GENERAL DESCRIPTION
R’o
Urique is the river that flows through the famous Barranca del Cobre (Copper
Canyon) proper. It can be divided
into three sections based on easy access points: an upper 76 km class IV
section from Puente Norogachi to the Puente Umir‡, a middle 88 km section of
class V with many portages through the main Barranca del Cobre from Puente
Umir‡ to the town of Urique, and a third 45 km section of class III-IV (only 45
km on R’o Urique) from the town of Urique to the confluence with the Fuerte and
then on to Tubares (the take-out).
The
first section, the ÒGates of the UriqueÓ run, is one of the finest in the
region and begins in the mesa area of Norogachi. There are dirt road access points in this area to several
villages, but the easiest to use and locate is on the main road to
Norogachi. Launching here and
continuing on down to Umir‡ will give 76 km of beautiful river. The first 21 km section down to Puente
Siquirichi is generally class I-II with some braided channels and shallow
shoals. These flatter initial sections require good rainfall to get enough
water to make floating over the wide shallow shoals easy. About 4 km past Siquirichi the bigger
rapids start and within 8 km the river enters an imposing gorge with high walls
and a gradient of >100 fpm, with many challenging rapids. When the rapids
start not as much water is needed for enjoyable floats. The river level can be ascertained at
Puente Umir‡ when driving to the put-in from Creel. This canyon section contains many class III-IV rapids and
several class V rapids that can be portaged. A little over halfway through this stretch where the gorge
opens up, the river passes between spectacular pillars reminiscent of a gateway. Just around the bend, an astounding wide
sliding falls (Cascada Urique) is encountered by some fantastic pillars on
river right. Here, looking
downstream from river level, the river seems to drop off the face of the earth.
Upon inspection, however, it is found to be two fun class III-V sliding falls
where the river drops vertically probably 20 m, followed by a third 2 m
drop. This is one of the most
amazing places in the Copper Canyon country for paddlers. Downstream of Cascada Urique, the river
enters gorge again with the usual high-elevation coniferous trees and
sandstone-type cliffs, and numerous runnable class III-IV rapids continue all
the way to the take-out at the Umir‡ Bridge. These upper sections will generally require 2-4 days to
float through, depending on where the put-in point is and how much water is
flowing down the river. On my trip
from Norogachi to Umir‡, I spent one night on the river, but would have
preferred two for a little more exploration time. If youÕre lucky enough to find it raining when approaching
the Norogachi turnoff, it would be possible to put-in even farther upstream and
add ~40 km more to the trip.
The
second section goes through the famous and notorious Barranca del Cobre, and is
only for experts willing to take on the challenges of an expedition-type trip
of 5-10 days with many class V rapids and portages (and I mean a lot of portages). The scenery on this section is
spectacular, and the rapids are extremely challenging, at both low and high
levels. It starts off with some
runnable class V drops (including a clean 6 m falls), around the ÒIncised
MeandersÓ in the first 4.5 km, but then slams into a steep gorge section (70m
in 2 km/~200 fpm) with house boulder choked drops requiring numerous and
creative portages. This section
ends around km 7 where Arroyo Umir‡ enters on the right. Although the next ~5 km section still
drops at 30m/km (~150 fpm), most of the rapids are runnable class IV-V to
Arroyo Basihaure (km 12), where several more portages are likely just upstream
and a little downstream of the arroyo.
More portages are likely when approaching a horseshoe bend around km
15.5, and then in a ÒFantasma FallsÓ section at ~km 19.5, named for water
pouring out of a tunnel in the canyon wall on RL that looks like a ghost from
upstream. Just past here one
enters the ÒBarranca del CobreÓ proper where copper mining took place. Downstream, a trail follows the river
from km 20-48, the canyon is more open, some abandoned structures are to be
found, and nearly all rapids are runnable (with the exception of a sieve at km
33). Around Arroyo San Ignacio (km 39), the river turns to the southwest and
within two km reaches a trail that ascends to Divisadero. This provides an access point, albeit
with a ~1300 m vertical climb (~4300 ft) and 10 km hike. Below here the river
is often in more open canyon areas, and everything is generally runnable class
III-IV with the possible exception of a spectacular narrows section around km
63, where a medium-high water portage over boulders may be necessary. The last
12 km section down to Urique (km 75-88) is class II-III with only 15 m/km
gradient (30-40 fpm). Thus, if you
donÕt mind numerous portages, potentially wildly fluctuating water levels, and
very challenging rapids, the trip will be one of the most rewarding in the world. [Overall on our trip we had ~20
portages: ~7 in first section to Arroyo Umir‡, 4 near Arroyo Basihaure, ~3 by
the Horseshoe Bend, ~4 in the Fantasma Falls area, and two more downstream. This number could probably be
reduced significantly with a higher, more optimal flow.]
