Discover the Mystery of Siccar Point rocky promontory in Scotland
If you have keen interest to dip delve into nostalgic past and take essence of the historical anecdotes related with old castles and shrines scattered in different corners of the globe totally out of the view of those who find pleasure in trodding on those untouched places you have to set foot on Siccar Point rocky promontory in Scotland, United Kingdom.
It is such a place where you are sure to be overwhelmed to view the very small hill fort constructed by the Britons who ruled over the entire area. There lies near by the ruins of an old chapel of the then time too.
Simple itinerary
All you have to do right now is to reach the parish of Cockburnspath formerly known as the Old Cambus parish.
Just take a small journey westward and you are amazed to view the ancient culmination of artistry and architechture depicted on the rocks with which the St Helen’s Chapel and the fort were once built.
It can be told with ease that the engineering innovation of the by gone days with the red standstone in a splendid Romanesque style is nothing but a wonder to the modern man.
The real wonder underneath
While you are on the mood of watching the engineering structure of the forgotten days of the Siccar Point rocky promontory in Scotland, I am going to inform you that the rocks with which the Chapel and the surrounding walls were constructed, were quarried from the Greenheugh Bay and the Greywacke rock nearby.
How the old artisans made the wonder is cetainly a matter of sheer mystery to those who are interested to find out the ABC of perfection with which the old constructions are actually tinged with.
Gelogical wonder
Yes, the Siccar Point rocky promontory in Scotland is ready to offer you another information too.
The Point is notable as it has taken a worthy place in the realm of geology as James Hutton and his associates noted the angular unconformity there that stirred the world with the uniformitarian thoery in the year 1788.
Undoubtedly the theory brought an epoch in the development of geology in the later period.
