A major principle of stratigraphy stating that within a sequence of layers of sedimentary rock, the oldest layer is at the base and that the layers are progressively younger with ascending order in the sequence. * O The law of relative dating O The law of original horizontality The law of superposition O The law of cross-cutting O The law of lateral continuity

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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A major principle of stratigraphy
stating that within a sequence of
layers of sedimentary rock, the
oldest layer is at the base and that
the layers are progressively
younger with ascending order in
the sequence.
The law of relative dating
The law of original horizontality
The law of superposition
The law of cross-cutting
O The law of lateral continuity
Transcribed Image Text:A major principle of stratigraphy stating that within a sequence of layers of sedimentary rock, the oldest layer is at the base and that the layers are progressively younger with ascending order in the sequence. The law of relative dating The law of original horizontality The law of superposition The law of cross-cutting O The law of lateral continuity
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