One of my favorite hiking trails near Santa Fe is the Chamisa Trail. Its trailhead is just within the border of the Santa Fe National Forest, off of Hyde Park Road, or NM 475, only a few miles from downtown. Because of its relatively low elevation, between 7800′ to 8500′, and the placement of the first mile of the trail along the west-facing slopes of a small open canyon, the trail makes a good walk nearly all year. The path reaches a saddle after about a mile, and then descends into a shadier drainage for another mile or so, where it intersects with the Winsor Trail along Tesuque Creek.
This is my go-to trail when I need a quick head-clearing walk. It is close by and well maintained. The light is always good. It is particularly luminous in the winter, a time when higher elevation trails require snowshoes. It is practically the poster child for a walk in a mixed conifer forest in the Southern Rockies. If I were designing a diorama for such an ecosystem for a museum, I would copy a few hundred square feet of the forest around the Chamisa Trail.
Ponderosa and White fir along the Chamisa Trail
But for a long time the rocks along this walk puzzled me. The outcrops along the path are not particularly notable; the one in the photograph below is about as good as they get:
A typical outcropping along the Chamisa Trail
Slopes are steep, but rounded, and are covered with a thin soil littered with fragments of rock:
Stony slopes in the forest
There is a distinctive mix of colors among the fragments, reflecting the underlying variability of the bedrock:
Rock fragments and pine needles
At a first glance these rocks don’t seem to fit into any straightforward category. They’re clearly metamorphic, with a steeply dipping foliation in outcrop, crystalline, but fine-grained and somewhat blocky close up. Under the hand lens they seem to be made up of either small crystals of quartz and pink feldspar, or small crystals of hornblende and white feldspar. There is very little mica overall. The rocks are moderately platy, but so fractured with finely spaced joints that they weather quickly into angular gravel-sized fragments. (This is not a pleasant trail on which to go barefoot)
Here are some examples:
Metamorphic rocks are classified in the field by their texture. These rocks are certainly not in the coarse-grained gneiss family, nor are they in the directionless-textured fels family. I decided to put them in the schist family by default, in spite of their high feldspar content and low mica content. Schists are typically rich in strongly-aligned micas, causing them to split freely into plates, and giving them a distinctive sheen. Perhaps the protoliths of these rocks – which I suspect are volcaniclastic – were unfavorable for mica to recrystallize. Some of the darker schists break into large angular blocks and are usually called amphibolite in local descriptions of the rocks.
In places along the Chamisa Trail, these metamorphic rocks are intruded by dikes of a distinctive unfoliated pink granite, rich in silvery muscovite mica:
A dike of orange-pink granite intruding the schist
These colorful granites add extra variety to the walk.
There is an entire belt of these schistose rocks in the mountains near Santa Fe, wedged between a mass of monotonous orange gneiss to the south and southwest, and the strongly foliated pink granite, grey tonalite, and high-grade gneiss that make up the core of the Santa Fe Range to the north and east. If you follow the Winsor Trail north from its intersection with the Chamisa Trail at Tesuque Creek, you can walk through the transition from schist to foliated granite within less than a mile.
In this Google Earth view, the Chamisa Trail follows the two end-to-end drainages in the center of the photograph. As far as I can tell, this is just about the center of the schist belt. The higher ridges just to the left of the sharp north turn in the road are made up of foliated granite, underlying Hyde Memorial State Park.
The Chamisa Trail looking north. Click on photo to enlarge.
Geologic maps of this area show large, but currently inactive, faults cutting through some of the north-south drainages that interrupt the western slopes and streams, including the one the Chamisa Trail follows. These faults were reactivated during past mountain-building activity in the American West, and their movement shattered the brittle schist, gneiss, and granite as they shifted. Shattered rock is more vulnerable to weathering and erosion than neighboring intact rock and as the highlands eroded, the old fault zones helped guide the network of evolving drainages. If you walk down the branch of the trail that follows the dry stream bed back to the Hyde Park Road trailhead, you can see examples of fault breccias:
Fault breccia in amphibolite
Slickensides – the ‘scratched’ pattern
in the outcrops. Perhaps these strains account for the closely-jointed character of the schist all along the Chamisa Trail.