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In hot water pools and springs most
of the colours are due to bacteria, algae, minerals and the natural
blue of water. Pools that are too hot to allow the growth of algae
and bacteria are normally blue because the water, unaffected by
alien growth, transmits only the blue of daylight reflecting from
the pools’ geyserite sides and bottom. A example of this blue
water can be found in the centre of Crested Glory Pool in Upper
Geyser Basin.
In cooler pools where algae and bacteria
can live the colour depends on the temperature and acidity of the
water. In water of low, or no acidity, yellow algae indicate that
the water is as hot as the algae can withstand. The yellow algae
combine with the blue of the water to form green, as in Emerald
Pool in Black Sands Basin. When temperatures drop in non-acidic
water, orange and brown algae appear. In acidic waters, the algae
that flourishes in high temperatures is bright green, such as Emerald
Spring in Norris Geyser Basin. In cooler acidic waters, a purplish
algae appears, then orange brown.
In running water such as Mammoth Hot
Springs, temperatures lower rapidly as the water moves further from
the source. Colours change rapidly. This is also true of run off
waters from hot pools and geysers.
The cones edges and walls of hot springs
and mud pots are coloured by minerals. Yellows are mostly sulphur.
Oranges, reds, browns and blacks are from various forms of iron
oxides and iron sulphides. Paint pots keep these minerals in suspension
and frequently have a combination of minerals, resulting in their
many varied colours.
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Prismatic Spring
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