

Autumn season in Tamil Nadu

The Autumn season in Tamil Nadu starts from September to October. There will be rainy days at the beginning of September, and also there will be bright, hot sunshine. As a result of mild showers, the temperature is down a little bit and paves the way for a cooler winter in the coming months.

This is the best time for tourists to visit Tamil Nadu. Tamil Nadu’s autumn may not be like Europe and the US.

S.No.Geographical LocationsWeather Recording StationsSummer Season (°C)Winter Season (°C)Rainy Season (°C)
1Coastal RegionsChennai40°C22°C25°C
2Interior PlainsVellore42°C21°C22°C
3Inland RegionsThiruchirappalli42°C20°C23°C
4Hilly RegionsKodaikanal11°C6°C14°C
5PlateauCoimbatore32°C26°C21°C
Table: Region-wise seasonal average temperature

Winter Season

Winter Season in Tamil Nadu – Ooty By https://www.flickr.com/photos/sankaracs/ – https://www.flickr.com/photos/sankaracs/3860105606/sizes/l/, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=7685040

Tamil Nadu’s climate during Winter is not the same as Temperate regions like Europe, Northern America, etc. There is no snowfall, just a reduction in temperature. In Tamil Nadu, the winter season comes during January and February. It is due to vertical rays of the Sun falling between the Tropic of Capricorn and the Equator. Thus, India and Tamil Nadu receive slanting Sun rays.

There is less difference between Summer and Winter. The weather is slightly cooler, and the temperature is not very high. The temperature during the winter varies from 15°C to 25°C. However, the Hill station in Tamil Nadu experiences below 5°C occasionally, and also some valleys in the Nilgiris recorded even 0°C. This drop in temperature leads to the formation of thick mist and frost, and the winter season in Tamil Nadu is practically dry.

Summer Season

The temperature of the state starts increasing in the second week of February and gradually increases in the months of March to June. The part of the summer season is known as Agni Nakshatram (Star of Fire) or Kathiri veyyil.

The apparent migration of the sun towards the north during March, April, and May result in the reception of vertical sun rays by South India. Thus, in the summer season in Tamil Nadu, there is a steady rise in temperature from the equator. Hence, Tamil Nadu, located to the south of the Tropic of Cancer, experiences high temperatures.

Generally, the temperature varies from 30°C to more than 40°C. During this season, particularly in the month of May, the southern part of the state receives some rainfall from pre-monsoon showers (Mango/Blossom showers) and some parts experience convectional rainfall.

Southwest Monsoon

The intense heating of the landmass of the north by the sun during March to May creates a well-developed low-pressure system in North India, which draws wind from the Indian Ocean. This results in the formation of the southwest monsoon.

During this Southwest Monsoon season, Tamil Nadu is located in the rain shadow region for the wind, which blows from the Arabian Sea. As a result, Tamil Nadu receives only a meagre rainfall from this monsoon. Rainfall during this season decreases from west to east. Coimbatore plateau receives an average of 50 cm of rainfall.

However, the southern districts like Kanyakumari, Tirunelveli, and The Nilgiris record 50–100 cm of rainfall during this period. The rainfall is scanty in the eastern part of the state.

SeasonsTamil NameTamil Month
Summer (April to August)Ilavenil MuduvenilChitirai, Vaikasi, Aani, Aadi
Rainy (August to December)Khar season, KhulirAvani, Puratasi, Iypasi, Karthigai
Winter (December to April)Mun Pani, Pin paniMarkhazhi, Thai, Masi and Panguni

Northeast Monsoon

The northeast monsoon season begins in October and lasts until mid-December. The high pressure created over Central Asia and the northern part of India becomes the source for the northeast monsoon winds. The apparent migration of the sun from the Tropic of Cancer to the Tropic of Capricorn causes a change in receiving temperature and air pressure during this season.

