GGR201H1 Lecture Notes - Lecture 2: Stratovolcano, Convergent Boundary, Viscosity

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2 1 geomorphic processes and sources of energy. Geomorphological processes are natural mechanics of weathering erosion transportation and deposition that results fromthe application of physical and chemical forces to materials and landforms at the. Looking at a discharge vs time we see. Magnitude frequency process: frequently the event occurs and how intense the event is e g magnitude. Exogenic forces from outside the system of earth a. solar radiation thermal weathering biological weathering gradient drive weather circulation wind evaporation gravity at earth s surface gravitational forces b w the earth and water ice sediments b. G m1m2)/d2] is the gravitational constant formula that tells us about what gravity is on earth where g 6 674x10- Endogenic forces from within the system of earth c. d. Internal geothermal sources radioactive decay mantle convection plate tectonics epeirogeny volcanism hotspots. Gravity of the earth internally isostasy gravitational equilibrium b w the crust and asthenosphere due to buoyancy.

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