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Volcano
Volcano

... Volcano-an opening in Earth’s crust through which lava may flow. Focus- the point where an earthquake starts. Lava- hot, melted rock that reaches Earth’s surface. Hot spot- a stationary location in Earth’s mantle where magma melts through a tectonic plate. 5. Epicenter- the point on Earth’s surface ...
Plate Tectonics U2L4 Cloze Name: ______ 1. The supercontinent
Plate Tectonics U2L4 Cloze Name: ______ 1. The supercontinent

... 1. The supercontinent called ________ formed 300 million years ago and began to break up 200 million years ago. 2. The process by which new oceanic lithosphere sea floor forms when magma rises to Earth’s surface, called ________ _________, occurs at mid-ocean ridges and solidifies, as older existing ...
questions
questions

... Alfred Wegener, a German who was educated as a meteorologist and geologist, was one of the first scientists to theorize about tectonic plates. Wegener suggested that past continents had drifted apart over time to form the present continents. This rearrangement of continents is known as continental d ...
plates - bethwallace
plates - bethwallace

... pudding in a pan you can watch the convection currents move in the liquid. When the convection currents flow in the mantle they also move the crust. The crust gets a free ride with these currents. A conveyor belt in a factory moves boxes like the convection currents in the mantle moves the plates of ...
How Can Continents Move?
How Can Continents Move?

... 12.1 Evidence for Continental Drift • The original supercontinent was named Pangaea by Wegener.  Wegener also realized that other evidence also supported his theory.  There were matching geologic features and rocks on different continents.  There were matching fossils, like Mesosaurus, on differ ...
The Earth Handbook
The Earth Handbook

... Why do you think scientists call Earth a ”living planet”? ...
Study Guide
Study Guide

... _____ 37. High pressure during metamorphism causes minerals to form layers in ____________ metamorphic rocks. (E3.1A, E3.1B) _____ 38. The process by which loose materials become solid rock, as by compaction or cementation. (E3.1A, E3.1B) _____ 39. High heat during metamorphism creates ___________ m ...
Lesson Plans for Bobby Mochman, Baker 6th Grade
Lesson Plans for Bobby Mochman, Baker 6th Grade

Earthquakes
Earthquakes

Theory Development
Theory Development

... Wegener’s theory was being dismissed because he did not have sufficient geological proof to explain why the continents moved, Holmes introduced his theory on thermal convection in the mantle. His theory explained that the molten material in the mantle moved in a circular current. As the magma heated ...
Study Guide Chapter 5 – Volcanoes GPS: S6E5. Students will
Study Guide Chapter 5 – Volcanoes GPS: S6E5. Students will

... 5. ________________________ from along the boundaries of Earth’s plates. 6. Many volcanoes form near ___________________ plate boundaries where oceanic plates collide. 7. A __________________________ is an area where material from deep within the mantle rises and then melts, forming magma. 8. Molten ...
unit 2 earth history lecture and study guide
unit 2 earth history lecture and study guide

WG3200 Unit 1 - Chapter 1 File
WG3200 Unit 1 - Chapter 1 File

... Earth's Crust • is not one continuous layer. • It is broken into many sections known as plates. • They all float and move on top of the molten asthenosphere. • When they push together and when they pull apart they create "tectonic forces". • Note; without this liquid layer called the asthenosphere ...
lightning gazette - Jerry Zucker Middle School Of Science
lightning gazette - Jerry Zucker Middle School Of Science

... This disease was found when French Canadian lumberjacks were in a forest. Whatever command was shouted at them, they followed it. There has been no cure found for it. Personally, I do not have a problem with it, but just who decided to call it Jumping Canadian Frenchman of Maine? ...
Rock Cycle - Duncanville ISD
Rock Cycle - Duncanville ISD

Worksheet: Volcanic eruptions
Worksheet: Volcanic eruptions

Using Earthquakes To Study the Earth`s Interior
Using Earthquakes To Study the Earth`s Interior

... How do they know, for example, that the lithosphere is rigid? Or that the asthenosphere is soft, like taffy? Or that the outer core is liquid? To understand how scientists study the earth’s interior, think about how they study the deepest parts of the ocean floor, which, like the depths of the earth ...
Geology 10 review- Test #1 Read Chapters 1
Geology 10 review- Test #1 Read Chapters 1

... asthenosphere; List and explain the evidence for plate tectonic theory ...
Glossary of Scientific Terms
Glossary of Scientific Terms

Chapter 14 Geology and Nonrenewable Mineral Resources
Chapter 14 Geology and Nonrenewable Mineral Resources

... 14-1 What are the earth’s major geological processes and hazards? CORE CASE STUDY: Gold extraction produces a tremendous amount of mining waste and can pollute the air and water. Cyanide is commonly used to extract gold and it is extremely toxic. In 2000 a cyanide leach pond was washed out in Romani ...
Evolving Earth: Plate Tectonics - Global Change
Evolving Earth: Plate Tectonics - Global Change

... seen in the velocity of energy waves over much if the Earth's volume. But other important observations can be made. The velocity changes do not always occur gradually. Relatively rapid increases occur at ~150 km, ~400 km and ~670 km. These steps must indicate that there are changes in material prop ...
I Can
I Can

... SC.O.E. 1.1 I can safely and appropriately use equipment, materials, organisms, and models. SC.O.E. 1.2 I can collect observations, data, and other evidence from a scientific investigation. I can use evidence collected from an experiment to explain what happened in the investigation. SC.O.E. 1.3 I c ...
Adlai E. Stevenson High School Course Description
Adlai E. Stevenson High School Course Description

... Describe how scientists measure earthquakes, identify their locations, and assess the damage caused. Describe how the processes of weathering, erosion, and mass wasting shape the features of the Earth. Describe the Earth’s grid system for identifying locations on the earth’s surface using the concep ...
Plate Tectonics - Nutley Public Schools
Plate Tectonics - Nutley Public Schools

... on opposite sides of the fracture move Ex. San Andreas Fault, California  Plate Tectonics: Theory that lithosphere is broken into segments/plates that float on the asthenosphere and is associated with earthquakes, and volcanic activity. ...
First Hour Exam, Fall, 2006
First Hour Exam, Fall, 2006

... d. mechanical weathering is the same as erosion, but chemical weathering is different from erosion because it involves chemistry. 20. Ice-wedging is a very effective mechanical weathering process because a. water expands as it freezes, pushing rocks apart from the inside. b. the ice grinds away at t ...
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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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