The
third section of the river below the town of Urique is a 61 km stretch that
goes through Barranca Urique with gradients of 5-20 m/km (25-100 fpm) and
contains runnable class II-IV rapids.
A trail follows near the river for the first 28 km (kms 88-116) to a
place called Cuesta Colorada. This
trip starts with class II-III rapids down to ÒCambioÓ a class IV rapid at km
96.5 where the river cuts through limestone and a steeper section begins. Although Richard Fisher commented that
this section required a 1/4-mile portage for their raft trip, I found all the
rapids runnable and only of class III-IV difficulty at the lower flow. At very high flows some rapids may
approach class V, but everything would still be runnable. This section goes through one of the
deepest canyons in North America, with elevation difference from river to rim
peak on either side 1840 m-1990 m (>6030 ft!). After the steeper section ends a few km downstream, there
are only class III rapids for the remaining 30 km to the confluence with R’o
Fuerte (at km 133). Below here
itÕs only 6 km to the take-out at Tubares. Before completion of Presa Huites, one could continue on down
through the Fuerte Canyon another 86 km to Agua Caliente, then take the Copper
Canyon train back up to Creel. Unfortunately, when full, the Huites reservoir
comes up to a point just ~10 km downstream of Tubares, prompting the alternate
Tubares take-out and long drive (~8 hr) back up to Creel.
FLOWS
As
with most of the rivers in the region, the best time to catch good water levels
is during the monsoon season from mid-July through mid-September. Occasionally, winter storms will
bring waters levels up as well, and it is during these storms that the highest
flows are encountered. Often after a strong winter storm, things will remain
runnable for several weeks. During
the month of August, R’o Urique has a mean flow of ~27 cms (~800 cfs) at
Siquirichi, and ~40 cms (~1400 cfs) just upstream of Urique. These should be considered medium
optimal levels as well for the easier sections above Umir‡ and below Arroyo San
Ignacio, with flows above 2X this average being high. For the Barranca del Cobre section, optimal would be about
half that of the easier sections.
While each individual paddler and group must determine their own limits
within which they will attempt descent, in general, higher flows are always
better, since they usually will not last more than a day or two, and thus you
can always wait for levels to drop.
Because high water can make river difficulty a class higher, you may
deem the conditions too dangerous on your trip and decide to spend a layover
day or two while waiting. Thus
itÕs usually better to plan on a potential extra day or two for the trip
through the Barranca del Cobre section.
On the opposite side of the water issue, it is more likely that youÕll
encounter suboptimal flows, which are usually sufficient to pass down the
canyon but not very fun. On our
2001 descent through the Barranca del Cobre, we had only ~3 cms (~80 cfs) at
Umir‡, and 6 cms (200 cfs) at Urique.
Although still enjoyable for the canyon experience and scenery, the
whitewater was not as challenging, pin and broach potential was increased, and
progress was much slower. But
there are some benefits of low water - the river water gets clearer and warmer,
inviting swims in the green pools between rapids, you donÕt get pushed around
as much, and water levels can usually only get better (an optimistic view -
important for lengthy multi-day expeditions).
Below
are the mean flows recorded at the UriqueII gauging station (for 31 years
within 1967-1999).
