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.