GES 3A — Climate history + glacial cycles

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Last updated 12:19 AM on 4/21/26
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21 Terms

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Hot-house climate

A climate state with no year-round ice at the poles.

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Cold-house climate

A climate state where ice is present at the poles year-round.

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Current climate state

Earth is currently in a cold-house climate state.

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Snowball Earth

An extreme cold-house state where nearly the whole planet is covered in ice.

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Glacial period

A colder time when glaciers advance and cover more of Earth.

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Interglacial period

A warmer time between glacial periods when glaciers retreat and sea level rises.

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Current glacial-cycle period

Earth is currently in the Holocene interglacial period.

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Holocene

The current interglacial period that began about 11,700 years ago.

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Glacial cycle

The natural advance and retreat of glaciers over time, including both glacial and interglacial periods.

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What drives glacial cycles

Milankovitch cycles plus Earth feedback loops.

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Oxygen isotopes and climate

The ratio of O-18 to O-16 in shells and ice cores helps scientists infer past temperature and ice volume.

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O-18 in seashells

A larger positive O-18 departure in seashell sediment usually means colder conditions.

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O-18 in ice cores

Colder climates leave less heavy oxygen in ice cores because O-18 condenses and falls out sooner.

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Why O-18 changes with climate

In cold climates, heavy oxygen precipitates more easily, enriching oceans and shells while leaving less in polar ice.

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Laurentide Ice Sheet

A huge ice sheet that covered much of North America during the last ice age.

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Evidence of the last ice age

Great Lakes, smoothed landforms, erratics, fertile plains soils, and cold-adapted fossils.

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Erratics

Rocks dropped by glaciers as the ice melts.

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Volcanism and deglaciation

As ice retreats, reduced ice mass can contribute to isostatic rebound and may influence volcanism.

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Younger Dryas

A sudden return to near-glacial conditions during the warming out of the last ice age.

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Why Younger Dryas matters

It is a famous example of abrupt climate change.

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Cause of Younger Dryas

It is believed to be linked to weakening of the Atlantic Meridional Overturning Circulation (AMOC).