_files/image002.jpg)
GRADIENT/DIFFICULTY (at a glance)
River km relative to Puente Norogachi (or Puente Umir‡); gradient in m/km; feet per mile (fpm); difficulty; elevations (top of 100 m drop)
|
km |
m/km |
fpm (map) |
class |
elevation |
|
-26 |
|
|
|
2300 m |
|
10 |
2.8 |
15(18) |
I-II |
2200 m |
|
21 |
9.1 |
48(48) |
II(IV) |
2100 m |
|
31 |
10.0 |
53 (53) |
IV-V |
2000 m |
|
47 |
7.7 |
41(40) |
III-IV |
1900 m |
|
59 |
5.8 |
31 (35) |
III-IV |
1800 m |
|
67.7 |
11.5 |
61(65) |
III-IV |
1700 m |
|
80.6 (4.6) |
7.8 |
41(42) |
IV-V |
1600 m |
|
84.2 (8.2) |
27.8 |
147(150) |
V-VI |
1500 m |
|
88.4 (12.4) |
23.8 |
126(140) |
V |
1400 m |
|
92.5 (16.5) |
23.4 |
129(160) |
V-VI |
1300 m |
|
98.8 (22.8) |
15.9 |
84(85) |
IV |
1200 m |
|
110.4(34.4) |
8.1 |
42(48) |
III-IV |
1100 m |
|
115.7(39.7) |
18.9 |
100(110) |
V |
1000 m |
|
126.4(50.4) |
9.3 |
49(50) |
IV |
900 m |
|
134.0(58.0) |
11.9 |
63(65) |
IV |
800 m |
|
145.1(69.1) |
9.0 |
47(48) |
III-IV |
700 m |
|
154.8(78.8) |
10.3 |
54(54) |
III |
600 m |
|
173.9(97.9) |
5.2 |
28(29) |
III |
500 m |
|
179.2(103.2) |
18.9 |
100(100) |
III-IV |
400 m |
|
211 (135) |
3.2 |
17(25) |
II |
300 m |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
Total length of R’o Urique from
Norogachi bridge to mouth: 209 km
(138 miles)
APPROXIMATE RAPIDS PER SECTION:
Upper Urique (Papajichi to Umir‡): 77
km: II(>30), III(>25), IV(25),
V(6)
Middle Urique (Umir‡ to A. San Ignacio): 38 km: II(>20), III(>20),
IV(>25), V(~23), VI(~16)
Middle Urique (A. San Ignacio to Urique):89 km:
II(>30), III(>30), IV (~18), V(4)
Lower Urique (Urique to R’o Fuerte): 46
km: II(>20), III(~15), IV (2)
Barranca del Cobre section
0.0 km Puente
Umir‡. Put-in
on river right (RR) upstream of the bridge. There is a path starting from the abandoned structure that
crosses a small arroyo and then descends to the river. The river is in a narrow chasm as it
goes under the bridge. Tom Diegel
and I launched with a very low flow of ~100 cfs Sun Sep 2, 2001, starting at ~3
pm in the rain. Driver: NecheÕs
friend. The first stretch down to
the Incised Meanders is easy (class II-III).
2.0-4.0 Incised
Meanders. At
the two saddles there are nice hikes up to view the river coursing around the
two adjacent horseshoe bends. We
hiked up the first one at km 2.1.
Good campspots can be found in this 2 km section.
2.7 Incised
Meander Falls #1 (V-VI; P). In a section of beautiful bedrock there are several channels with a
total vertical drop of approximately 8 m.
At the low flows we had, there were no clean routes, so we portaged
(easily). It looked like at higher
water an inviting route would open up on RL and possibly in the other
chutes. However, we could see a dangerous
sieve on the main RR chute that would be covered by water midway down. This has the potential to catch a
bow and pin the boater, and is quite dangerous since it would be obscured by
water at higher flows.
3.6 Incised
Meander Falls #2 (V). As the beautiful bedrock section
continues with some class II-III, there are good campspots to be found, and
then another large rapid in two parts.
The first fall aims to the right and is a 2 m 45 degree drop into a calm
pool. About 15 m downstream from
the first fall is a 6 m clean vertical falls. The pool below the falls is very
large and deep - no piton worries here.
This is one of the most enchanting places anywhere and one of the most
fun rapids on the entire river.
Downstream are several narrows sections where vertical overhanging walls
squeeze the river. About 0.5 km
downstream, two caves are passed on RR.
The steep boulder-choked section is 1.5 km past the falls, after some
class II-III rapids. On our
first trip down, we decided to camp just upstream of the falls on RR (after
running the first fall). The
following morning we re-ran the 2m falls and then the 6m lower falls. At low water, there were some more camp
spots in the next km.
