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There can’t be another short walk in the country where you can search out the fossil plants and animals from hundreds of millions of years ago including the oldest recorded amphibian footprints, walk across evidence of ancient earthquakes, touch rocks that were once 1200° molten magma and see the debris left by the last ice sheet to cover England, stroll past the site of a 10,000 year old Stone Age house, search out the tree stumps of a drowned forest where those Mesolithic people hunted, gaze at reefs that wrecked over 20 ships, look enviably of the bathing house built by a Prime Minister who invented a different cup of tea, smell kippers been smoked and all the time be surrounded by amazing wildlife.

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This the final part of this rail journey from close to the west coast of England to the east coast, starts in Hexham and finishes in Newcastle upon Tyne. On the way there's a little discussion about geological maps and their availability and accuracy. But mainly we'll be looking at the geology and landscape - the river deposits and the valley - the challenge such valley routes present to engineers and the coal that was is important to not only the economy of this line - but also to the invention of railways themselves.

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We got as far as Brampton station last time. We have changed bedrock from the red Triassic sandstones of the west to 335 to 310 million year old Carboniferous strata – a repeating mix of layers of sandstone, shale, limestone and coal. A product of different past environments when the tectonic plate we were part of was on the Equator.

Back then the land and sea kept changing places. Shallow coral seas produced the limestones, when sea level fell the environment became brackish coastal muddy lagoons – laying down the shales, which were then covered by sand from large rivers – the sandstones, and in turn they were covered by vegetation and swamps – ultimately decaying and compacting to form coal seams.

That repeating sequence of rocks – initially with more marine deposits like limestone and as we get closer to Newcastle – more land deposits like sand, mud and coal – is the story of the Carboniferous. Not that we will see much of it directly, this rail journey takes us through a landscape who’s shape and sediments owes most to that last glaciation, its melting and the action of rivers and gravity since.