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Chapman's Peak Drive facing southwards.
Chapman's Peak Drive facing southwards.
The official opening of Chapman's Peak Drive, Cape Town, on the 6 May 1922 by Prince Arthur of Conaught.
The official opening of Chapman's Peak Drive, Cape Town, on the 6 May 1922 by Prince Arthur of Conaught.
Chapman’s Peak Dr
Chapman’s Peak Dr
Chapman's Peak Drive. The pass is built on top of a layer of granite, cut into the softer sedimentary rocks above.
Chapman's Peak Drive. The pass is built on top of a layer of granite, cut into the softer sedimentary rocks above.
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View of the Cape Peninsula showing the City of Cape Town and False Bay in the background from the International Space Station, May 2019
View of the Cape Peninsula showing the City of Cape Town and False Bay in the background from the International Space Station, May 2019
The Cape of Good Hope; looking towards the west over Diaz Beach, from the coastal cliffs above Cape Point.
The Cape of Good Hope; looking towards the west over Diaz Beach, from the coastal cliffs above Cape Point.
The courses of the warm Agulhas current (red) along the east coast of South Africa, and the cold Benguela current (blue) along the west coast. Note th
The courses of the warm Agulhas current (red) along the east coast of South Africa, and the cold Benguela current (blue) along the west coast. Note that the Benguela current does not originate from Antarctic waters in the South Atlantic Ocean, but from upwelling of water from the cold depths of the Atlantic Ocean against the west coast of the continent. The two currents do not "meet" anywhere along the south coast of Africa.
Geology of the Cape Peninsula, showing where the Malmesbury Group and Cape Granite rocks and weathered soils are exposed, and overlain by the Cape Sup
Geology of the Cape Peninsula, showing where the Malmesbury Group and Cape Granite rocks and weathered soils are exposed, and overlain by the Cape Supergroup. The hard, erosion resistant Cape Supergroup form the mountains of the Peninsula.