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Siccar Point
Siccar Point is a prominent geological site in Scotland known for its angular unconformity between older, tilted layers of rock and younger, horizontal layers.
Unconformity
A boundary where two different layers of rock meet, signifying a time when erosion occurred or new layers were not formed.
Original Horizontality
The principle that most sediments and many volcanic units are deposited in layers that originally are more or less horizontal.
Lateral Continuity
A geological principle that states layers of sediment initially extend laterally in all directions; in other words, they are laterally continuous.
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