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Editing v0.34:Flow

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Fluids moving under '''[[pressure]]''' do not just move to adjacent tiles, they also trace a path through other full tiles of fluid trying to move to more distant tiles. Fluids moving under [[pressure]] can effectively teleport through other tiles that are already filled with fluid. When teleporting, fluids do not generate '''any''' flow, neither will they push objects around.
 
Fluids moving under '''[[pressure]]''' do not just move to adjacent tiles, they also trace a path through other full tiles of fluid trying to move to more distant tiles. Fluids moving under [[pressure]] can effectively teleport through other tiles that are already filled with fluid. When teleporting, fluids do not generate '''any''' flow, neither will they push objects around.
  
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When a fluid tries to move by pressure, it tries to trace a path through full 7/7 fluids going down, and horizontally, but ''not'' diagonally.  In this way it is like basic flow, except that pressure works faster; fluid from the source is teleported to the open space at the end, rather than having to wait for open space to open up at the source via normal flow. This is why, for example, diagonal squeezes in channels make water flow slower (they block pressure, forcing it to only spread out sideways), and why rivers and streams on the map are usually full of 7/7 water until close to the edge of the map where the rules of basic fluid motion are draining the water off the map while pressure teleports new water from the source all the way down to the end.
 
When a fluid tries to move by pressure, it tries to trace a path through full 7/7 fluids going down, and horizontally, but ''not'' diagonally.  In this way it is like basic flow, except that pressure works faster; fluid from the source is teleported to the open space at the end, rather than having to wait for open space to open up at the source via normal flow. This is why, for example, diagonal squeezes in channels make water flow slower (they block pressure, forcing it to only spread out sideways), and why rivers and streams on the map are usually full of 7/7 water until close to the edge of the map where the rules of basic fluid motion are draining the water off the map while pressure teleports new water from the source all the way down to the end.
  

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