— Ch. 1 · Historical Destruction And Loss —
Prairie restoration.
~3 min read · Ch. 1 of 6
In the mid-1830s, after the Black Hawk War ended, settlers from northern Europe and the northeastern United States began plowing up tallgrasses and wild flowers across North America. By 1849, most species of prairie grass had vanished to make room for crops like soybeans and corn. The U.S. state of Illinois once held over 35,000 square miles of prairie land. Today just 3 square miles remain of that original expanse. Over farming combined with drought periods left soil exposed to wind and rain. This exposure contributed directly to the Dust Bowls of the 1930s. Restored prairies now represent only a fragment of the abundant verdure that once stretched from western Ohio to the Rockies.
Erosion Control Mechanisms
Prairie restoration reintroduces extensive fibrous root systems that bind soil against water erosion. When tallgrass was removed, surface pressures wore away Earth's crust material unchecked. Wind and rain worsened by climate change now strike harder than before. Ecologically, these restored ecosystems conserve topsoil which is vital for long term productivity. Adequate water filtration strengthens the ground against heavy rainfall events. Continued erosion reduces the fertile fields needed for cereal crops like barley and wheat. Prairie roots act as anchors holding soil in place where it would otherwise wash away.