Crossword Solver > found answer > ANTICLIN

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

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anticlin

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

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

There are 8 letters in ANTICLIN ( A1C3I1L1N1T1 )

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

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

ANTICLINE CLINTONIA ANTICLING

6 letters out of ANTICLIN

ANILIN CATLIN INCANT ITALIC NIACIN TANNIC TINCAL

5 letters out of ANTICLIN

ACINI ACTIN ANTIC CILIA ILIAC LICIT LINAC LININ LITAI TICAL

4 letters out of ANTICLIN

ALIT ANIL ANTI CAIN CANT CLAN ILIA INIA INTI LAIC LAIN LATI LINN LINT NAIL TAIL TAIN TALC TALI

3 letters out of ANTICLIN

ACT AIL AIN AIT ALT ANI ANT CAN CAT INN LAC LAT LIN LIT NAN NIL NIT TAN TIC TIL TIN

2 letters out of ANTICLIN

AI AL AN AT IN IT LA LI NA TA TI

Searching in Dictionaries ...

Definitions of anticlin in various dictionaries:

ANTICLIN - In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core. A typical anticline is convex ...

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Anticlin might refer to
In structural geology, an anticline is a type of fold that is an arch-like shape and has its oldest beds at its core. A typical anticline is convex up in which the hinge or crest is the location where the curvature is greatest, and the limbs are the sides of the fold that dip away from the hinge. Anticlines can be recognized and differentiated from antiforms by a sequence of rock layers that become progressively older toward the center of the fold. Therefore, if age relationships between various rock strata are unknown, the term antiform should be used.
* The progressing age of the rock strata towards the core and uplifted center, are the trademark indications for evidence of anticlines on a geologic map. These formations occur because anticlinal ridges typically develop above thrust faults during crustal deformations. The uplifted core of the fold causes compression of strata that preferentially erodes to a deeper stratigraphic level relative to the topographically lower flanks. Motion along the fault including both shortening and extension of tectonic plates, usually also deforms strata near the fault. This can result in an asymmetrical or overturned fold.
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