Mud Crack Evidence
The most common theory about how dinosaur footprints were made and preserved as fossils is that the dinosaur stepped in mud along a lake shore leaving a footprint. The mud dried out in the sun and hardened. The next annual flood brought more sediment which buried the hardened footprints in more sediment which eventually hardened.
When mud quickly hardens in the sun the result are mud cracks. As the water is dried out of the mud the overall volume of the mud decreases, resulting in cracks. Mud cracks can also form under water. As sediment builds up underwater the weight of the sediment will squeeze the water out of the lower layers of water. Underwater mud cracks can also form as a result of changes in salinity of the water. In either case this results in mud cracks which can then fossilize. Mud cracks formed underwater have a different pattern than those formed in the sun. And the shape of mud cracks formed in the sun will vary depending on how many times the mud was wet, dried out, and re-cracked.
The dinosaur tracks in our museum come from the Connecticut River Valley in Massachusetts. This setting gives us a unique opportunity to study the relationship of dinosaur tracks and mud cracks. The local conditions were that of a shallow muddy lake shoreline, with frequent water level fluctuations and a high sedimentation rate. The result was rapid, deep, and successive episodes of burial that preserved dinosaur footprints, water ripples, raindrop impressions and mud cracks... but the mud cracks are only seen in certain locations. This should raise the question, why?