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CONTENTS
Water is essential to life. We need safe and regular supplies
of fresh drinking water and we rely on water to grow crops
for food. Yet, less than 1% of all the water on earth is accessible
as fresh drinking water. In global terms, water is a precious
commodity.

For many, Cumbria is synonymous with water. Water and ice
have moulded the landscape creating its myriad lakes, rivers
and waterfalls, and prodigious amounts fall as precipitation
- to the dismay of many visitors!

Water has influenced Cumbria's agricultural and industrial
processes and even our leisure pursuits. Sheep are better
adapted to coping with waterlogged soils and frequent rainfall
and have become the mainstay of Cumbrian farming systems.
Mills once harnessed running water to provide power for machinery.
And tourism - one of the main income generators in Cumbria
- is heavily dependent on water: the numerous lakes, rivers
and waterfalls being a magnet for visitors every year.
THE WATER CYCLE
The combination of mountains
and lakes in Cumbria provides the ideal conditions for the
production and storage of large amounts of pure, soft water.
Westerly winds bringing in moisture-laden clouds from the
Atlantic are forced to rise over the mountains. This causes
them to cool, and the moisture condenses and falls as rain.
The rain collects in streams and rivers and is ultimately
disgorged into the lakes or the sea. Evaporation returns water
to the atmosphere, creating a continuous water cycle.

However, heavy rainfall and rapid run-off can quickly swell
rivers and lakes beyond their normal capacity resulting in
flooding that is often highly localised. In June 1686, torrential
flooding in Hawkshead caused flooding 'the like of it was
never seen in these parts by noe man liveinge, for it did
throwe downe some houses and mills and tooke away several
briggs
the water wash't upp great trees, stocks, and
greate stones a greate way off and lay'd them on men's ground.'
In August 1966, exceptionally heavy rainfall fell in upper
Borrowdale with devastating effects. Swollen streams brought
down huge boulders, damaging walls and bridges. The water
flooded homes in Seatoller, Seathwaite and Rosthwaite and
swept away cars. The clean-up had barely started when a second
deluge occurred three weeks later.
In 1968 the Eden washed away the sandstone bridge at Langwathby.
More recently, the floods of January 2005 wreaked havoc in
residential areas of Carlisle, Keswick and Cockermouth and
caused extensive flooding throughout Cumbria.

In contrast to heavy rainfall, periods of drought can reveal
areas that are usually submerged. During the drought years
of 1984 and 1996 the drowned village of Mardale emerged from
the shrinking waters of Haweswater reservoir.

WEATHER RECORDING

In 1844 John Miller of Whitehaven established a 'water station'
at Seathwaite to carry out regular readings of the rainfall.
He later set up other gauges further up the valley and one
near the summit of Scafell Pike. These showed that the amount
of rainfall increased with altitude.
The central fells have 225 'rain days' on average, totalling
around 2500 mm (100 inches) of rainfall per year. Away from
the central mountains, the rainfall drops off rapidly with
most of the coastal fringe having less than 1000 mm (40 inches)
per year. The Eden Valley, lying in the rain shadow, normally
receives about 890 mm (35 inches) per year.
There
are a number of weather stations throughout Cumbria that record
rainfall, temperature, wind speed and cloud cover on a daily
basis. Figures over the last 100 years point towards increasing
rainfall in Cumbria.
The small hamlet of Seathwaite in Borrowdale holds the distinction
of being the wettest inhabited place in England with a mean
annual rainfall of over 3 metres (120 inches)!
| Did you know
?
The heaviest annual rainfall ever recorded in the UK was
at Sprinkling Tarn in 1954 when over 6½ metres
of rain fell over the course of the year. |
Average rainfall totals in Seathwaite,
Keswick and Sellafield

WATER FOR EXPORT!
In the late 19th century, the need for clean water (for industry
and through improved standards of hygiene and sanitation)
created unprecedented demand from the industrial towns of
Lancashire. Manchester Corporation sought to solve the problem
by finding new sites for reservoirs outside the confines of
the city. Two valleys in the Lake District - Thirlmere and
Haweswater - were identified as suitable for reservoirs, having
solid bedrock onto which to build the dam and impervious rock
strata to hold the water.

In 1879 the Corporation received Royal Assent to build a
dam at Thirlmere. Work proceeded soon after with the building
of a masonry dam (the first in England) to create a reservoir
connected by a 96 mile (155 km) long aqueduct to Manchester.
The aqueduct was officially opened on 12 October 1894. The
following day a fountain in Albert Square (Manchester) gushed
Thirlmere water into the air to the delight of the crowds,
many of whom had brought cups to sample their first drink
of Lakeland water. To this day, the Thirlmere aqueduct delivers
around 50 million gallons of water a day to the city.
In 1919 the Corporation successfully applied for permission
to flood the Haweswater valley, including the small village
of Mardale. Over the next decade, surveys were undertaken,
and land and buildings compulsorily purchased. The workforce
was recruited from all over the north-west and to accommodate
them the Corporation built the model village of Burnbanks
near the site of the dam.

