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The walls of the crater show good evidence for a fluctuating lava pond, which appears to have broken through and rafted away portions of the northeastern and southeastern crater walls. Backflow of the lava pond into the conduit is indicated by pahoehoe crust on the present crater floor.
The Jordan Craters lava flow field is mineralogically and chemically homogeneous, whereas proximal tephra and flow deposits exhibit significant chemical heterogeneity which correlates with the eruptive history. Also noteworthy are the many excellent examples of basalt flow and eruption features, including ropy and shelly pahoehoe surfaces, lava channels, lava blisters, pressure ridges and squeeze-ups, pit craters, lava-tube skylights, vertically striated internal crater walls, and re-fused cobbles of rhyolitic country rock...
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