Kingston is a town in the Shire of Hepburn, Victoria, Australia. At the 2021 census, Kingston had a population of 190.
Geology The geology of the Kingston area comprises an uplifted and fractured Palaeozoic bedrock landscape carved by natural forces. The resultant ancient valleys were in-filled with sediments during the Tertiary Age. These are overlain or interrupted by layers of basalt flows from volcanoes during the Neogene period. Shale and sandstone layers were formed around 435 to 500 million years ago. During a period about 345 to 395 million years ago, there was a major mountain-forming event that created gold-bearing quartz veins known as reefs. Erosion during the Oligocene–Pliocene period, which occurred about 26 to 2 million years ago, led to the formation of gold deposits in the ancient valleys of the upper Loddon River. Around 2 million years ago to less than 30,000 years ago, there was a period of volcanic activity that filled these valleys and covered the gold deposits with layers of gravel, sand, silt, clay, and some lignite. These deposits were mined extensively for gold during the mid to late 1800s in the Creswick area. Miners followed these deposits under the basalt layers, which they called 'deep leads.' Within and around the area, at least 15 volcanic eruption points formed small cones. The eruptions produced deposits of scoria, ash, and tuff near these cones. In between eruptions, clay layers formed between the basalt flows. Mount Kooroocheang, known locally as Mount Smeaton, just north of Kingston, is the largest volcano in the Uplands, rising 200 m above the plain to an elevation of 676 m. Young cones near Ballarat, Mount Warrenheip and Mount Buninyong, are visible from Spring Hill. The basalt layer, which is up to 100 metres thick over the ancient valleys, acts as a significant underground water source in the Kingston area. The fertile soil covering the basalts, particularly around the volcanic cones such as Kingston's Spring Hill, is excellent for agriculture, and potatoes are the dominant crop in those areas. Goulburn-Murray Water administers the Loddon Highlands WSPA Groundwater Management Plan under section 32A(5) of the Water Act 1989 of the Victorian Government.
Climate The Australian Bureau of Meteorology provides climate data for Creswick, 10 km SW of Kingston.
History
First inhabitants The Dja Dja Wurrung People are the Traditional Owners of the district of Kingston. Their country extended over lands from close to Bendigo to Avoca, from the Great Dividing Range to near Pyramid Hill and they were displaced by white settlement, with some retreating to Parker's Protectorate at Franklinford.
European settlement Kingston Post Office opened on 11 October 1858. A polling place for the Creswick electoral district was first opened in the town in October 1860. It became the administrative centre of the Creswick Shire until the merging of the Shire and Borough of Creswick on 29 May 1934.
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