Can anyone shed any light on the following formation. Curious as to how it may have formed. South side of Soay ....

Thanks
Rob
The top and bottom are Torridonian sandstone. This is a pre-Cambrian megasequence of mostly fluvial (i.e. river derived) sands and grits. The actual strata are almost horizontal, but the strata are divided into packages, called foresets, of cross-bedding. This is where sand bars in the ancient river channels migrated along, like underwater sand dunes, leaving locally inclined bedding, at the angle of repose of the cascading sand (if that makes any sense).
In the middle is a much more recent dolerite sill. These are slightly more evolved magmas than basalt, and were the last stages of the ancient volcanic centres associated with the Atlantic opening in this area around 55my ago. Basically the Cuillins, Rum, Skye etc.) are ancient dissected magma chambers filled with the residual crystal mush after all the plateau basalts (Antrim, Staffa etc.) were erupted. The residual magma got squeezed out as a series of horizontal sheets (sills) and radial vertical dykes as the centres collapsed. If you looked carefully, you would see a glassy margin where the sill chilled as it was injected into the cold rock, and a "cooked" contact against the sandstones.
rockhopper wrote:Crikey, that's technical
Well, I didn't want to insult anyone's intelligence with a "soundbite" explanation. I was working on the principal that if 95+% of the contributors here can grasp the nuances of meterology, vector navigation and hydrodynamics (which judging by past discussions most of us can in spades), then a little geology 101 is withing the capability of nearly all ;-)
Nothing irritates me more than the creeping tendency over the last 10-15 years for so-called documentaries to dumb-down and increasingly gloss-and simplify their subject matter. Disect any "Discovery" type docu and you'll note that 60% is repetition and restatement of some fairly simple premise with no detail or analysis.
rockhopper wrote:...and we got to stay in a hotel.... 20 or so 15 year olds.... in a hotel (with a serving bar!)... !!!
Ceegee wrote: especially when viewed with a teenage hangover ;~s)
John N wrote:I keep thinking I ought to check out the Open University - see what they have to offer.
at the end you get a nice certificate that employers laugh at.
Owen wrote:John N wrote:I keep thinking I ought to check out the Open University - see what they have to offer.
I did that, be warned it takes all your money and all your free time, at the end you get a nice certificate that employers laugh at. Still fascinating subject and very worth doing.
I keep thinking I ought to check out the Open University - see what they have to offer
janet brown wrote:
Main problem I had was that the OU year runs from Feb-end of Oct, and we'd moved into a new house with garden that needed a lot of work, plus son became more time consuming!
Janet
Bards wrote:I believe the 'nodding donkey' at Kimmeridge is the oldest productive oil well in the world, and is a (tiny!) part of the largest onshore oilfield in W Europe. Some of the oil-shales (although not believed to be a direct source for the productive oil beds and quite sulphurous) are so hydrocarbon-rich they are inflammable, though I can't remember any of the infamous spontaneous flaming cliff incidents for the past 10 years or so.
Bards wrote:The importance of local Dorset strata in the early days of geological study as a modern science have led to the terms 'Kimmeridgian' and 'Portlandian' still being recognised worldwide today as names for discreet geological Ages.