4.8-6.0 Boulder
Jumbles (V/P6). After the scenic beauty of the
canyon entrance and just past a small arroyo on RL (Turuceachi), huge boulders
clog the riverbed, creating sieves and necessitating several portages. Tomster commented it was Òjust like the
SespeÓ, referring to a similar reddish boulder-choked section that is portaged
on that Southern California creek.
We found an interesting small sauna-like cave to explore while doing the
first couple portages (total portage time ~30 min). After the first portages, there is some class IV-V water
that we ran (although midway down a rock wasnÕt covered with enough water,
making us get out of our boats to scoot over it). After some more technical water, portaging, and floating
through a cave under a huge boulder on RL, we stopped for lunch. Sometimes the portaging would
necessitate floating over a short pool to cross the river or get to the next
staging spot. It was strenuous at
times and seemed to go on forever.
We may have used ropes once, but in general all could be done by hand.
Below the cave part, approximately 0.5 km upstream of Arroyo Umir‡, there were
more portages. It took us
approximately 3 hr to get through this 3 km stretch down to Arroyo Umir‡. At higher water, portages might
decrease somewhat due to floatable channels opening up, but this section would
still have a lot of portaging.
6.7 Arroyo
Umir‡ (RR).
This arroyo enters on river right.
In M. John FayheeÕs book ÒMexicoÕs Copper Canyon Country: A Hiking and
Backpacking GuideÓ, kayaker Bob Gedekoh wrote about a 4-day reconnaissance trip
he did hiking down the arroyo and scouting out R’o Urique in this section. His party hiked down the Arroyo Umir‡
only to be cliffed-out where the arroyo plunged 175 m just before reaching the
Urique. Although he found a RL route down some steep cliff ledges to the river,
the descent was unnerving for him and one of his companions. He reported hiking down the Urique a
few km to Òa point beyond which the riverbed seemed impassable without climbing
gear.Ó The following day they
hiked upriver through the Incised Meanders to the road near the Puente
Umir‡. He evaluated the river as a
potential run. ÒAll agreed that it
would be a technical nightmare.
The river flows under rocks as much as around them. At high water, the
river would be ripe with undercuts and siphons. Portaging would be a logistical
horror show.Ó Although we agree in
general with their assessment of the stretch down to Arroyo Umir‡, we found it
completely passable and not as much a horror as they make it sound.
7-12 Runnable!
(IV-V)n.
The 5 km stretch downstream of Arroyo Umir‡ to near Arroyo Basihuare is mostly
runnable and contains many class IV-V rapids separated by pools and easier
rapids. We had two portages (P2) in this stretch due to the low
water.
~10.5 Gracias
Falls (V). One
of the nicer rapids in this section along a right wall. ÒGracias a DiosÓ for such a nice
rapid. Tomster called this one
ÒOutcised Meander FallsÓ and deemed it IV+ or V-.
~11.3 Whiz
Wall (RR; then IVs, P2). Warm
springs seeping out of the wall on the right, about 2 m above our low river
level. In one low spot there is a
little stream of warm water shooting perpendicularly out like a man
peeing. We filled up water bottles
here. Downstream are several class
III-IV rapids, then a boat-scoutable IV+.
We portaged two rapids shortly before the confluence with Arroyo
Basihuare.
12.3 Arroyo
Basihuare (RR).
This large arroyo enters in a boulder jumble. The steep-walled side canyon might make an interesting side
hike. Just downstream is the
rapid Basihuare (IV+), where the river drops ~3 m in one sliding drop between
boulders. We camped just
downstream of the next class IV on RR.
ThereÕs a cave around here if a sheltered location is desired, but itÕs
a bit of a scramble to get up to it.
I found some fishing poles here that apparently Tarahumara have
left. ThereÕs a long pool
downstream of here followed by a low-water sieve that we could portage in-boat
on RL. Class III below here until
La Dominga.
12.9 La
Dominga (V). Where a small arroyo comes in on RL
(named La Dominga), youÕll find this technical rapid that ends with a 2 m drop
by the RL wall. DonÕt get stuffed up by the wall! Below here were two more portages (P2), the first due to low water
(could be run RL with more water), and the next a congested boulder pile
portaged RR. Then thereÕs a IV, some IIIs, and a couple more III-IVs before the
Vado.
