* Ancient Gondwana: Antarctica was once part of the supercontinent Gondwana, a massive landmass that existed millions of years ago. This landmass included what is now South America, Africa, Australia, India, and the Arabian Peninsula.
* Tropical Climates: During the Carboniferous and Permian periods (around 359 to 252 million years ago), Gondwana's climate was much warmer and wetter than today's Antarctica. This allowed vast forests to flourish in the region.
* Swampy Environments: These forests grew in swampy, low-lying areas, similar to today's rainforests. As trees died, they fell into the water and were covered by sediment. Over millions of years, pressure and heat transformed this organic matter into coal.
* Continental Drift: The Earth's tectonic plates have been shifting for millions of years, slowly breaking apart Gondwana. Antarctica eventually drifted to its current location at the South Pole.
The coal deposits in Antarctica are a powerful reminder that the Earth's continents and climates are constantly changing.
