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Deciphering Earth’s History

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WJEC GCSE Geology Theory Paper - external assessment 75% 1½hr - 100 marks An on-screen non-tiered written paper consisting of compulsory structured data and stimulus response questions, marked by WJEC. Controlled internal assessment 25% 50 marks Option 1 Directed investigation of a virtual location presented as 'field' notes and a written report. Marked by centre. Or Option 2 Directed investigation of an actual location presented as field notes and a written report. Marked by centre. “The Present is the key to the past” “While the end goal lies, kilometers, days, weeks, years away, it is today that counts. It is what you do today, right now, this moment, on this day that you will look back on with pride, from which you will derive immediate joy and in the end satisfaction, regardless of how it turns out.” Pete Vordenberg (US National Cross Country Skiing Coach)
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Page 1: Deciphering Earth’s History

WJEC GCSE Geology

Theory Paper - external assessment 75% 1½hr - 100 marks

An on-screen non-tiered written paper consisting of compulsory structured data and stimulus response questions,

marked by WJEC.Controlled internal assessment 25% 50 marks

Option 1Directed investigation of a virtual location presented as 'field'

notes and a written report. Marked by centre.Or

Option 2Directed investigation of an actual location presented as field

notes and a written report. Marked by centre.

“The Present is the key to the past”

“While the end goal lies, kilometers, days, weeks, years away, it is today that counts. It is what you do today, right now, this moment, on this day that you will look back on with pride, from which you will derive immediate joy and in the end satisfaction, regardless of how it turns out.”

Pete Vordenberg (US National Cross Country Skiing Coach)

Page 2: Deciphering Earth’s History

Why is paper white?

What does the centre of the Earth look like?

Is the Earth’s atmosphere getting hotter?

How do we know?

Page 3: Deciphering Earth’s History

Deciphering Earth’s History

Learning Objectives:To understand the principle of

UniformitarianismTo know the concepts of original horizontality, comformability and

superposition.

Page 4: Deciphering Earth’s History

Langstone Rock

Page 5: Deciphering Earth’s History

Geology is one of the newest Sciences.In the mid 1600’s it was thought that the Earth

was only a few thousand years old – many people accepted this as it fitted with Christian Beliefs.

By the seventeenth and eighteenth centuries a ‘doctrine of catastrophism’ was developed.

Catastrophists believed that the Earths landscape had been developed primarily by sudden and great worldwide catastrophies.

Geology in the Past

Page 6: Deciphering Earth’s History

Birth of Modern Geology

Modern Geology began in the late 1700’s with James Hutton’s publication of his Theory of the Earth.

He put forward a fundamental principle that is the pillar of geology today: Uniformitarianism.

It simply states that, the physical, chemical and biological laws that operate today have also operated in the geological past.

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Some Fundamental Principles

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The Law of Superposition

A Dane, Nicolaus Steno, working in Italy in 1669, recognised a series of events in an outcrop of sedimentary rock layers. He applied a very simple rule, the law of superposition.

The law states that in an undeformed sequence of sedimentary rocks, each bed is older than the ones above it and younger than the ones below it.

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The Grand Canyon

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The Principle of Original Horizontality

Steno is also credited with recognising the importance of another basic principle, called the Principle of Original Horizontality.

The layers of sediment are generally deposited in a horizontal position.

Thus, if we observe rock layers that are flat, it means they have not been disturbed and still have their original horizontality.

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Page 12: Deciphering Earth’s History

Anticline and Syncline

Page 13: Deciphering Earth’s History

Law of Cross-Cutting Relationships

A rock or structure must be younger than any rock or structure it cuts across. For example a dyke must be younger than the sediments pierced by it.

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What was the order of events?

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What happened here?

Page 16: Deciphering Earth’s History

Unconformities

An unconformity represents a long period during which deposition ceased, erosion removed previously formed rocks, and then deposition resumed.

There are three types of Unconformity;An Angular UnconformityA DisconformityA Nonconformity

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Angular Unconformity

Siccar Point in Scotland

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Disconformity

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Nonconformity


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