Clinton Field Trip Report

Introduction On Saturday, March 12, 2011, about thirty students geographics 213 at Simon Fraser University had a cardinal-day field excursionist in British Columbia. The briny objectives of our field trip were to acquire skills as a structural detective and to make inferences from field observations on rush performance by multiple working hypotheses. During this trip, there were dozens of activities to do and some ideas such as the impact of glaciations to filling up. In this field trip we took the bus mainly on the Trans-Canada highway from Burnaby Mountain through variable topography and climate. The trip began in cast down mainland, and passed through the Sumas valley. After the prototypal two moolah, we went to trade unioneast to nicety three bumps near Hope. Then, we went a long trip north-centralward to the Thompson Valley to finish 4 stops. And we had overnight in Clinton at the Clinton Lodge. The second day, we went to the most north stop in this field, and then we finished the rest of fours stops near Thompson valley. These first five stops located at coast mass stray. It predominate by plutonic and fervid rock. Its compressed and mild. After entering Drynoch, the region was Interior. It dominate by Volcanic, and aqueous rock. Its much hotter and arid than the strand Mountain range region. Since different geology and climate produces different landforms, the phytology and the observation targets ar different. On the West of Fraser Valley, the majority of the landform was coast Mountain. Vegetation was dominated by maple trees, pine trees. On the eastmost side, the majority of the landform was change surface plateau. Vegetation was dominated by bush, Bunchgrass. Stop 2: Sumas Valley 2.1 mending The second stop of the field trip was Sumas Valley. Its organize was 49°0321 N, 122°1045W. As stop of the Fraser Valley, it lied mingled with the Coast Plutonic Complex to the north and the largel! y volcanic Cascade Fold Belt to...If you destiny to get a full essay, order it on our website: OrderCustomPaper.com

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