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Chapter 5 Section 1
Chapter 5 Section 1

... – All three layers differ in size, composition, temperature, pressure & density ...
Unit 2 - Todd County Schools
Unit 2 - Todd County Schools

... • Which scale more accurately measures the magnitude of large earthquakes? • a. modified Mercalli scale • b. Richter scale • c. moment magnitude scale • d. Mohs scale ...
File
File

... Atlantic Ocean floor. How many grams of Potassim-40 will be left from a 80g sample after 3,000 years? (If you forgot this, go watch the videos in Unit 1…) ...
Interior of Earth Graphic Organizer
Interior of Earth Graphic Organizer

... Earth has a diameter of about 12,756 km (7,972 mi). The Earth's interior consists of rock and metal. It is made up of four main layers: 1) the inner core: a solid metal core made up of nickel and iron (2440 km diameter) 2) the outer core: a liquid molten core of nickel and iron 3) the mantle: dense ...
Quick Review
Quick Review

... Igneous rocks: Magma cools deep below the earth’s surface to form crystalline granite. Lava flows out onto the surface of the Earth to create fine-grained basalt. ...
Exam review questions 2008 2
Exam review questions 2008 2

... 24. Table salt or halite is a mineral that forms from _________________________________________________. (hint: salt is soluble in water) 25. Another way that minerals form is from the cooling of hot melted rock material called ___________________. 26. Most common rock-forming minerals are in the gr ...
The Atmosphere: Structure and Temperature
The Atmosphere: Structure and Temperature

... What is the study of weather? What is another term that you associate with weather? Where does weather occur? What is our air made of? *lead them to water vapor is made in the atmosphere also = clouds/air ...
OCN 201: Plate Tectonics II
OCN 201: Plate Tectonics II

... • Continental crust has probably formed throughout Earth’s history by chemical differentiation at subduction zones – Oceanic crust forms by single stage melting of mantle at MOR  produces basalt – Continental crust probably formed by a second stage of melting… – Water driven off subducting oceanic ...
Journey to the Center of Earth
Journey to the Center of Earth

Plate Tectonics Test Review
Plate Tectonics Test Review

... Why did people not believe Wegners theory of Pangaea and Continental Drift? ...
Ch 18 PP
Ch 18 PP

... • Volcanoes are produced over lithosphere cracks and mantle hot spots. • Hot spots are rising plumes of hot mantle magma. As tectonic plates move over the hot spot, a chain of progressively younger volcanoes is formed opposite to the direction of plate movement. • Volcanic island chains and volcanic ...
The science of Geology - Portland State University
The science of Geology - Portland State University

... • Involves understanding the workings of our dynamic planet • Began in the early part of the twentieth century with a proposal called continental drift – the idea that continents moved about the face of the planet ...
Wind
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... • Once the core differentiated the heavier gases could be retained ...
WASL Review Homework #3
WASL Review Homework #3

... Which plate boundary are we closest to? What are the three types of tectonic plate boundaries? What is created at each boundary? 16. Describe what might happen when plate boundaries meet. Give examples of each type of plate boundary including convergent boundaries, divergent boundaries, and transfor ...
Thermosphere
Thermosphere

... 24. Explain what is causing ozone depletion. •CFC’s break down ozone layer  more UV reaches surface of earth 25. Explain one negative effect of ozone depletion. •Increased risk of skin cancer ...
The Rock Cycle - Cobb Learning
The Rock Cycle - Cobb Learning

... moved by wind, water, ice and gravity • Deposition: process where sediment is dropped or (deposited) • Uplift: the movement within the Earth that lifts buried rock to surface ...
The Rock Cycle
The Rock Cycle

Jigsaw Review 2 - Earth Science with Mrs. Wilson
Jigsaw Review 2 - Earth Science with Mrs. Wilson

Geology
Geology

... break the rocks suddenly and making earthquakes. The move of rock through a fault may be vertical or horizontal or both. There are two idea for faulting:1-Classic (Old) idea:-It must be a very large stress acting to break rocks along a fault because the faults are very hard. 2-New idea:- Fault are w ...
Slide 1
Slide 1

... Check Yourself! ...
Mount Pinatubo and the Ring of Fire
Mount Pinatubo and the Ring of Fire

... The reason why so many earthquakes and volcanoes occur here has to do with  plate  tectonics.  On  the  surface  of  the  earth  is  a  patchwork  of  enormous  plates,  millions of square miles across and about 50 miles thick, atop which all geographic  features—seas, oceans, fields, mountain range ...
SGM3DP01 - Finding And Using Rocks
SGM3DP01 - Finding And Using Rocks

... located under the crust. The rock in this layer is quite thick and can be very hot. ...
Plate Tectonics
Plate Tectonics

... Peruvian Trench the ________ • Crustal melting of the subducted crust and formation of island arcs • Folding of sedimentary rocks previously formed on the Pacific ocean floor • Magma rises to form sills, dykes and volcanoes ...
MB_volcano_Presentation
MB_volcano_Presentation

... plates pull slowly apart and magma effuses upward through the gap. Volcanoes are not generally found at strike-slip zones, where two plates slide laterally past each other. “Hot spot” volcanoes may form where plumes of lava rise from deep within the mantle to the Earth’s crust far from any plate mar ...
Earth
Earth

... • Earth’s internal heat and rock movement is related to what's happening on the surface • To get a look at the Earth’s interior – Study Earthquakes ...
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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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