The range of the Western Ghats enabled the Mahrattas to rise against their Mahommedan conquerors, to reassert their Hindu nationality against the whole power of the Mogul Empire, and to establish in its place an empire of their own.
The heaviest falls of rain occur along lines of mountain of some extent directly facing the vapour-bearing winds, as on the Western Ghats of India and the west coast of the Malay peninsula.
The birthplaces of these persons are still known, and to this day there are sequestered villages, nestling near the western base of the Ghats, which are pointed to as being the ancestral homes of men who two centuries ago had political control over half India.
It consists chiefly of an extensive plateau between the Eastern and Western Ghats, of a height varying from Boo to 1000 ft.
The bank of the river is entirely lined with stone, and there are many very fine ghats or landing-places built by pious devotees, and highly ornamented.
In addition to the Melghat mountain tract which walls it in on the north, Berar is divided into two sections, the Payanghat or lowland country, bounded on the north by the Gawilgarh hills, and on the south by the outer scarps of the Ajanta range, and the Balaghat or upland country above the Ajanta ridge, sloping down southwards beyond the ghats or passes which lead up to it.
This gap, which completely intersects the Ghats, is about 20 m.
To the south lies a rolling plateau of basaltic formation (with the sacred town of Multai, and the springs of the river Tapti at its highest point), extending over the whole of the southern face of the district, and finally merging into the wild and broken line of the Ghats, which lead down to the plains.
It is in shape an irregular parallelogram, divided into two nearly equal parts by the range of the Eastern Ghats, which intersects it throughout its entire length.
Again master of all that the Mahrattas had taken from him, and with empire extended to the Kistna, he descended through the passes of the Ghats amid burning villages, reaching Conjeeveram, only 45 m.
Assigning it the more extended of these limits, it comprehends the whole of the Indian peninsula, and in this view the mountainous system, consisting of the Eastern and Western Ghats, constitutes the most striking feature of the Deccan.
The surface of this table-land slopes from west to east, as indicated by the direction of the drainage of the country, - the great rivers, the Cauvery, Godavari, Kistna and Pennar, though deriving their sources from the base of the Western Ghats, all finding their way into the Bay of Bengal through fissures in the Eastern Ghats.
The Godaveri, Kistna and Kaveri all take their rise on the Western Ghats, a region where the rainfall is never known to fail in the monsoon season.
Long., forming a portion of the Western Ghats, after this range has been broken by the Palghat Pass, south of the Nilgiris.
The aspect of the country, in the eastern and southern parts, is flat and uninteresting; but the western parts, where it runs along the foot of the Eastern Ghats, as well as all the country northwards from Trivellam to Tripali and the Karkambadi Pass, are mountainous, with an agreeable diversity of scenery.
The Western Ghats rise to an elevation of 8000 ft.
The Periyar irrigation project conducts water through the ghats in a tunnel to irrigate the Madras district of Madura, for which compensation of Rs.
The eastern and western extremities of the Vindhya Ghats system, and run along the eastern and western coasts of India.
The Eastern Ghats stretch in fragmentary spurs and ranges down the Madras presidency, here and there receding inland and leaving broad level tracts between their base and the coast.
The Western Ghats form the great sea-wall of the Bombay presidency, with only a narrow strip between them and the shore.
In many parts they rise in magnificent precipices and headlands out of the ocean, and truly look like colossal " passes or landing-stairs " (ghats) from the sea.
The Eastern Ghats have an average elevation of 1500 ft.
The Western Ghats ascend more abruptly from the sea to an average height of about 3000 ft.
With peaks up to 4700, along the Bombay coast, rising to 7000 and even 8760 in the upheaved angle which they unite to form with the Eastern Ghats, towards their southern extremity.
On the eastern side of India, the Ghats form a series of spurs and buttresses for the elevated inner plateau, rather than a continuous Eastern mountain wall.
The Western Ghats form, in fact, a lofty unbroken barrier between the waters of the central plateau and the Indian Ocean.
The drainage has therefore to make its way across India to the eastwards, now turning sharply round projecting ranges, now tumbling down ravines, or rushing along the valleys, until the rain which the Bombay sea-breeze has dropped upon the Western Ghats finally falls into the Bay of Bengal.
