The concept of the 'Anthropocene' has gained significant traction in geological and environmental circles, proposing that human activity has become the dominant influence on the Earth's geology and ecosystems. Unlike previous geological epochs, which were defined by natural processes such as glaciation or tectonic shifts, the Anthropocene is characterized by markers like radioactive isotopes from nuclear tests, plastic pollution, and elevated carbon dioxide levels. Proponents argue that this new epoch began around the mid-20th century, a period of rapid industrialization and population growth known as the 'Great Acceleration.' However, critics contend that formalizing the Anthropocene as a geological epoch oversimplifies the complex, uneven impacts of human activity across different regions and time periods. They suggest that focusing on a single global start date obscures the historical roots of environmental change, which began much earlier with agriculture and colonialism. This debate highlights not only a scientific question but also a philosophical one about how humanity's role in shaping the planet should be conceptualized and periodized.