I live in a wondrous place. The problem I have is that, being surrounded by beauty has made me a little thick-skinned; I guess you could say that I take it all for granted. So, I am putting my thoughts down in words accompanied by images, not so much to convince anyone else, but to remind myself.
Fenton Lake is a small (less than 40 acres) manmade lake which was formed by construction of an earthen dam on the Rio Cebolla. The Cebolla itself is not really a river by most standards; it is, at most, three feet wide along most of its length. But, here in New Mexico, it qualifies. I made this image on a dark day. I was standing amongst the cattails at the north end of the lake. The ridge line to the southeast burned during the Lake Fire in 2002.
One of the most recognizable and well known features in the Jemez Valley is Battleship Rock. It is composed of rhyolite and was formed when the volcano that shaped the present-day Jemez Mountains erupted for the final (hopefully) time, the ash and lava flowed into a box canyon; when it cooled the rock filled the canyon and as the softer earth eroded away, the monolith was left exposed.
Jemez Springs is a small village (population: 250) that lies in the heart of San Antonio Canyon–the canyon formed by the Jemez River. Not much has changed, visually anyway, since I first came here in 1977. This is a typical mid-week, January evening.
New Mexico Highway 4 runs through San Antonio Canyon for about thirty miles before climbing onto the flanks of the Valle Grande and continuing across the mountain to Los Alamos (yes that Los Alamos: home of the atomic bomb). This stretch of the highway is about five miles south of Jemez Springs.
In the early years of the last century, there was an extensive logging operation in the Jemez Mountains. The logging company used a train to haul the logs to a mill in Gilman. They bored two tunnels through the solid granite that transects the Guadalupe Box and when the logging declined, the tracks were replaced by a road–New Mexico SR 485–which provides access to the Santa Fe National Forest. Some may recognize the tunnels from the role they played in the film “3:10 To Yuma”
The Jemez River cuts through Soda Dam, a large, seven thousand year old calcium carbonate formation left behind by a small, unassuming hot-spring next to Highway 4. It is located about three hundred yards from my door and is a huge tourist attraction as well as being the swimming hole for local youngsters.
The second image provides a better view of the river flowing through the “dam”, and of the swimming hole; the kids jump from the sides into the plunge pool. When the New Mexico Highway Department blasted through the formation to improve Highway 4, the building process was interrupted, and the dam has been eroding since then.
I spend a great deal of time wandering the badlands of the San Juan Basin and beyond in search of images. I have an unquenchable thirst for desert landscapes. Some people might consider me a little off kilter, especially since I live right in the middle of a place so full of natural beauty and geologic wonders that it draws visitors from around the world.
The first image is of Soda Dam, a large calcium carbonate formation that has been deposited over the ages by a small warm spring which is right on the shoulder of New Mexico state road 4. This naturally formed dam is pierced by the Jemez River which cascades over a small drop in elevation into a plunge pool which is a popular swimming hole for both locals and visitors from Germany, Japan, Russia… I can hear their squeals as they jump into the cold water on a hot summer day. Soda Dam is about two hundred yards from my door.
If I head in the opposite direction from Soda Dam on Hwy.4, it’s only a five minute drive to Battleship Rock, another geologic attraction that is visible from the highway. It was formed during the last volcanic eruption in these parts-around one million years ago. Lava from the eruption flowed into a narrow dead end canyon and hardened. Over time the softer material which made up the canyon walls eroded away, leaving the volcanic rock exposed.
If I continue up Hwy. 4, I will eventually come to the crowning jewel of the Jemez Mountains; the Valle Grande. Actually only one of several valles which were formed when a huge volcano exploded and collapsed to form a caldera about 1.6 million years ago. The Valle Grande was, until 2000, a privately owned ranch. It is now public land, administered by a trust. This is the view from a turn out on Hwy. 4 looking north.
So, you see, I really need not travel all that far to find a photogenic landscape, but I am in love with the desert; I am in love with the stark, naked, truthful beauty of the earth laid bare. The mountains, rivers, and alpine meadows are fine, but they do not speak to me in the way that the desert badlands do.