Chalybeate Spring, Mittagong

Aboriginal context The traditional owners of the country around Mittagong are Gandangara people. It is not known if they used the spring as a water source but this small spring, given its strong-tasting water and earthy odour, He named it 'Lady Mary's Well', after his wife Lady Mary FitzRoy who had been killed in a carriage accident in December 1847 in the Domain of Government House, Parramatta. Over the years, variants of the name involving 'Lady Mary' or 'Lady Fitzroy' were used occasionally but, on the whole, this official name did not stick. For a time, the spring was thought to be the only chalybeate spring in New South Wales. In fact, there were other chaleabeate springs in the Southern Highlands—near Berrima, Hill Top and Picton—and there were other springs within Mittagong, even in close proximity. The Mittagong spring remained known as 'The Chalybeate Spring' throughout its existence. == Description ==

The Chalybeate Spring was situated on the top of a grassy knoll on southern side of the Great South Road (now Old Hume Highway) about a quarter of a mile (400m) from the Mittagong railway station. It was described in 1896 as "no more than a little hole in the ground from which the water oozes up through the crevices among the hematite ore". The naturally-carbonated, iron-rich water was described as having "an inky taste and an earthy odour". The spring-water ran clear but turned ‘rusty’ in colour after a few hours. It was stated that "The water has considerable medicinal properties, the quantity of iron in solution being so minute as to be readily assimilated by systems needing the tonic effect that iron Imparts." or 'flowing'. Around 1901, there were three active springs; the largest—presumably the Chalybeate Spring—had an estimated flow rate of 100-gallons/hour (455-litres/hour), with the other two flowing at much lower rates. == Chemical analysis ==

The analysis of the mineral content of the water (1962) was: • iron bicarbonate* C2H2FeO6 ; 85.5 ppm • magnesium bicarbonate* Mg(HCO3)2 ; 32.0 ppm • calcium bicarbonate* Ca(HCO3)2 ; 29.1 ppm • sodium chloride NaCl ; 30.8 ppm • potassium chloride KCl ; 9.1 ppm • magnesium chloride MgCl2 ; 8.5 ppm *These compounds exist only in aqueous solution. The iron content of the spring-water was very high. It was over three times that of the famous Chalybeate Spring at Royal Tunbridge Wells in Kent, England. == Significance ==

. The Mittagong ore body, although relatively small, lay close to a rail connection to the Port Kembla steelworks and was the closest local deposit to it. Approximately 14,000 tons of ore was mined during 1941, from a location close to the spring. led in turn to the foundation of the township of New Sheffield, one of the small townships that were precursors to Mittagong. Tourist attraction Despite its proximity to the iron ore mine and the Fitzroy Iron Works—until that works closed for the last time on 1 July 1896—the Chaybeate Spring was already an attraction from the mid-19th century onwards. Around the time of Governor FitzRoy's visit in 1849, there were already moves to exploit the spring and it was reported that "invalids from Sydney and other parts will have the advantage of these waters, combined with an invigorating and cheerful atmosphere". Following Governor Fitz Roy's visit, the water was analysed and advice given that it was best drunk as soon as possible after it emerged from the spring. The water of the spring became well known. A newspaper article in 1909 attested to the popularity of the spring, "The chalybeate springs right in the town are being availed of at all hours of the day. All who partake of the cool, sparkling mineral water are unanimous In their praise of its curative and invigorating properties. Many, indeed, are recommended by their medical advisers to visit the town for the sole purpose of availing themselves of a course at the chalybeate spring." A newspaper article in 1921 described the facilities at the spring as follows: ''"The spring has been enclosed. There are summer-houses and seats, and provision made so that invalids taking the waters may rest and picnic, procuring refreshments on the spot. The waters have proved extremely beneficial to visitors, and are daily attracting others from all parts. The local Tourists' Association, recognising Its value, has taken great pains to make the spot comfortable and attractive."'' == Decline and disappearance ==

By 1938, mineral springs were no longer fashionable and the Chalybeate Spring at Mittagong had slipped from public consciousness. The iron ore mine and the Chalybeate Spring had co-existed for many years. The Fitzroy iron ore mining operation had been on a small scale, commensurate with the small capacity and sporadic operation of the 19th-century iron-works. In 1941, iron ore was again mined from a location close to the spring. Despite assurances that the spring would be protected, the mining activity caused the Chalybeate Spring to ‘deviate’ from its pre-war position. The land on which the Chalybeate Spring flowed had always been privately owned. In 1945, Nattai Shire Council was asked to approve a plan to erect poultry sheds at the site of the spring. In 1948, the spring was "now enclosed in a fowl run." However, in 1962, it was still possible to collect water for a chemical analysis. The Mineral Springs Historical Centre was open for less than a year in 1988. The focus of preservation and commemoration of the iron-works therefore moved to the north side of the Old Hume Highway, perhaps leaving the Mineral Springs Reserve with less justification for its existence. The Wingecarribie Shire Council's local environmental management plan of 2010 rezoned the Mineral Springs Reserve (Lot 33, DP9299), from 'public open space' to ‘operational land. In 2011, an application was put to the council, which had suffered huge losses on its investments during the 2008 financial crisis, to subdivide the land. On the westernmost lot, the former museum building became the Wingecarribie Aboriginal Community Cultural Centre in July 2012. The other lot was destined to go to the Mittagong RSL Club; it is still vacant land with the appearance of parkland. == Legacy and remnants ==

There is an interpretive sign with information about the spring and the history of the land, outside the former Mineral Springs Reserve near the entrance to the Mittagong RSL Club from the Old Hume Highway. The name of the nearby Springs Resorts—owned by the Mittagong RSL Club—refers to the old spring, There is still a significant amount of iron ore—deposited over millennia by chalybeate springs—on the southern side of the Old Hume Highway, at the western end of the former Mineral Springs Reserve and under nearby houses along the Old Hume Highway. Bare patches of the hillside are rust-coloured and ironstone rock outcrops in places. The Fitzroy Iron Works—built to exploit the iron ore—was important in the development of Mittagong, and left its own legacy and remnants. A pile of ironstone rocks, some rust-coloured buried concrete, stonework and brickwork, and some vandalised cast-iron lamp-posts—all still present in January 2019, at the top of the hill, in the former Mineral Springs Reserve—are the remnants of the last incarnation of the Chalybeate Spring. The Chalybeate Spring, at least as it was in 1988, no longer exists. A little further down the hill from the pile of rocks—towards the Old Hume Highway—there is a low retaining wall and a patch of permanently wet ground. Just above the wall an oozing chalybeate source had built a small soggy mound of water-saturated iron oxide that is covered in lush grass, by 2019. It may be all that remains of the once renowned Chalybeate Spring. == See also ==