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CPT Q. 009: Why are there so many volcanic seamounts on the interior of the Pacific Plate?
CPT Q. 010: Why do trenches not display mass excesses, if deeply subducted slabs lie beneath them?
CPT Q. 011: Why do earthquakes sometimes occur across zones broader than the width of a plate?
CPT Q. 012: Has seismic tomography demonstrated the reality of subducted plates in the mantle?
CPT Q. 013: Why are some Benioff zones nearly horizontal?
CPT Q. 014: Why would thick, buoyant continents not entirely prevent subduction?
CPT Q. 015: Is it true that the total length of trenches does not closely match the total length of ridges?
CPT Q. 016: How can a trench possibly intersect a ridge?
CPT Q. 017: Is it true that ancient trenches have never been found?
CPT Q. 018: How do the distinctive features of the mid-ocean ridge system form?
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