Notes on Copper & the low level trail linking to Bass:
Camping & Water
There are established sites where the Tonto trail crosses Copper, but no water there. In winter and spring, rain and trickling flow usually fills bedrock pools in the gneiss ~0.75 mile DC from the trail crossing near the mine area (see below). The Tonto plateau promontories on both sides of the mouth of Copper also have established campsites with spectacular views in all directions. Copper is on the inside of a 180-degree bend in the river, with the massive Shinumo drainage and Supergroup formations opposite.
Mine.
The mine area is a broad bench on the E side of Copper about 0.75 mile DC from the official Tonto trail crossing. It is easy walking DC until some pouroffs in the schist. Bypass these on the W side – there is an obvious place to walk up, then pick up a trail down through the pink gneiss. The mine area may also be reached by shortcutting straight down from the Tonto trail above the mine on either the E or W side. On the E side, there is a constructed miners’ trail down through the only break in the Tapeats cliffs, cairned but not so easy to find from above. This trail descends to the N end of the mine bench. On the W side the Tapeats is broken up, so you can walk down easily in several places.
Bass’s low-level trail from Copper
Bass constructed a trail below the Tapeats linking his mine in Copper with the Bass trail, and the route proved fairly easy to follow, with some of the trail still in good shape. From the Copper mine, start by ascending the trail at the S end of the mine bench. At a shoulder, the main trail heads right (S) to continue up through the Tapeats break to the Tonto on the E side of Copper. Instead, take the left side of the shoulder to contour N high above the mine bench. After about half a mile, this contouring trail turns down into a gully for no obvious reason; perhaps there was an exploratory dig here. (This gully does provide a moderate 3rd Class route down to the bed, but pouroffs soon prevent further progress DC.) I placed cairns here to indicate that one should stay high and right to continue contouring around, climbing slightly to the foot of the Tapeats cliff before turning the corner to head E. After descending through some Tapeats ledges, you face a transverse schist wall, at the top end of which there appears to be a boulder pile to help you up; this turns out to be a natural formation. There is a good trail from here. After a straightforward crossing of the only side canyon between Copper and Bass, descend a steepish slope and turn E onto a plateau for a mile or so of easy walking. This plateau is Bass Limestone and Hakatai Shale, much easier going than the basement rocks that are more usually found below the Tapeats. After crossing the head of a deep schist ravine and making a steep descent, you can either continue the descent to reach the small beach opposite the mouth of Shinumo Creek, or traverse about 200 feet above the river to connect direct with the end of the South Bass trail.