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Igneous and Metamorphic Petrology and Cal Poly Geology Club ...

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<strong>Igneous</strong> <strong>and</strong> <strong>Metamorphic</strong> <strong>Petrology</strong> <strong>and</strong> <strong>Cal</strong> <strong>Poly</strong> <strong>Geology</strong> <strong>Club</strong><br />

Field Trip - 2011<br />

Mother Lode Gold Belt - Yosemite National Park<br />

The 2011 <strong>Geology</strong> <strong>Club</strong> Spring Field Trip was held in conjunction<br />

with Dr. Jessey’s <strong>Igneous</strong> <strong>and</strong> <strong>Metamorphic</strong> <strong>Petrology</strong> field trip. <strong>Cal</strong><br />

<strong>Poly</strong> students toured the Mother Lode Gold Belt <strong>and</strong> Yosemite National<br />

Park. The trip provided the opportunity to examine a geologic<br />

cross section through a collisional plate boundary, see the remnants<br />

of Pleistocene glaciations of the Sierra Nevada <strong>and</strong> learn<br />

about the colorful mining history of <strong>Cal</strong>ifornia.<br />

After a long drive through <strong>Cal</strong>ifornia’s Central Valley the field trip<br />

began at the <strong>Cal</strong>ifornia State Mining <strong>and</strong> Mineral Museum in Mariposa,<br />

<strong>Cal</strong>ifornia where the students learned about <strong>Cal</strong>ifornia’s rich<br />

mining history, saw a collection of historic mineral specimens <strong>and</strong><br />

even took a brief stroll through an underground mine tunnel.<br />

From there we drove north on CA 49 (aka the Mother Lode Highway)<br />

toward the town of Coulterville where we stopped at various<br />

locations to view rocks along the Melones Fault Zone. Exposures<br />

of tectonic mélange (terrane accreted to North America<br />

during Mesozoic convergence) are among the finest in the continental<br />

U.S. We saw pillow basalts, sepentinite, gabbro, chert <strong>and</strong><br />

greywacke. We also visited some active gold exploration properties.<br />

Perhaps the best stop, however was as the sheared <strong>and</strong> tectonized<br />

harzburgite shown in this photo. Students got to collect<br />

some great “green” rock for their home aquariums!<br />

The latter part of the afternoon was devoted to geology of the Mother<br />

Lode Gold Belt <strong>and</strong> an examination of historic mine workings. We<br />

stopped at the Virginia Mine <strong>and</strong> saw an impressive exposure of the<br />

Mother Lode quartz vein <strong>and</strong> got to view the remnants of placer mine<br />

workings along Moccasin Creek. We also viewed an enigmatic outcrop of<br />

an albitite dike. But the highlight of the afternoon was the exposure of<br />

quartz-ankerite-mariposite in a road cut west of Coulterville. Mariposite<br />

is a rare, emerald green chromium mica that is closely associated with<br />

gold mineralization. Prospectors used the presence of mariposite as an<br />

indicator of nearby gold ore. Students got to sample the mariposite,<br />

although they learned it took a lot of manual labor to break even a small<br />

sample off the outcrop!


After enduring a hailstorm in the campground, we awoke on the<br />

second day to learn that the road to Yosemite National Park was<br />

closed due to heavy snow! Following much soul searching <strong>and</strong><br />

coffee at the local Burger King in Mariposa, a decision was made<br />

to push on to the park <strong>and</strong> try to make a few stops before the<br />

area of road closure. We followed the slow moving traffic along<br />

the Merced River <strong>and</strong> stopped at outcrops of the <strong>Cal</strong>averas Complex<br />

<strong>and</strong> Shoo Fly Complex to view Paleozoic rocks that acted as<br />

hosts for the intrusion of the Jurassic-Cretaceous Sierra Nevada<br />

batholith. The image to the right shows the folded <strong>and</strong> contorted<br />

chert beds of the <strong>Cal</strong>averas Complex along the Merced River.<br />

Much to our surprise <strong>and</strong> delight, by the time we reached the<br />

park entrance the road had been reopened into the valley. We<br />

were among the first vehicles into Yosemite Valley that morning.<br />

Below is the view that awaited us from the Wawona Tunnel.<br />

The remainder of the day was spent in Yosemite National Park where we got drenched at Bridalveil Falls, visited the USGS stream<br />

gauge at the Pohono Bridge, w<strong>and</strong>ered around in the crowds at the Visitor Center <strong>and</strong> hiked up to Yosemite Falls. We talked about<br />

the geology of the Tuolumne intrusive series, glacial features <strong>and</strong> the natural history of the park along the way. Unfortunately, we<br />

DID NOT collect any rock samples, much to the chagrin of some students. After our final stop at Yosemite Falls, the group split up<br />

with some electing to stop in the Mariposa Sequoia grove at the southern park entrance while others returned via Mariposa <strong>and</strong><br />

Merced, driving through exposures of the Great Valley Group. All in all. it was an exciting experience that provided screen saver


images for everyone’s computer <strong>and</strong> cell phone!.

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