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The Archaeology of Britain: An introduction from ... - waughfamily.ca

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Chapter Three<br />

Hunter-gatherers <strong>of</strong> the Mesolithic<br />

Steven Mithen<br />

<strong>The</strong> last Ice Age <strong>ca</strong>me to an end<br />

10,000 radio<strong>ca</strong>rbon years ago.<br />

Tundra lands<strong>ca</strong>pes that supported<br />

reindeer herds were colonized by<br />

birch and soon be<strong>ca</strong>me thick<br />

deciduous woodland with dispersed<br />

fauna including red deer and pine<br />

marten. Except in the far north,<br />

relative sea-levels rose so that<br />

<strong>Britain</strong>, formerly a peninsula <strong>of</strong><br />

Europe, had become an island by<br />

8,500 years ago. In this rapidly<br />

changing environment, people<br />

continued to live by hunting and<br />

gathering for several thousand years<br />

until agriculture be<strong>ca</strong>me an<br />

established way <strong>of</strong> life. This period<br />

was the Mesolithic (Figure 3.1).<br />

THE ENVIRONMENTAL<br />

CONTEXT FOR<br />

MESOLITHIC SETTLEMENT<br />

Eighteen thousand radio<strong>ca</strong>rbon<br />

years ago, ice sheets extended<br />

southwards to central England,<br />

beyond which lay an uninhabited<br />

polar desert. As the climate<br />

improved, Lateglacial hunters again<br />

<strong>ca</strong>me northwards (Chapter 2). By<br />

10,000 years ago, the global warming<br />

that marks the end <strong>of</strong> the<br />

Pleistocene was established: in a few<br />

de<strong>ca</strong>des, temperatures rose Figure 3.1 Mesolithic sites referred to in this chapter.

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