A new conceptual model of the magma system below Mono Lake and Mono Craters in eastern California gives scientists a more detailed understanding of volcanic processes at depth, and a better model for forecasting volcanic unrest.
The 3D resistivity images show at least two vertical magma columns 10 km (6 miles) deep. One column underneath Panum Crater, resembling the shape of a giraffe’s neck, veers off horizontally, suggesting the presence of hydrothermal fluids near the surface. The other column, below South Coulee, gives no indication of recent near-surface activity. An older body of granitic rock, a pluton, was also discernable amid the columns of younger magma in the 3D imaging.