Cataclysm in Cajon Pass Geology
This is a slickenside in a crushed granite rock from the San Bernardino Mountains lower Cajon Pass I photographed today. There are several cracks in rocks in these granite rocks showing the sudden uplift of this mountain range by the San Andreas (mainly), creating Punchbowl, and Cajon Faults offshoots. Rocks and boulders in the ancient river bed of Cajon Pass are rounded by flowing water showing huge amounts of water flowed out of Cajon Pass and Lytle Creek from the Mojave Desert into San Bernardino in the Pleistocene from the present dry lake. There are also Quaternary river terraces in the lower pass. One crack in this rock can be seen in the picture. These are common in suddenly uplifted rocks in this area. Evolutionists claim mountains rise during orogeny periods over millions of years. This is based on evolutionary assumptions. The evidence indicates mountains rise suddenly during worldwide earth quakes. The picture I took shows that a ...