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 45<br />
The vegetation is very sparse in this unit <strong>and</strong> fur<strong>the</strong>r monitoring is required to<br />
assess grazing <strong>and</strong> erosion threats. No endemic species are known from this unit.<br />
98.5% of this unit falls within <strong>the</strong> Richtersveld Community Conservancy.<br />
Upper Annisvlakte Succulent Shrubl<strong>and</strong><br />
19180.8018 total ha<br />
2013.2221 ha in Richtersveld Community Conservancy = 10.5%<br />
This shrubl<strong>and</strong> is found in <strong>the</strong> sou<strong>the</strong>rn parts of <strong>the</strong> Annisvlakte north <strong>and</strong> northwest<br />
of <strong>the</strong> Goariep Mountain from near Kuboes to <strong>the</strong> region sou<strong>the</strong>ast of Arrisdrif. The<br />
westernmost section, sou<strong>the</strong>ast of Arrisdrift, is virtually separated from <strong>the</strong> main<br />
area by a northwards moving duneveld of red s<strong>and</strong> (part of Richtersveld Red<br />
Duneveld), which at its nor<strong>the</strong>rn margin fades out to form a shallow s<strong>and</strong> sheet,<br />
which crosses <strong>the</strong> main road between Alex<strong>and</strong>er Bay <strong>and</strong> Khubus. The l<strong>and</strong>scape<br />
is mainly a very wide tilted plain, formed by <strong>the</strong> huge pediment of <strong>the</strong> Goariep<br />
Mountain, towards <strong>the</strong> Orange River. Some river courses are deeply incised into<br />
this plain. On <strong>the</strong> plains, habitats are controlled by soil salinity <strong>and</strong> texture, <strong>and</strong> by<br />
different states of degradation by overgrazing. The granite of <strong>the</strong> Kuboos Pluton of<br />
<strong>the</strong> Cambrian Kuboos-Bremen Suite is largely covered by alluvium loamy s<strong>and</strong>y<br />
gravel soils, mainly derived from granite <strong>and</strong> superficial calcrete deposits. The<br />
altitude ranges from 150 to 500 m.<br />
The predominantly winter rainfall varies between 55 to70 mm per annum. Light frost<br />
is a very rare event, but <strong>the</strong> unit receives sea fog from a southwesterly direction as<br />
well as “Malmokkie” fog. Strong winds to very strong storms occur <strong>and</strong> cause<br />
severe dust <strong>and</strong> s<strong>and</strong> storms with consequentially strong erosion of topsoil material<br />
<strong>and</strong> s<strong>and</strong>blasting.<br />
The present state of <strong>the</strong> vegetation is interpreted as result of strong grazing<br />
pressure over <strong>the</strong> past 100 years. At present, very sparse, dwarf vegetation cover,<br />
mainly Galenia fruticosa, Drosan<strong>the</strong>mum hispidum, Euphorbia gummifera, Galenia<br />
crystalline <strong>and</strong> Psilocaulon subnodosum <strong>and</strong> all indicators of disturbance, is<br />
observed. Ano<strong>the</strong>r indicator of disturbance is <strong>the</strong> high numbers of annuals <strong>and</strong>