
| Prof. Glazner's First Year Seminar, Fall 2003 |
| Field
Geology of Eastern California |
Lateral moraines along lower Pine Creek northwest of Bishop.
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The Bishop Tuff, remnants of a huge volcanic eruption 760,000 years ago.
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Curving columns in the Bishop Tuff.
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Steaming fumarole at Casa Diablo geothermal plant. It smelled like the House of the Devil--very sulfurous.
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The Casa Diablo plant is tucked away in the trees. It provides enough renewable, friendly power for about 40,000 homes. Magma is your friend.
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Obligatory shot of Devil's Postpile. Students are on top (about 3 pixels each).
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Columns are supposed to have 6 sides, but if you count a lot of them you see that 5 is more common than 6. Why?
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On top of the Postpile.
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Fall on the San Joaquin River upstream of the Postpile.
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We finished the day at Hot Creek. Pay no attention to the "DANGER--SCALDING WATER--UNSTABLE GROUND--KEEP OUT" sign.
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