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interglacial

[ in-ter-gley-shuhl ]

adjective

, Geology.
  1. occurring or formed between times of glacial action.


interglacial

/ ˌɪntəˈɡleɪsɪəl; -ʃəl /

adjective

  1. occurring or formed between periods of glacial action
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

noun

  1. a period of comparatively warm climate between two glaciations, esp of the Pleistocene epoch
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

interglacial

/ ĭn′tər-glāshəl /

Adjective

  1. Occurring between glacial epochs.

Noun

  1. A comparatively short period of warmth during an overall period of glaciation. Interglacials are characterized both by the melting of ice and by a change in vegetation.
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Word History and Origins

Origin of interglacial1

First recorded in 1865–70; inter- + glacial
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Example Sentences

The objects date from the end of a warm interglacial period 300,000 years ago, about when early Neanderthals were supplanting Homo heidelbergensis, their immediate predecessors in Europe.

The AWG demonstrated "beyond a reasonable doubt" that the "relatively stable interglacial conditions" that existed since the start of the Holocene Epoch 11,700 years ago no longer exist because of human activity; that the changes are irreversible; that geological strata associated with these changed conditions are "distinct from Holocene strata"; and that the plutonium concentrations from the stratotype section at Crawford Lake, Canada has been confirmed by precisely similar results in strata around the world.

From Salon

In the years that followed, extensive excavations have gradually yielded numerous wooden objects from a layer dating from the end of a warm interglacial period 300,000 years ago.

The thallium isotope ratios showed the global ocean lost oxygen overall during the last ice age compared to the current warmer interglacial period.

Geological evidence suggests this collapse happened at least once in the past several million years—perhaps during the last interglacial.

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