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Mon 1st July 2013

Cragside Challenge Walk 2013

Cragside Challenge Walk 2013

Thanks to everybody who joined us on the 2013 Cragside Challenge Walk.


We had 150 starters on the day and the weather could have not been better. With great weather and lots of smiling faces it was a great day.


Please enjoy the pictures and the YouTube film and I very much hope you can join us again next year.


Mon 1st July 2013

Cragside Challenge Walk 2013 - Guided group

Cragside Challenge Walk 2013 - Guided group

Thank you to all the folk who selected the guided option for your company and for making my day easy. It was a great day - the weather was perfect not too much sun, the wind was light and the rain of the day before stayed away.

The route was the opposite way round when compared to previous years and this raised a good deal of comment from those who had done it before. The consensus seemed to be that this 2013 way round was better. It is for sure that the views were spectacular and even from the first few minutes wandering through the grounds at Cragside the whole route could be seen in glimpses through the trees. Personally I liked the finish because as soon as we got back into Cragside we were straight to the finishing post.


The guided group this year was a great mix of friends from last year and those who had been on the training walk and a number of new enthusiasts. The group gelled really well and apart from Lesley wandering off intent on completing the whole of the Simonside ridge by herself there were no incidents. I think that the training walk, which we introduced for the first time this year, proved to be beneficial. Familiarisation with the route and the amount of up and down is always useful to know and it helps the actual day to be more enjoyable because it reduces anxiety. For me as the guide it is always helpful to get to know the reasons why folk want to do a challenge walk and if I meet them on the training walks and learn what they want to do I can adjust my approach and help to achieve the target that folk set themselves.


My favourite moment on the day was when the whole group were on the carriageway above Cragside with a couple of miles to go. Everyone was together walking a a good pace and chatting in groups of 2 or 3. The sense of camaraderie and relaxation in the group  was great to see. Well done to you all and I look forward to seeing you at the next training walk (for the St Cuthbert's Way on 13th July) or the next walk I'm involved in. A special mention must be made for Muriel who walked the whole way without her insoles in her boots (she'd forgotten to replace them after drying her boots) - what an excellent effort and she only told me at the end. Finally good luck to Andy who is off to climb Kilimanjaro shortly - don't forget your hand sanitizer - good talking about that too.


We did 13.4 miles at moving average of 2.7 miles an hour. The whole walk with breaks took just over 6 hours.



Chris.

Mon 1st July 2013

Northumberlands Mississippi Blog

Northumberlands Mississippi Blog

28th June 2013

Flaming June it certainly was not; cool, wet and windy conditions prevailed with the cloudbase almost exactly on the top of Simonside.  Nevertheless we started off at Tosson Lime Kiln with a quick introduction to the Carboniferous Period of geological time, an even quicker look at the geological map of the area and a closer examination of the kiln itself which brought all of the elements of that particular period of the earth’s history together i.e. the ancient geography and climate and the geology comprising of local Fell Sandstone, coal and limestone.  Darren was happy when I got my tape measure out to show just how relatively recent the Carboniferous period actually was in relation to the total age of the Earth.  Best of all we were able to do all of this sheltered under the draw arches of the kiln itself but we eventually had to go and get wet noting the now disused quarry close by.  Up past the distinctive Iron Age hillfort of Burgh Hill and over the appropriately named Windy Crag we entered the Simonside Forest (i.e. large Forestry Commission conifer plantation) to shelter for elevenses half an hour late but welcome all the same.  I found everyone a nice spot to sit and was sent down the hill to eat my scone; I think that everyone wanted some peace and quiet!

Elevenses over it was onward and upward up the scarp face of the Fell Sandstone towards the edge of the trees via the packhorse trail grooves cut in the sandstone and the nearby possible Neolithic rock shelter as archaeologist have interpreted it, it must have been a draughty spot but it did get everyone looking at the current bedding structures in the rock face.  Out onto the forestry road below the Simonside Crags we could just see parts of the Cheviots with their contrasting rounded topography consisting of the granite masses of Cheviot and Hedgehope surrounded by the lavas of the former Cheviot Volcano (there may have been more than one volcanic cone but all evidence has long been eroded away).  By contrast the crags of Fell Sandstone were bold, sharp and distinctive with more or less concordant summits as far as we could see into the murky gloom.  On the climb up to the crest of the escarpment we had plenty of opportunity to see the sandy hillwash resulting from recent weathering and erosion and see the acid loving, heather dominated, vegetation associated with sandstone bedrock.  It was time to introduce everyone to topset, foreset and bottomset beds in the current bedding and to appreciate how these predominantly shallow water sediments were originally deposited in the massive delta that formed Northumberland’s Mississippi in water that was quite shallow.  The fact that these shallow water deltaic sandstones eventually accumulated to a depth of 300 metres plus had us looking for other mechanisms to explain this, that and a sincere desire to stop for lunch very soon.

A quick lunch was taken in the shelter of Old Stell Crag; it was too cool and windy to sit for long just at the cloudbase with no view.  We moved quickly over Dove Crag and onto The Beacon descending by the old 13th century deer park wall to have a quick look at the Beacon Solar Observatory (re)discovered in 1987 by David Thompson.  We soon located the Central Holed Stone (CHS) a long horizontal hole through a substantial block of Fell Sandstone aligned north-west to south-east.  David did confirm that the sun shone directly through the hole at sunset on the summer solstice of 1988.  We of course took the opportunity to look at the grain size distribution and cement between the sediments and draw parallels with beach environments today – well, I did anyway.  Down off the steeper slopes we crossed Lordenshaws car park to have a look at the cup and ring marks etched into the Fell Sandstone relatively recently, only about 4,000 years ago by early settlers in the area!    Over the moor past the Iron Age hillfort, younger still as this covered the period from approximately 800 BC to the arrival of the Romans in 43 AD and down to Whittondean Farm and Whitton Hillhead, both built of Fell Sandstone.  Then it was back to our cars via Tosson Tower, a pele tower and reminder of the days of the Border Reivers disputes along the Anglo-Scottish Border between the late 13th and early 17th centuries.  The huge facing stones of the tower (pele) were also of Fell Sandstone.

Thanks to Val, Darren, Selina, Maggie and Alan for your company, witty banter and interest, I hope that you enjoyed the geology even if the summer weather didn’t come up to par and that you see the distinctive Simonside Ridge, and the rest of the Northumberland Sandstone Hills, through different eyes whenever you manage to get out onto them in the future.  Geological history really is “deep time” compared to human history.  Remember Darren and the tape measure back at the lime kiln?


Richard


Monday, 01 July 2013