An exploration of ethical conduct in the South African public sector: a case of the Eastern Cape Department of Education
- Authors: Gwanzura, Owen
- Date: 2012
- Subjects: Human capital -- South Africa -- Eastern Cape , Responsibility -- South Africa -- Eastern Cape , Political corruption -- South Africa -- Eastern Cape , Ethics -- South Africa -- Eastern Cape , Fraud -- South Africa -- Eastern Cape , Leadership -- South Africa -- Eastern Cape , Human services -- South Africa -- Eastern Cape , Civil service -- South Africa -- Eastern Cape , Eastern Cape -- South Africa -- Economic conditions , Accountability , Auditor-General , Code of Conduct , Corruption , Eastern Cape Department of Education , Ethical Conduct , Unethical Conduct
- Language: English
- Type: Thesis , Masters , MPA
- Identifier: vital:11672 , http://hdl.handle.net/10353/d1007121 , Human capital -- South Africa -- Eastern Cape , Responsibility -- South Africa -- Eastern Cape , Political corruption -- South Africa -- Eastern Cape , Ethics -- South Africa -- Eastern Cape , Fraud -- South Africa -- Eastern Cape , Leadership -- South Africa -- Eastern Cape , Human services -- South Africa -- Eastern Cape , Civil service -- South Africa -- Eastern Cape , Eastern Cape -- South Africa -- Economic conditions , Accountability , Auditor-General , Code of Conduct , Corruption , Eastern Cape Department of Education , Ethical Conduct , Unethical Conduct
- Description: The Eastern Cape Department of Education has become like a problem child in the Republic of South Africa. It is a cause for concern to both the provincial and national government. This is a department where service delivery is problematic. Schools are not built or renovated and children are taught in dilapidated structures or sometimes under trees. Hardly a week passes without the department making the headlines in the media for the wrong reasons. It is widely accepted that the department is dysfunctional and education is in a crisis. The department has emerged as the number one culprit of engaging in corrupt activities in the province. Public officials in the department have been identified as being at the helm of these corrupt activities. In the 200/10 financial year, the Auditor General issued a disclaimer to the department and highlighted a lack of direction, accountability and a total breakdown of internal control systems and supply chain management within the department. Numerous fraud risk indicators were identified during the audit and underlined by findings that are indicative of fraud and corruption within the department. This unfortunate state of affairs is contrary to the requirements of section 195(1) of the Constitution of the Republic of South Africa which provides for the democratic values and principles governing public administration including inter alia, that: A high standard of professional ethics must be promoted and maintained. Efficient, economic and effective use of resources must be promoted. Public administration must be accountable. This raises several questions about the ethical fitness of public officials in the department as the custodians of the public resources and trust. Though several reasons abound for this unfavourable state of affairs in the department, the researcher has singled out unethical conduct by public officials in the department and its impact on service delivery. The approach followed in this research was to analyse the 2009/10 Department of Education Annual Report and the 2009/10 Auditor General’s Report to the Eastern Cape Department of Education. The analysis confirmed the existence and occurrence of multiple cases of unethical conduct in the department. At the end scientific recommendations are proposed to alleviate this ill.
