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----------------------------------------------------------------- Site description When the first Blackwall Tunnel was completed in 1897 it was the longest underwater tunnel in the world and a remarkable engineering achievement, not least because of the unusual geology of the site.

Beneath the ‘drift’ deposits of sand and gravel dating from the Ice Age the surface of the bedrock in this part of London is usually fairly level with no variations more than about 5 metres (15 feet) in height.

Introduction Several definitions exist for the term periglacial.

The earliest definitions suggested that these geomorphic environments were located at periphery of past Pleistocene glaciers.

The two tunnels had passed through a buried, elongated, basin-like feature with almost vertical ‘cliff-like’ walls and completely filled with sand and gravel.

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