Relative Age Dating Lab

Relative Age Dating Lab




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Lab 7: Relative Dating and Geological Time - A Practical . . .
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Relative Age Dating Lab .docx - Relative Age Dating Lab . . .
SCIN100 -- Relative Age Dating Lab Flashcards | Quizlet
LAB 3: Relative and Absolute Ages in Geology
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We can tell the relative ages of rocks (for example, whether one rock is older than another) based on their spatial relationships; we can use fossils to date sedimentary rocks because we have a detailed record of the evolution of life on Earth; and we can use a range of isotopic techniques to determine the actual ages (in millions of years) of igneous and metamorphic rocks .
RELATIVE AGE DATING LAB INTRODUCTION Scientists have good evidence that the Earth is very old, approximately four and one-half billion years old . Scientific measurements, such as radiometric dating use the natural radioactivity of certain elements found in rocks to help determine their "absolute age " . Scientists also use direct evidence from observations of the rock layers themselves to help determine
Relative Age Dating Lab Purpose: In this activity you will learn to determine the sequence of geologic events from cross- sections of strata (rocks) in a given area . It is a bit of a mind-puzzler, so have fun!
In Figure 5, the age sequence of the rocks, from oldest to youngest is ________ . D, H, A, C, G, F, I, B, E . The geologic history revealed in Figure 4 is as follows: Layers G,C, A and F were deposited . A normal fault B cut layers G, C, A and F . A period of erosion followed which created an unconformity .
There are two parts to this lab exercise A . Part 1is on absolute age determinations using radioactive isotopes and their daughter products in geological materials . In Part 2you will use the principles of relative dating to determine sequences of geological events as indicated by the layers and structures in the rocks .
In addition to determining the relative age of the different strata, you need to determine the relative age of unconformities, cross-cuttings and inclusion . Procedure B: Below are cross-sections from four different locations in New York State . Reconstruct the complete sequence of events .
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Topic: Relative age dating of geologic cross sections Grade Level: 7-14 Content Standard: National Earth and Space Science Standard Content Objective: This exercise will introduce your students to the concept of relative age dating , and allow them to practice their new skills by determining the age sequence of geologic events in a cross section .
The principle of superposition is simple, intuitive, and is the basis for relative age dating . It states that rocks positioned below other rocks are older than the rocks above . The image below shows a sequence of Devonian-aged (~380 Ma) rocks exposed at the magnificent waterfall at Taughannock Falls State Park in central New York . The rocks near the bottom of the waterfall were deposited first . . .
33 Principles of Relative Dating Cindy Kearns and Elizabeth Johnson . Relative Dating . Placing of events in the order in which they occurred without any relationship to the actual time during which any one event occurred is known as relative dating . It is a qualitative way of describing the sequence of events .
SW Science 10 Unit 6 Relative Dating Worksheet Name: _____ Student #: _____ 6 .2 Geologic Time 6 .2 .2 Relative Dating The Law of Superposition In any undisturbed sequence of strata, the oldest layer is at the bottom of the sequence, and the youngest layer is at the top of the sequence . The Cross-Cutting Law
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