From Boulder, Dinosaur Mountain looks like a Stegosaur. The plates on the back of the beast--which paleontologists call osteoderms--are made up by the rocks in the third of the four main strata that crop out to form the mountain. From south (tail) to north (skull) one finds Stonehenge, Fee, Fi, Fo, Fum, Dum, and Dreadnaught. Though the summit of Dinosaur Mountain belongs to the fourth and westernmost stratum, from many angles it is the rocks of the third that one sees silhouetted against the sky--their smooth east faces beckoning to the climber.
Quadratic Equation contours the east face of Fo, rising from the left edge of the face to the summit, which is close to the cleft separating Fo from Fum. It is a seldom-repeated route, presumably because of the relatively long approach. The rock is consequently a bit dirty, especially in the first pitch, but the position is excellent and crowding is not an issue. The first ascent was by Gerry Roach in 1987.
From the NCAR parking lot, follow the Walter Orr Roberts trail to the intersection with the Mesa Trail, continue past the intersection on the popular Mallory Cave Trail.
The Finger Flatiron
The trail heads mostly south until the base of the east face of Dinosaur Rock and then rises with a series of switchbacks between Dinosaur Rock to the south and Der Zerkle to the north. Shortly after Der Zerkle, the trail forks. A sign instructs you that the left branch goes to Mallory Cave, while the right branch continues towards the summit of Dinosaur Mountain. Take the right branch and follow the steep trail until you reach a T junction. The right branch goes by The Box and then seems to dead-end. (A short Class 3 step takes one to the upper stretch of the trail.) The left branch from the T junction goes down the gully between the third and second strata. Descend this gully briefly until you reach the left (south) edge of Fo's east face. Opposite to this face is the striking west face of the Finger Flatiron. The best way to assure that you are climbing the right rock is to check its shape. Fo has a characteristic shoulder, which is separated from the summit tower by a deep cleft.
With a 70 m rope, Quadratic Equation can be climbed in two pitches. The first pitch, slightly more difficult, takes one from the base of the rock to the ridge atop the shoulder.
On the ridge
This first pitch is about 60 m, and it may be possible to cover it with a 60 m rope as well.
Otherwise, one has to belay a little lower. From the shoulder to the summit it is less than 50 m. Follow the narrow ridge atop the shoulder (exposed, but easy) to the cleft that delimits the summit tower. Downclimb into the gash until you can cross to the north. From there, follow a shallow crack to the summit. The crossing of the gash is quite exciting, but not hard, as the distance between the two faces is just right for classic chimney technique.
From the summit of Fo, Rossiter recommends to downclimb to the west until a ramp is met that heads north. The ramp takes one down to the saddle between Fo and Fum. This descent plan is certainly feasible; on the other hand, it is rather exciting and involves a few low-class 5 moves. Alternatively, sling a block immediately west of the summit and rappel down to the saddle. Each of us tried one option, and we agreed that rappel should be the more straightforward one.
From the saddle between Fo and Fum, a gully descends to the east to the corridor between the third and second strata. The initial stretch of this gully looks invitingly easy, but apparently it cliffs out further down. Descending to the west takes one to the gap between the third and fourth strata. This involves a little scrambling. Turn right (north) and follow the base of the west face of Fum to the gap between Fum and Dum. Cross to the east and follow the trail that steeply descends from the summit of Dinosaur Mountain. A short scrambling section takes you to The Box, where you close the loop.
A typical Flatiron rack, with a set of nuts and small to medium cams. The largest piece we placed was a #3 C4. Places for protection are not abundant on this route.
This route is described in Gerry Roach's Flatiron Classics
, where it is ranked among the "classic" routes. It is also described in Richard Rossiter's Rock Climbing the Flatirons
. On the web, a good page
is available at Mountain Project.