Crossword Solver > found answer > STYLOLIT

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Welcome to Anagrammer Crossword Genius! Keep reading below to see if stylolit 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 stylolit.

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stylolit

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

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

There are 8 letters in STYLOLIT ( I1L1O1S1T1Y4 )

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

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

STYLOLITE

6 letters out of STYLOLIT

SLITTY STILLY TOLYLS

5 letters out of STYLOLIT

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

4 letters out of STYLOLIT

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

3 letters out of STYLOLIT

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

2 letters out of STYLOLIT

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

Searching in Dictionaries ...

Definitions of stylolit in various dictionaries:

STYLOLIT - 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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Stylolit 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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