GEOLOGIC HISTORY – PowerPoint PPT Presentation

Using student-created metaphors to comprehend geologic time. Journal of Geological Education. Purpose To introduce students to the vastness of geologic time and the concept of scale. Background Unraveling time and the Earth’s biologic history are arguably geology’s most important contributions to humanity. Yet it is very difficult for humans to appreciate time beyond that of one or two generations, much less hundreds, thousands, millions and billions of years. Perhaps we can only hope that students catch glimpses of our rich geologic heritage, particularly when most of our teaching is done in a classroom and not in a field setting. This exercise begins to make time more “three dimensional” and most importantly, students gain a better appreciation for geologic time and our Earth’s history. Instructions To better understand the concept of geologic time, have students produce a time-scale metaphor to share with the class that is true to scale and reflects some of the important events in the history of the Earth see list on the following page. Write an essay that:

Major Plates of the Lithosphere: Earth’s Tectonic Plates

Volcanic time markers – a layer of volcanic dust covering layers. When a violent eruption of a volcano occurs it may send dust high into the atmosphere where it can spread over the entire planet. It settles out of the air and forms a layer over wide regions at the same time. Asteroid impacts can have the same effect. The remians of the impact site in Mexico as seen by satellite imagery. Ways of Measuring Absolute Time Tree rings- every year a tree grows a new ring.

Earth History Timeline This activity has students create a timeline using 6 meters of cash register ticker tape. They will lightly color the 4 eras, label important events, and tape or paste index fossils from the New York earth science reference tables.

Our FREE worksheet on How the Earth was Formed is composed of a word searches puzzle combined with a fun hidden words puzzle game for kids. This fun yet educational printable Earth Science worksheet about How the Earth was Formed is totally FREE for you to download and use completely free and you can use the activity sheet as often as you need for homeschooling or in school!

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Daily Life

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The longest part of Earth’s history is called the. Cambrian; Precambrian; Mesozoic; Jurassic. The most recent ice age was during the Pennsylvanian Period. Pleistocene Epoch. Jurassic Park. Mesozoic Era. The youngest period of the Mesozoic Era is known as the You need to be a member to access free printables.

There are many methods employed by these scientists, interested in the old, to get to know the age of items. It is possible to tell the number of years ago a particular rock or archeological site had been formed. Two broad categories of classification methods are relative dating and absolute dating. Though using similar methods, these two techniques differ in certain ways that will be discussed in this article.

As the name implies, relative dating can tell which of the two artifacts is older. This is a method that does not find the age in years but is an effective technique to compare the ages of two or more artifacts, rocks or even sites. It implies that relative dating cannot say conclusively about the true age of an artifact. Absolute dating, on the other hand is capable of telling the exact age of an item using carbon dating and many other techniques that were not there in earlier times.

Relative dating makes use of the common sense principle that in a deposition of layers.

A History: ’s Word of the Year

Dating techniques Photo by: Bastos Dating techniques are procedures used by scientists to determine the age of an object or a series of events. The two main types of dating methods are relative and absolute.

GEOLOGY: EARTH’S HISTORY. Use the links below to explore available resources covering major concepts associated with the study of the history of the Earth. Resources in this section pertain to the formation and evolution of the Earth and how it has been discovered through the relative and absolute dating of rocks and fossils.

Scientists are rarely able to perform an experiment and obtain meaningful results within a time frame of one or two class periods. The following investigations require an extended period of time. In performing these projects, students should have the opportunity to observe change, gather data, record information, and make conclusions about the world around them.

Some students may use this list of viable investigations to generate their own project ideas, but the teacher should approve all projects before they are conducted. Although library research is an important aspect of nearly any scientific inquiry, students are strongly encouraged to make the gathering and analysis their own observations and data the primary emphasis of their long-term projects. Establish communication that will enable you to measure the size of the Earth through a computer link with a number of other schools.

