East London: its foundation and early development as a port
- Authors: Gordon, B C
- Date: 1932
- Subjects: Smith, Harry George Wakelyn, Sir, 1788-1860 D'Urban, Benjamin, Sir, 1777-1849 Harbors -- South Africa -- East London East London (South Africa) -- History -- 1836-1866
- Language: English
- Type: Thesis , Masters , MA
- Identifier: vital:2606 , http://hdl.handle.net/10962/d1012046
- Description: The flourishing city of East London has received but scant attention from historians. Its importance has been overshadowed by that of Cape Town, Durban and Port Elizabeth, each with a foundation bordering on the romantic. The introduction to this thesis indicates traces of the existence of primitive man in these parts. The historical survey will commence with notices taken of the region by nautical and land expeditions in search of either shipwrecked sailors, or news of native races. The first serious notice of East London taken by the white people came in the time of Sir Benjamin D'Urban who sought a seaport for his new province of Queen Adelaide. Our port was opened in 1836 under the appellation of Port Rex, but faded into temporary insignificance, almost oblivion, with the reversal of Sir. B. D'Urban's frontier policy by Lord Glenelg and the abandonment of the new province in 1837. It was not destined to remain forgotten, for Sir Harry Smith at the end of 1847, saw in the mouth of the Buffalo River the same possibilities as had struck the advisers of Sir B. D'Urban. To him it was the future London of the East, and the connecting link between British Kaffraria and the world outside. From that time East London has grown steadily, and of recent years very rapidly. It is not proposed to carry this survey much beyond 1866 in which year British Kaffraria was annexed to the Cape Colony.
- Full Text:
- Date Issued: 1932
- Authors: Gordon, B C
- Date: 1932
- Subjects: Smith, Harry George Wakelyn, Sir, 1788-1860 D'Urban, Benjamin, Sir, 1777-1849 Harbors -- South Africa -- East London East London (South Africa) -- History -- 1836-1866
- Language: English
- Type: Thesis , Masters , MA
- Identifier: vital:2606 , http://hdl.handle.net/10962/d1012046
- Description: The flourishing city of East London has received but scant attention from historians. Its importance has been overshadowed by that of Cape Town, Durban and Port Elizabeth, each with a foundation bordering on the romantic. The introduction to this thesis indicates traces of the existence of primitive man in these parts. The historical survey will commence with notices taken of the region by nautical and land expeditions in search of either shipwrecked sailors, or news of native races. The first serious notice of East London taken by the white people came in the time of Sir Benjamin D'Urban who sought a seaport for his new province of Queen Adelaide. Our port was opened in 1836 under the appellation of Port Rex, but faded into temporary insignificance, almost oblivion, with the reversal of Sir. B. D'Urban's frontier policy by Lord Glenelg and the abandonment of the new province in 1837. It was not destined to remain forgotten, for Sir Harry Smith at the end of 1847, saw in the mouth of the Buffalo River the same possibilities as had struck the advisers of Sir B. D'Urban. To him it was the future London of the East, and the connecting link between British Kaffraria and the world outside. From that time East London has grown steadily, and of recent years very rapidly. It is not proposed to carry this survey much beyond 1866 in which year British Kaffraria was annexed to the Cape Colony.
- Full Text:
- Date Issued: 1932
Crocidolite in the districts of Prieska and Hay
- Authors: Schoeman, H E
- Date: 1930
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: http://hdl.handle.net/10962/6539 , vital:21133
- Description: From Introduction: The belt of hilly country extending from the southern extremity of the Doornbergen, through Prieska, Niekerkshoop, Griquatown and Kuruman, to a point far north or the latter, constitutes a region or great scientific and economic interest. Spoken of generally as the “Blue Asbestos Belt”, it has ramifications stretching in north, and north-westerly directions from Prieska. In the south it is known as the Doornbergen, passing into the “Asbestos Mountains” north of the Orange River, while farther north it becomes the Kuruman Hills. This large area is unique in that enormous deposits of fibrous crocido1ite or "blue asbestos" are known to occur scattered more or less irregularly over the entire belt. The mineral, often accompanied by some or all of its variations and alteration products, has been reported from nearly every farm, excepting only that portion covered by Ongeluk Volcanics, and the UPPER BEDS OF THE LOWER GRIQUATOWN SERIES, which thus form the only interruption to an otherwise unbroken extension of crocidolite bearing strata.
