Glaciation in Britain only extended as far south as East Anglia. The British ice cap was centred on the Scottish Highlands. In Verona, you would have seen terminal moraines from the Alpine ice cap; of course, there are still remnants of the Alpine ice cap on the shape of the various Alpine glaciers.
It must be true, as a new Ordnance Survey calculation has recorded the height of Ben Nevis at 1,345 metres, rather than the previous 1,344 metres.
Sorry - not so. It's a fluvial feature - river gravels and so on. The furthest south the glaciers got was well north of London. I live on a moraine deposit; the Isle of Ely is pretty much what used to be called tillite or Boulder Clay. This is a handy resource (Geology of Britain viewer | British Geological Survey (BGS))! I am a geologist, though.
Peter Fretwell, he of penguin poo fame and a regular on the BBC, used to work for me. His PhD thesis was on raised beaches in Scotland. They're very prominent round the east coast of the Clyde.
I assume you meant "sea level" rather than "seashore", or maybe that the seashore was lower than it is nowadays due to the post glacial lift.
They're very obvious - the main road from Gourock south to Largs runs on one, with obvious sea cliffs on the landward side of the road. They're particularly visible on Great Cumbrae. In fact, that's why mobile coverage is (or perhaps was - it's a while since I've been there) so awful along that coast; the masts are on the raised beach, so often the signal is masked by the cliffs at the back of the raised beach.
Never assume anything. When I said "seashore" I meant what I said. The seashore was higher up the hill then, than it is now. Do you see a difference between seashore and sea level?
Scotland is half empty whilst southern England is full. I blame the SNP.
There are some interesting glacial features in north Devon. From erratics, U shaped valleys and Ice Wedges.
Well, North Devon - in fact everywhere south of the Severn Estuary, except, perhaps for the very northernmost part of Somerset (present day Avon!) - was never under ice. It would have been a peri-glacial environment - ice-wedges etc. but the U-shaped valleys must have an alternate explanation. I don't know the area very well myself - Exmoor is almost as far as I know - and Exmoor certainly isn't classic glacial terrain.
@AntarcticPilot you might be interested in the following links. While not as big as the U shaped valleys further north, the chap who pointed St Catherine's tor was a Geologist.
Perhaps local glaciers? The main ice cap certainly stopped further north and didn't cross the Severn Estuary. The photograph isn't particularly convincing, and inspection of the geological map says that the deposits in the flat-bottomed valley are alluvial, not glacial.
I believe the last glacier sheet stopped around the area of the (current) North Norfolk Coast. Hence the creation of the Cromer Ridge.
If the collection is representative of Canis familiaris, then thank you, but no.