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Earth`s Layered Structure
Earth`s Layered Structure

... in California or Italy. However, it was observed that P waves were bent around the liquid outer core beyond about 100 degrees away from an earthquake. The outer core also causes P waves that travel through the core to arrive several minutes later than expected. This region, where bent P waves arrive ...
Structure of the Earth
Structure of the Earth

... - must have been covered with glaciers at one time near south pole ...
Earthquakes
Earthquakes

... Forces In Earth’s Crust • How does stress in earth’s crust change earth’s surface? ...
Draw a cross section along the line of section (B
Draw a cross section along the line of section (B

... 4) Put ∆‘s on the surface of the cross-section to illustrate where you would expect volcanic activity to occur. 5) Identify and label the positions of the following features on the cross-section: a. Plate boundaries and their types (e.g., label the East Pacific Rise and indicate that it is a mid-oce ...
TECTONIC PLATE MOVEMENT Tectonic plates rest on the
TECTONIC PLATE MOVEMENT Tectonic plates rest on the

... Tectonic plates rest on the asthenosphere, a layer of soft, hot rock. Rock in this layer and in the mantle just below it moves by convection currents. You have seen convection currents if you have ever boiled a pot of water. The water at the bottom of the pot heats up, becomes less dense, and rises. ...
Earth`s Structure - We can`t sign you in
Earth`s Structure - We can`t sign you in

...  sea-floor spreading – This occurs under oceans where plates move apart and magma rises to the surface and cools to form new crust. ...
Continental Drift Theory and Plate Tectonics
Continental Drift Theory and Plate Tectonics

... Support For Continental Drift Theory • The Shapes Match • The continents look as if they were pieces of a giant jigsaw puzzle • The Plants and Animals Match • Identical fossil species along the coastal parts of Africa and South America. • Rocks Match - These broad belts match when the end of the co ...
Sea-Floor Spreading
Sea-Floor Spreading

Ch. 5 - Power Point Review
Ch. 5 - Power Point Review

... 2. Place seismograms on a time distance chart 3. Line up seismogram (P & S waves on time ...
TOPIC WORD DEFINITION Volcanoes aftershock An earthquake
TOPIC WORD DEFINITION Volcanoes aftershock An earthquake

CH. 12 Notes
CH. 12 Notes

... The impacts of this law was that people abused the law and began to build essentially whatever they wanted on the land. Also because of this law, mining companies have to pay very small taxes, around2.3% of their royalties The law has been tightened up over the last couple of ...
Plate Tectonics
Plate Tectonics

... a moving electric field. It is a dynamo! Earth’s magnetic field varies over time and it protects us from cosmic radiation ...
James Day Assistant Professor Email address:
James Day Assistant Professor Email address:

Plate Tectonics - Tuslaw Local School District
Plate Tectonics - Tuslaw Local School District

... What is Plate Tectonics? • Remember what a theory was? – A scientific Theory is a well tested concept that explains many observations. • So, the Theory of Plate Tectonics is … – Pieces of the Earth’s Lithosphere are in slow, constant motion, driven by convection currents in the mantle. ...
2. Key Question 1
2. Key Question 1

... Section 5.1 Forces in Earth’s Crust Reading Notes ...
the earth`s life support systems - sohs
the earth`s life support systems - sohs

... surface. • The earth’s interior consists of: – Core: innermost zone with solid inner core and molten outer core that is extremely hot. – Mantle: solid rock, under which is the asthenosphere that is melted pliable rock. – Crust: Outermost zone which underlies the ...
Document
Document

... western part of Africa will rotate clockwise and crash into Europe causing great mountain building, while the far eastern region of Africa will rotate eastward toward the Arabian peninsula. Australia will move farther north into the tropics, while New Zealand will move to the south of Australia. All ...
Formation of the Atmosphere
Formation of the Atmosphere

C1.7 Changes in Earth and atmosphere
C1.7 Changes in Earth and atmosphere

... C1.7.1 The Earth’s crust Recognise that the Earth’s crust, atmosphere and oceans are the only sources of minerals and other resources that humans need Outline the structure of the Earth and the relative sizes of the three major parts Describe how the crust and upper mantle are divided into tectonic ...
Name: : Earth Science Mr. Herman Exeter SHS Chapter 10.1
Name: : Earth Science Mr. Herman Exeter SHS Chapter 10.1

...  Describe the origins of magma  Explain the relationship between plate tectonics and volcanism, including intraplate volcanism Anticipatory Questions 1. How are the locations of volcanoes related to plate boundaries? ...
Unit 3: Plate Tectonics: Test Review
Unit 3: Plate Tectonics: Test Review

Rocks - Daslos Studios LLC
Rocks - Daslos Studios LLC

... ONTO THE EARTH’S SURFACE. EXTRUSIVE ROCKS LACK DISTINCT MINERAL GRAINS DUE TO RAPID COOLING OF LAVA AT OR NEAR THE EARTH’S SURFACE EXTRUSIVE IGNEOUS ROCKS WILL RESULT IN FINE (APHANITIC) TEXTURE (EX. BASALT) ...
Shifting Plates Choice Board
Shifting Plates Choice Board

... Directions: You and your partner will choose two topics from the Shifting Plates Choice Board. Along with researching the topics, you and your partner will choose a product to create for each topic. You may only use one product once. ...
Introduction to Geol.. - hrsbstaff.ednet.ns.ca
Introduction to Geol.. - hrsbstaff.ednet.ns.ca

... in a definite and determinable order, and any time period can be recognized by its -different units of time and duration depend on the amount and variety of fossils found in a particular period ...
presentation
presentation

... mantle rocks have a higher magnesium to iron ratio, and a smaller portion of silicon and aluminum than the crust. • Lithosphere versus asthenosphere: While the lithosphere behaves as a rigid body over geologic time scales, the asthenosphere deforms in ductile fashion. The lithosphere is fragmented i ...
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Geophysics



Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
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