Laingsburg, Western Cape
||This article's lead section may not adequately summarize key points of its contents. (August 2014)|
A view of Laingsburg
|• Total||723.72 km2 (279.43 sq mi)|
|• Density||7.8/km2 (20/sq mi)|
|Racial makeup (2011)|
|• Black African||8.2%|
|First languages (2011)|
|Postal code (street)||6900|
The area where the town stands was initially a farm named Vischkuil-aan-de-Buffelsrivier (fishing pond on the Buffalo River).
In the 1870s, the government of Prime Minister John Molteno oversaw a massive expansion of the Cape Colony's railway system. The route (chosen by the Prime Minister with a map, pen and ruler) ran past the farm, which a man called Stephanus Greeff bought for the purpose of development. The line was completed in 1878 and a small siding named Buffelsrivier was built at the farm.
With railway access, a town soon began developing. It was initially renamed Nassau to avoid confusion with Buffalo River in East London, and finally changed to the name Laingsburg, after John Laing[disambiguation needed] who was Commissioner of Crown Lands at the time.
The town is situated in the Great Karoo, a semi-desert region of South-Africa. The town's total rainfall is about 150mm per year. The main water supply is the Buffels River. Summers are extremely hot and dry, with temperatures usually exceeding 30°C. Winters are crisp to sometimes very cold, with snow occasionally occurring in the surrounding region.
On 25 January 1981, in Laingsburg's centennial year, the largest part of the town was swept away within minutes by one of the strongest floods ever experienced in the Great Karoo. After a cloud burst to the north-eastern hinterland, south of the Komsberg, a massive wall of water rushed down the Buffels River and swept away everything it encountered in its way. Animals, humans and their possessions were swept along and later dumped under meters of silt. Archaeologists estimate that such a freak flood can only occur once every 100 years.
Before the flood, rain initially started with a light drizzle that was welcomed by farmers in the area, since it didn't rain often. But, the soil of the area is of such a nature that it can't absorb much rainwater. The consequence is that water drains directly into the rivers. Water built up in both the Baviaans and Buffels Rivers and their confluence at the little town. The rivers quickly grew from normally small streams to a roaring wall of water almost 6 m high. Within hours the whole town was under water and residents had to fight for their lives.