From dissolved minerals to kettle limescale
Rainwater starts out soft, but as it percolates through limestone and chalk, it dissolves minerals that travel invisibly to your kitchen tap. That dissolved calcium and magnesium is what makes water 'hard', and when a kettle heats the water, the chemical balance shifts and leaves solid calcium carbonate behind as crusty limescale.
Questions you could explore
- How is a dissolved mineral different from a visible deposit?
- Why does hardness alone not establish drinking-water safety?
Start reading
- US Geological SurveyHardness of Water
The USGS explains water hardness and its relationship to deposits and soap behavior.
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