Sl. NoDistribution of RainfallAmount of RainfallDistricts
1Very Low RainfallBelow 800 mmCoimbatore, Tiruppur
2Low Rainfall800 mm – 1000 mmNamakkal, Karur, Thoothukudi, Erode, Dharmapuri, Madurai, Thiruchirappalli, Perambalur, Krishnagiri
3Moderate Rainfall1000 mm – 1200 mmPudukkottai, Virudhunagar, Sivagangai, Thanjavur, Salem, Ramanathapuram, Dindigul, Theni, Vellore
4High Rainfall1200 mm – 1400 mmTirunelveli, Thiruvannamalai, Kanyakumari
5Very High RainfallAbove 1400 mmKancheepuram, Chennai, Villupuram, Thiruvallur, Thiruvarur, Cuddalore, Nagapattinam, Nilgiris
Rainfall Distribution in Tamil Nadu District-wise (with Data)

It makes the wind blow towards the Bay of Bengal from North India. After reaching the Bay of Bengal, the wind gets deflected by the Coriolis force and takes the northeast direction. Hence, it is known as the northeast monsoon. As the northeast monsoon is a part of the returning southwest monsoon wind, it is also called the retreating monsoon.

This is the main rainy season for Tamil Nadu, accounting for 48% of annual rainfall. Coastal districts of the state get nearly 60% of their annual rainfall, and the interior districts get about 40–50% of the annual rainfall during this season.

Tropical cyclones are common during this season. Cyclones originating from the Bay of Bengal bring heavy rainfall to the eastern coastal regions of Tamil Nadu. More than 50% of the state’s rainfall is received from tropical cyclones during this period, and the east coastal region receives 100 to 200 cm of rainfall.

The rainfall received by the central and northwestern parts is 50–100 cm. Cyclones sometimes disrupt crop cultivation and cause severe damage to life and property.

Please find the summary of the above post in the

SeasonTamil NameMonthsClimate
Autumnஇலையுதிர் காலம்September – OctoberMild showers, slightly reduced temperature, mix of rain and sunshine; transition to cooler season
Winterகுளிர் காலம்January – FebruaryCool and dry climate; temperatures range from 15°C to 25°C; mist and frost in hill areas
Summerகோடை காலம்March – MayHot and dry; temperatures from 30°C to above 40°C; occasional pre-monsoon showers
Southwest Monsoonதென்மேற்கு பருவமழைLow rainfall due to the rain shadow effect; moderate rainfall in western and southern regionsMain rainy season; heavy rainfall, cyclones are common; coastal regions receive high rainfall
Northeast Monsoonவடகிழக்கு பருவமழைOctober – DecemberMain rainy season; heavy rainfall, cyclones common; coastal regions receive high rainfall

References

https://environment.tn.gov.in/assets/report/CCM%20Document.pdf

Blossom showers in India UPSC

Blossom showers in India

Blossom shower or Mango shower is a colloquial term that describes pre-monsoon rainfall. These rains are also called April rains or Summer Showers.

These rains fall across South and Southeast Asia such as India, Cambodia, etc. In India, these rains have significant effects like affecting the growth of Mangoes and Coffee. Usually, this rain occurs from March to April.

In India, it occurs as the result of thunderstorm development over the Bay of Bengal. The other names of this shower are Kaal Baisakhi in Bengal, Bordoisila in Assam, and Cherry Blossom Showers or Coffee Shower in Kerala.

Mango Showers

This shower helps in the ripening of mangoes and is hence called Mango Showers.

The Mango showers are experienced prior to the regular monsoon. It is common in parts of Tamil Nadu, Kerala, and Karnataka. These showers are difficult to predict by the meteorological department.

This rainfall is a conventional type of rainfall that is less effective for crops. This is because of intense drainage, the water has a low capacity to percolate the soil.

The Mango growers in Karnataka, Tamil Nadu will worry if there is long dry weather during this season, as it might affect their harvest of Mango Fruit.

If there is deficient rainfall during March and April, the Mango harvest might get affected in the Urban and rule district of Karnataka around the Bangalore region, Kerala, and Tamil Nadu area nearer to Karnataka.

