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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


noun

  1. a period of comparatively warm climate between two glaciations, esp of the Pleistocene epoch

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

Her models incorporate data on how the creeping churning of the mantle and other geologic phenomena have altered land and sea elevation, particularly during interglacial periods when Earth’s temperatures were a few degrees higher than they are today.

The researchers also used computer models to simulate climate conditions the plants faced during glacial and interglacial cycles.

“This is an ice age, and so a lot of the Earth’s surface was very cold at different times of the year in both the glacial and interglacial scenarios,” Matthaeus says.

We’re technically in the midst of an ice age now, living through an interglacial that started about 11,000 years ago.

The last four interglacials, according to the USGS, have lasted over approximately 20,000 years, “with the warmest portion being a relatively stable period of 10,000 to 15,000 years duration.”

During the first and second interglacial epochs the climate appears to have been warmer than at present.

He also took up a much bolder attitude on the question of interglacial deposits and the relation of man to the Ice Age.

In both cases it is extremely difficult, or quite impossible, to assign the remains to definite glacial or interglacial times.

Many of the valleys of our present rivers are but patchworks of preglacial, interglacial, and postglacial courses (Fig. 366).

It was followed by the Third Interglacial epoch which may have extended over at least 100,000 years.

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