This summer I decided to stay in the US - because while I'm disappointed, concerned, and upset about the direction the country is going, I needed to remind myself that there are still good things to be found in some slightly disturbing places. I started my trip in El Paso, Texas, where I picked up my rental car and immediately drove out into New Mexico.
WHITE SANDS NATIONAL PARK
It was around 2:30 pm and ~94° when I got to White Sands National Park, located in the Tularosa Basin in the northern Chihuahuan Desert . White Sands encompasses the largest gypsum sand dunes in the world - about 225 square miles. Most sand dunes are comprised of silica, but the unique geography of this area made it the ideal place to develop gypsum dunes.About 250 million years ago, this area was covered by the Permian Sea, which deposited water-soluble gypsum into the ground. 70-30 millions years ago, tectonic activity pushed up this ground to form the San Andres Mountains to the west and the Sacramento Mountains to the east. During the wet weather of the Ice Age, gypsum was carried down into the Tularosa Basin and trapped there, forming Lake Otero - a huge lake that covered most of the basin. When the water evaporated, it left gypsum crystals (in the form of selenite) on the ground. The movement of wind and water breaks down those crystals into small grains of gypsum sand. The formation of the sand dunes really only began around 10,000 years ago.
Gypsum sand dunes are interestingly different than other sand dunes. They don't hold heat like regular sand, so it's cooler to the touch (but the glare is absolutely blinding and you basically have to shoot photos with your eyes closed and hope for the best). The sand behaves differently as well, since it dissolves in water and hardens, increasing wind resistance. This also means plants can grow faster and not get buried by the dunes.One of the most interesting things to observe is the rather quick adaptation made by the animals living in the dunes. Because lighter colored animals can blend into the sand and escape predation, animals such as the bleached earless lizard, the Apache pocket mouse, and several crickets and spiders have basically turned white.
Cool to see an oryx, but not cool that they are there... |
Hiking around White Sands during the day was hot and blinding so I didn't go too far, but after checking into my hotel and grabbing some dinner, I returned to the park for the sunset stroll later that evening. With the sun going down, it was much cooler and easier to see without the bright glare. We could also see flashes of lightning from the approaching thunderstorm, which made for a lovely and dramatic sky.
GUADALUPE MOUNTAINS NATIONAL PARK
The next day, I drove to Guadalupe Mountains National Park, home of the highest point in Texas - Guadalupe Peak (8,751 ft). This park is isolated and unassuming - while it isn't as visually stunning as many of the other parks I've been to, there's some pretty interesting geology and history behind it: namely, the mountain range used to be an underwater tropical reef!Shell fossils along the Devil's Hall trail |
Pinery Station, with a view of the Guadalupe Mountains |
Sadly, when I visited in late June, a huge portion of the park was closed due to 'high and extreme fire danger.' Which was kind of weird, since it rained every night (although there was a lot of lightning, so...). But it meant I had limited hikes and not a lot of places to see or things to do.
Aside from the short Pinery trail, there were only two other open trails - Devil's Hall and Guadalupe Peak. I spent some time in the Visitor's Center finishing my junior ranger book and waiting for the drizzle to stop, so by the time I got out to the hike it was too late for the longer Peak trail.Instead I followed a boulder-strewn wash to Devil's Hall, where steep canyon walls showcase interesting layers of rock. It's a poorly marked trail so I got lost a few times, which is a little nerve-wracking when you're hiking alone! But at the end, you enter a cool geologic formation. You enter through a steep ledge called the Hiker's Staircase and into the steep-sided canyon that is the Devil's Hall.
A bonus of it being fairly deserted is that there is more wildlife, and I spotted this little guy sunning himself... can you find him??:
I spy with my little eye.... (he's staring right at the camera!) |
Later in the hike, this fearless little glossy snake came right over to me before slithering off into the brush:
CARLSBAD CAVERNS NATIONAL PARK
Although it started raining again, I headed up to Carlsbad Caverns that evening because I wanted to see the bat flight program. There are actually 17 species of bats that live in the park, but the most famous is the Brazilian free-tailed bat. (In fact, in the early days of the cave's history, settlers would mine the cave for bat guano to be used as fertilizer for the California citrus groves.) Carlsbad Caverns are below the same mountains that form Guadalupe Mountains National Park, and on most summer evenings, up to 300,000 Brazilian free-tailed bats fly out at twilight to feed. (The number was as high as 793,000 in 2005!)When I arrived the ranger told us all to keep our expectations low - the weather, combined with a low population of bats (due in part to the long drought the region was experiencing) meant that they weren't seeing much activity. But he did spend about a half hour answering questions and dispelling myths about bats, until at about 8:15pm the first bats began exiting the cave. It wasn't a huge swirling mass that you sometime see in photos, but a slow and steady trickle where groups of a few hundred would come out together.
It was interesting that every bat always turns left coming out of the cave, then circles around before flying off (usually to the south) to feed on moths and other insects.
Those flying specks aren't bats - during the day they are cave swallows |
Because of the fire danger that also closed most of Guadalupe Mountains NP, almost all of the outdoor activities around Carlsbad Caverns were closed. But the good stuff is all underground, so I headed straight for the main caverns for my morning self-guided tour.
Carlsbad Caverns National Park is actually comprised of 120 different caves, formed about 5 million years ago. Oxygen rich rainwater seeped down to mix with H2S-rich groundwater that moved from deep underground. When the two waters met, they combined to form the sulfuric acid (H2SO4) that ate away at the limestone. The Carlsbad Cavern is about 30 miles long, and the Big Room in Carlsbad Cavern spans 8.2 acres. The newly discovered Lechuguilla Cave, which is only open to scientists and other researchers, is over 140 miles long!
Goin' down, down, down the Natural Entrance |
This ladder was installed in 1924 by a National Geographic team |
Year round, the temperature of the caverns stays at a fairly steady 56°, and there is a constant flow of air that circulates through the cave system. And the Big Room is truly massive - it took over an hour to wander through. It was easy to see why Will Rogers described it as "Grand Canyon with a roof on it."
Bonus: driving past Marfa Prada on my long and lonely roadtrip through |
At the base of the Davis Mountains is Fort Davis, an Indian War frontier military post that protected transportation routes across the Chihuahua Trail from El Paso to San Antonio. It was in operation from 1854 -1891, and was particularly interesting because several all-black regiments were stationed there. These groups became known as the "Buffalo Soldiers."
View of Officer's Row from the Scenic Overlook on the North Ridge |