semester plan

9
HOW IS A FOSSIL FORMED? 1. Sediment An animal is buried by sediment, such as volcanic ash or silt, shortly after it dies. Its bones are protected from rotting by the layer of sediment. 4. Erosion Erosion from rain, rivers, and wind wears away the remaining rock layers. Eventually, erosion or people digging for fossils will expose the preserved remains. 2. Layers More sediment layers accumulate above the animal’s remains, and minerals, such as silica (a compound of silicon and oxygen), slowly replace the calcium phosphate in the bones. 3. Movement Movement of tectonic plates, or giant rock slabs that make up Earth’s surface, lifts up the sediments and pushes the fossil closer to the surface.

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Semester Plan. Geologic Time Meteorology Astronomy Oceanography. How do scientists know the age of the rocks? How has life changed over time?. Chapter 10 Clues to Earth’s Past. EQ: How do scientists know the age of the rocks? . Fossils . - PowerPoint PPT Presentation

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Page 1: Semester Plan

HOW IS A FOSSIL FORMED?

1. SedimentAn animal is buried by sediment, such as volcanic ash or silt, shortly after it dies. Its bones are protected from rotting by the layer of sediment.

4. ErosionErosion from rain, rivers, and wind wears away the remaining rock layers. Eventually, erosion or people digging for fossils will expose the preserved remains.

2. LayersMore sediment layers accumulate above the animal’s remains, and minerals, such as silica (a compound of silicon and oxygen), slowly replace the calcium phosphate in the bones.

3. MovementMovement of tectonic plates, or giant rock slabs that make up Earth’s surface, lifts up the sediments and pushes the fossil closer to the surface.

Page 2: Semester Plan

FIVE MAIN TYPES OF FOSSILS

PetrifiedFossils

Molds andCasts

CarbonFilms

TraceFossils

PreservedRemains

Page 3: Semester Plan

Relative age

• Age of rocks and geologic features compared with other rocks and features nearby

Page 4: Semester Plan

10.3 Absolute age dating

Page 5: Semester Plan

Relative vs. Absolute Age Dating

Relative• Determines ages of rocks in

order that they were formed but without exact dates

Absolute• Determine absolute date of

the rock

Page 6: Semester Plan

Radiometric dating• Isotopes = atoms of the

same element that have the same number of protons but different number of neutrons

Page 7: Semester Plan

Carbon-14 dating• Radioactive decay: Some isotopes are

unstable, emit radiation and decay into “daughter” isotope– Carbon-14 is unstable isotope and decays into

nitrogen-14

• Over time: – The amount of “parent” isotope, carbon-14,

decreases– The amount of “daughter” isotope, nitrogen-14,

increases– The ratio of the two indicates the age of the rock

• Half life: time required for half of parent isotope to decay into daughter isotopes– E.g. Half life of carbon 14 is approx. 5730 years

Page 8: Semester Plan

Types of dating

• Radiocarbon dating: organic material (bones, wood, charcoal)

• Rock dating: living tissues replaced by minerals (e.g. U 235 Pb-207)

Page 9: Semester Plan

Types of dating

• Radioactive dating game• Quiz next class