Measure the quantity of air-borne particulate pollution at a number of locations. Correlation of your data with wind directions and time of year may also be appropriate. This is a good opportunity to show your skills in drawing isolines. Make a contour map of the area around your home. You may want to construct your own surveying instruments.


Hide This activity has benefited from input from a review and suggestion process as a part of an activity development workshop. This activity has benefited from input from faculty educators beyond the author through a review and suggestion process as a part of an activity development workshop. Workshop participants were provided with a set of criteria against which they evaluated each others’ activities.

For information about the criteria used for this review, see http: This page first made public: Mar 14, Summary In this classroom activity, students first use an interview with an older adult to construct a timescale.

Absolute Dating Practice Worksheet In this lesson well discuss both absolute and relative. Resources in this section pertain to the formation and evolution of the Earth and how it has been discovered through the relative and absolute dating of rocks and fossils.

In the very beginning of earth’s history, this planet was a giant, red hot, roiling, boiling sea of molten rock – a magma ocean. The heat had been generated by the repeated high speed collisions of much smaller bodies of space rocks that continually clumped together as they collided to form this planet. As the collisions tapered off the earth began to cool, forming a thin crust on its surface. As the cooling continued, water vapor began to escape and condense in the earth’s early atmosphere.

Clouds formed and storms raged, raining more and more water down on the primitive earth, cooling the surface further until it was flooded with water, forming the seas. It is theorized that the true age of the earth is about 4. The oldest rocks geologists have been able to find are 3.

Earth Day Printable Worksheets

The series has become a favorite of biology and environmental science classrooms for its amazing footage, groundbreaking quality, and depth of information. There are a total of 11 episodes of Planet Earth. The worksheets and student guides I have written for this series are all based on the BBC version starring David Attenborough as the narrator.

Biology Relative Dating Worksheet 1. How does the rock layer H compare to rock layer M? Why? 2. How come the rock layers on the left side of the picture do not line up with.

Much of northern New Jersey was covered with glaciers during the last ice age. While digging in this region, a geologists discovers bands of light- and dark-colored clays just below the surface. What are these sediments and how is the geologist most likely to determine their age? Identify the type of unconformity shown in the diagram below and describe how it formed.

Identify the two types of unconformities in the diagram below and describe how they formed. Contrast relative-age dating and absolute-age dating. Describe how geologists use index fossils. List the characteristics that make an index fossil. Radiometric dating has proved invaluable to scientists in the attempt to determine how long ago Earth formed.

Planet Earth Printable Outlines and Shape Book Writing Pages

Geologic Time, Geologic Processes Past and Present – Uniformitarianism And it seems like the time when after doubt Oh, never this whelming east wind swells But it seems like the sea’s return To the ancient lands where it left the shells Before the age of the fern; And it seems like the time when after doubt Our love came back amain. Oh, come forth into the storm and rout And be my love in the rain. We are reasonably adept at manipulating the physical world in terms of spatial relationships and physical parameters temperature, pressure , but one dimension of the physical world has so far escaped our manipulative powers TIME.

The time traveler’s machine from the ‘s George Pal adaptation of the H. Wells classic “The Time Machine”. Time is comprehensible to us as long as we can track it in terms of seconds, minutes, hours, days, and years, but once we go beyond the realm of our own time experience, our perception tends to get fairly vague.

Geologic History Reference Tables – The Mesozoic began million years ago and ended 65 million years ago – this is a time period of million years. If cm = 10 million years, then.

Acknowledgements Introduction his document discusses the way radiometric dating and stratigraphic principles are used to establish the conventional geological time scale. It is not about the theory behind radiometric dating methods, it is about their application, and it therefore assumes the reader has some familiarity with the technique already refer to “Other Sources” for more information.

As an example of how they are used, radiometric dates from geologically simple, fossiliferous Cretaceous rocks in western North America are compared to the geological time scale. To get to that point, there is also a historical discussion and description of non-radiometric dating methods. A common form of criticism is to cite geologically complicated situations where the application of radiometric dating is very challenging. These are often characterised as the norm, rather than the exception.

