Fossil Rocks Defy Evolution! Creation Geology fits the evidence...The Facts they do not want you to know...
The sedimentary layers do NOT support evolution and long ages. First a quick preface by Tas Walker...
by Tas Walker
Interestingly, the Grand Canyon strata extend over 400 km (250 miles) into the eastern part of Arizona.1 There, they are at least 1,600 m (one mile) lower in elevation. Supposedly, the uplift of the Grand Canyon area occurred about 70 million years ago—hundreds of millions of years after the sediments were deposited. One would expect that hundreds of millions of years would have been plenty of time for the sediment to cement into hard rock.Visitors to Grand Canyon hear the usual geological interpretation involving millions of years. We are told that the horizontal formation at the bottom, the Tapeats Sandstone, was deposited 550 million years ago, and the Kaibab Limestone that forms the rim is 250 million years old (see diagram below). It is difficult to imagine the immense time involved in this interpretation.
Yet, the evidence indicates that the sediments were soft and unconsolidated when they bent. Instead of fracturing like the basement did, the entire layer thinned as it bent. The sand grains show no evidence that the material was brittle and rock-hard, because none of the grains is elongated.1 Neither has the mineral cementing the grains been broken and recrystallized. Instead, the evidence points to the whole 1,200-m (4,000-ft) thickness of strata being still ‘plastic’ when it was uplifted. In other words, the millions of years of geologic time are imaginary. This ‘plastic’ deformation of Grand Canyon strata dramatically demonstrates the reality of the catastrophic global Flood of Noah’s day.
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Sedimentary rocks? Folds like putty are common in both small formations and mountain ranges! The rocks have all the appearance of having been left behind by a huge flood and then being formed and twisted by water pouring off of the continents, uplifts of still-pliable mudrock and glacial dike breaks.