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Chapter 20 The Precambrian Record
Chapter 20 The Precambrian Record

... perform specialized tasks are called __________. 57. Disk or frond-shaped fossil impressions of late Proterozoic age found represent the __________ ________. 58. Late Proterozoic locomotion is indicated by ______ __________ of crawling animals. 59. The first appearance of hard skeletal fossils is re ...
Chapter 7
Chapter 7

... zones and Arctic clues in tropical zones • Similar rock structures found on different continents ...
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THE DYNAMIC CRUST There are 4 major sub

... flat lying, horizontal layers called strata Observations show this Law is commonly violated 1. Anticlines & Synclines - folded rock strata - anticlines are upfolds while synclines are downfolds - folding occurs after the rocks formed horizontally 2. Tilted Strata - rock layers found to be resting a ...
PDF - Rosemont EIS
PDF - Rosemont EIS

... The moet ancient rocks, tbe Pinal Schist and Continental Granodiorite, show effects of the Mazatzal Revolution, which are typical of central Arizona. Alternating upward and downward epeirogenic movements throughout the Paleozoic Era are recorded hy a marine sequence whose continuity is interrupted b ...
Project 6: Reindeer Lake North (SE Quarter) Area Reconnaissance
Project 6: Reindeer Lake North (SE Quarter) Area Reconnaissance

... Migmatit e (6c) is similar to unit 6b except that the paleosome is predominantly rich in xenoliths of metasedimentary gneisses as well as diorite to amphibolite probably derived from rocks of unit 3. ...
North Cascades National Park (10 May)
North Cascades National Park (10 May)

... Arc complex in British Columbia (now offset along the Eocene Fraser Fault). It is uncertain whether they developed on the oceanic rocks of the Bridge River plate, but were likely part of the Insular Belt by late Jurassic time. The rock is metamorphosed at amphibolite facies. This stop illustrates th ...
Geological Glossary - The Old Courthouse Museum Batemans Bay
Geological Glossary - The Old Courthouse Museum Batemans Bay

... volcano: A vent in the earth's crust from which molten lava and pyroclastic material is erupted, also the mountain built up by the accumulation of these rocks. volcanic arc: A chain of volcanic islands adjacent to a continent, generally with a deep oceanic trench on the ocean facing side and a margi ...
Unit 2 Review and Solutions
Unit 2 Review and Solutions

... • Buildings are often built out of steel that can bend and contort as an earthquake shakes • Also the foundations of buildings are built on shocks to absorb the shaking • Lastly building are not built out of rigid concrete as they cannot withstand shaking ...
Plate Tectonics - Gull Lake Community Schools
Plate Tectonics - Gull Lake Community Schools

... Hawaii were formed. ...
Plate Tectonics - Faculty Perry, Oklahoma
Plate Tectonics - Faculty Perry, Oklahoma

... lithosphere is broken into plates that move over time. ...
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57. Practice reading seismographs: Can You Read a Quake?

... A hot spot is a mantle plume that weakens the lithosphere over it until at times the magma find vents and fissures to the surface and creates a volcano. If enough lava is released from the volcano it may produce enough new igneous rock in the area to rise above the surface of the ocean. The lithosph ...
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Which way*s up?

... are on a surface that tilts to the North at about 25 degrees. ...
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File - GEOLOGY ROCKS!

... Geologic Provinces of North Carolina Great Smoky Mountains 600 million year old sandstones & shales ...
Earth`s Interior
Earth`s Interior

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Word format

... Joints can be found in most rocks. They generally open by no more than ________________________. They often form dense networks that leave rocks intensely fractured. Joints are useful because they can tell us about the stresses that produced them. Joints form ____________________ to the direction of ...
Historical Geology
Historical Geology

... a. spreading centers are extensional b. transform boundaries are regions of crustal shearing c. convergent boundaries are dominated by compression. 2. different geologic structures are commonly associated with each type of boundary a. divergent boundaries produce normal faults, grabens, little or no ...
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1. The Earth system 1.1. introduction 1.2. Earth structure and plate

... process of rock transformation is called metamorphism. Rocks caught in subduction zones or between two colliding continents are subject to tremendous changes in temperature and pressure causing rock metamorphism (regional metamorphism). In addition, wherever rocks are in contact with magma, these ro ...
Marcie wanted to compare the lengths and masses of some different
Marcie wanted to compare the lengths and masses of some different

... number of fish that can be harvested from a stock of fish so that the population remains healthy enough to continue reproducing. Fish harvested from a fishery for a restaurant would be classified as a __________ resource. A. nonrenewable B. renewable C. scientific D. depleting ...
Mineral Resources and Geology
Mineral Resources and Geology

... c. Occurs when one plate passes under another. d. Occurs when oceanic plates diverge and form volcanoes. ...
Geomorphology Final Exam Study Guide
Geomorphology Final Exam Study Guide

... – steep linear bluff – Relief formed solely by movement • Fault-line scarp – Relief caused by differential erosion along fault • Composite scarp – Combination of the 2 above • Mountain landforms – Horst – Graben • Forms basin & range Within the Basin and Range Province, the Earth’s crust has been st ...
Midterm Review 1
Midterm Review 1

... Rocks can be metamorphosed (changed) into other rocks when subjected to high temperatures and pressures. The presence of fluids increases the rate of metamorphism Metamorphic changes occur in the solid state The three kinds of metamorphism are Regional, Contact and Hydrothermal Regional metamorphism ...
Michela Griffin
Michela Griffin

... that occur along faults where one rock mass slides past another one ‘Mysterious, sudden, and violent’ Worst death toll occurs in cities with poorly constructed buildings Most seismically active region in the U.S. is along the west coast where tectonic plates are colliding ...
The French Massif Central is the south-vergent
The French Massif Central is the south-vergent

... while metatexites in the core with an assemblage biotite + fibrolite + cordierite(?) are up-grade from the muscovite-out isograd and indicate temperatures over 650 C. The metamorphic grade also increases from east to west in Le Caroux. Unfortunately, the low-Al bulk composition of these rocks does ...
NAME - KCSE Online
NAME - KCSE Online

... (ii) How sedimentary rocks are formed through physical processes. - Pre-existing rocks of sedimentary and igneous types undergo weathering and erosion. - The weathered and eroded rock materials are then transported and deposited over the land or in the sea / ocean by wind, water or ice. - The deposi ...
Progressive Metamorphism P-T
Progressive Metamorphism P-T

... however, and in these glaucophane is developed (giving way to hornblende at higher grades) – Rocks are commonly called blueschists ...
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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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