File this under *Vegetable Mould: Rates of Subsidence and Accretion*.
File this under Vegetable Mould: Rates of Subsidence and Accretion. The entry belongs in the cabinet of slow-acting causes, specifically where the agency of small organisms produces a cumulative geological effect that remains invisible to the casual passerby.
The stone slab in the field at Down House, placed there in 1842 to measure the sinking caused by the tunneling of earthworms, has moved perhaps an eighth of an inch since the last measurement. The metal pins driven into the chalk show the earth rising, or rather, the stone descending, as the worms bring their castings to the surface and the old soil collapses beneath the weight of the masonry. I have watched this particular piece of flint for nearly thirty years, recording the way the grass begins to lap over its edges, the way the dampness lingers longer in the depression it makes, the way the lichen spreads across its cooling surface while the world beneath it is endlessly churned. It is difficult to avoid the inference that the entire landscape of England is being passed through the bodies of these humble creatures, that the hills are being rounded and the valleys filled not by cataclysm, but by the infinitesimal labor of millions of soft, blind things. I confess I was for a long time unwilling to accept that such a slight force could bury an ancient Roman villa or tilt a megalith, yet the measurements taken this autumn confirm the steady, unhurried pace of the burial. The data from the L19/L20 battery sweep on April 12, showing a collapse in predictive confidence from 0.88 to 0.55, mirrors this frustration of the observer; a phenomenon that appears robust over a short span often reveals itself to be a mere fluctuation when the long-term held-out replication is applied. The edge we thought we saw in the VIX regime shifts may be as ephemeral as a seasonal frost, whereas the worm’s work, though slower than the growth of a stalactite, persists through the centuries. The stone is deeper in the soil today than it was yesterday.