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The Bytham River was probably one of the most important routes of colonisation for Britains first human inhabitants.The Ingham deposits are, in contrast, much rarer and deeper layers.A large proportion of known human occupation sites, dating from before the Anglian Ice Age, have been shown to lie along the course of this river.Britain was a peninsula of the continent of Europe and Asia.Many of the major rivers we know today either did not exist, or flowed along a different course, as did the River Thames.The deposits laid down by the Bytham River are called the Ingham series, after the prototype description derived from layers exposed in the gravel workings at Ingham in Suffolk.This river, which was already some 250,000 years old at least, is traced along its presumed course through West Suffolk on the attached diagram.

The diagram relies upon connecting up known sites of deposits of the Ingham series of sands and gravels.However, it should be noted that most of the gravel extraction along the Lark Valley, including West Stow and Lackford pits, comes from much later glacial and post glacial deposits.Quick links on this page Anglian Glaciation 478,000 BC Abandoned by Rome 410 AD West Stow village in 440 AD Sigeberht at Bury 635 End of West Stow?720 Domesday West Stow 1086 John Croftes 1526 Basil Brown on site 1940 Stanley West excavations 1965 Reconstructions begin 1973 Site WSW 030 1979 Visitor Centre 1988 Anglo Saxon Centre 1999 New Centre Dig 2007 New Development Plan 2010 Organisational changes 2013 Foot of Page Before the Ice Ages Five hundred thousand years ago, before the time known to us as the Ice Ages, the British landscape was very different to what we see today.

It drained from the southwest Midlands and the Pennines through Warwickshire and parts of Leicestershire before turning south through the centre of East Anglia and eventually eastwards into what is now the North Sea but was then dry land.Its gravels included red quartzite pebbles and they are visible at Mildenhall and Icklingham.

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