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How steady are steady-state mountain belts? A reexamination of the Olympic Mountains (Washington state, USA)

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Figure

Figure 1. (a) Overview map of the Cascadia Subduction Zone showing the extent of the accretionary wedge
Figure 2. Map of new and previously published thermochronometric ages within the Olympic Mountains forBrandon, 2004) are indicated by circles with a black dot
Table 1. Data for the ocean drill cores shown in Fig. 3.
Figure 3. Map of the Cascadia Subduction Zone showing the age of the oceanic crust (Wilson, 1993) and sediment thickness, estimatedfrom the sediment cores of ocean drilling programs (holes ODP 888, OPD 1027, and DSDP 174) and seismic studies (Adam et al.,
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