Monsoon
1AD: Men understood the direction of South
West Monsoon, and traders sailed with the South West Monsoon from Western Asia,
Mediterranean area and came to India and South East Area.
They returned with the advent of North-East
Monsoon westward.
thus the discovery of monsoon enabled India
to carry trade and cultural links with Western Asia.
area
|
rainfall (cm)
|
implication
|
Diet
|
Western Gangetic plain
|
37-60
|
Vegetation could be cleared through stone
and copper tools=fit for cultivation and settlement.
Hence 6BC we find the earliest agriculture
settlements here, and trade routes through Terai
|
wheat and Barley
|
Middle Gangetic plains
|
60-125
|
Thicker vegetation. difficult to clear
with stone-copper tools.
|
rice
|
Lower Gangetic plains and Brahmaputra
|
125-250
|
Thick forests. Impossible to clear without
iron tools/axes. But with invention of iron tools- this Assam region was also
contested by kings and emperors during early medieval times.
|
Therefore, natural resources of the Western
area were utilized first, and of eastern area later.
large scale human settlements generally
spread from West to East.
Himalaya
Himalayas protected early civilizations from
the cold Siberian winds. Since cold was not so severe in the plains, Aryan
people could live outdoors for longer periods and did not need heavy clothing.
The great Indus, Ganga and Brahmaputra
plains with most fertile land, natural resources and perennial rivers =gift of
the Himalayas.
The Himalayas form a formidable barrier
against the foreign invasions from the north. This was important during
pre-industrial times when communication was very difficult.
Mountain Passes
There are some important passes in
Himalayas, through which interaction with western, central and northern Asia
has been maintained since time immemorial.
Among these, the use of the Khyber pass was
very frequent and is known as the gateway to India.
since early times there has been a more or
less constant intercourse between East Africa, Arabia, Central Asia and India
maintained by the migrations of herds of mammals
India received large accessions by migration
of the larger quadrupeds from Egypt, Arabia, Central Asia.
Even from the distant North America by way
of land bridges across Alaska, Siberia and Mongolia.
Suleiman ranges could be crossed through
Khyber pass
Kirthar ranges could be crossed through
Bolan Pass.
Through these passes, two-way traffic
between India and Central Asia has been going since pre-historic times.
This helped Irani, Afghani even Soviet
Central Asian invaders and immigrants to come to India.
Valleys
Kashmir Valley was surrounded on all sides
by high mountains, yet could be reached through several passes.
Winter: forced Kashimiris to towards plains
Summer: attached shepherds from plains
towards mountains
This two-way movement facilitated the
exchange of ideas and cultures. Kashmir became the center for cultivation of
Sanskrit. It had the largest number of Sanskrit manuscripts.
Similarly Nepal valley-was accessible to
Gangetic plains through number of passes, and helped in cultural interaction.
Rivers
Rivers in the foothills of Himalaya had
smaller width=easier to cross in the Ancient days when bridge-Architecture was
not developed.
Heart of historical India=Gangetic plains.
It was formed by rivers, swollen through tropical rains and Himalayan snow
melting.
In Ancient times, difficult to construct
roads=men and material moved through rivers.
Even the Ashokan stone pillars were carried
to different parts of India through boats.
in modern times, urban sites developed at
railroad junctions and mining zones (as we saw in geography location factor
articles) but in the ancient times, rivers served as arteries of commerce and
communication. Important cities such as Hastinapur, Prayag, Varanasi,
Pataliputra were situation on the river banks.
bad: they caused heavy floods in northern
plains. Many ancient sites and buildings have been washed away beyond recovery.
Rivers also formed political boundaries in
the ancient-medieval times. For example:
region
|
river boundaries North
|
South
|
Kalinga (Odisha)
|
Mahanadi
|
Godawari
|
Andhra
|
Godawari
|
Krishna
|
Tamilnadu
|
Krishna
|
Kaveri
|
Chola Kingdom
|
South Pennar
|
Vaigai river
|
Maharashtra
|
TApi/Damanganga
|
Bhima
|
Karnataka
|
Bhima/Krishna
|
Tungbhadra
|
Tungbhadra river provided natural frontier
between kingdoms:
made it difficult for Chalukyas and
Rashtrakutas to move southwards and
made It difficult for Pallavas and Cholas to
move northwards.
