Section 21.2 relative-age dating of rocks

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Nicolaus Steno introduced basic principles of stratigraphythe study of layered rocks, in Relative Dating of Rocks Layers Age of Earth • Early s: years old • Today: billion years old How did scientist come up with this number? 1) Relative. Explain why scientists need a geologic time scale.

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This preview shows page 1 - 2 out of 2 pages. Relative Dating of Rocks Layers Age of Earth • Early s: years old • Today: billion years Easy comparison of fossil ages Geologic Principles a) Original Horizontality – sedimentary rocks Guided Reading Question Chapter Provincial forests and Yoho National Park are neighbours to the west, while Kootenay National Park is located to the south and Kananaskis Country to the southeast.

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Chapter 1: The Nature of Science Section 1. Apply the principles for determining relative age to interpret rock sequences. The concept of relative-age dating places the ages of rocks and the events that formed them in order, but without .. Section Study Guide. Ultrasound estimate of rocks.

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We think you have liked this presentation. Name Class Date SECTION Relative–Age Dating of Rocks Chapter 21 Earth Science: SECTION Relative–Age Dating of Science. For complaints, use another form.

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Relative age dating of rocks C 1 section 2 telling relative age of. the matching of unique rock outcrops or fossils exposed in one geographic region to similar outcrops or fossils exposed in other geographic regions. key bed .

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Start studying Earth Science: Chapter 21, Section 2 - Relative-Age Dating. The principle that sedimentary rocks are deposited in HORIZONTAL or nearly horizontal Earth Science Chapter Discovering Earth's History Review 13 Terms.

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Section Relative-Age Dating. Objectives. Describe uniformitarianism and explain its importance to geology. Apply geologic principles to inter- pret rock.

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View from ECONOMICS at University of Toronto. Vocabulary Strata multicoloured layers of rock Unit 3.

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Relative-Age Dating and. Absolute-Age Dating. FOLDABLES Use this Foldable with Sections and As you learn about age dating of rocks, summarize.


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