https://vital.seals.ac.za/vital/access/manager/Index ${session.getAttribute("locale")} 5 https://vital.seals.ac.za/vital/access/manager/Repository/vital:26870 Wed 12 May 2021 23:06:43 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28072 Wed 12 May 2021 20:53:20 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28046 2mm) under BSE imagery were identified, with the abundance of gypsum salts (below surface level) and rock coatings indicating active sulphuric acid weathering, in western Dronning Maud Land, Antarctica. Were mechanical processes faster than chemical, weathering rinds and solution features on silicate rocks would be uncommon in the Antarctic, periglacial landscape. However, this is not the case as the existence of these landforms implies that chemical weathering may occur faster than mechanical weathering processes (Pope et al., 1995). In a changing world, one needs to monitor these processes at a micro-scale in order to fully understand how periglacial environments react to global climatic changes, and the subsequent impacts on these sensitive environments.]]> Wed 12 May 2021 19:32:00 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:27040 Wed 12 May 2021 18:33:38 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28211 Wed 12 May 2021 16:44:41 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:27356 Tue 09 May 2023 15:48:03 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28169 Thu 13 May 2021 03:49:57 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:27791 Thu 01 Sep 2022 09:29:45 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28380 Mon 19 Jul 2021 10:25:41 SAST ]]> https://vital.seals.ac.za/vital/access/manager/Repository/vital:28034 Fri 02 Jun 2023 11:43:09 SAST ]]>