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Grade: 3rd Activity #: 1 Activity Title: Studying Rocks and Minerals
Grade: 3rd Activity #: 1 Activity Title: Studying Rocks and Minerals

... Minerals must occur naturally. This means man-made substances such as steel would not be considered to be minerals. Inorganic substances are those substances that are not living and are not formed by living processes. Minerals will have definite chemical compositions, but these compositions ...
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... erupts and then cools down quickly on the Earth’s surface or at the bottom of the oceans.. Volcanic rocks often have got cavities in them, produced by gas. These are called bubbles or vesicles ...
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Restless Continents
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... About 245 million years ago, all of the continents were joined into a single supercontinent. This supercontinent was called Pangaea. The word Pangaea means “all Earth” in Greek. About 200 million years ago, Pangaea began breaking apart. It first separated into two large landmasses called Laurasia an ...
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Compositional symmetry between Earth`s crustal building blocks
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... and helps to define our unique place in the solar system (Allègre, 1997; Taylor and McLennan, 2009). Despite isotopic evidence that suggests the Archean depleted mantle source (at least by 3.8 Ga) was likely similar to today (Vervoort and Blichert-Toft, 1999), the mechanisms driving the production a ...
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... 
the
sediments
deposited
during
the
orogeny.
The
Antler 
foredeep
(between
the
thrust
front
and
the
miogeocline) 
records
the
sediments
derived
from
the
mountain
building 
event
that
occurred
as
the
deep‐water
sediment
overrode 
the
shallow
sediments.
 In
the
foredeep,
we
see
both
sediments
derived
 ...
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... lakes. The sound of the explosion could be heard as far away as Canada. Giant mudflows raced down the mountain into local rivers destroying bridges, vehicles and houses. The sound of the explosion could be heard as far away as Canada. Mount St. Helens is one of the Cascade Volcanoes that reach from ...
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Volcanism and volcanic rocks

... lakes. The sound of the explosion could be heard as far away as Canada. Giant mudflows raced down the mountain into local rivers destroying bridges, vehicles and houses. The sound of the explosion could be heard as far away as Canada. Mount St. Helens is one of the Cascade Volcanoes that reach from ...
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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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