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Continental Margin Subduction Zone

Continental Margin Subduction Zone

  • edolie
  • 3 Slides

volcanic arc. asthenospheric mantle. oceanic crust...

Mineral Reactions Mineral reactions are the basis for much of our understanding of metamorphism.

Mineral Reactions Mineral reactions are the basis for much of our understanding of metamorphism.

  • winnie
  • 6 Slides

Our estimates of pressures and temperatures experi...

1. Clapeyron slope - general features.

1. Clapeyron slope - general features.

  • brown
  • 10 Slides

Although the indicated chemical reactions (below) ...

3D density structure model of the upper mantle in the Mediterranean Sea and surrounding region deri

3D density structure model of the upper mantle in the Mediterranean Sea and surrounding region deri

  • blanko
  • 23 Slides

Fayez . Harash. , . Chao Chen. China University of...

Chapter 9 Air Masses and Fronts

Chapter 9 Air Masses and Fronts

  • caitlin
  • 67 Slides

ATMO 1300. Summer II . 2017. Air Mass. A large bod...

What is the GEOSPHERE? All solid parts of Earth

What is the GEOSPHERE? All solid parts of Earth

  • amber
  • 35 Slides

Rocks, soils, minerals, sediments, magma. The Gran...

Plates Group of rocks all moving in the same direction

Plates Group of rocks all moving in the same direction

  • felicity
  • 25 Slides

Can have . both. oceanic and continental crust or...

Ch. 23 The Ocean Floor Studying the ocean floor

Ch. 23 The Ocean Floor Studying the ocean floor

  • jade
  • 30 Slides

Submersibles, satellites, and other technology all...

B.P. #4 Materials move within each sphere and between spheres

B.P. #4 Materials move within each sphere and between spheres

  • elise
  • 31 Slides

Plate tectonic cycle . Plate tectonics -. What is...

Plate Tectonics Imagine the Earth as a hardboiled egg…………………….

Plate Tectonics Imagine the Earth as a hardboiled egg…………………….

  • amey
  • 12 Slides

The thin brittle shell is the crust that humans li...

A block is launched up a frictionless 40° slope with an initial speed v and reaches a maximum vert

A block is launched up a frictionless 40° slope with an initial speed v and reaches a maximum vert

  • eve
  • 4 Slides

h/2. h. 2h. Somewhere between h and 2h. Somewhere ...

Outline Estimation of terrain

Outline Estimation of terrain

  • fauna
  • 10 Slides

(. Bouguer. ) density. : . Principles. Nettleton. ...

1 Petrology Lecture 5 Reaction Series and Melting Behavior

1 Petrology Lecture 5 Reaction Series and Melting Behavior

  • garcia
  • 36 Slides

GLY 4310 - Spring, 2020. 2. Norman Levi Bowen. Ca...

Facts with Statistics Seminar

Facts with Statistics Seminar

  • riley
  • 37 Slides

1. Many Ways to Look at the . Correlation . Coeffi...

APPLIED GEOMORPHOLOGY SLOPE DEVELOPMENT THEORIES

APPLIED GEOMORPHOLOGY SLOPE DEVELOPMENT THEORIES

  • jade
  • 27 Slides

W.M. DAVIS. . ...

The 3 main types of plate boundaries/margins

The 3 main types of plate boundaries/margins

  • priscilla
  • 9 Slides

1. 2. Oceanic crust. 1-Convection currents pull pl...

The Theory of Continental Drift

The Theory of Continental Drift

  • jainy
  • 27 Slides

The World. ALFRED WEGENER. THEORY OF CONTINENTAL D...

Our Lesson Essential Question (6.E.2.2):

Our Lesson Essential Question (6.E.2.2):

  • callie
  • 22 Slides

“What are tectonic plates?. Classifying the Laye...

Continental Drift, Theory of Tolerance

Continental Drift, Theory of Tolerance

  • mia
  • 26 Slides

&. Major Biomes of the World. Dr. . Habibur....

B.P. #5 Present state of earth is temporary - different in past, future

B.P. #5 Present state of earth is temporary - different in past, future

  • ximena
  • 49 Slides

B.P. #6 Rates and scale of earth change are diff...

