Saturday, April 27, 2013

Pike of Blisco from Three Shire Stone 2007






www.trekkingbritain.co.uk presents Pike of Blisco from Three Shire Stone walk from March 2007 all by myself wild camping. Visit the Trekking Britain website for more info on this walk...
Video Rating: 4 / 5









walking from keswick to mt skiddaw, camping overnight, then back around to keswick
Video Rating: 5 / 5


Wednesday, April 24, 2013

Christmas In The Lake District Idyllic

We've all been warned that the snow is heading this way, it's the middle of November and the bets are being placed for another white Christmas! Will it or won't it? The tips of the Lakeland Mountains are covered with snow, but at such a distance we cannot make out whether the depth is adequate to justify a white Christmas. How does the white Christmas bet system work anyway? Is it based on snow actually falling on this festive day or does it mean to wake up on this day, to draw back your curtains and be greeted with a white feathery like view?
Either way whether this is on or prior to the day there really is nothing better than to wake up on one of the most glorious days known to man, with a crackle of the fire in the background and ever so melting scent of mulled wine seeping through.

The perfect vision, the idyllic dream of waking up on Christmas morning with the greeting of excited children scampering into the bedroom to enthuse you with the same enthralling attitude they have, to jump onto the bed ever so lively while you lie toasty under the feather filled duvet, daring to dip your toe out into the air.

When energy gained and a certain percentage of enthusiasm has been allowed to grasp you, you are then able to take a leisurely stroll into the living quarters where yet again the children ensure you are wide awake by ever so kindly increasing the volume as well as adding musical notes to the unwrapping of their gifts. This is now the time where the mulled wine or bucks fizz comes into play, a large glass of your favourite Christmas tipple first thing in the morning is acceptable on this particular day, besides it's so full of snow out there, there is certainly no way you are willing to take the risk of venturing into the frozen midst of the beautiful Lake District while you can enjoy the comfort of your log fire and the magnificent view on your terrace.

If you are lucky enough to stay in a cottage with an Aga then Christmas dinner is a case of letting the Aga do the work, alternatively you may be also be lucky enough to stay in a Lake District village with restaurants that are open for Christmas day, in which case do ensure it is not far to walk as to make plans for journeys using your vehicle at this time of the year in the Lake District is not a wise idea!

Whatever your plans your Christmas in the Lake District is a sure set winner, there really is no better place to be at this magical time of year with or without children, the Lake and mountainous terrain add further sparkle and the crackling of the fire the smell of the fire fumes that add warmth to the cold night air, brings back all memories of Christmas past, present and for the future.

Sunday, April 21, 2013

Corrie basins in the Lake District

One striking feature of corrie basins is the way in which the majority have a north or northeast aspectThings to do in Windermere
. There are obvious exceptions like those which serrate the southern slopes of Blencathra, but taken as a whole a northeast orientation is dominant. It is this preferential development which gives many 66 of the ridges their asymmetrical appearance. No greater contrast of landforms exists than on the opposing sides of Helvellyn or the internally ridge separating Ennerdale and Buttermere.

On the one side are smooth even slopes broken occasionally by rock crags and low precipices while on the other glacial erosion has bitten deeply and successfully to create what has been called 'biscuit topo¬graphy'.

With rock type not exerting any great influence, other explanations have to be sought to account for the preferential northeast aspect. As early as 1917 Enquist noted that the aorries tended to lie on the lee side of a mountain range, that is in relation to the dominant snow bearing wind. More recently Manley has shown that in this situation the wind which blows over the ridge top the helm wind considerably aids snow accumulation on the upper part of the lee slope through the development of a back eddy. The presence of the eddy can often be detected on the waters of a tarn where wavelets move towards the back¬wall of the corrie basin. During the Ice Age thick snow would be likely to accumulate in any hollow on the lee slope, and through the addition of successive layers be ultimately transformed into ice.

In time this ice would gouge out a deeper hollow and ultimately a true corrie basin. Having reached this stage, the rapid build up of snow and ice would bring about increased erosion of the floor of the hollow. Due to the effect of the helm wind, the greatest amount of snow would accumulate on the upper part of the corrie glacier just below the bare upper part of the backwall. Differential loading on the upper surface of the corrie glacier would tend to cause the ice to move in a rotatory manner. With continuous additions at the head and constant depletion at the snout through melting, the rotatory movement could be instrumental in scooping out the floor of the corrie .

