Clearwater Spring (Yellowstone)
Yellowstone National Park, Wyoming, United States
Other media
- Type
- Other medium
Hydrothermal system of the Yellowstone caldera. Palmer and Sturchio (1990): waters from -9.3 to +4.4 ‰; Norris and Upper Geyser basins, Calcite Springs and Clearwater stay close to fresh rhyolite (-5.2 ‰), Mammoth, Sheepeater and Rainbow near -8 ‰, like altered rhyolite (-9.7 ‰) or sediments outside the caldera.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −6 ‰ | 1 | thermal water Single analysis (Y88-2 Clearwater). Y88-2 Clearwater: 93 °C, pH (7.1), B 0.71 mmol/kg, Cl 12.2 mmol/kg (pH in brackets measured in the laboratory). | Palmer & Sturchio (1990), The boron isotope systematics of the Yellowstone National Park … |
Deposits of the same type
Cite this page
IsoFind Atlas (2026). Clearwater Spring (Yellowstone), isotope signatures. https://www.isofind.tech/isotopes/en/sites/source-clearwater-yellowstone/ (accessed 2026-10-20).
@misc{isofind2026clearwaterspringyellowstoneis,
title = {Clearwater Spring (Yellowstone), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/source-clearwater-yellowstone/},
note = {Accessed 2026-10-20}
}Updated : 2026-10-20