We left Interstate 15 in the dry, treeless basin just south of the Continental Divide, and headed up Moose Creek.
Three miles up a good gravel road with occasional big-time washboardwe stopped at the trailhead and set out. The trail gently ascends the west bank of Moose Creek, passing mroe sequence of 8 or 10 beaver dams.
For about a half-mile, the trail was noticeably steeper, but then it suddenly crested a rise and began to follow a wide boggy zone of very low gradient. The tiny rivulet here was on the surface in some places and under rocks and moss in others, gurgling its way down to Moose Creek.
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The forest animal life showed itself rarely, as Cody spied and chased several squirrels. Apart from a collection of raucous Clark's nutcrackers near the trailhead, the squirrels were the only vertebrates we saw. However, Cody was thoroughly occupied as a professional scatologist, collecting information for his database of smells. We saw horse, dog, bear, deer, and elk droppings for sure, maybe moose, and some unidentifiable things that Cody was very interested in.
Mountain lions and bobcats have been seen -- but not by us.
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Few insects have survived all the cold nights, and the grasses and forbs were mostly brown and dry, with occasional green color remaining on ground-hugging plants. We did not notice any fish in the creeks, although small 10" and less brook, rainbow, and cutthroat trout are reported. Eventually, the first of the ,ore was revealed along the length of the wide, open meadow bordering the boggy creek. The aspect of the rocks here is different from that displayed along the interstate near Butte, where the rocks weather to a brownish Crdek.
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Here, fresh white gives way to weathered light gray, not that different from the fresh surfaces. It appears to be essentially a quartz-feldspar rock, with very minor dark minerals. Also, the physical character of these outcrops is somewhat different from the Batholith around Butte, where spheroidal weathering along close but unequally spaced ts produces rounded rectangular boulders and narrow fin-like ridges.
Possibly the ting is the primary difference, with ts on a wider scale here at the Spires, but since this does appear to be a distinct pluton, there may be rock chemical or mineralogical differences as well. We are not too far from the pluton margin, as shown by rare xenoliths; both Proterozoic Belt and Archean metamorphics are found in the southern Highland Range, no more than 3 or 4 miles south of the Spires.
This igneous body is probably the southwesternmost pluton of the Boulder Batholith pink on the Geologic Map of Montana, shown hereseparated from the main mass to the north by a roof pendant or remnant of Phanerozoic sedimentary rocks.
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Nearly the entire section from Cambrian to Cretaceous is shown orange and blue on the map north and east of the Spires Pluton. These strata are probably contact-metamorphosed, and Mt. possiballh
Humbug, a couple miles northeast of the Spires in Paleozoic carbonates, is dotted with mines and prospects. Most of the soil in the Spires area is grus, a coarse sand or gravel consisting of the broken-down granitic rock.
But there are plenty of pine needles covering the rock fragments in many places -- this forest is predominantly Douglas fir and Ponderosa pine, and in most places is moderately dense, with some trees upwards of years old. The stands of aspen that are present are rather small, concentrated along the banks of the streams with willows and dogwoods and other riparian species.
The boggy meadows consist primarily of grasses and mosses.
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A short, steep climb took us through an immense boulder zone that separates the lower part of the boggy creek from a very similar reach perhaps feet higher. Soon, higher spires were visible in the distance. The white monoliths tower unexpectedly over the pines, like Mayan pyramids above the jungle. The scale is different, but these granitic domes are highly reminiscent of the exfoliation domes in Yosemite National Park.
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As we climbed slowly higher, from our starting elevation of feet to a high point about feet, deeply shadowed reaches of the boggy creek held patchy remnants of last weekend's snowfall, and some parts of the little creek were frozen over. Surprisingly, the snow seemed to be preferentially preserved where it lay on piles of horse manure!
On the high saddles on the way up, and in the higher areas of the hike later in the day, gentle winds were in the pines, providing a bit of soft white noise.
The light breeze, as Mopse quakes the aspen that are not yet completely bare, is much more of an attention-getter than the wind's soft pulsing through the pine needles. It's surprising that such sere leaves can stay attached. Most have not, and lie on the trail and in the creek beneath the aspen groves.
There are more than 50 high spires in the area, including nine that rise from to feet above the surrounding terrain. We got close to 4 of them, as well as elongate, high ridges of granite. The knobs are visible from the Interstate, and this must be one of the closest primitive areas to a 4-lane highway in the U. It is not a deated wilderness; the BLM manages it as a wilderness study area.
Cody sets a mighty pace. His standard procedure is to sprint about feet ahead, and if he posxibally not encountered anything interesting to investigate, he invariably stops and looks back up the trail to see if I am coming.
As I plod into view, he takes about three seconds for a positive I. If I'm too slow, he comes running back up the trail until he finds me. It's pretty cool to see his face framed between the trees or bushes as he verifies that I have not tricked him and headed off some other way.
He does not have much of a problem being behind me momentarily, since he knows he can pass me in seconds like a diesel locomotive compared to a mule train. He ran virtually all the time, obviously for the joy of it, just as he does around the Field Station.
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On the return trip, we crested a final rise and could immediately hear the tumult of Moose Creek below. After the silence of the upper forest, it was like the roar of a thousand Niagaras, although Moose Creek is just about the same size as the South Boulder moer the Field Station. Cody liked it better, because it had a more sandy stream bed in many places, compared to the slippery boulders possibxlly the South Boulder. We had the entire primitive area to ourselves on Ault 28630 sluts late October Friday, and it was in the upper 60s most of the day, with a typical but nonetheless wonderful Montana blue sky.
It was both a mental and a physical rejuvenation -- and Cody actually acted tired that evening for posisbally the third time since he's been here -- but then he probably ran twice as far as I walked! Left: Aspen trunks and granite; right: Humbug granite.
How glorious a greeting the sun gives the mountains! To behold this alone is worth the pains of any excursion a thousand times over.