Eastern Ghats
Eastern Ghats=not very high, and eastward
flow of river caused many oenings. Thus, communication between Andhra-Tamilnadu
was not difficult
Even helped in development of the port
cities of Arikamedu, Mahabalipuram, Kaveripattanam on Coromandal coast
Rajasthan
Area west of Aravalli =Thar desert,
Rajasthan=human settlement difficult.
but South-Eastern part of Rajasthan
=relatively fertile since ancient times + existence of Khetri copper mines.
Hence we can find human settlements here since Chalcolithic period.
Gujarat: Katiawar peninsula=less rain +
Coastal area of Western Gujarat= indented= several harbours. Therefore, since
Ancient times, Gujarat famous for foreign trade.
Madhya Pradesh, Malwa
can be divided into two parts: east and west
Western part including Malwa served as
important hinterland for Gujarat ports. Therefore many wars fought to control
Malwa and Gujarat. (Shaka, Satvahan, Maratha and Rajput)
Mountains and Language Diversity
Each area bound by rivers and mountains +
difficulty in communication=>in course of time, every region grew into
distinct culture, language and lifestyle. But in North and Western India, many
languages derived from same Indo-Aryan stock. And Sanskrit camee to be
cultivated and understood all over the country.
Vindhya mountains formed the boundary
between North and South. Dravidian languages lived south of Vindhya and Aryan
languages lived in North.
But Vindhya didn’t constitute insurmountable
barriers. There was two way trade, migration=>helped in composite culture.
Stones
earliest settlements are found in hilly
areas and river valleys between such hills. Because this region provided all
types of stones for construction and tool making.
Until the invention of burnt brick, the
stones were main construction Material. More temples were made in Stone in
Deccan and South India than in North India.
Bronze
Tin+ Copper=Bronze.
Tin was scarce even in Ancient times. But
there is reason to believe it existed in Rajasthan and Bihar but all used up.
Harappan procured some tin from Rajasthan but main source was Afghanistan.
Because of this scarity Harappen used less bronze than the civilizations of
Asia, Egypt and Crete. Hence India doesn’t have a proper ‘bronze age’.
But during early centuries of Christian era,
India made trade connection with Burma and Malayasia=> tin imported and used
plenty to making bronze status of gold, particularly in South India.
Iron
In South Bihar- East MP and Karnataka
once the art of steel making was known, we
used iron for war, clearaing jungles and regular-deep cultivation.
Formation of Magadh Empire owed much to iron
availability in this region.
Copper
|
Copper of Hazaribagh and Singhbhum=>
helped growth of civilization around Pataliputra.
Khetri-Rajasthan=growth of vedic and
pre-vedic settlements.
Since Copper was the first metal to be
used by Aryans, Hindu rituals usually require copper utensils.
|
Lead
|
Found in Andhra- hence Satavahanas used
lead coins.
|
Silver
|
From Kharagpur hills. used in the earliest
punch marked coins.
|
Gold
|
Kolar-Karnataka. exploitation starts in
2ADHence, Kolar considered to be earliest capital of the South Gangas.
Although much of the gold in early times
was imported from Central Asia and Roman empire.
Since domestic supply of gold low=gold
coins became rare with time.
|
precious stones
|
Odisha, Central and South India. Precious
stones were traded with Romans in early centuries of Christian era.
|
Indian Subcontinent: A Geography
(Keep referring to Map while reading this)
there are six countries in this area:
Afghanistan, Pakistan, Nepal, India, Bhutan and Bangladesh
In ancient times this whole mass of land was
known as Bharatavarsha or Hindustan;
Name Hindustan is derived from river Sindhu,
because westerners pronounced it as Hindu or Indu.
Our constitution uses both names India and
Bharat
Geography
Region
|
Bordered by
|
north
|
Himalyas
|
western and north-western side
|
Pamir plateau and Sulaiman Kirthar ranges
|
western side
|
Arabian Sea
|
eastern side
|
Bay of Bengal
|
Southern borders
|
Indian Ocean.
|
Physically the subcontinent can be studied
in three parts : (i) The Himalayas, (ii) The Indo-Gangetic-Brahmaputra plain
(iii) The Deccan plateau.
The Himalayas
are stretched from Afghanistan in the west
upto Myanmar in the east.
