Glacial deposits often form at high latitudes near the poles. Explain why glacial deposits have been found in Africa.

COntinents drift, so a place that is near the equator now was not necessarily close to the equator a long time ago.

Also, there is some evidence that there has been a global glaciation:

http://en.wikipedia.org/wiki/Snowball_Earth

Glacial deposits are typically found in regions near the poles because these areas experience long, cold winters, which allow snow and ice to accumulate over time. However, glacial deposits have also been found in some parts of Africa. This occurrence may seem peculiar, considering Africa's mostly warm and tropical climate.

The presence of glacial deposits in Africa can be attributed to past climate conditions and geologic history. Millions of years ago, during different geological periods, the Earth's climate was drastically different from what it is now. Africa, like other continents, has experienced numerous geological and climatic changes throughout its history. This includes periods when the climate was colder and ice sheets formed in higher latitudes.

One notable example is the glacial deposits found on Mount Kilimanjaro, the highest peak on the African continent. These deposits are remnants of ancient glaciers that formed during previous ice ages when the climate in the region was much colder and mountainous areas were able to support the growth of glaciers.

To determine if glacial deposits exist in Africa or any other region, scientists primarily rely on geological evidence and dating techniques. They analyze sedimentary layers, the presence of distinct glacial landforms like moraines, striations, and drumlins, as well as the composition of rocks and minerals. By studying these features and comparing them with known glacial deposits elsewhere, scientists can deduce the presence and characteristics of glacial activity in various regions, including Africa.

So, in summary, glacial deposits have been found in Africa due to past periods of colder climates when ice sheets and glaciers could form in regions that are now warmer and predominantly non-glacial. The geologic record and evidence gathered through scientific research help us reconstruct the Earth's climatic history and understand the diverse phenomena that have shaped our planet over millions of years.