Geology of the Golden Gate Highlands National Park

Koedoe - African Protected Area Conservation and Science

 
 
Field Value
 
Title Geology of the Golden Gate Highlands National Park
 
Creator Groenewald, G.H.
 
Subject — Karoo, Beaufort Group, Molteno Formation, Elliot Formation, vertebrate fossils, Clarens Formation, Drakensberg Formation.
Description The Golden Gate Highlands National Park is underlain by stratigraphic units belonging to the upper part of the Karoo Sequence. These units include part of the Beaufort Group and the Molteno, Elliot, Clarens and Drakensberg Formations. Dolerite dykes and sills are intruded into the succession while recent alluvium and scree cover the valley floors and mountain slopes. The Beaufort Group is represented by red mudstone and light brown fine-grained feldspathic sandstone of the Tarkastad Subgroup. The Molteno Formation consists of medium- to coarse-grained trough cross-bedded sandstone, while the Elliot Formation comprises a thick succession of red mudstone, siltstone and interlayered fine- to medium-grained, light yellow-brown sandstone. The most characteristic feature of the park is the yellowish sandstone cliffs of the Clarens Formation. Cave formation is caused by exudation, differential weathering due to different degrees of carbonate cementation and undercutting of the sandstone. The highest peaks are capped by numerous layers of amygdaloidal and massive varieties of basaltic lava of the Drakensberg Formation. A possible volcanic pipe occurs in the eastern part of the park. The Elliot and Clarens Formations are rich in vertebrate fossil remains, especially Massospondylus sp. Remains of Notochampsa sp., Pachygenelus monus, Clarencea gracilis, Lanasaurus scalpridens and a cluster of unidentified dinosaur eggs have also been found. The formations underlying the Golden Gate Highlands National Park were formed during the Late Triassic Epoch and the Jurassic Period (roughly 150 to 230 million years ago). The strata in the park show very little structural deformation and the only obvious structures are faults which are intruded by dolerite.
 
Publisher AOSIS Publishing
 
Contributor
Date 1986-11-27
 
Type info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion — —
Format application/pdf application/pdf
Identifier 10.4102/koedoe.v29i1.529
 
Source Koedoe; Vol 29, No 1 (1986); 165-181 2071-0771 0075-6458
 
Language eng
 
Relation
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https://koedoe.co.za/index.php/koedoe/article/view/529/555 https://koedoe.co.za/index.php/koedoe/article/view/529/880
 
Coverage — — —
Rights Copyright (c) 1986 G.H. Groenewald https://creativecommons.org/licenses/by/4.0
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