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The Sandstone Ridge Trust Ltd 
Company limited by guarantee Number 7673603 
Registered Charity Number 1144470
David Joyce
1 Water usage 
2 Types of water source and associated features 
3 Water characteristics and oddities 
4 Water tasting exercise 
5 Case studies 
6 What next?
Water consumption 
Modern Water usage 
45 – 100 m3/person/year 
Drinking Water 
2-3 litres/day 
Approx. 0.5 to 1 m3 /year 
Since 1900 water consumption in 
Europe has gone up 500 fold.
Water usage 1 m3 
= 1000 litres = 220 gallons 
25 metre pool; 1.5 metres 
deep; lane 1 metre wide 
= 37.5 m3/lane 
So 1 lane of the pool is 
enough drinking water for up 
to 75 people for a year. 
It takes about 1,000 litres of water to produce 1 litre of milk 
(includes irrigation, drinking, cleaning of cows and equipment, waste disposal etc.) 
It takes 5,000 - 20,000 litres of water to produce 1 kg of 
meat 
It takes 500 - 4000 litres of water to produce 1 kg of wheat
The water cycle
Rainfall 
Cheshire Lake District Essex 
790 mm/year 
31 inches/year 
1660 mm /year 
65 inches/year 
580 mm/year 
23 inches/year
Dew ponds
Dew ponds 
 A dew pond is an artificial pond usually sited 
on the top of a hill, intended for watering 
livestock. 
 Dew ponds are used in areas where a natural 
supply of surface water may not be readily 
available. 
 The name dew pond (sometimes cloud pond 
or mist pond) is first found in 1865. 
 Despite the name, their primary source of 
water is believed to be rainfall rather than 
dew or mist.
Marl pits
Marl 
Pits 
1953 
map
Major 
lakes, 
streams 
and 
brooks
Spring-fed lake: Harmer’s Lake, Helsby
River source
Sources of water
Wells
Spring source
Well or borehole
Typical 
borehole 
construction
Wells 
and 
springs 
1953 
map
Marl Pits Wells and springs
Named 
Wells 
Wanlow’s, 
Wandlow’s, 
Wanless Well? 
= green 
Lord’s well 
= red 
Swan’s well 
= purple 
1953 map
Water well in a perfect 
world
Water well in reality
Communal dipping well 
Woodhouses
Dropping stone well 
Bickerton hill
Beeston Castle Well
Brick and concrete reservoirs
Water towers 
Pale Heights 
Eddisbury Hill Farm
Harthill School Fountain, 1862
Characteristics of water 
The following is a list of indicators of water quality: 
 Alkalinity 
 Colour of water 
 pH 
 Taste and odour 
 Dissolved metals and salts (sodium, chloride, potassium, 
calcium, manganese, magnesium) 
 Heavy metals and metalloids (lead, mercury, arsenic, etc.) 
 Dissolved organics 
 Radon 
 Pharmaceuticals 
 Hormone analogues 
 Microorganisms
Variation in water composition 
Mouldsworth 
Water bearing 
stratum at 250 ft 
Mouldsworth 
Water bearing 
stratum at 800 ft 
Calcium carbonate 170 170 
Magnesium sulphate 6 60 
Magnesium 
chloride 
155 22 
Sodium chloride 780 300 
Total hardness 440 260 
Water analysis in parts per million 
Thresh, Beale and Suckling (1949)
Water hardness (mg/l CaCO3) 
soft up to 50 
moderately soft 50 – 100 
slightly hard 100 – 150 
moderately hard 150 – 200 
hard 200 – 300 
very hard over 300
Water quality
Water-borne diseases 
Bacteria Protozoa Viruses Parasites 
Salmonella typhi 
Vibrio cholerae 
Campylobacter 
Leptospira 
Salmonella 
E coli 
Shigella 
Legionella 
pneumophilia 
Giardia 
Entamoeba 
Cryptosporidium 
Several groups 
cause diarrhoea 
Hepatitis 
Several
Sources of contamination
Cholera in Soho 
In August 1854, a major 
outbreak of cholera struck 
Soho. By 10 September, 
500 people had died. 
John Snow eventually 
linked the outbreak to 
contaminated water. The 
local council disabled the 
well and the outbreak 
declined.
Perrier Water - 1 
Rainfall 
LIMESTONE 
Water plus Carbon dioxide plus impurities 
‘Boiling 
pool’ 
Clean carbon 
dioxide 
FAULT 
IMPERMEABLE MARL 
CAP ROCK 
Perrier 
water 
LIMESTONE 
CLAY CAP 
SAND
Perrier 
water 
Perrier Water - 2 
CLAY CAP 
Rainfall 
LIMESTONE 
Water plus Carbon dioxide plus impurities 
‘Boiling 
pool’ 
Clean carbon 
dioxide 
FAULT 
IMPERMEABLE MARL 
CAP ROCK 
LIMESTONE 
Filter 
Discard water 
SAND
Buxton water – 5000 years 
old
Buxton water – 5000 years 
old
Sulphur well at Bolton 
Abbey, Yorkshire
Water from the Republic of Georgia 
 “Borjomi spring water is beneficial 
in the treatment of diseases due to 
its mineral properties.” 
