What was the Wisconsin Glaciation?
The Wisconsin glaciation (also known as the Devensian, Midlandian, Würm, and Weichsel glaciation in different areas around the world) was the last Ice Age, during which glaciers extended as far south as modern-day California, New York, France, Germany, and Poland. Most of Europe was either frozen solid or steppe-tundra, much as Siberia is today. The Wisconsin glacial advance began about 70,000 years ago, reaching its maximum extent 18,000 years ago, before receding. Although there were numerous Ice Ages throughout the last few million years, the Wisconsin glaciation is what is usually being referred to when people say “Ice Age,” because it is the most recent, sculpted many modern geological features (particularly in the Northern hemisphere), and affected human evolution and culture the most. Because of successive glaciations, it is sometimes difficult to determine exactly which Ice Age had an effect on which geological feature, but thorough investigation has largely been able to piece
The Wisconsin glaciation (also known as the Devensian, Midlandian, Würm, and Weichsel glaciation in different areas around the world) was the last Ice Age, during which glaciers extended as far south as modern-day California, New York, France, Germany, and Poland. Most of Europe was either frozen solid or steppe-tundra, much as Siberia is today. The Wisconsin glacial advance began about 70,000 years ago, reaching its maximum extent 18,000 years ago, before receding. Although there were numerous Ice Ages throughout the last few million years, the Wisconsin glaciation is what is usually being referred to when people say “Ice Age,” because it is the most recent, sculpted many modern geological features (particularly in the Northern hemisphere), and affected human evolution and culture the most. Because of successive glaciations, it is sometimes difficult to determine exactly which Ice Age had an effect on which geological feature, but thorough investigation has largely been able to piece
