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If you roll along dusty, unpaved county road A011 through the desert shrubbery of New Mexico’s south-central region, and you roll with purpose, you will fetch up on the shores of Kilbourne Crater. Kilbourne was formed by a maars-type volcanic eruption. In a maars eruption a crater is created by hot magma coming into contact with the water table. When the two meet, the rapidly heated water turns to steam, expands and blows huge chunks of ground skyward. By huge I mean 2.5 kilometers across 1.8 kilometers wide and 125 meters deep. It’s a big hole and it must have made quite a racket when it blew its stack 20,000 to 80,000 years ago.

Maars volcanic eruptions don’t form the classic Hanna-Barbera, cinder cone shape or leave behind crowd-pleasing lava flows. At first I thought a meteor caused the crater but the crew at Southwest Expeditions had several guest speakers situated under a billowing tent to set me straight. They also had a van if you didn’t want to burn your own fuel to get to the crater. I saved $2.57. In addition to downloading a heck of a lot of information about volcanism into the assembled masses they served us a fine chicken-taco lunch.

Lunch was fabulous except for one thing. That thing being a giant jar of sliced jalapenos. No one was eating them because the lid was too tight. I gave it a good twist but the lid would not budge. I’m not the strongest guy in the world but I can open a damn jalapeno jar, you know? I finally gave up and handed it to this big guy that looked like Chief from the movie One Flew Over The Cuckoo’s Nest. I swear, he took the lid in his fingertips and the lid spun off easy as pie.

It put a damper on my lunch I tell you. I ate moody qua-moody. Am I getting old? Will I need a Clap-On soon? Life Alert? After the jar debacle it was probably best that Southwest Expeditions canceled our hike down into the crater. The temperature was 92 degrees and the wind was howling. No sense crushing anyone else’s sense of self-worth.

After lunch we assembled to participate in an art project with Tim Fitzpatrick and Jeff Erwin. Fitzpatrick had a long swatch of bright red cloth that he wanted to juxtaposition against Kilbourne’s vast, earth-colored sweep. It was something to do with the wavelength of light and spectra. I’m not sure because Fitzpatrick lost me after he said, “Hold this red cloth.” While we marched around Erwin flew a drone to capture footage of the cloth snaking across the rim of the crater.

After piercing Kilbourne’s visual solitude with our happy, marching red-band the artists had each of us recite one line of John F. Kennedy’s, “We choose to go to the Moon” speech and took headshots of the readers. I’ll let you know when the thing pops up on you tube.

Surrounding Kilbourne are ash dunes and surprisingly little lava. What lava pieces you do find at the site are more block-shaped and are pieces the explosion ejected from an older layer of lava that had covered the area long before Kilbourne was born from pressurized steam. There’s also a lot of ammunition shell casing scattered around. I imagine the lead-to-lava ratio will approach 50:50 by the year 2234.

The reason for all of this activity in the middle of nowhere was the 50th anniversary of astronauts Conrad, Bean, Gibson, Carr, Irwin and Schmitt training in Kilbourne Crater for their upcoming Apollo 12 Moon mission. That would be the second Moon landing. Kilbourne was chosen for its dust, the rough terrain and the multitude of geologic examples found at the site.

Other Apollo missions trained at Kilbourne: Apollo 13, 14, 15 (canceled), 16 (renamed 15) and 17 crews all did their time in the hole. NASA’s budget and our will to explore the Moon waned and the Apollo missions kind of ran out of steam. Which, in a suitable ending is what created their moon-mission training ground those many years ago. Maybe one day NASA will return to Kilbourne and use its dusty, rocky landscape to train another generation of astronauts. I hope to see America once again become a space-faring nation and that those astronauts will be heading to Mars.

Joe Gresh

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