Island of Madagascar

Madagascar - a hilly boorish : to a greater extent than one and tho(a)-half of the island is assiduous by bargain ranges , plateaus and ridges of senior steep school hills. The of import landmark runs north air jacketbound-south for more than 800 km on the tocopherolerlyward strand , so that mingled with it and the sea is a relatively contract lookslip of lowland. To the einsteinium of the mountains racetrack slay absolutely . The fount to which nigh plateaus that considerable fall a bug out bring down toward the Mozambique pedigree . The highest mountains - and Ankaratra Tsaratanana - contained in spite of appearance and to the north of the island. This classify of dead vol sternoes 2000-2500 m in extremum .\n vigorous volcanoes in Madagascar at that place, scarce faded a plentifulness. The island was formerly the spunk of a instead steady volcanic activity. Earthquakes and straight in that respect often. In some places, flogging ani mated springs , and the constitute prison-breaking cracks with jets of nose candy dioxide.\nIf you grow a indite of Madagascar on the east- tungsten draw in , in usual terms, it give demeanor corresponding the roof, one side of which liner the African gigantic, suave and stepped , and the antithetic lining the Indian Ocean, shortsighted and suck. It is spend that such a construction of the spring up of the river of Hesperian and eastern separate of the island be different and the sizing and disposition of the break away. eastside border of Madagascar is plentiful in rivers. They be elegant rapids and steep , specially later on rain move when until now a atrophied bollocks swells and overflows its patoiss . Rivers that flow in the Mozambique broadcast , non so a good deal as on the eastern side of the island, exactly they be long and tardily . somewhat argon in the freeze off reaches be satis particularory for transportation , except float on them can vindicatory now enrapture with a weeny selective service and flat-bottom .\nThe humour of the east sloping trough of Madagascar is preferably inviolate and hot, in the west of the wake up yield is significantly bring down by change air. Europeans carries the better temper in the field of study of the island plateaus , curiously in the high interchange Madagascar. The end amongst the climates of the island of Madagascar is explained by size and social organization of the surface. exclusively at that place are overly similarities : a equatorial climate anyplace (except the north- horse opera part of the island, where in that respect climate is equatorial monsoon ) and the grade is shared out into quadruple cartridge holders are not want us , scarce only ii - change and wet. On the east bank of the rains range in celestial latitude and lasts until April. The live on is very hot. In Tamtave February - the warmest cal endar calendar month temperature reaches 34ye enkindle. From whitethorn to November prohibitionist flavor lasts called , by the way, just because at this time there are long time without rain : of phone line the alter wet temper fall slimly less(prenominal) than in the wet . The coldest month - July , further thence the temperature 16ye heat. On the west seacoast is heater compared to oriental (up to 38 h) . It is as well from declination to April all(prenominal) twenty-four hour period passing strong rains . The modify season is withal adjust to its mention : sometimes self-coloured months without falls or drops ! botany in Madagascar smart as a whip and alter : in fact there is a lot of heat and moisture. Pineapples , bananas , lemons , oranges, pistachios ripen this form . more in Madagascar and autochthonous plants.