The mango showers in these regions are around 70mm in April. These regions are famous for mango varieties such as Alphonso, Mallika, Baneshah, Raspuri, Totapuri, Badami, Sendhoora, etc.

Also, this will down the Mango output by at least 25%, as the Mangoes will drop prematurely from the trees. The droop of mangoes from these prematurely is due to the low moisture content in the soil that makes the trees wilt.

Also, the roots of mango trees do not go deep into the soil and as a result, the trees cannot tap water from the below water table.

These pre-monsoon showers in Karnataka, Kerala, and Tamil Nadu that help the ripening of mangoes are called Mango Showers.

Cherry Blossom or Coffee Shower

Coffee Showers in India
Coffee Showers in India By Abdulla Al Muhairi – Flickr, CC BY 2.0, https://commons.wikimedia.org/w/index.php?curid=12186904

It is also called Cherry Blossom or Coffee Shower in Karnataka. It is a local wind that blows in the interior of Karnataka in the hot weather season and this shower is good for coffee cultivation.

This shower is the one that gives a superior taste of the coffee from Coorg (Kodagu), Karnataka. The other regions that benefit from the showers are Chikmagaluru, Hassam, and Wayanad. These regions are known to grow the best variety of Coffee, known as Robusta.

These pre-monsoon showers known as Coffee showers are good for the blossoming of the floral buds of the Coffee plant. Also, the Coffee shower is essential and its delay causes harm to the coffee crop’s quality.

Kalbaisakhi

Kalbaisakhi is a dreaded evening thunderstorm that occurs in West Bengal and Assam. These showers are useful for the cultivation of tea, jute, and rice cultivation. This thunderstorm is called Kalbaisakhi as it occurs in the month of Baisakh, referred to as the month of calamity.

Kalbaisakhi in Assam is referred to as Bardoli Chheerha.

Loo

It is a hot and dry wind, with dust that blows regularly over the plains of North-West India. These winds are oppressive in nature. This blows in the northwestern plains from Punjab to Bihar.

Also between Delhi to Patna.

FAQ

  1. Pre-monsoon rainfall is called in Karnataka?

Pre-monsoon rainfall in Karnataka is known as Mango Showers.

2. Mango shower in which state?

Karnataka, Kerala and Tamil Nadu

Downloads

1.Mango showers in India upsc pdf

2.Mango Shower, Blossom Shower, Nor Westers, Loo upsc pdf

Major tribes in Tamil Nadu

Tribal people are concentrated mainly in the Nilgiris district. Major Tribes in Tamil Nadu are Kodas, Thodas, Irulas, Kurumbas, Badagas, Kattunayakan and Paliyan. They form larger groups and mainly have pastoral work. The tribal population in Tamil Nadu, as per the 2011 census, is 7,94,697.

Tamil Nadu has 38 tribes and sub-tribes. These people depend mainly on forest lands and agriculture.

Toda

Tribes in Tamilnadu - Toda

Men from these tribes are occupied in Milking and grazing with buffalo. Toda’s settlement is known as Munds. These people do not worship any god, and their consciousness is cosmic. Toda live in Nilgiris. The Toda tribe is a small pastoral community that lives on the isolated Nilgiri Plateau of Southern India. They are one of the oldest and most unique tribes in India, with a rich culture and history.

The Toda are traditionally buffalo herders, and their culture revolves around the buffalo. They have a deep understanding of buffalo husbandry and produce a variety of dairy products, including milk, yoghurt, and butter. The Toda also uses buffalo dung as fuel and fertiliser.

The Toda live in small settlements called munds, which are typically located on hill slopes. Their houses are made of bamboo and thatch and have a distinctive half-barrel shape.

The Toda are a matriarchal society, and women play a key role in all aspects of community life. They are responsible for milking the buffaloes, making dairy products, and managing the household finances. Men are responsible for herding the buffalo and performing religious rituals.

The Toda have a rich oral tradition, and their songs, stories, and poems are an important part of their culture. They also have a unique system of writing, which is based on symbols and geometric patterns.

