From find to skeleton
Preparing the fossil was an enormous task. The pelvis, for example, had to be extracted from very hard sandstone. The challenge was that the fossilized bone is almost as hard as the surrounding rock, making it difficult to distinguish where bone ends and stone begins. This makes the preparation process extremely time consuming. The neck vertebrae were embedded in claystone, which brought its own difficulties. Many of the vertebrae were deformed, but the preparator skillfully reconstructed them, creating a slightly S-shaped neck. This shape matches what has been seen in previous reconstructions. The Allosaurus is displayed in an active pose, as if it is walking away.
Brown
The skeleton appears mostly brown due to the presence of iron oxide (rust). There are also whitish patches visible on the fossil. These marks were likely caused by an unknown mineral that, as it broke down, partially dissolved the iron oxide, creating the lighter spots.
Where did we find the Allosaurus?
The Allosaurus at Museon-Omniversum was discovered in the world-famous Morrison Formation. This sedimentary layer formed between 155 and 148 million years ago in the central United States and covers an area of 1.5 million km². At that time, the climate was much warmer than today. A subtropical climate extended as far north as 60° latitude roughly the southern tips of Greenland and Finland and there are indications that dry seasons also occurred. In the southern part of the Morrison Formation, sandstone layers were formed as dunes in a desert environment. Further north, the formation consists of sediments deposited by meandering rivers, which left traces in the form of sandy channels. It was within these river deposits that the Allosaurus was found.