Wild Camping On Grasmoor Lake District

Posted in Grasmoor Lake District on July 25th, 2011 by David Murphy

 

On the 18th September 2011 I parked along side Crummock Water in the Lake District to hike up to Grasmoor for a bit of Wildcamping on the summit.
Walking on Lad Hows Ridge between Cinderdale Beck on the left and Rannerdale Beck to my right, the summit is only 1.6 miles away.

I arrived and parked along side Crummock Water around 4.30pm I purposely left it late been a sunday I didnt want to arrive on the summit too early as I have done in the past, Ingleborough to name one where I was hanging around for hours before I was able to pitch without scores of hikers on the summit, this time was a miss judgement.
I didnt estimate the time it would take to the summit via lad Hows Ridge it was a challenge I didnt expect, very tiring on the legs and some scrambling near the top was needed.
Near dark on reaching the summit entering low cloud my great views a few hundred feet lower had gone wish I put my tent up lower down when I said in my video would have witnessed a great sunset  instead rain and wind and no views this brings back many bad memories with Paul lol
I proceeded to errect the Akto in thick fog by this time, and thought to myself I would get a brew of tea on quick sharp then Daves Wild Camping Kitchen was in full swing on the menu this even was Sheperds Pie and Chicken Korma “Pack’n’ Go” from Be-Well Ltd and how nice of a change for me they were, easy cooked with 350ml of boiling water stir and leave to stand for 6 mins.
After spending all the evening a prisoner in my tent due to rain I read the newspaper and then it was time to retire, I woke several times during the night to look out the opening in the top of my door hoping but not expecting to see stars only to see the same fog, it never shifted all night.

Morning came I had my alarm set for 6.20am to catch what I didnt really expect to see, the sunrise and there was no change at all a thick covering no views whatsoever, I turn back over to sleep till around 9am when I got up to my breakfast, Cereal Start “Pack’ n’ Go” by Be-Well ltd.

 I started to packup my tent then the heavens opened I got soaked 🙁 on walking back to the car I was hoping I didnt leave the headlights on, all was well.

Thanks for reading and supporting my website with your comments, till next time,

David Murphy
Daves Wildcamping

My Route up Grasmoor

Grasmoor Summit Shelter

Hilleberg Akto Summit of Grasmoor

My Akto On Grasmoor

View of Crummock & Buttermere

View from Lad How on way Up to Grasmoor

View from to Grasmoor Summit

Waterfall on way back down

My Actual Route

 

Grasmoor
Grasmoor.jpg
The huge bulk of the Grasmoor mountain seen over the Crummock Water valley
Elevation 852 m (2,795 ft)
Prominence 519 m (1,703 ft)
Parent peak Scafell Pike
Listing Marilyn, Wainwright, Hewitt, Nuttall
Location
Grasmoor is located in Lake District
Grasmoor
Cumbria,  England
Range Lake District, North Western Fells
OS grid NY174203
Coordinates 54°34′16″N 3°16′45″W / 54.57115°N 3.27918°W / 54.57115; -3.27918Coordinates: 54°34′16″N 3°16′45″W / 54.57115°N 3.27918°W / 54.57115; -3.27918
Topo map OS Landranger 89, 90, Explorer OL4

Grasmoor is a mountain in the north-western part of the Lake District, northern England. It is the highest peak in a group of hills between the villages of Lorton, Braithwaite and Buttermere, and overlooks Crummock Water.

Grasmoor is distinguished by its steep western flank, dropping dramatically to Crummock Water. This face is however not suitable for rock climbers as there is little clean rock, although Alfred Wainwright describes a challenging route up the face in his Pictorial Guides to the Lakeland Fells.[1] To the east the fell is linked to others by Crag Hill and Coledale Hause. Grasmoor is also home to the most extensive scree slopes in the North Western Fells.

Name

Grasmoor takes its name from the Old Norse element grise, meaning wild boar. This element appears in other Lake District place names, including Grisedale Pike and Grizedale Forest.[1]

Topography

The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter Pass and Newlands Pass, includes Grasmoor.

The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Grasmoor has the greatest elevation, although Crag Hill stands at the hub of the range.