The Toda are a close-knit community, and they have a strong sense of identity. They are proud of their culture and heritage, and they are committed to preserving their traditional way of life.

The Toda tribe is a valuable part of India’s cultural heritage, and their unique way of life is a reminder of the country’s rich diversity.

Badaga

Badaga Tribe in Tamil Nadu
Badaga Tribe in Tamil Nadu By Dinesh Kumar N – Own work, CC BY-SA 4.0, https://commons.wikimedia.org/w/index.php?curid=86775148

They belong to the backward class and are not classified as Tribal. Badaga was an agricultural community with dwellers in the higher plateau of Nilgiris district. They also engaged in tea cultivation and potato growing, and they also have a rich oral tradition of folk tales, songs, and poetry.

They belong to the Shiva Section of the Hindu religion. The Badaga tribe is an ethno-linguistic community living in the Nilgiri district in Tamil Nadu, India. There are over 300 Badaga villages in the district, and the Badagas make up the largest ethnic group in the Nilgiris.

The Badagas have a rich and unique culture. They speak their own language, Badaga, which is a Dravidian language closely related to Kannada. The Badagas also have their own unique customs and traditions, such as their marriage rituals and their festivals.

One of the most important Badaga festivals is the Devva Habba, which is a harvest festival that is celebrated in the month of October. During the Devva Habba, the Badagas thank their gods for a good harvest and pray for a prosperous future.

Badagas Temple in Tamil Nadu

The Badagas are also known for their traditional crafts, such as pottery, weaving, and wood carving. Badaga pottery is particularly famous for its unique designs and colours.

The Badaga tribe are an important part of the Nilgiri Hills ecosystem. They have a deep understanding of the local environment and have developed sustainable agricultural practices that have helped to preserve the region’s natural resources.

The Badagas are friendly and welcoming people, and they are always happy to share their culture and heritage with visitors. If you are ever in the Nilgiri Hills, be sure to visit a Badaga village and experience their unique way of life.

Kota

Kota tribe in Tamil Nadu
Kota tribe in Tamil Nadu By Forbes Watson, John William Kaye – The People of India, Volume 8, published in 1875, Public Domain, https://commons.wikimedia.org/w/index.php?curid=12370705

The Kota tribe is a small indigenous community living in the Nilgiri Hills of Tamil Nadu, India. They are one of the oldest and most unique tribes in India, with a rich culture and history.

The Kota tribe is concentrated in the Tiruchigadi area in the Nilagiri Hills. They are known for Folk dances and are musicians who play at Badaa funerals.

These are engaged in funerals. They are experts in Iron Smiths, Potters, and carpenters. Kota implements elaborate tattoos in order to maintain status in society. The Kotas are traditionally metalworkers, and they are known for their skill in crafting silver jewellery and other metal objects. They also make a variety of pottery, baskets, and other handicrafts.

The Kotas are a matriarchal society, and women play a key role in all aspects of community life. They are responsible for making crafts, managing the household finances, and educating the children. Men are responsible for metalworking and agriculture.

The Kotas have a unique religion that is based on the worship of nature spirits. They believe that the Nilgiri Hills are sacred, and they have a deep respect for the environment.

The Kotas are a close-knit community, and they have a strong sense of identity. They are proud of their culture and heritage, and they are committed to preserving their traditional way of life.

Kurumbas

Kurumba Tribe in Tamil Nadu
Kurumba Tribe in Tamil Nadu By த*உழவன் – Own work, CC BY 3.0, https://commons.wikimedia.org/w/index.php?curid=8247767

They are known for Black Magic and witchcraft. From hunting and Gathering, they changed to working in Tea and Coffee Plantations. They are the only caste in the state with a distinctive language known as the Kurumba Language.

The Kurumbas tribe is one of the six ancient tribal groups in Tamil Nadu. They are believed to be the original inhabitants of the Nilgiri Hills, and they have a rich culture and history.