 “Borjomi mineral water has been 
used for centuries to treat chronic 
gastritis, gastric and duodenal 
ulcers, chronic diseases of the liver 
and bile ducts, gallstones, kidney 
stones, urinary tract infections and 
respiratory diseases.”
Chemical composition 
Borjormi (mg/l) Peckforton (mg/l) 
Calcium 100 90 
Bicarbonate 3500-5000 
Sodium and 
Potassium 
1200-2000 36 
Chloride 250-500 11 
Sulphate Less than 10 28 
Total solids 5500 - 7500
Water from the Lake District 
• The Willow aquifer is the source of the legendary Holy Well of 
Cartmel dating as far back as the 12th Century. 
• Filtered through what was once a white willow forest, and 
limestone, willow water has a unique mineral composition 
including Calcium and Salicin.
Whistlebitch well
Whistlebitch well today
Horsley bath
Helsby Water Tower 
Cheshire Observer 11 April 1896
Manley water supply 
Location of storage tank 
Location of feeder reservoir 
Location of water ram
Manley water supply
Water ram 
Basic components of a hydraulic ram: 
1. Inlet — drive pipe 
2. Free flow at waste valve 
3. Outlet — delivery pipe 
4. Waste valve 
5. Delivery check valve 
6. Pressure vessel 
Hydraulic Water Ram systems need no external source of power -- 
the force of moving water gives them the power they need. 
They are extremely simple, with just two moving parts
Bulkeley Hill 
Staffordshire Potteries Water Board 
Hauled tramway for the construction of the reservoir 
(c1953) and water storage tanks
‘ The Spring... 
Mineral Composition Mg Per Litre 
Calcium 90 
Magnesium 21 
Potassium 3.9 
Chloride 11.4 
Sulphate 27.9 
Sodium 32 
The village of Tattenhall, 
beneath Cheshire's beautiful 
Peckforton Hills, is home to the 
spring which has provided this 
pure, clear and refreshing water 
for over 70 years. 
The original borehole for the 
water was sunk in 1938, and 
over the years provided millions 
of litres of fresh water. A new 
borehole was created in 1993 to 
meet the highest modern 
standards of production.
Frodsham Mineral Water Co 
1900 to 1913 
Two cousins by the name of Ellison 
and Corker founded a mineral water 
company in 1888. It was behind 
Millbank Cottages, off Main Street. 
It was renamed Frodsham Mineral 
Water Co. in 1912 and many of their 
old bottles with 'glass alleys' in the 
neck still remain. The man holding 
the horse is Joe Ellison, a son of the 
founder, and the boy on the cart , 
Billy Booth
General Discussion

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The Evolution of Water Usage

  • 1. The Sandstone Ridge Trust Ltd Company limited by guarantee Number 7673603 Registered Charity Number 1144470
  • 3. 1 Water usage 2 Types of water source and associated features 3 Water characteristics and oddities 4 Water tasting exercise 5 Case studies 6 What next?
  • 4. Water consumption Modern Water usage 45 – 100 m3/person/year Drinking Water 2-3 litres/day Approx. 0.5 to 1 m3 /year Since 1900 water consumption in Europe has gone up 500 fold.
  • 5. Water usage 1 m3 = 1000 litres = 220 gallons 25 metre pool; 1.5 metres deep; lane 1 metre wide = 37.5 m3/lane So 1 lane of the pool is enough drinking water for up to 75 people for a year. It takes about 1,000 litres of water to produce 1 litre of milk (includes irrigation, drinking, cleaning of cows and equipment, waste disposal etc.) It takes 5,000 - 20,000 litres of water to produce 1 kg of meat It takes 500 - 4000 litres of water to produce 1 kg of wheat
  • 7. Rainfall Cheshire Lake District Essex 790 mm/year 31 inches/year 1660 mm /year 65 inches/year 580 mm/year 23 inches/year
  • 8.
  • 10. Dew ponds  A dew pond is an artificial pond usually sited on the top of a hill, intended for watering livestock.  Dew ponds are used in areas where a natural supply of surface water may not be readily available.  The name dew pond (sometimes cloud pond or mist pond) is first found in 1865.  Despite the name, their primary source of water is believed to be rainfall rather than dew or mist.
  • 13. Major lakes, streams and brooks
  • 17. Wells
  • 21. Wells and springs 1953 map
  • 22. Marl Pits Wells and springs
  • 23. Named Wells Wanlow’s, Wandlow’s, Wanless Well? = green Lord’s well = red Swan’s well = purple 1953 map
  • 24. Water well in a perfect world
  • 25. Water well in reality
  • 26. Communal dipping well Woodhouses
  • 27. Dropping stone well Bickerton hill
  • 29. Brick and concrete reservoirs
  • 30. Water towers Pale Heights Eddisbury Hill Farm
  • 32.
