|Nine Mile Hill
The climbing along Nine Mile Hill exists on the Cretaceous-era Dakota Sandstone formation. Although not as solid as its famous Wingate brother, the Dakota is certainly capable of moments of brilliance. Several cliffs along Nine Mile Hill have been developed with both traditional crack climbs and bolted sport routes. However, the main draw along Nine Mile Hill is bouldering.
The boulder fields along CO-141 extend the entire nine miles from the Gunnison river to the top of the Uncompagre Plateau, at an average width of over a mile. Now that is a lot of boulders! It is true that a lot of these boulders don't contain climbable rock; for every climbable boulder there are perhaps 5 unclimbable boulders. But in an area where the boulders literally number in the thousands, that leaves about (hmmm lets see [several X 1,000 X (1/6)= uhmmm]) a lot of climbable rock. Whats more, a lot of those boulders that have routes have amazing routes.
The bouldering in this area is still largely undeveloped, and much that has been developed has gone unreported. This often gives the bouldering an adventurous feel.
The earliest known bouldering in this area was developed in the late '80s and early '90s by the climbers heading out to the main canyon. Many areas were developed throughout the '90s, and there were a few chipping incidents whose offenders shall go nameless here. Many of the classic areas were explored and developed by the reticent hardman Matt Lisenby and friends throughout the late '90s and early 2000s. Many more strong climbers have developed boulders as of late. Several of them have posted these areas to this database, and I will let them tell their own stories.
The land in the Nine Mile Hile area is all BLM, and few regulations are in place. There is no camping in the East Creek Day Use Area. Once you pass the cattle guard at the base of the real hill there is legal at large camping with the usual 14 day limit. Please help keep this area free of regulation by being respectful of this great resource.
From Grand Junction, Colorado, head south out of town on US 50, towards Montrose and Delta. After traveling about 9 miles south of Grand Junction, turn right on CO-141, toward Gateway. This intersection is located in the small town of Whitewater.
The Nine Mile Hill area begins about 1 mile past this intersection and continues along CO-141 for about, you guessed it, nine miles.
Driving directions to crags are generally measured from the intersection of CO-141 and US 50, or from the cattle guard just past East Creek Day Use Area and the beginning of Nine Mile Hill proper.
Per Nick Reecy: these are the distances I've found, I don't however know where the Petrified Wall is though.
All distances were measured heading south from the US 50/CO Hwy 141 intersection.
Superchief Boulders Area (1.3 miles, road left)
Late Bloomer Boulder Area (1.35 miles, road right)
East Creek Day Use Area (~2.0 to ~2.2 miles, road right & left)
Bondi Boulder (2.2 miles, road right)
Nine Style Boulder Area (2.4 miles, road right; 2.7 miles, road right)
Cattle Guard sign parking (3.2 miles, road right)
Texas Boulder Area (3.0 miles, road left; 3.2 miles, road right)
Crack Hole Boulder (3.4 miles, road right)
Reba Boulders (3.6 miles, road right)
Rubber Rock (3.8 miles, road right)
Rock Garden (4.3 miles, road left)
Four Blocks Crag/Boulder Area (4.9 miles, road left & right)
Bone Park (5.1 miles, road right)
The Animal Farm (5.4 miles, road right)
Triangle Boulder Area (5.4 miles, road right)
Dave Loves Donna Boulder Area (6.0 miles, road right)
Grit Wall/Area 51 (6.4 miles, road right)
The Black Wave Area (7.0 miles, road right, 7.1 miles, road right, 7.3 miles, road right)
Pool of Plenty Boulder Area (7.3 miles, road right)
Blue Moon Boulder Area (7.7 miles, road right)
Chinese Algebra Area (8.0 miles, road left; 8.1 miles, road right)
625 Total Routes
['4 Stars',28],['3 Stars',197],['2 Stars',318],['1 Star',68],['Bomb',3]
Browse More Classics in Nine Mile Hill
Mountain Project's determination of some of the classic, most popular, highest rated routes for Nine Mile Hill:
Featured Route For Nine Mile Hill
Stilt Fiction V3 6A CO
: Grand Junction area
: ... : Aegis Rock
Stilt Fiction climbs a slightly overhung arete on perfect slopers.Stand start with a left hand at the arete and a high right hand on a crescent-shaped crimp. From there, make a big right hand move (crux) to a perfectly textured sloping edge, slap the left hand further up the arete till reaching the better pinch/slopers, find a high foot edge, and continue up the arete's bumps, commit to the slab, and mantle on top the boulder....[more] Browse More Classics in CO
Local Information for Nine Mile Hill
Latest Regional Forum Messages
May 27, 2013
While I absolutely applaud the new route activity going on on the long overlooked walls lining this canyon, you guys need to start using painted hangers. It is getting pretty bad. You can bet the land managers see it too.
Aug 30, 2013
I was climbing Four Blocks Crag out in Nine Mile Canyon with a friend last night, Aug. 29th, and my friend accidentally pulled our rope with a knot in the end. It was too dark to climb it again, and so we left it. We came back the next day and SOMEONE HAD STOLEN OUR ROPE!! I would appreciate if anyone knows about this to please contact me and help us get our rope back, so we can continue to climb another day. Thank you.
|By Nick Reecy|
From: Clifton, CO
Mar 7, 2014
I've always been curious about Nine Mile's range of rock quality. From what I understand, it's Dakota sandstone. But when I consider how different the rock is, it just doesn't make sense to me. For instance, the rock quality at the Texas Boulders is nothing like the rock quality of the Chinese Boulders. Is this just a natural range of Dakota sandstone in general or is there something else to it?
Mar 9, 2014
That's the natural range of the rock. The Dakota sandstone and Burro Canyon Formation that we climb on in Nine Mile will have a lot of variability. It can be coarse sandy layers that are pretty weak and crumbly but within just a few feet have sandy, iron rich rock that is patina'd and pretty tough. The idea is that this formation was a series of braided streambeds originating from no longer existing mountains in Utah before it became a rock. This is why you can also find old petrified logs, dino bones, and more predominantly pebbles in the sandstone and conglomerate layers. Message me if you have more questions, and I'll try to make up some more BS.