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L10
L10

... The Earth's lithosphere is broken up into major plates and minor ones. Tectonic plates can include both continental and oceanic areas. Major plates are African Plate, Antarctic Plate, Indian Australian Plate, Eurasian Plate, American Plate, and Pacific Plate. Minor plates include the Arabian Plate, ...
Notes - Sayre Geography Class
Notes - Sayre Geography Class

... The Ocean's Cooling and Warming Effects Bodies of water affect climate in another way too: Why is a beach on a hot summer day cooler by the ocean? • Water takes __________________than land. • In the summer, a place near the ocean or a lake will be cooler than an area farther away. ...
ISNS 4359 EARTHQUAKES AND VOLCANOES Spring 2005
ISNS 4359 EARTHQUAKES AND VOLCANOES Spring 2005

... ~30% of the world population lives on or near an active fault ~10% of the world population lives on or near an active volcano Postscript: Impacts of Living on Unstable Land - Growing up with an abusive parent, Mother Nature Humans have coped with unpredictable agents of geologic violence for as long ...
Unit 4: The Rock Cycle - Ann Arbor Earth Science
Unit 4: The Rock Cycle - Ann Arbor Earth Science

... metamorphic, and sedimentary rocks and describe the processes that change one kind of rock into another. E 3.1B Explain the relationship between the rock cycle and plate tectonics theory in regard to the origins of igneous, sedimentary, and metamorphic rocks. ...
Earth major plates:
Earth major plates:

Overheads for Pat`s lecture
Overheads for Pat`s lecture

Powerpoint Presentation Physical Geology, 10th ed.
Powerpoint Presentation Physical Geology, 10th ed.

... hydrospheric (ocean currents) circulation • Controls weathering of rocks at Earth’s surface ...
CHAPTER 17
CHAPTER 17

... layer of the atmosphere  It’s height ranges from 100 to 400 km  This is where most small meteorites burn up and is also the location in the atmosphere that the northern lights occur ...
FREE Sample Here
FREE Sample Here

... played by water vapor, which is a source of precipitation and latent heat energy as well as being the most important greenhouse gas, are given particular attention. Current concern over increasing concentrations of another constituent, carbon dioxide, and its possible effect on global climate are al ...
Study Guide for Sea-Floor Spreading Test Please know the following
Study Guide for Sea-Floor Spreading Test Please know the following

... 10.What is the process by which new oceanic crust forms as magma rises towards the surface and solidifies? 11.Where is new seafloor material formed? 12.What provides evidence that the continents on tectonic plates have moved away from each other in the past? 13.Where does the recycling of seafloor m ...
platetectonics-1232003374497953-1 - RCPL
platetectonics-1232003374497953-1 - RCPL

... The size of the Earth -- about 12,750 kilometers (km) in diameter-was known by the ancient Greeks, but it was not until the turn of the 20th century that scientists determined that our planet is made up of three main layers: crust, mantle, and core. ...
Standard III, Objective 1, Indicator A
Standard III, Objective 1, Indicator A

The Rock Cycle
The Rock Cycle

... principal divisions of Earth’s surface. • Lands and mountains are the two categories of features found on the continents. Near sea lands are usually flat and green, and mountains are high and rocky most of the time. ...
Earth Sciences 089G MIDTERM EXAMINATION MARKING KEY Part
Earth Sciences 089G MIDTERM EXAMINATION MARKING KEY Part

... Raising global temperature would put more water vapour into the atmosphere (1/2) and, through the greenhouse effect, make the temperature even higher (1/2). At extremely high temperatures, photosynthesizing organisms could not survive (1), leading to the accumulation of volcano-sourced carbon dioxid ...
MSWord file
MSWord file

... Raising global temperature would put more water vapour into the atmosphere (1/2) and, through the greenhouse effect, make the temperature even higher (1/2). At extremely high temperatures, photosynthesizing organisms could not survive (1), leading to the accumulation of volcano-sourced carbon dioxid ...
What are Earth`s Systems
What are Earth`s Systems

... electrical forces, or bonds, in an arrangement called a molecule. Each hydrogen atom shares its electron with the oxygen atom creating a bond between the atoms.  Vapor. This form of water has no shape or cohesion. It is created when water molecules are heated to such a fast and furious movement tha ...
ch 7 study guide Answers
ch 7 study guide Answers

... A mid-ocean ridge is a mountain chain found on the ocean floor. It is formed at a divergent boundary where plates are separating. The magma is pushing up through the plate boundary causing the plates to move away from each other. The youngest rock is found at the mid-ocean ridge. The rock get older ...
the File
the File

... America "fit" together. Structural, fossil and mineral evidence seemed to support Wegener's Continental Drift Theory but it was not accepted by the scientific community. In the 1960's, scientists began to realize that there might be a connection between continental drift, earthquakes and volcanoes. ...
IgPetLab6
IgPetLab6

Document
Document

... • What force could move continents? • Studies of the ocean floor in the 2 decades following WWII led to the development of the plate tectonic theory ...
A Brief History of Planetary Science
A Brief History of Planetary Science

... Venus revolves around the Sun with a period of 225 days ...
Tectonic plates - Hobbs High School
Tectonic plates - Hobbs High School

Volcano Case Studies
Volcano Case Studies

Mtg01
Mtg01

... Notice how the temperature in the vertical varies systematically defining the troposphere, the stratosphere, the mesosphere and the thermosphere. The troposphere ends when the temperature ceases to decrease with increasing height, at the so-called tropopause. The temperature ceases to decrease in th ...
Plate Tectonics Review Sheet
Plate Tectonics Review Sheet

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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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