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Sunset Looking Down The River Tyne
Nothing definite is known of the origin of the designation "Tyne",
nor is the river known by that name until the Saxon period:
Tynemouth is recorded in Anglo-Saxon as Tinanmuðe (probably dative case).
There is a theory that Tīn was a word that meant "river" in the local Celtic language or in a language spoken in England before the Celts came: compare Tardebigge.
There is also a river Tyne that rises in Midlothian in Scotland and flows through East Lothian into the North Sea.
The River Vedra on the Roman map of Britain may be the Tyne, or may be the River Wear.
The late Thomas John Taylor supposed that the main course of the river anciently flowed through what is now Team Valley, its outlet into the tidal river being by a waterfall at Bill Point.
His theory is not far from the truth, as there is evidence that prior to the last Ice Age, the River Wear did once follow the current route of the lower River Team, merging with the Tyne at Dunston.
Ice diverted the course of the Wear to its current location, flowing east the course of the Tyne) and joining the North Sea at Sunderland
Nothing definite is known of the origin of the designation "Tyne",
nor is the river known by that name until the Saxon period:
Tynemouth is recorded in Anglo-Saxon as Tinanmuðe (probably dative case).
There is a theory that Tīn was a word that meant "river" in the local Celtic language or in a language spoken in England before the Celts came: compare Tardebigge.
There is also a river Tyne that rises in Midlothian in Scotland and flows through East Lothian into the North Sea.
The River Vedra on the Roman map of Britain may be the Tyne, or may be the River Wear.
The late Thomas John Taylor supposed that the main course of the river anciently flowed through what is now Team Valley, its outlet into the tidal river being by a waterfall at Bill Point.
His theory is not far from the truth, as there is evidence that prior to the last Ice Age, the River Wear did once follow the current route of the lower River Team, merging with the Tyne at Dunston.
Ice diverted the course of the Wear to its current location, flowing east the course of the Tyne) and joining the North Sea at Sunderland
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