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ES Chapter 10 Notes
ES Chapter 10 Notes

... - similar fossils were found on inter-locking continents EX. 1: Mesosaurus was found in South America and in Africa. It never could have crossed the Atlantic Ocean, so it must have been able to walk between the two continents. Therefore, they must have been connected. EX. 2: Glossopteris (fossil fer ...
Student Notes
Student Notes

... - A force of erosion in the development of continental drainage systems. - Glaciers move materials towards the oceans. Origins of Ocean Water: How was the water in the ocean formed? - Oceans formed 3 billion years ago. - Outside of Earth cooled but the inside remained hot. - Water trapped in volcani ...
Quiz 4
Quiz 4

... 12. According to the diagram above, which of the following plates is all oceanic crust? A) North America B) Africa C) Nasca D) South America E) Eurasian 13. According to the diagram above, which of the following is the largest plate? A) Pacific B) Africa C) Nasca D) South America E) Eurasian 14. The ...
6th Grade Science Sample Assessment Items S6E3c.
6th Grade Science Sample Assessment Items S6E3c.

... elements plus others combine to form the salts in the oceans. Which of the following sources is a major source of calcium and sodium in oceans? A. gases from active volcanoes B. weathering and erosion of rocks* C. pollutants from industrial wastes D. acid rain caused by air pollution ...
Clouds - the Elementary Science Teachers Wiki!
Clouds - the Elementary Science Teachers Wiki!

... River 1. Flood water causes redeposit of silt to flood plain- Go to Soil 2. Sediments form- Go to Soil 3. Water washes away layers- Go to Mountains 4. Ice melts carrying rocks- Go to River 5. Silt washed into ocean- Go to Ocean 6. Sediments under pressure- Go to Earth’s Interior ...
18.3 - Faculty Perry, Oklahoma
18.3 - Faculty Perry, Oklahoma

... divergent boundary occurs where tectonic plates move apart convergent boundary occurs where tectonic plates push together transform boundary occurs where tectonic plates scrape past each other rift valley a gap formed between two diverging plates magnetic reversal when Earth’s magnetic north and sou ...
Plate Tectonics PowerPoint
Plate Tectonics PowerPoint

...  According to this hypothesis, continents have moved slowly to their current locations.  He suggested that all continents once were connected as one large landmass that broke apart about 200 million years ago.  Pangaea ...
Plate Tectonic Theory
Plate Tectonic Theory

... oceanic and continental-type crusts discussed in the next section. Asthenosphere. The upper reaches of the mantle are not solid; they are considered plastic and flow very slowly. This is due to the reduction in pressure as we approach the top of the mantle- the rocks are more likely to begin to melt ...
Where did the water for the oceans come from?
Where did the water for the oceans come from?

...  Earliest direct evidence for voyaging was from the Mediterranean. There may well have been intentional or unintentional ocean travel previous to that time.  The origins of marine science lie in voyaging – traveling on the ocean for a purpose, which varied form one culture and time to another. Tec ...
File - Varsity Field
File - Varsity Field

... • What mistakes did Alfred Wegener make in formulating his theory of continental drift? Do you think the geologists of his era were justified in rejecting his theory? • Why are there active volcanoes along the Pacific coast in Washington and Oregon but not along the east coast of the United States? ...
Document
Document

... continental drift from acceptance by the majority of scientists, particularly those in the northern hemisphere. ...
Practice Questions: Plate Tectonics
Practice Questions: Plate Tectonics

... B) Mesosaurus came into existence on several widely separated continents at different times. C) The continents of South America and Africa were joined when Mesosaurus lived. D) The present climates at locations X and Y are similar. 17. Which statement best supports the theory of continental drift? A ...
Plate Tectonics: A Unifying Theory
Plate Tectonics: A Unifying Theory

... Similarities exist between plant fossils on the southern continents. Glossopteris is the most conspicuous example of a unique flora in India, South Africa, Australia Similar glacial evidence also exists on these southern continents The southern supercontinent was named Gondwana ...
Group Quiz Review Game
Group Quiz Review Game

... 2a. It contains the oldest rocks known. 3a. It is located where magma rises to the surface of the oceanic crust. 4a. It creates composite volcanoes from the melting of low-density crust. 5a. It is the longest mountain chain in the world, but most of it is under water. 6a. They intersect mid ocean ri ...
Study Guide: Plate Tectonics Test
Study Guide: Plate Tectonics Test

