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The Guardian - UK
The Guardian - UK
Environment
Mark Hillsdon

Blossoming among spoil heaps: how 1,000 years of lead mining gave birth to banks of pansies and pennycress

Someone out of focus lying down and looking at a purple petalled flower with a yellow centre among grass blades
A mountain pansy at Briarwood Banks, one of the increasingly rare calaminarian grasslands in Northumberland. These ‘metallophyte’ plants have adapted to live in polluted soils. Photograph: Christopher Thomond/The Guardian

At first, the small purple flowers are hard to spot in the weak May sunshine. Slowly the drifts of delicate mountain pansies, along with the white rosettes of alpine pennycress, begin to jump out, scattered across an area little bigger than a football pitch, on the banks of the River Allen in Northumberland.

This is a pocket of calaminarian grassland, an increasingly rare habitat where specialist plants called metallophytes have adapted to live in soils deeply contaminated by heavy metals, the legacy of more than 1,000 years of lead mining.

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