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The most compelling evidence of ancient glacier debris in Southern Africa would likely be found in the form of glacial till, which consists of unsorted sediments deposited by glaciers. This material can include a mix of rocks, clay, silt, and boulders that were transported and left behind as glaciers advanced and retreated. Additionally, features such as striations on bedrock, indicating glacial movement, or moraines, which are ridges formed by accumulated debris, could also provide evidence of past glacial activity in the region. These geological formations suggest that Southern Africa experienced glacial conditions during past ice ages.

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1mo ago

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