0.6" Palaeolagus Hayeni Fossil Jaw Section Teeth Oligocene Epoch South Dakota Display Cricket where the movement of frozen

where the movement of frozen lake ice during winter often exposes new stones in the spring

It is a hydrated copper silicate mineral that belongs to the phyllosilicate group

indicates that these organisms thrived during periods of favorable climate and nutrient-rich seas

This natural stone offers a unique texture that reflects its deep-earth origins

0.6" Palaeolagus Hayeni Fossil Jaw Section Teeth Oligocene Epoch South Dakota Display Cricket where the movement of frozenLocation: Brule Formation, Pennington County, South Dakota Weight: 0. 2 Ounces Dimensions: 0. 6 Inches Long, 0. 4 Inches Wide, 0. 2 Inches Thick Comes with a free display. The item pictured is the one you will receive. Oligocene epoch, 33. 9 to 23 million years ago Palaeolagus hayeni is an extinct species of lagomorph, an ancient rabbit, that lived in North America during the Oligocene epoch. It belongs to the genus Palaeolagus, one of the earliest