Near the equator.
Evidence of continental drift in Antarctica includes the presence of similar rock formations and fossils found on the continent that match those in South America, Africa, and Australia, indicating these landmasses were once connected. Additionally, glacial deposits and geological features, such as mountain ranges, show patterns consistent with the theory of plate tectonics and past continental configurations. Paleoclimate data also suggest that parts of Antarctica were once located in warmer climates, supporting the idea of its movement over geological time.
it was connected to antarctica as shown by how it fits perfectly together with it
Scientists have found evidence in sediment cores and ice cores that indicate Antarctica was once much warmer than it is today. Fossils of plants and animals that could not survive in the current polar climate have been discovered, as well as ancient climate indicators like soil composition and isotopic analysis. These findings suggest that Antarctica had a different climate in the past due to changes in greenhouse gas concentrations and the position of the continent.
Lava flows in Antartica
Once located closer to the equator
It is said that Antarctica was once a warm continent, Therefore it once held warm weather animals, But the climate started to change and it became cold, Therefore the fossils of warm blooded animals can be found in Antarctica. +++ The world's climate was warmer and Antarctica was part of a much larger continent lying further North.
Allan Hills 84001 is a meteorite that was found in Antarctica in 1984. It gained attention in 1996 when scientists reported possible evidence of ancient Martian life within the meteorite, though this claim is still debated within the scientific community.
he found plants from antarctica that were the same as the ones from africa, proving they were once connected
Fossils in Antarctica can provide information on past climatic conditions by indicating the types of plants and animals that lived in the region. For example, the presence of fossils from species that typically thrive in warmer climates may suggest that Antarctica was once much warmer than it is today. Similarly, evidence of glacial deposits in fossil records can indicate periods of ice growth and retreat, providing insights into past climatic fluctuations in the region.
Evidence for continental drift includes the fit of continents like South America and Africa, similar rock formations and mountain ranges on different continents, and the distribution of fossils that were once found on now widely separated landmasses. These pieces of evidence suggest that the continents were once connected in a single landmass called Pangaea.
The coal deposits in Antarctica are explained by Pangaea where Antarctica was located next to South America, Africa, Australia, and India.
During the Cretaceous Period, Antarctica was covered with forests and was for a period of time, tropical. The continent gradually drifted southward to its present position over the south polar region.