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Thread: Salt Wash Road

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    Salt Wash Road

    May 2013!

    Coming from the Goblin Valley area over Clay Hills Road we reached the point where this road intersects with Coal Mine Road on Factory Bench. (Utah, Emery and Wayne County). At this place (12S 0506411 4261697) a third road goes the the southwest skirting North Caineville Reef. This one is said to be a dead end but this might not be true. Rumors are that there is an old connection to Last Cahnce Wash between Cathedral Valley and I 70 to the north. We found some mostly short spurs leading into nowhere. Years ago driving into Salt Wash Canyon was possible up to some springs but we decided to turn around at this place.

    The trip started in the early evening around 6 pm. Wonderful evening light for colorful rocks.


    The road starts here, but the one seen on the right side is Clay Hills road

    Salt Wash Road descends from Factory Bench into a shallow valley south of North Caineville Reef. Reaching the Reef it turns to southwest. At a first glance it is a lifeless place - but it isn't!


    Along the Reef in southwestern direction

    The land is dark grey to black with white patches. This must be minerals. Another thing to find is brown gravel. No gravel at all, these are Billions (?) of petrified mussels.


    On the left the rim to Factory Bench. Again North Caineville Mesa


    Impressing landscape

    After a little more than a Mile the road switches trough a gap onto the opposite side of the Reef.


    At this point the road turns right

    It is not only a switch of the side it is of switching colors too. The other side is red.


    Red

    Now we are there where Salt Wash is flowing in a northern direction to discharge into Muddy Creek.


    Muddy Creek flows in front of the Moroni Slopes


    Salt Wash Road. North Caineville Reef is now on the left side.


    Salt Wash Valley in northern direction


    The road crosses flowing Salt Wash for the first time


    Another cliff line to the west

    The incline of these layers is caused by the rise of the San Rafael Swell. Bedding goes up to the west at an angle of approximately 25 degrees.


    From Entrada (bottom) to Mancos Shale


    Evening light

    A second ford through Salt Wash where it comes out of a slightly deeper canyon. There we drove in 20(?) years ago.


    Wood Bench in the south


    Deep red coused by evening light


    Gray North Caineville Mesa

    The road climbs up onto a hill.


    Looking back to Salt Wash


    Remains from Salt Wash


    This seems to be the reason for building the road.


    Factory Butte

    Not far away from the drill hole the trail ends above a tributary of Salt Wash, dry at the time. We noticed some ATV tracks going down into the drainage.


    Road end


    Wood Bench Rim

    The rim of Wood Bench looks similar to Cathedral Valley. No surprise, it has more or less the same geological structure.

    Time to turn around! We are heading back to Coal Mine Road.


    Near Salt Wash

    Once again going through North Caineville Reef and its color diversity.


    Red North Caineville Reef


    Gray part of it

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