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***That definition would, of course, have resulted in a significantly different picture where the ''air'' is thicker than the ''ground'' only inside small areas around mid-ocean ridges. Mid-ocean ridges are where new crust is created and the plates are spreading apart; because the crust is new, it is hot and relatively less dense, causing it to float higher up than the surrounding crust. However, the lithosphere thickens over time as the crust cools, these areas have the thinnest "ground."
 
***That definition would, of course, have resulted in a significantly different picture where the ''air'' is thicker than the ''ground'' only inside small areas around mid-ocean ridges. Mid-ocean ridges are where new crust is created and the plates are spreading apart; because the crust is new, it is hot and relatively less dense, causing it to float higher up than the surrounding crust. However, the lithosphere thickens over time as the crust cools, these areas have the thinnest "ground."
 
***Because the lithosphere is comprised only in part of the crust, and in part of a cool, solid layer of mantle, an alternate definition of "ground" including only the crust (and not the mantle lithosphere) could have led to an alternate version of this map where air was thicker in all locations. The crust is rarely more than 70 km thick, still less than even the 80 km Air Force definition of the atmosphere.
 
***Because the lithosphere is comprised only in part of the crust, and in part of a cool, solid layer of mantle, an alternate definition of "ground" including only the crust (and not the mantle lithosphere) could have led to an alternate version of this map where air was thicker in all locations. The crust is rarely more than 70 km thick, still less than even the 80 km Air Force definition of the atmosphere.
**Although most authorities use the FAI definition of the Kármán line since it is the international organization of record for aeronautics, there are good scientific reasons for the U.S. Air Force definition.{{Citation needed}}
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**Although most authorities use the FAI definition of the Kármán line since it is the international organization of record for aeronautics, there are good scientific reasons for the U.S. Air Force definition {{Citation needed}}.
 
**The Kármán line is named for {{W|Theodore von Kármán}}, who originally calculated the height at which a vehicle would have to travel faster than orbital velocity to generate lift from wings (therefore making the vehicle a spacecraft in orbit rather an "air"craft using aerodynamics for flight).   
 
**The Kármán line is named for {{W|Theodore von Kármán}}, who originally calculated the height at which a vehicle would have to travel faster than orbital velocity to generate lift from wings (therefore making the vehicle a spacecraft in orbit rather an "air"craft using aerodynamics for flight).   
 
**Von Kármán originally calculated this height as 51.9 miles (83.6 km) - closer to the Air Force definition.   
 
**Von Kármán originally calculated this height as 51.9 miles (83.6 km) - closer to the Air Force definition.   

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