This clay is from a core sample taken on another raised bog, Kirkconnel Flow in Dumfries and Galloway. It was deposited there at the end of the last ice age around 10,000 years ago.
This clay is from a core sample taken on another raised bog, Kirkconnel Flow in Dumfries and Galloway. It was deposited there at the end of the last ice age around 10,000 years ago.
Robin A Crawford 