The Lake District

Haweswater is a reservoir in the English Lake District, built in the valley of Mardale in the county of Cumbria. The controversial construction of the Haweswater dam started in 1929, after Parliament passed an Act giving the Manchester Corporation permission to build the reservoir to supply water for Manchester. At the time, there was public outcry about the decision, as the valley of Mardale was populated by the farming villages of Measand and Mardale Green and the construction of the reservoir would mean that these villages would be flooded and lost and the population would have to be moved. In addition, the valley was considered one of the most picturesque in Westmorland and many people thought it should be left alone. Haweswater is a reservoir in the English Lake District, built in the valley of Mardale in the county of Cumbria. The controversial construction of the Haweswater dam started in 1929, after Parliament passed an Act giving the Manchester Corporation permission to build the reservoir to supply water for Manchester. At the time, there was public outcry about the decision, as the valley of Mardale was populated by the farming villages of Measand and Mardale Green and the construction of the reservoir would mean that these villages would be flooded and lost and the population would have to be moved. In addition, the valley was considered one of the most picturesque in Westmorland and many people thought it should be left alone. Originally, Haweswater was a natural lake about four kilometres long, almost divided in two by a tongue of land at Measand; the two reaches of the lake were known as High Water and Low Water. The building of the dam raised the water level by 29 metres (95 feet) and created a reservoir six kilometres (four miles) long and around 600 metres (almost half a mile) wide. The dam wall measures 470 metres long and 27.5 metres high; at the time of construction it was considered to be cutting-edge technology as it was the first hollow buttress dam in the world, being constructed using 44 separate buttressed units joined by flexible joints. There is a parapet, 1.4 metres (56 inches) wide, running the length of the dam and from this, tunnelled supplies can be seen entering the reservoir from the adjoining valleys of Heltondale and Swindale. When the reservoir is full, it holds 84 billion litres (18.6 billion gallons) of water. The reservoir is now owned by United Utilities plc and plays a vital role in supplying about 25% of the North West's water supply. Before the valley was flooded in 1935, all the farms and dwellings of the villages of Mardale Green and Measand were demolished, as well as the centuries-old Dun Bull Inn at Mardale Green. The village church was dismantled and the stone used in constructing the dam; all the bodies in the churchyard were exhumed and re-buried at Shap. Today, when the water in the reservoir is low, the remains of the submerged village of Mardale Green can still be seen as stone walls and the village bridge become visible as the water level drops. Manchester Corporation built a new road along the eastern side of the lake to replace the flooded highway lower in the valley, and the Haweswater Hotel was constructed midway down the length of the reservoir as a replacement for the Dun Bull. The road continues to the western end of Haweswater, where a small car park has been built; this is a popular starting point for walkers who want to climb the surrounding fells of Harter Fell, Branstree and High Street. A map of Haweswater Reservoir from 1948 Lake District writer and fell walker Alfred Wainwright had this to say on the construction of the Haweswater dam in his A Pictorial Guide to the Lakeland Fells: "If we can accept as absolutely necessary the conversion of Haweswater [to a reservoir], then it must be conceded that Manchester have done the job as unobtrusively as possible. Mardale is still a noble valley. But man works with such clumsy hands! Gone for ever are the quiet wooded bays and shingly shores that nature had fashioned so sweetly in the Haweswater of old; how aggressively ugly is the tidemark of the new Haweswater!"

Wast Water or Wastwater (/ˈwɒst.wɔːtər/ WOST-waw-tər) is a lake located in Wasdale, a valley in the western part of the Lake District National Park, England. The lake is almost 3 miles (4.8 km) long and more than one-third mile (540 m) wide. It is the deepest lake in England at 258 feet (79 m), and is owned by the National Trust. It is one of the finest examples of a glacially 'over-deepened' valley. The surface of the lake is about 200 feet above sea level, while its bottom is over 50 feet below sea level. The head of the Wasdale Valley is surrounded by some of the highest mountains in England, including Scafell Pike, Great Gable and Lingmell. The steep slopes on the southeastern side of the lake, leading up to the summits of Whin Rigg and Illgill Head, are known as the "Wastwater Screes" or on some maps as "The Screes". These screes formed as a result of ice and weathering erosion on the rocks of the Borrowdale Volcanic Group, that form the fells to the east of the lake, towards Eskdale. They are approximately 2,000 feet, from top to base, the base being about 200 feet below the surface of the lake. A path runs the length of the lake, through the boulders and scree fall at the base of this craggy fell-side. On the northwestern side are the cliffs of Buckbarrow (a part of Seatallan) and the upturned-boat shape of Yewbarrow. Wast Water is the source of the River Irt which flows into the Irish Sea near Ravenglass.

Bowfell (named Bow Fell on Ordnance Survey maps) is a pyramid-shaped mountain lying at the heart of the English Lake District, in the Southern Fells area. It is the sixth-highest mountain in the lakes and one of the most popular of the Lake District fells. It is listed in Alfred Wainwright's 'best half dozen' Lake District fells.

Grasmere is one of the smaller lakes of the English Lake District, in the county of Cumbria. It gives its name to the village of Grasmere, famously associated with the poet William Wordsworth, which lies immediately to the north of the lake. The lake is 1680 yd (1540 m) long and 700 yd (640 m) wide, covering an area of 0.24 mi² (0.62 km²). It has a maximum depth of 70 ft (21m) and an elevation above sea level of 208 ft (62 m). The lake is both fed and drained by the River Rothay, which flows through the village before entering the lake, and then exits downstream into nearby Rydal Water, beyond which it continues into Windermere. The waters of the lake are leased by the Lowther Estate to the National Trust. The waters are navigable, with private boats allowed and rowing boats for hire, but powered boats are prohibited. The lake contains a single island, known as The Island.

