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Notes: Ocean Floor
Notes: Ocean Floor

... •What type of plate boundary make deep oceanic trenches? ________________________ •Where is sediment carried by rivers deposited in our oceans? ______________________ •What type of plate boundary is located at mid-ocean ridges? _______________________ •How does Earth’s climate effect the sea level? ...
Continental Drift and Plate Tectonic
Continental Drift and Plate Tectonic

... What were points of contention with the Theory of Continental Drift? How did the Theory of Plate Tectonics affirm the Theory of Continental Drift? ...
Sea-Floor Spreading
Sea-Floor Spreading

... Hess devised a theory called sea-floor spreading which states that at mid-ocean ridges, molten material rises from the mantle and erupts. It then spreads out, pushing older rock to both sides of the ...
Plate Tectonics - Holy Angels School
Plate Tectonics - Holy Angels School

... • About 245 million years ago, the continents were joined in a single large landmass called Pangaea. • About 200 million years ago, a large rift formed and Pangaea began to break into two continents, Laurasia and Gondwana. • Then, Laurasia began to drift northward, and a new rift separated Laurasia ...
Dynamic Ocean Floor
Dynamic Ocean Floor

... Fossils of glossopteris; a tree - like plant from the Permian Period and dominant plant of Gondwana are found throughout India, South America, southern Africa, Australia, and Antarctica. ...
Richard Bailey “How Did Continents Begin?”  COLLOQUIUM
Richard Bailey “How Did Continents Begin?” COLLOQUIUM

... is so young, why the continents drift. But there are problems which plate tectonics sensu strictu does not solve. Why did a continental collision make Tibet so high? Why is their such massive lateral extension visible in the Basin and Range province of the US? How can plate subduction start, given t ...
File
File

... together in a single large land mass he called Pangea (meaning “all land” in Greek). • He proposed that Pangea had split apart and the continents had moved gradually to their present positions - a process that became known as continental drift. ...
Final Plate Tectonics Review
Final Plate Tectonics Review

... over 250 million years ago the continents were one big landmass that eventually drifted over time to the positions they are today ? Continental drift theory ...
Unit Six Notes
Unit Six Notes

... Transform Fault Boundary  The plates may move in opposite directions or in the same directions but at different rates and frequent earthquakes are created (example: San Andreas Fault) ...
Chapter 17- Plate Tectonics
Chapter 17- Plate Tectonics

... • Early mapmakers noticed the apparent fit of continents on either side of ocean (matching coastlines) • Continental drift (Wegener)- Earth’s continents had once been joined as Pangaea ...
Introduction to Plate Tectonic Theory
Introduction to Plate Tectonic Theory

... layer is made up of plates, which have moved throughout Earth's history. The theory explains the how and why behind mountains, volcanoes, and earthquakes. ...
Key to Investigation 2: Plate Tectonics
Key to Investigation 2: Plate Tectonics

... By dating the age of the lavas at hot spots, and measuring how far apart they are from each other, scientists can determine the rate and direction of plate movement. 5a. These two ranges are the results of the subcontinent of India colliding with the southern coast of Asia about 40 – 50 million yea ...
Notes: The Theory of Plate Tectonics
Notes: The Theory of Plate Tectonics

...  Expanding Earth idea…In the beginning the Earth’s _________ was evenly _________ over the ____________ ... but got stretched and thinned when the _________ expanded forming the ocean __________.  But, ocean _________ are too wide to have formed by any reasonable __________.  Contracting Earth id ...
Plate Tectonics Vocabulary
Plate Tectonics Vocabulary

... forms between two tectonic plates that are pulling away from each other the region where one ...
Evolution of the Ocean Basins
Evolution of the Ocean Basins

... meters below sea level) over most of their ...
sea-floor spreading
sea-floor spreading

... The pattern of "stripes" or anomalies is symmetrical around the oceanic ridge. The youngest oceanic rocks are near the ridges with the oceanic rocks becoming older as they move away from the ridge. The black stripes represent rocks that cooled under "normal" conditions and are normally polarized, wh ...
File
File

... theorized that Pangaea divided into two supercontinents 205 million years ago. Du Toit called the northern supercontinent Laurasia and the southern one Gondwanaland. ...
Chapter 33
Chapter 33

... shorelines of South America and the western shoreline of Africa fit like a puzzle – Alfred Wegener proposed that all continents had once been one big land mass • Pangaea – supercontinent that once existed • Broke into several large pieces ...
Continental Drift - CoconinoHighSchool
Continental Drift - CoconinoHighSchool

... geological sequences with rocks of similar age, type, formation and structure occurring in different countries - e.g. the Appalachians (E. USA) show a geological match with mountains in NW Europe and if they were fitted together would form a single ...
8.1 Earth has several layers
8.1 Earth has several layers

... no where else ...
Continental Drift
Continental Drift

... geological sequences with rocks of similar age, type, formation and structure occurring in different countries - e.g. the Appalachians (E. USA) show a geological match with mountains in NW Europe and if they were fitted together would form a single ...
Chapter 8 Plate Tectonics With Video
Chapter 8 Plate Tectonics With Video

... years; the last one was 780,000 years ago. ...
Theory Development
Theory Development

... Pangaea Theory – claimed that the continents had formed a single landmass, which split apart. Wegener was not the first to suggest that the continents had been one, but was the first to present evidence from several fields. 1912 - Continental Drift Theory – Wegener noticed that there were similar gl ...
Structure of the Earth
Structure of the Earth

... mantle are separated into plates. Plates float on the mantle. ...
LESSON 5 - PANGEA STAGE ONE: Lesson is designed to be taught
LESSON 5 - PANGEA STAGE ONE: Lesson is designed to be taught

... which position they take. Inform the students that existence of Pangaea generally accepted by most scientists. After discussion elaborate on the evidence identified by students and discuss any that was left out. One prominent example of continental coastline fitting together is to fit the coastline ...
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Pangaea



Pangaea or Pangea (/pænˈdʒiːə/) was a supercontinent that existed during the late Paleozoic and early Mesozoic eras. It assembled from earlier continental units approximately 300 million years ago, and it began to break apart about 175 million years ago. In contrast to the present Earth and its distribution of continental mass, much of Pangaea was in the southern hemisphere and surrounded by a super ocean, Panthalassa. Pangaea was the last supercontinent to have existed and the first to be reconstructed by geologists.
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