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Minerals, Rocks and Resources
Minerals, Rocks and Resources

Name
Name

... 16. What is humidity? What is the difference between low and high humidity? What is humidity? Humidity is the amount of water in the air. What is the difference between low and high humidity? Low has less water in the air relative to what it can hold at that temperature. High is the opposite. 17. W ...
Mountain Building
Mountain Building

... • Form as a result of tensional stress – At divergent boundaries or above subduction zones. ...
1 - Net Start Class
1 - Net Start Class

... 39. Sediment-Weathered material 40. Loess-Wind blown sediment; causes wind erosion 41. Rain Shadow-Dry area on the leeward side of a mountain range; all the moisture is trapped on the windward side 42. Convection- Precipitation created by heated, humid air rising high into the atmosphere where it co ...
the course overview
the course overview

... formation of rocks. You will also examine the properties of such minerals, the technologies used to extract them, and the impact of the exploitation of such materials. Some other topics to be covered are: - The investigation of sedimentary, metamorphic, and igneous rocks. - The role of Earth materia ...
Natural Disasters
Natural Disasters

... • An avalanche is a sudden rapid flow of snow down a slope, occurring when either natural triggers or human activity causes a critical escalating transition from the slow equilibrium evolution of the snow pack. • Typically occurring in mountainous terrain, an avalanche can mix air and water with the ...
Time - Research School of Earth Sciences
Time - Research School of Earth Sciences

Mars Tectonics & Volcanology
Mars Tectonics & Volcanology

... • Larger calderas than the tholi • Probably represent larger volcanoes • Buried beneath flows and sediment ...
Benchmark 3 Study Guide
Benchmark 3 Study Guide

The solid, outer layer of Earth that consists of the crust and the rigid
The solid, outer layer of Earth that consists of the crust and the rigid

Basic Geology
Basic Geology

... Heat and pressure are produced by various processes, including but not limited to tectonic activity, deep burial, and contact with magma. shale is transformed to slate or schist, sandstone to quartzite, and limestone to marble gneiss forms when an intrusive magma cools next to igneous or sedimentary ...
Powerpoint 1
Powerpoint 1

... Relative dating uses the Law of Superposition to estimate the age of an artifact or fossil. Absolute dating uses the amount of radioactive substances in an artifact or fossil to determines its age more precisely. Discussion? ...
Mini Task SC.7.E.6.5
Mini Task SC.7.E.6.5

Volcano Notes 6.0
Volcano Notes 6.0

(granite) and the deep
(granite) and the deep

... They differ from continents because they have no margins. ...
Plate Boundaries Handout
Plate Boundaries Handout

... The “hot spot” is an area of magma (called a plume) that has risen up and broken through the lithosphere, erupting on the surface ...
press release,
press release,

... the atmosphere and tend to be evenly distributed around the globe, aerosols vary greatly in local concentration and tend to be found near emission sources such as industrial centers in Asia and North America. Moreover, Human  activities  have  increased  atmospheric  concentrations   aer ...
Name - sfox4studentteacher
Name - sfox4studentteacher

... currents are caused by the heat in the core to increase the temperature of material in the m_______________. The hot material in the mantle rises to the c____________________ while the cooler material sinks towards the core. This causes p______________ t__________________________, or movement of Ear ...
File - Thomas Tallis Science
File - Thomas Tallis Science

... the features of the Earth’s surface were the result of the shrinking of the crust as the Earth cooled down following its formation. The Earth’s crust and the upper part of the mantle are cracked into a number of large pieces (tectonic plates). Convection currents within the Earth’s mantle, driven by ...
Inside the Earth, Why do the plates move?
Inside the Earth, Why do the plates move?

plate tectonics and california geology - FOG
plate tectonics and california geology - FOG

Atmosphere - Spring Branch ISD
Atmosphere - Spring Branch ISD

... into space to avoid temperature extremes in order to support life. ...
Plate Boundaries - Learn Earth Science
Plate Boundaries - Learn Earth Science

... of plates that ride on top of the asthenosphere • The plates move due to convection currents in the mantle ...
Plate Boundaries
Plate Boundaries

... of plates that ride on top of the asthenosphere • The plates move due to convection currents in the mantle ...
CRCT Review Warm Ups
CRCT Review Warm Ups

... B. cool material rises, heats up, and sinks C. dense material sinks until it comes to rest. D. dense material rises and then begins to sink ...
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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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