The Pahl fault

dc.contributor.advisor	Coetzee DS	en_US
dc.contributor.advisor	Legnani A	en_US
dc.contributor.author	Roux AJ	en_US
dc.date.accessioned	2013-07-02T14:10:44Z
dc.date.available	2013-07-02T14:10:44Z
dc.date.issued	19980600	en_US
dc.identifier.uri	http://hdl.handle.net/11070.1/4455
dc.description.abstract	Abstract by author:	en_US
dc.description.abstract	Buildings erected on this fault zone prior to the second world war often show renewed signs of settlement. Cracks which are patched periodically tend to reappear. During the construction of the larger buildings in the Central Business District of Windhoek, several minor subsidaries of the Pahl Fault were encountered, and had to be bridged by careful foundation design	en_US
dc.description.abstract	A number of hot springs emanate from the fault. The water is enriched in sulphate and calcium minerals which have caused widespread mineralization of the fault zone. Pyrite is associated with quartz veins, and yellow staining of breccia is caused by elemental sulphur. In spite [of] this, the water pumped from the fault zone has an acceptable quality for general use	en_US
dc.format.extent	43 p	en_US
dc.language.iso	eng	en_US
dc.title	The Pahl fault	en_US
dc.type	thesis	en_US
dc.identifier.isis	F004-199299999999999	en_US
dc.description.degree	Pretoria	en_US
dc.description.degree	South Africa	en_US
dc.description.degree	Technikon Pretoria	en_US
dc.description.degree	B Technology (Geology)	en_US
dc.masterFileNumber	2770	en_US

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