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Unit 4 Notes
Unit 4 Notes

... demonstrate where ocean crust was being created and old crust was sinking back into earth’s mantle -Scientists concluded that the surface of the planet is divided into a number of moving sections, called tectonic plates. -Where these plates interact, there are numerous earthquakes and volcanoes! ...
CTY Course Syllabus: Dynamic Earth
CTY Course Syllabus: Dynamic Earth

... Lab - plotting surface currents Activity: assemble water mass model of Pacific ocean using ocean water from Mary’s sampling in Monterey Demo- Deep water that you drink! Lab- Tides and the water bulge – figuring out tide charts for specific latitudes ...
southern alps: geology - Geoscience Research Institute
southern alps: geology - Geoscience Research Institute

chapter 17 - Geoclassroom Home
chapter 17 - Geoclassroom Home

... 6. Moraines, striations, outwash, and various other glacial landforms are found throughout Canada, in the northern tier of states, and in many mountain ranges where valley glaciers are present. Figure 17.10 Origin of End Moraines and Outwash Figure 17.11 Terminal and Recessional Moraines in the Mid- ...
Chapter 14
Chapter 14

... 14-2 How Are the Earth’s Rocks Recycled? • Concept 14-2 The three major types of rocks found in the earth’s crust—sedimentary, igneous, and metamorphic—are recycled very slowly by the process of erosion, melting, and metamorphism. ...
PowerPoint Fill-in-the-Notes for Unit 2
PowerPoint Fill-in-the-Notes for Unit 2

... Seasonal, but almost never below freezing Moderate rain In General: A wide variety—forests of deciduous trees, tall shrubs, low bushes, a variety of grasses Humid Subtropical: Has the most heat and precipitation and many types of vegetation Marine West Coast: Mountainous and cooled by ocean currents ...
Chapter 15 Geology and Nonrenewable Mineral Resources “It`s A
Chapter 15 Geology and Nonrenewable Mineral Resources “It`s A

8-Plate_Tectonics short
8-Plate_Tectonics short

... Oceanic trench (deep linear trough) = where subduction begins. As crust + mantle melt (partially), produces explosive volcanic eruptions + volcanic mountains See Google Earth trenches ...
Americas - Tectonic Plates - Central Michigan University
Americas - Tectonic Plates - Central Michigan University

... 1. Make copies of the map on slide 3 for each student. 2. Show PowerPoint and discuss slides. Students will follow directions to complete their maps (and add to the legend). 3. Discuss questions on slides 21 and 22. 4. Have students write a paragraph answering one of the following questions: “What i ...
Understanding continental subduction: A work in
Understanding continental subduction: A work in

Chapter 19 - Heritage Collegiate
Chapter 19 - Heritage Collegiate

... continents were always where they are now, then these glaciers must have moved in from the sea. Wegener explained that if Pangaea was situated with South Africa centered on the South Pole, then the presence of glaciers on Pangaea near the South Pole could explain the existence of the glacial till an ...
Plate Tectonics
Plate Tectonics

Unit Title: Physical Systems and Forces of Change
Unit Title: Physical Systems and Forces of Change

... boundaries, one of which involves two of the same type of plate composition (continental-continental or oceanic-oceanic). This plate boundary causes the formation of folded mountains. The second type of converging plates involves the movement of continental and ocean plates toward each other. The he ...
Unit Title: Physical Systems and Forces of Change
Unit Title: Physical Systems and Forces of Change

... boundaries, one of which involves two of the same type of plate composition (continental-continental or oceanic-oceanic). This plate boundary causes the formation of folded mountains. The second type of converging plates involves the movement of continental and ocean plates toward each other. The he ...
Model Answers - Step Up IAS Coaching
Model Answers - Step Up IAS Coaching

... atmosphere is increasing day by day mainly due to activities like burning of fossil fuels, deforestation and production of cement. The carbon dioxide thus released in the atmosphere is absorbed by the oceans which play a very significant role in moderating climate change. When atmospheric carbon dio ...
Subsoil - Eniscuola
Subsoil - Eniscuola

Subsoil - Eniscuola
Subsoil - Eniscuola

Interactive comment on “Energy of plate tectonics calculation and
Interactive comment on “Energy of plate tectonics calculation and

File
File

Mull and Iona - Scottish Natural Heritage
Mull and Iona - Scottish Natural Heritage

... possibly well over two kilometres thick in places. The lava plateau ...
2 The Geology and Tectonics of the Tohoku Region
2 The Geology and Tectonics of the Tohoku Region

... subduction zone, like all others, can be subdivided into the trench axis, trench slope, forearc basin, volcanic arc, and backarc regions. The tectonic activity associated with subduction comes in the form of faulting, magmatic intrusions and extrusions and vertical movements that range from folding ...
Year at a Glance:
Year at a Glance:

Plate Boundaries - Geog
Plate Boundaries - Geog

... • The continental crust is crumpled by the collision of the two plates creating Fold Mountains. • If the magma rises offshore it will form an Island Arc, like the West Indies and Japan. ...
Earth`s Crust - Student Handouts - PITA
Earth`s Crust - Student Handouts - PITA

... 21) Mt. St. Helens is a famous volcano in Washington state. It is a part of the volcanic mountain range (volcanic arc) called the Cascades, which was formed when the little Juan ___ Plate got pushed underneath the North American Plate. 23) The skinniest crust is strangely the most dense (heaviest). ...
PLATE TECTONICS
PLATE TECTONICS

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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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