Sentinel Vision EVT-227 South African Great Escarpment 19 April 2018 Sentinel-1 CSAR IW acquired on 30 August 2017 from 17:17:27 to 17:18:42 UTC Sentinel-2 MSI acquired on 03 September 2017 at 08:19:59 UTC ... Se ntinel-1 CSAR IW acquired on 08 September 2017 from 16:53:05 to 16:53:30 UTC Sentinel-3 SLSTR RBT acquired from 04 January 2018 to 07:59:47 UTC Author(s): Sentinel Vision team, VisioTerra, France -
[email protected] 2D Layerstack Keyword(s): Land, mountains, geology, faults, subduction, plateau, orogeny, South Africa Fig. 1 - S2 (03.09.2017) - 11,8,2 colour composite - Zoom on Cape Town region evidencing Table Mountain. 3D view 2D view Table Mountain, Sandstone layers form the ramparts overlying a basement of Precambrian slates and granite - source: Cape Town University Department of Geological Sciences of Cape Town University describes the Geology of the Cape Peninsula: "The late-Precambrian age Malmesbury Group is the oldest rock formation in the area, consisting of alternating layers of dark grey fine-grained greywacke sandstone and slate, seen along the rocky Sea Point and Bloubergstrand shorelines. These sediments were originally deposited on an ancient continental slope by submarine slumping and turbidity currents. The sequence was subsequently metamorphosed by heat and pressure and folded tightly in a NW direction so that the rock layers are now almost vertical. The Peninsula Granite is a huge batholith that was intruded into the Malmesbury Group about 630 million years ago as molten rock (magma) and crystallized deep in the earth, but has since then been exposed by prolonged erosion.