The Evolution of Britain’s Landscape.

Britain and Scotland come together: Ordovician(510-439 Ma.) 
and Silurian (439-408 Ma.) ( Lower Palaeozoic) times. Part 1 of 3

­­­­­­

During Ordovician times, most of Scotland and N. Ireland were separated from England & Wales by a wide ocean called Iapetus.

Scotland and northern Ireland formed part of an ancient continent called Laurentia, now N. America while England, Wales & Southern Ireland formed part of a continent called Avalonia which was about 27 deg. south of the equator. (See diagrams).

The Skiddaw Slates (or Skiddaw Group) of the Lake District consist of metamorphosed marine sediments laid down on the northern margin of Avalonia. These slates can now be seen in the northern part of the Lake District, e.g. around Blencathra and Skiddaw. Have a look at some chiastolite slate.

 

The map to the left shows the disposition of the continents during Early Ordovician times. “England, Wales and Southern Ireland” (Avalonia) are separated from “Scotland and Northern Ireland” by the spreading Iapetus Ocean.

During Late Ordovician times the Iapetus Ocean began to close, initiating a subduction zone resulting in the volcanic rocks of the Lake District (the Borrowdale Volcanic Group).

Home Page

Geology tour of Northern England

Rocks under the Microscope

Recommended Reading

Links

Top of page

Above Paleomap from “The Geology of Britain. An Introduction” Peter Toghill. 2000. Swan Hill Press. (cf. Recommended Reading for more information about this book.)

Click for part 2