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📘 How a hot spring stays hot

Follow groundwater through deep rock, geothermal heat, faults, mixing, and mineral-rich discharge.

10
lessons
~10 min
to learn
🔬 Science
subject
Adults
level
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What you’ll learn

  1. Rainfall recharge
  2. Geothermal gradient
  3. Convection loop
  4. Fault pathway
  5. Mixing
  6. Mineral load
  7. Steady discharge
  8. Chemistry and life
  9. Human withdrawals
  10. 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.

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