the richtersveld cultural and botanical landscape - SAHRA
the richtersveld cultural and botanical landscape - SAHRA
the richtersveld cultural and botanical landscape - SAHRA
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Richtersveld Cultural <strong>and</strong> Botanical L<strong>and</strong>scape World Heritage Site Nomination 42<br />
it is restricted to specific geomorphological locations, e.g. limited to <strong>the</strong> pediment<br />
west of <strong>the</strong> main mountains <strong>and</strong> to locations along <strong>the</strong> river beds, which are both<br />
protected against deflation by strong winds, e.g. in <strong>the</strong> Numees area. The small<br />
nor<strong>the</strong>astern part of this area is underlain by granites of <strong>the</strong> Vioolsdrif Suite, <strong>the</strong> rest<br />
occurs on Cenozoic alluvium, aeolian s<strong>and</strong> <strong>and</strong> calcrete; loamy or silty soils, which<br />
are, as a rule, formed by aeolian deposition; not deeper than 40 cm below <strong>the</strong><br />
surface calcrete layers or o<strong>the</strong>r calcium carbonate accumulations. Often <strong>the</strong> soils<br />
also show high salinity. The silt component is subject to local aeolian erosion <strong>and</strong><br />
sedimentation, resulting in erosion in <strong>the</strong> bare areas between <strong>the</strong> bushes <strong>and</strong> silt<br />
deposition underneath <strong>the</strong> bushes - <strong>the</strong>se biogenic mounds regularly attract ants<br />
<strong>and</strong> termites.<br />
Due to <strong>the</strong> wide range of <strong>the</strong> unit, also a wide spectrum of climatic conditions can<br />
be found. The predominantly winter annual rainfall may vary from 50 - 100 mm. Fog<br />
can be important, but not east of <strong>the</strong> V<strong>and</strong>ersterrberge. A few days of frost per year<br />
can occur in <strong>the</strong> units of higher altitude, for instance on <strong>the</strong> Koeroegabvlakte.<br />
Similarly, temperatures can follow a wide spectrum. However, in <strong>the</strong> nor<strong>the</strong>astern<br />
Richtersveld, well developed Scorpionstailveld is seldom found in <strong>the</strong> hotter areas<br />
below an altitude of 330 m.<br />
Brownanthus pseudoschlichtianus (<strong>the</strong> vernacular name, “scorpion’s tail”, referring<br />
to <strong>the</strong> segmented stems) is typically dominant <strong>and</strong> forms low “cussion-like” plants of<br />
1 to 1.5 m in diameter with interspaces of 1 to 3 m. In between <strong>the</strong> plants of B.<br />
pseudoschlichtianus, numerous o<strong>the</strong>r species co-exist, some of <strong>the</strong>m with high<br />
predictability, such as <strong>the</strong> geophyte Trachy<strong>and</strong>ra muricata. Most of <strong>the</strong> Nor<strong>the</strong>rn<br />
Richtersveld Scorpionstailveld is covered by a regular pattern of heuweltjies, which<br />
mostly are inhabited by Mesembryan<strong>the</strong>mum hypertrophicum, M. squamulosum, M.<br />
pellitum <strong>and</strong> Psilocaulon subnodosum.<br />
Aside from <strong>the</strong> Conservancy, 20% of this unit is statutorily conserved in <strong>the</strong><br />
Richtersveld National Park. It is susceptible to grazing pressures <strong>and</strong> more<br />
protection is recommended for this unit.