From the valley floor near Little Town at the eastern end, the ridge requires four miles (6 km) of gradual ascent to attain the summit of Grasmoor. Starting at the shores of Crummock Water in the west, the same is achieved by a single slope of scree in less than a quarter of the distance. Grasmoor is Lakeland's terminal height par excellence.

The summit area is a gently domed promenade of moss and short grass,[1] running along the ridgeline with a narrow constriction in the middle. This is created primarily by the scooped-out bowl of Dove Crags on the northern face. To the east of this plateau are broad smooth slopes descending to a wide unnamed col at 2,368 ft (722 m). This connects onward to Crag Hill. At the western end the summit area narrows, culminating at the subsidiary top of Grasmoor End (2,445 ft) which crowns the western face. Great fans of scree descend to the lakeside road below. Grasmoor has one minor ridge which descends south westward over Lad Hows (1,397 ft) before a steeper fall to the valley floor.

To the south of Grasmoor is the valley of Rannerdale, which flows to Crummock Water between Lad Hows and the neighbouring Wandope. This drainage is supplemented by Cinderdale Beck, separating Lad Hows from the main body of the fell. The northern flank of the ridge stands above Liza Beck. This stream also makes due west for Crummock Water, but is diverted northward by the low top of Lanthwaite Hill to join the Cocker after its exit from the lake. An area of lowland to the north west is thus annexed to Grasmoor from the natural territory of Whiteside.

Geology

The surface rocks of Grasmoor are composed primarily of the Ordovician Kirkstile Formation. These are laminated mudstone and siltstone, typical of the Skiddaw range.[2] There is no history of mining beneath the slopes of Grasmoor.[3]

Summit and view

The top of the fell lies toward the western end of the summit plateau, marked by a huge sprawling cairn. There are many smaller cairns and the top is characterised by sheep-mown grass.[1] The view is extensive although robbed of some foreground by the extent of the summit. All of the major Lakeland ranges are in sight with the exception of the Far Eastern Fells, with High Stile above Crummock Water perhaps the highpoint.[1] This is best seen from the western end of the plateau.[4]

Ascents

The obvious way is direct up the screes from Lanthwaite on the Crummock Water road, picking through the rock scenery above to appear on Grasmoor End from the north west. This involves 2,000 ft (610 m) of ascent in about half a mile. From the same starting point a detour along Liza Beck/ Gasgale Gill can be used to give access to the northern slopes. A way can then be found almost direct to the summit around the rim of Dove Crags. From Rannerdale a choice of routes arises, either climbing the Lad Hows ridge or following Red Gill a little to the west. Finally Coledale Hause can be used to gain the main ridge between Crag Hill and Grasmoor. This can be reached from Lanthwaite or as the first objective of a longer march from Braithwaite in the east. Coledale Hause connects to Hopegill Head and the fells to the north, providing further indirect possibilities.[1][4] The summit was conquered by a Rolls Royce in 1982.[citation needed]

References

  1. ^ a b c d e f Alfred Wainwright: A Pictorial Guide to the Lakeland Fells, Book 6, The North Western Fells: Westmorland Gazette (1964): ISBN 0-7112-2459-5
  2. ^ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 29: BGS (1999)
  3. ^ Adams, John: Mines of the Lake District Fells: Dalesman (1995) ISBN 0-85206-931-6
  4. ^ a b Bill Birkett: Complete Lakeland Fells: Collins Willow (1994): ISBN 0-00-713629-3

External links

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Great End Lake District Cumbria

Posted in Great End on June 28th, 2011 by David Murphy

Its the 29th June 2011 Myself, Paul my usual Wildcamping partner and Chris this will be my second Wildcamp with Chris on a Hill right next to our first one Great Gable.

I Planned two Routes both of which are from Seathwaite one would take us past Styhead Tarn and Springling Tarn which was 4.4 miles but we all decided to take the shorter Route along Grains Gill below.  