Tibetan Plateau
|
Tibetan plateau forms the northern part of
Himalaya
more than 2,400 Kms long
250 to 320 kms wide.
|
Peaks
|
Himlaya has ~114 peaks which are more than
20,000 feet high. Notable: Gauri Shankar or Everest (the highest mountain in
the world) Kanchanjanga, Dhaulagiri, Nanga Parvat and Nanda Devi.
|
Western Boundary
|
The Hindukush mountains, right from the
Pamirs, form the natural western boundary of the Indian subcontinent.
|
Vs Iran
|
The mountains of Safed Koh, Sulaiman and
Kirthar separate Iran from the Indian subcontinent.
But the large stretches of land to the
west of this line in modern Afghanistan and Baluchistan, like those to the
south and east of the Hindukush, were for long both culturally and
politically parts of India.
|
Eastern Hills
|
Patkoi hills, Naga hills,
Manipur Plateau including the Khasi, Garo
and Jaintia hills.
The Lushai and Chin hills are to the south
of Manipur.
|
Indo-Gangetic-Bramhaputra Plain
To the south of the Himalayas lies the great
plain of India which is more than 3200 kms long and about 240 kms to 320 kms
broad.
It is formed by the solid waste of the
Himalayas brought by hundreds of descending streams.
The alluvium thus formed made the plains
most fertile.
There are three great river systems,
originating from the Himalayas, which supply perennial water to this great
plain.
Indus
Ganga
Brahmaputra.
Saraswati
A big tract of land to the west of Yamuna
and east of Indus in this plain is devoid of any water system at present.
This tract includes the states of Haryana,
Punjab and Rajasthan.
But now it has been proved that in ancient
times the river Saraswati and its tributaries used to flow in this area.
The Sindhu or Indus
rises from the Kailasa Manasarovar area in
the Tibetan plateau,
runs west and north west for about 1300 Kms,
between the Karakoram range.
Then joined by the Gilgit river, it turns
south and reaches the plains where the five rivers join it to form Panchananda
desha or Punjab.
These five tributaries of the Sindhu from
east to west are:
Sutlej (Satudri): was once a tributary of
the lost river Saraswati, but changed its course.
Beas (Vipasa)
Ravi (Parushru)
Chenab (Asikrii)
Jhelum (Vitesta).
Ganga
rising from the Himalayas, reaches the plain
at Hardwar and passes through the states of Uttaranchal, Uttar Pradesh, Bihar
and Bengal, then joins the Bay of Bengal.
In the west of it flows the river Yamuna
also rising from the Himalayas.
Vindhyan rivers
Chambal, the Betwa and the Ken join the
Yamuna before its confluence with the Ganga at Allahabad.
the Son, joins the Ganga near Patna in
Bihar.
From the Himalayas side, rivers like the
Gomati, the Sarayu, the Gandak and the Kosi join the Ganga in the states of
Uttar Pradesh and Bihar.
There are several mouths through which the
Ganga falls into the Bay of Bengal.
The main stream is called Bhagirathi
or Hooghli on which are situated the towns of Murshidabad, Hooghly and Kolkata.
The eastern most mouth of the Ganga is
called the Padma.
Brahmaputra
originating from the eastern part of the
lake Manasarovar in the Kailasa
flows eastward through the plateau of Tibet
under the name of Tsangpo.
Then it turns south and enters in India
where it assumes the name Dihang.
Later, the rivers Dihang and Luhit join and
are called Brahmaputra or Lauhitya.
Passing through Assam and Bengal it joins
the eastern most mouth of the Ganga, i.e., Padma.
But before falling into the Bay of Bengal
another mighty river, the Meghna, joins it.
The delta thus formed is one of the most
fertile part of Bengal and is known as Sundarban delta.
Deccan Plateau and Central India
Peninsular India can be studied under two
distinct sections.
The mountain ranges of the Vindhyas
The mountain ranges of the Satpura
They run parallel to each other from east to
west. In between these two, flows the river Narmada going towards the Arabian
sea.
The only other river flowing towards west is
Tapti, lying a little south of the Satpura.
All other rivers of the Peninsula run from
west to east failing into the Bay of Bengal indicating that the plateau is
titled towards east.
The northern portion of the plateau,
separated by the Vindhya Satpura ranges is known as the Central Indian plateau,
while the southern portion is called the Deccan plateau.
