How to Match (Correlate) Rock Columns These 3 columns represent rock layers from 3 separate areas. Some columns may be missing layers due to erosion. No.

Slides:



Advertisements
Similar presentations
GEOLOGIC HISTORY THE RULES OF THE GAME
Advertisements

RELATIVE AGE DATING LAB ACTIVITY
Relative Dating of Rocks
Relative Dating : Which Came First?
Relative Dating and Sequencing Relative vs. Absolute Time Laws Unconformities Correlating Geologic Cross Sections.
RELATIVE TIME: When the age of rock is compared to the ages of other rocks or events in geological time. Can determine which layers are older than others.
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
Principles of Relative Dating
The Relative Age of Rocks 10-2
Concept Review – Geologic Time
1 Lab 08 ONLINE LESSON. 2 If viewing this lesson in Powerpoint Use down or up arrows to navigate.
Relative Dating of Strata. Relative Dating Determining relative ages of rocks or strata compared to another rock or strata. Can say which layer is older.
Topic: Relative Dating What is the usual order these meals are eaten during the day? A C B D.
Discovering Earth’s History Rocks Record Earth’s History 1. Rocks record geological events and changing life forms of the past. 2.Scientists have learned.
 The composition, structure, position and fossil content of Earth’s rocks provide information about Earth’s geologic history.  The geologic history dates.
Determining geological ages
Earth History- Table of Contents RELATIVE vs. ABSOLUTE LAWS UNCONFORMITIES GEOLOGIC SECTIONS.
Ch.6 Earth’s History. Who’s got the TIME? RELATIVE: order/sequence known, but not the actual date of occurrence. “Time Line” ABSOLUTE: actual date determined.
7.4.c Students know that the rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally.
Geologic Time and Relative Dating. Geologic Time Geologic time—beer goggles for geologists – Ex. geologically recent events Earth is 4.6 billion years.
Stratigraphy Stratigraphy is the branch of geology that deals with the arrangement of rocks in layers.
The Geologist as Detective Chapter 6 : Interpreting Geologic History.
Relative Time: Ages of events are placed in order of occurrence. No exact date is identified.  Ex. WWI and WWII  Ex. I am the second child in my family.
GEOLOGICAL TIME. GEOLOGY NEEDS A TIME SCALE An investigation of the history of Earth Understanding how features of landscape developed and formed Reconstructing.
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
Laws of Geologic History. Law of Superposition The oldest layer is at the bottom and the youngest layer is at the top. The oldest layer is at the bottom.
Geologic History Relative Dating. Birth of Modern Geology Began in the late 1700’s when James Hutton published his Theory of the Earth. He was the first.
An introduction Geologic Time. Which elephant is older????
Interpreting Earth’s Rocks to Determine Its Past History.
Catastrophism vs Uniformitarianism and Relative Age Dating
Earth’s History Introduction: The earth is about 4.6 billion years old. Much of its history is recorded in the rock. Observations of fossils, rock types,
Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc.
TOPIC 13 – GEOLOGIC HISTORY. DATING ROCKS There are two ways to get the ‘age’ of a rock: 1.) RELATIVELY ex) Rock layer ‘A’ is older than rock layer ‘B’
Relative Dating: Which Came First?
Aim: How can we describe major events in Earth’s history? Do Now: How did Early Earth’s atmosphere differ from modern Earth? Could early Earth support.
Sedimentary Rocks. Where do sedimentary rocks come from? Can you think of an example of sedimentary rock? What processes are involved in the formation.
Geologic Sequencing: The order of geologic events
Determining a Sequence of Geologic Events
GEOLOGIC HISTORY.
Discovering Earth’s History
Relative Age Quiz.
Unit 3 Earth History: Day 3 and 4
Earth’s History.
Geologic Time Notes Page 3
EARTH’S HISTORY Relative Dating.
Unit 2: Relative Dating - Part 2
Relative Time: Ages of events are placed in order of occurrence.
Time and Stratigraphy Basics
Geologic Time Notes Page 3
Interpreting Earth’s Rocks to Determine Its Past History
DO NOW Pick up notes and Review #12
Geologic History Relative Dating.
Geologic Principles Notes
How Old is Old? Geologic Time.
Unconformity:rock layers are missing because they were eroded away.
How to Match (Correlate) Rock Columns
The History of Earth Chapter 6 Sections 1 and 2.
The History of Earth Chapter 6 Sections 1 and 2.
How to Match (Correlate) Rock Columns
The History of Earth Chapter 6 Sections 1 and 2.
Relative Age of Rocks Activity
Wednesday DO NOW: Pick up the “Fossils” notes sheet up front
Relative Dating.
Aim: How can we explain relative dating?
Relative Age.
Based on fossil evidence, most scientists infer that
Geologic Time Notes By studying the characteristics of rocks and the fossils within them geologists can… interpret the environments in which the rocks.
The History of Earth Chapter 6 Sections 1 and 2.
Principles of Geological History
Monday DO NOW: Pick up the “Fossils” notes sheet up front
Presentation transcript:

How to Match (Correlate) Rock Columns These 3 columns represent rock layers from 3 separate areas. Some columns may be missing layers due to erosion. No single column represents a complete record. Your job is to line them up so a complete record of the region can be seen. The key to doing this is to find one or more layers present in all 3 columns that can be matched. In this example line up the conglomerate. Click for next frame.

According to the ‘law of supersposition’ the youngest rock layer will be on top and Youngest  the oldest layer will be on the bottom Oldest 

Here’s another example from a different regents exam. There are four columns from neighboring regions. The numbers represent different fossils found in the rock layers. Unconformities (buried erosional surfaces) indicate that material is missing. Try to find a fossil (number) that is common to all four columns and use it to line them up as in the previous example.

The fossil common to all columns is #7. The rock with fossil #6 is the youngest because it’s on top. Youngest  The rock with fossil #8 is the oldest. It’s on the bottom. The layer with fossil #3 is missing from the rightmost column due to erosion. Oldest 

Now try to reconstruct the geohistory of this region by listing the layers in order from the oldest to the youngest: Oldest  ,9 1 4 Youngest  6 Each column by itself is incomplete but by using information from all of them we can develop a complete history of a geologic region.

Let’s try one more..... Try to find a layer common to all 3 columns that you can use to help place these in the proper order. Note: the wavy lines marked x~~x are unconformities.

The sandstone layer is common to all the columns. Glacial deposits are on top. They are youngest Youngest  and gray limestone is on the bottom. It is oldest. Oldest  Why do you think the layer of black shale is thicker in column C than in column A? Not sure? Ask your teacher