BUILDING A GEOLOGIC HISTORY FROM AN ARCHEAN TO PLEISTOCENE COLLAGE: LEARNING ABOUT GEOLOGIC PROCESSES THROUGH LOCAL GEOLOGY IN THE MINNEAPOLIS-ST. PAUL, MN, REGION
The exposed bedrock in the Twin Cities is an essentially flat-lying Paleozoic sedimentary sequence, which directly overlies basement rocks of the 1.1 b.y. Midcontinent Rift. Paleoproterozoic and Mesoproterozoic igneous and metamorphic rocks are exposed northwest of the Twin Cities in the St. Cloud region. Bedrock units are overlain by glacial and glacio-fluvial sediments ranging from 0 to 1000m in thickness.
In this course the teachers were introduced to isolated components of the stratigraphic sequence, and through answers to their own questions, or the questions we ask of them, they learn to use principles of correlation and relative age to develop a rudimentary geologic history. Local geologists with expertise in a variety of geologic subdisciplines lead the investigation each day by posing a series of questions that will lead the teachers to recognize the geologic relations between the isolated components. Rock units not present in the metro area are investigated through use of an urban walking tour of facing stone; we also use walls composed of till-derived boulders to investigate the variety of Archean and Proterozoic terranes of northern Minnesota.
Investigation of the bedrock geology is complemented by studies of surficial processes, such as stream gauging and calculation of waterfall retreat rates based on field observations in bedrock, till, and outwash units. A trip to the St. Anthony Falls Research Lab introduces the teachers to the role of modeling in surficial processes and basin analysis.