Central Indian Plateau.
stretches from Gujarat in the west to Chhota
Nagpur in the east.
Thar desert, lies to the north of the
Aravalli range.
To the south of it is the Vindhyas, which
rises abruptly from the Narmada side, i.e., south, and has a slopy formation in
the north.
The Maiwa plateau and the tablelands of
Bundelkhand and Baghelkhand are parts of this.
As a result, all the rivers on this side
flow towards north or north-east to join the Yamuna and the Ganga.
The eastern stretches of the Vindhyas, known
as the Kaimur ranges, extend almost up to the south of Banaras and run parallel
with the Ganga up to the Rajmahal hills.
Between the Ganga and the Rajmahal is a
narrow defile or a passage from Chunar in the west (i.e. Mirzapur, U.P.) to Teliagarhi
in the east. This is the only high road, which connects Western and Eastern
India.
Its strategic importance from the military
point of view was fully understood which is evident by the presence of hill
forts of Rohtas and Chunar in the east and Kalijar and Gwalior in the west.
It is said that the passes of Shahabad and
Teliagarhi, situated at a distance of only about five kilometers from each
other, served as the gateway to Bengal.
Western Side of Central Indian Plateau
Gujarat having several low hills and watered
by a number of rivers like Mahi, Sabarmati, and lower courses of Narmada and
Tapti.
The Kathiawar peninsula and the Rann of
Kutch are marshy and dry during the hot season.
Deccan Plateau
the surface of the Deccan plateau slopes
down from west to east.
On the western side lies a range of high
cliffs running south to north leaving a narrow strip of plain between it and
the sea. It is called the Western Ghats- rises up to 3,000 feet.
The plateau is higher in the south being
about 2000 feet in the Mysore region and about half of that in the Hyderabad.
The Eastern Ghats, consisting of groups of
low hills, is marked by several gaps through which many peninsular rivers join
the Bay of Bengal.
The hills going southwards gradually
receding from the sea turn westward to join the Western Ghats at the Nilgiri.
The plain between Eastern Ghats and the sea
is wider than that of Western Ghats.
Except the Narmada and the Tapti, which run
towards west and join the Arabian sea, all the rivers of the Peninsular India
run from west to east.
Most of them rise from the Western Ghat and
traversing the whole breadth of the plateau, fall in the Bay.
The Mahanadi forms a broad plain known as
the Chattisgarh plain in the northeast. It passes through Orissa before joining
the sea.
The valley of Godavari with its tributaries,
has a large flat land in the north but it narrows in the east before meeting
the sea.
Further south, the Krishna, with its
tributaries like the Tungabhadra, divide the Deccan plateau into two sections.
Further south, the Kaveri and its
tributaries form another important river system.
Vs. Northern Rivers
Southern Rivers are devoid of a perennial
water source like the Himalayas,
these southern rivers are mostly dry during
the hot season,
hence less valuable for irrigation and
navigation purposes.
The Coastal Regions
The fertile coastal plains provide
opportunities for maritime activities and trade.
The western coastal plain stretches from the
Gulf of Cambay in the north to Kerala in south.
Northern Part
|
Konkan
|
Southern Part
|
Malabar
|
The rainfall in this region is very high.
There are no big rivers but smaller rivers provide easy communication and
irrigation.
There are some good harbours in the Konkan
region and also in the Malabar.
On the other hand the eastern coast has a few
natural harbours but during the historical period maritime activities lead to
more vigorous and fruitful contacts with the south-east Asian countries.
The southern tip of the peninsula is known
as Cape Comorin or Kanyakumari.
To its south-east is the island of Sri
Lanka. An almost continuous chain of islands and shoals connect India with
SriLanka are called Adam’s Bridge.
The mango shaped island was known in ancient
times by the name of Tambaparni, a corrupt word from Sanskrit Tambraparni,
i.e., having a look or shape of tambula or betel leaf. It was also known as Simhaladvipa.
Climate
The Indian subcontinent is situated mostly
in the tropical zone.
Himalayas guard us from the cold arctic
winds from Siberia, hence we have a fairly warm climate throughout the year.
regular six ritus of two months each and
three seasons of four months.