Continental Drift: Alfred Wegener

Continental Drift: Alfred Wegener

  • madeline
  • 6 Slides

http://www.sciencechannel.com/tv-shows/greatest-di...

Notes on the Ocean Floor

Notes on the Ocean Floor

  • rodriguez
  • 9 Slides

Ocean . Floor Features. When we look across the oc...

Can continental margin sediments be globally correlated during Pleistocene

Can continental margin sediments be globally correlated during Pleistocene

  • bella
  • 58 Slides

glacio-eustatic. fluctuations?. Cecilia M. McHugh...

The Embarrassing Details about Geochemical Mass Balance Models for Calculating Mantle Composition

The Embarrassing Details about Geochemical Mass Balance Models for Calculating Mantle Composition

  • ida
  • 5 Slides

(they are trivially simple, but they do give some ...

UHT/ UHP Met UHT Ultrahigh-temperature metamorphism

UHT/ UHP Met UHT Ultrahigh-temperature metamorphism

  • lam
  • 14 Slides

(UHT) represents extreme crustal . met . with . T ...

Oceanic density/pressure gradients and slope currents

Oceanic density/pressure gradients and slope currents

  • ariel
  • 10 Slides

John Huthnance. 1. , Mark Inall. 2. , Neil Fraser....

Chapter 9 Deflection of Beams

Chapter 9 Deflection of Beams

  • maisie
  • 32 Slides

Introduction. A new aspect in the design of beams ...

Circular Failure Plane and wedge failures are concerned with the stability of rock slopes containin

Circular Failure Plane and wedge failures are concerned with the stability of rock slopes containin

  • carny
  • 21 Slides

It is also necessary to design cuts in weak materi...

Characterizing patchy soil and bedrock cover is useful for hydrology, ecology, and geomorphology

Characterizing patchy soil and bedrock cover is useful for hydrology, ecology, and geomorphology

  • delcy
  • 1 Slides

Airborne lidar is addressing the need, however: . ...

Geophysical and Isotopic Constraints on Crustal Structure Related to Mineral Trends in North-Centra

Geophysical and Isotopic Constraints on Crustal Structure Related to Mineral Trends in North-Centra

  • finley
  • 7 Slides

Goals: . Review isotopic and geophysical data, dis...

Chapter 8 - Plate Tectonics

Chapter 8 - Plate Tectonics

  • eloise
  • 68 Slides

http://sos.noaa.gov/datasets/Land/paleo.html. Anim...

Motion with Constant Acceleration

Motion with Constant Acceleration

  • catherine
  • 12 Slides

Lesson . 2. Position with Constant Acceleration. T...

Plate Tectonics Do Now SWBAT create a concept map of plate tectonics terms as a pre-assessment

Plate Tectonics Do Now SWBAT create a concept map of plate tectonics terms as a pre-assessment

  • amey
  • 88 Slides

Enter . Silently. Grab Materials. Begin Do Now. Wr...

Title Slide Navigation 2 Minute Teaser

Title Slide Navigation 2 Minute Teaser

  • abigail
  • 27 Slides

Elevation validation and geomorphic metric compari...

A sub-crustal piercing point for North Atlantic

A sub-crustal piercing point for North Atlantic

  • martin
  • 32 Slides

reconstructions and tectonic implications. Randell...

Activating Strategy : Watch Ice Age:

Activating Strategy : Watch Ice Age:

  • cadie
  • 84 Slides

Scrat. Continental Crack Up. video clip and have...

Oceanography notes (part 1):

Oceanography notes (part 1):

  • deborah
  • 23 Slides

Ocean size and names. Nearly 71% of the Earth’s ...

Rivers Rivers Almost half of the water that falls to the Earth’s surface eventually ends up in a

Rivers Rivers Almost half of the water that falls to the Earth’s surface eventually ends up in a

  • lucy
  • 52 Slides

runoff. ), where it travels overland to the oceans...

NOW, you will learn • How the continental drift hypothesis was developed

NOW, you will learn • How the continental drift hypothesis was developed

  • lauren
  • 11 Slides

• About evidence for plate movement from the sea...

Chatham Rise Phosphorite Mining – Impact Assessment Challenges

Chatham Rise Phosphorite Mining – Impact Assessment Challenges

  • amber
  • 47 Slides

Paul Kennedy and Carmen Taylor, Golder Associates ...

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