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Neil D. Burgess, Paul Harrison, Peter Sumbi, James Laizer, Adam ...

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SPATIAL PLANNING BASELINE: TANZANIA’S COASTAL FORESTS 2011<br />

Figure 13: Forest areas on the Mbwalawala and Uchungwa Plateaux in Kilwa district, also showing<br />

the location of the bioshape biofuel plantation areas (Perkin et al. 2008c – using data provided by<br />

Sokoine University and Conservation International)<br />

3.8 Lindi Landscape<br />

The landscape includes a narrow coastal plain, rising in a series of sandstone ridges that run more or less<br />

parallel to the coast. The lowland areas have deep, leached sandy soils derived from terrestrial sands,<br />

gravels, calcretes and laterites of Miocene to Pleistocene age (Perkin et al. 2008c).<br />

The Rondo, Noto, Chitoa, Mputwa and Likonde plateaus are composed of soft friable Miocene sands and<br />

the smooth tops of these plateaus appear to be remnants of an ancient rolling Miocene surface that is<br />

being eroded away through a process of retreating scarp erosion (<strong>Burgess</strong> and Clarke 2000). Small<br />

patches of forest are located on and around these plateaus, as well as near the coast.<br />

The altitude of the landscape ranges from 0 m-asl at the coast to 900 m-asl on the western side of the<br />

Rondo plateau. The Noto Plateau extends up to 534 m and the Chitoa plateau extends up to 260 m.<br />

Table 14: Summary of forest reserves in the Rondo Landscape<br />

Forest<br />

Reserves<br />

Area Status Altitude<br />

(m)<br />

Vegetation types<br />

Reference<br />

Chitoa 770* CGFR 240-420 Dry evergreen forest, riverine Clarke (1995),

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