- Full Text:
- Authors: Gwanzura, Owen
- Date: 2012
- Subjects: Human capital -- South Africa -- Eastern Cape , Responsibility -- South Africa -- Eastern Cape , Political corruption -- South Africa -- Eastern Cape , Ethics -- South Africa -- Eastern Cape , Fraud -- South Africa -- Eastern Cape , Leadership -- South Africa -- Eastern Cape , Human services -- South Africa -- Eastern Cape , Civil service -- South Africa -- Eastern Cape , Eastern Cape -- South Africa -- Economic conditions , Accountability , Auditor-General , Code of Conduct , Corruption , Eastern Cape Department of Education , Ethical Conduct , Unethical Conduct
- Language: English
- Type: Thesis , Masters , MPA
- Identifier: vital:11672 , http://hdl.handle.net/10353/d1007121 , Human capital -- South Africa -- Eastern Cape , Responsibility -- South Africa -- Eastern Cape , Political corruption -- South Africa -- Eastern Cape , Ethics -- South Africa -- Eastern Cape , Fraud -- South Africa -- Eastern Cape , Leadership -- South Africa -- Eastern Cape , Human services -- South Africa -- Eastern Cape , Civil service -- South Africa -- Eastern Cape , Eastern Cape -- South Africa -- Economic conditions , Accountability , Auditor-General , Code of Conduct , Corruption , Eastern Cape Department of Education , Ethical Conduct , Unethical Conduct
- Description: The Eastern Cape Department of Education has become like a problem child in the Republic of South Africa. It is a cause for concern to both the provincial and national government. This is a department where service delivery is problematic. Schools are not built or renovated and children are taught in dilapidated structures or sometimes under trees. Hardly a week passes without the department making the headlines in the media for the wrong reasons. It is widely accepted that the department is dysfunctional and education is in a crisis. The department has emerged as the number one culprit of engaging in corrupt activities in the province. Public officials in the department have been identified as being at the helm of these corrupt activities. In the 200/10 financial year, the Auditor General issued a disclaimer to the department and highlighted a lack of direction, accountability and a total breakdown of internal control systems and supply chain management within the department. Numerous fraud risk indicators were identified during the audit and underlined by findings that are indicative of fraud and corruption within the department. This unfortunate state of affairs is contrary to the requirements of section 195(1) of the Constitution of the Republic of South Africa which provides for the democratic values and principles governing public administration including inter alia, that: A high standard of professional ethics must be promoted and maintained. Efficient, economic and effective use of resources must be promoted. Public administration must be accountable. This raises several questions about the ethical fitness of public officials in the department as the custodians of the public resources and trust. Though several reasons abound for this unfavourable state of affairs in the department, the researcher has singled out unethical conduct by public officials in the department and its impact on service delivery. The approach followed in this research was to analyse the 2009/10 Department of Education Annual Report and the 2009/10 Auditor General’s Report to the Eastern Cape Department of Education. The analysis confirmed the existence and occurrence of multiple cases of unethical conduct in the department. At the end scientific recommendations are proposed to alleviate this ill.
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Sedimentary environments and provenance of the Balfour Formation (Beaufort Group) in the area between Bedford and Adelaide, Eastern Cape Province, South Africa
- Authors: Oghenekome, Monica Enifome
- Date: 2012
- Subjects: Geology -- South Africa -- Balfour , Sedimentary basins -- South Africa -- Eastern Cape , Sediments (Geology) -- South Africa -- Eastern Cape , Sedimentation analysis , Beaufort Group (South Africa)
- Language: English
- Type: Thesis , Masters , MSc (Geology)
- Identifier: vital:11524 , http://hdl.handle.net/10353/d1004354 , Geology -- South Africa -- Balfour , Sedimentary basins -- South Africa -- Eastern Cape , Sediments (Geology) -- South Africa -- Eastern Cape , Sedimentation analysis , Beaufort Group (South Africa)
- Description: The research examines the sedimentary environments and provenance of the Balfour Formation of the Beaufort Group (Karoo Supergroup) in the Eastern Cape Province, South Africa. This Formation occurs in the southeastern part of the Karoo Basin. It consists of sedimentary rocks, which are an alternating siltstone, shale and mudstone succession with subordinate interbedded sandstone and subsequently intruded by Karoo dolerite in the form of sills and dykes. ithostratigraphically, the Balfour Formation is subdivided into five units namely, from the base to the top, the Oudeberg, Daggaboersnek, Barberskrans, Elandsberg and Palingkloof Members. The Balfour Formation is overlain by the Katberg Formation. This study involved field investigations in the vicinity of the towns of Bedford and Adelaide with integrated stratigraphical, sedimentological and petrological studies. A geological map was constructed after field investigations. Lithofacies of the Balfour Formation that were studied are characterised by sandstone facies (Sh, Sm, St, Sr, Sp) and fine-grained sediments (Fl or Fsm) which reflect point-bar, cut-bank, channel and floodplain deposits. Lithologically, the Oudeberg Member consists of sandstone of which some units are internally massive alternating with thin laminated siltstone and mudstone. The Daggaboersnek Member is characterised by regular, generally non-lenticular, overall stratification, in the Barberkrans Member consists of sandstone lithosomes, while the Elandsberg Member is an argillaceous unit, similar to the Daggaboersnek Member. The Palingkloof Member is composed predominantly of red mudstone that can be used to distinguish the Balfour Formation from the overlying Katberg Formation, which consists predominantly of sandstone. The stratigraphic sequence displays two fining upward megacycles of sedimentary deposits with change in the sediment supply pattern from low-sinuosity to high-sinuosity river systems which reflect both braid and meandering deposits, respectively. Sedimentary structures in the sandstone units and the provenance of the Balfour Formation indicate that these deposits were produced by rivers flowing from the southeast with minor drift towards the northwest. According to the composition of the sediments and their sequence of deposition the Formation represents a fluvial environment. Mineralogical and grain size data from the sandstones of the various members of the Balfour Formation indicate the same source area of granitic, metamorphic and older sedimentary rocks and show no significant petrographic differences. The petrographic and geochemical investigations confirmed the sandstone to be feldspathic litharenite and ultralithofeldspathic sandstone. The palaeocurrent investigation indicates the main provenance to have been situated to the southeast of the Karoo basin. Heavy-mineral concentrations within the sandstones also give an indication that the source had a transitional arc plate tectonic setting.
