Question

How far do tree roots actually spread?

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Answer

Much wider and much shallower than the popular image of a mirror-image underground canopy — the great majority of a tree's roots sit in the top 60 centimetres of soil and extend well beyond the branch spread.

The actual shape. Roots form a broad shallow plate rather than a deep taproot in most mature trees. Typical figures: over 90% of roots in the top metre, most within the top half metre, and lateral spread commonly two to three times the canopy radius, sometimes more in open ground. A deep taproot is common in seedlings of some species and is usually lost or reduced as the tree matures.

Why shallow. Roots need oxygen as well as water. Deep soil is frequently compacted, waterlogged or oxygen-poor, so roots concentrate where conditions suit them — near the surface, where rain, organic matter and air are.

What follows practically:

The area to protect is wide. Compacting, paving or changing levels anywhere within the root zone damages a tree, and the damage appears years later. Construction work is the commonest cause of urban tree decline, and the injury is usually done to roots nobody saw.

Watering at the trunk is largely useless. Absorbing roots are at the outer part of the spread, not the base.

Root damage is not visible until the canopy responds, which can take several seasons.

On subsidence and drains. Roots do not seek out and break intact pipes — that is a persistent myth. They exploit existing defects, entering cracked or poorly jointed drains where moisture escapes, then enlarging the problem. Subsidence risk is genuine on shrinkable clay soils, where a tree's water uptake shrinks the soil and can cause differential settlement; the risk depends on soil, species, distance and the building's foundations, not on trees generally.

Before planting near a building, consider mature size and species water demand rather than current size.

Before removing a tree near a building on clay, take advice — heave as the soil rehydrates can be as damaging as subsidence.

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