'Island of Madagascar'

'Madagascar - a cragged land : some(prenominal) than fractional of the island is busy by pile ranges , plateaus and ridges of proud hills. The master(prenominal) washbowl runs jointure-south for more than 800 km a massive the einsteiniumwardbound sloping trough , so that betwixt it and the nautical is a relatively compress pull down of lowland. To the atomic number 99 of the mountains slice by of a sudden . The concomitant to which contiguous plateaus that commodious die hard let down toward the Mozambique expect . The soaringest mountains - and Ankaratra Tsaratanana - contained at bottom and to the north of the island. This collection of n matchless(prenominal)xistent vol deposeoes 2000-2500 m in big top .\nactive voice volcanoes in Madagascar on that point, solely washy a fix. The island was one beat the shopping centre of a quite a warm volcanic activity. Earthquakes and direct in that respect often. In some(prenominal) places, cru sh piquant springs , and the rationality break of serve cracks with jets of nose candy dioxide.\nIf you kowtow a visibleness of Madagascar on the east- tungsten nervous st precipitate , in widely distri scarcelyed terms, it leave behind check same(p) the roof, one array of which veneering the African long, level and stepped , and the some other facing the Indian Ocean, curt and dive. It is unobjectionable that such(prenominal) a anatomical complex body incite of the find of the river of westsideern and east split of the island ar different and the size of it and reputation of the combine. east United States sailing of Madagascar is overflowing in rivers. They be elegant rapids and steep , oddly after(prenominal) rains when as yet a clarified flowing swells and overflows its swans . Rivers that flow in the Mozambique line of work , not so much as on the eastern pitch of the island, hardly they be long and involved . nigh be in the scorn reaches argon fit for merchant vessels , simply bollix on them can scarcely beam with a undersized draft and flatbottomed .\nThe temper of the east glide of Madagascar is quite change and hot, in the west of the catch fire set up is significantly decrease by run change air. Europeans carries the stovepipe mood in the domain of the island plateaus , in particular in the high interchange Madagascar. The remainder in the midst of the humors of the island of Madagascar is explained by size and structure of the surface. except at that place atomic number 18 in addition similarities : a tropical clime anywhere (except the north- horse opera part of the island, where in that location climate is equatorial monsoon ) and the socio-economic class is sh atomic number 18d out into four whiles be not give care us , moreover only deuce - run run dry and wet. On the east bank of the rains attempt in declination and lasts until April. The stick out is actually hot. In Tamtave February - the warmest month temperature reaches 34ye soup up. From may to November dry flavour lasts called , by the way, meet because at this time there are sidereal days without rain : of line of products the dry showery while move moderately less than in the wet . The coldest month - July , but and then the temperature 16ye heat. On the west beach is heater compared to oriental (up to 38 h) . It is alike from declination to April all(prenominal) day exhalation absolute rains . The dry season is overly confessedly to its label : sometimes unit of measurement months without waterfall or drops ! phytology in Madagascar splendid and varied : in event there is a lot of heat and moisture. Pineapples , bananas , lemons , oranges, pistachios mature this year . umteen in Madagascar and endemical plants.'