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Dirt: The Erosion of Civilizations - Kootenay Local Agricultural Society

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When asked how the great stone statues had been transported, the few<br />

remaining islanders did not know how their ancestors had done it. <strong>The</strong>y<br />

simply replied that the statues walked across the island. For centuries the<br />

bare landscape fueled the mystery <strong>of</strong> the heads. No one, including the<br />

sculptors’ descendants, imagined that the great stone statues were rolled on<br />

logs—it seemed just as likely that they had walked across the island on<br />

their own.<br />

Many <strong>of</strong> the statues were left either unfinished or abandoned near their<br />

quarry, implying that their sculptors ignored the impending timber shortage<br />

until the very end. As timber became scarce, competition for status and<br />

prestige continued to motivate the drive to erect statues. Even though the<br />

Easter Islanders knew they were isolated on a world they could walk<br />

around in a day or two, cultural imperatives apparently overcame any concern<br />

about running out <strong>of</strong> trees.<br />

European contact finished <strong>of</strong>f what was left <strong>of</strong> the native culture. In the<br />

1850s most <strong>of</strong> the island’s remaining able-bodied men, including the king<br />

and his son, were enslaved and shipped <strong>of</strong>f to Peruvian guano mines. Years<br />

later, the fifteen surviving abductees repatriated to their island introduced<br />

smallpox to a population with no immunity. Soon thereafter the island’s<br />

population dropped to just one hundred and eleven, unraveling any remaining<br />

cultural continuity.<br />

<strong>The</strong> story <strong>of</strong> how Easter Islanders committed ecological suicide is preserved<br />

in the island’s soil. Derived from weathered volcanic bedrock, thin<br />

poorly developed soil, in places only a few inches thick, blankets most <strong>of</strong><br />

the island. Just as in other subtropical regions, the thin topsoil held most<br />

<strong>of</strong> the available nutrients. Soil fertility declined rapidly once vegetation<br />

clearing allowed run<strong>of</strong>f to carry away the topsoil. After that only a small<br />

part <strong>of</strong> the island remained cultivatable.<br />

Distinctively abbreviated subsoil exposed at the ground surface testifies<br />

to erosion <strong>of</strong> the island’s most productive soil. Exposures at the foot <strong>of</strong> hillslopes<br />

reveal that a layer <strong>of</strong> material brought down from higher on the<br />

slopes covers the eroded remnants <strong>of</strong> the older original soil. <strong>The</strong>se truncated<br />

soil pr<strong>of</strong>iles are studded with telltale casts <strong>of</strong> the roots <strong>of</strong> the now<br />

extinct Easter Island palm.<br />

<strong>The</strong> relationship <strong>of</strong> soil horizons to archaeological sites reveals that most<br />

<strong>of</strong> the soil erosion occurred after construction <strong>of</strong> stone dwellings (ahus)<br />

associated with the rise <strong>of</strong> agriculture on the island. <strong>The</strong>se dwellings were<br />

built directly on top <strong>of</strong> the native soil, and younger deposits <strong>of</strong> material<br />

islands in time 219

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