Beryl but not emerald |
Brenner, whose bio explains her expertise as, "[a] stint as Manager of the California State Mining and Mineral Museum," launched into a primer on mineral identification. She nibbled around the edges of crystal shape by claiming that "Minerals fall into five basic shape categories," listing Massive, botryoidal, reniform, tabluar, and acicular. In point of fact massive, botryoidal and reniform refer to the shape of mineral aggregates, not to the minerals themselves. So much for "shape."
Brenner then harped briefly on mineral streak, telling her readers that,
"...the hematite stone is black when polished, but it leaves a red streak across unglazed porcelain or ceramic."Out staff geologist shuddered at the construction "hematite stone," since hematite is a mineral... But, then, Laurie the journalist is the expert, not some guy with a couple of degrees in geology. Next, we learn to inspect the luster, then the cleavage, of which Brenner rattles off bogosity like,
"Flat flakes break in one piece... Rhombic breakage occurs on several planes at diagonal angles... Long blocks result in breakage in two planes..."
What we will do, however, is point out that Brenner did her readers a great disservice by prattling about gems. Instead, she should have started by explaining that gemstones are, by and large, exceptional specimens of more "ordinary" minerals. If you want to find emeralds, for instance, you look for beryl; to find sapphires and rubies, hunt for corundum.
Maybe our Dumbass of the Day should have started there...
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SI - MINERALS
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