Transport in Lesotho central Lesotho have also been improved, as part of the construction needs of the Lesotho Highlands Water Project. The only railway line in Lesotho is the Maseru branch line, which connects the capital city Maseru to the Bloemfontein–Bethlehem line in the railway network of South Africa. The final of this line, which opened on 18 December 1905, lies within the borders of Lesotho, running from the border bridge on the Mohokare River through the northern industrial district of Maseru to that city's station, the only railway station in the country. As of 2008, there have been talks of building new
Geology of Lesotho only large fault in the country, running northeast-southwest with a vertical displacement of 300 meters near Mafeteng, although there are other smaller faults. More than 50% of Lesotho's territory is underlain by fractured igneous rock aquifers, such as the low permeability basalt of the Lesotho Formation. Dolerite-dike related aquifers have high water productivity in fractures that formed in the surrounding rock due to the high temperature of the intrusion. The sandstones of the Clarens Formation, Elliot Formation and Burgersdorp Formation are small or low quality aquifers, but the Molteno Formation is regarded as the best aquifer in Lesotho with high