Just downstream of Taos Junction Rapid, on the Rio Grande of northern New Mexico, is a group of basalt rocks that, at high water, are vigorously washed by strong currents. The sediment carried by the high water sculpts and polishes these rocks. To my eye, the sculpting of the rocks model the river’s waves, while the polish on the rocks model the river’s gleam.
These basalt rocks are derived from the lava flows that the Rio Grande has cut through, in excavating the Rio Grande Gorge. Here, the river follows a very large systems of faults which, together, form the Rio Grande Rift. In New Mexico, this rift stretches north to south from the Colorado border, in the north, to the Texas border, in the south. It is these faults that spewed out the lava that covers much of this area. This north-central part of the state is now contained in the Rio Grande del Norte National Monument, New Mexico, which makes us very proud. The Rio Grande Gorge is the centerpiece of the Monument, and it is neighbored by volcanic cones that stand above the flat lava-covered plateau, with herds of bighorn sheep, elk, pronghorn antelope and deer that graze there. The gorge also provides nesting habitat for raptors such as the golden eagle and peregrine and prairie falcons, while a winter retreat for bald eagles. One will see beaver, muskrats and even otters in the river, along with plenty of waterfowl, including wintering flocks of canada geese, goldeneyes, buffleheads, widgeons and gadwalls. And one can catch brown and rainbow trout, smallmouth bass, northern pike and carp in the river.
Here are some of the critters mentioned above, all photographed along the Rio Grande.
What else? Well, of course, there is world-class whitewater available in the summer months, which includes the Taos Box run (and Taos Junction Rapid) that carries you 16 miles through the wilderness of the Rio Grande Gorge. Come visit us summer or winter!