The peninsula south of the Satpura range consists chiefly of the triangular plateau of the Deccan, terminating abruptly on the west in the Sahyadri range (Western Ghats), and shelving to the east (Eastern Ghats).
This plateau is swept by the south-west monsoon, but not until it has surmounted the western barrier of the Ghats; and hence the rainfall is, as a rule, light at Poona and places similarly situated under the lee of the range, and but moderate over the more easterly parts of the plateau.
At the junction of the Eastern and Western Ghats rises the bold triangular plateau of the Nilgiris, and to the south of them come the Anamalais, the Palnis, and the hills of Travancore.
In the strip of low country that fringes the peninsula below the Ghats the rainfall is heavy and the climate warm and damp, the vegetation being dense and characteristically tropical, and the steep slopes of the Ghats, where they have not been artificially cleared, thickly clothed with forest.
In Lower Burma the western face of the Arakan Yoma hills, like that of the Western Ghats in India, is exposed to the full force of the south-western monsoon, and receives a very heavy rainfall.
On the face of the Western Ghats, and on the Khasi hills, overlooking the Bay of Bengal, where the mountains catch the masses of vapour as it rises off the sea, the rainfall is enormous.
The Bombay monsoon, after surmounting the Ghats, blows across the peninsula as a west and sometimes in places a north-west wind; but it leaves with very little rain a strip 100 to 200 m.
In width in the western Deccan parallel with the Ghats, and it is this part of the Deccan, together with the Mysore table-land and the Carnatic, that is most subject to drought.
The forests, though occasionally very dense, as in the Western Ghats, are usually drier and more open than those of the Malayan type, and are often scrubby.
The hill jungles of the country, in the Western Ghats, in Central India, in Assam, and in Burma.
The coffee tract may be roughly defined as a section of the landward slope of the Western Ghats, extending from Kanara in the north to Travancore in the extreme south.
From 1840 to 1860 the enterprise made slow progress; but since the latter date it has spread with great rapidity along the whole line of the Western Ghats, clearing away the primeval forest, and opening a new era of prosperity to the labouring classes.
It is also the most prevalent and valuable product of the forests at the foot of the Ghats in Bombay, and along the Satpura and Vindhya ranges, as far as the middle of the Central Provinces.
The sandal-wood flourishes all along the southern portion of the Ghats, especially about Mysore and Coorg; and in the same regions, as well as in Upper India, the blackwood occurs.
In name Sivaji was a feudatory of the house of Bijapur, on whose behalf he held the rock-forts of his native Ghats; but in fact he found his opportunity in playing off the Mahommedan powers against one another, and in rivalling Aurangzeb himself in the art of treachery.
Shut off by the line of Decline of the the Ghats from Mahommedan India of that day, they Portu- were able to dominate the petty chiefs of Malabar, guese.
The recognized head of the confederacy was the peshwa of Poona, who ruled the hill country of the Western Ghats, the cradle of the Mahratta race.
Rising in Coorg, high up amid the Western Ghats, in 12° 25' N.
The Bhor Ghat, on the northern border of the state, has always been the main pass over the Western Ghats, or means of communication between the seacoast and the Deccan.
Speaking generally, a range of hills, known as the Western Ghats, runs down the coast, at places rising in splendid bluffs and precipices from the water's edge, at others retreat moun- i n inland, and leavin g a flat fertile strip of to o m.
The Konkan lies between the Western Ghats and the sea.
The streams which, rising in the Sahyadri range, or Western Ghats, flow westward into the Arabian Sea, are of little importance.
One of them, the Sharawati, forcing its way through the western ridge of the Ghats, plunges from the high to the low country by a succession of falls, the principal of which is 890 ft.
The Sahyadri, or Western Ghats, also throw off to the eastward the two principal rivers of the Madras Presidency, the Godavari and the Kistna.
The table-land of the Deccan above the Ghats, on the contrary, has an agreeable climate except in the hot months, as has also the southern Mahratta country; and in the hills of Mahabaleshwar, Singarh, and other detached heights, Europeans may go out at all hours with impunity.
A succession of plateaus descends from the highest ridges on the north to the south, where a series of small ghats march with the nizam's territory.
"above the ghats or passes," the highlands), a district of British India in the Nagpur division of the Central Provinces.