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  • Holocene - Wikipedia
    The Holocene is an interglacial period within the ongoing glacial cycles of the Quaternary, and is equivalent to Marine Isotope Stage 1 The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth's obliquity
  • Holocene epoch | Causes, Effects, Facts | Britannica
    Holocene Epoch, younger of the two formally recognized epochs that constitute the Quaternary Period and the latest interval of geologic time, covering approximately the last 11,700 years of Earth’s history
  • The Holocene Epoch
    The Holocene is the name given to the last 11,700 years* of the Earth's history — the time since the end of the last major glacial epoch, or "ice age "
  • Holocene - New World Encyclopedia
    The Holocene epoch is the geological period extending from the present day back to about 10,000 radiocarbon years, approximately 11,430 ± 130 calendar years before present (BP) (between 9560 and 9300 B C E )
  • Holocene - an overview | ScienceDirect Topics
    Holocene comprises the last ∼ 11000 years and is the shortest epoch in the history of our planet This time span is important in many aspects, particularly in terms of man's development and subsequent interventions and modifications of the land and the natural resources
  • What Is the Holocene Extinction and What Causes It?
    However, the popular and established term remains the Holocene Extinction, referring to the geological epoch that began approximately 11,700 years ago The defining feature is the unprecedented acceleration of species loss since the rise of human civilization and industrialization
  • Smithsonian Institution - Global Volcanism Program: Worldwide Holocene . . .
    The Global Volcanism Program (GVP) seeks better understanding of all volcanoes through documenting their eruptions during the past 12,000 years
  • Holocene Explained
    The Holocene is an interglacial period within the ongoing glacial cycles of the Quaternary, and is equivalent to Marine Isotope Stage 1 The Holocene correlates with the last maximum axial tilt towards the Sun of the Earth's obliquity
  • Holocene - Simple English Wikipedia, the free encyclopedia
    The Holocene is the present geological epoch It started around 11,000 years ago after the last ice age We are now in a relatively warm climate in Earth's history This is the second epoch of the Quaternary and the seventh of the Cainozoic Holocene comes from two Ancient Greek words
  • A mid-Holocene age for Monte Verde challenges the timeline of . . . - AAAS
    They defined the younger Monte Verde Formation as a Late Pleistocene and Early Holocene alluvial terrace that preserves the MV-II component at its base We refer to the sands and gravels of the Salto Chico Formation as stratigraphic unit 1a (SU1a) Conformably overlying SU1a are fine-grained clastic and organic sediments we call SU1b, -c, -d





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