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Geology of the Hawaiian Islands
Geology of the Hawaiian Islands

... Meteorites and Moon rocks (that are thought to have had a very simple history since they formed), have been dated by up to 10 independent isotopic systems all of which have given the same answer. However, scientists continue to critically evaluate this data. ...
Michelle Mindick
Michelle Mindick

... oxygen   and   iron   form   rust   on   rocks.   Freeze-­‐thaw   cycles   occur   when   water   runs   into   cracks   where   it   then   freezes   and   expands,   causing   the  rock   formations  around   it   to   fracture.   After   ...
Marine Geology Final Exam Information and Review
Marine Geology Final Exam Information and Review

... Continental drift, seafloor spreading and Plate tectonics • What is Wegener's hypothesis of continental drift? • What observations did Wegener use to justify his hypothesis? • Why did geologists of Wegener’s time reject his continental drift hypothesis? • How can paleomagnetism studies tell us where ...
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unit 2 earth history - possible test questions

December Final 2013
December Final 2013

... According to Figure 10-1, what type of plate boundary occurs between the North American Plate and the Eurasian Plate? a. transform boundary b. divergent boundary c. convergent oceanic-continental plate boundary d. convergent oceanic-oceanic plate boundary ...
Earth*s Interior - Mr. Cramer
Earth*s Interior - Mr. Cramer

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The Earth-Mars-Moon System - Geophysical Journal International
The Earth-Mars-Moon System - Geophysical Journal International

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Atmosphere, Hydrosphere, and Lithosphere - ReneeASD

... can cause skin cancer and cataracts.  An excess level of UV rays could lead to the death of the phytoplanktons, that are an important component of the food web of the oceans. ...
Table of Contents - Milan Area Schools
Table of Contents - Milan Area Schools

... changes on Earth during the remote past. • Periods of geological history are marked by mass extinctions or by dramatic increases in diversity called evolutionary radiations. • Although the fossil record is fragmentary before 550 mya, it is still good enough to show that the total number of species a ...
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... • IT MAKES UP ABOUT 30% OF THE EARTH’S MASS. ...
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8th Grade Science Units

... A combination of constructive and destructive geologic processes formed Earth’s surface. - Earth’s surface is formed from a variety of different geologic processes, including but not limited to plate tectonics. ...
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Ch08_Geologic Time

... • Only useful for dating events from historic past and very recent geologic history – Carbon-14 is present in small amounts in all organisms – C-12/C14 ratio constant while alive – After organism dies C-14 no longer taken in ...
Earth`s Interior - Poster Project
Earth`s Interior - Poster Project

... Students are responsible for creating an informational poster about the layers of the Earth. The purpose is to identify the Earth’s layers and describe their physical characteristics (i.e. thickness, viscosity, temperature, etc.). Students are expected to successfully present information in a clear, ...
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... 5. Examine the diagram above. Which rock unit is the youngest? Explain.___________________________________________________________________ 6. In the disturbed layers of sedimentary rock shown above, which is older—layer D or intrusion 1? ______________________________________________________________ ...
Plate Tectonic Notes: Lab Science 9
Plate Tectonic Notes: Lab Science 9

... I can illustrate and describe the interior layers of the earth. ...
Ch. 7 Plate Tectonics Section 1 Inside the Earth
Ch. 7 Plate Tectonics Section 1 Inside the Earth

... Wegner’s theory of continental drift explained many puzzling facts, including the fit of the Atlantic coastlines of South America and Africa. Today’s continents were originally joined together in the ancient continent Pangaea. ...
Study Guide Chapter 2 – Minerals and Rocks GPS: S6E5. Students
Study Guide Chapter 2 – Minerals and Rocks GPS: S6E5. Students

... 2. A mineral is______________________, which means that it cannot contain materials that were once part of living things. 3. The repeating pattern of a mineral’s particles forms a solid called a ________________________. 4. _____________________ such as copper, silver, and gold are examples of miner ...
Chapter 1 Unit C
Chapter 1 Unit C

... What do you predict Earth will look like 200 million years from now?  The Atlantic Ocean is getting wider pulling North America and Europe farther apart.  The Pacific Ocean is getting smaller. ...
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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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