Port Elizabeth in the context of "Internal resistance to apartheid"

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👉 Port Elizabeth in the context of Internal resistance to apartheid

Several independent sectors of South African society opposed apartheid through various means, including social movements, passive resistance, and guerrilla warfare. Mass action against the ruling National Party (NP) government, coupled with South Africa's growing international isolation and economic sanctions, were instrumental in leading to negotiations to end apartheid, which began formally in 1990 and ended with South Africa's first multiracial elections under a universal franchise in 1994.

Apartheid was adopted as a formal South African government policy by the NP following their victory in the 1948 general election. From the early 1950s, the African National Congress (ANC) initiated its Defiance Campaign of passive resistance. Subsequent civil disobedience protests targeted curfews, pass laws, and "petty apartheid" segregation in public facilities. Some anti-apartheid demonstrations resulted in widespread rioting in Port Elizabeth and East London in 1952, but organised destruction of property was not deliberately employed until 1959. That year, anger over pass laws and environmental regulations perceived as unjust by black farmers resulted in a series of arsons targeting sugarcane plantations. Organisations such as the ANC, the South African Communist Party, and the Pan Africanist Congress (PAC) remained preoccupied with organising student strikes and work boycotts between 1959 and 1960. Following the Sharpeville massacre, some anti-apartheid movements, including the ANC and PAC, began a shift in tactics from peaceful non-cooperation to the formation of armed resistance wings.

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Port Elizabeth in the context of Baakens River

The Baakens River, also known as Gqeberha River (Xhosa: [ᶢǃʱɛ̀ɓéːxà]), is a river that empties at Port Elizabeth's city centre and harbour in Algoa Bay.

The river flows for about 23 km (14 mi) from its catchment area at Sherwood, Hunter's Retreat, and Rowallan Park through mainly urban area to its mouth. Mostly, it is a small quiet stream. Near its mouth, it runs into a gorge on the south side of the hill on which Fort Frederick lies.

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Port Elizabeth in the context of Noble Automotive

Noble Automotive Limited, more commonly known simply as Noble, is an English sports car manufacturer based in Leicester. It was established in 1999 by Lee Noble in Leeds, West Yorkshire, for producing high-speed sports cars with a rear mid-engine, rear-wheel drive layout. Lee Noble was the chief designer and part owner of Noble. The company was sold in August 2006. He left the company in February 2008 and shortly after announced his new venture, Fenix Automotive in 2009.

Noble is a low-production English sports car company, its past products include the M12 GTO, M12 GTO-3, M12 GTO-3R and Noble M400. The M12 GTO-3R and M400 share chassis and body, but have minor differences in engines and suspensions. The M15 has a new space frame chassis. The body and chassis of the Noble is built by Hi-Tech Automotive in Port Elizabeth, South Africa alongside Superformance cars. Once the body shell is completed, it is sent to the Noble factory where the engines, transmissions, etc. are added.

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Port Elizabeth in the context of Cape Fold Belt

The Cape Fold Belt (CFB) is a 1,300 kilometres (810 mi) long fold-and-thrust mountain belt along the western and southern coastlines of Western Cape, South Africa. The Cape Fold Belt formed during the Permian period (300 to 250 million years ago) in the late Paleozoic age, affecting the sequence of sedimentary rock layers of the siliciclastic Cape Supergroup with folding and faulted rocks, which were deposited in the Cape Basin in the southwestern corner of South Africa.

The Cape Fold Belt was once part of a larger orogenic belt with other mountain ranges that formed as part of the same tectonic event that originally extended from Argentina, across southern Africa, and into Antarctica. It included the Ventana Mountains near Bahía Blanca in Argentina, the Pensacola Mountains in East Antarctica, the Ellsworth Mountains in West Antarctica, and the Hunter–Bowen orogeny in eastern Australia. The rocks involved in this fold system are primarily sandstones and shales, with shales from the Bokkeveld Group persisting in valley floors, while the more erosion-resistant sandstones of the Peninsula Formation form the parallel ranges of the Cape Fold Mountains. The highest peak in the range is Seweweekspoortpiek, which reaches 2,325 meters.

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