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Building a Theory
Building a Theory

... • 1 Collection of facts based on observations and measurements • 2. Develop possible explanations (hypotheses) (a stories) – Multiple working hypotheses ...
Weathering, Erosion, and Plate Tectonics
Weathering, Erosion, and Plate Tectonics

... volumes of heated and molten rock moving around the earth’s interior form massive solid plates that move extremely slowly across the earth’s surface.  Tectonic plates: huge rigid plates that are moved with convection cells or currents by floating on magma or molten rock. ...
Plate Tectonics PPT
Plate Tectonics PPT

... Plate Tectonics • The theory explaining how the movements of earth’s “TECTONIC PLATES” or “moving plates” create the geologic events like earthquakes, volcanoes and tsunamis. • Lithospheric Plates- giant puzzle pieces connecting on the surface of earth. – These sit on top of mantle so they can move ...
Plate Tectonics
Plate Tectonics

... Convection Currents • Hot magma in the Earth moves toward the surface, cools, then sinks again. • Creates convection currents beneath the plates that cause the plates to move. ...
Wegener and his Theory of Continental Drift
Wegener and his Theory of Continental Drift

... opposite shores of oceans and which contain evidence of events over extended intervals of geologic time. For example, studies of rocks from many localities on the eastern coast of South America and western coast of Africa (Figure 3) suggest that these regions had remarkably similar histories for the ...
Hall of Planet Earth Educator`s Guide
Hall of Planet Earth Educator`s Guide

For Creative Minds - Arbordale Publishing
For Creative Minds - Arbordale Publishing

... skin). It is very thin compared to everything else. If you could dig very deep, you could dig through the crust. But nobody can dig that deep—not even oil drillers or miners. The next layer is the Earth’s mantle (represented by the kiwi’s green flesh). It is a dense, hot layer of semi-solid rock. Th ...
t.7. the earth`s dynamics.
t.7. the earth`s dynamics.

... Nearly 90 % of these rest in the Ring of Fire, a band circling the _____ ______. Their location is no accident. While the Earth’s surface looks stable, its crust is made up of a net of* slabs of rock, like puzzle pieces, but constantly shift. Where these ______ ______ interact, volcanoes often form. ...
Plate boundaries - MrD-Home
Plate boundaries - MrD-Home

Teacher`s Name: ___Julie
Teacher`s Name: ___Julie

... Students will take notes from a Power Point Formative Assessment Lesson Topic: Introduction to the correct names and the properties of each. over the Earth’s layers. Students will Writing to learn Writing to demonstrate learning the layers of the earth, their complete a diagram of the Earth’s layers ...
GEOLOGY 11 EXAM I STUDY QUESTIONS What are the
GEOLOGY 11 EXAM I STUDY QUESTIONS What are the

... Why does the asthenosphere transmit seismic waves but does not generate earthquakes? If the asthenosphere does not generate earthquakes, why are the deepest recorded quakes as deep as 700 km? What is a Wadati-Benioff zone? What is a Richter magnitude for an earthquake? What is the global distributi ...
Plate tectonics
Plate tectonics

... People once thought that the oceans and the continents were formed by shrinkage from when the Earth cooled down after being formed. Alfred Wegener proposed something different. Consider Africa and South America: These continents look like they “fit” together. They also have similar rock patterns and ...
Plate Tectonics and the cycling of Earth materials
Plate Tectonics and the cycling of Earth materials

... motion, the older volcano is carried away and a new one forms. The map on the right shows the Hawaiian Island chain of volcanic islands. Kauai, the oldest Hawaiian island, is 10 million years old ...
Plate Tectonics and the cycling of Earth materials
Plate Tectonics and the cycling of Earth materials

... motion, the older volcano is carried away and a new one forms. The map on the right shows the Hawaiian Island chain of volcanic islands. Kauai, the oldest Hawaiian island, is 10 million years old ...
PLATE TECTONICS
PLATE TECTONICS

... • Paleomagnetism magnetic minerals align and dip with Earth's internal magnetic field lines – Steeper dip angles indicate rocks formed closer to the magnetic poles ...
the physical world - worldgeographywhs
the physical world - worldgeographywhs

... • It is also the _____________ of the Solar System's four _____________ planets & sometimes referred to as the world or the _________ Planet • The planet is home to ___________ of species including __________ (some smart & some not so smart) • ___________ interacts with other objects in ___________, ...
anddestructiveforces_powerpoint
anddestructiveforces_powerpoint

... land itself is totally changed. You can see scars across the landscape. Those scars appear when one block of land has moved compared to another. Roads often change their placement. They either become uneven or just crack. Streams can also change course. Sometimes rocks can fall and block the stream. ...
Grade 8 Science
Grade 8 Science

... areas where plates separate. Has helped build continental divides in areas where plates have collided and mountain building occurs. ...
Programme title: Awesome Forces
Programme title: Awesome Forces

... In this programme, students explore the inner workings of our planet. They experience what it is like at the centre of the Earth and uncover the layers of the Earth. Students piece together the puzzle of plate tectonics before investigating the causes of earthquakes and volcanoes. Finally, they disc ...
Name Date Period ______ Plate Tectonics Study Guide 1. Explain
Name Date Period ______ Plate Tectonics Study Guide 1. Explain

The Appalachian Story sheet
The Appalachian Story sheet

... 12. The ancient seabed contains other clues within the sands and the clays: _____________________. 13. Generally the sediments are approximately _________ million years old in this region, formed in the ancient ocean called "__________________________". 14. The breccia was originally formed by under ...
Outline Miller Chapter 14 Review Chapter 14: Nonrenewable
Outline Miller Chapter 14 Review Chapter 14: Nonrenewable

... earths it produces and may soon need to important some types of rare earths from other countries to meet its industrial needs a. The transition from developing to developed Geological processes determine the quantity and location of a nonrenewable mineral resource in the earth’s crust, but economics ...
Plate Tectonics Study Guide for Earth Science Chapter 17
Plate Tectonics Study Guide for Earth Science Chapter 17

... Give evidence to explain why we believe Antarctica was warmer in the past. Be able to explain 4 supporting evidences for the theory of Continental Drift. Be able to explain seafloor spreading and give supporting evidence for it. Study all notes from Layered Earth B “Tectonic Plates,” Power Point and ...
Wanganui High School
Wanganui High School

... Mid ocean ridge within the earth. A mid-ocean ridge is formed when hot magma rises through the upper mantle in the ocean at plate boundaries. The magma cools rapidly in the cold sea water, forming underwater mountains. Eg the MidAtlantic ridge. The process is also called sea floor ...
Pre/Co-Requisite Challenge for Field Courses
Pre/Co-Requisite Challenge for Field Courses

... Taking  the  Pre/Co-­‐Requisite  Quiz   All  students  without  the  pre/co-­‐requisite  MUST  meet  with  or  email  an  instructor  of   the  field  course  to  discuss  preparing  for  the  quiz  and  registering  for  the  class.  It ...
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History of geology



The history of geology is concerned with the development of the natural science of geology. Geology is the scientific study of the origin, history, and structure of the Earth. Throughout the ages geology provides essential theories and data that shape how society conceptualizes the Earth.
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