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Unformatted text preview: ateral Folds Layers can Layers be folded be Anticline Syncline Anticline Syncline 08.05.a Domes and Basins Dome Basin 08.05.a Monocline 08.05.a Geometry of Folds
g in H e Limb
08.05.b Limb Plunging Plunging fold fold Axial Surface Upright fold Asymmetric fold Overturned fold Rock Cleavage
Cleavage Cleavage plane plane 08.06.a Foliation
08.06.b Schistosity Gneissic foliation Flattened pebbles Foliation from shearing Lineation
Oriented minerals Stretched crystals Shearing marks
08.06.c Other Metamorphic Features Preserved features Preserved Shear zone Folded pebbles Folded Deformed foliation 08.06.d Metamorphism of Sedimentary Rocks
Increasing metamorphism of shale Increasing 08.07.a Slate Schist Sandstone Sandstone becomes quartzite quartzite Limestone Limestone becomes marble marble Gneiss...
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- Fall '08