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cinders) from repeated Quaternary eruption of local cinder
cones in the Panamint valley, south-eastern California.
Photo: Ken Addison
footwalls of the Amargosa range (1,525-1,900 m OD), and
crossed by small fault scarps, on the south-eastern flank of
Death Valley, California.
Photo: Ken Addison
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eastern hanging wall of the Panamint range (2,700-3,500m
OD), on the west flank of Death Valley.
Photo: Ken Addison
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Figure 13.12
Block diagram to show the major sedimento-
logical environments associated with an active continental
Source: After Leeder and Gawthorpe (1987)
Basin ephemeral lake in Death Valley in the United States at
the lowest point of -86 m OD.
Photo: Ken Addison