GEOL105- Final Exam Guide - Comprehensive Notes for the exam ( 26 pages long!)

• School: University of Delaware
• Department: Geology
• Course: GEOL105
• Professor: Susan Mc Geary

Document Summary

Imagine trying to squish a glass bottle (somewhat similar to the mineral quartz) between your fingers. The bottle is much stronger than mud, as quartz is much stronger than clay: a(cid:374)other (cid:862)(cid:449)eak(cid:863) (cid:373)i(cid:374)eral calcite, limestone & marble rocks composed of calcite, minerals summary, elements consist of protons, neutrons, and electrons. If the hale is (cid:271)uried deeper, heat a(cid:374)d pressure (cid:373)a(cid:455) (cid:373)eta(cid:373)orphose it i(cid:374)to : slate, a metamorphic rock. Igneous, sedimentary, metamorphic: relati(cid:448)e (cid:862)stre(cid:374)gth(cid:863) of, granite, sandstone, shale. Why: he (cid:272)ould(cid:374)"t e(cid:454)plai(cid:374) how or why continents moved, wegener dies in 1930 at the age of 40. I(cid:374) (cid:1005)96(cid:1004), harr(cid:455) hess pu(cid:271)lished his (cid:862)essa(cid:455) i(cid:374) geopoetr(cid:455)(cid:863) The(cid:455) get older; at the (cid:272)rust, the(cid:455)"re (cid:271)ra(cid:374)d (cid:374)e(cid:449), (cid:271)ut as the(cid:455) (cid:373)o(cid:448)e apart, they get older: modern evidence from satellites. If there is water in the ground, the ground can become like jell-o, and the buildings sink into the ground: new topography, ground moves up, tsunami.