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Relevant bibliographies by topics / Molteno Formation (South Africa)

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Dissertations / Theses

Academic literature on the topic 'Molteno Formation (South Africa)'

Author: Grafiati

Published: 4 June 2021

Last updated: 17 February 2022

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Dissertations / Theses on the topic "Molteno Formation (South Africa)"

1

Walters, P. S. "English in Africa 2000 : towards a new millennium : inaugural lecture delivered at Rhodes University." Rhodes University, Grahamstown, 1988. http://hdl.handle.net/10962/d1020747.

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2

Ashton, Eugéne Mark. "The historiography of the formation of the Union of South Africa." Pretoria : [S.n.], 2010. http://upetd.up.ac.za/thesis/available/etd-03102010-183227.

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3

Lester, Alan John. "Conceptualizing social formation : producing a textbook on South Africa." Thesis, University College London (University of London), 1995. http://discovery.ucl.ac.uk/10021574/.

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The ultimate goal of the thesis is the construction of a text, appropriate for student use, on South Africa's social and spatial formation. The first part of the thesis is the most lengthy. It is a sophisticated account of South Africa's historical geography since 1652. This is written in an academic style, not for students, but for a learned readership, and contains some original insights. In itself, it represents an innovative contribution to the literature on South Africa's social development. The second part is a review of existing texts on South Africa's history and geography, written pur

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4

Moodley, Jason Anthony. "Petrogenesis of the Bysteek and Koenap Formation Migmatites, Central Namaqualand." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1001574.

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The Mesoproterozoic rocks of the Bysteek and Koenap Formations of the Arribees Group are exposed within a NW-SE striking antiformal structure comprised of mafic granulites and metapelitic diatexites, and a number of marble and calc-silicate rock layers. The mafic granulites of the Bysteek Formation show a typological variety of anatectic features, including nebulitic, stromatitic mesosomes, melanosomes, quartz syenitic leucocratic vein networks and syenitic pools. Melanosomes consist of hedenbergitic to diopside-rich clinopyroxene (XMg: 0.40), anorthitic plagioclase (An90), with some quartz, m

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5

Busakwe, Nolukholo Sinovuyo. "Stratigraphy and sedimentology of the Msikaba formation in KwaZulu Natal South Coast, South Africa." Thesis, University of Fort Hare, 2015. http://hdl.handle.net/10353/2501.

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The Msikaba Formation is a Late Devonian fluvial and marine succession which outcrops from Hibberdene to Port Edward along the south coast of KwaZulu-Natal Province, South Africa. The Formation is composed of brownish conglomerate at the bottom and white-greyish quartz arenite sequence in the middle and mixed quartz-arenite with feldspathic sandstone in the upper sequence. Previous studies put more emphasis on the correlation of Msikaba Formation with the Natal Group and Cape Supergroup, whereas this study revised the stratigraphy, and also put new insight on the petrography, sedimentary facie

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6

Duncan, Kenneth Foster. "A comparative study of L1 and EFL reading abilities amongst junior primary students using different reading schemes in black schools." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1002628.

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This thesis examines the development of children's reading skills, in both the mother tongue and English as a foreign language, during their first four years of school. It is an attempt to enter the reading world of very young learners in underdeveloped, mainly rural communities in search of practical insights into the teaching of reading in the junior primary classroom. The research focuses specifically on two approaches to reading instruction. The first is the approach traditionally used in black South African schools, characterised by teacher-centredness and rote-recall techniques. The seco

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7

Howarth, David R. "Black consciousness in South Africa : resistance and identity formation under apartheid." Thesis, University of Essex, 1995. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.520285.

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8

Tsikos, Harilaos. "The mineralogy and geochemistry of the Voëlwater banded iron-formation, Northern Cape Province." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1005589.

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Banded iron-formations (BIFs) are chemically precipitated sedimentary rocks in which Fe-rich bands or laminae alternate with Fe-poor ones. They formed within a specific time-span of the geological record. Their occurrence is restricted between 2.3 and 1.9 Ga, and characterises virtually all the major Precambrian-aged sedimentary basins of the world. The Precambrian Transvaal Basin in Griqualand West, South Africa, is noted for its well-developed BIF units. The Kuruman and Griquatown BIFs comprising the Asbesheuwels Subgroup (up to 1000m thick) are the best known and thickest of these. As far a

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9

Francis, Michele Louise. "Soil Formation on the Namaqualand Coastal Plain." Link to the Internet, 2008. http://hdl.handle.net/10019/806.

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10

Becker, Carl. "South African art institutions : their formation and strategy with particular reference to the question of legitimacy." Thesis, Rhodes University, 1993. http://hdl.handle.net/10962/d1007622.

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I have examined the relationship between the art institution and its social base, and the way in which legitimacy is sought and maintained under changing social circumstances. The social pattern of 'avante garde artist' vs. 'philistine public' has tended to be the context within which 20th century art has developed. The consequent disjuncture between the public art institution and its social base was subsequently accepted as the natural condition of Fine Art production. During the 1980's, two significant factors were to influence this 'natural' condition: i) The demise of 'modernism' internati

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