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Science 3360 - Kennesaw State University | College of Science and
Science 3360 - Kennesaw State University | College of Science and

Cracking Up
Cracking Up

... A new ocean will one day separate Africa. A group of nomads got a shock several years ago in a desert in Ethiopia. A series of earthquakes rattled the ground one night, making a deafening noise. The next morning, the nomads discovered that a 3-foot cliff had risen from the ground behind them. ...
petrology of continental rocks
petrology of continental rocks

... Geologists know that rocks are not so petrified and still as most people think, but full of movements and action. Much like a biological species, so a rock species has a »life» and a history from cradle to grave. The continental rocks are, of course, the rocks that build up the continents — they occ ...
ch08
ch08

Chapter 2
Chapter 2

Chapter 7 Section 1
Chapter 7 Section 1

... 2. Think of the lithosphere like a jigsaw puzzle. 3. Each of the plates is a piece of the puzzle. 4. These plates move causing earthquakes, mountain building, seafloor spreading and volcanoes. ...
Historical Geology, Chapter 1 Learning Objectives and Study
Historical Geology, Chapter 1 Learning Objectives and Study

Oceanic Crust - River Dell Regional School District
Oceanic Crust - River Dell Regional School District

weather quiz - Travelling across time
weather quiz - Travelling across time

... 15. Which pressure system brings rain/stormy weather? High pressure A. Low pressure B. 16. __________ is used to photograph and track large scale air movements such as typhoons etc. 17. The process in which liquid water changes into a gas or water vapor Transpiration A. Evaporation B. Condensation C ...
Do Now - North Thurston Public Schools
Do Now - North Thurston Public Schools

... • There are several other volcanoes that are not created near a plate boundary but instead in the middle of a plate • They are created when a mantle plume is super heated by the core and burns through the crust building a volcano • In the case of an oceanic hotspot, the plate continues to move and t ...
Chapter 9
Chapter 9

... that are not that warm, since water can do a lot of erosion (assuming everything else is the same, of course). Rotation rate: Planets that spin faster have faster winds. This results in more erosion. 10. The Moon’s history begins with its birth 4.55 billion years ago. At this time, it was still hot ...
CAUSES OF CHANGE: GEOLOGICAL EVOLUTION
CAUSES OF CHANGE: GEOLOGICAL EVOLUTION

... result a Rift Valley forms. These area contain volcanoes and earthquakes but generally are less violent then areas of Convergent Boundaries. ...
Mineral resource
Mineral resource

File - Vagabond Geology
File - Vagabond Geology

... But first a word about the earth’s crust Oceanic Crust: Under all of the deep seas About 5 miles thick Continental Crust: Comprises all continents About 20 to 50 miles thick ...
Global Tectonics Summary
Global Tectonics Summary

... Earth’s mantle loses its internal heat with a combination of heat conduction and convection. As part of this process, the upper 100-200 km layer of Earth cools and stiffens to form the lithosphere. Internal heat conducts through the lithosphere to the Earth surface. Beneath the lithosphere, internal ...
Weathering and Erosion/Erosion Prevention Test Name______
Weathering and Erosion/Erosion Prevention Test Name______

... E. Biological Weathering _____1. Process that moves rocks from one place to another _____2. When a rock is chemically changed before breaking apart. _____3. When a rock is physically broken down. _____4. The breaking down of rock and other materials through a variety of ways. _____5. When living bei ...
Plate Tectonics Review With 4 Hot Spots
Plate Tectonics Review With 4 Hot Spots

8th Grade Science Meteorology Review
8th Grade Science Meteorology Review

... Currents carry warm A: water along the ocean surface ...
Plate tectonics/boundaries
Plate tectonics/boundaries

... ______ 1. A break in Earth’s crust where rocks have slipped past each other is called a a. plate. b. layer. c. boundary. d. fault. ______ 2. Continental crust consists mainly of the rock a. nickel. b. basalt c. mantle. d. granite. ______ 3. Scientists rejected Wegener’s theory because he could not a ...
File
File

... Volcanoes are usually found where two tectonic plates meet (plate boundaries). Remember some volcanoes can form at a hotspot (away from boundaries). ...
tectonic plates.
tectonic plates.

... and are created by subduction. • If we could pull a plug and drain the Pacific Ocean, we would see a number of long narrow, curving trenches thousands of kilometers long and 8 to 10 km deep cutting into the ocean floor. ...
The Rock and Minerals of the Earth*s Crust
The Rock and Minerals of the Earth*s Crust

What forces shape the earth?
What forces shape the earth?

... called the atmosphere. It contains the oxygen we breathe, protects the earth from radiation and space debris, and provides the medium for weather and climate. The solid rock portion of the earth's surface is the lithosphere,which includes the crust and uppermost mantle. Under the ocean, the lithosph ...
Plate Tectonics
Plate Tectonics

... Arabian and African Plates ...
Plate Tectonics
Plate Tectonics

... has been left in your pocket for too long)... This hot substance (lava) from the mantle rises under the underwater ridge and breaks through a split at the top of the ridge (the crust... Remember, the plate). The split is called a rift valley. The rock then spreads out in both directions from the rid ...
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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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