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8 - Balbharatipp.org
8 - Balbharatipp.org

... Q1. What is the difference between weathering and erosion? Weathering is the breaking up of the rocks on the earth’s surface. Erosion is the wearing away of the landscape by different agents like water, wind, and ice. Q2. What are endogenic and enogenic forces? The forces which act in the interior o ...
SuperVolcanoQuestions
SuperVolcanoQuestions

... 3. Yellowstone would be classified as this category of volcano: a. Extinct b. Dormant c. Active d. Living 4. Yellowstone is in the middle of a plate rather than at an edge. A volcano occurring in this location is explained by this phenomenon of tectonic plates. a. subduction b. hot spot c. divergent ...
Ohio`s Learning Standards Rocks and Minerals Objectives
Ohio`s Learning Standards Rocks and Minerals Objectives

... deposition - the settling out or placement of rock, particles of rock, or organic matter, generally referred to as sediments, after transportation by wind, water, ice, or gravity. ...
Rocks
Rocks

Chapter 8 Study Guide
Chapter 8 Study Guide

... 43. Oceanic crust is always subducted under continental crust because it is more dense 44. Hawaii is not located on a plate boundary, but it is the most volcanically active place in the world due to a hot spot 45. How do volcanoes provide evidence of plate tectonics? Happen along with earthquakes on ...
Volcanic Activity
Volcanic Activity

... Cascade Range (Washington, Oregon, northern California), or on the islands of Hawaii. The Hawaiian Islands represent an exception to the rule that Pacific volcanoes are located along the boundary of the oceanic plate. Volcanoes located within the interiors of plates are typically the result of volca ...
File
File

Powerpoint for today
Powerpoint for today

... Earth's surface heated by Sun. What would happen if it couldn't get rid of the energy as fast as it gets in? ...
Igneous Rock Classification Lab
Igneous Rock Classification Lab

... Extrusive – magma solidifies above the Earth’s surface •magma cools very fast •minerals can not be seen with un-aided eye •very fine-grained texture (no visible minerals •referred to as Volcanic rocks ...
IGCSE Physical Geography
IGCSE Physical Geography

... An earthquake is the vibration of the Earth’s crust caused by shock waves travelling outwards from sudden movement deep within the crust. The source is the focus which is directly below the epicentre on the surface. Shockwaves are measured on a seismograph which measures the magnitude on the Richter ...
Metamorphic_Rocks
Metamorphic_Rocks

12earth6s
12earth6s

... Just the moon parts ...
Review Sheet
Review Sheet

... Explain convection currents & how they are related to density. List plate boundary information by: plate type (O-O, O-C, C-C); formations that are made there; plate names involved; & specific examples around the world. 7. List some sources of material for continental growth. 8. How do coal deposits ...
EGU2008-A-05921 - Copernicus Meetings
EGU2008-A-05921 - Copernicus Meetings

16_terrestrials_student
16_terrestrials_student

... Result: Earth is the ONLY world to have stratovolcanoes, because it’s the only world to have plate tectonics ...
Chapter 17 Study Guide Answers
Chapter 17 Study Guide Answers

... • The Atlantic Ocean is expanding because 4 plates form a divergent boundary in the middle of the ocean. This is causing the seafloor to spread apart. The Pacific Ocean is shrinking because the Pacific Plate is surrounded by convergent plate boundaries that have subduction. Basically the Pacific Oce ...
Quiz 1 Rocks and Plates
Quiz 1 Rocks and Plates

... Cooler, older, oceanic lithosphere sinks into the mantle at ________. A. subduction zones along convergent plate boundaries B. transform fault zones along divergent plate boundaries C. rift zones along mid-ocean ridges D. sites of long-lived, hot spot volcanism in the ocean basins A transform plate ...
The formation of mountains 1) Fold mountains Complete
The formation of mountains 1) Fold mountains Complete

... _______________ _________________ mountains are formed when two of the Earth’s plates move ______________. The middle section of rock is pushed _____________. This block is then ___________ by the wind and water to create a familiar mountain shape. ...
Chapter 2 Physical Geography: A Living Planet
Chapter 2 Physical Geography: A Living Planet

... rock created by weathering (mud, sand or silt) v. Mechanical Weathering – processes that break rock into smaller pieces (doesn’t change the composition of rock, but the size) example: road construction ...
Ch. 7 Plate Tectonics Section 1 Inside the Earth
Ch. 7 Plate Tectonics Section 1 Inside the Earth

... The process of ridge push, convection, and slab pull provide some possible driving forces for plate tectonics.  Convection is the hot material deep within the Earth rising to cool. ...
Geology Test08
Geology Test08

... present location of part of the Hawaiian Island chain. These volcanic islands may have formed as the Pacific Plate moved over a mantle hot spot. This diagram provides evidence that the Pacific Crustal Plate was moving toward the ...
Document
Document

... …….work just the same as boiling up some pea soup! ...
Planet Earth
Planet Earth

... This is the name of the molten rock found deep below the earth’s crust? ...
seismic waves
seismic waves

... where large quantities of magma move to the surface in large, column-like plumes – Can occur away from plate boundary – When under a oceanic plate, volcanic island chains forms ...
third quarter - New Haven Science
third quarter - New Haven Science

... 1. Earth’s surface features, such as mountains, volcanoes and continents, are the constantlychanging result of dynamic processes and forces at work inside the Earth. 2. Earth is formed of three basic layers, with the densest being the iron and nickel core. The middle layer, the mantle, of the Earth ...
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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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