Share to: share facebook share twitter share wa share telegram print page

 

Breede River Valley

Breede River Valley is a region of Western Cape Province, South Africa known for being the largest fruit and wine producing valley in the Western Cape, as well as South Africa's leading race-horse breeding area. It is part of the Boland bordering on becoming Little Karoo towards the east.

Geography

Breede River Valley aerial showing intensive viticulture and surrounding mountains

The Breede River Valley is relatively broad and flat for a Western Cape valley, averaging at a floor height of 80m-250m above sea-level. Western regions are mostly alluvial and flat, while eastern regions have more hills of the Bokkeveld Group with narrow alluvial deposits. The valley is framed by the high mountains of the Cape Fold Belt, with the Hex River Mountains and the Skurweberge to the northwest, the Langeberg Mountains (up to 2000m) to the north, the smaller Boland Mountains to the southwest, and the Riviersonderend Mountains to the south. It stretches from Tulbagh in the north to McGregor in the south and Rawsonville in the west to Ashton and Bonnievale in the east. Its namesake, the Breede River, flows through the broad valley as a consequent stream.

The largest town in the valley is Worcester, which lies almost in the centre of the valley, virtually equidistant from Tulbagh in the north and the other major town, Robertson to the south-east. The main north-south rail and road routes traverse the valley, including the N1 highway linking Cape Town and Johannesburg.

It is climatically diverse, however it completely falls within a Mediterranean Climate with most precipitation falling in winter (May through September). Towards the north and west, rainfall approaches upwards of 1000mm p.a., particularly in the Slanghoek Region near Rawsonville, whilst it becomes drier towards the south and west, with most areas averaging 300mm p.a., with areas near Worcester only receiving 175mm p.a. Thus Karoo Shrub dominates eastern hills (particularly the unique Robertson Karoo vegetation type) with lush Fynbos vegetation dominating western regions.

Summers can be very hot, due to its inland location, usually averaging 30 °C from December to March, but sometimes peaking near 40 °C during the hottest of days. This is due to the Du Toitskloof and Riviersonderend Mountains blocking cooling oceanic breezes from reaching the valley. During winter however, the valley is often colder than other seaward regions, like the Overberg. Snow is a regular occurrence on the surrounding mountains; snow does not fall on the valley floor, although light frost does occasionally occur. Spring and Autumn are transitional periods of variable rainfall, occasional light snow on the highest peaks and mild temperatures.

References

33°45′S 19°30′E / 33.750°S 19.500°E / -33.750; 19.500

Kembali kehalaman sebelumnya


Index: pl ar de en es fr it arz nl ja pt ceb sv uk vi war zh ru af ast az bg zh-min-nan bn be ca cs cy da et el eo eu fa gl ko hi hr id he ka la lv lt hu mk ms min no nn ce uz kk ro simple sk sl sr sh fi ta tt th tg azb tr ur zh-yue hy my ace als am an hyw ban bjn map-bms ba be-tarask bcl bpy bar bs br cv nv eml hif fo fy ga gd gu hak ha hsb io ig ilo ia ie os is jv kn ht ku ckb ky mrj lb lij li lmo mai mg ml zh-classical mr xmf mzn cdo mn nap new ne frr oc mhr or as pa pnb ps pms nds crh qu sa sah sco sq scn si sd szl su sw tl shn te bug vec vo wa wuu yi yo diq bat-smg zu lad kbd ang smn ab roa-rup frp arc gn av ay bh bi bo bxr cbk-zam co za dag ary se pdc dv dsb myv ext fur gv gag inh ki glk gan guw xal haw rw kbp pam csb kw km kv koi kg gom ks gcr lo lbe ltg lez nia ln jbo lg mt mi tw mwl mdf mnw nqo fj nah na nds-nl nrm nov om pi pag pap pfl pcd krc kaa ksh rm rue sm sat sc trv stq nso sn cu so srn kab roa-tara tet tpi to chr tum tk tyv udm ug vep fiu-vro vls wo xh zea ty ak bm ch ny ee ff got iu ik kl mad cr pih ami pwn pnt dz rmy rn sg st tn ss ti din chy ts kcg ve 
Prefix: a b c d e f g h i j k l m n o p q r s t u v w x y z 0 1 2 3 4 5 6 7 8 9