... To prepare for the test, please review your notes, graphic organizers, homework worksheets, and look over PowerPoint lectures on Continental Drift, Plate Tectonics Theory, Sea Floor Spreading, Plate Boundaries. 1. Wegener’s Continental Drift Theory was based on the idea that the continents had once ...
Plate Tectonics Study Guide
Plate Tectonics Study Guide

... Physics of the Earth CP – Plate Tectonics / Geologic Age Test Study Guide Test Date: ___________ ...
Cross section of the Earth
Cross section of the Earth

... have been wrinkled & bent to make mountains and valleys. The thinnest parts of the crust are under the oceans; the thickest parts are in mountainous regions on the continents.  The Mantle is the layer under the crust. It is a very thick layer of red-hot solid rocks; some of these rocks are so soft ...
EPSS 15 Introduction to Oceanography – Spring 2017 Physiography
EPSS 15 Introduction to Oceanography – Spring 2017 Physiography

... 3. Abyssal plains are found near some "Atlantic" type continental margins where sediments from turbidity currents have flowed off the continental rise and spread out over the ocean floor producing extremely flat stretches of the ocean floor. Other features include seamounts (hills >1 km above the oc ...
platetectonics
platetectonics

... (youngest) layer is lava flows. The same three layers are in the same order in areas now separated by great distances. Wegener proposed that the rock layers were made when all the continents were part of Pangaea. Thus, they formed in a smaller contiguous area that was later broken and drifted apart. ...
SEA FLOOR SPREADING Mid
SEA FLOOR SPREADING Mid

... ocean floor sinks beneath a deep-ocean trench and back into the mantle. ...
9-4 Sea Floor Spreading
9-4 Sea Floor Spreading

... What is the evidence for sea floor spreading? Evidence of sea floor spreading includes molten material, magnetic stripes, and evidence from drilling samples Where would the oldest rocks in the ocean floor be found? The oldest rocks would be found the farthest away from the MOR. ...
PowerPoint
PowerPoint

... portions of subducting plates melt and form molten magmas that rise to the surface in mountain belt volcanoes, carrying CO2 and other gases from Earth’s interior to it’s atmosphere. ƒ At the margins of divergent plates (ocean ridges), where hot magma carrying CO2 erupts directly into ocean water. ...
The two major areas of the ocean floor are the and the
The two major areas of the ocean floor are the and the

... 5. Explain why it is summer in Australia (southern hemisphere) when it is winter in California (northern hemisphere): ...
Notes # ______ Sea Floor Spreading Mid Ocean Ridge underwater
Notes # ______ Sea Floor Spreading Mid Ocean Ridge underwater

... shaped like ​ pillows​  or ​ squeezed­out toothpaste​  in the central valley of mid­ocean ridges.  These rock formations only form when ​ magma erupts underwater and hardens very quickly​ ...
Chapter 33 Plate Tectonics
Chapter 33 Plate Tectonics

... – The continents are slowly moving – All the continents has once been attached in a supercontinent and this was called Pangaea “all land” – Pangaea split and the continents moved apart – The boundary of each continent is not at the shoreline but the continental shelf ...
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Geological history of Earth



The geological history of Earth follows the major events in Earth's past based on the geologic time scale, a system of chronological measurement based on the study of the planet's rock layers (stratigraphy). Earth formed about 4.54 billion years ago by accretion from the solar nebula, a disk-shaped mass of dust and gas left over from the formation of the Sun, which also created the rest of the Solar System.Earth was initially molten due to extreme volcanism and frequent collisions with other bodies. Eventually, the outer layer of the planet cooled to form a solid crust when water began accumulating in the atmosphere. The Moon formed soon afterwards, possibly as the result of a Mars-sized object with about 10% of the Earth's mass impacting the planet in a glancing blow. Some of this object's mass merged with the Earth, significantly altering its internal composition, and a portion was ejected into space. Some of the material survived to form an orbiting moon. Outgassing and volcanic activity produced the primordial atmosphere. Condensing water vapor, augmented by ice delivered from comets, produced the oceans.As the surface continually reshaped itself over hundreds of millions of years, continents formed and broke apart. They migrated across the surface, occasionally combining to form a supercontinent. Roughly 750 million years ago, the earliest-known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia, 600 to 540 million years ago, then finally Pangaea, which broke apart 180 million years ago.The present pattern of ice ages began about 40 million years ago, then intensified at the end of the Pliocene. The polar regions have since undergone repeated cycles of glaciation and thaw, repeating every 40,000–100,000 years. The last glacial period of the current ice age ended about 10,000 years ago.
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