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Earth`s Interior
Earth`s Interior

... learn about the earth’s interior by studying seismic waves  Velocities of P & S waves vary as they travel through the earth  Travel ...
PHYSICAL GEOLOGY
PHYSICAL GEOLOGY

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Class Agenda Week of 8-13 Oct 2007

... Scientists measure Earth’s geological and biological events using the _____________________ , which is divided into ___________________ and _____________________. The ___________________________ is the name of a period of rapid change during which the ancestors of most animal groups emerged. A layer ...
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Layers Directed Reading

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GEOL1033-SQS07R
GEOL1033-SQS07R

... 11. Referring to the question above, what is the name of the boundary between these two subdivisions? ________________________ 12. How many subdivisions of Earth's core are there? 1, 2, 3, 4, or 5? 13. Which subdivision of the Earth's core is molten? ...
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... 3. The L_______________ is made up of the C_______________ and the upper part of the M_______________. 4. The hot softer part of M___________ that the L_______________ sits on top of is called the A_______________. 5. Materials that are L__________ D_______________ rise to Earth’s surface. 6. Materi ...
Professor Bruce Watson
Professor Bruce Watson

... The first 700 million years of Earth’s existence (the Hadean Eon) are widely regarded as the most geodynamically vigorous period in the history of our planet. It has been variously inferred that during this time the Earth: 1) collided with a Mars-sized-object; 2) formed a deep magma ocean; 3) grew t ...
Geology 3
Geology 3

... Geology: Essential Question #2: What impact does the movement of tectonic plates have on the development of the Earth’s crust? Earthquake- A sudden release of pressure caused by plate movements. Seismology- The study of earthquakes. Seismograph- An instrument that determines the location and strengt ...
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Earth Formation: Accretion

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The Planet Oceanus

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Question you are trying to answer. Ex

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What on EARTH is going on here? (Mrs. Rodriguez tells the story of

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Plate Tectonics Review The rock at the Earth`s surface forms a

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... There are eight planets that circle the sun: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. All the planets orbit the Sun. The inner planets are the four planets closest to the Sun: Mercury, Venus, Earth, and Mars. They are all small and made up of solid, rocklike materials. The ...
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Applying Concepts 33. a. Index fossils in each sequence can be

... time on Earth, and have a broad geographical distribution. 19. There is no complete stratigraphic sequence of rock layers that shows the whole history of Earth. It had to be pieced together using sequences from many locations around the world. Index fossils are used to fit the pieces of the puzzle t ...
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Section 1.2 A View from Earth

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4 Lithosphere Research

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Go here for PPT

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Chapter 8: Geologic Time

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OUTLINE (GEOS 418)

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Name date

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Age of the Earth



The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.
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