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List 1 fact about Earth. Agenda for Monday Nov 22 nd 1.Finish Movie 2.Layers of the Earth notes
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Layers of Earth
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Crust Thin, solid, outermost 1% of Earth’s mass Oceanic crust: crust beneath oceans Continental crust: makes up the continents – Less dense
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Mantle Layer under the crust 2,900 km thick Solid and becomes more liquid
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Core Center Outer Core = liquid layer Inner Core = solid layer
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Earth’s Interior Earth’s interior gets warmer with depth Radioactive elements contribute to high internal temp – Nuclei break up, release energy
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What are the layers of Earth? Agenda for Tuesday Nov 23 rd 1.Continental Drift
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Wegener’s Hypothesis Continental drift – Earth’s surface is made up of large moving plates – Proposed by Alfred Wegener
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Evidence for Continental Drift Fossil Evidence: fossils of the same plants and animals are found where continents were connected
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Evidence for Continental Drift Rock Formations Evidence: ages and types of rocks on coasts of widely separated areas match
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Evidence for Continental Drift Climatic Evidence: changes in climate suggests the continents have not always been where they are now Temp. is affected by where the continents are located – Study geologic past and see change in temps.
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How did the continents move? Wegener thought the continents moved through the ocean floor This was disproved by other geologist
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Sea Floor Spreading Geologist Harry Hess suggested if the sea floor is moving, the continents might be moving also Sea-floor spreading - sea floor forms as magma rises to Earth’s surface and solidifies at a mid- ocean ridge Rocks closer to mid-ocean ridge are younger than rocks farther away
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Paleomagnetism Paleomagnetism - study of magnetism in rocks Magnetic poles reverse in an alternating pattern – Helps determine the age and that the rock forms in the middle
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How Plates Move plate tectonics - explains how large pieces of the lithosphere, plates, move and change shape Continents and oceans are carried on moving tectonic plates Scientists have identified about 15 major plates – studying data from earthquakes and volcanoes
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How Plates Move Convection – Heat rises and cool sinks – Hot material rises through asthenosphere (portion below lithosphere)
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Why doesn’t the earth grow in thickness?
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Convergent Boundary
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The Supercontinent Movement of plates toward convergent boundaries causes continents to collide Happened about 250 million years ago – End of the Permian – mass extinction – Supercontinent Pangaea (Pangea)
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The Supercontinent Pangea 250 million years ago Broke up into 2 continents – Gondwanaland - Africa, South America, India, Australia, and Antarctica – Laurasia - North America and Eurasia Slowly over the last 250 million years moved to where they are today
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Future 50 million years
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Future + 150 million years
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Future + 250 Million Years
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3 types of plate movement Divergent – move apart Convergent – come together Transform – plates slide past each other
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Homework Read 705 – 717 Questions 1 – 6 on page 708 Questions 1-3, 5, & 6 on page 717
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List the 3 types of plate boundaries Agenda for Monday Nov 29 th 1.Plate Boundaries 2.Go over Homework 3.Relative and Absolute Age
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Recall 3 Types of Plate Boundaries – Divergent – Convergent – Transform
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Divergent Plates move apart – Creates a gap – New Earth is created – sea floor spreading – Mid oceanic ridge
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Convergent Plates come together – 1 plate slides under the other – subduction Densities – Subduction of ocean crust generates volcanoes Volcanic mountains – Colliding tectonic plates create mountains
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Transform Plates slide past each other – Crack created is called a fault – Causes earthquakes
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Earthquakes Occur at all plate boundaries Richter scale
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Volcanoes Convergent plate boundaries Underwater volcanoes occur at divergent plate boundaries
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