In the popular imagination, the "Ice Age" happened in the distant past, but in fact, the ice age is still ongoing today. We just live in a warm pocket known as an interglacial period, also known as the Holocene. Our ice age began 2.6 million years ago at the start of the Pleistocene epoch. Repeated periods of glacial incursions during the Pleistocene created the permanent ice sheets that cover Antarctica, Greenland, and parts of the Arctic. The changing environment also allowed for the development of large animals known as megafauna adapted to the climate, including the woolly mammoth.

A full-grown woolly mammoth, just one species of the genus Mammuthus, stood 10-12 feet at the shoulder with shaggy hair. The woolly mammoth's hair provided a substantial advantage in the struggle to stay warm.

As pictured above, this specimen is a Woolly Mammoth bone cross section with an included display stand. The material is 22,000 years old and comes from Sibera, where the animals once roamed the Pleistocene tundra.

Each specimen is sold individually by size and comes with a certificate of authenticity. You can see all available mammoth bone specimens in the collection below.

Please Note: This specimen is US shipping only. It is untreated, prehistoric, bone material and has a slight natural scent (similar to linseed oil.) Please keep the specimen in a climate controlled environment and away from pets (as they may try to take a bite!)

"Various legends exist about frozen mammoths. It has been said that the scientists who excavated the Beresovka mammoth, discovered in the year 1900, enjoyed a banquet on mammoth steak. What really appears to have happened is that one of them made a heroic attempt to take a bite out of this meat but was unable to keep it down, in spite of a generous use of spices." ~ Björn Kurtén in "How to Deep Freeze a Mammoth"

Roughly the mass of a modern African elephant, the woolly mammoth evolved some 400,000 years ago in Siberia from the steppe mammoth widespread on that continent, and ultimately spread westward into Europe and eastward into North America via the Beringian land bridge that once connected modern-day Russia and Alaska.

This event may have been the second mammoth invasion of the New World, as the steppe mammoth forayed to North America about 1.5 million years ago and evolved there into the endemic (and enormous) Columbian mammoth.

Mammoths were an important food source to early humans and neanderthals. They even used their bones and hides to create huts and other structures.

In Pleistocene North America, woolly mammoths primarily roamed the cold, treeless tundra-grasslands immediately below the continental ice sheets—the American reach of the mammoth steppe—while Columbian mammoths occupied a more southerly, temperate range encompassing most of today's Lower 48 States and which extended deep into Mexico.

They shared this territory with fellow Pleistocene grazers, subsisting mainly on grasses and sedges along with willows, alders, and other stunted trees that grew sparsely in the high-latitude steppe lands, far more diverse biomass than the modern Arctic tundra.

After disappearing from continental ranges roughly 10,000 years ago, small, isolated populations of woolly mammoth survived on Alaska's St. Paul Island until about 5,600 years ago and on Russia's Wrangel Island until perhaps 4,000 years ago. All of these pockets eventually died out due to the lack of genetic diversity that comes from metropolitan interactions with larger populations.

Some woolly mammoth teeth have been discovered with a uniquely blue coloring to them. This stunning shade is due to vivianite implantations, a mineral formed by the combination of animal phosphorous and iron in the soil.

Vivianite is usually pale or colorless when it forms, but when it is exposed to air the oxidation causes it to turn to a brilliant blue. In the right conditions, this process can produce incredible streaks of dark to light blue coloring in mammoth teeth, which is an incredible reminder as to the deep history of the fossil.

Interestingly, this can also occur on the skin of a well perserved animal as well. In fact, some ancient bisons have been found in the ice with blue coatings over their horns and bodies. It reminds us of the other famous blue megafauna we know: Babe the Big Blue Ox!