Originally Posted by
Richie_B
As you can see, Ireland is sitting on the Eurasian plate but is nowhere near any place where tectonic plates meet. Despite this, we still have mountains. Without continental drift, I ask you (Balaam), how is this possible? The majority of the mountains here were formed during the Armorican foldings, which took place between 250 - 270 million years ago. (I hope you don't disagree with the methods used to date rocks too. :)) That is why the highest mountains would not be very tall considering how old they are. (The highest one is only about 1000 metres/3400 feet tall.)
This proves to me that at the time these mountains were formed, the land now known as Ireland, was on the edge of two plates (possibly as part of a super-continent) and then gradually drifted away into it's current position in the Eurasian plate.