
MOVIE
Indiana Jones and the Dial of Destiny
A legend will face his destiny.
Finding himself in a new era, and approaching retirement, Indy wrestles with fitting into a world that seems to have outgrown him. But as the tentacles of an all-too-familiar evil return in the form of an old rival, Indy must don his hat and pick up his whip once more to make sure an ancient and powerful artifact doesn't fall into the wrong hands.
STORY RECAP
What happened before Indiana Jones and the Dial of Destiny?
Indiana Jones Collection
This recap covers
Includes spoilers for the films listed above.
KNOW BEFORE WATCHING
A few things worth knowing first
TERM
Antikythera mechanism
The Antikythera mechanism is an ancient Greek geared astronomical calculator, recovered from a shipwreck near the island of Antikythera. Dating to around the second or first century BCE, it modeled celestial cycles and could predict eclipses. The real artifact is not known to have any ability to enable time travel.
TERM
Archimedes
Archimedes was an ancient Greek mathematician, inventor, and scientist from Syracuse (c. 287–212 BCE). His work on geometry, buoyancy, and mechanics became foundational to later mathematics and science. He lived during the period when Rome fought for control of Syracuse.
TERM
Siege of Syracuse
The Siege of Syracuse (214–212 BCE) was a Roman military campaign against the Greek city of Syracuse in Sicily during the Second Punic War. The city resisted with formidable defenses, including machines traditionally associated with Archimedes, before it fell to Roman forces.
TERM
Temporal paradox
A temporal paradox is a logical inconsistency that can arise in stories about time travel, such as a traveler changing the past in a way that prevents their own journey. It is a philosophical and science-fiction idea, not an experimentally established effect of real time travel.
TERM
Continental drift
Continental drift is the historical idea that Earth’s continents have changed position over geological time. Modern plate tectonics explains this movement through the motion of lithospheric plates. The continents shift extremely slowly, generally by centimeters per year, rather than abruptly on a human timescale.