GEOG 2OC3 Final: Geography Summary Notes
Document Summary
Palaeography the earth is 4. 5 billion years old - began as a fiery ball of lava in the hadean period formation of canada"s landforms timeline: Mountain belts: built from convergent stress/strain - when two tectonic plates overlap, mountains form. Epeiric seas: inland sea caused by high sea levels. Pleistocene period: recent glacial episodes beginning 2. 5 mya - beginning of quaternary period homo sapiens bagan to evolve. Orbital control + glaciation: earth orbits sun in ellipse and some factors contribute to how much solar insolation the earth will receive: Orbital eccentricity: departure of earth"s elliptical orbit from circular shape - influences solstices/equinox. Axial precision: change in orientation of earth"s rotational axis bc of pull of sun and moon. Glacial landforms: result from erosion by ice/meltwater and deposition. Drumlins: elongated hill in shape of inverted spoon by advance of glacier. Moraines: ridges/mounds of glacial material deposited close to ice margin - uneven topography.