Question on Indian Events
1) Palni Hills, 2) Nilgiri Hills, 3) Palghat Gap, 4) Annamalai Hills. Know the answer? Add it here! Khushi; Genius. Nilgiri are the hills in India, where Eastern and Western Ghats merge or meet each other. Q The Eastern Ghats and the Western Ghats meet at (A) Nilgiri Hills (B) Cardamom Hills (C) Annamalai Hills (D) Palani Hills. Answer: (A) Nilgiri Hills. Q
In some parts frost is common, and temperatures touch the freezing point during the winter months. It has also been observed that the coldest periods in the South Western Ghats coincide with the wettest.
The heavy, eastward-moving rain-bearing clouds are forced to rise and in the process deposit most of their rain on the windward side. The total amount of rain does not depend on the spread of the area with areas in northern Maharashtra receiving heavy rainfall followed by long dry spells, while regions closer to the equator receive less annual rainfall and have rain spells lasting several months in a year.
The northern portion of the range is generally drier than the southern portion, and at lower elevations makes up the North Western Ghats moist deciduous forests ecoregion, with mostly deciduous forests made up predominantly of teak.
The Eastern and Western Ghats meet in the -
Above 1, meters elevation are the cooler and wetter North Western Ghats montane rain forestswhose evergreen forests are characterised by trees of family Lauraceae. The evergreen forests in Wayanad mark the transition zone between the northern and southern ecologic regions of the Western Ghats. The southern ecologic regions are generally wetter and more species-rich.
At lower elevations are the South Western Ghats moist deciduous forestswith Cullenia the characteristic tree genus, accompanied by teak, dipterocarpsand other trees. The moist forests transition to the drier South Deccan Plateau dry deciduous forestswhich lie in its rain shadow to the east. Above 1, meters are the South Western Ghats montane rain forestsalso cooler and wetter than the surrounding lowland forests, and dominated by evergreen trees, although some montane grasslands and stunted forests can be found at the highest elevations.
The South Western Ghats montane rain forests are the most species-rich ecologic region in peninsular India; eighty percent of the flowering plant species of the entire Western Ghats range are found in this ecologic region. Its inaccessibility made it difficult for people from the plains to cultivate the land and build settlements.
Western Ghats - Wikipedia
After the arrival of the British in the area, large swathes of territory were cleared for agricultural plantations and timber. The forest in the Western Ghats has been severely fragmented due to human activities, especially clear felling for tea, coffee, and teak plantations during to Geography[ edit ] The Eastern Ghats are older than the Western Ghats, and have a complex geologic history related to the assembly and breakup of the ancient supercontinent of Rodinia and the assembly of the Gondwana supercontinent.
- Navigation menu
- Newest Questions
- Select Your Exam
The Eastern Ghats are made up of charnockitesgranite gneisskhondalitesmetamorphic gneisses and quartzite rock formations. The structure of the Eastern Ghats includes thrusts and strike-slip faults  all along its range. Limestonebauxite and iron ore are found in the Eastern Ghats hill ranges.
Where do eastern and western ghats meet? - Quora
The Eparchaean Unconformity of the Tirumala Hills is a major discontinuity of stratigraphic significance that represents an extensive period of erosion and non-deposition. It is seen at the steep natural slopes, road scars and ravines in the Tirumala ghat roads in the Chittoor district of Andhra Pradesh.
At their southern end, the Eastern Ghats form several ranges of low hills. The climate of the higher hill ranges is generally cooler and wetter than the surrounding plains, and the hills are home to coffee plantations and enclaves of dry forest.
The hill station of Yercaud is located in the Shevaroy Hills. The Ponnaiyar and Palar rivers flow from headwaters on the Kolar Plateau eastward through gaps in the Ghats to empty into the Bay of Bengal; the Javadhu Hills lie between the two rivers. There are waterfalls in remote areas, such as the Kiliyur Falls.
Its northern boundaries are marked by the flat Palnadu basin, while in the south it merges with the Tirupati hills. An extremely old system, the hills have been extensively weathered and eroded over the years.