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Chapter 02 Earth Structure and Plate Tectonics
Chapter 02 Earth Structure and Plate Tectonics

... 1. Identify all of the types of plate boundaries that are associated with active volcanism. 2. Identify all of the different observations Alfred Wegener used to support his theory of continental drift. 3. Identify all of the different observations used to support Harry Hess' theory of seafloor sprea ...
Changing Earth*s Surface
Changing Earth*s Surface

... the mechanical and chemical process that changes Earth’s surface over time  Physical vs Chemical Weathering:  Physical: process of breaking down rock without changing the composition  Chemical Weathering: The process that changes the composition of rocks  Sediment: The material formed from rocks ...
The plate tectonic revolution part I.
The plate tectonic revolution part I.

... • Proposed transform plate boundary hypothesis in 1965 to explain linear fracture zones in oceans • Realized that motion on an oceanic transform fault is opposite to apparent offset of ridges ...
4_Ocean126_2006
4_Ocean126_2006

... – Refraction of waves led to discovery of earth’s core and Moho – Travel time of waves led to discovery of layers ...
Quiz # 6
Quiz # 6

... 2. Regions where the continents or the sea floor are pulling apart are called a. subduction zones b. magnetospheric zones c. enterprise zones d. convection zones e. rift zones 3. In which region of the Earth's atmosphere have you spent most of your life? a. the mesosphere b. the troposphere c. the s ...
Inside the Earth
Inside the Earth

... – Oceanic (very dense, made of basalt) – Continental (less dense, made of granite) ...
Chapter 17 Study Guide 16
Chapter 17 Study Guide 16

... Explain how mid-ocean ridges and deep-sea trenches are different. Describe their many differences: how they form, what they look like, their elevations, etc. ...
Introduction to Geography
Introduction to Geography

... Introduction to Geography By Arthur Getis Judith Getis Jerome D. Fellmann ...
Science SOL 5.7d Earth`s Layers
Science SOL 5.7d Earth`s Layers

... 1) What are the four layers of the Earth? 2) The Earth’s crust is very ______? 3) The mantle is the largest layer of the Earth? True or False 4) Is the Outer Core a liquid or a solid? ...
The Dynamic Earth Ch. 3 Sect. 1 Objectives Describe the
The Dynamic Earth Ch. 3 Sect. 1 Objectives Describe the

... 1.Sunlight enters Earth’s atmosphere 2.Earth’s surface radiates heat back to the atmosphere Some heat escapes Some heat is trapped by Greenhouse Gases Ex: water vapor, carbon dioxide, methane, nitrous oxide 3.Trapped heat radiated back to Earth’s surface, warming the air. Without this Earth would be ...
The entire earth is still changing, due to the slow convection of soft
The entire earth is still changing, due to the slow convection of soft

... – Study of sound vibrations within earth – Used to determine earth’s inner structure ...
Plate Tectonics - Helena High School
Plate Tectonics - Helena High School

... Antarctica, therefore Antarctica must have been closer to the equator at one time. ...
Essentials of Geology, 9e
Essentials of Geology, 9e

... The Earth system is also powered from Earth’s interior ▪ Heat remaining from the Earth’s formation and heat that is continuously generated by radioactive decay powers the internal processes that produce volcanoes, earthquakes, and mountains ...
Plate Tectonics
Plate Tectonics

... Plate Tectonics Lithosphere ...
Evidence for a Plate Tectonics Debate - IG
Evidence for a Plate Tectonics Debate - IG

... Germany, and this was the beginning of the idea of continental drift, or Kontinentalverschiebung in German. Alfred Wegener was a “drifter”. Although elegant and interesting models of continental drift have been proposed since then by well known geologists, such as Arthur Holmes, Du Toit, and Sam Car ...
Earth`s Layered Structure
Earth`s Layered Structure

... Layers Defined by Physical Properties ...
P-waves - Fort Thomas Independent Schools
P-waves - Fort Thomas Independent Schools

... • When stress leads to strain, energy is released suddenly, and it causes rock to lurch to a new position. • A fault is a crack along which movement has taken place. • The sudden energy release that goes with fault movement is called elastic rebound. ...
Earth`s Interior Chapter-1 Section-1
Earth`s Interior Chapter-1 Section-1

... and wear down the land  The earth looks very different than it did thousands of years ago. ...
Heat From the outer core causes convection currents in the semi
Heat From the outer core causes convection currents in the semi

... Earthquakes occur when rocks move along faults or cracks in the earth’s outer layers. Severe earthquakes happen when plates move past each other or towards each other. ...
Continental Drift: The Beginning of Plate Tectonics
Continental Drift: The Beginning of Plate Tectonics

... What is Pangaea? What process showed Continental Drift is correct? ...
EARTH`S FORMATION AND STRUCTURE The earth formed
EARTH`S FORMATION AND STRUCTURE The earth formed

... accreted to the nebular midplane where it formed progressively larger clumps. Eventually, bodies of several kilometers in diameter formed; these are known as planetesimals. The largest planetesimals grew fastest, at the expense of the smaller ones. This process continued until an earth-sized planet ...
6th Grade Exam Review - Ms. Moreno's Science Classes
6th Grade Exam Review - Ms. Moreno's Science Classes

... continue moving in a straight line or a stationary object to remain in place is called ...
The Earth`s Structure - Warren County Schools
The Earth`s Structure - Warren County Schools

... - Wegner thought that all of the continents were once together in a super-continent he called _____________________________________ - Explains _______________________ formation, ___________________________, ________________________, and how similar ________________________ could have lived at the sa ...
6th grade Science Unit 1.3 Structures of the Earth and Energy
6th grade Science Unit 1.3 Structures of the Earth and Energy

Midterm Review - Earth Science
Midterm Review - Earth Science

... Similar rock types or mountain ranges Shape of coastlines ...
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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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