Show simple item record

dc.contributor.advisorXu, Yongxin
dc.contributor.advisorAdams, Shafick
dc.contributor.authorNetili, Khangweleni Fortress
dc.contributor.otherDept. of Earth Science
dc.contributor.otherFaculty of Science
dc.date.accessioned2013-10-24T08:48:35Z
dc.date.available2007/11/06 13:52
dc.date.available2007/11/06
dc.date.available2013-10-24T08:48:35Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/11394/2314
dc.descriptionMagister Scientiae - MScen_US
dc.description.abstractThe Table Mountain Group (TMG) Aquifer is the second largest aquifer system in South Africa, after dolomites. This aquifer has the potential to be a signinficant source of water for the people of the Western Cape. The occurrence of hot water springs in the TMG in relation with the main geological fault systems in SOuth Africa shows that deep flow systmes do exist. Little is known about these deep aquifer systems in South Africa (i.e. flow mechanisms). To close the above-mentioned knowledge gap, this study was initiated. The current study gave a review of some of the aspects that needs to be considered when distinguishing deep groundwater from shallow groundwater.en_US
dc.language.isoenen_US
dc.publisherUniversity of the Western Capeen_US
dc.subjectGroundwater flow - South Africaen_US
dc.subjectAquifers - South Africaen_US
dc.subjectBiotic communities - South Africaen_US
dc.titleA preliminary understanding of deep groundwater flow in the Table Mountain group (TMG) aquifer systemen_US
dc.typeThesisen_US
dc.rights.holderUniversity of the Western Capeen_US
dc.description.countrySouth Africa


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record