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Working collaboratively, groups of students [3-4]develop hypotheses addressing the paleotopography of a Miocene river channel [Table Mountain Latite] and processes that have resulted in its current topographic expression. Students use observations/data gained from topographic maps [Sonora, Keystone, Melones Dam and Knight's Ferry 7.5 minute quadrangles], San Francisco-San Jose Regional Geological Map, aerial photos, and Google Earth [120 39 01W; 37 48 15N to 120 26 17W; 37 57 36N]. Using PowerPoint, students present and defend their hypotheses and plans for further research during the final week of the semester. Designed for a geomorphology course
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