Britain and Scotland
united. Devonian 408-362Ma.(Upper Palaeozoic times)
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By late Silurian early Devonian times, approximately 410-380 million years ago, the Iapetus Ocean had closed causing Laurentia to collide with Avalonia and Baltica. This continental collision resulted in the formation of the Caledonide mountains in Scandinavia, northern Great Britain and Greenland, and the Northern Appalachian mountains along the eastern seaboard of North America. The collision led to the deformation, folding and uplift of the Ordovician, Silurian and older rocks of Northern England, as can be seen most dramatically at Pettico Wick near St. Abb's Head, Northumberland. |
During the Devonian, a period lasting about 50 million
years, fold mountains of Himalayan proportions, rugged uplands, and
intervening basins were formed over most of Britain. To the south, an ocean
called the Rheic existed, part of its shoreline
extending across southern Britain. |
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It was during the Devonian period that thousands of
metres of rocks were weathered and eroded away. Although the climate was hot
and desert-like, seasonal rainfall resulting in flash floods led to the
deposition of sands and conglomerates. This resulted in a series of Devonian
age rocks known as "Old Red Sandstone" as opposed to the "New
Red Sandstone" of Permian-Triassic age. Britain would have been 20 deg.
south of the equator, with only limited seasonal rainfall. |
The famous unconformity at Siccar Point, Grid Ref.
NT813710, about 20km SE of Dunbar, discovered by the 18th. century
geologist James Hutton consists of near horizontal Devonian red sandstones
overlying almost vertical Silurian mudstones and sandstones (greywackes). The
photo above right shows the lady's feet resting on almost vertical Silurian
while she is sat upon near horizontal Devonian (O.R.S.) rocks. |
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