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Geological Time © NASA
Outline of Talk Part 1. The Age of the Earth Practical: Saltiness of Ocean Part 2. The History of the Earth Practical: Dawn of a New Age Part 3. Radiometric dating
Age of the Earth: Eternity ,[object Object],[object Object],[object Object],© NASA
Age of the Earth: The Bible 4004 BC ,[object Object],[object Object],[object Object],Bishop Ussher  (1581-1656) en.wikipedia.org/wiki/Image:Ussher.jpg
Age of the Earth: Experiments Comte de Buffon (1707-1788) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],iron ball
Age of the Earth: The Sun http://en.wikipedia.org/wiki/Image: Hermann_von_Helmholtz.jpg http://upload.wikimedia.org/wikipedia/en/9/93/Cropped_Earth_with_Sunburst.PNG Hermann von  Helmholtz (1821-1894) ,[object Object],[object Object],[object Object],[object Object]
Age of the Earth: More Physics http://en.wikipedia.org/wiki/Image:Lord_ Kelvin_photograph.jpg Lord Kelvin (1824-1907) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Geothermal  gradient
Age of the Earth: Geology Charles Lyell (1797-1875) ,[object Object],[object Object],[object Object],[object Object],http://en.wikipedia.org/wiki/Image:Charles_Lyell.jpg http://en.wikipedia.org/wiki/Image:Colorado_River_edit.jpg
Age of the Earth: Sea Salt ,[object Object],[object Object],[object Object],[object Object],[object Object],Obituary Notices of F.R.S. ,  1 , 260 (1933)   John Joly (1857-1933) http://www.bigfoto.com/miscellaneous/photos-16/index.htm salt  crystals
Age of the Earth: Assumptions ,[object Object]
Exit Slip ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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History Of Age Of The Earth

  • 2. Outline of Talk Part 1. The Age of the Earth Practical: Saltiness of Ocean Part 2. The History of the Earth Practical: Dawn of a New Age Part 3. Radiometric dating
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Editor's Notes

  1. Presenter notes: Planet Earth is more than 4500 million years old (that is, 4.5 billion years old). Such a vast abyss of time is hard to comprehend. When geologists talk about this kind of ‘deep time’ they use the term geological time to distinguish geological ages from the shorter timescales involved in human history. In this talk we will learn about geological time and how geologists first discovered the deep history of our planet. Background notes: One way to convey the vastness of geological time is to use the analogy of a 24 hour clock. If the earth was formed at midnight, then life did not appear until 06:00, the first animals and plants only made it onto land as late as 22:00, and humans evolved about 23:59, less than one minute before midnight.
  2. Presenter notes: There are three parts to this talk. In the first part we will learn about early ideas concerning the age of the Earth. It was through trying to work out the age of the Earth that geological time was first discovered. In Exercise 1, you will have a go at calculating the age of the Earth using a nineteenth century method (now considered incorrect) based on the saltiness of the ocean. In the second part we will learn about how geologists divide up geological time into different eons, eras, periods and epochs based on fossils and other evidence. This is important for sorting out the order that events occurred through the history of the Earth. In Exercise 2, you will investigate whether humans have altered the planet to such an extent that we are now entering a new geological age. In the final part, we will explore how a twentieth century technique called radiometric dating revolutionized our understanding of the age of the Earth. As a result we will see how geologists can now precisely date events like the extinction of the dinosaurs rather just talk about the relative order that events occurred.
  3. Presenter notes: So let’s begin by looking at early ideas about the age of the Earth. As we do so, its worth reminding ourselves that this fundamental question did not arise for many of the earliest societies. In Hindu thought and especially in the classical Greek world most people thought the Earth was eternal. For Greek philosophers like Aristotle time was a circle and there was no beginning or end. To him, the question of the age of the Earth was entirely irrelevant.
  4. Presenter notes: In a sense, thinking about the age of the Earth began with birth of Judaism and the belief in a God that had created the world out of nothing. Following the rise of Christianity, interest in God’s creation increased further and most early attempts to establish the age of the Earth were based on the Bible. Scholars used the chronological records in the Bible, together with dates found in other Middle Eastern literature to establish the amount of time between the creation of Adam and the birth of Jesus. The first person known to attempt this kind of calculation was Theophilus of Antioch in AD169 but other notable attempts were made by the physicist, Sir Isaac Newton (1643-1727), and most famously by Bishop James Ussher (1581-1656). All these calculated dates were roughly the same (as they relied on the same method) but Ussher’s date of 4004 BC became so popular that it was printed as a marginal note in the Book of Genesis. Background note: Although often ridiculed today, in their time, these Biblical calculations were the height of good academic scholarship (see Stephen Jay Gould, "Fall in the House of Ussher." Natural History 100 (November 1991): 12-21 ). That said, creationist groups that promote a Young Earth today (often citing Ussher’s 4004 BC) are examples of bad scholarship. They ignore or distort the advances in understanding that have accumulated since Ussher’s day.
