An examination of the factors influencing the spatial distribution of the Indian communities in Grahamstown, King William's town, Queenstown and Uitenhage from 1880 to 1991
- Authors: Dullabh, Neela
- Date: 1995
- Subjects: East Indians -- South Africa -- Social conditions East Indians -- South Africa -- Economic conditions Apartheid -- Law and legislation -- South Africa
- Language: English
- Type: Thesis , Masters , MA
- Identifier: vital:4831 , http://hdl.handle.net/10962/d1005506
- Description: This study examines the factors influencing the spatial distribution of the Indian communities of Grahamstown, King William's Town, Queenstown and Uitenhage from 1880 to 1991. Primary sources of information were used to determine both the spatial distribution of the four communities and the factors influencing the distribution found. These primary sources included the use of directories, municipal and archival sources of information, interviews as well the work of various authors. The study found that the spatial distribution of Indians in the four study areas were similar with the Indians occupying residential and commercial premises in the central areas of the urban centres. After 1980 there was a substantial movement to other areas. Prior to 1950 the municipalities played an important role in influencing spatial distribution. However, after the introduction of the Group Areas Act, the govennment controlled Indian spatial distribution. Thus the Group Areas Act was the most important factor affecting Indian spatial distribution. Indians in small urban centres in the Cape Province were segregated and their spatial distribution was controlled both prior to and after 1950. Anti-Indian legislation and restrictions were the main factors influencing Indian spatial distribution.
- Full Text:
- Date Issued: 1995
- Authors: Dullabh, Neela
- Date: 1995
- Subjects: East Indians -- South Africa -- Social conditions East Indians -- South Africa -- Economic conditions Apartheid -- Law and legislation -- South Africa
- Language: English
- Type: Thesis , Masters , MA
- Identifier: vital:4831 , http://hdl.handle.net/10962/d1005506
- Description: This study examines the factors influencing the spatial distribution of the Indian communities of Grahamstown, King William's Town, Queenstown and Uitenhage from 1880 to 1991. Primary sources of information were used to determine both the spatial distribution of the four communities and the factors influencing the distribution found. These primary sources included the use of directories, municipal and archival sources of information, interviews as well the work of various authors. The study found that the spatial distribution of Indians in the four study areas were similar with the Indians occupying residential and commercial premises in the central areas of the urban centres. After 1980 there was a substantial movement to other areas. Prior to 1950 the municipalities played an important role in influencing spatial distribution. However, after the introduction of the Group Areas Act, the govennment controlled Indian spatial distribution. Thus the Group Areas Act was the most important factor affecting Indian spatial distribution. Indians in small urban centres in the Cape Province were segregated and their spatial distribution was controlled both prior to and after 1950. Anti-Indian legislation and restrictions were the main factors influencing Indian spatial distribution.
- Full Text:
- Date Issued: 1995
The morphology and sedimentology of two unconsolidated quaternary debris slope deposits in the Alexandria district, Cape Province
- Authors: Illgner, Peter Mark
- Date: 1995
- Subjects: Slopes (Physical geography) -- South Africa , Weathering -- South Africa , Geomorphology -- South Africa
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: vital:4843 , http://hdl.handle.net/10962/d1005519
- Description: Research on hillslope surface processes and hillslope stratigraphy has been neglected in southern Africa. The amount of published literature on hillslope stratigraphy in southern Africa is very limited. Hillslope sediments provide a record of past environmental conditions and may be especially useful in calculating the recurrence interval of extreme environmental conditions such as earthquakes and intense rainfall events. The characteristics of hillslope sediments provide information as to their origin, transport and mechanisms of deposition. No published work could be found that had been undertaken on hillslope surface processes or stratigraphy in the eastern Cape coastal region. This study attempted to fill this gap in the geomorphic literature for southern Africa. The surface processes acting on hillslopes at Burchleigh and Spring Grove in the Alexandria district of the eastern Cape were examined in terms of slope morphology, surface sediment characteristics and the internal geometry of the hillslope sedimentary deposits. The late Quaternary hillslope sedimentary deposits at the two study sites are composed of fine grained colluvial sediments intercalated with highly lenticular diamicts. The fine grained colluvial sediments were emplaced by overland flow processes while the diamicts were deposited by debris flows. The sedimentary sequences at both study sites have a basal conglomerate interpreted as a channel lag deposit. Most slope failures preceding debris flow events were probably triggered by intense or extended periods of rainfall associated with cold fronts or cut-of flows. Seismic events may also have triggered slope failure, with or without the hillslope sediments being saturated. The results of this study indicate that a continuum exists between the slopewash dominated processes of the presently summer rainfall regions of Natal to the present winter rainfall regions of the western Cape where mass movement processes are significant. Hillslope deposits, therefore, provide a record of environmental conditions which may greatly facilitate proper management of the landscape.
- Full Text:
- Date Issued: 1995
- Authors: Illgner, Peter Mark
- Date: 1995
- Subjects: Slopes (Physical geography) -- South Africa , Weathering -- South Africa , Geomorphology -- South Africa
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: vital:4843 , http://hdl.handle.net/10962/d1005519
- Description: Research on hillslope surface processes and hillslope stratigraphy has been neglected in southern Africa. The amount of published literature on hillslope stratigraphy in southern Africa is very limited. Hillslope sediments provide a record of past environmental conditions and may be especially useful in calculating the recurrence interval of extreme environmental conditions such as earthquakes and intense rainfall events. The characteristics of hillslope sediments provide information as to their origin, transport and mechanisms of deposition. No published work could be found that had been undertaken on hillslope surface processes or stratigraphy in the eastern Cape coastal region. This study attempted to fill this gap in the geomorphic literature for southern Africa. The surface processes acting on hillslopes at Burchleigh and Spring Grove in the Alexandria district of the eastern Cape were examined in terms of slope morphology, surface sediment characteristics and the internal geometry of the hillslope sedimentary deposits. The late Quaternary hillslope sedimentary deposits at the two study sites are composed of fine grained colluvial sediments intercalated with highly lenticular diamicts. The fine grained colluvial sediments were emplaced by overland flow processes while the diamicts were deposited by debris flows. The sedimentary sequences at both study sites have a basal conglomerate interpreted as a channel lag deposit. Most slope failures preceding debris flow events were probably triggered by intense or extended periods of rainfall associated with cold fronts or cut-of flows. Seismic events may also have triggered slope failure, with or without the hillslope sediments being saturated. The results of this study indicate that a continuum exists between the slopewash dominated processes of the presently summer rainfall regions of Natal to the present winter rainfall regions of the western Cape where mass movement processes are significant. Hillslope deposits, therefore, provide a record of environmental conditions which may greatly facilitate proper management of the landscape.
- Full Text:
- Date Issued: 1995
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