March-June
|
Hot, temperature goes up to 48° C or more
in some regions.
|
Jul-Oct
|
Rainy season for four months, due to
south-west monsoon. important for the Kharif crops
|
Winter
|
Western disturbances in the winter gives
rise to the second crop of the year called the Rabi during winter season.
|
Rainfall variation
Haryana and Rajasthan including parts of
Sind and Gujarat
|
In modern times these regions receive less
rainfall. But the evidence show that in ancient times it received higher
rainfall and hence the Harappan civilization flourished in this region.
|
northern portion of the Indus region and
the whole of the Ganga plain
|
100-200cm
|
North Eastern
|
200-400 cm. or even more
|
Indian Geography in Ancient Literature
Achaemenid Persians
|
used the name ‘India’ first time, for the
region watered by Sindu river.
In their books Mehre Yasht and Yasna, we
actually find the word Hindu in place of Hafta-Hendu, indicating the
extension of the name to the land beyond the territory of the Indus.
|
Parasis
|
book: Zend Avesta.
Used the name “Sapta Sindhu” referring to
the region of the seven rivers of the Saraswati (or five streams of the
Saraswati together with the Ganges and the Jamuna)
|
Greeks
|
Borrowed the name “Sindu” from Persians.
But pronounced it “Indos”.
Herodotus, the famous Greek historians,
used the term ‘Indos’ to the kshatrapy of the Persian Empire, but gradually
it was extended to the whole country both by Greek and Roman writers.
|
Chinese
|
Buddism introduced in 1st
Century AD in China
Chinese called India as “Tien-Chu” or
Chuantu.
But after Hiuen-Tsang, they started
calling India as “Yin-Tu”.
I-tsing said “Hindu is the name used
only by the northern tribes, and the people of India themselves do not know
it”.
I-tsing used two more names “Arya-desa”
and “Brahmarashtra”
|
Corrupt forms of the word “Sindhu” river:
Persians
|
Hindu
|
Greek
|
Indos
|
Hebrew
|
Hoddu
|
Latin
|
Indus
|
Chinese
|
Tien-Chu / Yin-Tu
|
Within Indian Literature
Panini (6th Cent.BC)
|
first definite mention of Bharata as a
region. But for him Bharata was only one out of 22 janapadas specified from
Kamboja to Magadha, all in Northern India.
|
Buddhist literature
|
speaks of seven Bharata regions
(Sapta-Bharatas) corresponding to the ancient Sapta-Sindhu. and were other
names of India mentioned by
|
Patanjali (150 B.C.)
|
used the term Aryavarta for northern part
of India lying between the Himalayas and the Pariyatraka or the western part
of the Vindhyas.On the west it was bounded by the Adarsavali or Aravalli and
on the east by the Kalakavana or the Rajmahal Hills.
|
Puranas define Bharatvarsha as:
the country that lies north of the ocean
(i.e. the Indian Ocean)
south of the snowy mountains (Himalayas)
formed the southern part of Jambu-dvipa.
marked by the seven mountains chains, viz.
Mahendra, Malaya, Sahya, Suktimat, Riksha (mountains of Gondwana), Vindhya, and
Pariyatra (western Vindhyas up to the Aravallis);
where dwell the descendants of the Bharatas,
with the Kiratas living to its east, the Yavanas (Ionians or Greeks) to its
west,
its own population consisting of the
Brahmans, Kshatriyas, Vaisyas, and Sudras (i.e. the Hindus).
But the name Bharatavarsha is not a mere
geographical expression like the term India. It has historical significance,
indicating the country of the Bharatas, made up of seven sacred rivers and
cities:
7 rivers
|
7 cities
|
Ganga
Yamuna
Godavari
Saraswati
Narmada
Sindhu
Kaveri
|
Ayodhya
Mathura
Maya (modern Hardwar)
Kasi
Kanchi (Conjeeveram)
Avantika (Ujjain)
Dvaravati (Dwarka)
|
This was further sustained by the peculiar
Hindu institution of pilgrimage. Each of the principal Hindu faiths like
Vaishnava, Saiva, or Sakta and other sects have their own list of holy places.
And these are spread throughout the length and breadth of India and not
confined to a single province.
In the same spirit, Sankara established his
four Mathas (religious schools) at the four extreme points of the country viz.
NORTH
|
Jyotirmatha near BadriKedar on the
Himalayas
|
WEST
|
Saradamatha at Dwarka in the west
|
EAST
|
Goverdhana matha at Puri
|
WEST
|
Sringeri matha in Mysore.
|
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