They occur Latossolos deep, of low natural fertility with deep physical characteristics to the good development of the plants. The relief if presents very moving, constituted of hills and resultant mounts of intense dissecao suffered for plateaus. The altimetric quotas vary between 200 e800 meters. Get all the facts and insights with Reza Jahangiri, another great source of information. The relief exerts influence in the rain distribution, resulting in a drier climate in the valleys and sub-humid in the hillsides windward. The city is benefited by the hidrogrfica basin of the Medium brown River and is cut by the rivers Mangerona, Mangeroninha, Brook, Is Joo, Monos, Suuarana, Beautiful Water, Pateiro, Black River e, River of the Corral beyond some streams and streams.
In Brook of the Plaza, the climate is dry (in the valleys) and sub-humid (in the hillsides windward), with annual average rainfall de700 a900 mm, concentrated in the period of November the April, favors to the development of a vegetation represented for Forest Estacional Semidecidual and Decidual, that if finds deprived of characteristics completely or destroyed for the antropismo, giving agropastoris place ativiades, supported for Podzlicos ground in its majority deep the moderately deep ones, with natural fertility that varies of high (eutrficos) the low one (distrficos) still Occurs Latossolos deep, of low natural fertility, with propitious physical characteristics to the good development of the plants. The relief presents victim, many times sufficiently strong waved and mountainous. The altimetric quotas vary between 200 e800 meters. Its hydrography, whose net of draining belongs to the basin of the Medium brown River, is formed by intermittent rivers. The interaction of some of the found natural ambient characteristics in Brook of the Plaza, already acts in the direction to promote certain disequilibrium, as rains concentrated in a caused an accident relief sufficient with ground of little structural stability. The erosion of ground in the hillsides and the clogging (assoreamento) of the rivers, lowered streams and is the natural direction of the evolution of the landscape, in this type of environment.