In the taiga, many lakes and ponds were formed by glacial activity during the last Ice Age. As glaciers advanced and then retreated, they carved out depressions in the landscape, which later filled with water, creating lakes such as Lake Baikal in Siberia. Additionally, kettle ponds formed from melting ice blocks left behind by glaciers are common in this region. These bodies of water play a crucial role in the local ecosystem and support diverse wildlife.
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