By Mark Monmonier

Within the subsequent century, sea degrees are estimated to upward push at unheard of premiums, inflicting flooding around the globe, from the islands of Malaysia and the canals of Venice to the coasts of Florida and California. those emerging water degrees pose severe demanding situations to all facets of coastal existence—chiefly financial, residential, and environmental—as good as to the cartographic definition and mapping of coasts. it's this part of coastal existence that Mark Monmonier tackles in Coast strains. atmosphere sail on a trip throughout moving landscapes, cartographic know-how, and weather swap, Monmonier finds that coastlines are as a lot a suite of principles, assumptions, and societal ideals as they're reliable black traces on maps.Whether for crusing charts or estate maps, Monmonier indicates, coastlines problem mapmakers to seize on paper a hugely abnormal land-water boundary perturbed by way of tides and storms and complex by means of rocks, wrecks, and shoals. Coast traces is peppered with pleasing anecdotes concerning the complex attempt to expunge fictitious islands from nautical charts, the tough dimension of a coastline’s size, and the contentious notions of beachfront estate and public access.Combing maritime historical past and the background of expertise, Coast traces charts the old development from offshore sketches to satellite tv for pc pictures and explores the societal impression of coastal cartography on every thing from worldwide warming to native land safety. Returning to the shape of his celebrated Air obvious, Monmonier ably renders the subject of coastal cartography obtainable to either basic readers and historians of technological know-how, know-how, and maritime stories. within the post-Katrina period, while the map of whole areas should be redrawn by way of a unmarried traditional occasion, the problems he increases are extra very important than ever.

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Extra info for Coast Lines: How Mapmakers Frame the World and Chart Environmental Change

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3 The “bulge” is apparent in the range between high tide and low tides, which increased as March 10 approached and declined thereafter. High tides occur twice a day at Springmaid Pier, once when the moon is near its highest point above the horizon and again a halfday later, when the moon is on the opposite side of the rotating earth. This second tidal rise reflects the centrifugal force caused by our planet and its satellite spinning about a common center of mass. Centrifugal force is the outward pull one feels near the edge of a spinning carousel.

4. Coast Survey crew measuring a base line in Epping Plains, Maine, 1857.

2 Both bodies pulling in the same direction produce a spring tide, characterized by lower lows and higher highs. 3 The “bulge” is apparent in the range between high tide and low tides, which increased as March 10 approached and declined thereafter. High tides occur twice a day at Springmaid Pier, once when the moon is near its highest point above the horizon and again a halfday later, when the moon is on the opposite side of the rotating earth. This second tidal rise reflects the centrifugal force caused by our planet and its satellite spinning about a common center of mass.

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