Terroir 2004 banner
IVES 9 IVES Conference Series 9 Geological history and landscape of the Coastal wine-growing region, South Africa

Geological history and landscape of the Coastal wine-growing region, South Africa

Abstract

The geology of the Western Cape testifies to the former existence of a late Precambrian supercontinent, its fragmentation, the closure of an ocean between the South African and South American continental precursors (Kalahari and Rio de la Plata cratons), the accumulation of marine sediments and limestones, and their compression during a collision between these cratons. This event took place during assembly of the southern supercontinent of Gondwana, over 500 million years ago. During the Cambrian the landscape of the western and southern parts of the Cape was eroded to form an alluvial plain with granite hills. From the Ordovician to the Carboniferous this plain intermittently subsided. The resultant Agulhas Sea, which at times extended from Vanrhynsdorp in the north to beyond Port Elizabeth in the east, and which was bordered by mountains to the west and north, received considerable volumes of sediment. These sediments were lifted and folded during the Permo-Triassic Cape Orogeny to form the mountains of the Cape Fold Belt, which are capped with erosion-resistant sandstones, whilst softer shales are locally preserved in downfolds.
After Gondwana rifted, a remnant of the Rio de la Plata craton remained attached to South Africa where it underlies the vineyards of the Coastal Region. Erosion was rapid under the warm, wet conditions which prevailed through much of the Cretaceous. By the end of the Cretaceous the main topographic features of the Coastal Region had already been roughed-out. Sculpting of the landscape into its modern form took place during the Tertiary and Quaternary, a time of sub-aerial erosion, pronounced changes in sea level and climatic variation, tending toward increasing aridity. The form of the modern landscape reflects the abilities of the rock structures and materials to resist protracted weathering and erosion.

DOI:

Publication date: January 12, 2022

Issue: Terroir 2004

Type: Article

Authors

J. Wooldridge

ARC Infruitec-Nietvoorbij, Private Bag X5026, 7599 Stellenbosch, South Africa

Contact the author

Keywords

Geology, landscape, South Africa, terroir, vineyard, Western Cape, wine

Tags

IVES Conference Series | Terroir 2004

Citation

Related articles…

EXPLORING RED WINE TYPICITY OF CORBIÈRES: EVALUATION OF THE DEGREE OF IMPACT OF VINIFICATION PROCESS ON THE CHEMICAL COMPOSITION AND ORGANOLEPTIC PROPERTIES OF WINES FROM DIFFERENT TERROIR

It is important nowadays for wine producers to create a product that is an expression of their terroir, a concept including the interaction between a place (topography, climate, soil), the people (tradition, winemaking and viticultural practices) and the resulting product (grape varieties, wines) [1]. Nonetheless, wine’s typicity linked to those terroirs must be easily recognizable by consumers thanks to distinctive sensory characters and composition [2]. Among the compounds of interest, aromatic compounds and polyphenols play an important role in the quality of red wines, by impacting on the odour, color and astringency. To explore the influence of terroir factors, including climate, soil and human practices, on the chemical and sensory profile of wines, red wines from five terroirs of the Corbières appellation were subjected to a general study approach.

Control of microbial development in wines elaborated by carbonic maceration

Carbonic Maceration (CM) winemaking is typically used in different European regions. But It is paradoxical that being a traditional processing system and widely used in many wineries, some of the phenomena that take place and the parameters that characterize them are barely known. In this vinification system the intact grape clusters are placed in a carbon dioxide (CO2) enriched medium, and they immediately change from a respiratory metabolism to an anaerobic fermentative metabolism called intracellular fermentation, which is carried out by grape enzymes. But some grapes located in the lower zone of the tank are crushed by the weight of the ones above and release must, which is fermented by yeasts.

« Wine routes »: a collective brand to build a wine reputation on the basis of terroir and landscapes

Le marché international du vin est désormais tourné vers la qualité et les vignobles de vin de masse se transforment pour construire la qualité et la réputation de leurs produits. Cette construction s’appuie notamment sur la valorisation de ressources territoriales de nature physique (terroir, pacage, écosystème) et humaine (savoir-faire, culture, patrimoine…). Les « Routes des Vins » sont des exemples concrets de ces processus de «territorialisation», combinant ces ressources territoriales pour communiquer sur l’ancrage géographique et la spécificité des vins. Les «Routes des Vins» émergentes, observées dans les régions vitivinicoles en transition vers la qualité, en Languedoc Roussillon, à Mendoza (Argentine) et au Western Cape (Afrique du Sud), participent souvent à la valorisation des terroirs, en organisant un itinéraire sur le territoire associé, en faisant découvrir les vins «de qualité», les paysages, les pratiques et le savoir-faire associés à leur élaboration.

Développement du concept d’Appellation d’Origine Contrôlée et d’Indication Géographique

L’identification des produits par le nom de la ville, de la région, de la province d’origine d’un produit tend aujourd’hui à se développer partout dans le monde et notamment dans le secteur agro-alimentaire, mais aussi dans les secteurs des produits artisanaux.

Environmental and viticultural practice effects on the phenolic composition of grapes: impact on wine sensory properties

Grape phenolic compounds are located in the internal layers of grape skins and seeds. They are synthesized via the phenyl-propanoid biosynthetic pathway which is modulated by both biotic and abiotic factors.