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No Slide Title
No Slide Title

... – indicate that much of the volcanism was – under water, probably at or near a spreading ridge ...
Earthquake handout
Earthquake handout

... Mr Moynihan ...
Igneous Rocks
Igneous Rocks

... Melting point of minerals increases with increasing pressure In the hottest regions within the upper mantle and crust, pressure can be low enough for melting to occur ...
Explain with reference to examples you have studied how plate
Explain with reference to examples you have studied how plate

... The Japan tsunami of 2011 was caused by the collision of the pacific plate (oceanic plate) and the North American plate (continental). The pacific plate was subducted under the North American plate causing the north American plate to rise and produce the gigatic waves. This was a 8.9 magnitude eart ...
continental drift - East Hanover Township School District
continental drift - East Hanover Township School District

... insight to the mechanism for how the continents moved. • The magma which pushes up at the mid-ocean ridge provides the new land pushing the plates, and the subduction zones gobble up the land on the the other side of the plates. ...
Plate Tectonics The Theory of Plate Tectonics
Plate Tectonics The Theory of Plate Tectonics

... the layers within Earth’s interior. The cold and rigid outermost rock layer is called the lithosphere. The crust and the solid, uppermost mantle form the lithosphere. The lithosphere varies in thickness. It is thin below midocean ridges. It is thick below continents. Earth’s tectonic plates are larg ...
Stage 2 - FreshmanBiology
Stage 2 - FreshmanBiology

...  Humans diverged from other primates about 6 to 7 million years ago.  Our species, Homo sapiens, originated about 195,000 years ago.  If the Earth’s history were compressed into an hour, humans appeared less than 0.2 seconds ago! ...
THE AZORES
THE AZORES

...  The Azores lie at a triple junction between the Eurasian, North American and African Plate.  The Archipelago is also bisected by the mid Atlantic ridge (the solid black line running N-S in figure 1)  The islands are of varying compositions getting progressively older towards the East. Figure 1: ...
Metamorphism: The Role of Fluids
Metamorphism: The Role of Fluids

Different plate boundaries
Different plate boundaries

... 3. Explanation of processes. Once they have completed the card sort, they should use this information to complete their student table worksheet. This could be done in one of three ways to differentiate for ability level of class/individual. 1. They could stick the cards onto the table once they have ...
File
File

... Volcanic islands within a plate  Island chains  Systematic variation of age Record ancient plate motions ...
The Quest for Self-Consistent Generation of Plate Tectonics in
The Quest for Self-Consistent Generation of Plate Tectonics in

Objectives
Objectives

... The crustal portion of the subducting slab contains a significant amount of surface water, as well as water contained in hydrated minerals within the seafloor basalt. As the subducting slab descends to greater and greater depths, it progressively encounters greater temperatures and greater pressures ...
mineralnotes
mineralnotes

... different physical properties? ...
The Earth and the Moon
The Earth and the Moon

Leaving Certificate GEOGRAPHY - English Language Support
Leaving Certificate GEOGRAPHY - English Language Support

... (to erupt) in AD 79, also ________________ (to attract) many visitors. In Iceland natural steam _______________ (to use) to generate electricity. The geothermal energy produced is used to heat houses, grow tomatoes and provide pools for swimming all the year round, even though the temperatures outsi ...
Unit 4 Lesson 8
Unit 4 Lesson 8

... • Earthquakes are ground movements that occur when blocks of rock in Earth move suddenly and release energy. • The energy is released as seismic waves that cause the ground to move. ...
Plate Tectonics - Flushing High School
Plate Tectonics - Flushing High School

... all geologic observations. Most geologic phenomenon observed near the Earth’s surface are linked in some way to plate tectonic processes. The theory states that the outer 60-100 km of the Earth is divided into slabs of rigid rock (the lithosphere). These slabs (the plates) rest upon a semi-viscous l ...
Tsunamis - LsSharks
Tsunamis - LsSharks

... wave will hit. Sudden flooding will occur. There is no warning. However, if the trough arrives first, a drawback will occur. The wave produces a vacuum effect. It sucks water out towards the sea. The ocean floor is exposed. This is an important warning sign of a tsunami. Beachgoers have about five m ...
Plate Tectonics Map - Teacher Created Materials
Plate Tectonics Map - Teacher Created Materials

Yosemite National Park
Yosemite National Park

... Rocks can be broken down or chemically altered on the earth’s surface. Mechanical Weathering: Rocks are physically broken down by various surface processes into smaller parts without changing physical properties. Chemical Weathering: Rocks are altered from one form to a completely new form with a di ...
Record - cloudfront.net
Record - cloudfront.net

... Differential erosion of old structures by rivers is not regarded as a morphotectonic phenomena; the diversion of rivers by tectonic movements, or the extension of rivers onto newly uplifted coastal plains certainly is. Several authors use the term 'morphostructure' as virtually synonymous with 'morp ...
GY 111 Lecture Note Series Intrusive Igneous Rocks
GY 111 Lecture Note Series Intrusive Igneous Rocks

... rocks in the lab. And how about those igneous textures? You just gotta love a subject which uses terms like pegmatite, phaneritic, porphyritic and phenocryst in a single lecture! We also discussed igneous rock compositions. The terms ultramafic, mafic, intermediate and felsic should be familiar to y ...
8-Plate_Tectonics short
8-Plate_Tectonics short

... In cross-section, tectonic plate = lithosphere - ~cool, outer rigid layer where rocks can break, ~100 km thick, includes entire crust + outer part of mantle; below lithosphere is asthenosphere - layer of ~hot, weak rock that flows, from ~100 - ~300 km in depth, only mantle rock . ...
Tectonic Plates Boundaries
Tectonic Plates Boundaries

... (Mt. St. Helen’s) ...
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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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