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EPS050 – Review for Midterm 1 (Fall 2009)
EPS050 – Review for Midterm 1 (Fall 2009)

... 16. What
is
the
difference
between
a
pyroclastic
flow
and
a
lava
flow?
How
does
SiO2
 content
factor
into
these
differences?
Where
are
pillow
basalts
formed?
How
are
 shield
 and
 strato‐volcanos
 distinguished
 in
 terms
 of
 eruptive
 style
 and
 general
 ...
Chapter 3: Mountains, Coast and Shelf
Chapter 3: Mountains, Coast and Shelf

... Broad alluvial fans have built up at the base of slopes backing the coastal plain. Gravelly material has accumulated on subtle fans or aprons where streams exit from the hills; the sediments gradually become finer down slope (see sketch). It is believed that the main valleys and the coastal plains b ...
Welcome to Mrs. Thompson`s 5th Grade Class
Welcome to Mrs. Thompson`s 5th Grade Class

... molten rock cools and solidifies. • Molten rock is called magma when it is below the Earth’s surface and lava when it is above. ...
2007 Exam 1 - MSU Billings
2007 Exam 1 - MSU Billings

... A) a divergent plate boundary. B) an ocean-ocean convergent boundary. C) an ocean-continent convergent boundary. D) a continent-continent convergent boundary. 13. Which is not a fine-grained rock type? A) granite B) andesite C) basalt D) rhyolite 14. Fragments of country rock surrounded by igneous r ...
Chapter 8 Test Review Notes
Chapter 8 Test Review Notes

... Only a portion of the North American craton is visible because the rest has been buried beneath other materials. ...
our Chocolate Geology outdoor learning resource
our Chocolate Geology outdoor learning resource

... Using the globe: What is geology? It is the study of the origins of the earth, its history and what it is made of. The earth looks like a solid mass. But is it? Using the cross section diagram we can look at the composition of our planet. Talk about the interesting facts of each layer. The Inner Cor ...
UNIT 2 INTERNAL ENERGY AND LANSFORMS The movement of
UNIT 2 INTERNAL ENERGY AND LANSFORMS The movement of

... Fluvial landforms: rain and rivers are the basic agents. Water and vegetation cause chemical weathering of the rocks. Erosion and transportation take place in the upper course, a steep slope in a mountain. Sediments are transported and sedimented in the middle-lower course. In the mouth of the river ...
8-3 Unit HW Sheet Name: Date: Standard 8
8-3 Unit HW Sheet Name: Date: Standard 8

... 11. What is the movement, position, speed, and state of matter it travels through of a Secondary wave? Up and Down at right angles to the primary wave/2nd to leave/Slower than the P waves/Only travel through solids 12. Which seismic wave is the fastest wave and which wave stops at the outer core-Ex ...
Microsoft Word - 2011 KCSE NDTHIWA GEO P1.DOC - KCPE-KCSE
Microsoft Word - 2011 KCSE NDTHIWA GEO P1.DOC - KCPE-KCSE

... (ii) Identify & describe three plate tectonic boundaries. (6mks) Extension boundary. This is a boundary created when plates move away from each other resulting from tensional forces. Compressional boundary. This is a boundary created when plates crush against each other resulting from compressional ...
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... Earthquakes can cause landslides, the downhill movement of large amounts of rock and soil. Earthquakes under the ocean can cause a tsunami, waves large enough to destroy things when they crash into a coastline. ...
Rocks and Minerals - Georgia Standards
Rocks and Minerals - Georgia Standards

... Sedimentary, igneous, metamorphic, rock composition, mineral formation, pressure, rock cycle, Minerals can be identified by their physical properties. Igneous rocks are dominated by silicate minerals. Rocks are composed of minerals. Minerals are the building blocks of rocks. The rock cycle explains ...
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY

