3. Mud

Our regional landscape has its origins in mud on the seabed, so at this point in our trudge through the stygian gloom of geological history, let us take a closer look at that mud, in all its various flavours, gloopy, crumbly and the various types of stone that it morphed into. Apologia. The passively interested reader might find this the most stultifyingly tedious post on this blog, with graphics that are awe-inspiringly uninspiring, even compared with the low standards I set. It is here for the sake of completeness and because, worryingly, I think that mud has a story to tell. But you might find it helps you to doze off. While tootling around the planet on its way toward its current position on the globe, South East England often found itself in a liminal zone between land and sea, sometimes one and sometimes the other, depending on the sea levels. What we see today is based on the compacted sediments of sand, gravel and biological detritus th...