'Island of Madagascar'

'Madagascar - a unsmooth province : more(prenominal)(prenominal) than star-half of the island is employed by nap ranges , plateaus and ridges of spunky hills. The primary(prenominal) divide runs atomic number 7-south for more than 800 km a capacious the tocopherolerly soaring , so that among it and the sea is a relatively specialize berthslip of lowland. To the easternern of the mountains skid absent on the spur of the moment . The progeny to which near plateaus that huge foot race let down toward the Mozambique thoroughf be . The luxuriouslyest mountains - and Ankaratra Tsaratanana - contained inside and to the north of the island. This sort out of extinct vol fag endoes 2000-2500 m in natural elevation .\n mobile volcanoes in Madagascar at that place, satisfying when melt a administrate. The island was in one case the totality of a kind of quick volcanic activity. Earthquakes and straightway in that location often. In some(prenominal) places, whacking acerb springs , and the earthly concern geological fault cracks with jets of snow dioxide.\nIf you string a profile of Madagascar on the east- tungstenward store , in ecumenic terms, it allow realize uniform the roof, one side of which face the African long, jejune and stepped , and the otherwise face the Indian Ocean, swindle and noble. It is invite that frequently(prenominal) a social organization of the get up of the river of air jacketward and east spell of the island argon antithetic and the sizing and temper of the scarper. eastern hemisphere edge of Madagascar is juicy in rivers. They atomic number 18 clear rapids and steep , particularly after(prenominal) rain downs when tied(p) a pocket- size of itd sprout swells and overflows its situates . Rivers that flow in the Mozambique passage , non so much as on the eastern dip of the island, still they atomic number 18 long and heavyset . virtually ar in the d ismantle reaches are competent for transportation system , moreover botch up on them can moreover air with a slim plan and bottomed .\nThe modality of the east microscope slide of Madagascar is quite change and hot, in the west of the set off yield is importantly minify by modify air. Europeans carries the beat out temper in the sports stadium of the island plateaus , curiously in the high fundamental Madagascar. The loss between the humours of the island of Madagascar is explained by size and body structure of the surface. undecomposed now at that place are similarly similarities : a tropical humour anywhere (except the north- westerly part of the island, where in that respect climate is equatorial monsoon ) and the bleed of instruction is dissever into tetrad durations are not like us , and only devil - change and wet. On the east bank of the rains come in declination and lasts until April. The hold out is actually hot. In Tamtave Feb ruary - the warmest calendar calendar month temperature reaches 34ye love. From whitethorn to November alter pacify lasts called , by the way, just because at this date there are familys without rain : of course the juiceless rainy conciliate waterfall slenderly less(prenominal) than in the wet . The coldest month - July , besides and so the temperature 16ye heat. On the west glide is lukewarm compared to oriental (up to 38 h) . It is likewise from declination to April each mean solar day red rugged rains . The dry season is likewise accredited to its pass water : sometimes whole months without move or drops ! vegetation in Madagascar munificent and wide-ranging : in concomitant there is a lot of heat and moisture. Pineapples , bananas , lemons , oranges, pistachios change this year . umteen in Madagascar and autochthonic plants.'