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1 The Earth in Context
2 The Way the Earth Works: Plate Tectonics
3 Patterns in Nature: Minerals
4 Up From the Inferno: Magma and Igneous Rocks
5 A Surface Veneer: Sediments and Sedimentary Rocks
6 Change in the Solid State: Metamorphic Rocks
7 The Wrath of Vulcan: Volcanic Eruptions
8 A Violent Pulse: Earthquakes
9 Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building
10 Deep Time: How Old is Old?
11 A Biography of Earth
12 Riches in Rock: Energy and Mineral Resources
13 Unsafe Ground: Landslides and Other Mass Movements
14 Streams and Floods: The Geology of Running Water
15 Restless Realm: Oceans and Coasts
16 A Hidden Reserve: Groundwater
17 Dry Regions: The Geology of Deserts
18 Amazing Ice: Glaciers and Ice Ages
19 Global Change in the Earth System


The Discovery of Pleistocene Mammals

by Stephen Marshak
Overview Image

Shown here is a plaster cast scull of Dinotherium giganteum. These ancient relatives of the modern elephant inhabited Earth from the Miocene into the Pleistocene. They reached a height of 4 m (13 feet) at the shoulders, and used their tusks to uproot plants.

Credit: Stephen Marshak

As early as the 1600s, scholars were arguing over the meaning of enormous bones found in sedimentary deposits in Europe. Most thought the bones were relicts of giant humans that had been drowned in Noah's flood. But in 1796, the French anatomist Georges Cuvier used his detailed knowledge of anatomy to show that these giant bones instead resembled those of elephants but were not the bones of any elephant species then alive. Since no one had ever seen these elephants and it seemed unlikely that they could be hiding anywhere, Cuvier reasoned that they must be extinct. The concept seemed outrageous to people of Cuvier's time, who could think of no reason for extinction to occur.

In the early 1800s, explorers discovered still more bones of extinct mammals: cave bears, giant lions, hyenas, and saber-toothed cats. Construction workers even unearthed hippopotamus bones in glacial drift beneath London. The final documentation of Pleistocene mammals came in the early twentieth century, when several Russian expeditions found wooly mammoths that had been frozen intact in the Siberian ice. Much of the mammoth's skin, hair, and flesh remained, and their 30,000-year-old meat was still edible (as far as the sled doges were concerned).


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