- Full Text:
- Date Issued: 1930
- Authors: Schoeman, H E
- Date: 1930
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: http://hdl.handle.net/10962/6539 , vital:21133
- Description: From Introduction: The belt of hilly country extending from the southern extremity of the Doornbergen, through Prieska, Niekerkshoop, Griquatown and Kuruman, to a point far north or the latter, constitutes a region or great scientific and economic interest. Spoken of generally as the “Blue Asbestos Belt”, it has ramifications stretching in north, and north-westerly directions from Prieska. In the south it is known as the Doornbergen, passing into the “Asbestos Mountains” north of the Orange River, while farther north it becomes the Kuruman Hills. This large area is unique in that enormous deposits of fibrous crocido1ite or "blue asbestos" are known to occur scattered more or less irregularly over the entire belt. The mineral, often accompanied by some or all of its variations and alteration products, has been reported from nearly every farm, excepting only that portion covered by Ongeluk Volcanics, and the UPPER BEDS OF THE LOWER GRIQUATOWN SERIES, which thus form the only interruption to an otherwise unbroken extension of crocidolite bearing strata.
- Full Text:
- Date Issued: 1930
Clays derived from the Lower Dwyka Shales, occurring in the vicinity of Grahamstown
- Authors: Blignaut, J J G
- Date: 1928
- Subjects: Clay -- South Africa -- Grahamstown Clay -- Economic aspects -- South Africa -- Grahamstown Geology -- South Africa -- Grahamstown Mineralogy -- South Africa -- Grahamstown
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: vital:4935 , http://hdl.handle.net/10962/d1005547
- Description: The Lower Dwyka Shales in South Africa oocur south of latitude 32⁰; resting conformably upon the Witteberg quartzites, which extend as coastal mountain rangee along the length of the South Coast. The shales, being less resistant to weathering than the quartzites below, and the Dwyka Tillite immediately above, are consequently found in valleys between these two formations. In one of these valleys Grahamstown is situated; where the Lower Dwyka Shales have been eroded by the various rivulets forming the eource of the Blaauwkrantz River. A geological map of the country round Grahamstown was prepared in eome detail, showing all the various rock formations occurring in the area, the full extent of the Lower Dwyka Shales being mapped with the Dwyka Tillite and the Witteberg Quartzite along its margins. The map includes an area of about six miles by three, with the Cathedral spire occupying an approximately central position, and is prepared on a scale of 5.65 inches to one mile. Traversing was done by means of prismatic compass and pacing.
- Full Text:
- Date Issued: 1928
- Authors: Blignaut, J J G
- Date: 1928
- Subjects: Clay -- South Africa -- Grahamstown Clay -- Economic aspects -- South Africa -- Grahamstown Geology -- South Africa -- Grahamstown Mineralogy -- South Africa -- Grahamstown
- Language: English
- Type: Thesis , Masters , MSc
- Identifier: vital:4935 , http://hdl.handle.net/10962/d1005547
- Description: The Lower Dwyka Shales in South Africa oocur south of latitude 32⁰; resting conformably upon the Witteberg quartzites, which extend as coastal mountain rangee along the length of the South Coast. The shales, being less resistant to weathering than the quartzites below, and the Dwyka Tillite immediately above, are consequently found in valleys between these two formations. In one of these valleys Grahamstown is situated; where the Lower Dwyka Shales have been eroded by the various rivulets forming the eource of the Blaauwkrantz River. A geological map of the country round Grahamstown was prepared in eome detail, showing all the various rock formations occurring in the area, the full extent of the Lower Dwyka Shales being mapped with the Dwyka Tillite and the Witteberg Quartzite along its margins. The map includes an area of about six miles by three, with the Cathedral spire occupying an approximately central position, and is prepared on a scale of 5.65 inches to one mile. Traversing was done by means of prismatic compass and pacing.
- Full Text:
- Date Issued: 1928