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Archaeology is the scientific study of human history and prehistory through the excavation and analysis of artifacts, structures, and other physical remains. This category delves into the history of human civilizations, ancient cultures, and the evolution of societies. Explore the techniques used to uncover the past, the discoveries that have changed our understanding of history, and the ongoing efforts to preserve our shared cultural heritage.
Great Ages Archaeology refers to the study of distinct historical periods that are often classified according to the material primarily used during that era. These periods include the Stone Age, Bronze Age, and Iron Age.
In the field of Archaeological Anthropology, DNA dating offers a new dimension to understanding human history. This innovative technique incorporates knowledge from genetics, bioinformatics, and archaeology to estimate the age of human remains or artifacts.
The Pleistocene Epoch, often referred to as the Ice Age, is a significant period in Earth's history. Spanning from 2.6 million to 11,700 years ago, it was characterized by repeated glaciations, the evolution of modern humans, and the extinction of large mammals.
The Pliocene Epoch is a period in Earth's history that spanned from about 5.3 million to 2.6 million years ago. It is the last epoch of the Neogene Period in the Cenozoic Era, following the Miocene Epoch and preceding the Pleistocene Epoch.
The Miocene epoch, a significant period in Earth's history, extended from about 23 million to 5.3 million years ago. Characterized by drastic climate changes, the rise of new mammalian species, and the formation of new landscapes, the Miocene has left an indelible imprint on the planet.
The Oligocene epoch, a significant period in Earth's geological history, spanned from approximately 33.9 million to 23 million years ago. This epoch, nestled between the Eocene and Miocene epochs, was a time of considerable change and evolution, both in terms of climate and life on Earth.
The Eocene Epoch, one of the most intriguing periods in Earth's history, spans from around 56 to 33.9 million years ago, following the Paleocene Epoch and preceding the Oligocene Epoch.
The Paleocene epoch, a term derived from the Greek words "palaios" (old) and "kainos" (new), marks the beginning of the "old new" world following the extinction of the dinosaurs. This epoch, which spanned from 66 to 56 million years ago, was a time of significant global change and evolutionary innovation
The Mesozoic Era, often known as the Age of Reptiles, marks a pivotal time in Earth's history characterized by the dominance of dinosaurs and the emergence of flowering plants and modern mammals. This era is divided into three geologic periods: the Triassic, Jurassic, and Cretaceous.
The Cenozoic Era, also known as the Age of Mammals, is the current and most recent of the three Phanerozoic geological eras, following the Mesozoic Era and extending from 66 million years ago to the present day.
The Cretaceous period, spanning from approximately 145 to 66 million years ago, is the last geological period of the Mesozoic Era, following the Jurassic period and preceding the Paleogene period.
The Permian period, occurring approximately 299 to 252 million years ago, signifies the final epoch of the Paleozoic era, pre-dating the Mesozoic era, and is known for its immense biodiversity and the eventual mass extinction event.
