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Lecture 2.5 - St. Mark`s Boise
Lecture 2.5 - St. Mark`s Boise

... • Caused by rising hot magma near the earth’s core while cooler magma near the crust sinks. This rising and falling of magma of different temperatures set up these currents the plates move on. • Convection currents are the driving force of plate movement. ...
Internal Assessment Resource
Internal Assessment Resource

... Taupo Volcanic Zone. The reasons for the types of magma produced needs to be explained. It is assumed that the geological processes of weathering and/or erosion are discussed in relation to the formation of the TVZ current landforms. For grade differentiation, holistic judgement of student presentat ...
Why Earthquakes Occur
Why Earthquakes Occur

... carefully, because they tell us that the Earth has already shifted in this area. That means another shift is likely. Seismographs are set up in these areas to record any vibrations from the Earth. Hundreds of earthquakes can happen each year, but they are so small that humans cannot feel them. Howev ...
Oreo Cookies and Plate Tectonics
Oreo Cookies and Plate Tectonics

... do you notice about the cookie edges? _________________________________________________________ _________________________________________________________ (You can feel and hear that the “plates” do not slide smoothly past one another, but rather stick then let go, stick then let go. The cracking sou ...
Petrology
Petrology

...  Rarely reacts with acid  Usually has no layering  Usually made of two or more minerals  May be light or dark colored  Usually made of mineral crystals of ...
Earthquakes - Fair Lawn Public Schools
Earthquakes - Fair Lawn Public Schools

... • 4. Seismic waves slow down as they travel through hot material. From this information, scientists model convection currents in Earth's mantle. • 5. A seismometer measures and records how much the ground moves and can be used to determine distance seismic waves travel. • 6. A seismogram is a graph ...
HANDOUTAWITHANSWERS
HANDOUTAWITHANSWERS

... boundary with two pieces of eggshell? Why or why not? What results when two continental crusts collide? Give an example of one that began millions of years ago and is still going on today. They buckled upward. This represents a convergent (continental collision); no; because they are the same densit ...
the File
the File

... America "fit" together. Structural, fossil and mineral evidence seemed to support Wegener's Continental Drift Theory but it was not accepted by the scientific community. In the 1960's, scientists began to realize that there might be a connection between continental drift, earthquakes and volcanoes. ...
Practice Exam #1
Practice Exam #1

... 4. Why must a planet with divergent plate boundaries also have convergent plate boundaries? 5. How does the temperature of a substance affect its volume, density and buoyancy? 6. What is the energy source and driving mechanism for the movement of plates? Describe how this process works. 7. Two ident ...
Chapter 10 study guide
Chapter 10 study guide

... He believed that if the continents had been joined that fossils of the same plants and animals could be found in areas that had once been connected. In addition, the age and types of rocks in both of these areas were very similar.  Glaciation Geologists discovered layers of debris from ancient glac ...
Ch 17 Reading
Ch 17 Reading

Portraying the Earth
Portraying the Earth

... continents embedded within them This idea was first suggested by a German scientist Alfred Wegener in 1915. He suggested the theory of Continental Drift, based on the congruity of the shapes of the continents across the Atlantic Ocean He also looked at shapes of both South America and Africa and ...
Changing Earth - Ms. Stinson's Science Class
Changing Earth - Ms. Stinson's Science Class

... Earth's crust and part of the upper mantle are broken into sections. These sections, called plates, move on a plasticlike layer of the mantle. The plates can be thought of as rafts that float and move on this layer. Composition Of Earth's Plates Plates are made of the crust and a part of the upper m ...
Continental Drift
Continental Drift

...  Theoretical ...
What do we teach - Pender County Schools
What do we teach - Pender County Schools

... Activity 3 in Project Earth Science: Divergent boundary Geology http://www.nsta.org/store/ Plate Tectonics or Mid-Ocean Ridge Search internet for other edible tectonics Isostasy ...
Lec05_ch05_earthmoon
Lec05_ch05_earthmoon

... • Will the ozone layer, which is now being depleted, naturally replenish itself? • Who was the first person to walk on the Moon and on what Apollo space mission did this landing occur • Do we see all parts of the Moon’s surface at some time throughout the lunar cycle of phases? • Does the Moon rotat ...
How are seismic waves generated-Elastic rebound theory Describe
How are seismic waves generated-Elastic rebound theory Describe

... movements that occur beneath the earth's surface. They could occur on a Convergent Boundary, Divergent Boundary or a Transform Fault. ...
File - GEOLOGY ROCKS!
File - GEOLOGY ROCKS!

... As we define the history and geology of the Appalachian Mountains we’ll also focus on how human history was shaped by the geological events that created these mountains ...
Plate Evidence 09
Plate Evidence 09

... The Theory of Plate Tectonics • Explains all evidence • Similar to continental drift, but more complex • Earth’s crust is composed of “plates” that make up the crust under the ocean and on the continents • Continents DO NOT float on the oceans • Plate boundaries do not always occur at the edges of ...
Cenozoic Earth History
Cenozoic Earth History

... Evolution of the Atlantic Coastal Plain Following Maximum Advance of the Tejas Transgression • The Tejas Transgression began in the Paleocene, peaked in the Eocene, having advanced as far inland as where Augusta, Columbia, Raleigh, Richmond, and Philadelphia are now located ...
REINFORCEMENT
REINFORCEMENT

... Use the words in the box to fill in the blanh ...
Name:
Name:

...  What do inner/terrestrial planets have in common, and how do they differ from gas giants?  What do most outer planets (gas giants) have in common (5 things)?  Why was Pluto declassified as a planet? What is Pluto’s classification now?  Compare asteroids, comets, and kuiper belt objects (locatio ...
tectonic plate boundaries
tectonic plate boundaries

... Answer this question…  How do we know so much about the mantle and the core? – Seismic waves, or vibrations produced from earthquakes, travel at different speeds through the Earth. Their speed depends on the density and composition of the material they pass through. – Traveling through a solid wil ...
Geography - Sanskriti School
Geography - Sanskriti School

class outline - WordPress.com
class outline - WordPress.com

... Students answer one or more short answer questions (e.g., slides 3,4,5) related to video content to allow instructor to confirm comprehension. ...
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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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