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the earth`s interior
the earth`s interior

... Conduction – heat transfer within a material or between materials that are touching ...
Inside Our Earth
Inside Our Earth

... ● indirect evidence from seismic waves ○ Study how waves travel through Earth - speed and path of wave gives clue to structure. ...
Document
Document

... Ring of Fire Seismic Waves Seismogram Tectonic plates ...
inside earth ppt
inside earth ppt

... How do we know what inside Earth is like if we can’t travel through it? • Scientist know this by studying seismic waves/data from earthquakes ...
14 8 This question is about the structure of the Earth.
14 8 This question is about the structure of the Earth.

Name Date Period ______ Reading Guide 2.1 Earth: A Unique
Name Date Period ______ Reading Guide 2.1 Earth: A Unique

... 8. ___________________ is the third planet from the sun in our solar system. 9. Earth formed about ______________________ year ago and is made mostly of _________________. 10. About 70% of the Earth’s surface is covered with water, called the ________________ _____________. 11. Earth appears to be a ...
Earth`s Structure notes 5/26/15 • Crust
Earth`s Structure notes 5/26/15 • Crust

Plate Tectonics
Plate Tectonics

... Lithosphere- made of crust and upper mantle Asthenosphere- made of “plastic” part of mantle Mesosphere- made of strong part of mantle Outer Core- liquid layer of core Inner Core- solid layer of core ...
Appendix F - Mineralogical Society
Appendix F - Mineralogical Society

... transition zone, the enigmatic lowermost mantle region and the solid iron inner core. Seismology, however, detects primarily the velocity of the media it images. To convert this into an understanding of building blocks of the Earth requires input from mineral physics, to describe the nature and beha ...
Chapter 21 – Section 1 - Earth`s Interior and Plate Tectonics
Chapter 21 – Section 1 - Earth`s Interior and Plate Tectonics

... represents 0.8%. The Earth’s core, however, makes up only 18% of the Earth’s volume while the mantle makes up nearly 84% of the Earth’s volume. What does this data suggest about the Earth’s core? ...
science ch 9 earths changing surface sg
science ch 9 earths changing surface sg

Changing Earth Study Guide My assessment is on What is the age
Changing Earth Study Guide My assessment is on What is the age

...  Thickest layer of the Earth  Made up of heavy rock  Can change from liquid to solid (plasticity)  Made of molten iron and nickel (molten metal=liquid rock) ...
Convection Currents and Hot Spots
Convection Currents and Hot Spots

... begins to rise; • Colder and/or denser rock sinks ...
HOT SPOTS - Norwich High School
HOT SPOTS - Norwich High School

... begins to rise; • Colder and/or denser rock sinks ...
Earthquake Crossword - Science
Earthquake Crossword - Science

... 1 The fracture along which blocks of crust move relative to each other. (5) 2 City destroyed by earthquake in 1923. (5) 4 The place where two plates collide and one goes over top the other. (10,4) 5 Sudden stress changes in the earth that cause ground shaking. They occur at fault lines and near volc ...
Review Unit 1 - Effingham County Schools
Review Unit 1 - Effingham County Schools

... #60. A fossil of an ocean fish was found in a rock outcrop on a mountain. This probably means that the mountain was raised up after the fish died. ...
PowerPoint Presentation - Introduction to Earthquakes EASA
PowerPoint Presentation - Introduction to Earthquakes EASA

... where (circle the correct answer): A. light is not detected B. only P waves are detected C. only S waves are detected D. no seismic waves are detected. ...
Earth`s Interior and Geophysical Properties
Earth`s Interior and Geophysical Properties

... (thickest under mountains) ...
Earth`s Structures and Earthquake Study Guide
Earth`s Structures and Earthquake Study Guide

... 28. In a strike-slip fault, the rocks on either side of the fault slip past each other sideways with little up-or-down motion. 29. The Mercalli Scale would most likely be used to tell how much earthquake damage was done to homes and other buildings. 30. A fold in rock that bends upward into an arch ...
Changes to Earth`s Surface Vocabulary Builder
Changes to Earth`s Surface Vocabulary Builder

... 15. fault - a break in Earth’s crust where rocks can slide past each other 16. earthquake - the snap and slide of rocks as energy is released in Earth’s crust 17. focus - the point inside Earth where and earthquake begins 18. epicenter - the point on Earth’s surface directly above the focus of an ea ...
Earth`s Interior PP
Earth`s Interior PP

... iron and nickel, sank to the center of the Earth and became the core. The surface of the Earth slowly cooled off and hardened. These surface rocks became the crust. ...
Earth`s Interior Introduction
Earth`s Interior Introduction

... The Earth’s Interior Glencoe Ch. 12-3 Pages 370-372 ...
Earth - altaastronomy
Earth - altaastronomy

... the same side you get a higher than normal tide called a spring tide. • When the are on opposite sides you get a lower than normal tide called a Neap tide. Alta High Astronomy ...
File
File

... S__________ because of the immense amount of pressure that it is under. 9. A C_______________ C_______________ occurs when hot rock in the mantle R__________ toward the crust, C__________ and then F__________ in a continuous motion. 10. At a D_______________ B_______________ plates move A___________ ...
Inside the Earth
Inside the Earth

... the distant point. ...
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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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