Coastal and Britain relation and more factors you know
Coastal Archaeology of Britain
The
recognition of the wealth and diversity of England’s coastal archaeology has
been one of the most important developments of recent years. Some elements of
this enormous resource have long been known. The so-called ‘submerged forests’
off the coasts of England, sometimes with clear evidence of human activity, had
attracted the interest of antiquaries since at least the eighteenth century,
but serious and systematic attention has been given to the archaeological
potential of the coast only since the early 1980s.
It is
possible to trace a variety of courses for this concentration of effort and
interest. In the 1980s and 1990s, scientific research into climate changes and
its environmental impact spilled over into a much broader public debate as
awareness of these issues grew; the prospect of rising sea levels over the next
century, and their impact on current coastal environments, has been a
particular focus for concern. At the same time, archaeologists were beginnings
to recognise that the destruction caused by natural processes of coastal
erosion and by human activity was having an increasing impact on the
archaeological resource of the coast.
The
dominant process affecting the physical form of England in the post-glacial
period has been the rise in the altitude of sea level relative to the land, as
the glaciers melted and the land mass readjusted. The encroachment of the sea,
the loss of huge areas of land now under the North Sea and the English Channel,
and especially the loss of land bridge between England and France, which
finally made Britain an island, must have been immensely significant factors in
the lives of our prehistoric ancestors. Yet the way in which prehistoric
communities adjusted to these environmental changes has seldom been a major
theme in discussions of the period. One factor contributing to this has been
that, although the rise in relative sea level is comparatively well documented,
we know little about the constant reconfiguration of the coastline. This was
affected by many processes, mostly quite localised, which have not yet been
adequately researched. The detailed reconstruction of coastline histories and
the changing environments available for human use will be an important theme
for future research.
So great
has been the rise in sea level and the consequent regression of the coast that much
of the archaeological evidence now exposed in the coastal zone, whether being
eroded or exposed as a buried land surface, is derived from what was originally
terrestrial occupation. Its current location in the coastal zone is the product
of later unrelated processes, and it can tell us little about past adaption to
the sea. Estimates of its significance will need to be made in the context of
other related evidence form dry land sites. Nevertheless, its physical
environment means that preservation is often excellent, for example, in the
case of the Neolithic structure excavated at the Stumble in Essex.
In some
cases, these buried land surfaces do contain evidence for human exploitation of
what was a coastal environment, and elsewhere along the modern coast there is
similar evidence. Where the evidence does relate to past human exploitation of
the resources and the opportunities offered by the sea and the coast, it is both
diverse and as yet little understood. We are not yet in a position to make even
preliminary estimates of answers to such fundamental question as the extent to
which the sea and the coast affected human life in the past, what percentage of
the population at any time lived within reach of the sea, or whether human
settlements in coastal environments showed a distinct character from those
inland.
The most
striking evidence for used of the sea in the form of boats, yet we still have
much to learn about their production and use. Most of the known wrecks around
our coast are not unexpectedly of post-medieval date, and offer an unparalleled
opportunity for research which has as yet been little used. The prehistoric sewn-plank
boats such as those from the Humber estuary and Dover all seem to belong to the
second millennium BC; after this there is a gap in the record of a millennium,
which cannot yet be explained, before boats reappear, but built using a very
different technology. Boatbuilding must have been an extremely important
activity around much of our coast, yet we know almost nothing about it. Boats
were some of the most complex artefacts produced by pre-modern societies, and
further research on their production and use made an important contribution to
our understanding of past attitudes to technology and technological change.
Boats
needed landing places, yet here again our knowledge is very patchy. In many
cases, the natural shores and beaches would have sufficed, leaving little or no
archaeological trace, but especially in later periods, many ports and harbours,
as well as smaller facilities such as quays, wharves, and jetties, were built.
