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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 Tickets 2026 Concert Schedule - Bandsintown
Be the first to know about new shows at Holocene, buy official tickets, see photos, read reviews, explore upcoming events, and get directions
- Venue Info - Holocene
Holocene is a music + arts venue, nightclub and events space in the core of inner-SE Portland Since the summer of 2003, Holocene has been hosting touring acts from folk to minimal techno, Portland’s own most exciting musicians, unforgettable dance parties, and all manner of arts and multimedia parties that blur the line between highbrow and
- Holocene extinction - Wikipedia
Some experts mark the transition from the Holocene to the Anthropocene at the onset of the industrial revolution They also note that the official use of this term in the near future will heavily rely on its usefulness, especially for Earth scientists studying late Holocene periods
- 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 Epoch - Climate, Biota, Human Impact | Britannica
In the high to mid-latitudes after the early Holocene, with its remnants of ice-age conditions (tundra passing to birch forests), there was a transition to the mid-Holocene, marked by a progressive change to pine forest and then oak, beech, or mixed forest
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