conchoidal fracture in quartz |
Oh, Kwak managed to skim the surface of a couple web pages devoted to the two minerals, and he also skimmed the first paragraph of the Wikipedia article about quartz. That, in fact, is where he made his first science boo-boo:
"...quartz is the second most abundant mineral making up the Earth's crust..."...except that Patrick didn't realize that the same sentence says that "feldspar" is more abundant. Only one problem with that: even G101 students know that there are two feldspars, orthoclase and plagioclase (and plagioclase is further subdivided). Ergo, quartz is the most abundant single mineral.
Kwak copies, rewords, and pastes a lot of details that we're pretty certain he didn't understand such as the notion that
"Both mineral crystal structures fall under the trigonal-crystal-shape category [sic]..."...which is a bass-ackwards way to say that both minerals are in the trigonal class (quartz is trapezohedral and calcite is scalenohedral). And then there's the discussion of cleavage, where Patrick allows that quartz
"...does not break cleanly and has an indistinct cleavage."Such are the dangers of simply parroting information you don't understand, Patrick. When a middle-school earth science student or a college pre-law major taking "Rocks for Jocks" asks about the physical properties of calcite and quartz, it's a pretty safe bet that the OQ wants you to tell them that
- Calcite cleaves into well-defined rhombohedra, while quartz exhibits conchoidal fracture (see image above).
- Quartz is stable in (most) acids, while calcite effervesces even in household vinegar.
- Calcite is fluorescent, quartz is not
¹ If you'd like to see one freelancer's excuse for sloppy work, check out Shanea Patterson's comment here...
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SI - MINERALS
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