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Week 2 Essential Reading
Week 2 Essential Reading

6.E.2.3- Questions and Answers -Worksheet
6.E.2.3- Questions and Answers -Worksheet

... rodents, and other organisms. The upper-most layer of the continental crust is covered by soil.The ingredients in soils can vary from place to place and around the Earth. Different soils have many properties such as texture, particle size, pH, fertility and ability to hold moisture. Depending upon t ...
Structural Geology Introduction/Review of Basic Principles
Structural Geology Introduction/Review of Basic Principles

... 1. Process of metamorphism involves transformation of pre-existing rock (ig. sed. or even met.) under temperature and/or pressure. Result in change in both composition/mineralogy; and texture of rock as well. 2. The "grade" or degree of metamorphism ranges from slight (low grade) e.g. >compaction; t ...
File - Earth Science
File - Earth Science

... small and large pieces called plates that are continuously but very slowly moving on the very hot rocks below it. These hot rocks constitute the athenosphere of the earth. ...
UNIT 5 Text: Where to Look for Petroleum Grammar Revision
UNIT 5 Text: Where to Look for Petroleum Grammar Revision

... 5. Certain features of ancient glaciations have been explained by some scientists on the basis of changes in the position of poles. 6. Mountain climate is more influenced by the elevation than by any other factor. 7. Strong submarine earthquakes are followed by seismic waves, technically called tsun ...
continental drift and plate tectonics
continental drift and plate tectonics

C2 Key Facts Sheet - North Leamington School
C2 Key Facts Sheet - North Leamington School

... - This increases the nitrate/phosphate levels in rivers. - This causes algae to bloom (grow uncontrollably.) - This blocks off sunlight to other plants which die. - Aerobic bacteria thrive and use up the oxygen. - This causes most fish and other aquatic animals to die. To prepare a fertiliser in a l ...
Layers PangaeaCont drift Convection
Layers PangaeaCont drift Convection

Tour of Plate Boundaries
Tour of Plate Boundaries

... explore these Tectonic Landscapes and put into “realworld” context what we have learned in class. ...
Archaean Crustal Evolution Protocontinents to Microcontinents
Archaean Crustal Evolution Protocontinents to Microcontinents

... time was formed by volcanic activity, either from hot spots or subduction zones. Continents, even small ones, are still a distance in the future. ...
Metamorphic rocks
Metamorphic rocks

... temperature and pressure (usually deep within the Earth). The extreme temperature and pressure conditions cause the atoms in existing minerals to rearrange (or change form). ...
Prezentace aplikace PowerPoint
Prezentace aplikace PowerPoint

... One of the things we are very interested in is how close the sediment has gotten along its path of evolution. This is the concept of sediment maturity. Thus, above the arkosic and lithic fields, but below the quartz field are two more fields, subarkosic and sublithic. Rocks in these fields have bet ...
Chapter 7 Answers
Chapter 7 Answers

... 16. Wegener’s theory was unaccepted at first because there was no scientific evidence to support the theory and scientists could not conceive of any force able to move continents. Evidence that supports continental drift includes the discoveries of the same plant and animal species found on both sid ...
Igneous rocks
Igneous rocks

- Lake Fenton Community School District
- Lake Fenton Community School District

the significance of the volcanic rocks in the fossil creek area, arizona
the significance of the volcanic rocks in the fossil creek area, arizona

... NEW MEXICO GEOLOGICAL SOCIETY O THIRTEENTH FIELD CONFERENCE ...
C1b 6.2 The restless earth
C1b 6.2 The restless earth

... 1) Scientists discovered 50 years later that the Earth generates massive amounts of heat through radioactive decay in the core. This heat generated convection currents in the mantle causing the crust to move 2) We also now know that the sea floor is spreading outwards from plate ...
Catastrophic Granite Formation Rapid Melting of
Catastrophic Granite Formation Rapid Melting of

Performance Benchmark N
Performance Benchmark N

... A. Volcanoes and earthquakes are found in similar regions or zones around Earth. There is a large concentration of these two events along the west coast of North and South America extending around the Pacific Ocean – Ring of Fire. Geologic events such as earthquakes and volcanoes are most often foun ...
Earth Space Science - Laconia School District
Earth Space Science - Laconia School District

... a little), a stream that has a mudslide come through it might become more of a river, and then from there maybe even turn into a small lake or pond. An earthquake can change the ocean floor because if the floor moves then the water gets misplaced or unbalanced. This then can cause a tsunami. When ro ...
Plate Tectonics Study Guide KEY The Earth started off as a molten
Plate Tectonics Study Guide KEY The Earth started off as a molten

... surface or is deflected off to the side, where it slides along under the crust/lithosphere. When the rock cools, it becomes more dense and drops towards the core again. Then the cycle repeats. 27. Tell how the currents move the pieces of the crust around on the surface of the Earth. ...
EmilyB
EmilyB

... Most earthquakes have been occurring around mainly Japan, China, Indonesia, Malaysia, and much around eastern Asia. Also many have occurred around the Ring of Fire. Most earthquakes are more likely to occur at plate boundaries. The plates smash and grind against each other sometimes causing earthqua ...
June 2003
June 2003

Plate Tectonics
Plate Tectonics

... 2. Sea Floor Spreading ...
Handout 2.3-2 Standard 2 Objective 3.a, b, d, and e
Handout 2.3-2 Standard 2 Objective 3.a, b, d, and e

... 1. The major mountain belts are located along • B. convergent plate boundaries. ...
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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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