Steak

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Our Tents In The Mist

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Cloud Over Great Gable

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Out of the Breeze in Shelter

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Myself Paul and Chris

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Great End Looking Up Grains Gill

Scafell Pike from Great End

Looking Down to Springling Tarn from Great End

Great End
Great end.jpg
Great End from the top of Grains Gill
Elevation 910 m (2,986 ft)
Prominence 56 m (184 ft)
Parent peak Ill Crag
Listing Hewitt, Wainwright, Nuttall
Location
Great End is located in Lake District
Great End
Cumbria,  England
Range Lake District, Southern Fells
OS grid NY226084
Coordinates 54°27′50″N 3°11′38″W / 54.464°N 3.194°W / 54.464; -3.194Coordinates: 54°27′50″N 3°11′38″W / 54.464°N 3.194°W / 54.464; -3.194
Topo map OS Landrangers 89, 90, Explorer OL6
Listed summits of Great End
Name Grid ref Height Status
Round How NY218081 741 m (2,431 ft) Nuttall

Great End is the most northerly mountain in the Scafell chain, in the English Lake District. From the south it is simply a lump continuing this chain. From the north, however, it is appears as an immense mountain, with an imposing north face rising above Sprinkling Tarn (lake). This is a popular location for wild camping, and the north face attracts many climbers.

Alfred Wainwright wrote of Great End in his Pictorial Guide to the Lakeland Fells: "This is the true Lakeland of the fellwalker, the sort of terrain that calls him back time after time, the sort of memory that haunts his long winter exile. It is not the pretty places - the flowery lanes of Grasmere or Derwentwater's wooded bays - that keep him restless in his bed; it is the magnificent ones. Places like Great End..."[1]

Topography[edit]

The imposing north eastern cliffs, riven by gullies, rise some 600 ft from the Esk Hause path. Their orientation ensures that the sun rarely reaches them, the gullies often retaining snow well into the spring. From the left when viewed from below the principal fissures are South East Gully, Central Gully and Cust's Gully (see below). To the west of the cliffs a ridge descends more gradually in the general direction of Sty Head. This is known as The Band, and it too sports a harsh gash across its features. On the western side of The Band is the deep ravine of Skew Gill, a tributary of Wasdale-bound Lingmell Beck. At the base of The Band the ridge continues as the complex top of Seathwaite Fell, replete with numerous tarns.[1] The largest is Sprinkling Tarn with its beautifully indented shoreline providing perfect foreground for views of the cliff.

Sty Head is one of the focal points of the District for walkers. The name strictly applies to the col between Great End and Great Gable at a height of 1,560 ft, but is now more generally given to the path which crosses it. This connects two of the most popular starting points for walks in the high fells, Wasdale Head and Seathwaite. Sty Head is also a walker's crossroads with other paths leading direct up Great Gable and following the outflow of Sprinkling Tarn up to Esk Hause.

Westward from the summit Great End makes a rocky descent toward the arms of Lingmell Beck. This flank is crossed by the Corridor Route, the popular path to Scafell Pike from Sty Head. Above the path are the subsidiary top of Round How (a Nuttall) and the tiny, beautifully clear tarn of Lambfoot Dub.[2][3]

The southward ridge to the Scafells crosses a shallow saddle and then climbs over Ill Crag and Broad Crag, a well blazoned path leading across the stony terrain to the summit of Scafell Pike. To the east of the first depression is Calf Cove, its easy slopes leading down to Esk Hause.

The summit has two cairns of very similar height, that to the north west being nearer to the cliff edge and having the better view. Northwards along Borrowdale the vista is unsurpassed, but the whole panorama is excellent. The heads of the gullies can also be approached for startling views down the face.[1]

Geology[edit]

The summit is formed by the laminated volcaniclastic claystone and siltstone of the Esk Pike Formation overlying the dacitic welded lapilli-tuff of the Lincomb Tarns Formation. The latter is revealed in the great north front.[4]

Ascents[edit]

Great End may be ascended from Sty Head Tarn via The Band (not to be confused with the more famous Band on Bowfell), from Wasdale Head along Lingmell Gill and Spouthead Gill, from Borrowdale via Grains Gill, from Great Langdale via Rossett Gill and Esk Hause, or from Eskdale. As an intermediate objective Great End may easily be climbed from the main path between Esk Hause and Scafell Pike, requiring only a detour of some 400 m.[3]

Cust's Gully[edit]

Cust's Gully at the western end of Great End's cliffs is named after 19th-century pioneer climber and sketcher Arthur Cust, a classical scholar from Yorkshire also known for his watercolour sketches of the Matterhorn and Mont Blanc. Cust's Gully is a Grade 1 rock climb, but a difficult obstacle for walkers ascending from Sprinkling Tarn. Cust's first winter ascent of the gully was recorded in 1880, although he is thought to have ascended it earlier.

