2022
Yasmin Smith
Forest 2022
eleven coal fly ash glazes on stoneware slip (details)
top to bottom:
glaze 11: Tarong (Tarong Power Station, South Burnett region, Queensland)
glaze 10: Mount Piper (Mount Piper Power Station, Lithgow, New South Wales)
glaze 9: Wallerawang (Wallerawang Power Station, Lithgow, New South Wales)
glaze 8: Millmerran (Millmerran Power Station, Darling Downs region, Queensland)
glaze 7: Bayswater (Bayswater Power Station, Hunter region, New South Wales)
glaze 6: Eraring (Eraring Power Station, Lake Macquarie, New South Wales)
glaze 5: Vales Point (Vales Point Power Station, Lake Macquarie, New South Wales)
glaze 4: Gladstone (Gladstone Power Station, Gladstone, Queensland)
glaze 3: Hazelwood (Hazelwood Power Station, Latrobe Valley, Victoria)
glaze 2: Yallourn (Yallourn Power Station, Latrobe Valley, Victoria)
glaze 1: Energy Australia (unknown location)
In 2022 I completed a four-year research project into coal ash in Australia. Through collaborations with community, scientists and industrial workers, I collected ash from eleven different power stations in Australia to make the glazes that furnish ceramic casts of coal rocks. The glazes in Forest show a gradation in colour spanning a timeline of 300 million years. The lightest glazes come from the oldest black coal ash; having been underground for 250-300 million years, this coal has leached out most of its organic and inorganic life. As the seam progresses, the glazes begin to take on more colour. The youngest brown coal, that is 23-66 million years old, express a much richer glaze aesthetic as they still retain their mineral and plant memories.
Growth> death> coalification> extraction> reduction> return. From the Industrial Revolution onward, sections of humanity have dug vast amounts of coal from the earth leaving voids where forests once stood. A seam of geological time is removed. The coalified remains of these ancient forests are burned and its ashes resown back into geological time, returning the ashes to the earth’s surface and creating a new stratum.
When considering the massive, industrialised extraction and use of coal undertaken by humans since the mid-19th century as a contributing factor to changes in earth’s systems and climate, I think about the morphological changes that this activity leaves behind: the physical void 300 million years down, where coal was removed from geological time and the drastic changes to contemporary terrain to reach those depths. To officially enter the Anthropocene into the geological record, however, evidence of humanity must be defined in geochemical strata as it is laid down on the earth and contributes to a new geological age. If you ask what humans contribute to the geological fabric of the earth, one answer is fly ash from coal combustion. The spectrum of the coal-ash glazes in Forest, presents a visual understanding of this geochemical contribution and narrates this timeline over 300 million years.
Vales Point Power Station, Lake Macquarie, New South Wales, Australia. Supplied by Hunter Community Environment Centre.
Installation view: Yasmin Smith, Forest, 2022, at The Commercial, Sydney, photo: The Commercial, courtesy the artist and The Commercial, Sydney © the artist
Installation view: Yasmin Smith, Forest, 2022, at The Commercial, Sydney, photo: The Commercial, courtesy the artist and The Commercial, Sydney © the artist