Interglacial

The interglacial environment supported a variety of animal life.

The interglacial atmosphere had higher concentrations of carbon dioxide than the preceding glacial period.

The interglacial period was marked by milder temperatures than the preceding glacial period.

The interglacial period witnessed the evolution of various animal species.

The interglacial soil was fertile and perfect for farming.

The interglacial terrain was shaped by the action of glaciers and rivers.

The interglacial period allowed for the growth of lush vegetation.

The interglacial climate made it possible for human civilizations to thrive.

The interglacial environment was favorable for the development of human civilizations.

The interglacial atmosphere was rich in oxygen.

Interglacial climates were characterized by abundant vegetation cover.

The interglacial climate supported the proliferation of marine life forms.

The Holocene epoch, which began about 11,700 years ago, is the current interglacial period.

The end of an interglacial period typically marks the beginning of an ice age.

Scientists have studied ancient pollen records to learn more about interglacial periods.

The melting of glaciers during an interglacial period can cause sea levels to rise.

An interglacial is a time period between two ice ages.

Many species of animals have evolved and adapted during interglacial periods.

During the last interglacial, the Earth's climate was warmer than it is today.

The length of interglacial periods can vary greatly.

During an interglacial period, the Earth's temperature is warmer and the glaciers recede.

The interglacial atmosphere was different from what we experience today.