... Lithospheric Plate Boundaries: Volcanism? Earthquakes? Which boundary type? Convergent: (# of types? Give examples and description of landforms possible) Subduction Zone surface/topographic Features Divergent ( # of types? Description/Examples) Topographic features? ...
Structure of the Earth Study Guide with Answers
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... 31) What is the lithosphere? THE CRUST AND THE TOP RIGIDE PART OF THE MANTLE – TECTONIC PLATES ARE MADE OF IT 32) What happens to density as you get closer to the core? IT INCREASES THE CLOSER YOU GET 33) What are all of the layers made out of? CRUST = SOLID ROCK, MANTLE = MOLTEN ROCK, OUTER ...
Activity: Classifying Igneous Rocks
Activity: Classifying Igneous Rocks

... Which three (besides obsidian) have the most quartz? Which 6 are volcanic? Which 3 are plutonic? Which 3 cooled slowly beneath the surface? Which are the two most common types of igneous rocks? Which one is the Boulder Batholith made of? (recent notebook entry may help) Which one is the Columbia Pla ...
chapter 6 Metamorphic Rks.pptx
chapter 6 Metamorphic Rks.pptx

... –  Low-grade metamorphism- 200 to 350 OC and relatively low pressures –  Intermediate-grade metamorphism - 350 to 550 OC and moderate to high pressures –  High-grade metamorphism - very high temperatures, usually above 550OC and/or very high pressures ...
2. Geologic History Agenda Physical Geographers Intro to Calif
2. Geologic History Agenda Physical Geographers Intro to Calif

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8 Geology Revision
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... Words: pressure from sediment above, limestone, minerals in water, coal, conglomerate, sandstone, claystone, shale. Mudstone. a. Erosion is the movement of rocks and/or weathering products by water, wind, ice or gravity down the slope and also by living organisms. b. What is the difference between w ...
How Do Geologists Classify Rocks?
How Do Geologists Classify Rocks?

... http://www.indiana.edu/~g103/G103/ wk3/wk3.html site on rocks with crystallization demo (need 3-D glasses for one section) http://www.youtube.com/watch?v=fC GrXtdSv2c ...
How Do Geologists Classify Rocks?
How Do Geologists Classify Rocks?

... http://www.indiana.edu/~g103/G103/ wk3/wk3.html site on rocks with crystallization demo (need 3-D glasses for one section) http://www.youtube.com/watch?v=fC GrXtdSv2c ...
11th Grade Earth Science
11th Grade Earth Science

... Sedimentary Rocks: How do they form? Know the following terms: weathering, erosion, deposition, lithification, cementation, compaction ...
Constructive and Destructive Forces
Constructive and Destructive Forces

... • A volcano is an opening in the Earth's surface or crust, which allows hot, molten rock, ash and gases to escape from deep below the surface. • Volcanic activity involving the extrusion of rock tends to form mountains or features like mountains over a period of time. ...
Constructive and Destructive Forces
Constructive and Destructive Forces

... • A volcano is an opening in the Earth's surface or crust, which allows hot, molten rock, ash and gases to escape from deep below the surface. • Volcanic activity involving the extrusion of rock tends to form mountains or features like mountains over a period of time. ...
Constructive and Destructive Forces
Constructive and Destructive Forces

... • A volcano is an opening in the Earth's surface or crust, which allows hot, molten rock, ash and gases to escape from deep below the surface. • Volcanic activity involving the extrusion of rock tends to form mountains or features like mountains over a period of time. ...
File
File

...  Over billions of years, some elements will change into other elements  In 4.5 billion years, half of a mass of _________________will change into lead which will not change  The uranium is called the parent __________________.  This time period is called the half-life of uranium  Radiometric Da ...
Chapter 2 - MrJardina
Chapter 2 - MrJardina

... over long periods of time.  The squeezing removes the water and leaves behind the carbon that makes up the coal. Jardina-Conelway Elementary ...
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Provenance (geology)



Provenance in geology, is the reconstruction of the history of sediments movements over time. The Earth is not a static but a dynamic planet, all rocks are subject to transition between the three main rock types, which are sedimentary, metamorphic, and igneous rocks (the rock cycle). Rocks exposed to the surface, sooner or later, are broken down into sediments. Sediments are expected to be able to provide evidence of the erosion history of their parent source rocks. The purpose of provenance study is to restore the tectonic, paleo-geographic and paleo-climatic history.
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