GEOL 1304 Lecture Notes - Lecture 7: Outwash Plain, Glacier Morphology, Cryosphere
Document Summary
The fate of the hydrosphere and lithosphere that are perennially frozen. Inetrnally, below the rigid surface level , fractuures as the underlying plastic zone motion forward. No, they move under the insistency of their own great weight and the pull of sombreness (stream-like patterns) When one species bene t and another is harmed by the association (fleas and frump ) The process by which plants produce their own nutrient from co2 and water system , powered by solar. Energy ; releases o2 and vigour -rich organic material, simoleons , and starches. Sort when an isolated pulley-block of ice persists in a ground moraine, and outwash plain, or a valley after a glacier retreat ; steepsided hole that frequently lling with water. High level canopy that is shuf ing up of the top of huge trees that jut above the surrounding forest; not continuous; biomass is concentrated here.