  5. Presenter notes: Following the Renaissance and the birth of modern science, thoughts about the age of the Earth moved away from Biblical evidence. Instead it became popular to rely on the new science of Physics for answers. In 1760, a French naturalist called Comte de Buffon, aka Georges Louis Leclerq (1707-1788), hypothesized that the Earth had originated as a fiery ball after a comet had collided with the Sun. He experimented by heating iron balls of different sizes and then measured how long they took to cool down. Using this information, he scaled up to the much larger size of the Earth and predicted that would have taken about 75,000 years for the planet to cool down from a molten state. This seemed like an eternity to the people of Buffon’s day who were used to hearing that the Earth was only 6,000 years old based on the Bible.
  6. Presenter notes: By the mid-nineteenth century, physicists were proposing ingenious new ways to date the age of the Earth. In 1858, a German scientist, Hermann von Helmholtz (1821-1894) started to think about the origin of the Sun. He thought that the Sun had formed by the contraction of a nebula of gas and dust. He calculated that if would have taken about 20 million years for the Sun to shrink to its current diameter and brightness. Therefore the Earth could be no younger than 20 million years.
  7. Presenter notes: In 1862, William Thomson (1824-1907), aka Lord Kelvin, tried a different approach based on Physics. Kelvin knew that the temperature of the Earth increased by 1 degree of Fahrenheit for every 50 feet you went into the ground. He also assumed that the temperature of the early Earth had been around 7000 degrees of Fahrenheit when molten. Applying his knowledge of how fast heat is conducted through rocks he calculated that it would have taken around 20 million years for the Earth to cool to its present state. The fact that two independent approaches had arrived at roughly the same answer gave Physicists a lot of confidence that they were right. However, as we will see later their age calculations were quite wrong because they assumed that the Earth was steadily losing heat. In fact the discovery of radioactivity in the early twentieth century showed that the Earth was also producing some heat. Therefore the Earth must have been much older than allowed by Lord Kelvin’s calculations
  8. Presenter notes: One group of scientists who had a hunch that Lord Kelvin’s age of the Earth was far too young were the geologists. The geologist Charles Lyell (1797-1875) thought that the key to understanding the age of the Earth might lie in the way that mountains slowly erode down. Lyell thought that the rate at which the erosion and deposition of sediment occurs had stayed more or less constant through geological time. If he was correct and ‘the present was the key to the past’ then it must have taken many hundreds of millions of years to form the vast repository of sediment seen in the geological record, much longer than the ages allowed by Lord Kelvin and the Physicists. Background notes: Through the nineteenth century there was many attempts to use this approach to estimate the age of the Earth. To do this calculation one needed to know the total thickness of sediment on the Earth’s surface and also the average rate at which sediment accumulates today. However, it proved enormously difficult to get hard numbers for either of these figures. The main problem was than sediment accumulates at widely differing rates in different environments so in the deep sea a single millimetre of mud might take a thousand years to build up whereas in an active river channel, a metre of sand might be deposited in a few hours. These problems made geological estimates of the age of the Earth seem very inaccurate compared to the precise numbers put forward by the Physicists.
  9. Presenter notes: At the end of the nineteenth century, a new approach to understand the age of the Earth was put forward by the Irish geologist, John Joly (1857-1933). This approach relied on Edmund Halley’s work on the saltiness of the ocean. Halley (who is more famous for his comet) had earlier shown how salt is weathered out of rock on land and carried by rivers to the oceans, where it gradually builds up. In 1899, Joly argued that if you knew how salt was in the ocean and you knew how much salt was being added each year by rivers then you could work out the time when there was no salt in the the oceans, and hence the age of the Earth. After several attempts the figure he finally came up with was an age ranging between 80-150 million years. Unfortunately, what Joly didn’t realize is that salt doesn’t simply accumulate in the oceans over time. Rather there are geological processes that are constantly taking salt out of the oceans. Hence, Joly’s age was far too low.
  10. Presenter notes: As we have seen, all the methods put forward in the nineteenth century to figure out the age of the Earth relied on certain assumptions that couldn’t necessarily be proven. Kelvin assumed the Earth was steadily cooling from a molten state, Lyell assumed that the rate of sedimentation had been constant through history, and Joly assumed the saltiness of the ocean was being added to year after year. This meant that all these estimates of the age of the Earth were highly uncertain.
  11. Presenter notes: As we have seen, all the methods put forward in the nineteenth century to figure out the age of the Earth relied on certain assumptions that couldn’t necessarily be proven. Kelvin assumed the Earth was steadily cooling from a molten state, Lyell assumed that the rate of sedimentation had been constant through history, and Joly assumed the saltiness of the ocean was being added to year after year. This meant that all these estimates of the age of the Earth were highly uncertain.