Peter Miller wrote:

On 22 Aug 2009, at 12:03, Chris Hill wrote:

Well I'm pleased that they agree with me, but I'm not the oracle!  This is another source quoting the same general information.  Do the Scottish and Northern Irish counties generally extend to the low water mark too? Drawing from the NPE maps seems to be our only reasonable source for the low water mark.

Great stuff.

Low water does however change much more rapidly that high water so NPE is the 'least good' source of that date as it is 50 years old. If one is fortunate enough to have detailed enough recent aerial photography that that should be used.
The biggest problem with aerial photos is that you don't know what the state of the tide was at the moment the photo was taken.  You can sometimes guess a high water mark on a beach by the strand line, but low water is always covered except at low water.

Fyi, for Suffolk the low water mark has changed by 50 meters in places in the past 5 years (huge amounts of shingle has arrived near Felixstowe Ferry extending low water by that amount since I have lived in the area). Even the high water mark has moved by many meters over 50 years in some places including Dunwich. One can see the different in Potlatch comparing the OSM coastline with NPE base mapping.

The coast along the East Riding eroded by at least 50 metres, about 100 metres in a few places in the 50-60 years since NPE.  i have been trying to estimate the low water mark from a combination of NPE and aerial photos of the cliff line, then moving the low water mark inland by the same amount as the cliff has moved.  Still an estimate, but a bit better than NPE (not much updated yet).  A visit with a GPS and a camera helps, but low water is very hard to measure on the ground over any distance because the tide comes in as you walk along!  GPS and camera helps with man-made changes.
We have good yahoo aerial photography for pasts of the coast in Suffolk.

However... I support the idea we use best low-water source availale for each area. It might be good to create areas between high and low water tagged with 'shingle', 'beach' etc.
Sometimes the beach or foreshore reaches much higher than the high water mark, but not usually on quickly eroding coastlines so NPE would be good there.

Should be also use low water as the edge of 'Wales' itself or has any evidence for the 3 mile limit mentioned by the wiki by someone been found? 

Good question, and what about the 12nm limit?

Regards,


Peter
Cheers, Chris
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