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Play-Doh Plates
Play-Doh Plates

... melting of hot, hydrated rocks produces a mafic-composition magma, producing a basalt when it extrudes during volcanic eruptions.  For oc-cont, the magma produced from the melting of hot, hydrated rocks produces a mafic-composition magma. But the pieces of the granite (felsic)-composition continent ...
History of Meteorology
History of Meteorology

... Ancient Period Romans – didn’t contribute much except in the field of organization, law, medicine, agriculture and the building of aqueducts Seneca – interested in meteorology  Middle Ages – stagnation in the arts and sciences – burned the library in Alexandria  Arabs – mathematics, optics and as ...
TCSS Earth Systems Unit 2 – Plate Tectonics Information
TCSS Earth Systems Unit 2 – Plate Tectonics Information

... Continental Drift Map: Lab based activity that allows students to observe all the supercontinents that have existed and how they changed over time. Plate Tectonics Latitude and Longitude Activity (Use World Map): Students will plot on a world map volcanic eruptions and earthquakes so they can see th ...
HMH Storytown 4 Mountains Final
HMH Storytown 4 Mountains Final

... “Worn down steadily and slowly”; “chemical changes”; and 327. Which words or phrases give you clues to the meaning “changing temperatures, water freezing in cracks and of the word erosion? expanding, wind blows sand”; “rock slide or avalanche”; “carve away” (accept any appropriate text-based answers ...
Lab: Metamorphism: minerals, rocks and plate tectonics!
Lab: Metamorphism: minerals, rocks and plate tectonics!

... The mineralogy of a particular metamorphic rock also depends upon the chemical composition of its protolith. For example, aluminum-and potassium-rich minerals such as muscovite and biotite cannot form during the metamorphism of a pure quartz sandstone. Protolith compositions can be extremely varied; ...
GEOL_10_mid_term_I_s..
GEOL_10_mid_term_I_s..

GEOL_10_mid_term_I_s..
GEOL_10_mid_term_I_s..

... (30) 2 pts. Assume that you have just examined several flat-lying sedimentary layers. After much study you determine that there is a considerable span of time for which no sedimentary rock layer exists at this site. You have just discovered a(n) ________. A) disconformity B) example of cross-cutting ...
THE EXAM WILL INCLUDE TH FOLLOWING QUESTIONS PART A
THE EXAM WILL INCLUDE TH FOLLOWING QUESTIONS PART A

... Describe two ways a rock can undergo metamorphism. Explain how the mineral composition of rocks changes as the rocks undergo metamorphism. Describe the difference between foliated and non-foliated metamorphic rock. Explain how metamorphic rock structures are related to deformation. ...
Chapter 3 HW (due 8 Feb for Section 5803, 9 Feb for Section 5804)
Chapter 3 HW (due 8 Feb for Section 5803, 9 Feb for Section 5804)

Ionic bonding
Ionic bonding

... What solid product is formed when zinc carbonate is heated? What is the name of the product formed when calcium oxide (CaO) is reacted with water (H2O)? 4. What is the chemical formula of the solid formed when carbon dioxide (CO2) is bubbled through calcium hydroxide (Ca(OH)2)? 5. List 2 benefits of ...
Ionic bonding
Ionic bonding

Chapter 3 Notes
Chapter 3 Notes

... • Fault- break in Earth’s crust preventing it from sliding • When it breaks and creates vibrations in crusts  creates earthquakes • Occur all the time most are too small to feel • Richter scale- quantify the amount of energy reassessed by an earthquake or its magnitude • Smallest magnitude that can ...
World of quakes - Science Learning Hub
World of quakes - Science Learning Hub

On the geoethical implications of wind erosion
On the geoethical implications of wind erosion

... in plains, especially taking into account the effects of climate change. Atmospheric dust resulting ...
Final Earth Pacing
Final Earth Pacing

Name: Section: Date: Plate Tectonics Learning Objectives
Name: Section: Date: Plate Tectonics Learning Objectives

... Predict how changes in composition and temperature change crust density and buoyancy. Predict tectonic movement based upon compositional and physical characteristics of each plate. ...
Phet Plate Tectonics Inquiry
Phet Plate Tectonics Inquiry

B. A. Part-I Geography Title english.pmd
B. A. Part-I Geography Title english.pmd

3.4 Metamorphic Rocks
3.4 Metamorphic Rocks

Poster list
Poster list

... High  precision  Sr-­‐Nd-­‐Hf-­‐Pb  isotopic  data  on  northern  Cascade  arc   basalts  reveal  spatial  gradients  in  mantle  source  compositions  and   subducting  sediment  input Thermal  Structure  of  Convergent  Plate  Boundaries  Incorpo ...
3A8 Week 01 Lecture 03-Rocks and minerals 02
3A8 Week 01 Lecture 03-Rocks and minerals 02

Tectonics Rock!! manual
Tectonics Rock!! manual

Geochemical Characterization of Intermediate to Silicic Rocks in the
Geochemical Characterization of Intermediate to Silicic Rocks in the

... Rift/Continental Margin ophiolites are predominantly basaltic andesite and andesite, whereas MOR type (mid-ocean ridge) ophiolites exhibit nearly equal proportions of basaltic andesite/andesite and rhyodacite and Plume/MOR type ophiolites are characterized by rhyolites. Intermediate to silicic volca ...
Unit 2: Meteorology
Unit 2: Meteorology

Name: ____ Due Date: Guidelines: A.) Each item is to be done on a
Name: ____ Due Date: Guidelines: A.) Each item is to be done on a

... 1.) Draw a cross-section of the Earth showing its 6 layers – crust, lithosphere, asthenosphere, mantle, outer core, and inner core. Be sure to label each layer and draw the convection current. List the elements that are found in each layer. 2.) Explain what occurs as you go down into the Earth as fa ...
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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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