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Daily Review #1 What happens in radioactive decay? Define half-life.

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Presentation on theme: "Daily Review #1 What happens in radioactive decay? Define half-life."— Presentation transcript:

1 Daily Review #1 What happens in radioactive decay? Define half-life.
The element chaparralium has a half-life of 24,000 years. If a fossil contains 25% of the original amount of chaparralium, how old is this fossil? Explain how you arrived at this answer. What do you think happened to create the rock in this picture?

2 Relative vs. Absolute Dating
Definition Example Relative Order of events X is older/younger than Y Less specific Three major techniques

3 Law of Superposition What order were the layers of the cake put down?
How are rocks similar? Oldest… Youngest… When layers are horizontal

4 What if the layers aren’t horizontal?

5 Principle of Horizontality
Rock forms layers horizontally If not horizontal Happened after rock cooled Folding Caused by pressure

6 Cross-Cutting Occur after rocks form Faults Caused by earthquakes
Shift rock layers

7 Cross-Cutting cont. Intrusions Magma invades cracks Cools into rock

8 Tell the rock’s story…

9 Mapping Interior No drilling past crust Seismographs Earthquakes
Wave speed effected by density and thickness Study times to pick up seismic waves

10 Composition of Earth 3 layers Crust Based on compounds present
Density differences Crust Outermost 5-100 km Thinnest layer Types Continental Oceanic

11 Mantle Middle layer 2900 km thick Never visited Conclusions based on
Observations on Earth surface Pushes to surface Oceanic volcanoes

12 Core Center Radius of 3430 km Mostly Fe, some Ni 1/3 of Earth’s mass
Very little O, Si, Al, Mg 1/3 of Earth’s mass

13 Physical Structure Lithosphere Asthenosphere Solid, outer layer Crust
Upper mantle Asthenosphere Solid, slow flowing rock Mantle

14 Outer core Liquid layer Inner core Center Solid, dense

15 Daily Review #2 Tell the rock’s story…
Review quiz – make corrections

16 Plate Tectonics Plates Divisions of lithosphere Moving on
asthenosphere Plate Tectonics

17 Wegener – Continental Drift Theory
Early 1900s Once single landmass - Pangaea Broke up – Laurasia, Gondwana Drifted to present location

18 Daily Review #3 Put in order of age: Gondwana, Pangaea, South America
Sketch the layers of the Earth and label the asthenosphere, lithosphere, outer core, inner core, mantle and crust Fill in the boxes on your layers of the Earth worksheet Composition = if it contains any specific elements (you will not fill this in for all boxes) Thickness = rank from thinnest to thickest

19 Continental Drift Evidence
For Wegener Fitting together of continents Similar things on distant continents Fossils Rocks

20 How would you explain this evidence?

21 Sea-Floor Spreading Evidence for continental drift Mid-ocean ridges
Tectonic plates moving separating New magma rises Form new oceanic crust Older crust pushed away

22 Magnetic Reversals Evidence for continental drift Molten rock
Magnetic minerals Align with magnetic field Magnetic field reverses 177 times in 85 million years Last 600,000 years ago Recorded in rock Similar pattern to age of rocks

23 Causes for Plate Tectonics
Convection Cools Asthenosphere More dense Heated rock Expands and rises

24 New material pushed up at ridges Subduction zone
Pushes older material away Subduction zone Denser plate sinks Pulls rest of plate


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