Ut313 - Gemini Bridges
Road(sh)
It is
hard to believe that as late as 1961, hardly
anybody knew of the existence of the natural
bridges along this route. The fact, that now just
about everybody does, hinges on a rockhound named
Lin Ottinger, who was tipped off by a local. Then
it took a decade for him to find them again a
second time. Things have changed - there are still
arches to be discovered and named in the remote
canyons of Utah, but Gemini Bridges are not among
them.
As Todd Campell already noted in his 1991 guide
book "now it isn't uncommon to hear of people
hackysacking on them, or wheelying across them.
Natural selection has its own special way of
dealing with folks so inclined". In order to
achieve this kind of popularity, a rockhound
cannot bear sole responsibility. You need more.
Somebody has to profit from all this beauty for
things to really start happening, This is where
all the able, energetic Moab merchants come in.
They help feed hungry cyclists, sell gasoline
canisters to motorcyclists, house them if the feel
so inclined and even rent portable toilets to the
campers. And yet, something is different
about this town, different from so many other
towns on the edges of National Parks. I think it
is this: there are no mini golf courses, pony
rides or christmas ornament stores in Moab (or at
least I didn't see any). There are just plain
fewer tourist trap businesses in general. Instead
the town attracts business generated through
organized marathon events like Outerbike or the 24
hours of Moab, and also organized bike tours over
the La Sal
Loop Road s(u). And then there are the music
festivals ...
click on profile for more detail
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1.(3960ft,mile00) START-END
EAST: Colorado River bridge north of Moab
2.(4580ft,mile08) Gemini Bridges Road
trailhead
3.(4780ft,mile13) route continues right
4.(4910ft,mile14) stay left
5.(5110ft,mile15) Gemini Arch overlook is
on left
6.(6050ft,mile21) TOP: road joins paved
Ut313. Profile continues right
7.(4580ft,mile35) same as 2
8.(3960ft,mile42) START-END WEST: same as
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Approaches
From East. Part of the fun of riding this
route from Moab is the excellent biketrail,
utilizing an abandoned roadbed between Arches
National Park and the Gemini Bridges trailhead -
and not paying the parking fee at the private ATV
staging area at the trailhead.
Past the trailhead the route is now well signed
with "Gemini Bridges" sings, and after that Ut313
signs. There are several additional alternate
loops and junctions along the way. Many options
dead end below the cliffs of the Wingate
formation. The area appears to be totally closed
to camping these days (Oct/11). As a result I
didn't see any people at all on the road during my
last visit, except for a group of five Bridge
frolickers. This is much less than during previous
years.
Continuing from the trailhead, the dirt road
parallels the highway for a short distance back to
Moab, then climbs the first lip to deliver the
picture perfect view of Moab between power lines
and rocks shaped like a million times magnified
tire track. Here the route enters Little Canyon.
If you were to guess that rain falling here,
should end up back down near US191 (let's assume
it rains really hard, and the water does not just
absorb into the ground), you would a reasonable
person, but taking a closer look will show
otherwise. The water drains towards the Colorado
on the west side. Little Canyon hangs above US191,
put there by the Moab fault, where displacement
has taken place due to massive underlying salt
layers. The road rolls down the upper part of
Little Canyon. But then rather than following the
canyon down to the Colorado River, the route turns
west and follows what has been named "the
Boulevard". There is no shopping here, but there
are plenty of turnoffs to spend much possible time
exploring. After traversing lone standing rock
outcrops, grouped into garden like formations by
the big gardener in the sky - or geology, a steep
sandy turn to the right at a junction signals the
exit from "the Boulevard". These slickrock
outcrops in this area are somewhat of an oddity.
This too can be the Wingate formation, the
ubiquitous cliff-forming orange, burnt sandstone,
that makes up so much of the cliffs around here.
Only here, the caprock - the Entrada formation, is
not present and it erodes into fins and domes.
A short series of climbs traverses sand mixed
with rock outcrops to the Gemini Bridges viewing
area. Here it is not uncommon to wander around
with clickety clackety cleats searching for -
where the heck is this arch anyway - when
discovering that your are standing on top of it.
Another thing you are standing on is the Entrada
formation - welcome back. The bridges formed right
at the edge of the reappearing contact point
between the Entrada and Wingate.
Natural bridges are formed when a river meander,
deeply incised into a canyon, becomes a cutoff
meander. Arches are formed by all other erosional
forces of wind and water, including seepage. Now
that we have that out of the way ... It is not
really clear that Gemini Bridges are natural
bridges. They could be "just" regular old arches.
The road continues to the right of the
arch/bridge viewing area, then immediately turning
left (just like the signs indicate) Traffic past
the bridge is much lighter, after heavy bridge
viewpoint visitation desire has been satisfied and
people return to Moab. Some maps refer to this as
the Gemini Bridges Bull Canyon road. This may be
misleading. Following directions for Bull Canyon
from the bottom, the road terminates and does not
offer a easy route to the rim, although Todd
Campbell's guide books reports several portagable
cracks through the Wingate. Once on top of this
big lip of sandstone, the road traverses Arth's
Pasture and summits at the junction with Ut313.
From West. The road joins the Ut313 island in
the sky s(u), a few miles north of the Ut313
summit, but only few feet below its point of
highest altitude. There is more on the
Ut313 Island in the Sky s(u) page.
History
Cycling: An early mountain biking guide
book, that included a detailed description of part
of this route, including a geological primer was
Tod Campbell's "Above and Beyond Slickrock",
published in 1991. He describes the ride as a one
way affair from top to bottom, ie. starting at its
junction with Ut313 and ending at the junction
with Ut191. Going downhill only it is not
surprising that he rates this as physically easy
and technically moderate. Today a number of single
track turnoffs have been added.
Dayrides with this point as highest summit
PARTIALLY PAVED / UNPAVED
Ut313 - Gemini Bridges Rd(sh) , Mineral
Bottom Rd(sh) : Willow Springs Road
> US191 south > up Gemini Bridges Rd >
Gemini Bridges Rd s(u) > down Ut313 a short
distance <> out and back on Mineral Bottom
Rd > to a turn around point a mile or two
inside Canyonlands NP, along the Green River
>> Mineral Bottom Rd(sh) > down Ut313
> back to starting point: 78.1miles with 4830ft
of climbing in 2:55hours (VDO MC1.0 m3:11.10.14).
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