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WHO LIVED HERE? If you have visited the pages on this site
dedicated to the Wolverton project then you will know that evidence for
occupation in the Bronze Age and during the Anglo Saxon period was found
at the site. But who were these people and what might have led them
to live in the Alkham Valley? Beaker People.
About 2500 B.C. an influx of migrants settled in Britain. These newcomers
have been called the Beaker People because of the shape of the pottery
vessels that are so often found in their round barrow graves. The stocky
newcomers, although few at first, seem to have quickly over shadowed their
Neolithic landlords, becoming a sort of nouveau aristocracy. The Beaker
folk were farmers and archers; they were also the first metal smiths in
Britain, working first in copper and gold, and later in the bronze that
has given its name to this era.
How they lived
There was a changeover during this period to round houses,
echoed in the mushroom-like growth of
stone circles and round barrow mounds
The Beaker Folk introduced a pastoral pattern to the
agricultural lifestyle of Neolithic times. As population grew, more
marginal land was brought into cultivation, and was farmed successfully
for hundreds of years, until climate changes forced its abandonment. The
Beaker Folk were a patriarchal society, and it is during the Bronze Age
that the individual warrior-chief or king gained importance, contrasting
with the community orientation of the Neolithic times. Towards the end of the Bronze Age the
climate changed drastically. According to tree ring evidence, a major
volcanic eruption in Iceland may have caused a significant temperature
drop in just one year. At this time the settlements on Dartmoor were
abandoned, for example, and peat started to form in many places over what
were once farms, houses, and their field systems. It seems likely that
warfare and banditry erupted as the starving survivors fought over land
that could no longer support them.
Religion
Both men and women were accorded
barrow burials. A curious fact was noted in studying these Bronze Age
burials; in many cases the corpses were carefully laid with the head to
the south, men facing east, women facing west. We can only guess that this
was to allow the corpse to see the sun at a particular time of day. The
Angle, Saxon and Jute tribes, who arrived in Britain in the fifth and
sixth centuries AD, are known as Anglo-Saxons. The Anglo-Saxons eventually
settled and took control of most of England, but never conquered Scotland,
Wales or Cornwall. England was divided into five Kingdoms. By around 600
AD these five main Anglo-Saxon Kingdoms were Northumberland, Mercia,
Wessex, Anglia and Kent.
Saxon Britain 600-900 AD
These tribes brought with them the beginnings of the
English language. Their rule came to an abrupt end with the Norman
invasion of Britain after the decisive battle of Hastings in 1066.
SETTLEMENT
We know little of the first several hundred years of the
Anglo-Saxon, or “English”, era, primarily because the invaders were an
illiterate people. Our earliest records of them are little more than
highly inventive list of rulers. We know that they established separate
Kingdoms, the Saxons settling in the south and west, the Angles in the
east and north, and the Jutes on the lsle of Wight and mainland opposite.
They probably thought of themselves as separate people, but shared a
common language and similar customs.
ROADS AND COMMUNICATION The Alkham Valley road dates back
at least a few hundred years and was eventually turnpiked between
1750-1780. It is impossible to venture how old this route could be
although there has probably been a cart track more or less on the modern
alignment since Roman times. Many of the tracks that criss-cross the
valley today, may have their origins as far back as the Bronze Age period.
Some of these tracks are now narrow tarmac roads and evidence for their
age can be observed in the deep hollows they lie in. These tracks were
eroded down through the chalk level over hundreds of years, without a
fixed metalled surface, rain washed the worn away loose material downhill
finally creating the deep sunken hollows were the roads traverse the
valley to this day. Leaving the northern end of the
Town and Port of Dover, the Alkham road (B2060) meanders through Kearsney
Abbey and the small hamlets of Chilton, Wolverton, Alkham, South Alkham
and Drellingore before joining the A260 & A20 near Folkestone. The route
of the Alkham road hugs the lower slope contour just above the base of the
valley following for the most part, the northern escarpment before
traversing to the southern side of the valley just past Drellingore. In
travelling through this mainly green undulating and picturesque landscape,
notable are the numerous coomb nooks along its course. Here in ancient
times, many of these glacially cut locations would have offered sheltered
and well-drained surfaces to settle. One of the most important features to
our ancestors would have been a readily available supply of fresh water
for themselves and their livestock. Through the centuries in areas without
reasonable access to running water, wells were sunk to great depths
through the chalk bedrock but this required much labour and danger.
Although difficult to imagine in modern times, an ancient river once
flowed through the Alkham Valley rising to a depth of ten feet in winter,
before entering the River Dour and out-falling into Dover Harbour some 4
km distant. It is believed the source of the river is located near
Drellingore, and once provided enough water for at least two corn-mills.
Over a thousand years ago, the Alkham river was likely to have been very
wide, deep and navigable to small vessels, at least as far as Drellingore
if not beyond. Nowadays, the Alkham River, now known as the Nailbourne,
for most of its course runs below ground and only surfaces in the valley
in times of severe rainfall as flooding across the fields. What remains of
this once large river can now only be seen as a small section of dyke
running into the pond at Chilton Farm, before flowing into the manmade
brick lined ponds at Kearsney Abbey and thence onto the sea.
The main reason for the loss of these rivers over the
centuries is due to the constant rise in sea levels. These days, sea
levels are around 2-3 metres higher than in roman times causing a knock-on
effect that slows the river flows. In this instance, the silts normally
washed downstream and eventually into the sea basin, builds-up on the
bottom of the now slowly moving river until, it becomes choked. Reed beds,
vegetation and agricultural developments have all added to the demise of
our rivers.
Until the annexing of Britain to the Roman Empire, and the
subsequent construction of their extensive road network all over Britain,
our ancestors communicated with other settlements via at best, dusty
pitted tracks in summer and impassable churned-up mud tracks in the depths
of winter. For these reasons, the river systems provided important inland
transport for goods throughout Kent and were a much easier, cheaper and
safer way to travel. Even after the roman’s enormous road building
projects, many of Kent’s rivers were still used to carry the bulk of
commodities inland from Europe, the Mediterranean and Rome itself. Landing
stages would have been commonplace along the banks of our rivers near to
settlements or major road arteries, very few can now be identified
however; the name “slip Lane” in the village of Alkham may indicate a
small long-lost dock access. The farm at Chilton almost certainly had a
stage on the river along with Wolverton and Drellingore but most are
probably long since buried by overburden slippage from the sides of the
valley. |