kestvusperioodid
Kestvusperioodid, also known as interglacial periods, are recurring intervals of relatively warm climate that occur between glacial periods. These warm periods are characterized by the absence of large ice sheets, allowing for the expansion of vegetation and the presence of various animal species that are adapted to temperate climates.
During kestvusperioodid, the average global temperature is often 2-3°C higher than during glacial periods. This warming
Kestvusperioodid have played a significant role in shaping the Earth's geological history, allowing for the establishment
These warm periods are also crucial for understanding current and future climate change, as they provide valuable