Europe with a tongue of ocean.
Or perhaps humans could make a difference.
Time would tell.
Afterword
In 1931 a fishing trawler called the Colinda, working forty kilometres off the eastern coast of England, dragged up a lump of peat. Inside, the skipper found an elegantly barbed spear point made from a deer antler. Entirely unexpected, it was a relic of a country now lost beneath the ocean.
In 8000 BC sea levels were much lower than today, as vast quantities of water were still locked up in the ice caps, and around the world ocean floors were exposed. Britain was not an island. The bed of the North Sea was a vast plain now known as ‘Doggerland’, a country larger than modern Britain whose northern coast ran directly from England to Denmark. The present Dogger Bank was a shallow upland (called the First Mother’s Ribs here), and to its south was a salt-water estuary the size of the Bristol Channel, now known as the Outer Silver Pit (and here called the Moon Sea). With twenty-four major lakes and wetlands and sixteen hundred kilometres of river courses, Doggerland was a rich, well-watered landscape that would have been very attractive to human hunters, more so than the surrounding higher land - and probably the centre of north Europe’s culture at the time.
But as the last ice melted the sea levels rose, and the land itself, released from the ice’s weight, rose and fell in a complex geometry of rebound. Doggerland began to drown. The sea rise may have been punctuated by sudden events such as storm surges - or even by tsunamis, as depicted here. In c.6200 BC a massive undersea landslip occurred off the coast of Norway at Storegga (see Bondevik et al, Eos, vol. 64, pp. 289-300, 2003). My earlier tsunami originates in the same undersea area.
By c.6000 BC Britain was severed from continental Europe, by c.4000 BC the last islands were submerged, and that was the end of ‘Doggerland, a country that had been central to the cultural development of north-west Europe for perhaps twelve thousand years’ (chapter five of Europe’s Lost World: The Rediscovery of Doggerland, V. Gaffney et al, Council for British Archaeology, 2009). The question asked in this series is: what if this northern heartland, on the brink of the Neolithic, had not been lost to the ocean?
Doggerland’s existence was suspected long before the Colinda’s chance find. Observations of submerged offshore forests - ‘Noah’s woods’ - had been recorded since the twelfth century. Geologist Clement Reid, in his Submerged Forests (Cambridge, 1913), was the first to speculate that a drowned landscape might once have joined Britain to the continent. A key survey was published in 1998 by Professor Bryony Coles (Proceedings of the Prehistoric Society, vol. 64, pp. 45-81), who coined the name ‘Doggerland’. This built on data about the North Sea gathered by geologists, environmentalists, marine engineers and others. (The Northland map in this volume is based on Coles’s projections.) A recent work led by the University of Birmingham utilised two decades’ worth of geological data, gathered by the oil and gas companies, to produce a detailed study of a large area south of the Dogger Bank (see Mapping Doggerland by V. Gaffney et al, Archaeopress, 2007).
The importance of Doggerland is now recognised. Doggerland is one of the three largest preserved drowned landscapes in the world, the others being Beringia, under the Bering Strait, and Sundaland, between Indochina and Java. Archaeologists are seeking World Heritage status for the site, and there are proposals for further work with undersea archaeology and sea-bottom coring. My portrayal of Doggerland here, inspired by the excitement of the ‘discovery’ of this lost country, respectfully draws on the work done by these generations of researchers.
In the Netherlands people have been struggling to keep their land from the sea since before Roman times. Their earliest efforts, as in the novel, were to build artificial hills called terpen or werden in flood-affected areas, from about 500 BC. If anybody really did try to save Doggerland by building polders and dykes and drainage channels, the evidence is lost beneath the North Sea.
This book is set in Britain’s Mesolithic period, c.10,000 BC- 4,000 BC. For an overview see Late Stone Age Hunters of the British Isles, C. Bark, Routledge, 1992. The Mesolithic roughly corresponds culturally to the ‘Archaic’ period in the Americas; see Prehistory of the Americas, S. Fiedel, Cambridge, 1992. My Doggerland Mesolithic culture is an invention, but draws on evidence of comparable cultures around the world (see