Crossword Solver > found answer > STYLOLI

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Welcome to Anagrammer Crossword Genius! Keep reading below to see if styloli is an answer to any crossword puzzle or word game (Scrabble, Words With Friends etc). Scroll down to see all the info we have compiled on styloli.

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styloli

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The answer STYLOLI has 0 possible clue(s) in existing crosswords.

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The word STYLOLI is NOT valid in any word game. (Sorry, you cannot play STYLOLI in Scrabble, Words With Friends etc)

There are 7 letters in STYLOLI ( I1L1O1S1T1Y4 )

To search all scrabble anagrams of STYLOLI, to go: STYLOLI?

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Scrabble results that can be created with an extra letter added to STYLOLI

LOYALIST XYLITOLS STOLIDLY

6 letters out of STYLOLI

STILLY TOLYLS

5 letters out of STYLOLI

LILOS LILTS SILLY SILTY SLILY STILL STYLI TILLS TOILS TOLLS TOLYL YILLS

4 letters out of STYLOLI

ILLS ILLY LILO LILT LILY LIST LITS LOST LOTI LOTS OILS OILY SILL SILO SILT SLIT SLOT SOIL SOLI SYLI TILL TILS TOIL TOLL TOYS YILL

3 letters out of STYLOLI

ILL ITS LIS LIT LOT OIL SIT SLY SOL SOT SOY STY TIL TIS TOY

2 letters out of STYLOLI

IS IT LI LO OI OS OY SI SO TI TO YO

Searching in Dictionaries ...

Definitions of styloli in various dictionaries:

STYLOLI - Stylolites or styolite (Greek: stylos, pillar; lithos, stone) are serrated surfaces within a rock mass at which mineral material has been removed by ...

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Keep reading for additional results and analysis below.

Styloli might refer to
Stylolites or styolite (Greek: stylos, pillar; lithos, stone) are serrated surfaces within a rock mass at which mineral material has been removed by pressure dissolution, in a process that decreases the total volume of rock. Insoluble minerals, such as clays, pyrite and oxides, as well as insoluble organic matter, remain within the stylolites and make them visible. Sometimes host rocks contain no insoluble minerals, in which case stylolites can be recognized by change in texture of the rock. They occur most commonly in homogeneous rocks, carbonates, cherts, sandstones, but they can be found in certain igneous rocks and ice. Their size vary from microscopic contacts between two grains (microstylolites) to large structures up to 20 m in length and up to 10 m in amplitude in ice. Stylolites usually form parallel to bedding, because of overburden pressure, but they can be oblique or even perpendicular to bedding, as a result of tectonic activity.
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