Monday, November 19 dawned cool and cloudless in Carlsbad, New Mexico, and we were heading home. This was the twelfth and final day of my wonderful fortieth birthday trip to two National Parks. Although we were saying goodbye, we intended to make a quick stop at Guadalupe Mountains National Park as we departed.Continue reading
On Friday, November 16, after a full day of exploring the underground palaces of Carlsbad Caverns National Park, we decided to visit a very special aboveground part of the Park in our final hour of daylight: Rattlesnake Springs, the site of a lush oasis in the Chihuahuan Desert beneath the Guadalupe range. Rattlesnake Springs is a small, twenty-four acre unit of Carlsbad Caverns National Park purchased by the National Park Service in 1934 as a means to ensure a reliable water source for the development of the National Park. Because of its water and array of trees and shrubs, Rattlesnake Springs hosts 350 bird species, forty species of reptiles and amphibians, and thirty species of mammals. John had been monitoring the site’s bird lists on eBird and was keen to visit, so we decided to check it out on our way back to Carlsbad.Continue reading
On the afternoon of Thursday, November 15, we concluded our adventures at Guadalupe Mountains National Park with a private visit to the gypsum sand dunes beneath the magnificent western escarpment of the Guadalupes. Beginning around twenty-six million years ago, the area west of the range began dropping and the mountains began rising along a steep vertical fault. Slowly the fossilized Permian coral reef emerged as softer rock layers eroded away. Meanwhile, the dunes out in Chihuahuan Desert lowlands west of the range and were formed by an ancient lake. Much like in Death Valley and huge portions of the Great Basin Desert, all of the streams on the western side of the southern portion of the Guadalupes did not reach the sea but instead flowed to a lake in the depression beneath the escarpment. When the climate became warmer and drier, the lake evaporated, leaving a huge salt flat basin. The gypsum dunes were formed by the wind collecting the sand from the vanished lake.Continue reading
Thursday, November 15 was our day of transition from Guadalupe Mountains National Park to Carlsbad Caverns National Park. With the backpacking trip as part one, car camping with Phil, Adam, and Sylvan as part two, we were now going to embark on part three and be joined by John, Catherine, and Mariana down from Chicago. But we wouldn’t be checking into our AirB&B in Carlsbad, New Mexico until the evening, so we still had much of the day to see a few more wonders in the Guadalupe Mountains.Continue reading
Devil’s Hall is a short, narrow chasm a few miles up Pine Canyon from its wide mouth. It is accessible via a two-miles-and-change hike from the Pine Springs Trailhead. After the crazy events of the previous night and morning, our afternoon’s adventure on Wednesday, November 14 was a hike up to Guadalupe Mountains National Park’s only accessible slot canyon of note.Continue reading
Before dawn on Wednesday, November 14, Sean nudged me awake. We were curled up in a nest of pillows and comforters left behind by Adam, Phil, and Sylvan who, not keen on another night of freezing temperatures, had decamped to a nearby hotel. “Nearby” is relative here. Adam had texted Sean the night before that there were no available rooms in Carlsbad, New Mexico an hour away so they’d continued on and found “the last available room” in Artesia, New Mexico an hour and a half away.
Lying there in the blankets, Sean nudged me and handed me his phone. It took me a moment to understand what I was seeing in the texts from Adam. Around midnight, a truck had driven through the wall of their hotel room.Continue reading
After lunch on Tuesday, November 13, Phil climbed into the tent with Sylvan for the little guy’s nap. Meanwhile Sean, Adam, and I decided to get in a second short hike for the day, this time one a bit more ambitious than our walk through the foothills with the baby that morning.
We chose to check out at least part of the Permian Reef Geology Trail near the entrance to McKittrick Canyon. The entire trail is a 4.2-mile out-and-back 2,000 feet up onto Wilderness Ridge near the Texas-New Mexico state line. We wouldn’t be able to do the entire trail, but we figured it would be worth it to see some of it. We were particularly keen to see fossils.Continue reading