Rating: 7/10
The folks who brought us Is Genesis History? have crafted a sequel of sorts. Host Del Tackett is back, and just as inquisitive as ever. Mountains after the Flood looks at areas of the Grand Canyon, and exposed layers around the world, including in our mountains, to show how quickly they were formed.
The conventional evolutionary thinking is that all these layers took eons to form. However, there are folds in these rock layers... and how could that be? If these layers took so long to form then they would have been hardened and unable to fold – any bending would have resulted in cracks and fracturing instead. So these smooth folds serve as evidence against the prevailing "long age" dating of the Grand Canyon.
But what if, instead of forming over hundreds of thousands of years, the folds were formed quickly in the cataclysmic aftermath of the Flood? Then the layers wouldn't be the result of millions of years, but would have been rapidly formed as the sediment settled during the Flood. And the bending could have happened while the layers were still soft. Under these circumstances we would understand how these still soft layers could have been bent over on themselves without cracking.
Mountains after the Flood is more technical than the previous film, and that's part of the point. In addition to exploring the evidence for the Flood, Tackett and his crew are also trying to show what doing good creation science really involves. They want to show its rigor, and highlight its credibility – what they are doing here is following well establish scientific protocols to produce findings that can't be dismissed and need to be contended with.
While there's loads of information for anyone already interested in the subject, this is not a film I’d show anyone, kids or adults, to try and get them interested. For that I'd point to the original Is Genesis History?
Find out more about Mountains after the Flood at IsGenesisHistory.com, including how to rent and stream it, or buy the DVD.
Finally, you can watch the trailer below.
