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Do now: Read 4.2.

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Presentation on theme: "Do now: Read 4.2."— Presentation transcript:

1 Do now: Read 4.2

2 You will learn to explain seafloor spreading.
Module F: 4.2 Seafloor Spreading Objectives: You will learn to explain seafloor spreading. You will learn to recognize how age and magnetic clues support the theory of seafloor spreading.

3 Clues on the Ocean Floor
- invention of ____________________ allowed the construction of accurate maps of the ______ floor - using sound waves, researchers discovered an ___________ system of _______, or __________, and valleys like those found on the ____________ echo-sounding devices ocean underwater ridges mountains continents

4 Seafloor Spreading!!! Harry Hess
- Early 1960s: __________ proposed this theory - the idea that _______ from Earth’s _______ rises to the surface at mid-ocean ridges and cools to form new ________, which new magma slowly pushes away from the ridge magma mantle seafloor

5 Evidence for Seafloor Spreading!!!
1. Age Evidence __________________ ____________ 2. Magnetic Clues

6 1. Age Evidence - there were no rocks older than ___________ years, however, some ___________ rocks are almost _________ years old - youngest rocks were at _________________ - age of rocks became ______ farther from the ridges on both sides 180 million continental 4 billion mid-ocean ridges older

7 2. Magnetic Clues - magnetic data is recorded by a ______________
- rocks on the ______ floor showed magnetic reversals - the magnetic alignment of the rocks reverses back and forth in strips ________ to the mid-ocean ______ magnetometer ocean parallel ridge

8

9 LET’S REVIEW! The invention of _____________ allowed the construction of accurate maps of the ocean floor. What are mid-ocean ridges? Who discovered the idea of seafloor spreading? What is a trench? When is one formed? What two pieces of evidence proved the theory of seafloor spreading to be correct?

10 Homework!!! Read section 4.2 and do questions #1-5 Due Wednesday
Notes Packet due Thursday Study for 4.2 quiz Thursday


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