El Capitan |
After making a long loop that extended approximately 15 miles to the west on US 180, we turned around at a large salt flat with a panoramic view of the west side of the reef. This salt flat was at one time the bottom of a 40 foot deep lake near the end of the Pleistocene epoch only about 12,000 years ago when the Guadalupe Mountains area received an abundance of rainfall. As the climate changed over the next few millennia, this basin and other areas like it ultimately evaporated and left deposits of salt, potash, and gypsum. However, the actual deposits were generated in a much earlier epoch several million years ago following the uplift that created the Guadalupe Mountains. The uplift of the mountains was accompanied by a downward drop of the Earth’s surface on the western side of the mountains creating a basin or “graben” from which water could not escape. Continual evaporation of the trapped water gave rise to the great wealth of salt deposits in this region.
Salt flats west of the Capitan Reef |
The potash from such basins in this part of the country has supplied the US with 90% of its fertilizer, and I wondered how much of the gypsum has ended up in the sheet rock walls of our houses. After we reflected on the history of the salt flats, we slowly made our way back around El Capitan taking pictures. We had originally planned to get a shot at sunset, but we were too tired from the day and decided to make the return trip to civilization, a 55 mile drive back to Carlsbad.
R & R
The Chili’s Restaurant near the Inn in Carlsbad seemed to be the most popular spot in town. So having had our fill of Tex-Mex from the night before, we took a table at Chili’s and had a tall, cold Sam Adams on draught, a delicious salad, and lots of laughs about our new sport of "rock crawling". Back in our room at the Inn, a warm bath soothed the weary bones, and we looked forward to our adventure tomorrow on the McKittrick Canyon trail.
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