Editing 1874: Geologic Faults

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===Fictional faults===
 
===Fictional faults===
 
;Taffy fault
 
;Taffy fault
This appears to involve one tectonic plate, that is being stretched out like a piece of {{w|Taffy (candy)|taffy}}.  [https://s3.amazonaws.com/academia.edu.documents/41229455/Crustal_thinning_recorded_by_the_shape_o20160113-25699-1vca65l.pdf20160115-19908-17j9qxl.pdf?AWSAccessKeyId=AKIAIWOWYYGZ2Y53UL3A&Expires=1502469630&Signature=hcKl8ViPa2JrofM%2Bob7qu9TmjP4%3D&response-content-disposition=inline%3B%20filename%3DCrustal_thinning_recorded_by_the_shape_o.pdf Ductile crustal thinning] of this type actually occurs in rocks under tension at {{w|Brittle–ductile_transition_zone|sufficient depths}}.  Such deformation is not a fault, however, as there is no fracture along which movement takes place.
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This appears to involve one tectonic plate, that is being stretched out like a piece of {{w|Taffy (candy)|taffy}}.  [https://s3.amazonaws.com/academia.edu.documents/41229455/Crustal_thinning_recorded_by_the_shape_o20160113-25699-1vca65l.pdf20160115-19908-17j9qxl.pdf?AWSAccessKeyId=AKIAIWOWYYGZ2Y53UL3A&Expires=1502469630&Signature=hcKl8ViPa2JrofM%2Bob7qu9TmjP4%3D&response-content-disposition=inline%3B%20filename%3DCrustal_thinning_recorded_by_the_shape_o.pdf Ductile crustal thinning] of this type actually occurs in rocks under tension at [https://en.wikipedia.org/wiki/Brittle%E2%80%93ductile_transition_zone sufficient depths].  Such deformation is not a fault, however, as there is no fracture along which movement takes place.
 
;Splinted fault
 
;Splinted fault
 
This appears to be a normal or reverse fault that someone has attempted to fix in position by attaching a large splint, as you might with a broken bone. This is unlikely to prove effective.{{Citation needed}}
 
This appears to be a normal or reverse fault that someone has attempted to fix in position by attaching a large splint, as you might with a broken bone. This is unlikely to prove effective.{{Citation needed}}

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