The concept of the 'Anthropocene' has gained traction among geologists as a proposed new geological epoch defined by significant human impact on Earth's systems. Unlike previous epochs, which were shaped by natural forces such as volcanic activity or orbital variations, the Anthropocene is marked by distinctive stratigraphic signatures, including radioactive isotopes from nuclear tests, microplastics, and elevated carbon dioxide levels. However, the formal recognition of this epoch remains contentious. Some scholars argue that the term oversimplifies the complex, heterogeneous nature of human-environment interactions, while others contend that it serves as a powerful catalyst for interdisciplinary research and public awareness. The debate underscores broader questions about how scientific classifications reflect cultural and political values, and whether naming a new epoch might inadvertently reinforce a narrative of inevitable environmental degradation rather than encouraging proactive stewardship.