The Kurumbas are traditionally hunter-gatherers, and they have a deep knowledge of the local flora and fauna. They also collect honey and other forest produce. In recent years, many Kurumbas have also taken up agriculture and cattle rearing.

The Kurumbas are a matriarchal society, and women play a key role in all aspects of community life. They are responsible for gathering food, making handicrafts, and managing the household finances. Men are responsible for hunting, agriculture, and cattle rearing.

The Kurumbas have a unique religion that is based on the worship of nature spirits. They believe that the Nilgiri Hills are sacred, and they have a deep respect for the environment.

The Kurumbas are a close-knit community, and they have a strong sense of identity. They are proud of their culture and heritage, and they are committed to preserving their traditional way of life.

Irula

Irula tribe in Tamil Nadu
Irula tribe in Tamil Nadu By Sankar.s – Own work, CC BY-SA 3.0, https://commons.wikimedia.org/w/index.php?curid=18462059

They occupy the lower slopes and forests of the Nilgiris Hills. They are the second largest tribe after the Badagas tribe and are similar to Kurumbas in character. They produce Honey, fruits, herbs, roots, gums, dyes, etc. They also trade with people in the plains.

They are famous for catching snakes and collecting snake venom.

The Irula tribe is a Dravidian ethnic group inhabiting the Indian states of Tamil Nadu, Kerala and Karnataka. A scheduled tribe, their population in this region is estimated at around 200,000 people. People of Irula ethnicity are called Irula, and speak Irula, which belongs to the Dravidian language family.

The Irulas are mainly concentrated in northern Tamil Nadu: in a wedge extending from Krishnagiri and Dharmapuri districts in the west to Ariyalur and Cuddalore districts in the south and Tiruvallur district in the north. Small populations live in Coimbatore and Nilgiris districts and were classified by Thurston as a different population.

The Irulas are traditionally snake catchers and herbal healers. They have a deep knowledge of snakes and their venom, and they are able to catch and handle snakes with great skill. The Irulas also have a vast knowledge of medicinal plants, and they use this knowledge to treat a variety of ailments.

In recent years, the Irulas have also taken up other occupations, such as agriculture, cattle rearing, and handicrafts. However, they continue to practice their traditional snake-catching and herbal healing skills.

Paliyan

Paliyan tribe in Tamil Nadu
Paliyan tribe in Tamil Nadu By Vdakshinamurthy – Self-photographed, Public Domain, https://commons.wikimedia.org/w/index.php?curid=98732976

The Paliyan, or Palaiyar or Pazhaiyarare, are a group of around 9,500 formerly nomadic Dravidian tribals living in the South Western Ghats.

They’re food-gathering communities. It is believed that the Paliyan tribe belongs to the Palani Hills. They are distributed in the districts of Madurai, Thanjavur, Pudukkottai, Tirunelveli, and Coimbatore.

Paliyar tribes were once nomadic, and now they are more progressive than modern society.

The Paliyan tribe is a Dravidian tribal group living in the southern Western Ghats montane rainforests in South India, especially in Tamil Nadu and Kerala. They are traditionally nomadic hunter-gatherers, honey hunters and foragers. Yams are their major food source.

In the early part of the 20th century, the Paliyans dressed scantily and lived in rock crevices and caves. Most have now transformed into traders of forest products, food cultivators and beekeepers, with some working intermittently as wage labourers, mostly on plantations. They are a Scheduled Tribe.

The Paliyan tribe are a unique and fascinating people with a rich culture and history. They have a deep understanding of the local environment and have developed sustainable practices that have helped to preserve the region’s natural resources.

The Paliyan tribe are also known for their traditional crafts, such as pottery, weaving, and basketry. Their handicrafts are made from natural materials such as bamboo, rattan, and clay.

Conclusion

The Tamil tribes are a valuable part of the Tamil Nadu community, and their unique way of life is a reminder of the country’s rich diversity.

* * All the Notes in this blog, are referred from Tamil Nadu State Board Books and Samacheer Kalvi Books. Kindly check with the original Tamil Nadu state board books and Ncert Books.