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Deerbone Spring (Yellowstone)

Lower Geyser Basin, Wyoming, United States

Other media

Type
Other medium

Yellowstone National Park. Water with 200 ppm SiO2, pH from 8.4 (pool, 76 °C) to 10.1 (6.5 m downflow, 34 °C), undersaturated in amorphous silica; H3SiO4- dominates downflow.

δ30Si in ‰ (per mil) Values of the same system

Standard : NBS 28

ValueRangenMineral or matrixSource
−0.24 ± 0.06 ‰−0.32 / −0.17 ‰5thermal water (dissolved silicon)
Mean and standard deviation recalculated from 5 samples. DB1 to DB5, lighter than at Cistern.
Chen et al. (2020), Silicon isotope variations in hydrothermal systems at Yellowstone Nat…
−0.51 ± 0.27 ‰−0.81 / −0.11 ‰5siliceous sinter (opal-A)
Mean and standard deviation recalculated from 5 samples. DB1 to DB5: pool-edge sinter (DB1) heavier than the water (Δ +0.21 ‰, near equilibrium), the others lighter (Δ -0.21 to -0.64 ‰).
Chen et al. (2020), Silicon isotope variations in hydrothermal systems at Yellowstone Nat…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Deerbone Spring (Yellowstone), isotope signatures. https://www.isofind.tech/isotopes/en/sites/source-deerbone-yellowstone/ (accessed 2026-10-13).

@misc{isofind2026deerbonespringyellowstoneisot,
  title = {Deerbone Spring (Yellowstone), isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/sites/source-deerbone-yellowstone/},
  note = {Accessed 2026-10-13}
}

Updated : 2026-10-13