Other processes like frost shattering of the bare rocks of the upper part of the backwall and the grinding action of rock debris within the glacier would also contribute to the enlargement of the corrie basin. It follows that if the prevailing snowbearing wind was from the southwest then the northeast facing lee slopes would become the most suitable sites for corrie development. This northeast aspect also happens to be one of minimum isolation so that snow and ice would persist longer here. When the snow had long since disappeared from the upland peaks and plateau tops, some of the deep shadowy hollows would retain their active glaciers. Even today snow patches last until late Mayor early June in situations like the steep northfacing buttress of Great End.

Wordsworth, in his poem Fidelity, mentioned the persistence of snow under the lee of Helvellyn which he had noticed on a walk across to Patterdale in early June. The ice which was so prominent in fashioning the landscape of the central high part of the Lake District also left its mark in the peripheral lowland, though to different effect. Here various ice streams jostled for occupation of the low ground. In addition to the local glaciers fanning out from the mountainous core, a great wall of ice moved in from the Irish Sea and impinged on the western coasts. Passing over the softer rocks of the lowlands, the ice was able to incor¬porate great quantities of sands, clays and rocks which it subsequently deposited on melting. In contrast to the highland area, the glacial landforms of the margins 68 are nearly all associated with deposition rather than erosion.

Saturday, April 20, 2013

Railways And Tourism In The Lake District

However, other routes clearly had tourist potential, and the Lakeside and Coniston lines turned increasingly to this source of revenue. The Furness Railway also encouraged the development of select seaside resorts at Seascale and Grange. At Seascale a grandiose design never came to fruition, the location being too remote. However,Grange became quite a success as a retirement resort, although it never took off as a centre for family holidays; it was essentially a genteel seaside version of residential Windermere.

Rail closures began in the 1920s and continued through to 1972 with the final closure of the Penrith to Keswick line. Tourism was not the saviour of the railways, chiefly because the companies did not rise to the challenge it presented. Perhaps if the closures had been postponed only a few years, more lines would have survived, for some of the railways once feared by Wordsworth and Ruskin have come to be revered as tourist attractions in their own right.

If many lines were short-lived, their impact on the landscape was immense; within a few years green fields sprouted mines and quarries, with all their buildings and spoil tips. The arrival of the railways allowed the minerals to be mined and then used in industrial processes; mining villages and industrial hamlets sprang up in the landscape, and some settlements such as Aspatria, Harrington, Frizington and Millom grew into sizeable towns. The established towns such as Maryport and Workington grew as well; Whitehaven by contrast was already a town of 20,000 in 1851, and grew more slowly.

The effects of the railways were complex; they did not always allow rural industries to survive, but agriculture benefitted by being able to send milk, butter, cheese and meat to the industrial towns. They allowed local people to migrate out of the Lakes, whilst allowing other workers to migrate in (notably to Cleator Moor); tourist access was meanwhile dramatically improved. They provided employment both in the construction and the running of the lines, yet their impact was concentrated on the industrial development of the mining areas and the ports, to the detriment of much of the rest of the area; in a few years the whole social and economic pattern of life in the Lake District, and more especially around the Lakeland margins, was radically altered.
Little now remains of many lines; some are neglected and overgrown, rapidly disappearing into the landscape, with their station buildings converted into houses, whilst others have suffered the indignity of having roads built over them (notably the Keswick to Cockermouth line). The wheel has now come full circle, and the brief intervention by the railways in the provision of transport in the Lake District is essentially over.

Thursday, April 18, 2013

A Lake District Trip with my Brother






Extended version of a trip to the Lakes with my brother
Video Rating: 0 / 5









Pictures and video from camping trip with friends at Waterside House Camp Site, Pooley Bridge on Lake Ullswater in the Lake District.


Castlerigg Hall Caravan And Camping Site, Keswick. 2002






HAVE YOU TWIGGED THE ACCENT YET DAVID? www.castlerigg.co.uk
Video Rating: 0 / 5


Tuesday, April 16, 2013

Sharp Edge & Blencathra (Wild Camping) - 9 & 10 April 2011






Wild camping at Scales Tarn beneath Blencathra in the Northern Fells of the Lake District. We set off from Mungrisdale at about 8:10pm, climbing Souther Fell under moonlight before reaching our wild camp location at Scales Tarn about 10:00pm. The following morning we took a similar route to a previous walk, climbing Blencathra via Sharp Edge, then heading to the Bannerdale Crags and Bowscale Fell before descending steeply to Bowscale Tarn before returning back to Mungrisdale. The weather was perfect both days.
Video Rating: 5 / 5