Mount Morrumbala | |
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Highest point | |
Elevation | 1,172 m (3,845 ft) |
Coordinates | 17°26′44.6″S35°23′30.8″E / 17.445722°S 35.391889°E |
Naming | |
Language of name | Portuguese |
Geography | |
Location | Morrumbala District, Zambezia Province, Mozambique |
Mount Morrumbala, also known as Mount Tembe, is a mountain in Morrumbala District of Zambezia Province in central Mozambique.
Mount Morrumbala rises as an isolated massif at western edge of the Morrumbala Plateau. The Morrumbala Plateau reaches over 400 meters elevation, descending gently to the north, more sharply to the south and east, and steeply towards the valley of the Shire River to the west. [1] The Morrumbala escarpment separates the plateau from the Shire and Zambezi lowlands to the west and south. The Shire River valley is a graben, part of the African Rift Valley system.
The mountain's climate is cooler and wetter than the adjacent plateau and lowlands. Moist oceanic air masses moving in from the southeast rise up the mountain slopes and cool, and the moisture in the air condenses and falls as rain, or forms low clouds and morning mists. The windward south and east slopes receive more moisture than the north and west slopes, which are in the rain shadow of the mountain.
The cooler, wetter climate of the mountain sustains several communities of plants and animals, including moist evergreen forests, distinct from the surrounding lowlands.
Mount Morrumbala's montane forests are an inland enclave of the Southern Zanzibar-Inhambane coastal forest mosaic ecoregion, which extends along the more humid coast. The Eastern miombo woodlands ecoregion extends to the east on the Morrumbala Plateau. The Zambezian and mopane woodlands ecoregion lies to the west in the valley of the Shire and Zambezi rivers.
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The Eastern Cascades Slopes and Foothills ecoregion is a Level III ecoregion designated by the United States Environmental Protection Agency (EPA) in the U.S. states of Oregon, Washington, and California. In the rain shadow of the Cascade Range, the eastern side of the mountains experiences greater temperature extremes and receives less precipitation than the west side. Open forests of ponderosa pine and some lodgepole pine distinguish this region from the Cascades ecoregion, where hemlock and fir forests are more common, and from the lower, drier ecoregions to the east, where shrubs and grasslands are predominant. The vegetation is adapted to the prevailing dry, continental climate and frequent wildfire. Volcanic cones and buttes are common in much of the region.
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