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Karen Luttrell, David Mencin, Olivier Francis and Shaul Hurwitz Constraints on the upper crustal magma reservoir beneath Yellowstone Caldera inferred from lake-seiche induced strain observations Geophysical Research Letters 40

Version of Record online: 13 FEB 2013 | DOI: 10.1002/grl.50155

Key Points

  • Strain induced by seiche waves in Yellowstone Lake is observed 30 km away
  • Observed strainfield requires some support from an upper crustal magma reservoir
  • Top of shallowest upper crustal partial melt is at 3 - 6 km depth

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