14.0 Vado
(V-). On the map where the river makes a
90-degree turn left there is a trail crossing, and just below here is a class
IV-V that we took the middle channel through ending in a 2 m drop. Below here are more technical III-IV
rapids.
14.3-16.0 Technical
Rapids/Portages (V/P3). We had
about 3 portages in this section down into the horseshoe bend, and ran many
IV-V rapids.
16.0-17.3 Horseshoe
Bend (V/P3). In the first part of
the horseshoe bend the river drops a lot over multiple class V rapids and some
sieves. We portaged about three in
here. At one spot there is a cave formed under some boulders that we passed
through. There are numerous springs
on RR. At one spot under the
springs after portaging I seal launched into the river, only to hit the nose of
my boat and crack it open. I duct-taped it up. We had lunch near the middle of the Horseshoe (2pm). There are a couple more runnable IV-V
rapids to the end of the Horseshoe.
It is followed by a long stretch of II-III.
19.5 Cave
Rapid (V, then P3). After a
big beach on RR, we ran a cave rapid here where there was a fallen plant from
the wall, starting RR at the cave, and then moving left (route only available
at low water). After this we had 3
moderate portages (P3) around giant boulders. Near the start of the portages,
thereÕs a giant undercut cave on RL.
The last one we portaged actually was runnable Obscured (V/P). Around here there is a ton of
driftwood. A giant boulder on RL
blocked the full view of this rapid. After our portage, we saw that it actually
was a runnable class V in the far RL channel, but it was committing to get over
there an look at it.
19.7 Fantasma
Falls (V). As
we got out of our boats and scouted far above this rapid, downstream it looked
like a white ghost was wavering on the RL side by the wall. Quite eerie! This rapid is just above it and is a 3 m falls along the
left wall. The ÒghostÓ turned out
to be water pouring out of a tunnel in the bedrock, probably something drilled
for the mining in the area and abandoned, although thereÕs a possibility it was
a natural hole that water seeped out from. The water pouring out was seemed to
be the color of the river, however, making us suspect it had been diverted in
there at some place upstream.
~20 Tough
(V/P, V). In
some technical slots Tom attempted passage and ended up swimming. We also portaged one in this area. Around here are some minerÕs ruins on
RR, then another class IV-V that also briefly stuck one of us (video).
20.7 Ruins
(RL). We explored an abandoned decrepit
homestead on river left. This is the bottom of Barranca del Cobre proper, where
mining operations occurred. We
found a nice beach on river right just downstream of the ruins where we camped
(camp #3 at km 20.8 RR). I think this is a
beach mentioned in one of FayheeÕs hikes. Across the river is a mineshaft 5 m
above the river. A cable car
crossing is just downstream, with an arroyo on RL that was discharging some
blood red water on our trip (possibly mining operations). A trail also crosses
the river here and continues upstream on RR for ~0.3 km before ascending to the
rim at Tejab‡n. The hike on this trail is described by Richard Fisher in his
book, ÒMexicoÕs Copper CanyonÓ. At
Tejab‡n, you may find abandoned structures. There was a hotel here at one time, but the first guest, who
left the wood stove on while going out for a walk, burned it down
accidentally. In this section of
the river there arenÕt as many giant boulders, and rapids are usually class
II-III (maybe a few IV) for at least 5 km. It is still quite scenic and you will pass through a short
narrows at ~km 23. Congratulations
if you made it here, since from this point down there are only 1-2 more
portages!
~24.0 Dilapidated
Footbridge.
This failed structure still spanned the river. The following section is generally II-III, with maybe
some IV. The riverbed is much more
open.
29.3 Arroyo
(RL). We purified water out of this one. Reached here around noon. Before reaching the next large Arroyo
Cusarare downstream there are several class IVs.
31.7 Arroyo
Cus‡rare (RR). This is the same large arroyo that has
the often-visited wide 30 m falls near Creel (about 5 km from the road). The falls are, of course, most
impressive after recent rains.
However, theyÕre still pretty when running low. Farther down in this side canyon are
the Basirecota Hot Springs, thought to have curative properties by the
Tarahumara. On R’o Urique about 1
km below this arroyo confluence the gradient picks up a lot and boulders choke
the riverbed again (it soon becomes ~110 fpm down to Arroyo San Ignacio).
32.7 &