Styhead Tarn is a tarn in the English Lake District, near the top of the Sty Head pass, at the head of Borrowdale. It is on the route from Wasdale to Borrowdale, and is therefore a well visited point in the Lake District. It is also passed by walkers ascending Scafell Pike from Borrowdale via the Corridor Route. It is permissible to fish the tarn which contains wild brown trout. The Styhead Gill is the tarn′s outlet which flows into the River Derwent.

Pavey Ark is a fell in the English county of Cumbria. It is one of the Langdale Pikes, lying to the north of Great Langdale, in the heart of the Lake District, immediately to the north-east of Harrison Stickle. From the shores of Stickle Tarn, Pavey Ark gives the impression of being a rocky ridge. In fact this is misleading, and the north-western side is simply an undulating area of moorland, rising towards Thunacar Knott. The summit plateau is characterised by tarns, rocky outcrops and bilberry terraces. Pavey Ark is the largest cliff in the Langdales, but faces east over Stickle Tarn and is less prominent from the floor of Great Langdale away to the south. The main face is a little over a quarter of a mile across and drops about 400 ft. To the south-west it merges into the crags of Harrison Stickle, while the northern end peters out into the valley of Bright Beck. Stickle Tarn is wholly within the territory of the Ark, a corrie tarn which has been dammed to create additional capacity. The stone-faced barrage is low enough not to spoil the character of the pool, and the water is used for public consumption in the hotels and homes below. The tarn has a depth of around 50 ft. The face is an outcrop of the formation named for the fell, the Pavey Ark Member. This consists of pebbly sandstone and breccia and is set within the Seathwaite Fell Formation of volcaniclastic sandstone with interbeds of tuff, lapilli-tuff, breccia and conglomerate. Pavey Ark is most often climbed from the New Dungeon Ghyll Hotel, located some 1 1⁄4 miles (2.0 km) to the south. The route follows Mill Gill up to Stickle Tarn, which can also be reached via a much less popular and more strenuous path following the Dungeon Ghyll ravines. From Stickle Tarn there is a choice of routes; one of the most popular is to follow a diagonal slit on Pavey Ark's craggy south-eastern face. This route is known as Jack's Rake, and requires scrambling. Alternative, easier, ascents are available on either side of the main crag. Jack's Rake is the most famous ascent of the Pavey Ark precipice. It is classified as a Grade 1 scramble, but it is within the capability of many walkers, though it does require a head for heights and is considerably harder in bad weather. The rake starts beneath the East Buttress at the precipice's eastern end, near a large cairn (with a tablet marked 'JWS 1900') immediately north of Stickle Tarn, and then climbs west across the face of the crag. The rake follows a natural groove in the precipice face and is clearly indicated by several Ash trees. Wainwright wrote that for fellwalkers Jack's Rake is "difficult and awkward", although there is "curiously little sense of exposure, for a comforting parapet of rock accompanies all the steeper parts of the ascent".The summit is a short walk from the top exit of the rake, which is also used as a descent route and by rockclimbers accessing the climbs on the cliff face. In separate incidents, two walkers fell to their deaths from Jack's Rake in June 2012. As with Lord's Rake on Scafell Crag, the word 'rake' refers to a path across major precipices, originally used by climbers for access to rock climbs, but which can also be used by walkers. Pavey Ark can also be ascended from Stickle Tarn via Easy Gully, North Rake or by the path to Harrison Stickle. Easy Gully is a steep walk on scree between the crags at the eastern end of the precipice, starting from the same place as Jack's Rake, and is blocked by large boulders near the top, where tough scrambling is required. North Rake (so named by Wainwright) starts from the path to High Raise at the very eastern end of the cliff and rises west over the top of the East Buttress. This is a much less exposed and strenuous walking route to the summit.

Rydal Mount is a house in the small village of Rydal, near Ambleside in the English Lake District. It is best known as the home of the poet William Wordsworth from 1813 to his death in 1850. It is currently operated as a writer's home museum. Wordsworth was born in Cockermouth in Cumberland in 1770, and knew the Lake District well from his childhood. He moved away to study at the University of Cambridge in 1787, and then travelled in Britain and Europe for 12 years. He spent over 8 years at Dove Cottage in nearby Grasmere from 1799 to 1808, but was forced to move to accommodate his growing family and many visitors. After a period in Allan Bank in Grasmere, the Wordsworths moved to Rydal Mount in 1813. Both Grasmere and Windermere lakes can be seen from the hillside grounds of Rydal Mount. William designed the layout of the gardens at Rydal, and he often said that those grounds were his office as opposed to the spacious office/writing room in his house. On the high side of the grounds, tucked away from the main house, but overlooking both the grounds and the two nearby lakes, he built the "Writing Hut" where he spent most of his writing time. This hut consisted merely of a bench with a small roof, but it provided shelter from the frequent rains and escape from the house. He lived the rest of his life there until his death at the age of 80, and he frequently was visited by Samuel Taylor Coleridge who would walk down from his home in Keswick. The Wordsworths continued to rent this property for 46 years, following William's death in 1850 to the death of his wife, Mary, in 1859. Rydal Mount was acquired in 1969 by Mary Henderson (née Wordsworth), William's great great granddaughter. It remains in the ownership of the Wordsworth family, and has been opened to the public since 1970.

Rydal Water