I thought it would be useful to present an example where the geology is simple, and unsurprisingly, the method does work well, to show the quality of data that would have to be invalidated before a major revision of the geologic time scale could be accepted by conventional scientists. Geochronologists do not claim that radiometric dating is foolproof no scientific method is , but it does work reliably for most samples.

It is these highly consistent and reliable samples, rather than the tricky ones, that have to be falsified for “young Earth” theories to have any scientific plausibility, not to mention the need to falsify huge amounts of evidence from other techniques. This document is partly based on a prior posting composed in reply to Ted Holden. My thanks to both him and other critics for motivating me. Background Stratigraphic Principles and Relative Time Much of the Earth’s geology consists of successional layers of different rock types, piled one on top of another.

The most common rocks observed in this form are sedimentary rocks derived from what were formerly sediments , and extrusive igneous rocks e. The layers of rock are known as “strata”, and the study of their succession is known as “stratigraphy”.

Geologic Time Scale Analogy

Early history[ edit ] In Ancient Greece , Aristotle BCE observed that fossils of seashells in rocks resembled those found on beaches — he inferred that the fossils in rocks were formed by living animals, and he reasoned that the positions of land and sea had changed over long periods of time. Leonardo da Vinci — concurred with Aristotle’s interpretation that fossils represented the remains of ancient life.

Steno argued that rock layers or strata were laid down in succession, and that each represents a “slice” of time. He also formulated the law of superposition, which states that any given stratum is probably older than those above it and younger than those below it.

in summary we may say that radiometric age determinations have helped us to scale our geologic column, helped us to determine the absolute age of the earth, and helped us realize that most of earth history is contained in the lowly precambrian.

Resources in this section pertain to the formation and evolution of the Earth and how it has been discovered through the relative and absolute dating of rocks and fossils.. Recording Dysfunctional Thoughts This form can be used to by clients to record and change dysfunctional thoughts and to see how these thoughts affect their moods. The 20thcentury art historian Andr BerneJoffroy stated, “What begins in the work of Caravaggio is, quite simply, modern painting. Baglione accused Caravaggio and his friends of writing and distributing scurrilous doggerel attacking him; the pamphlets, according to Bagliones friend and witness Mao Salini, had been distributed by a certain Giovanni Battista, a bardassa, or boy prostitute, shared by Caravaggio and his friend Onorio Longhi.

PDF ACT, meditation, happiness, depression, Compromising With Yourself This worksheet is intended to help people make compromises rather than be stuck between two extreme positions. PDF Your Perceptions About Yourself This worksheet asks clients to think about themselves objectively, based on the facts in their lives rather than on a subjective interpretation of their experiences..

How do we know when the dinosaurs died out? Mental health worksheets for adults This worksheet can be used in writing a CBT oriented treatment plan Click on the “Playlists” tab, then click “Create playlist”.

Prehistory (Origins & Stone Age)

Draw Figure 1 on the classroom board, or show students a suitable diagram or projected image. The inner core, mantle and crust are solid, and the outer core is molten, or liquid. The crust is the thinnest layer of the Earth and is the layer on which we live. The inner core, outer core and mantle experience extremely high pressures and temperatures. Most research about the Earth comes from studying the crust. Can you guess why?

1. How the Earth Was Made narrates a fascinating timeline of the Earth’s history. In small groups, ask students to create projects on posters or in PowerPoint format.

These major concepts are part of the Denver Earth Science Project’s Paleontology and Dinosaurs module Relative dating tells scientists if a rock layer is. Regents Earth Science Resources: DatePer Radiometric Dating Lab used to answer; both absolute and relative dating are help describe Earth events 3 points answer connects back to. Principles of Relative Dating Quiz Answers. Absolute and Relative Dating.

Earth science lab Earth science lab Earth science lab Earth science lab Using the diagram below, and the rules of relative dating, answer the follow Regents Earth Science Resources: Earth Science Relative Dating Answers. To introduce students to relative age dating.

Earth History, Dating the earth

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