References[edit]

  1. ^ a b c Wainwright, A. (2003). "Great End". A Pictorial Guide to the Lakeland Fells, Book 4 The Southern Fells. London: Francis Lincoln. p. 2. ISBN 0-7112-2230-4. 
  2. ^ Blair, Don; Exploring Lakeland Tarns; Lakeland Manor Press (2003); ISBN 0-9543904-1-5
  3. ^ a b Richards, Mark: Mid-Western Fells: Collins (2004): ISBN 0-00-711368-4
  4. ^ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 38: BGS (1998)

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Hiking in the Cheviots and WildCamping

Posted in The Cheviots on March 28th, 2011 by David Murphy

In 2008 I set off from Wooler in Northumberland for a Hike through the Cheviot’s and a planned wild camp alone after around 5 miles hike i believe i had to find somewhere to pitch my tent, this was my first try of my Hilleberg Akto.

 

Been my first time out Wildcamping by myself I was a little nervous when in the pitch black with only the sound of a river next to me, in the morning I hiked up the Cheviot great views on the way up but i thought I would save my battery power for some better photos from the summit, which I was met with a flat boggy top with no views very disappointing.

 

The Cheviot
The Cheviot from Broadhope Hill.jpg
The Cheviot, from Broadhope Hill
Elevation 815 m (2,674 ft)
Prominence 556 m (1,824 ft)
Parent peak Broad Law
Listing Marilyn, Hewitt, County Top, Nuttall
Location
Location Cheviot Hills, England
OS grid NT909205
Topo map OS Landranger 74/75

The Cheviot is the highest summit in the Cheviot Hills in the far north of England, only 2 km from the Scottish border. It is the last major peak on the Pennine Way, if travelling from south to north, before the descent into Kirk Yetholm.

Other than the route via the Pennine Way, most routes up The Cheviot start from the Harthope Burn side to the northeast, which provides the nearest access by road. The summit is around 5 km from the road-end at Langleeford. There are routes following the ridges above either side of the valley, and a route that sticks to the valley floor until it climbs to the summit of The Cheviot from the head of the valley.

Although the Pennine Way itself does a two-mile out-and-back detour to the Cheviot, many walkers who come this way omit it, since the stage (the last) is 29 miles long.

The Pennine Way approaching the summit of The Cheviot

The summit of the Cheviot is very flat. It is an ancient, extinct volcano[citation needed]. It is covered with an extensive peat bog up to 2 m deep; the Northumberland National Park authority have laid down stone slabs on the main access footpath to prevent erosion damage to the peat and to make access to the summit safer for walkers.

North of the summit, in the peat bogs, are the remains of a crashed B-17 bomber, which hit the mountain due to a navigational error in World War II. The more recognisable pieces of wreckage have been removed, but pieces of the aircraft can still be found.

The landing gear of a B-17 bomber that crashed in World War II.

View

A smoke grenade found near the summit of The Cheviot. The area around the mountain is used for training by the British Army.

The view is obscured greatly by the flatness of the summit plateau. Nevertheless, on a clear day the following are visible (from west, clockwise); Broad Law, Moorfoot Hills, Pentland Hills, the Ochils, Lammermuir Hills, Lochnagar, Ros Hill, Long Crag, Urra Moor, Tosson Hill, Burnhope Seat, Cross Fell, Helvellyn, Scafell Pike, Skiddaw, Sighty Crag, Peel Fell, Queensberry.

External links

Coordinates: 55°28′42″N 2°08′44″W / 55.47823°N 2.14553°W / 55.47823; -2.14553

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