When you view layers of rock as exposed in highway cuts, canyons like the Grand Canyon of Arizona and river banks, and you see massive layers, sometimes twenty, thirty feet thick, seemingly as smooth and cohesive as if they had been mixed in a blender, lying conformably atop each other in orderly succession, it is logical to assume the layers on the bottom if no evidence of faulting, such as tilted, folded, or fractured strata: isoclines, synclines, etc.
I hope you will have the most magical time while visiting us and I am proud to welcome you into our The Upside Down Amsterdam family.
Would advise to visit as early as possible because they only allowed a number of people inside the museum at one time.
To give you a little taste, we reveal some of our experience highlights below.
What did you think of the Upside Down Museum? He just doesn't see what all the hubbub for Disney is all about.
Take as many pictures as you like.