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Precambrian Rohbaugh
Precambrian Rohbaugh

... • Archean: Water vapor forms oceans, oxygen starts to be made by photosynthetic organisms • Proterozoic: Significant oxygen in atmosphere, massive drop in carbon dioxide ...
Earth`s crust, the surface layer of the planet, is
Earth`s crust, the surface layer of the planet, is

... and unbroken. The forces that rage inside the planet have fractured this brittle layer. Some of these fractures, called faults, lie beneath the surface of the crust. Other faults, however, have ruptured the surface, cracking the crust into various-sized blocks of rock. These blocks dip and rise alon ...
3_GC1_Plates2_09
3_GC1_Plates2_09

... 3. HOW DOES THE FORMATION OF NEW OCEAN FLOOR RELATE TO THE DEFORMATION OF THE EARTH’S ...
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8.3 Destruction from EQ 8.4

... of the destruction was caused by fires that started when gas and electrical lines were cut. ...
8. Mid-Ocean Ridge
8. Mid-Ocean Ridge

... • A plate boundary where two tectonic plates slide, grind, and past each other in opposite directions along a transform fault. (also known as transform fault boundary, sliding boundary, or conservative plate boundary). • San Andres Fault in California is an example of transform ...
101 The Earth - BegaTAFE-GeneralEd-CGVE
101 The Earth - BegaTAFE-GeneralEd-CGVE

... into soft, brown coal. If the pressure and heat were more intense, or continued for a longer period of time, black coal would be produced. Black coal is a solid rock, much harder than brown coal. Most of the coal found on Earth formed between 15 and 350 million years ago, making coal very, very old. ...
International Year of Planet Earth – Activities and Plans in Mexico
International Year of Planet Earth – Activities and Plans in Mexico

... “Standing on Archimedes” and “Foucault and the Climate”. Books are distributed to school children, with more than 10,000 copies given free of first volumes. Other publications include the special issues of El Faro science magazine edited by the National University, with last issue published and dist ...
ES Chapter 14 Study Guide
ES Chapter 14 Study Guide

... Approximately how much of Earth’s surface is covered by land? Approximately how much of Earth’s surface is covered by water? Approximately when did the ocean become an important area of study? Which ocean has the greatest average depth? The largest of Earth’s oceans is __________________ Where trenc ...
Science Study Guide - Thomas C. Cario Middle School
Science Study Guide - Thomas C. Cario Middle School

... 7. Compare and contrast oceanic and continental crust Oceanic-basalt, more dense, thinner. Cont-granite, less dense, thicker 8. Compare and contrast lithosphere and asthenosphere Lith- rigid layer of Earth’s surface including crust and upper mantle. Asthn-flowing layer (hot rock) beneath lithosphere ...
Moving Plates: Restless Earth
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QUAKE NOTES

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NASC 1100
NASC 1100

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9 Geography Investigating Australia`s Physical Environments Term 1
9 Geography Investigating Australia`s Physical Environments Term 1

... Earth’s mantle. Heating from the Earth’s core causes the semi-molten material in the mantle to churn in currents. These currents, called convection currents, carry the crustal plates up to as much as 15 centimetres per year. The movement of the plates is known as the theory of continental drift. Sci ...
Plate Tectonics Reading
Plate Tectonics Reading

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... Tertiary rocks (= oldest rocks) These are associated with rver flood plains, coastal plains, and shallow sea environments that occurred due to fluctuating sea levels. Oldest rocks are Late Cretaceous marine rocks (70-82 million years old) outcrop in Bienville parish. These are highly fossiliferous m ...
Geosphere in Motion Pre-Post Test
Geosphere in Motion Pre-Post Test

... The rock found in California is igneous, but the rock found in Massachusetts is sedimentary California is located on the boundary of two crustal plates, but Massachusetts is not. The rock under California is soft, but the rock under Massachusetts is hard. California is located on a continental plate ...
Notes_-_Earths_Layers
Notes_-_Earths_Layers

...  Exists under oceans  Average thickness is 7 Km  Chemical composition: rocks rich in iron and magnesium silicates  Common rock types: basalt, obsidian, gabbro  Rocks are more dense, darker in color than continental crust Mantle  Lies underneath the crust  2900 Km thick  The lithosphere is a ...
Rock Formations: How Igneous, Sedimentary, and Metamorphic
Rock Formations: How Igneous, Sedimentary, and Metamorphic

... Rock Formations: How Igneous, Sedimentary, and Metamorphic Rock Types are Formed Investigating how the 3 basic rock types are created. There are 3 basic types of rock: igneous, sedimentary, and metamorphic rocks. Igneous rock Igneous rock is formed by the cooling and solidification of magma or lava, ...
Chapter 28 Notes
Chapter 28 Notes

... of continents and other geological events like earthquakes and volcanoes.  The term tectonics means construction or building.  The theory of plate tectonics, stated in 1965, refers to the movement of giant pieces of solid rock on Earth’s surface called tectonic plates.  In 1915, Alfred Wegener (1 ...
Abstract template - Institute for Planetary Materials
Abstract template - Institute for Planetary Materials

... scientists working in the area of geophysical observation of deep-seated rocks (seismic tomography and MT imaging), material science of fluids including high-pressure experiments and molecular dynamics on chemistry and physical properties of fluids and microstructure of fluid-bearing rocks, and forw ...
Plate Tectonic Quiz Name: Label the four layers of the Earth Use the
Plate Tectonic Quiz Name: Label the four layers of the Earth Use the

... 17. Draw and label a subduction zone, then describe what it is in writing. ...
Mineral Resources and Geology
Mineral Resources and Geology

Making a Scale Model of the Earth`s Interior
Making a Scale Model of the Earth`s Interior

... Making a Scale Model of the Earth’s Interior Information gained from the study of earthquake waves that pass through the Earth’s interior has helped scientists to develop a picture of what it may be like inside the Earth. In this activity, you will make a scale model of the Earth that shows what the ...
Desk Copy Changing Earth Common Assessment
Desk Copy Changing Earth Common Assessment

... a. A large amount of magma or lava along a plate boundary b. Areas of extreme heat and pressure c. Landforms found along the Ring of Fire d. A vent in the Earth’s lithosphere where magma erupts. 25. At a convergent boundary between oceanic and continental crust, where do the volcanoes form? a. they ...
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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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