Editing 1874: Geologic Faults

Jump to: navigation, search

Warning: You are not logged in. Your IP address will be publicly visible if you make any edits. If you log in or create an account, your edits will be attributed to your username, along with other benefits.

The edit can be undone. Please check the comparison below to verify that this is what you want to do, and then save the changes below to finish undoing the edit.
Latest revision Your text
Line 13: Line 13:
 
A {{w|Fault (geology)|fault}} is a geologic feature involving a planar fracture with displacement in a large mass of rock, including the boundaries of two {{w|tectonic plates}}.
 
A {{w|Fault (geology)|fault}} is a geologic feature involving a planar fracture with displacement in a large mass of rock, including the boundaries of two {{w|tectonic plates}}.
  
===Real geologic faults===
+
====Real geologic faults====
 
;Normal fault
 
;Normal fault
 
In a {{w|Fault (geology)#Dip-slip faults|normal fault}}, the hanging wall (the lower wall; right) moves downward relative to the footwall (the upper wall; left). The Earth's crust is extended in this type of fault.  
 
In a {{w|Fault (geology)#Dip-slip faults|normal fault}}, the hanging wall (the lower wall; right) moves downward relative to the footwall (the upper wall; left). The Earth's crust is extended in this type of fault.  
Line 23: Line 23:
 
A {{w|thrust fault}} is when older rocks are pushed (or thrust) on top of younger rocks. The angles are typically lower (more horizontal) than in reverse faults.
 
A {{w|thrust fault}} is when older rocks are pushed (or thrust) on top of younger rocks. The angles are typically lower (more horizontal) than in reverse faults.
  
===Fictional faults===
+
====Fictional joke 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.
 
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.
 
;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}}.
 
;Squeezed-bar-of-soap fault
 
;Squeezed-bar-of-soap fault
 
Two plates seem to be moving towards each other, while a third smaller plate is squeezed between them and pushed upwards, much as a slippery bar of soap might pop up when squeezed between two hands.
 
Two plates seem to be moving towards each other, while a third smaller plate is squeezed between them and pushed upwards, much as a slippery bar of soap might pop up when squeezed between two hands.
Line 34: Line 34:
 
;Brio fault
 
;Brio fault
 
{{w|Brio (company)|BRIO}} is a company from Sweden that makes wooden toys, including train sets. The Brio fault seems to be two tectonic plates which join together like the Brio train track pieces do. (However, this join is obvously incorrect because of the height difference.)
 
{{w|Brio (company)|BRIO}} is a company from Sweden that makes wooden toys, including train sets. The Brio fault seems to be two tectonic plates which join together like the Brio train track pieces do. (However, this join is obvously incorrect because of the height difference.)
;(Title text) Torn-bag-of-potato-chips-where-the-tear-is-rapidly-growing fault
+
;Torn-bag-of-potato-chips-where-the-tear-is-rapidly-growing fault
 
The title text refers to when a bag of chips gets a tear in it. When this happens, any further stress on the bag, such as reaching in to get more chips, can easily increase the size of the tear, sometimes very quickly. It would be frightening to live near a fault that behaved like this{{Citation needed}} because it could cause major seismic events very quickly. If you were close enough to the fault, you might be afraid that the crack would grow underneath you, causing you to fall into the bag of chips — or, rather, the Earth.
 
The title text refers to when a bag of chips gets a tear in it. When this happens, any further stress on the bag, such as reaching in to get more chips, can easily increase the size of the tear, sometimes very quickly. It would be frightening to live near a fault that behaved like this{{Citation needed}} because it could cause major seismic events very quickly. If you were close enough to the fault, you might be afraid that the crack would grow underneath you, causing you to fall into the bag of chips — or, rather, the Earth.
  
 
==Transcript==
 
==Transcript==
 +
{{incomplete transcript|Do NOT delete this tag too soon. Lacks small description for each item.}}
 
:[The comic shows nine different schematic views to present geographic faults and some more.]
 
:[The comic shows nine different schematic views to present geographic faults and some more.]
  
Line 44: Line 45:
 
:[Two planes with a slip fault drifting against each other from left and right.]
 
:[Two planes with a slip fault drifting against each other from left and right.]
 
:Reverse fault
 
:Reverse fault
:[Two planes moving sideways away from each other.]
+
:[Two planes moving sideways.]
 
:Transverse fault
 
:Transverse fault
  
Line 68: Line 69:
 
{{comic discussion}}
 
{{comic discussion}}
  
[[Category:Geology]]
+
[[Category:Science]]
 
[[Category:Puns]]
 
[[Category:Puns]]

Please note that all contributions to explain xkcd may be edited, altered, or removed by other contributors. If you do not want your writing to be edited mercilessly, then do not submit it here.
You are also promising us that you wrote this yourself, or copied it from a public domain or similar free resource (see explain xkcd:Copyrights for details). Do not submit copyrighted work without permission!

To protect the wiki against automated edit spam, we kindly ask you to solve the following CAPTCHA:

Cancel | Editing help (opens in new window)