View of the Billion year old Torridonian / Lewisian nonconformity on the NE spur of A' Mhaighdean |
In 1891 the discovery in the NW Highlands of Olenellus fossils in the Fucoid beds of the Saltera Grits formation, finally determined their position in the stratigraphic column as lower Cambrian in age. The fossil discovery again changed the geological history of the rocks in the NW Highlands, as the underlying Torridonian sedimentary rocks were relegated from their presumed Cambrian age and down into the Precambrian. The angular unconformity between the newly assigned Cambrian rocks with the underlying Torridonian, showed compelling evidence that the Torridonian were some way down into the Precambrian too. The Cambrian sedimentary rocks were deposited on a planation surface that had eroded away the Torridonian rock and also an unknown thickness of the underlying rocks of the Lewisian complex. Which implies there had been a long period of erosion and before that a long period of time to deposit the thick pile of Torridonian sediments. The Torridonian sediments are deposited on rocks of the Lewisian Complex and on a palaeo land surface with over 600m of relief between hill summits, valleys, cliffs and a surface covered with weathering debris. This presented another long period of time. Then there were the rocks of the Lewisian Complex, whose very nature implied a long and rich geological history.
The Torridonian inselberg Suilven rising above the Lewisian. |
Coincidentally in 1907 the chemist Bertram Boltwood in a pioneering example of geophysics used the then estimate of the radioactive decay rate of uranium into lead, to measure the ratio of lead and uranium from some rocks and determined ages of 400 million - 2,200 million years. It is reasonable to suggest the ages were the subject of some controversy with some prominent geologists and Boltwood's interest in geological dating then waned. The challenge of dating rocks through radioactive decay was taken up by Arthur Holmes, it is difficult to challenge the hard science of physics and the geological community then set about ordering the rocks into the timeline of Earth's history. Dating of rocks has become ever more sophisticated and innovative, currently the Torridonian rocks have been dated to between 1.2 and 0.95 billion years old. It is worth stating that a billion seconds equates to a few months short of 32 years, a billion years is a vast stretch of time.
The Lewisian complex comprises rocks with an age spread from 1.6 to 3.0 Billion years, confirming their place in the depths of Deep Time.
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