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Biodiversity (1 - SRK Consulting

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Topography and drainage<br />

The topography is generally flat and open, except for the few quartzite mountains<br />

and, given the low rainfall, recent drainage lines that are relatively lightly incised and<br />

shallow. The area does form part of the palaeo-drainage system of the Gariep River<br />

basin, evident on and around the site as the rather ill-defined Koa River wash(es)<br />

and some of their pans (Figs 2-5). The mountains on site generally have their<br />

steepest and coolest sides facing southwest, into the prevailing wind, and their<br />

warmest and less steep sides facing northeast, with associated effects on the<br />

biodiversity on either side.<br />

Soil<br />

Much of the area is covered in deep (up to 30 cm) red sands, forming scattered<br />

and/or fields of red dunes in places most subject to the prevailing southwest wind<br />

and with structures that impede their movement (Fig. 5). The quartzite gravels occur<br />

in three main forms, small fine-grained patches on the tops and foothills of the<br />

mountains, more variable and widespread sizes around the erosion zones below the<br />

mountains, and small feldspar patches (with pink Hoogoor Suite gneiss evident), with<br />

calcrete gravels also emerging in a few patches where exposed by erosion on the<br />

flats. The effects of the mountains, plus the prevailing winds, result in sand and<br />

dunes accumulating mainly on their southern foothills, or in channels between them,<br />

with more exposed and gravelly plains forming in their northeast lee.<br />

Land Use<br />

The only agricultural land use is livestock grazing at low densities (?about 4 large<br />

stock units (LSU)/100 ha), with sheep, cattle and goats currently present on site. A<br />

few game animals (springbok, ostrich) also occur.<br />

5.3 Vegetation Types<br />

The main vegetation type on site is classified as the Bushmanland Sandy Grassland<br />

vegetation unit (NKb 4), with the isolated mountains creating conditions for the<br />

Aggeneys Gravel Vygieveld (SKr 19, Mucina & Rutherford 2006).<br />

The Khai Ma local municipality (KMLM) lies to the east of the Richtersveld and<br />

contains virtually the entire extent of the Bushmanland Inselberg priority area - one of<br />

the nine zones identified through the SKEP process as important conservation areas<br />

SATO Aggeneys July 2011 27

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