The Geologist as Detective.  THE PRINCIPLES USED IN DETERMINING THE ORDER IN WHICH ROCKS WERE FORMED.

Slides:



Advertisements
Similar presentations
Fossils, Relative Time and Absolute Time
Advertisements

Who’s First? What is relative dating?
Unit 2 Lesson 2 Relative Dating
Unit 2 Lesson 2 Relative Dating
Relative and Absolute Dating
Relative Dating : Which Came First?
FOSSILS.
A Trip Through Geologic Time
Sci. 3-2 Relative Dating: Which Came First?
FINDING RELATIVE AGE. What is relative age?  1. The age of a rock compared to the ages of other rocks.  Absolute age-the EXACT age of rock (add to your.
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.
Fossils Fossil are the preserved remains or traces of living things. They form when living things die and are buried by sediment. They are usually.
Section 4.2  The relative age of a rock is its age compared to the ages of other rocks.  Ex. Mrs. Herrscher is older than her sister and brother. 
The Relative Age of Rocks
Unit 5: Age of the Earth Objective:
Finding the Relative age of Rocks
The Relative Age of Rocks 10-2
The relative age of rocks
Chapter 9 – 1 FOSSILS.
Dating Rock Layers.
Studying the Past Fossils, Relative Time and Absolute Time.
PRESERVED REMAINS OR TRACES OF AN ORGANISM THAT LIVED IN THE PAST
The Relative Age of Rocks
Key Ideas State the principle of uniformitarianism.
Beginning with a History of Geology. 1. Catastrophism 1. Earth was shaped by dramatic events called catastrophes 2. Like MASSIVE earthquakes, floods,
Earth’s History.
Do Species Change Over Time?
Book G Chapter 4 – Section 1
 The composition, structure, position and fossil content of Earth’s rocks provide information about Earth’s geologic history.  The geologic history dates.
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.
Aim Aim: How do we know the age of the Earth? I. Earth’s History Uniformitarianism A. Uniformitarianism – the principle that most of the geologic events.
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.
Bell Ringer How do fossils form? Where are they found and describe each?
Relative Dating Superposition Original Horizontality Faulting Tilting/Folding Intrusions Unconformities Geologic Columns Rock Puzzles.
Jump to first page Geologic Time Chapter 34. Jump to first page Dating rocks n Relative dating F Compare events and put them in order based on their sequence.
The Geologist as Detective Chapter 6 : Interpreting Geologic History.
I can: describe methods used to assign
2 Types.  Relative Dating  Absolute Dating  1. Law of superposition – youngest layer on top; oldest layer on bottom.
Fossil/Age of Rock Notes Use the Purple book to get notes for fossils and relative age of rock notes. – Write the word and definition for all of the vocab.
Unit 3 Review Please see pages in your book for more information *This study guide is just to get you started studying– please look at your notes.
Earth’s History How do we know about it?. What is Uniformitarianism? Uniformitarianism: –Is a theory developed by the Scottish geologist, James Hutton,
Geologist interpret Earth’s history by studying sedimentary rocks Relative Dating.
Earth History Dating geologic events like volcanic eruptions, uplift, subsidence, deposition, impacts, intrusion, ice ages, etc.
Fossils Fossils are the remains, impression, or other evidence preserved in rock of the existence of life Fossils can be preserved as: –Molds –Casts –Original.
The Rock and Fossil Record
Relative Dating: Which Came First?
The Law of Superposition Any method of determining whether an event or object is older or younger than another event. Comparing rock layers or fossils.
Earth’s History.
A Trip Through Geologic Time
Law of Uniformitarianism
GEOLOGIC HISTORY.
Discovering Earth’s History
A Trip Through Geologic Time
EARTH’S HISTORY Relative Dating.
Earth’s Materials and Processes-Part 3 Fossils & Relative Dating
Earth’s Materials and Processes-Part 3 Fossils & Relative Dating
The History of Earth Relative Dating Absolute Dating
Earth’s History Review
A Trip Through Geologic Time
Earth’s History: The Law of Superposition Guided Notes
Relative Dating 12/7/2018.
Original Horizontality
A Trip Through Geologic Time
Original Horizontality
SEVEN PRINCIPLES Of GEOLOGY 1. UNIFORMITARIANISM:
Geologic Time 1.
Earth’s History: The Law of Superposition Guided Notes
A Trip Through Geologic Time
Relative Dating Write on RIGHT Side.
5.2 Faults, Folds & Fossils Unit 5: Earth’s History January 29, 2012
Presentation transcript:

