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A third fault in a row from Li... oh and another!
Then a third fault in a row... but not a fourth.
Then a third fault let loose; that one is about 150 kilometers southwest of the first and parallel to it, and slipped as much as 21 meters along a rupture zone about 150 kilometers long.
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Here we focus on earthquake rupture behavior when a continuous planar main fault has a second fault branching off of it.
If one fault slips it might cause a second fault in the vicinity to slip earlier than expected, meaning you wait ages for one earthquake and then two show up at once (this bus analogy has no limits!).
During a field trip in 1998, the vent notion grew more plausible still as the two men discovered a second fault, which they named Kerna after a well-known spring, going north-south under the temple.
If the receiving player chooses to take a faulty first serve, play proceeds as if the serve had been good; otherwise the server must serve again; if he serves a second fault he loses his service to his partner or opponent, as the case may be.
Finally, a fourth fault slipped, the sides of the fault moving as much as 6 meters past each other along a 50-to-100-kilometer segment of fault in just 15 seconds.
A second fault trace can be observed running parallel to the Kumering segment within the high mountains west of the Liwa Basin.
They lie south of a second fault line running from Ballantrae towards Dunbar.
They lie south of a second fault line (the Southern Uplands fault) that runs from Girvan to Dunbar.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com