The image on the left shows modern mud cracks. The image on the right shows mud cracks preserved in ancient sedimentary rock. The processes that formed cracks in a dried-up puddle are assumed to be the same that formed the mud cracks in the ancient sedimentary rock. The idea that physical processes we observe today also operated in the past, at roughly comparable rates, is called the Principle of Uniformitarianism Principle of Original Horizontality Principle of Cross-Cutting Relations Principle of Laterial Continuity Principle of Faunal Succession

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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The image on the left shows modern mud cracks. The image on the right shows mud
cracks preserved in ancient sedimentary rock. The processes that formed cracks in a
dried-up puddle are assumed to be the same that formed the mud cracks in the
ancient sedimentary rock. The idea that physical processes we observe today also
operated in the past, at roughly comparable rates, is called the
Principle of Uniformitarianism
Principle of Original Horizontality
Principle of Cross-Cutting Relations
Principle of Laterial Continuity
Principle of Faunal Succession
Transcribed Image Text:The image on the left shows modern mud cracks. The image on the right shows mud cracks preserved in ancient sedimentary rock. The processes that formed cracks in a dried-up puddle are assumed to be the same that formed the mud cracks in the ancient sedimentary rock. The idea that physical processes we observe today also operated in the past, at roughly comparable rates, is called the Principle of Uniformitarianism Principle of Original Horizontality Principle of Cross-Cutting Relations Principle of Laterial Continuity Principle of Faunal Succession
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