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  • The body fluid

    "We shed many skin cells – at a rate per hour it comes close to a million cells per day. New cells generated at the bottom of our layered epidermis push their way to the top, where they are weathered by the environment and our daily activities. ​ As the living body breaks down, it becomes lodged in skin pores and clothing fibres. It is inhaled, irritates, is sneezed out and blown afar; it collects in corners, and gathers on surfaces. It welcomes company, joining with soil or, lifted by weather patterns, combines with volcanic eruptions, pollution and plant pollen, or with animal bodies, minerals, and even with burnt meteorite particles – all the while becoming increasingly microscopic and indistinct. The body, now fluid and divisible, transgresses boundaries. Transformed and nomadic, it inhabits spaces without detection. That is, until a ray of sunlight reveals drifting motes hovering in the air, or a missing shoe leads to the surprise discovery of a copulating fluffle of dust bunnies under the bed. In Gutspeak, these former remnants of ourselves are gathered by the artist Dominique Edwards from the tools used to seemingly eliminate them, and turned into sheets of paper. On closer inspection, these sheets reveal a multitude of its separate components: eyelashes, cosmetics, grains of sand, diminished chewing gum wrappers and pubic hair. There is also glitter. And a surprising amount of it. Are these cosmetic ingredients? Or...perhaps meteorite particles?"
  • The Tide Turns Installation

    Tumble dryer lint
  • The Tide Turns Installation

    Paper works made from new mops, used mops and tumble dryer lint. Sculptural installation consisting of one small intermittently rotating mop and one large continuously rotating mop.
  • Mop

    Videos projected onto a floating screen
  • Pompei casts

  • Deductions from smooth rocks

    Extract from Bettie Higgs's reading of rocks in 'Visual Practices Across the University'. Most of the rocks in this photograph are about 360 million years old, so the grains that comprise them are substantially older. The grains came originally from a mountain range, as large as the Himalayas, whose roots can still be seen in counties Mayo and Donegal, in the northwest of Ireland. The grains were carried south by rivers and deposited in this area; the smallest grains were carried all the way to the ocean, which was far south of Cork at the time, in what is now the Atlantic Ocean south of Ireland. (There was very little rainfall at the time: the portion of land that is now Cork was 10° south of the Equator. This can be deduced from the properties of the iron in the rock.) The water in which the grains were transported was oxygenated, and the iron precipitated out as iron oxide (haematite), which cemented the grains and which accounts for the red color (Elkins 2007: 74 - 78).
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