  • 33. Characteristics of water The following is a list of indicators of water quality:  Alkalinity  Colour of water  pH  Taste and odour  Dissolved metals and salts (sodium, chloride, potassium, calcium, manganese, magnesium)  Heavy metals and metalloids (lead, mercury, arsenic, etc.)  Dissolved organics  Radon  Pharmaceuticals  Hormone analogues  Microorganisms
  • 34. Variation in water composition Mouldsworth Water bearing stratum at 250 ft Mouldsworth Water bearing stratum at 800 ft Calcium carbonate 170 170 Magnesium sulphate 6 60 Magnesium chloride 155 22 Sodium chloride 780 300 Total hardness 440 260 Water analysis in parts per million Thresh, Beale and Suckling (1949)
  • 35. Water hardness (mg/l CaCO3) soft up to 50 moderately soft 50 – 100 slightly hard 100 – 150 moderately hard 150 – 200 hard 200 – 300 very hard over 300
  • 37. Water-borne diseases Bacteria Protozoa Viruses Parasites Salmonella typhi Vibrio cholerae Campylobacter Leptospira Salmonella E coli Shigella Legionella pneumophilia Giardia Entamoeba Cryptosporidium Several groups cause diarrhoea Hepatitis Several
  • 39. Cholera in Soho In August 1854, a major outbreak of cholera struck Soho. By 10 September, 500 people had died. John Snow eventually linked the outbreak to contaminated water. The local council disabled the well and the outbreak declined.
  • 40.
  • 41. Perrier Water - 1 Rainfall LIMESTONE Water plus Carbon dioxide plus impurities ‘Boiling pool’ Clean carbon dioxide FAULT IMPERMEABLE MARL CAP ROCK Perrier water LIMESTONE CLAY CAP SAND
  • 42. Perrier water Perrier Water - 2 CLAY CAP Rainfall LIMESTONE Water plus Carbon dioxide plus impurities ‘Boiling pool’ Clean carbon dioxide FAULT IMPERMEABLE MARL CAP ROCK LIMESTONE Filter Discard water SAND
  • 43. Buxton water – 5000 years old
  • 44. Buxton water – 5000 years old
  • 45. Sulphur well at Bolton Abbey, Yorkshire
  • 46. Water from the Republic of Georgia  “Borjomi spring water is beneficial in the treatment of diseases due to its mineral properties.”  “Borjomi mineral water has been used for centuries to treat chronic gastritis, gastric and duodenal ulcers, chronic diseases of the liver and bile ducts, gallstones, kidney stones, urinary tract infections and respiratory diseases.”
  • 47. Chemical composition Borjormi (mg/l) Peckforton (mg/l) Calcium 100 90 Bicarbonate 3500-5000 Sodium and Potassium 1200-2000 36 Chloride 250-500 11 Sulphate Less than 10 28 Total solids 5500 - 7500
  • 48. Water from the Lake District • The Willow aquifer is the source of the legendary Holy Well of Cartmel dating as far back as the 12th Century. • Filtered through what was once a white willow forest, and limestone, willow water has a unique mineral composition including Calcium and Salicin.
  • 52. Helsby Water Tower Cheshire Observer 11 April 1896
  • 53. Manley water supply Location of storage tank Location of feeder reservoir Location of water ram
  • 55. Water ram Basic components of a hydraulic ram: 1. Inlet — drive pipe 2. Free flow at waste valve 3. Outlet — delivery pipe 4. Waste valve 5. Delivery check valve 6. Pressure vessel Hydraulic Water Ram systems need no external source of power -- the force of moving water gives them the power they need. They are extremely simple, with just two moving parts
  • 56. Bulkeley Hill Staffordshire Potteries Water Board Hauled tramway for the construction of the reservoir (c1953) and water storage tanks
  • 57. ‘ The Spring... Mineral Composition Mg Per Litre Calcium 90 Magnesium 21 Potassium 3.9 Chloride 11.4 Sulphate 27.9 Sodium 32 The village of Tattenhall, beneath Cheshire's beautiful Peckforton Hills, is home to the spring which has provided this pure, clear and refreshing water for over 70 years. The original borehole for the water was sunk in 1938, and over the years provided millions of litres of fresh water. A new borehole was created in 1993 to meet the highest modern standards of production.
  • 58. Frodsham Mineral Water Co 1900 to 1913 Two cousins by the name of Ellison and Corker founded a mineral water company in 1888. It was behind Millbank Cottages, off Main Street. It was renamed Frodsham Mineral Water Co. in 1912 and many of their old bottles with 'glass alleys' in the neck still remain. The man holding the horse is Joe Ellison, a son of the founder, and the boy on the cart , Billy Booth