Earliest times to present day
Countless ages ago, the earth threw up the molten rock which was to become Dartmoor, the backbone of the County of Devon. Convulsive movements raised and lowered the land, so that the great rock mass became part of a vast continent which included the land which we now call France.
Then the sea rushed in, filling the depression which was to become the English Channel and making islands of the rocky promontories of the Continental coasts. Movements continued intermittently over thousands of years, and masses of sand, silt and pebbles were laid down around the rock mass. The ice ages came and went and, although they did not reach as far south as the embryonic Dartmoor, snow-
In warmer intervals between the centuries of ice, there were great floods of rain, which weathered and split the great rock plateau and rushed down from the high land in steep, stormy torrents -
The Teign carried with it thousands of tons of rotted granite, which it laid down in its lower reaches as boulder clay. It cut for itself a narrow course through the softer rocks below the Moor and eventually poured into the sea through a sunken valley which we now call the Teign Estuary.
At the mouth of the valley, the current of the river, checked by the sea and by broken rocks, silt and sand, built up an area of beachy mud. The river, deflected by this barrier, took a sharp turn to the right and cut a way for itself at the foot of the great cliff which we now call the Ness.
The heaving crust of the earth had now become more stable. Life had established itself on the land and the brown bear, the mammoth and the sabre-
Thousands of years later, Bronze Age man lived on Haldon and he regarded the shores of Teignmouth as a good place to obtain supplies of salt for preserving his meat and for adding savour to his food.
References in the works of Greek and Roman writers show that in pre-
At the mouth of the valley, the current of the river, checked by the sea and by broken rocks, silt and sand, built up an area of beachy mud. The river, deflected by this barrier, took a sharp turn to the right and cut a way for itself at the foot of the great cliff which we now call the Ness.
The heaving crust of the earth had now become more stable. Life had established itself on the land and the brown bear, the mammoth and the sabre-
The caves at Brixham and Torquay show traces of man’s habitation and there are signs that wild beasts lived there too. No doubt Palaeolithic man hunted over the hills around Teignmouth and fished in the Teign, but there is no record of inhabited caves in or near Teignmouth.
Thousands of years later, Bronze Duke of Cornwall is a title in the Peerage of England, traditionally held by the eldest son of the reigning British monarch, previously the English monarch.
The Duchy of Cornwall was the first duchy created in England and was established by royal charter in 1337.
“ DEVON “
The earliest reference to the shire by name is to be found in the Anglosaxon Chronicle under the year 851, when “ the Alderman ceorl with the men of Defenasoir fought the heathen army at Wicganbeorg and after making great slaughter obtained the victory.” In 894 the form Defnum occurs , Defenum in 897, and Defenun in a charter of 955. Somewhat earlier , in 823, the Chronicle speaks of “ the men of Devon ” as Defnas.
This tribal name was transferred, as in several other English counties, In the territory inhabited by the tribe. the Defnas , to trace the name further, derived their name from the British Dumnonii, the name of the Celtic inhabitants of south-
The theory that the old name for south-
This is a piece of folke mythology but it has no other authority.
Thus the name of Devon is derived ultimately from a Celtic tribal Name -
Both the modern forms— Devon and Devonshire— are equally ancient, dating from the earliest days of the shire in the 9th century. Neither usage is more correct than the other. The form we use to-
Thus we speak of Red Devon Cattle, and we used to speak of Devonshire cream.
THE ENGLISH SETTLEMENT when the countryside was being colonised and populated , and large areas of land were changing hands by
THE DANES The Danes began visiting the English coasts for plunder early in the 9th century, the first known raid being on Sheppey in 835.
During the next thirty years they made more than a dozen descents on different parts and did great damage. In 851 they came as far west as Devon, but the Anglo-
almost certainly in Devon and probably near the south coast, has been variously identified, but Wickaborough or Weekaborough, less than four miles from the shores of Tor Bay at Paignton , seems the likeliest site.
The whole of Tor Bay was wide open to sudden attack from the open sea before help could arrive—history repeated itself in the tip-
From the shores of the bay old trackways led inland over the hills to further plunder and pillage, but by the time the invaders were four miles along the lanes Ceorl and his men had reached the scene and defeated them decisively. Twenty-
with many of Alfred’s thegns, at a place called by Asser Arx Cynuit. Here he was killed with more than eight hundred of his men, and the resistance movement in the Somerset marshes received a powerful stimulus. Arx Cynuit, too, has been variously id
THE DANES
The Danes began visiting the English coasts for plunder early in the gth century, the first known raid being on Sheppey in 835. During the next thirty years they made more than a dozen descents on different parts and did great damage. In 851 they came as far west as Devon, but the Anglo-
Twenty-
In 893 there were renewed Danish attacks, one force attacking Exeter, another “ a fort in Devonshire by the north sea ” (so says the Chronicle) which can probably be identified as the burh of Pilton. These attacks were beaten off. Thereafter the south-
In 997 a more formidable force attacked the coasts of Wessex, begin-
THE DANES 53
ning with the northern coasts of Cornwall and Devon, as well as south Wales. Then they turned back around Land’s End and went up the Tamar “ burning and slaying everything that they met,” says the Chronicle, as far north as the burh of Lydford. Here they were repulsed and they returned to their ships in the river with incalculable plunder, some of it from Ordulf’s new abbey at Tavistock—founded less than twenty years earlier—which they had burned to the ground. Then they moved eastwards to Dorset, Hampshire, Sussex, and Kent.
In the year 1001 they were back in Devon, “ where Pallig came to meet them with the ships which he was able to collect; for he had shaken off his allegiance to King Ethelred, against all the vows of truth and fidelity which he had given him, as well as the presents which the king had bestowed on him in houses and gold and silver.” So says the Anglo-
The uneasy truce of 1002 was ended by Ethelred’s massacre of the Danes, in which the sister of King Swein of Denmark is traditionally supposed to have perished. Swein, probably to avenge his sister’s death, invaded England in 1003. The south-
The Danes, during all this time, had made no settlements in Devon: they had attacked the south-
burrator |
blackdown |
monachorum |
bere ferrers |
totenesium |
buckfast |
bellever |
drew |
cliffordbridge |