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The
Royal Burgh of North Berwick coat of arms |
The
Early Settlers
By Douglas
Seaton, Local
Correspondent The
formation of the landscape around North Berwick dates back over 340 million
years, when this area was desert. Berwick Law and the islands of Craigleith,
Fidra, Lamb and Bass Rock are composed of igneous fire work formed during
the early carboniferous era. This
was the site of many volcanic eruptions and these famous landmarks are
the result of the mouth of the volcano being choked with its own molten
lava, forming a plug when extinct. During the ice-age, Scotland was
covered in a frozen glacial blanket that rubbed and wore away the volcanic
ash and soft sedimentary layers. When the glacier receded it exposed
the black rock visible today.
The oldest rock
in the area can be seen at Smiley Knowe. In both the East and West Bays,
there is evidence of lava-flow of the most extensive nature with enormous
deposits of volcanic ash or scoriae, forming the flat red tuffs visible
at low tide. Farther east the colour changes to green and a basalt dyke
of considerable length appears on the shore opposite the Leithies. Tuff
is much easier to work than basalt and the resulting Red Leck in Milsey
Bay was quarried for building and oven lining in the late Middle Ages.
Professor Fleming of Edinburgh University was the first to observe the
marks of glacial action on the striated rocks at the Auld Kirk in 1846.
According to some
writers the first inhabitants of North Berwick came from the Elbe, they
settled on the coast where water was available and their principal food
was shell fish gathered from the rocks. There are traces of four such
settlements in the district, first and most important was on the hill,
above the west beach. A midden containing a large number of shells of
edible species were found in the grounds of Tusculum, the house at number
8 York Road. Their burial ground was between that house and the shore,
which was discovered when the gasworks were being erected close to what
is now the eighteenth fairway on the West Links. Since ancient times
there was a burn in this area which flowed into the sea, and was crossed
by a timber footbridge, still being used in 1854.
There was another
settlement east of the Eil Burn where several internments and urns were
found. These internments are believed to date from the beginning of
the Christian era. The fourth settlement was above the Leithies on the
Rhodes Farm where a kitchen midden was found, it contained a stratum
of shells, pieces of broken pottery, fragments of bones and wood ashes.
A similar site was also detected on Castle Hill, the grassy mound between
Marine Parade and Tantallon Terrace, where a castle once stood owned
by the Earls of Fife.
On the south of
Berwick Law there is evidence of at least eighteen hut circles, rich
middens and a field system dating from 2000 years ago. There is also
the remains of a defensive stone dyke and ramparts which were not just
military artifacts but show that farming and a peaceful settlement was
a feature here. Activity in more recent times can also be found near
the summit, notably a rare example of a stone-built Napoleonic period
watch-tower with the outline of a garden.
During the upgrading
of the town water mains in October 2002 deposits of animal bones, shellfish
and fragments of pottery were discovered buried beneath the High Street.
Several midden layers were traced less than half-a-metre below the surface,
dating from the 14th century. The material contained a variety of shellfish,
mediaeval pottery and bones from sheep and cattle lodged between layers
of sand. The largest concentration was found west of the Council Chambers,
consistent with a midden pile where the inhabitants would discard their
waste into the street.
In May 2003, the
foundations of a 15th century wall was discovered in Melbourne Place,
leading to speculation that this was the town's eastern boundary wall.
This theory was reinforced when the shell and bone fragments discovered
in East Road came to an abrupt end opposite the Vennel in line with
what may have been the boundary wall.
The remains of an
old metal road made up of large red sandstone blocks was exposed 30cm
beneath Victoria Road. According to the archaeologists, the road from
Quality Street to Victoria Road is the oldest road in the burgh, and
among the artefacts unearthed in Quality Street was a whale bone scarred
with the marks of a sharpe implement similar to a cooking knife.
The records suggest
that a form of Celtic language similar to Welsh, Cornish and Breton
was spoken in East Lothian in post-Roman times. During the Roman occupation
of Lowland Scotland, Traprain Law which literally translated means the
hill of staves because of the wooden fortifications, was an important
Roman settlement. Later this site was the tribal capital for the Votadini,
the main tribe of the Lothians who were a peaceful people despite their
Celtic and Viking ornamentation on their weaponry. A sculpture depicting
the Votadini tribal carvings can be seen in the grounds of the supermarket
in Dunbar Road.
The Anglo-Saxons
then moved north pushing the local tribes westwards and establishing
the Kingdom of Northumbria from the Humber to the Forth. In the eleventh
century the King of Scots through conquest reclaimed the territory as
part of Scotland and the Gaelic language was heard for the first time
in East Lothian.
The name North Berwick
means North 'barley farmstead'. Bere in Old English means 'barley' and
wic in Old English is 'farmstead'. The word North was applied to distinguish
this Berwick from Berwick-upon-Tweed, which throughout the Middle Ages
the Scots called South Berwick. It was recorded as Northberwyk in 1250.
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