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Isostasy chap 9 LECT..
Isostasy chap 9 LECT..

... the weight of the mountains: the strength of the crust for small mountains, and a bouyant low density root beneath large mountains. ...
Chapter 2: Global Tectonics Our Dynamic Planet Introduction
Chapter 2: Global Tectonics Our Dynamic Planet Introduction

Atmosphere Hydrosphere Lithosphere
Atmosphere Hydrosphere Lithosphere

...  All of the water on planet Earth  “71% of the earth is covered by water and only 29% is terra firma” (University of Florida).  “Blue Planet” – water is not found on any other planets in our solar system.  “It is because the Earth has just the right mass, the right chemical composition, the righ ...
Chapter 1—Plate Tectonics and California
Chapter 1—Plate Tectonics and California

Section 2 Crossword
Section 2 Crossword

... stress above which a material ceases to deform elastically (2 words) quicksand condition in wet soil induced by seismic waves planar break between offset segments of a spreading ridge along which two plates move horizontally in opposite directions (2 words) measure of earthquakes’s damaging effects ...
Section 2 Crossword
Section 2 Crossword

Earthquakes Unit STUDY GUIDE
Earthquakes Unit STUDY GUIDE

... The strongest earthquakes usually occur a. near divergent boundaries. c. near transform boundaries. b. near convergent boundaries. d. along normal faults. The last seismic waves to arrive are a. P waves. c. surface waves. b. S waves. d. body waves. Strike-slip faults are prominent along ____ plate b ...
Subduction Zones
Subduction Zones

... equator. What land forms would you fly over? ...
CH. 8 Pre-Test
CH. 8 Pre-Test

... a. drive away from the area. b. stop the car and stay inside. c. stop the car and seek shelter in a ditch. d. drive slowly to the nearest overpass. ...
Earth Science, Level 3
Earth Science, Level 3

... 30. Use the Mohs’ Scale on pg. 195 to answer the following: A. What is the softest mineral? Hardest mineral? B. Can Feldspar scratch Quartz? Why or why not? C. Can Apatite scratch Gypsum? Why or why not? ROCKS (check 6/1) 31. How can rocks be changed as they move through the rock cycle? 32. Rocks ar ...
Plate Tectonics
Plate Tectonics

... continents had formed a single land mass which has split apart over time. Wegner was not the first to suggest this theory, but he was the first to present information from several fields. ...
A brief introduction to minerals, rocks and the rock cycle
A brief introduction to minerals, rocks and the rock cycle

... Silicon and Oxygen combine to form the most common mineral group, the silicates. Every silicate mineral contains the elements ...
6.01 Earth Science Intro - Plate Tectonics - California K
6.01 Earth Science Intro - Plate Tectonics - California K

... develops a prediction of where plates will be in 50 million years based on the plate movement from the past 200 million years. Having learned that continents have moved and are continuing to move in Lesson 4, students in Lesson 5 “Seismic News” explore evidence that years of earthquake records start ...
Chapter 2
Chapter 2

... • When a rift occurs, pressure is released and hot mantle material rises up through the rift • This molten rock pushes the oceanic crust up to form the mid-ocean ridge and new oceanic crust • Therefore the rifts are known as spreading ...
Plate Tectonics or Does the earth move under your feet?
Plate Tectonics or Does the earth move under your feet?

Semester Review #2 Multiple Choice. Circle the best answer. Which
Semester Review #2 Multiple Choice. Circle the best answer. Which

... ____________32. forms along subduction zones ____________33. buildup of basaltic layers, forming a broad volcano with gently ...
Plate Tectonics Virtual Lab Directions 1. Go to the following website
Plate Tectonics Virtual Lab Directions 1. Go to the following website

... 1. Scientists used what to figure out the interior of the Earth?  Use the diagram of the Earths interior to answer the following  2. This layer is made up of the crust and a tiny bit of the upper mantle.  It is divided  into several constantly moving plates.  3. The plates move on this hot, malleabl ...
Plate tectonics II: Earth`s structure and plate boundaries
Plate tectonics II: Earth`s structure and plate boundaries

... •  Crust versus mantle: The crust is a product of mantle melting. Typical 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, th ...
layers of the earth
layers of the earth

... Homeroom Make sure all science homework is complete Do not walk around! ...
Name Class___________ Date Grade 7 Science: Benchmark #2
Name Class___________ Date Grade 7 Science: Benchmark #2

... _____5. Many scientists believe that crustal plate movement occurs because of convection cells contained in Earth’s (1) crust (3) outer core (2) mantle (4) inner core _____6. Dust and ash entering the atmosphere as a result of volcanic eruptions can affect Earth’s (1) tidal activity (2) orbital shap ...
Lithospheric plates - The Old Courthouse Museum Batemans Bay
Lithospheric plates - The Old Courthouse Museum Batemans Bay

... The rocks that we see at the Earth’s surface today have been subjected to very significant physical and chemical processes during the many phases of their evolution throughout geological history. This is called the Rock Cycle. Rocks may be formed near the surface or deep within the Earth. They may t ...
8th Grade Science Final Review
8th Grade Science Final Review

...  Matter cannot be created or destroyed it just changes ...
Inside the Earth - Pacific Climate Change Portal
Inside the Earth - Pacific Climate Change Portal

... • What parts of the earth’s structure are represented by the shell, the white, and the yolk? The shell represents the lithosphere, or the crust and uppermost mantle—earth’s plates. The white represents all the remaining mantle, and the yolk represents the core of the earth. • What about the egg’s me ...
Lab: Plate Tectonic and Earthquake Extravaganza
Lab: Plate Tectonic and Earthquake Extravaganza

Bellringer: Oceans are not just places… The Water Planet
Bellringer: Oceans are not just places… The Water Planet

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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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