The Geologist as Detective

 THE PRINCIPLES USED IN DETERMINING THE ORDER IN WHICH ROCKS WERE FORMED

 The idea that processes that shape the Earth, such as volcanoes, earthquakes, deposition and erosion, are the same processes that occurred in the geologic past

 THE PRINCIPLE IS BASED ON THE FACT THAT SEDIMENT IS USUALLY DEPOSITED IN HORIZONTAL LAYERS  IF SEDIMENTARY ROCKS LIE AT AN ANGLE THEN SOME TECTONIC FORCES MUST HAVE ACTED ON THE ROCK

 THAT SEDIMENTARY ROCKS ARE OLDEST ON THE BOTTOM AND YOUNGEST ON TOP  THIS IS TRUE AS LONG AS NO TECTONIC FORCES HAVE TURNED THE LAYERS UPSIDE DOWN OR ON THEIR SIDE

 ROCK MUST FIRST EXIST BEFORE ANYTHING CAN HAPPEN TO IT  THEREFORE AN INTRUSION IS YOUNGER THAN THE ROCK IT HAS ENTERED  INTRUSION: WHEN MAGMA SQUEEZES INTO OR BETWEEN LAYERS OF PRE-EXISTING ROCK  EXTRUSION: WHEN MOLTEN ROCK FLOWS ONTO THE EARTH’S SURFACE, THEN COOLS  INCLUSION: OLDER ROCKS SURROUNDED BY MOLTEN MAGMA

 ONE PIECE OF ROCK FOUND IN ANOTHER ROCK MUST BE OLDER THAN THE ROCK IT IS FOUND IN  A PEBBLE FOUND IN CONGLOMERATE IS OLDER THAN THE CONGLOMERATE

 WHERE LAYERS OF ROCK ARE MISSING  IF THE SURFACE OF THE ROCK WAS ERODED SOME TIME IN ITS HISTORY  UNCONFORMITIES ARE GAPS IN GEOLOGICAL TIME

 FOLDS: BENDS IN ROCK LAYERS PRODUCED BY CRUSTAL PLATE MOVEMENTS  FAULTS: BREAKS IN ROCK WHERE MOVEMENT HAS OCCURRED  FOLDING OR FAULTING CAN LEAD TO EXCEPTIONS TO THE LAW OF SUPERPOSITION

 FOSSILS: PRESEVED REMAINS OR TRACES OF LIVING THINGS  RELATIVE AGE: COMPARATIVE AGE; AGE EXPRESSED AS BEFORE OR AFTER OTHER EVENTS WITHOUT SPECIFYING THE AGE IN UNITS  ABSOLUTE AGE:AGE OF A ROCK UNIT, FOSSIL OR EVENT EXPRESSED IN UNITS OF TIME, SUCH AS YEARS

 Casts and Molds- shapes/outlines left behind; these are COPIES of originals.  Petrifaction- mineral replacement of organic material  Amber and Ice- organisms “frozen” in time  Trace Fossils- footprints, fecal pellets, burrows  Impressions- 2-Dimensional leftovers

 NYS HAS FOSSILS OF CORAL AND WARM- WATER MARINE ORGANISMS, INDICATING THAT THE AREA WAS ONCE A TROPICAL SEA  IT ALSO HAS MORE RECENT FOSSILS OF WOOLY MAMMOTHS AND MASTODONTS, REVEALING THE COLD, SNOWY CLIMATE OF THE LAST ICE AGE