Sugar Loaf railway station from the train there. Sugar Loaf railway station Sugar Loaf railway station is a railway station in Powys, Wales, and is the most geographically remote station on the Heart of Wales Line. It is located one mile to the north-east of a small but prominent knoll known as Sugar Loaf, around which the A483 road loops. The line through here was opened by the Central Wales Extension Railway in 1868; the station was closed to passengers in 1965 but subsequently reopened to traffic in 1984. This station is a request stop used mainly by trekkers and cyclists, since it is
Sugar Loaf Islands subsequently shifted to Kaitake (580,000 years ago), then migrated southeast to Pouakai (230,000 years ago) and the current centre of activity, Taranaki (last erupted in 1755). The Sugar Loaf Islands are the type locality of taranakite, a phosphate mineral that forms from the reaction of bird guano with the aluminous rocks comprising the islands. This was the first new mineral species to be discovered in New Zealand. Sugar Loaf Islands The Sugar Loaf Islands (often Sugarloaf Islands) () are a collection of five small uninhabited islands and several sea stacks near Port Taranaki, Taranaki, New Zealand. The largest island, Moturoa