Figure txu-oclc-6445288-b-017-f-08
FIGURE 8.-Section across northeastern part of
Dagger Flat area, showing the four erosion surfaces typical
of the Marathon Basin. Surface a
is suggested only by the even summit levels of
the novaculite ridges. Surfaces b
and c are widely
developed rock plains. Surface d
is the present stream grade.from
Professional Paper 187
GEOLOGY OF THE MARATHON REGION, TEXAS
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