MINERARLS:
- naturally occuring
- homogeneous
- inorganic
- color
- luster; subvitreous (less than glass), earthy (dull), greasy (oil), pearly, silky
- streak
- crystal structure
- cleavage
- density; m/v
- hardness; Moh's Scale applicable
- magnetism; only applicable to magnetite
- acid rxn; proof of calcite
- taste; salty for proof of halite
ROCKS:
- composed of one or more minerals
- classified by their origin/formation ------->
categorized by
- grain size ---> intrusive(inside Earth, slowly formed) visible vs. extrusive (Earths exterior, quickly formed) not visible
- mineral content---> felsic (feldspar, silica) light vs. mafic (magnesium, iron) dark
EX) basalt, rhyolite, gabbro, diorite, granite, obsidian, scoria, pumice, tuff
2.) Sedimentary: formed from existing rock sediments, compaction/cementation
-weathering
-erosion
-transportation
-deposition
-lithification; compacts/cements together to harden
categorized by content
fragmental (clastic) grain size--> energy of the environment formed*
vs.
organic (bioclastic): animal remains/fossils
Other; Chemical- rock salt by evaporation
EX) Clastic; conglomerate, breccia, sandstone, siltstone, shale
Bioclastic; limestone, halite, coal, gypsum
*energy level correlates to grain size; high energy large grain, low energy small grain
2.) Metamorphic: Igneous of sedimentary rock changed by heat/pressure deep below Earth's surface. Exposed by plate shifts and mountains
categorized by foliation/banding (light/dark layers)
& grain size; fine, medium coarse
EX) foliated; slate, schist, gneiss
nonfoliated; marble*, anthracite, quartzite
*reacts with acid due to calcite content
this is amazing melina, thanks!!
ReplyDeletecouldn't have said it better myself...thanks melina
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