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Mormon Mesa
Mormon Mesa is a classic mesa topped by a layer of harder stone with steeply eroded sides of weaker, softer material. The elevation in some points is well over 1000 feet from the valley floor to the mesa top.

Between Mormon Mesa and its stratigraphic neighbors are two giant chasms created by the Muddy and Virgin Rivers that created the mesa. The Muddy River is sourced from several artesian springs. While ultimately the springs which the Muddy depends on are rain fed, deep underground water sources are much more reliable than water sources that are basically rain and snow fed, as the Virgin River is.

The Virgin River is also spring fed in places along its course and in good years its flow seems to be more reliable than the Muddy River. Because in reality the Muddy River is more reliable, we see that it has carved itself a larger valley. Whether the Muddy is or always was the only source of erosion in the Muddy River valley is unknown but that explanation fits best.

Mormon Mesa is an interesting geographical feature for several reasons. It is visually stunning. Mormon Mesa dominates the Moapa Valley. It can be seen from a great distance so it is a great landmark to get your bearings from if you are hunting or hiking in the area. If you are looking for the location of archeological sites it is perfect because the Southwest Museum photos of digs in the late 1920'2 have the mesa in the background. 

When the photos were taken the objective was to show the height and vastness of Mormon Mesa. What the viewer can notice however is how close the mountains are in the top photo taken on the Virgin River side of the mesa. While the angle is almost north instead of east to give an accurate depiction, we can still see that the Virgoin River valley is relatively confined.

In the bottom photo we are looking north from a point on the mesa edge due east of the airport at Overton. Just the mesa tailing to its 1st step alone, is wider than the Virgin River valley. Each photo was taken from a point east of the airport.
 
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