New evidence of Noah’s Flood from Mexico

Dinosaur Velafrons coahuilensis

Dinosaur dig reveals dramatic insights into the degree of devastation, not so long ago

by Dr Tas Walker

A new dinosaur find from Mexico gives a vivid insight into the enormous extent of Noah’s Flood catastrophe as well as the magnitude of the processes involved. An international research team led by scientists from the Utah Museum of Natural History unveiled the fossilized remains of one of the casualties of that event, a previously unknown species of dinosaur, which they called Velafrons coahuilensis.

The team, of course, did not report the evidence within a Flood framework. So, although the team hopes the find will give fresh insights into the ancient environments of western North America, they have not considered the most important factor—Noah’s Flood. It’s a bit like trying to explain the history of Europe without reference to the Second World War.

The dinosaur skeleton was excavated in the 1990s in north-central Mexico about 27 miles west of Saltillo, near a small town called Rincon Colorado in the state of Coahuila. The creature was a hadrosaur, or duck-billed dinosaur, with a large crest on its head that looked like a small sail.

Even though the animal was judged to have been young when it died it would still have been some 25 feet long. Its remains would have needed to be buried promptly to be preserved, and this would require a considerable quantity of sediment.

The sedimentary layers in which the remains of the animal were buried were thick. They are part of the sedimentary rock unit called the Cerro del Pueblo Formation, and its characteristics indicate something of the enormous magnitude of the watery catastrophe involved.

Paleocurrent analysis reveals that the floodwaters were flowing to the east while the enormous quantities of sediment comprising the formation were deposited in huge sheets over a wide geographical area.

The thickness of the formation varies from about 500 m in the west to 150 m in the east near Saltillo, a distance of 70 km. The Cerro del Pueblo Formation is part of a much larger sedimentary package many kilometres thick deposited in the extensive Parras Basin. Such a huge depth of sediment would not accumulate unless the relative sea level in the area was rising continually to provide the necessary accommodation.

The flow of water was highly variable during deposition, as indicated by characteristics of the different strata. There was ample evidence of cross-stratification within the strata, including planar cross-stratification, trough cross-stratification and ripple cross-lamination, all of which indicate strong water flow.

Some sandstone strata contained pebbles and granules, which also give insight into the water currents involved.

Another indication of the power of the water was the thicknesses of the individual strata. The beds of sandstone were frequently massive and many metres thick. There were numerous multi-metre beds of massive mudstone that coarsened upwards, suggesting repeated, enormous and extensive mudflows. Beds often displayed what is called ‘soft sediment deformation’, indicating a deposition so rapid that the beds slumped and moved before they had time to settle and consolidate….


image credit: by Dinoraul