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…

Estimation of chemical age of red wines with the use of Fourier transform infrared spectroscopy (FT-IR) and chemometrics

The color of a red wine is one of the most important parameters of its quality, giving much information on its status, such as the grape variety used or the winemaking style. As the result of a complex equilibrium between different forms of anthocyanins and polymerization reactions which occur over the course of time, color can also serve as an indication of a wines’ age. For this purpose the “chemical age” i and ii indexes have been introduced by Somers in 1977. The chemical age index i measures the color absorbance after the addition of acetaldehyde while chemical index ii provides an indication of how much of the total red pigments are resistant to SO2 bleaching.

Produce wines with no quantifiable phytosanitary residues – Impact of washing grapes?

Consumer expectations are increasingly shifting towards “residue-free wines.” However, from an analytical standpoint, “zero” does not exist. Laboratories often use the quantification limits of analysis methods to signify ‘zero.’ Improved techniques now allow for the quantification of levels that were previously undetectable. This is why we prefer to use the term “unquantifiable residue” rather than “absence of residues.”

Time stability of visitors’ preferences for preserving the worldwide cultural landscape alto douro wine region

The Alto Douro Wine Region (ADWR) was classified a world heritage site, specifically as a cultural landscape, by UNESCO, in 2001. The well known “Porto Wine” and other high quality wines are produced in the Douro region. As an attraction and touristic site, the cultural site has to meet the needs of more demanding visitors and to compete with a growing number of cultural sites, also classified by UNESCO. To achieve this goal, landscape managers and public authorities have much to profit from knowing and understanding visitors’ preferences regarding the attributes associated to its outstanding universal value.

Sustainable wine industry: supercritical fluid extraction as key technology for biorefinery enhancement

Supercritical carbon dioxide (sc-CO2) extraction is an environmentally friendly technology employed for bioactive compounds recovery from various natural sources and biomasses. The advantages of sc-co2 extraction include its selectivity, relatively mild operating conditions, which minimize the degradation of sensitive compounds, and the absence of potentially harmful organic solvents.

Determination of aromatic characteristics from Syrah and Tempranillo tropical wines elaborated in Northeast Brazil

Dans la region Nord-Est du Brésil, située à la Vallée du São Francisco, localiséee entre les paralleles 8-9º HS, la production de vins tropicaux a commencé il y a une vigntaine d’années. Dans cette région, il est possible d’avoir au minimum deux récoltes par an, car la moyenne de température est de 26 ºC, avec une pluviosité moyenne de 550 mm entre les mois de janvier-avril.