what are the main features of tropical evergreen forest
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(i) The trees reach a great height upto 60 m or even above. Trees are tall, thick and have vigorous growth.
(ii) As the region is warm and wet throughout the year, it has a luxuriant vegetation of all kinds-trees, shrubs and creepers giving it a multilayered structure.
(iii) There is no definite time for trees to shed their leaves, as such these forests appear green all the year round.
(ii) As the region is warm and wet throughout the year, it has a luxuriant vegetation of all kinds-trees, shrubs and creepers giving it a multilayered structure.
(iii) There is no definite time for trees to shed their leaves, as such these forests appear green all the year round.
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Found in the Tropics (23.5° N - 23.5° S) hence called Tropical.
Evergreen, means that they do not shed leaves seasonally like Deciduous trees that they are always green. They occupy about seven per cent of the earth's land surface and habours more than half of the world’s plants and animals. They are also Called as “Selvas”
Stratification: See, they are found in the region where the factors accelerating growth in a forest are in abundance, Moisture and Sunshine.
Rainfall is high and so is the temperature.Take a look at this graph. It is due to the geographical location. It receives max Insolation that results into high rate of evapotranspiration resulting into condensation and eventually precipitation.
Evergreen, means that they do not shed leaves seasonally like Deciduous trees that they are always green. They occupy about seven per cent of the earth's land surface and habours more than half of the world’s plants and animals. They are also Called as “Selvas”
Stratification: See, they are found in the region where the factors accelerating growth in a forest are in abundance, Moisture and Sunshine.
Rainfall is high and so is the temperature.Take a look at this graph. It is due to the geographical location. It receives max Insolation that results into high rate of evapotranspiration resulting into condensation and eventually precipitation.
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