Bottled Water of the World

SOH2O - Blue Spring

Print E-mail
Written by m2   
Monday, 29 November 1999 18:00
Last Updated ( Thursday, 03 September 2009 10:13 )

Spring Water - Still/Sparkling

SOH2O - Blue Spring Bottled Water

SOH2O - Blue Spring Description:


Balance Still Still
Light Light
Virginality Virginality
Minerality Low
Orientation Neutral
Hardness Soft
Carbonation A
Vintage 100

 

SOH2O - Blue Spring Analysis:


Temp. at source: 51.8°F (11.0°C)
129 TDS
6.8 ph factor
12.43 Hardness
2.62 Calcium
5.7 Chloride
1.47 Magnesium
0.54 Nitrate
3.86 Potassium
77.8 Silica
8.52 Sodium
milligrams per liter (mg/l)

For more details see: Minerals and Mineral Water & Sparkling Water

Country of Origin:  New Zealand
Region:  North Island
Place Name:  Mamaku Plateau
Established: 
Company:  Aquasplash Limited
Web Site:  www.soh2o.co.nz
phone:  +64 (0)7 883 3985
fax:  +64 (0)7 883 3984
email:  ed@aquasplash.co.nz
 
SOH2O - Blue Spring

The water for Blue Spring comes from an aquifer that penetrates deep under the bush clad Mamaku Plateau where rain that fell over 100 years ago has made its way through numerous aquifers between granite rock formations. 

The water that flows from the Blue Spring just to the east of the township of Putaruru in the North Island of New Zealand, predates European settlement.  Water gushes out of the spring into the Waihou river at a rate of 42 cubic metres per minute (9,240 gallons per minute) and is a constant 11 degrees Celsius all year round emerging from a depth of 250 meters (820 ft).

Because of its contact with geological formations, unique mineral composition is imparted into the Blue Spring water and many of these compositions are reputed to have health giving properties.



Add this page to your favorite Social Bookmarking websites
Digg! Reddit! Del.icio.us! JoomlaVote! Google! Live! Facebook! StumbleUpon! Yahoo! Free social bookmarking plugins and extensions for Joomla! websites!

View Michael Mascha's profile on LinkedIn


Mamaku Ranges

The Mamaku Ranges are a range of rugged hills in the North Island, New Zealand.  Located to the west of Lake Rotorua and north of Lake Taupo, they lie to the immediate south of the Kaimai Ranges , Coromandel Peninsula. The hills terminate in the south with the valley of the Waikato River. Extending from Karangahake Gorge near Paeroa, southward to the Mamaku Plateau, the Kaimai-Mamaku Forest Park gives protection to the rugged bush covered ranges for soil, water, ecological, scenic and recreational values. The range is extensively forested, with the Kaimai-Mamaku State Forest and Kinleith Forest both covering a considerable part of them. The forest includes Kauri trees growing at the far southern limit of their natural range.

Human activity throughout the ranges from early Maori to the present has left a vast historical legacy including old Maori trails and sites, early coach routes, gold mining relics and logging remains, amongst others.  

From the eruptions that created Lake Rotorua, they provide layered aquifers within fractured rock and volcanic sand aquifers.

Rainfall recharge moves rapidly through the surface sandy soils, and into the aquifers that discharges as springs to rivers at the edges of the plateau, such as the famous Blue Spring SOME 80 - 100 years later.

Waihou River

Te Waihou "The New Water" - The history of the Waihou River, as a multi purpose focus for the people of the region, dates back to the time of the first human visitors.  The river comes from as far up as the Ngatira Marae, which significantly marks the Eastern boundary of "Raukawa Ki Te Kaokaoroa o Patetere" and therefore the Northern boundary of the Ngati Raukawa.

It was a journeying place of King Te Wherowhero Tawhiao, the second Maori King of New Zealand, as it provided him with his main travelling route.  The river gave him food and the flax was used for many purposes. Also, Kahupeka, a Tainui tupuna, set off with her son shortly after her husband's death to wander around the Central North Island.  On her travels, the Upper Waihou River was one of the main rivers that her and her son crossed while travelling from Pirongia to Te Aroha, and again from Te Aroha to Whakamaru. The river was an important thoroughfare and provided food and flax for local people and visitors alike. The upper Waihou River was one of the main rivers crossed during her travels through the Waikato.

In 1938 the Edmeades family settled and farmed the land alongside the Upper Waihou.  They cleared much of the fern and manuka that previously clothed the riverbanks.

During WWII trenches were dug along the upper river due to fears of foreign invasion.  They were never used and eventually were filled.

The Waihou Stream is totally spring fed.  Water from the Mamaku Plateau takes anywhere between 50-100 years to reach the Blue Spring Water flows from the Blue Spring at a rate of 42 cubic metres per minute (9240 gallons per minute).  The water temperature of the Blue Spring is a constant 11 degrees celsius, come winter or summer. 

The reason for the blue colour (and high visual clarity) of the Waihou River and its spring source is the high optical purity of the water. Pure water is intrinsically blue in hue because it absorbs red light leaving only blue and (some) green light to be transmitted to the observer's eye. Pure natural waters are blue to blue-green in colour because they lack light absorbing constituents. They also tend to be very clear because they lack light absorbing particles. Both particles and light-absorbing matter are efficiently removed during the long residence time of spring water while in aquifers.

Featured Waters

Banner

Bottled Water Ads

Water Events

Joomla Templates by JoomlaShack