As we dug down, the range of materials surviving increased. By the time the adjacent turf-line was at the level of our waists, that range broadened dramatically. The grey clays we had been removing gave way to something very different. This blackened peat below was full of all the things that had decayed from the sediments above. Our trowels teased their way through, to reveal leaves, nuts, and vast quantities of wood. As pieces of the freshly exposed peat were pulled apart, branches of birch buried for over two millennia revealed their silvery, flaky bark. Blades of grass could still be seen that still seemed to be green, as if the chlorophyll within them had remained intact. Now that they had been exposed to the air, that green colouration quickly changed to brown, just as a host of other processes of breakdown and decay set in. That exposed peat was soon peppered with insect holes, as burrowing soil animals responded with enthusiasm to the opening of the larder door. Waterlogged and sealed off from the air, the organic peats had been protected from the foraging of these creatures. We archaeologists had taken that protection away and now the limbo in which these fragments of life had been suspended would soon come to an end. In the case of the wood, this change took place before our eyes. When first exposed, the wood fragments within the peat seemed solid enough. Their surface features and patterned grain were clear to see, the main distinction from modern wood being their darkened colour. Once lifted and exposed on the grassy verge beside our trench, these pieces began to shrink as the water within them evaporated. They would twist and crack, and their surfaces would become flaky. Their solidity had been an illusion, only maintained while they remained within their enclosed and waterlogged refuge.