Dirt: The Erosion of Civilizations - Kootenay Local Agricultural Society
Dirt: The Erosion of Civilizations - Kootenay Local Agricultural Society
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