A Place Where Darkness Is A Good Thing
By: Melissa Aragon
While I was at home over break, I ventured down from Albuquerque to Carlsbad, New Mexico to see Carlsbad Caverns National Park. This was something I had done a few times before, once with my parents when we also visited White Sands National Park and the Atomic Museum in Alamogordo. This time I went to southern New Mexico with one purpose, and one purpose only, to see caves and bats.
The Drive from Albuquerque to Carlsbad is about a three and a half to four hour drive, depending on traffic (it was about five hours on the way back because of traffic in Albuquerque). The drive from Carlsbad to the park is another hour and a half. The actual time I spent in the cave was about four hours, from 9:00am-1:00pm.
The Park itself is situated on a very tall hill, or a very small mountain depending on how one looks at it. Upon entering the actual park, it’s about a half an hour drive from the base to the top, where the welcome center and all attractions are located. Right before the park entrance, I saw laid out alongside the road a few buildings, basically an overpriced gas station and a plaza with a gift shop. I drove through the gates welcoming me to Carlsbad Caverns National Park. I thought to myself how excited I was that we were finally there, but little did I know about the long drive up to the top. We winded up this mountain, yes, I would call it a mountain, until we reached our destination.
I went with the intention of seeing the bat flight the evening before I went into the cave, but it was rained out, and I did not get to make it to the amphitheater. Those raindrops were huge- and not by New Mexico standards, either. The drive up the mountain into the greeting center and the path towards the amphitheater to see the bat flight had the densest fog I had ever driven in. Come to think of it, it was the only fog I had driven in. With visibility at what seemed of only five feet ahead, I left the greeting center, which never officially canceled the viewing- I mean, they could never tell the bats “NO,” but as I talked to people in my tour group the next day, the rain only got worse and it made for a less than enjoyable bat flight- with the park ranger less than enthused about speaking to a small group of huddled umbrellas.
I started out early the next morning, and with a long drive ahead of me, and a less than optimistic view of what the Carlsbad Caverns were, overrated and not worth the drive. Day two was definitely a much more productive day. I arrived at the Caverns around 9:00am and was in the depths of the cavern by half after. I had the option of taking the ‘original route,’ in which one enters the way the first group of explorers did, through a steep and narrow path about a mile and a half long. I chose instead to take the path more traveled- the approximately two minute elevator ride. We descended over 700 feet, and were still far above sea level, even at the lowest part of the cave.
I first took a self-guided tour around the Big Room, where there were placards spaced out, describing possible theories as to cave formation, information of preservation, chemical makeup and descriptions of stalagmites and stalactites. The one and a half mile path of the Big Room took about an hour, and after wandering through the cave in as near authentic silence that I could get in a National Park, it was time for the guided tour I bought earlier that morning to start.
I left the Big room and met my tour guide, along with about 30 other people of my tour. While the tour guide was waiting for everyone to show up, he asked us all where we were from, and in our tour alone we had people who had traveled from as far as Taiwan and Germany. I would never had thought of New Mexico, let alone the small town of Carlsbad, which takes about fifteen minutes to drive through, and is surrounded by desert, would be a place worth traveling 7000 miles or more for, but this was one of those times when I was proven wrong.
Before taking us through the guided section of the cave, our park ranger gave us two explanations as to how this cavern was formed millions of years ago. One explanation was that sulfuric acid, which came from below slowly rose to where we were, dissolving large pieces of rock, and leaving the large cavern we see today. Our tour guide described how he had tried an experiment in which he dropped either sulfuric acid, or hydrochloric acid (I can’t recall now) on a rock, and that within a week, signs of erosion and breakdown of the rock had occurred. He even had the rock with us, and showed us a dent in the rock, and he explained that that’s where he had been putting his chemical. Though the validity of his individual “experiment” may be doubted, the theory behind it seemed to be a credible one. Another theory was that the cavern was formed by dripping water. Slightly acidic water that trickles down onto rocks such as limestone has the power to erode it over time, and many geologists believe this, along with the prevalence of sulfuric acid is what formed the cavern we can see today.
We proceeded through the tour, and at one point we were shown a large room in which, during a time when cave preservation was not as an important issue is it is now, senate meetings were held, and even the movie Journey to the Center of the Earth was filmed, and a wedding and reception that took place, completely flattening and sanding out the part of the cave the size of about two the size of Coles gym floor. The park ranger explained that the process to restore the effects will take thousands of years to recover, if it ever recovers at all.
The park ranger talked about all the ways the National Park Service tried to help preserve the cave, and in some instances ended up degrading some of it instead. He explained how the parking lot and welcome center were situated right over the cave, and how though this road allows visitors into park, the asphalt has completely stopped the ability for water to drip down into the cave from that area. Usually, he explained, ground water will trickle down into the cave, but because a large piece of asphalt does not let the water be absorbed, water cannot flow down and continue to create formations.
The tour ended with one last speech by the park ranger, one that I distinctly remember from my last trip to Carlsbad. He discussed problems that the park was having with the preservation of the cavern. There are new parts of the Cavern that are still being discovered and explored for the first time, and they are finding that the cave may extend past the park’s boarder. Recently, certain companies, as the ranger explained, have been building closer and closer to the parks boarders. One of these companies in particular have become very interested in drilling very close to the boarder, near where this cave lies, and Cavern preservationists are concerned that drilling could either disturb the rock around the cave, or actually puncture part of a cave that has not been mapped out yet, completely disturbing and even destroying the cave’s ecosystem. He ended the tour saying something along the lines of, “during this election, make sure you vote wisely, or else you may elect someone who will let this cave be destroyed.”
I took more from this trip than any other, as I actually paid attention to what the park ranger had to say. Taking this last trip made me realize that I come from a place where even a hole in the ground is something pretty special.






















