Sign up for Lesson Plans, discounts & more!

The Quaternary Period:
Ice, Giant Mammals, Humans and More

The Quaternary Period began with an ice age about 1.8 million years ago. Throughout the period glaciers have been present, sometimes more and sometimes less. It is also the time of giant mammals, humans, Saber toothed cats and other fierce predators all share the stage as the earth takes its present form.

 It is sometimes called the Age of Humans because this is the only period humans have been around.

It continues up to the present time and is the period that we live in. It is divided into two epochs :

  • The Pleistocene Epoch - 1.8 million to 11,000 years ago
  • The Holocene Epoch - 11,000 years ago to present

Each epoch has unique characteristics for climate and geography, so the plants and animals that lived during those times are unique to each epoch, too.

Quaternary Ice age

The Geologic Time Naming System
In the early 1800’s a system for naming geologic time periods was devised using four periods of geologic time. They were named using Latin root words. In Latin, quatr means four. Early geologists chose the name Quaternary for the fourth period in this system. We no longer use this system of dividing geologic time, but the name, Quaternary, is still commonly used for the most recent period in geologic time.

The system for naming the periods is constantly changing. As more information is collected, analyzed, and debated, the divisions created for looking at geologic time changes. There have been recent changes to the way scientists look at this time. There was talk of dropping the old name for a new one called the Neogene Period. The old name had many defenders and there was debate about changing the name. Eventually the matter was settled and the old name kept its place.

Traditional Periods
New Periods


Holocene Epoch
Pleistocene Epoch
Pliocene Epoch
Miocene Epoch
Oligocene Epoch
Eocene Epoch
Paleocene Epoch

Continents Arrive at Present PositionsDuring the quaternary period the positions of the continents were much the same as they are today. What has changed during this time is the climate. The Pleistocene Epoch began with polar ice sheets far bigger than they are now. At times, the glacial ice reached far down into parts of North America, Europe, and Asia. This is commonly referred to as an Ice Age.

The Climate of The Quaternary Period
Generally temperatures were cooler everywhere on earth during this time. But the climate of the Pleistocene did not stay the same throughout the entire Pleistocene. The polar ice advanced and retreated. The earth warmed and cooled. Scientists have cataloged over 60 cycles of glacial expansion and contraction during the Pleistocene.

Still In The Ice Age?
There is a reason the polar ice advances and retreats. It isn’t random. The variations are because of changes in the Earth's orbit. These are called Milankovitch cycles. The last major glacial advance was about 18,000 years ago. Some scientists say that we are still in an ice age and the current warming trend is just an interglacial period or temporary retreat of the polar ice.

Glaciers Lower Sea Levels

When the polar ice advances, huge amounts of water become locked up in the ice. This causes sea levels to drop. Land once covered by water is left high and dry. During a time of advancing glaciers, the Bering land bridge revealed itself between Alaska and Siberia. This happened many times during the Quaternary Period.

Animals Adapt To The Cold
Even though many of the plants and animals of the Quaternary Period are virtually the same as those living today, there are some important differences. First, there were certain animals that were well-adapted to the cold climate of the early Pleistocene Epoch. The wooly mammoth, mastodon, wooly rhinoceros, reindeer, and musk ox all developed thick fur to help them survive the frigid temperatures. Most of these animals became extinct when climates warmed in the Holocene Epoch. No one knows why. But as with all mysteries lots of theories have been put forth. One popular theory says that humans hunted them to extinction. Another says that these animals could not adapt to the warmer climate. The only thing that is for sure is that these huge beasts no longer walk the earth!

The Quaternary Period: A Time Of Giant Mammals or Megafauna

The Pleistocene is known for its megafauna or “giant mammals.” Along with the wooly mammoth and wooly rhinoceros there were other giants: bison, ground sloths, and deer. There were giant carnivores as well. The saber tooth cat, cave bear, and dire wolf were bigger than their modern counterparts. The megafauna disappeared at the end of the Pleistocene. All that remains are a few species of smaller, though still good-sized, animals in Africa: the elephant, hippopotamus, and rhinoceros.

The Rise of Humans
For us, the most important development of the Quaternary Period is the development of the hominids: Humans. From the first primates in the Tertiary Period to modern man, the hominid species has evolved amazing abilities. The earliest hominid fossils found so far date from the late Tertiary Period. They were found in Africa. As the Pleistocene Epoch continued, hominids spread throughout the world. Their larger brains allowed a level of thought and feeling that was, and is, unique among the animals. We think and solve. We change and control. The future of our planet will be greatly affected by the Age of Humans.

Go to Geologic Time Line

Before the Quaternary Period is the Tertiary Period

Check out some of the Educational Materials for sale on our sister site

Share this page:
Enjoy this page? Please pay it forward. Here's how...

Would you prefer to share this page with others by linking to it?

  1. Click on the HTML link code below.
  2. Copy and paste it, adding a note of your own, into your blog, a Web page, forums, a blog comment, your Facebook account, or anywhere that someone would find this page valuable.

interested in more? If so, you may want to check out our other sites: - Our online fossil and mineral rock shop. - An educational site about rocks, minerals, and geology.