Marble Mountains

  January
                is a great month to explore the Marble Mountains. Our plan
                was to explore them on Saturday, camp there, then meet the
                Yucaipa Valley
                Gem and Mineral Society for a trilobite fossil
                hunt on Sunday.  We left Highway 40 at Ludlow and drove
                the old National Trails Highway, Route 66, through Amboy to
                Chambless. What a 
difference from Highway 40!  You
                could almost lie down in the middle of the road and take
                a nap there was so little traffic!  Arriving at Chambless we
                turned north toward the Marble Mountains and the Trilobite Wilderness
                Area.  James Mitchell has excellent directions and detailed
                maps on pages 66 and 67 of his book Gem
                Trails of Southern California.  Our goal was to
                explore what he refers to as Site B.  This area literally
                has a small mountain covered in dark red and brown garnet crystals.  Most
                of the crystals are very small and form a druzy covering of the
                rocks.  However, a few larger crystals can be found.  There
                is also a large amount of lime green epidote and bright metallic
                hematite in the area.  The idea is to find these two mixed
                together in the same rock.  The results are quite showy!
          
difference from Highway 40!  You
                could almost lie down in the middle of the road and take
                a nap there was so little traffic!  Arriving at Chambless we
                turned north toward the Marble Mountains and the Trilobite Wilderness
                Area.  James Mitchell has excellent directions and detailed
                maps on pages 66 and 67 of his book Gem
                Trails of Southern California.  Our goal was to
                explore what he refers to as Site B.  This area literally
                has a small mountain covered in dark red and brown garnet crystals.  Most
                of the crystals are very small and form a druzy covering of the
                rocks.  However, a few larger crystals can be found.  There
                is also a large amount of lime green epidote and bright metallic
                hematite in the area.  The idea is to find these two mixed
                together in the same rock.  The results are quite showy!As
                we drove toward the site the dirt road began to get rocky.  A
                stout vehicle would probably make the trip, but four wheel drive
                is advised.  We drove up the wash and then headed steeply
                uphill to a turn around at the dead end that made a good base
                for our exploration.  To cover more ground we hiked in different
                directions and kept in contact with our  radios.  They
                provide not only a safety factor, but also make it possible to
                share information on what is being found.  The climb from
                the dead end is steep in any direction.  It was hard to
                hear anything 'cause my heart was thumping so loudly!  We
                
                gained elevation quickly and some nice vistas unfolded.  I
                also found a nice example of one of the larger garnet crystals
                in the wash I was scrambling up.  Soon the epidote and hematite
                deposits began appearing and then some rocks containing both.  These
                specimens looked great in the bright sun!  A call from Niki
                informed me that she had flushed some big horn sheep and managed
                to get a very distant photo of the head of one as it looked back
                down on her before disappearing over a ridge.  I also was
                seeing scat and tracks that indicated they were in the area.  The
                climbing and scrambling was hard work, but we really enjoyed
                the scenery and were very pleased with the rock samples we found.
          
                gained elevation quickly and some nice vistas unfolded.  I
                also found a nice example of one of the larger garnet crystals
                in the wash I was scrambling up.  Soon the epidote and hematite
                deposits began appearing and then some rocks containing both.  These
                specimens looked great in the bright sun!  A call from Niki
                informed me that she had flushed some big horn sheep and managed
                to get a very distant photo of the head of one as it looked back
                down on her before disappearing over a ridge.  I also was
                seeing scat and tracks that indicated they were in the area.  The
                climbing and scrambling was hard work, but we really enjoyed
                the scenery and were very pleased with the rock samples we found.As
                evening approached we drove back down into the wash to find a
                level spot that wasn't too rocky so that we could put up our
                tent.  As we set about our campsite chores the sun slowly
                set, washing the hills with a rosy glow.  We had dinner
                around the campfire, but the night got cold quickly and
                we retreated into the tent which was quite cozy.  At dawn
                I heard a loud swoosh, swoosh, swoosh sound and popped my head
                out to find that all that noise was being made by the wings of
                a raven that was flying over!  Now that's solitude!  We
                packed up and drove back to Amboy for breakfast and waited for
                the rock club to arrive and start on our trilobite adventure.  The
                Marble Mountains south of Chambless and east of Cadiz have exposed
                a window to the past.  This window is shale. The shale
                that has now been uplifted in these mountains was once the mud
                bottom of an ancient ocean.  These shales are as old as
                600 million years.  Trilobites, creeping crablike creatures,
                were very common in these seas.  They lived and died in
                uncounted numbers.  As they drifted to the mud bottom they
                became entombed.  The mud, under heat and pressure, became
                shale, and the shale still has within its layers the imprints
                of these trilobites that have been extinct for nearly 300 million
                years.  Wow!  We were really excited to split some
                shale!  Very few whole trilobite fossils are found.  Most
                of the finds are of heads, legs, etc.  But what the heck,
                even that is pretty neat!
          
After
                breakfast our small group headed out to the fossil area.  Mitchell's
                book also has good maps and directions to this area on pages
                64 and 65.  The first shale outcrop we stopped at was my
                favorite.  The shale had a reddish glow to it and the hillside
                was bathed in morning sunshine.  Shortly we were all finding
                bits and pieces of trilobites.  Holding the remains of a
                300 million year old organism is a real treat.  After a
                while we decided to move to the best known site.  This
                site is high on a hillside and usually produces some larger specimens.  That
                didn't happen today, but the hike was nice and the views spectacular.  We
                left with a new appreciation for time, it actually made me feel
                a lot younger!As
                we returned to old Route 66 for the journey home, we saw one
                last inexplicable sight.  Off to the side of the highway,
                between Chambless and Amboy, a large tree had been covered
                by pairs of shoes that had been thrown into it!  Was it
                the work of aliens?  Bored travelers, who then continued
                on barefoot?  Maybe 300 million years from now geologists
                will be digging up fossils of the amazing shoe tree!
        