George is the second largest city in the Western Cape province of South Africa. The city is a popular holiday and conference center, as well as the administrative and commercial hub and the seat of the Garden Route District Municipality. It is named after the British Monarch George III.
Prior to European settlement in the late 1700s the area was inhabited by the Khoekhoen tribes: the Gouriquas, Attequas and Outeniquas. Many places in the area, such as the surrounding Outeniqua Mountains, come from Khoekhoen names for these location.
The settlement that was to become George was established as a result of the growing demand for timber and the wood used in building, transport and furniture. In 1777 the Dutch East India Company established an outpost for the provision of timber; its location is thought to be near the western end of York Street. The Timber Post had its own Poshouer (manager), some 12 woodcutters, a blacksmith and a wagon maker with their families, as well as 200 oxen. After 1795 and the British occupation of the Cape, a caretaker of the forests in the area was appointed. After the second British occupation in 1806, it was decided that the Swellendam magistracy was too large and needed to be sub-divided. George was chosen because of the availability of good water.
In 1811 George was declared a separate district and Adrian van Kervel was appointed the first Landrost (magistrate) and the town was proclaimed by the Earl of Caledon, governor of the Cape Colony on St George’s Day, 23 April 1811, and named after the reigning British monarch, King George III. The town’s main street, York Street, was named after King George’s second son Prince Frederick, Duke of York.
One of Van Kervel’s first acts as Landrost (Mayor), was to dig a furrow to supply the first thirty six plots in George with water. An 1819 map shows the original furrows and storage dam where they remain to this day in the Garden Route Botanical Garden. The first Furrow originated from the Rooirivier (Red river) and later a diversionary weir was built in the Camphersdrift River. George gained municipal status on 24 March 1837from the Oudtshoorn side. The track was blasted out of the rock, and seven tunnels were excavated. At one stage some 2 500 workers were employed. During April 1913 this most scenic railway line was completed. Sir David de Villiers Graaff performed the official opening on 6 August 1913. The line was built at the enormous cost of £465 000 (equivalent to £406,300,000[9] or R 7.75 billion in 2020 currency).
The Outeniqua forests were the reason the Dutch East India Company, in 1776, established a woodcutters outpost on the site of what became George in 1811. It was declared a drostdy by the Earl of Caledon on 23 April 1811. George gained municipal status in 1837.
During the construction of the Montagu Pass, in about 1847, a stone toll house, with a thatched roof, was erected on the George side of the mountain. According to a proclamation in the Government Gazette of 24 February 1848, a toll gate was set up, and a tariff of tolls publicized. Upon payment of the prescribed fee the toll keeper would raise the bar across the road to enable the vehicle or animal to pass.
The first toll-keeper was John Kirk Smith, born in Nottingham, England in 1818. During 1849 he collected the amount of £400.13.8p in toll fees. His son William Kirk Smith was appointed toll-keeper in 1880. William and his son made “veldt schoens” (simple leather shoes) at the toll-house for sale to travelers and transport riders. Soon they had a thriving business and J.K. Smith, grandson of the first toll-keeper, expanded this concern to Market Street in George. From this humble beginning grew the large and flourishing shoe industry J.K. Smith and Company, which was the forerunner of Modern Shoes Ltd.
Other early toll-keepers were James Scott (1852) and Charles Searle (1858). The toll-house caught fire on 23 July 1855 and the entire roof was destroyed, later being replaced with corrugated iron. In the Government Gazette dated 16 July 1867, the toll-tariffs were: Each wheel of a vehicle – two pence; Animal drawing a vehicle – one penny; Animal not drawing a vehicle – two pence; Sheep, goat or pig – one halfpenny.
All tolls were abolished on 31 December 1918, but thanks to the fact that it was declared a National Monument in 1970, this interesting relic of the last century has been saved for posterity.
Henry Fancourt White, enchanted by Outeniqualand, bought a portion of the farm Modder River in 1848. He sold a portion to Frances Cook, who named his farm Oaklands, and subdivided the rest into erven. The little village was called ‘Whitesville’ in honor of Henry Fancourt White, but at his suggestion the name was changed to Blanco, the Spanish term for white.
In 1859 Henry White built a beautiful double storey thatched mansion, which he named Blanco House. In 1903 his son Ernest Montagu White renamed the house Fancourt – in honour of his father. Today Fancourt is a National Monument and a well-known hotel.
The main route from Mossel Bay to the Langkloof passed through Blanco, where a settlement of merchants was soon established. The village was also the main postal centre. This caused dissatisfaction among the businessmen of George, and so a direct link from George to the toll-house was built in about 1882. This road was called Bain’s Trace and was probably built by Thomas Bain, who surveyed the new route.
The lakes originated about 20 000 years ago during the Late Pleistocene at the end of the last era of ice ages which was largely centered in the Northern Hemisphere. Consequently, these lakes can be regarded as geologically relatively young. During that last glacial period, the sea-level dropped to about 130 m lower than at present as a result of the accumulation of ice in the Northern Hemisphere.
Rivers then extended into the newly exposed coastal areas, cutting deep valleys into them. At the end of the last glacial period the sea-level rose again, drowning these newly formed valleys until, after a last slight rise and fall of sea-level, a level of about one to three meters above the present level was reached some 6 000 years ago.
The sea level then slowly receded to reach the present level about 4 000 years ago. The partial draining of these valleys exposed part of the coastal area, thereby forming all the present Wilderness Lakes except for Langvlei and Rondevlei. Martin (1962) postulates the Langvlei could have been formed by wave erosion preceding the last rise in sea level while Rondevlei, during the same time, probably originated as a wind-deflating basin. Ruigtevlei, to the east of Swartvlei, was a lake that disappeared, leaving a large area that is only inundated after floods (Martin, 1960). During this last change (drop) in sea level, the mouth of Swartvlei Estuary moved 2 km eastward to the present position at Sedgefield, Groenvlei lost its connection to the sea through the Swartvlei Estuary, and sand dunes now effectively covered any traces of a previous connection to the sea. The city is situated roughly halfway between Cape Town and Port Elizabeth on the Garden Route. It is situated on a 10-kilometre plateau between the Outeniqua Mountains to the north and the Indian Ocean to the south. The former township of Pacaltsdorp, now a fully incorporated suburb, lies to the south.