📘 How a hot spring stays hot
Follow groundwater through deep rock, geothermal heat, faults, mixing, and mineral-rich discharge.
What you’ll learn
- Rainfall recharge
- Geothermal gradient
- Convection loop
- Fault pathway
- Mixing
- Mineral load
- Steady discharge
- Chemistry and life
- Human withdrawals
- A moving heat budget
Questions this course answers
What is the geothermal gradient?
The crust generally becomes warmer downward.
Why can warm water rise in a convection loop?
Density differences drive circulation through connected pathways.
What role can a fault play?
A permeable fault can connect the heated reservoir to an outlet.
Why do mineral terraces form?
Changing temperature and chemistry at the outlet promotes precipitation.
How can pumping affect a hot spring?
A spring is part of a connected groundwater system.
Grounded in trusted sources
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