(Are you) Cummingtonite??? Tees by fossiliferous

Cummingtonite is a metamorphic amphibole with the chemical composition (Mg,Fe)7Si8O22(OH)2. It is commonly found in metamorphosed magnesium-rich rocks and occurs in amphibolites. It has also been found in some felsic igneous rocks such as dacites.

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Basic American Apparel T-Shirt

Enjoy the feel of 100% fine jersey cotton against your skin. This unisex shirt, by American Apparel, is the softest, smoothest shirt we sell. It’s medium weight and made from combed cotton for your added comfort. Gives a flattering and stylish fit to virtually any body type. Made in the USA.

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Found in the geology store category on Zazzle, this exceptional men's t-shirt idea was designed by "fossiliferous". With the title of “(are you) cummingtonite??? tshirt”, this creme chemistry t shirt is just a minute fraction of the many awesome chemistry creations that are available online from Zazzle. While fossiliferous has titled this regular men's American Apparel t-shirt the (are you) cummingtonite??? tshirt, you can discover other similar t-shirts by searching our marketplace for the tags: "science tee shirts", "geology tshirts", "humor t shirts", or "chemistry shirts".

Zazzle's classic American Apparel tee shirt is an absolutely perfect match for this science concept. Created with 100% fine jersey cotton and finely combed for the perfect comfort, this tee shirt option is available for ordering in a number of colors and in sizes as large as 3XL. Featuring a stretchy, ribbed neck-band, this Bad Geology Puns store section shirt fits wonderfully on any lady or gentleman. Once it is printed with this seller's random idea, this light-weight t-shirt can be worn anytime.

(Are you) Cummingtonite??? Tees

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Created By fossiliferous:

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(Are you) Cummingtonite???

Cummingtonite is a metamorphic amphibole with the chemical composition (Mg,Fe)7Si8O22(OH)2. It is commonly found in metamorphosed magnesium-rich rocks and occurs in amphibolites. It has also been found in some felsic igneous rocks such as dacites.

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