Work on the dam started in the 1930s and was completed in
1940. The dam is the highest in Britain at 30 metres (96 ft)
and is a rare example of a hollow buttress concrete dam. The
reservoir waters rose over the next two years, gradually submerging
the village of Mardale with its church and inn. The level
of the lake was raised by 30 metres and its capacity increased
to 85 million cubic metres or the equivalent of nearly 38,000
Olympic-sized swimming pools! Every day, around 300,000 cubic
metres (66,000,000 gallons) of water are discharged to Manchester
via an underground pipe. The water flows by gravity for nearly
100 miles, descending at a rate of 30 cm per km (7 inches
per mile) during its two-day journey.
Reservoir
levels are regulated by allowing water abstractions from other
lakes. Windermere and Ullswater support storage levels in
Thirlmere and Haweswater reservoirs during times of drought.
The capacity of Haweswater was enhanced by the completion
of a new reservoir at Wet Sleddale in 1967.
The urban and industrial areas surrounding the central Cumbrian
fells have also exploited the local water resources: Workington
takes its water from Crummock, Whitehaven from Ennerdale,
and water from Wastwater is used to cool the nuclear reactors
at Sellafield.
This network of reservoirs, pumping stations and underground
pipes are part of an integrated water management system to
ensure that adequate supplies of water are delivered to the
thirsty urban areas of Manchester, Cumbria and Lancashire.
United Utilities is now responsible for the collection, storage,
purification and supply of clean, safe drinking water throughout
the region. The company owns much water catchment land in
the Cumbria Fells and Dales, and works with various organisations
to improve public access and make environmental improvements.
They are also responsible for the treatment of waste water
and returning it to our rivers and the sea in a clean form.
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Reservoir Rambles
At Thirlmere and Haweswater
it is possible to walk around the reservoirs using local
footpaths primarily. At Thirlmere, information panels
provide details on access routes at different localities.
A leaflet on Thirlmere Reservoir is available from local
Tourist Information Centres or contact United Utilities
on 01768 772334.

Reproduced by permission
of United Utilities.
The 9km circuit takes around
5 hours.
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DOWN THE DRAIN!
Waste water is continually being flushed away through underground
sewer pipes. This waste has to be treated before it can be
returned to rivers or the sea in a clean form. The process
of cleaning up waste water goes through the following stages:
1. First, the effluent is screened to remove paper, leaves
and other large objects.
2. The water then passes into large sedimentation tanks where
solid particles and organic matter settle on the bottom, forming
sludge (after further treatment, the sludge can be used as
a fertiliser or fuel to generate electricity).
3. From the sedimentation tanks the water is passed through
filtration beds, where micro-organisms feed on the remaining
organic material converting it to carbon dioxide, water and
nitrogen compounds.
4. The cleaned water is then returned to a river or the sea.

Samples of water are analysed throughout the treatment to
ensure stringent safety standards are met. In the UK, around
83% of our water is treated, compared with only 51% in Europe
as a whole. Globally, around a third of the world's population
do not have access to even basic sewerage treatment, leaving
them vulnerable to water-borne diseases such as cholera and
dysentery.
WATER QUALITY
Streams, rivers and lakes gather pollution as run-off from
agricultural, domestic and industrial sources. Nitrates and
phosphates (from fertilisers and organic matter) cause enrichment
of inland waters leading to algal blooms and deoxygenation
of the water that can severely affect fish and invertebrate
life. Pesticides, particularly from sheep dip, are highly
toxic to aquatic life. Sediment deposition can quickly silt
up lakes and affect fish spawning grounds. Furthermore, the
plethora of hotels, guest houses and private dwellings along
lake shores collectively contribute to the levels of phosphates
(derived from sewage) finding their way into water courses.
Loweswater Project
Over recent years Loweswater has suffered from algal blooms
caused by modern farming and tourism practices. However, local
farmers and the wider community are collaboratively looking
at ways to reduce the amount of effluent being discharged
into the lake from septic tanks and agricultural run-off.
Their overall aim is to enhance the environment, improve the
lake's waters, restore healthier soils and encourage 'greener'
attitudes to land and tourism management. The lake will be
periodically sampled to evaluate the effects of these new
management techniques on water quality and fish stocks. For
more information on this scheme, contact Danny Leck on 01946
861465.
Bassenthwaite Lake Restoration Programme
Bassenthwaite Lake is a National Nature Reserve because of
its wildlife interest, but this diversity is being threatened
because of increasing levels of pollution (particularly from
phosphates) and sedimentation. The restoration programme is
a multi-agency approach that is targeting the whole of the
Bassenthwaite catchment area, and aims to mitigate the pollution
effects by reducing fertiliser run-off from the land, improving
septic tank discharges, reducing grazing pressure, planting
broadleaved trees and involving the whole community. For more
information on the scheme, contact John Pinder at the Environment
Agency on 01768 215731. The Lake District Tourism & Conservation
Partnership (tel: 015394 34630; www.lakespartnership.co.uk)
offers advice to tourism businesses on how to minimise the
risk of pollution getting into the lake.
Eden Rivers Trust
The Trust was set up in 1996 to conserve, protect and improve
the River Eden and its catchment. Surveys have been undertaken
and much work has gone into restoring riverine habitats, banksides
and adjacent wetlands and water meadows; protecting fish stocks;
reducing pollution; resisting water abstraction; working with
farmers to improve stock management; improving access points;
and raising local awareness of the importance of maintaining
the health of the river Eden and its tributaries.
For more information, contact the Eden Rivers Trust on 01768
353992
or www.edenriverstrust.org.uk.

