Tag Archives: Study in Niger

With no access to the sea, Niger is limited to the SW by the great river that gives it its name. A typical example of a state that arose artificially from the colonial partition and became independent in 1960, Niger corresponds to the former territory of the same name in French West Africa.; it includes to the S a short Sudanese and Sahelian (or sub-Saharan) belt, to the center and to the N a large section properly Saharan. Conditioned by drought, it has an overall desert territory (as much as 86%), with the maximum population concentrated in the southwestern region. Ecologically fragile, Niger also appears devoid of modern communication routes and exportable resources, taking the form of the country that, in the area, is in the most critical conditions. Despite the attempts in the 1970s to get out of underdevelopment thanks to the exploitation of uranium, since the 1980s, the decline in mining revenues has made the country’s economic survival dependent on international aid and the outcome of the negotiations on reducing the foreign debt. According to COUNTRYAAH, Niger is a nation in Western Africa, the capital city of which is Niamey. The latest population of Niger is 24,206,655. REMZFAMILY: Lists and descriptions of main religions and beliefs in Niger, including religion demographics and statistics on Christianity, Islam, Judaism, etc.
GEOGRAPHY
From the morphological point of view, the territory of Niger is not very rugged. Its surfaces are mostly peneplanate and the only reliefs are in the Saharan region, where, almost in the center of the country, the Aïr (or Azbine) massif rises, elevation of the crystalline archaeozoic base whose endogenous activation is due the volcanic formations of the area. The Aïr reaches a maximum height of 2022 m (Idoûkâl-en-Taghès) and is formed by long rocky ridges that stretch towards the underlying paleozoic rock surfaces, to which Mesozoic and Cenozoic sedimentary plateaus yield in the most depressed areas; towards the NE, beyond the vast predominantly sandy region of the Ténéré, one of the most ungrateful in the whole of the Sahara, the ground rises in the plateau (Plateau) of the Djado, continuation of the reliefs of the Fezzan (Libya). The whole of southern Niger is flat, mainly lowering in correspondence with the vast subsidence of Lake Chad to the SE, the depression crossed by the Niger River to the SW. Long fossil valleys, witnesses of a once vigorous hydrography, branch off from the Aïr towards the two aforementioned depressions; among these valleys, morphologically still characterized by traces of erosive activity in a non-arid environment, one of the most marked is that of the Azaouak, which furrows the often pebbly slopes of Talak and tends towards the course of the Niger. Corresponding to these ancient river valleys are the oases, numerous especially in the eastern section (oasis of Bilma, Dirkou, Aney etc.) where there are outcrops of aquifers fed by the Djado plateau. § The hydrographic network, extremely poor, is centered on various uidians, all directed from N to S, whose riverbeds are occupied by waters only at the time of the rains. Roughly half of the territory is included in the endorheic basin of Lake Chad (wadi Dilia and others), on whose northern shores the Niger overlooks; the other half pays tribute to the Niger River, one of the largest African rivers, which however only crosses the country marginally for about 500 km, largely navigable. § The climate varies from S to N in relation to the different penetration of the Atlantic air masses coming from gulf of Guinea and manifests itself, during the summer months, by the loosening of the anticyclonic regime on the Saharan continental surfaces. The two seasons are markedly characterized throughout the country (the dry one goes from October to June, the rainy one affects mainly July and August) but in the Saharan area the rainy season is short and almost insensitive, becoming gradually more relevant towards the S: here rainfall reaches 500 mm annually, decreasing progressively towards N. In northern Niger in certain years there may be no rainfall completely, and in any case there is an irregularity in the rainfall regime that occasionally, perhaps cyclically, determines critical situations in the country. Drought years occurred around 1919 and a difficult period was the recent one, between 1970 and 1973. harmattan, which in winter expires from N and NE. The temperature reaches its highest values ​​in the desert, where the daily temperature variationsare strong; the average is around 28 ºC, but daytime values ​​can easily reach 38 ºC.