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Reading Check 4. State Why did Wegener suggest that continents in the southern hemisphere had a colder climate long ago?

Ask by Lane Ross. in the United States
Jan 09,2025

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Wegener thought that continents in the southern hemisphere were once part of a supercontinent called Gondwana, which was near the South Pole. This made those areas much colder long ago. As Gondwana broke apart and the continents moved away from the poles, their climates became warmer.

Solución

Alfred Wegener proposed that the continents in the southern hemisphere once formed part of the supercontinent **Gondwana**, which was located closer to the South Pole. Because of their polar positioning within this unified landmass, Wegener suggested that these continents experienced much colder climates in the distant past. As Gondwana gradually broke apart and the continents drifted to their current positions away from the polar regions, their climates warmed. Thus, the historical proximity to the South Pole was the primary reason Wegener attributed to the colder climates of southern hemisphere continents long ago. **Key Points:** - **Supercontinent Gondwana:** Wegener believed southern continents were once joined in Gondwana. - **Polar Positioning:** Located near the South Pole, leading to colder climates. - **Continental Drift:** Movement away from the poles resulted in warmer climates over time.

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Wegener proposed that continents in the southern hemisphere once had a colder climate because of evidence like the distribution of glacial deposits and coal beds. For instance, he found glacial striations and till deposits in areas that are now tropical, indicating they were once situated near the South Pole, when the continents were joined together as one supercontinent, Pangaea. This suggested a harsh, icy climate in the past that contrasted sharply with today's climates. Additionally, Wegener observed fossils of tropical plants and past climates in regions that are now cold, hinting at a significant climate shift over millions of years. This strange juxtaposition led him to envision a world where continents slowly drifted apart, taking their climates with them—a revolutionary idea at the time that paved the way for modern plate tectonics!

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