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Background Information
Background Information

... Almost everyone who has experienced an earthquake has been awed by the ability of the seemingly solid ground to move. From daily micro-quakes to massive tremors that drastically alter the landscape, California is home to one of the most active and researched fault zones in the world. The San Francis ...
G19-1pow
G19-1pow

... * pg. 529 ...
Earth
Earth

... a. Formed from another rock by heat and pressure. b. Usually form beneath the earth’s crust (which means they often heat up and become magma again—it’s a cycle—the Rock Cycle!) c. Fact: Both igneous and sedimentary rocks can change into metamorphic rocks. d. Characteristics: These rocks are usually ...
9 Geography Investigating Australia`s Physical Environments Term 1
9 Geography Investigating Australia`s Physical Environments Term 1

... crustal rocks buckle as one plate slides under another (subduction). Some of the crust is forced down and becomes part of the magma; other rocks are forced upwards and bent or folded. ...
geologic highlights of southeastern arizona and vicinity
geologic highlights of southeastern arizona and vicinity

... Mountains, called the Mogollon Highlands, begin to build up in southern Arizona, as great quantities of granitic magma intrude the crust of western North America. Some molten rock erupts onto the Earth’s surface, e.g., 20,000 feet of volcanic rock in the Santa Rita Mountains. These high volcanic pea ...
Emma Wilson Extra Credit #3 Unit 1: 1. Which of the following does
Emma Wilson Extra Credit #3 Unit 1: 1. Which of the following does

... kingdom, astronomy is the study of the stars, and geology is the study of the earth. 3. Geologists had predicted a hurricane would hit the Gulf of Mexico and warned many decades prior to Hurricane Katrina. A. True B. False This statement is true. Geologists find out where dangerous areas are and war ...
Rocks - Macmillan Learning
Rocks - Macmillan Learning

... Fig. 3.11a ...
Section 19.1 Forces Within Earth
Section 19.1 Forces Within Earth

... • This type of strain produces permanent deformation. ...
Agents of Metamorphism
Agents of Metamorphism

... Tarbuck and Lutgens Pages 48 - 49 ...
Sedimentary rocks are composed of
Sedimentary rocks are composed of

... Sedimentary rocks are composed of: Clasts vs. Matrix Gilbert’s Mineralogical Classification Figure 5.5 ...
EPS050 – Review for Midterm 1 (Fall 2009)
EPS050 – Review for Midterm 1 (Fall 2009)

... 24. What
is
the
composition
(name)
of
typical
volcanic
rocks
erupted
at
a)
divergent
 plate
 boundaries,
 b)
 and
 island
 arc
 where
 two
 oceanic‐plates
 meet,
 c)
 a
 convergent
boundary
where
the
volcanic
arc
is
on
a
continent?
 ...
Earth Revealed #10: Geologic Time
Earth Revealed #10: Geologic Time

... 7. What kind of conditions exist for the formation of gold, silver and copper (in other words, how do they form)? ...
Paper Number: 2077 - American Geosciences Institute
Paper Number: 2077 - American Geosciences Institute

... India consists predominantly of tectonic slices representing various units of ancient ocean-floor rocks that include the ultramafic body (main ophiolite suite), mafic dykes and sills, pillow lavas, kindred rocks and pelagic sediments in a jumbled manner. The assembly of these different tectonic slic ...
The Earth An Intimate History R.Fortey August 18
The Earth An Intimate History R.Fortey August 18

... reference to Euler and the sphere, but wherein that actually consists is left as a mystery. Rigid motions along a sphere is mathematics, and the understanding of which is essential to the appreciation of tectonic movement. So what does the author present instead of mathematics? Diversions. Historic ...
INDUSTRIAL MINERAL POTENTIAL OF THE TERTIARY ROCKS
INDUSTRIAL MINERAL POTENTIAL OF THE TERTIARY ROCKS

... control their deve,lopment, in a southeasterly trending area extending 150 kilometres from east of Kamloops (921) through the Vernon map area (82L) to north of Beaverdell (82E). In this area, the industrial minerals of major interest are kaolinite, diatomaceous earth, swelling clay, zeolites. perlit ...
Document
Document

... • Metamorphism means “to change”. • Metamorphic rocks arise from the transformation of existing rock types. • The original rock is subjected to heat (temperatures greater than 150 to 200 °C) and pressure (1500 bars), causing profound physical and/or chemical change. • Through heat and pressure an ig ...
Metamorphic_Rocks
Metamorphic_Rocks

... Recrystallization: This is the growth of new mineral crystals from other rocks. ...
Metamorphic Rocks
Metamorphic Rocks

... Regional Metamorphism – both heat and pressure change rock on a grand scale; this usually occurs during major tectonic events such as mountain building ...
Faults Folds and Mountains
Faults Folds and Mountains

... Axial plane near axis should be close to horizontal ...
Science 8—Chapter 13 Vocab PP Less 2 Quiz
Science 8—Chapter 13 Vocab PP Less 2 Quiz

... • the natural process that moves sediments from place to place ...
CEE 437 Lecture 1
CEE 437 Lecture 1

... • Origins in late 18th and early 19th Centuries • Catastrophism and Uniformitarianism – Age of Earth – Uniformity of Processes ...
magma
magma

... a. Formed from another rock by heat and pressure. b. Usually form beneath the earth’s crust (which means they often heat up and become magma again—it’s a cycle—the Rock Cycle!) c. Fact: Both igneous and sedimentary rocks can change into metamorphic rocks. d. Characteristics: These rocks are usually ...
Section Quiz - TheVirtualNeal
Section Quiz - TheVirtualNeal

... C D Folded mountain ranges form when two tectonic plates with continental crust collide. The crust is forced upward at the point of collision, which forms mountains over a long period of time. ...
The Geologic Time Scale
The Geologic Time Scale

... ages of most of the rocks on Earth’s surface. Over many years, geologists have used rock formations to develop a time scale that divides geologic time into units. The geologic time scale (pages 668–669) is a summary of major events in Earth’s past that are preserved in the rock record. Although seve ...
Rocks and Minerals
Rocks and Minerals

... Figure 4.18. Types of magmatic intrusions ...
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Algoman orogeny



The Algoman orogeny, known as the Kenoran orogeny in Canada, was an episode of mountain-building (orogeny) during the Late Archean Eon that involved repeated episodes of continental collisions, compressions and subductions. The Superior province and the Minnesota River Valley terrane collided about 2,700 to 2,500 million years ago. The collision folded the Earth's crust and produced enough heat and pressure to metamorphose the rock. Blocks were added to the Superior province along a 1,200 km (750 mi) boundary that stretches from present-day eastern South Dakota into the Lake Huron area. The Algoman orogeny brought the Archaen Eon to a close, about 2,500 million years ago; it lasted less than 100 million years and marks a major change in the development of the earth’s crust.The Canadian shield contains belts of metavolcanic and metasedimentary rocks formed by the action of metamorphism on volcanic and sedimentary rock. The areas between individual belts consist of granites or granitic gneisses that form fault zones. These two types of belts can be seen in the Wabigoon, Quetico and Wawa subprovinces; the Wabigoon and Wawa are of volcanic origin and the Quetico is of sedimentary origin. These three subprovinces lie linearly in southwestern- to northeastern-oriented belts about 140 km (90 mi) wide on the southern portion of the Superior Province.The Slave province and portions of the Nain province were also affected. Between about 2,000 and 1,700 million years ago these combined with the Sask and Wyoming cratons to form the first supercontinent, the Kenorland supercontinent.
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