. Shore processes and shoreline development . ends to obliterate the larger irregularities of acoast and not to make them, one still finds the tidal and waveorigin of such drowned valleys as those of the Maine coastmaintained in recent editions of a standard textbook on geology^^. (6) Fjord Shorelines. — Perhaps no type of shoreline has givenrise to so much discussion as has the fjord shoreline. We maynote in the first place that geologists and geographers may bedivided into two main groups whose ideas regarding the originof fjords are mutually opposed. The first group may be desig-nated as th
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