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- Fissility_(geology) abstract "Fissility or Fissionability (American English) refers to the property of rocks to split along planes of weakness into thin sheets. This is commonly observed in shales, which are sedimentary rocks, and in slates and phyllites, which are foliated metamorphic rocks. The fissility in these rocks is caused by the preferred alignment of platy phyllosilicate grains due to compaction, deformation or new mineral growth. A highly fissile rock splits easily along the cleavage.".
- Fissility_(geology) thumbnail Muzeum_Złota_w_Złotoryi_fyllit_Panenska_Hůrka_21.07.2011_p.jpg?width=300.
- Fissility_(geology) wikiPageID "6181420".
- Fissility_(geology) wikiPageLength "1923".
- Fissility_(geology) wikiPageOutDegree "14".
- Fissility_(geology) wikiPageRevisionID "618256674".
- Fissility_(geology) wikiPageWikiLink Category:Structural_geology.
- Fissility_(geology) wikiPageWikiLink Cleavage_(geology).
- Fissility_(geology) wikiPageWikiLink Compaction_(geology).
- Fissility_(geology) wikiPageWikiLink Fabric_(geology).
- Fissility_(geology) wikiPageWikiLink Foliation_(geology).
- Fissility_(geology) wikiPageWikiLink Metamorphic_rock.
- Fissility_(geology) wikiPageWikiLink Phyllite.
- Fissility_(geology) wikiPageWikiLink Rock_(geology).
- Fissility_(geology) wikiPageWikiLink Sedimentary_rock.
- Fissility_(geology) wikiPageWikiLink Shale.
- Fissility_(geology) wikiPageWikiLink Silicate_minerals.
- Fissility_(geology) wikiPageWikiLink Slate.
- Fissility_(geology) wikiPageWikiLink File:Muzeum_Złota_w_Złotoryi_fyllit_Panenska_Hůrka_21.07.2011_p.jpg.
- Fissility_(geology) wikiPageWikiLinkText "Fissile".
- Fissility_(geology) wikiPageWikiLinkText "Fissility (geology)".
- Fissility_(geology) wikiPageWikiLinkText "fissile".
- Fissility_(geology) wikiPageWikiLinkText "fissility".
- Fissility_(geology) wikiPageUsesTemplate Template:Geology-stub.
- Fissility_(geology) wikiPageUsesTemplate Template:Reflist.
- Fissility_(geology) subject Category:Structural_geology.
- Fissility_(geology) comment "Fissility or Fissionability (American English) refers to the property of rocks to split along planes of weakness into thin sheets. This is commonly observed in shales, which are sedimentary rocks, and in slates and phyllites, which are foliated metamorphic rocks. The fissility in these rocks is caused by the preferred alignment of platy phyllosilicate grains due to compaction, deformation or new mineral growth. A highly fissile rock splits easily along the cleavage.".
- Fissility_(geology) label "Fissility (geology)".
- Fissility_(geology) sameAs Q5455231.
- Fissility_(geology) sameAs Fissilitat_(geologia).
- Fissility_(geology) sameAs m.0fvg_y.
- Fissility_(geology) sameAs Q5455231.
- Fissility_(geology) wasDerivedFrom Fissility_(geology)?oldid=618256674.
- Fissility_(geology) depiction Muzeum_Złota_w_Złotoryi_fyllit_Panenska_Hůrka_21.07.2011_p.jpg.
- Fissility_(geology) isPrimaryTopicOf Fissility_(geology).