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Some of the lasting effects of the ice ages that can still be seen today include the formation of various landforms such as valleys, lakes, and hills due to the movement of glaciers. The ice ages also led to changes in sea levels and the distribution of flora and fauna. In some areas, remnants of ice sheets can still be found.
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During the 1800s, scientists came to the consensus that the Earth had experienced a number of ice ages in which large parts of the planet had been covered in ice sheets. During the last glacial maximum, the location of what is now Boston had more than a full kilometer of ice above it. Toronto had two kilometers. Montréal had more than three. The southernmost edges of the North American ice sheet were in northern Kentucky and West Virginia.
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How should investors manage the inevitabilities of risk? What are the most powerful wealth-building tools that require little technical skill? How do...
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