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- Authors: Oghenekome, Monica Enifome
- Date: 2012
- Subjects: Geology -- South Africa -- Balfour , Sedimentary basins -- South Africa -- Eastern Cape , Sediments (Geology) -- South Africa -- Eastern Cape , Sedimentation analysis , Beaufort Group (South Africa)
- Language: English
- Type: Thesis , Masters , MSc (Geology)
- Identifier: vital:11524 , http://hdl.handle.net/10353/d1004354 , Geology -- South Africa -- Balfour , Sedimentary basins -- South Africa -- Eastern Cape , Sediments (Geology) -- South Africa -- Eastern Cape , Sedimentation analysis , Beaufort Group (South Africa)
- Description: The research examines the sedimentary environments and provenance of the Balfour Formation of the Beaufort Group (Karoo Supergroup) in the Eastern Cape Province, South Africa. This Formation occurs in the southeastern part of the Karoo Basin. It consists of sedimentary rocks, which are an alternating siltstone, shale and mudstone succession with subordinate interbedded sandstone and subsequently intruded by Karoo dolerite in the form of sills and dykes. ithostratigraphically, the Balfour Formation is subdivided into five units namely, from the base to the top, the Oudeberg, Daggaboersnek, Barberskrans, Elandsberg and Palingkloof Members. The Balfour Formation is overlain by the Katberg Formation. This study involved field investigations in the vicinity of the towns of Bedford and Adelaide with integrated stratigraphical, sedimentological and petrological studies. A geological map was constructed after field investigations. Lithofacies of the Balfour Formation that were studied are characterised by sandstone facies (Sh, Sm, St, Sr, Sp) and fine-grained sediments (Fl or Fsm) which reflect point-bar, cut-bank, channel and floodplain deposits. Lithologically, the Oudeberg Member consists of sandstone of which some units are internally massive alternating with thin laminated siltstone and mudstone. The Daggaboersnek Member is characterised by regular, generally non-lenticular, overall stratification, in the Barberkrans Member consists of sandstone lithosomes, while the Elandsberg Member is an argillaceous unit, similar to the Daggaboersnek Member. The Palingkloof Member is composed predominantly of red mudstone that can be used to distinguish the Balfour Formation from the overlying Katberg Formation, which consists predominantly of sandstone. The stratigraphic sequence displays two fining upward megacycles of sedimentary deposits with change in the sediment supply pattern from low-sinuosity to high-sinuosity river systems which reflect both braid and meandering deposits, respectively. Sedimentary structures in the sandstone units and the provenance of the Balfour Formation indicate that these deposits were produced by rivers flowing from the southeast with minor drift towards the northwest. According to the composition of the sediments and their sequence of deposition the Formation represents a fluvial environment. Mineralogical and grain size data from the sandstones of the various members of the Balfour Formation indicate the same source area of granitic, metamorphic and older sedimentary rocks and show no significant petrographic differences. The petrographic and geochemical investigations confirmed the sandstone to be feldspathic litharenite and ultralithofeldspathic sandstone. The palaeocurrent investigation indicates the main provenance to have been situated to the southeast of the Karoo basin. Heavy-mineral concentrations within the sandstones also give an indication that the source had a transitional arc plate tectonic setting.
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