Sunday, March 4, 2012

Welcome to Big Thunder: the Biggest Little Boom Town in the West

(Thunder Mountain’s inspired by Bryce Canyon National Park, Utah (left), Walt Disney Imagineering's Senior Vice President of Creative Development, Tony Baxter (right), designed the ride in the 1970s)

(The hoodoos reddish color is from a mixture of limonite, iron and magnesium oxide)
Located in Frontierland, Big Thunder Mountain Railroad was formed from layers of iron-rich sandstone, shale, and conglomerates deposited in layers.  At one point this area was a plateau until streams weathered over the rock creating fins.  Water seeped into the fins and froze during the night causing the ice to expand and fracture the rocks.  The structure erodes away creating the tower like formations call hoodoos.
Within the mountain sits a section called Dinosaur Gap which holds the skeletal remains of a T-Rex.  Millions of years ago after this particular dinosaur died it was quickly buried by sediment encasing the remains.  When particles were washed away from weathering with the desiccation of the rock half the skeleton became visible.
 (Geothermal heated water rising to the surface by convection through porous and fractured rocks)
Geysers sit just beyond Dinosaur Gap ejecting water up into the air. Generally on fault lines geysers have to build up pressure before an eruption happens.  Heat is needed for the geyser came from magma near the earth’s surface.  Pressure and heat brings the water to the boiling point where it travels through an underground “plumbing system” made up of deep pressurized fissures in the crust.
(Miners created the cave sitting near the fall with dynamite then placed a railroad inside)
This small tiered waterfall was formed from the streams that carved out the surfaces of Thunder Mountain.  The water dropped over multiple vertical tiers shaped from the movement of small sediment particles downstream.  This water holds organic acid forming moss that is eating away at the rocks it splashed onto.
The waterfall enters into a huge lake behind the hoodoos.  This lake was formed from the streams flowing through the area over a long period of time forming a deep curve.  Once the river overflows whatever can’t be held in the curve continues flowing over leaving the water the rest inside the deeper area.  



 “This here’s the wildest ride in the wilderness!”
Photo Courtesies (in order):