Ellison, R.A.; Woods, M.A.; Allen, D.J.; Forster, A.; Pharaoh, T.C.; King, C.. 2004 Geology of London : special memoir for 1:50000 geological sheets 256 (north London), 257 (Romford), 270 (south London), and 271 (Dartford) (England and Wales). Nottingham, UK, British Geological Survey, 114pp. (Memoir (Sheet) British Geological Survey (England & Wales)).
Abstract
This book brings together information that results from
research on the ground beneath the streets of London. It
describes the geological strata, how they came to be there,
and how they impinge on the life of those who live and
work in the city, in its maintenance and sustainable development.
The development of London is intimately tied to the
ground conditions. The original settlement was originally
located at a crossing point on the River Thames in an
area of dry land where sand and gravel banks were surrounded
by rather boggy marshland.
A ready supply of
gravel and brick clay helped with the early infrastructure
development, and much later the extensive underground
tunnel network grew because of the ease of excavating
the London Clay. Water was always readily available, initially
from riverside springs and later, in larger volumes,
from underground Chalk.
This explanation of the strata that underlie London
gives an insight into the geological history of the last 500
million years. Over the past 200 years, boreholes have
explored the deeper layers and countless geologists have
systematically recorded the near-surface strata in quarries
and excavations. The geological history includes periods
of earth movement, inundations by the sea, the development
of coastal mudflats and the effects of great ice
ages.
Exploration for oil and gas in the North Sea has benefited
from an understanding of the rocks beneath
London, and their geological history. Effective use of
water resources, efficient ground investigation for new
buildings and infrastructure, and sustainable planning
and development are all founded on the use of information
about the condition and structure of the ground.
This book provides the background information for the
maintenance of good practice in these activities, and
illustrates some aspects of the ground that have in the
past caused difficulties.
Environmental concerns such as the legacy of contamination,
sea level rise as a consequence of global climate
change, and the recycling of water are issues that will
increase in importance in this century. Basic data, fundamental
for dealing with these concerns are presented in
this book, and on the associated 1:50 000 scale geological
maps for London.
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