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Oceanic Crust
Oceanic Crust

... mostly focused at plate ...
ch03_sec1 revised
ch03_sec1 revised

... • The Earth’s surface is continually battered by wind and scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natur ...
Plate Tectonics Review Worksheet
Plate Tectonics Review Worksheet

... 1. Continental Drift: A theory proposed by Alfred Wegner that said all continents were once joined 300 million years ago in a single land mass called Pangaea. Over time the continents moved to their present day locations. 2. What are four pieces of evidence for continental drift? Fossils, puzzle fit ...
What is Plate Tectonics?
What is Plate Tectonics?

... If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle. ...
007.DKKSP-01(INTRODUCTION)2009-08-03 07:372.7 MB
007.DKKSP-01(INTRODUCTION)2009-08-03 07:372.7 MB

... cold, strong rock exhibits rigid behavior 5 to 250 km thick ...
Chapter 9 Planetary Geology: Agenda Ad Hoc Rover Update
Chapter 9 Planetary Geology: Agenda Ad Hoc Rover Update

... • Why do some planetary interiors create magnetic fields? – Requires motion of charged particles inside planet ...
File
File

... Long wavelength wave produced by the sudden movement of a very large volume of water  Convergent plate boundary, abrupt slippage of one plate against another results in an underwater earthquake and then a tsunami ...
Internal Structure of the Earth
Internal Structure of the Earth

... Theory of Continental Drift • The theory that continents drifted across the ocean to get their current spots on the globe. • First suggested by Alfred Wegner • First used the idea of one super giant continent called Pangaea. ...
Sea-Floor Spreading - Catawba County Schools
Sea-Floor Spreading - Catawba County Schools

... sound waves. Sonar mapped midocean ridges. ...
Unit 1 Review - Hicksville Public Schools
Unit 1 Review - Hicksville Public Schools

... o Condensation: Water changes from gas to liquid, formation of clouds o Precipitation: rain, snow, sleet, hail o Run-off: Water moves from a high elevation (mountain) into a body of water (ocean, lake) ...
Dynamic Earth Interactive Web Quest
Dynamic Earth Interactive Web Quest

... What happens at divergent boundaries that are located along two continental plates? ___________________________________________________________________________ ___________________________________________________________________________ ________________________________________________________________ ...
Geography Progress Sheet Earth Forces
Geography Progress Sheet Earth Forces

... Earth’s Structure I know the location of the four main layers of the Earth’s structure I can describe the crust, mantle, inner core and outer core I can describe why the Earth’s plates move I can discuss the effects of plate movements e.g. volcanoes, fold mountains and earthquakes I can discuss what ...
31.3 Sedimentary Rocks Blanket Most of the Earth`s Surface
31.3 Sedimentary Rocks Blanket Most of the Earth`s Surface

... Two kinds of weathering Mechanical– physically breaks rocks into smaller pieces  chemical- chemical reactions that involve water and decompose rock into smaller pieces Erosion- process that removes weathered rock particles and transports them by wind, water, or ice ...
Earth Movements - Delta Education
Earth Movements - Delta Education

... ACTIVITY 2 Students explore the structure and composition of the Earth’s crust. They compare oceanic crust with continental crust and discuss some of the geographic features of each. Then they build a model of the Earth’s crust that consists of ocean floor and an adjacent continent. ACTIVITY 3 Stude ...
Earth Science
Earth Science

... • Index fossil: fossils that occur only in rock layers of a particular geologic age (used to determine the relative age of rock layers) • Must be present in rocks scattered over a large region • Must have features that clearly distinguish it from other fossils • Organism must have lived during a sho ...
Thermal Convection
Thermal Convection

... and brings heat to the boundary between the core and the mantle where some of it is transferred into the mantle. Temperatures are hot enough in the upper mantle ( 1200 C) to cause thermal convection of the highly viscous upper mantle rocks, although it flows very slowly – approximately one cm/yr. Th ...
Science 7 Unit 5 Planet Earth This book belongs to: Topic 1
Science 7 Unit 5 Planet Earth This book belongs to: Topic 1

... - Crystals are the building blocks of minerals. They occur naturally, having straight edges, flat sides and straight angles. - There are 6 different crystal types: cubic, tetragonal, hexagonal, orthohombic, monoclinic and triclinic (Table 5.2 p. 355) Identification of Minerals The properties that ca ...
23.6 Earth`s History
23.6 Earth`s History

... At some boundaries between eras, many different organisms became extinct within a relatively short time–an event called a mass extinction. Theories to explain mass extinctions include asteroid impacts, volcanic activity, disease, and climate change. ...
Sea Floor Spreading
Sea Floor Spreading

... Age of Ocean Floor • Late 1960s deep-sea drilling • Radiometric dating of ocean rocks • Symmetric pattern of age distribution about mid-ocean ridges • Oldest ocean floor only 180 million years old ...
Inside Earth - cloudfront.net
Inside Earth - cloudfront.net

... mainly just about the upper crust. Only in rare instances does a mineral, such as diamond, come to the surface from the lower crust or mantle. Scientists know about Earth’s interior mainly from indirect evidence such as seismic waves. Seismic waves are caused by the energy from earthquakes traveling ...
Light: The Cosmic Messenger
Light: The Cosmic Messenger

... can be attributed to plate tectonics, which gradually remakes Earth’s surface Venus does not appear to have plate tectonics, but entire surface seems to have ...
earthquake
earthquake

... 8.2 Measuring Earthquakes Earthquake Waves  Body Waves • Identified as P waves or S waves • P waves - Are push-pull waves that push (compress) and pull (expand) in the direction that the waves travel - Travel through solids, liquids, and gases - Have the greatest velocity (speed) of all earthquake ...
Plate Tectonics Review Sheet
Plate Tectonics Review Sheet

... rises to the surface, solidifies and pushes the old sea floor away subduction - the process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle ocean basin -bottom of the deep ocean floor trench - a deep canyon in the ocean floor rift valley - a deep valley that forms w ...
Unit B: Earth Systems
Unit B: Earth Systems

... The earth is composed of layers. The surface is made up of plates and the movement of the plates causes the features of the surface. The composition of the atmosphere is responsible for heat transfers and the earth is warm enough for life. The ocean regulates the earth’s temperature. The continuous ...
Name
Name

... are aligned and gravity is strongest on the water, making the tidal range bigger. Neap tides occur during quarter moons when the Sun, Earth, and Moon make a 90 degree angle. Neap tides have the smallest tidal range. ...
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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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