Despite a growth of interest in the waterfront archaeology of some of our more
important Roman and medieval towns, very little attention has been paid to the
multitude of smaller landing places. Redevelopment of harbour sites and other
development and natural pressures along the coast are subjecting these
important locations to unprecedented threats, yet few surveys of such sites
have been undertaken.
One of the
most important revelations of recent research has been the extent of industrial
activity along the coast. Fishing and salt production are among the better
documented activities, but even here our knowledge is patchy. Many forms of
fishing will leaves little archaeological trace, and one of the surprises of
recent surveys has been the extent of past investment in facilities for
procuring fish and shellfish. Elaborate wooden dish weirs, often of
considerable extent and responsive to aerial photography in shallow water, have
been identified in areas such as Essex and the seven estuary. The production of
salt, especially in the late Iron Age and early Roman periods, has been
recognised for some time, especially in the Thames estuary and around the
Solent and Poole Harbour, but the reasons for the decline of that industry and
the nature of later coastal salt working are much less well understood. Other
industries were also located along the coast, either because the raw materials
outcropped there or for ease of working and transport: mineral resources such
as sand, gravel, stone, coal, ironstone, and alum were all exploited. These
industries are poorly documented, but their remains are sometimes extensive and
striking.
Some
appreciation of the variety and importance of the archaeological remains
preserved in the coastal zone, albeit only in preliminary form, can thus be
gained from recent work, but the complexity of the problem of managing that
resource is also being realised. The problem arises not only from the scale and
variety of the archaeological remains, but also from two other sources: the
very varied natural and human threats to the resource, and the complex web of
organisations with authority over, or interests in, the coastal zone. Human threats
include the redevelopment of historic towns and old dockland areas, and the
increased importance of the coast for the leisure and tourism industries,
resulting in pressure for the increased provision of facilities such as marinas.
The larger size of ferries has also caused an increase in the damage caused by
their wash to fragile deposits in the intertidal zone. The most significant
natural threat is the predicted rise in sea level over the next century,
especially in the south and east of England. Its impact on archaeology is not
easy to predict, and though it is likely to be highly localised, it will be at
a scale much larger than that of most archaeological sites. Thus protecting one
site may simply result in transposing the threat to a point further along the
coast. The management of the archaeological remains will have to be considered
in a much longer timescale and a much wider geographical scale than is common
in the case of dry land sites and this will pose a serious challenge for
archaeologists.
Question 1-3
Choose the
correct letter A, B, C or D
1. What has caused public interest in
coastal archaeology in recent years?
A. The rapid development of England’s
coastal archaeology
B. The rising awareness of climate
change
C. The discovery of an underwater
forest
D. The systematic research conducted on
coastal archaeological findings.
2. What does the passage say about the
evidence of boats?
A. There’s enough knowledge of the
boatbuilding technology of the prehistoric people.
B. Many of the boats discovered were
found in harbours.
C. The use of boats had not been
recorded for a thousand years.
D. Boats were first used for fishing.
3. What can be discovered from the air?
A. Salt mines
B. Roman towns
C. Harbours
D. Fisheries
Question
4-10
True if the statement agrees
with the information
False if the statement contradicts
the information
Not given if there is no information on this
4. England lost much of its land after
the ice age due to the rising sea level.
5. The coastline of England has changed
periodically
6. Coastal archaeological evidence may
be well protected by sea water.
7. The design of boasts used by
pre-modern people was very simple
8. Similar boats were also discovered
in many other European countries
9. There are few documents relating to mineral
exploitation.
10. Large passenger boats are causing
increasing damage to the seashore.
Question 11-
13
Choose the
three letters A-G
Which three
of the following statements are mentioned in the passage?
A. How coastal archaeology was
originally discovered.
B. It is difficult to understand how
many people lived close to the sea
C. How much the prehistoric communities
understand the climate change
D. Our knowledge of boat evidence is
limited
E. Some fishing ground was covered to
ports.
F. Human development threatens the
archaeological remains.
G. Coastal archaeology will become more
important in the future.
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