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During this time the Uncompaghre Highlands were being elevated which bordered the north and eastern sides of the basin (Stevens and McCarrick 8). As the basin carved in it was filled with marine water from a sea that use to exist in this area. This basin soon became cut off from the sea and began to evaporate from the hot, dry climate of the area. Evaporation of this sea left gypsum, sodium, potassium and magnesium bearing sediments (Sprinkel, Chidsey and Anderson 14). The basin would occasionally fill with salt water and then become cut off again which caused another cycle of evaporation with salt left behind...
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