CUMBRIAN FISH
Cumbria's lakes harbour many species of fish; some of which
are 'glacial relics' from the last Ice Age, including the
Arctic char, schelly and vendace. These species are currently
under threat because of higher water temperatures, decreasing
water quality, silting up of spawning grounds and competition
from other species.

The Arctic Char (Salvelinus alpinus) favours
the deeper lakes and is found in Wastwater, Coniston Water,
Ennerdale Water, Buttermere, Crummock Water, Thirlmere and
Haweswater.

Schelly (Coregonus lavaretus) were once commercially
fished from Ullswater and sold at Pooley Bridge fish market.
The fish is currently found in Ullswater, Brotherswater, Haweswater
and Red Tarn on Helvellyn.

The Vendace (Coregonus albula) is an endangered
species that is found only in Derwentwater and Bassenthwaite
Lake. The fish needs clean gravel to lay its eggs on, but
its traditional spawning grounds in Bassenthwaite Lake are
gradually silting up. Eggs from the vendace have recently
been taken to Sprinkling Tarn (Borrowdale) to create new populations.

Atlantic Salmon (Salmo salar) and Brown
Trout (Salmo trutta) are found in clean waters
with suitable spawning grounds throughout Cumbria. However,
there has been a decline in the numbers of salmon migrating
upstream. The Environment Agency, Eden Rivers Trust, United
Utilities and others have instigated schemes to help migrating
fish, such as the installation of 'ladders' (stepped pools)
to enable fish to bypass any obstacles and the insertion of
an 'acoustic barrier' at Heltondale Beck (near Penrith) to
warn fish away from the water abstraction point.
CUMBRIAN SPRING WATER
As
well as the quality water that emerges from our taps, Cumbria
has three water bottling companies that take their water from
underground sources.
Lakeland Spring Water is collected at Standing Stones,
high above Ennerdale Water and bottled at Hensingham, near
Whitehaven
(www.lakeland-spring.com).
Lakeland Willow Water contains traces of salicin,
a natural analgesic derived from white willow bark. The original
spring was known for its therapeutic powers and a holy well
was built on the site by the monks of Cartmel Priory. Today,
water from the same source is pumped from an underground aquifer
and bottled nearby. Tours of the bottling plant can be made
by arrangement.
Contact 015395 59452 or www.willowwater.com.
The Eden Valley Mineral Water Company takes around
250 million litres of spring water per year from 5 boreholes
near Armathwaite, for retail under the Aqua Pura brand. www.princes.co.uk/brands/aquapura
GETTING AROUND
For details on public transport, please contact Traveline
on 08700 608 2608.
Email: info@traveline-cumbria.co.uk.
Website: www.traveline.org.uk.
CREDITS
Produced by Anna Grayat Voluntary Action Cumbria for LEADER+
(Cumbria Fells & Dales)
Concept design: copyright Andrew Lathwell Design Ltd
Illustration by Juliet Whitworth
Printed by Reeds of Penrith, 2006.
Front cover photographs by Anna Gray and Val Corbett.
Other photographs supplied by Val Corbett, Richard Spiers,
Peter Pedley Postcards, LDNPA, Met Office, United Utilities,
Environment Agency, Kingfisher Publications, Honister Yew
Tree, Princes Soft Drinks and Anna Gray.
LEADER+ (Cumbria Fells & Dales)
The Old Stables,
Redhills,
Penrith,
Cumbria,
CA11 0DT
Tel: 01768 869533
Email: info@fellsanddales.org.uk
Website: www.fellsanddales.org.uk
Fells and Dales LEADER+ Programme is based at Voluntary Action
Cumbria, a company limited by guarantee, Charity No. 1080875,
Companyh No. 3957858.
This is one of a series of themed trails being produced
by LEADER+ (Cumbria Fells & Dales) to promote the area
and its local products.
Whilst every effort has been made to ensure that the content
of this trail is accurate and up to date at the time of writing,
no liability can be accepted for any errors, omissions or
misrepresentations of fact contained herein.
This project is being part financed by the European Agriculture
Guidance adn Guarantee Fund of the European Union and the
Department for Environment Food and Rural Affairs through
the Cumbria Fells and Dales LEADER+ Programme.
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