|Professional Paper 1643: FIGURE 36|
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Faults (A, B)exposed in a vegetated roadcut 900 m southeast of the fault exposed at Utsalady Point (s in figure 27), cutting inferred Vashon glaciofluvial advance deposits. The faults, which juxtapose well-stratified sand and massive gravel, are 15 m apart and occur within the Utsalady Point fault zone.
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