Crossword Solver > found answer > ARGIL

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CROSSWORD
ANSWER

argil

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The answer ARGIL has 1 possible clue(s) in existing crosswords.

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The word ARGIL is VALID in some board games. Check ARGIL in word games in Scrabble, Words With Friends, see scores, anagrams etc.

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Definitions of argil in various dictionaries:

noun - a white clay (especially a white clay used by potters)

Clay, especially a white clay used by potters.

noun - a white clay

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Keep reading for additional results and analysis below.

Possible Crossword Clues
Potter's clay

Last Seen in these Crosswords & Puzzles
Mar 8 2009 The Times - Concise

Possible Dictionary Clues
Clay, especially a white clay used by potters.
clay, especially potter's clay.
a white clay (especially a white clay used by potters)
Clay, especially potter's clay.

Argil might refer to
Clay is a finely-grained natural rock or soil material that combines one or more clay minerals with possible traces of quartz (SiO2), metal oxides (Al2O3 , MgO etc.) and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure. Clays are plastic due to particle size and geometry as well as water content, and become hard, brittle and nonplastic upon drying or firing. Depending on the soil's content in which it is found, clay can appear in various colours from white to dull grey or brown to deep orange-red.* Although many naturally occurring deposits include both silts and clay, clays are distinguished from other fine-grained soils by differences in size and mineralogy. Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in particle size and other physical properties. The distinction between s

Argil might refer to

Clay is a finely-grained natural rock or soil material that combines one or more clay minerals with possible traces of quartz (SiO2), metal oxides (Al2O3 , MgO etc.) and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure. Clays are plastic due to particle size and geometry as well as water content, and become hard, brittle and nonplastic upon drying or firing. Depending on the soil's content in which it is found, clay can appear in various colours from white to dull grey or brown to deep orange-red.* Although many naturally occurring deposits include both silts and clay, clays are distinguished from other fine-grained soils by differences in size and mineralogy. Silts, which are fine-grained soils that do not include clay minerals, tend to have larger particle sizes than clays. There is, however, some overlap in particle size and other physical properties. The distinction between s

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