Independent 4-star boutique hotel at the heart of the London Bridge Quarter
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Geology and topography of Southwark, Central London

The underlying geology of this area of Southwark consists of alluvial silts overlying sand and gravel flood plain deposits.

North Southwark lies over sand capped gravel islands or 'eyots' that lay within a much wider River Thames.

These islands would have been formed by glacial drifts after the end of the last Ice Age, c 10,000 years ago.

A section through the excavations for the lift shaft during the hotel reconstruction, revealed the following:

cross section through lift shaft

every room has
LCD TV with wide range of satellite TV channels
Complimentary wi-fi / wired internet access
DDI telephone
Air-conditioning
Minibar
Tea and coffee making facility
Mineral water
Hairdryer, iron and ironing board
Duvet and choice of pillow
White Company toiletries
Fibre optic reading lights
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primary contacts
LONDON BRIDGE HOTEL
8-18 London Bridge Street
London SE1 9SG UK

Tel.: +44 (0)20 7855 2200
Fax: +44 (0)20 7855 2233
Reception Fax: +44 (0)20 7855 2234 (For Hotel Guests)

email

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