Lab 5 - Igneous Rocks-2

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Montclair State University *

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105

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Geology

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Jan 9, 2024

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Points: /50 Chapter 5: Using Igneous Rocks to Interpret Earth History Exercise 5.3 (14 points) (a) i The crust (1 pt) (a) ii The crust will cool faster because of its greater surface area, so more of the hot material is in contact with the cold environment . (2 pt) (a) iii Circle answers: ( faster , slower), ( larger , smaller) (2 pt) (b) I The coffee in the plastic cup is going to cool faster. Styrofoam is a poor heat conductor. You can’t hold a plastic cup of a hot liquid without burning your fingers, but you can easily hold a Styrofoam cup of hot liquid because it is a better insulator. (3 pt) (b) ii Circle answer: ( faster , slower) (1 pt) (d) i Circle answer: ( finer , coarser) (1 pt) ii Circle answer: (finer, coarser ) (1 pt) iii aphanitic rock (1 pt) iv pegmatitic and phaneritic rocks (2 pt) Exercise 5.7 (36 points) Identify all of the samples listed below. Fill in the chart on the next page. Hand in the chart along with the lab answer sheet. *** You do not need to fill out the last column in the chart. Sample #s: 1, 2, 4, 6, 8-10, 12, 14. Basalt Granite Pegmatite Porphyritic Andesite Gabbro Obsidian Porphyritic Basalt Granite Rhyolite Pumice
(porous, glassy, fine, coarse, porphyri3c, pegma33c) (2 pts each) 1 9 2 4 8 6 10 12 14 (2 pts each) Fine-Grained Basalt (aphani3c) Coarse-Grained Gabbro (phaneri3c) Pegma33c Granite Pegmatite Fine-Grained Rhyolite (aphani3c) Porphyri3c Porphyritic Basalt Glassy Obsidian Coarse-Grained Granite (phaneri3c) Porphyri3c Porphyri3c Andesite Porous (vesicular) Pumice
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