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E.S. Ch. 3 Study Guide
E.S. Ch. 3 Study Guide

... collide/crash into each other and form mountains over millions of years. Example: Himalayan Mountains. A special type of convergent boundary = Subduction where oceanic crust meets continental crust and forms deep-ocean trenches. Transform- is when the plates slip past each other. Continental plates ...
SCIENCE IN THE NEWS | Plate Tectonics
SCIENCE IN THE NEWS | Plate Tectonics

Inside the Earth
Inside the Earth

... •Gives Earth its magnetic field ...
File - Gonzaga Geography
File - Gonzaga Geography

... invention of the theory of plate tectonics theory. We now know that the Ring of Fire is located at the borders of the Pacific Plate and other major tectonic plates. ...
Name: Introduction to Meteorology Homework #3 (Chapters 5 and 6
Name: Introduction to Meteorology Homework #3 (Chapters 5 and 6

Plate Tectonics Lecture Notes Page
Plate Tectonics Lecture Notes Page

... have volcanic activity. But what about areas such as Hawaii, and Yellowstone National Park, where volcanic activity occurs in the middle of a tectonic plate, not associated with either of these boundaries? These areas are called “Hot Spots”. ...
Introduction to Meteorology Homework #3 (Chapters 5 and 6) Due
Introduction to Meteorology Homework #3 (Chapters 5 and 6) Due

... 6. The atmosphere is “stable” when the environmental lapse rate is small, that is, when there is a _________________________________________________________________________ between the surface air and the air aloft. Therefore, the atmosphere “stabilizes” when the air aloft _______________________ an ...
Glossary - The Polesworth School
Glossary - The Polesworth School

... A method for separating a liquid from a mixture by evaporating and condensing it at its boiling point. Easily ignited and burned. A method used to separate a mixture of two or more liquids with different boiling points. The process involves boiling the mixture, then condensing the vapour at differen ...
What’s Shakin? - Oklahoma Alliance for Geographic
What’s Shakin? - Oklahoma Alliance for Geographic

... Alfred Wegner first proposed this idea as a hypothesis. •He called the large landmass Pangaea •Means “all lands” in Greek ...
REGENTS Review Homework
REGENTS Review Homework

...  Cools fast (extrusive): small/no/fine crystals -air pockets (pumice)  Cools slow (intrusive): large (coarse) crystals -ex: granite  MINERALS they contain are below ...
The Layer`s Of The Earth!
The Layer`s Of The Earth!

... 1) What are the four layers of the Earth? 2) The Earth’s crust is very ______? 3) The mantle is the largest layer of the Earth? True or False 4) Is the Outer Core a liquid or a solid? ...


A combined study of melt inclusions and classical petrology on the
A combined study of melt inclusions and classical petrology on the

Slide 1
Slide 1

... • Earth's gravity is not strong enough to hold lighter gases • Earth still did not have a differentiated core (solid inner/liquid outer core) which creates Earth's magnetic field (magnetosphere = Van Allen Belt) which deflects solar winds. ...
Ocean waves that wear away an island`s shoreline
Ocean waves that wear away an island`s shoreline

... 26. What is a fossil? Any trace of an ancient organism that has been preserved in rock. 27. What technology did scientists use in the mid-1900s to map the mid-ocean ridge? Sonar 28. Explain why old oceanic crust is more dense than new oceanic crust? Because old oceanic crust is cooler than new ocean ...
PANGEA
PANGEA

READING-STUDY GUIDE 3-5
READING-STUDY GUIDE 3-5

... 1. The major mountain belts are located on __________________ plate boundaries. 2. In your own words, explain how mountains form at subduction zones. ________________ _____________________________________________________________________ _______________________________________________________________ ...
Lecture 6: Igneous Rocks (Melting and Differentiation) Oct. 4, 2006
Lecture 6: Igneous Rocks (Melting and Differentiation) Oct. 4, 2006

Limestone is a sedimentary rock!
Limestone is a sedimentary rock!

... • Extrusive means to stick out. Extrusive rocks form when they cool at the Earth’s surface. Because of their rapid cooling, they have smaller crystals. ...
Earth's Structure - Kentucky Department of Education
Earth's Structure - Kentucky Department of Education

... along the edge of one continent match rocks and minerals along the edge of another continent. ...
Intrusive and Extrusive Igneous Rocks - cK-12
Intrusive and Extrusive Igneous Rocks - cK-12

Restless World - ARK Elvin Academy
Restless World - ARK Elvin Academy

... Ocean trenches are associated with subduction zones and destructive plate margins. As an ocean plate subducts beneath another plate (either oceanic or continental) the plates drag each other down creating the deepest part of the oceans. Examples include the Peru-Chile trench off the coast of South A ...
History of the Earth Chapter 2: The Hadean
History of the Earth Chapter 2: The Hadean

... How do they interact? 1. Pull Apart from one another (Diverge) (New rock is formed) 2. Push into one another (Converge) (Rock is destroyed) 3. Slide past one another (Rock is conserved) ...
Intrusive and Extrusive Igneous Rocks
Intrusive and Extrusive Igneous Rocks

... Granite is the most common intrusive igneous rock. Pictured below are four types of intrusive rocks (Figure 1.1). Geological processes have brought some igneous rocks to the surface. Pictured below is a landscape in California’s Sierra Nevada made of granite that has been raised to create mountains ...
The Restless Earth - Whitworth Community High School
The Restless Earth - Whitworth Community High School

... Key Words ...
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Tectonic–climatic interaction



Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.
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