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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land and birch forest. Following the arrival <strong>of</strong> agriculture, pollen from<br />
crops and weeds coincide with a threefold increase in the sediment deposition<br />
rate. After the Bronze and Iron Ages, erosion decreased dramatically<br />
for almost two thousand years as native plants regenerated across a largely<br />
abandoned landscape—until erosion accelerated again in the modern era.<br />
Similar cores taken from small lakes in southern Sweden also record the<br />
transition from little preagricultural erosion to much higher rates after<br />
arrival <strong>of</strong> the plow. One from Lake Bussjösjö shows that forest stabilized<br />
the landscape from 7250 to 750 bc until erosion accelerated following forest<br />
clearing. <strong>Erosion</strong> increased further under intensified agriculture in the<br />
sixteenth and seventeenth centuries. A core pulled from Havgårdssjön provides<br />
a 5,000-year record <strong>of</strong> vegetation and erosion. <strong>The</strong> archaeological<br />
record around the lake has no Bronze or Iron Age artifacts. Lakebed sediments<br />
piled up four to ten times faster after agricultural settlement began<br />
around ad 1100. All across the glaciated terrain <strong>of</strong> Scandinavia, Scotland,<br />
and Ireland, farmers could not make a living until enough ice-free time<br />
passed to build soil capable <strong>of</strong> sustaining cultivation.<br />
Put simply, European prehistory involved the gradual migration <strong>of</strong> agricultural<br />
peoples, followed by accelerated soil erosion, and a subsequent<br />
period <strong>of</strong> low population density before either Roman or modern times.<br />
Just as in Greece and Rome, the story <strong>of</strong> central and western Europe is one<br />
<strong>of</strong> early clearing and farming that caused major erosion before the population<br />
declined, and eventually rebounded.<br />
As the Roman Empire crumbled, the center <strong>of</strong> its civilization shifted<br />
north. Abandoning Rome as the capital, Diocletian moved his government<br />
to Milan in ad 300. When <strong>The</strong>odoric established the Gothic kingdom <strong>of</strong><br />
Italy on the ruins <strong>of</strong> the Roman Empire, he chose Verona as his new capital<br />
in the north. Even so, many <strong>of</strong> northern Italy’s fields lay fallow for centuries<br />
until an eleventh-century program <strong>of</strong> land reclamation began<br />
returning them to cultivation. After several centuries <strong>of</strong> sustained effort,<br />
most <strong>of</strong> northern Italy’s arable land was again under cultivation, supporting<br />
prosperous medieval cities that nurtured a renaissance <strong>of</strong> literature and<br />
art.<br />
As northern Italy’s population rebounded, intensive land use increased<br />
silt loads in the region’s rivers enough to attract the attention <strong>of</strong> Leonardo<br />
da Vinci and revive the Roman art <strong>of</strong> river engineering and flood control.<br />
Intensive cultivation on hillside farms spread into the Alps, producing similar<br />
results on the Po River as Roman land use had on the Tiber River.<br />
Eventually, after eight centuries <strong>of</strong> renewed cultivation, even northern<br />
let them eat colonies