Presentation is loading. Please wait.

Presentation is loading. Please wait.

ordering of rock layers.

Similar presentations

Presentation on theme: "ordering of rock layers."— Presentation transcript:

1 ordering of rock layers.
Standard 8-2.6 Infer the relative age of rocks and fossils from index fossils and the ordering of rock layers.

2 Name and give 3 facts about the main 3 types of rocks.
Falcon Focus Name and give 3 facts about the main 3 types of rocks.

3 What is the law of superposition?
ESSENTIAL QUESTION What is the law of superposition?

4 Objective FF EQ Intro to Law of Superposition Take Notes
Brief Review for Fossil Quiz Take Fossil Quiz Closure Note: Mosby points are due tomorrow!!!

5 Finding the Relative Age of Rocks
Standard – Infer the relative age of rocks and fossils from index fossils and the ordering of the rock layers.

6 Extra Question Which is most likely to become a fossil?
A. a skeleton in a large lake B. a jellyfish in the ocean C. an earthworm in a damp forest D. a skeleton in a riverbed that is drying up

7 Essential Question Explain how the law of superposition can be used to determine the relative ages of rocks.

8 The relative age means the age of one object compared to the age of another object. Relative age does not tell the exact age of an object. The relative age of rocks and fossils can be determined using two basic methods: ordering of rock layers and index fossils:

9 Relative and Absolute Ages
Relative Age The age of a rock compared to the ages of rock layers. Ex: younger vs. older Absolute Age The age of a rock given as the number of years since the rock formed. Ex: 10, 20, 50, 100

10 Position of Rock Layers
Its difficult to determine the absolute age so geologists use methods to find a rock’s relative age. Use the: LAW OF SUPERPOSITION: in horizontal sedimentary rock layers, the oldest layer is at the bottom. Each higher layer is younger than the layers below it.

11 Other Clues to Relative Age
Clues from Igneous Rocks: 1. Lava that hardens on the surface is called an Extrusion (example – an eruption would put a layer of igneous rock on top of sedimentary rocks. Rock layers below an extrusion are always older than the extrusion.

12 The extrusion is in black

13 Now the extrusion is the youngest layer.

14 Clues from Igneous Rocks:
2. Magma that cools and pushes into bodies of rock and hardens is called an Intrusion An intrusion is always younger than the rock layers around and beneath it.

15 The intrusion (in red) is now younger than the surrounding rocks.

16 Draw this in your notes and label each of the parts listed below.
Intrusion Extrusion Oldest rock Youngest rock Understand that these are all rocks that are millions of years old. You can use the color pencils I have provided. Which one would you draw first?


18 Fault: is a break in the Earth’s crust.
Clues from Faults: Fault: is a break in the Earth’s crust. Forces inside the Earth cause movement of the rock on opposite sides of a fault. Fault is always younger than the rock it cuts through. Movements along faults can make it harder for geologists to determine the relative ages of rock layers. (book figure 10 B)



21 `

22 REVIEW Geologists use the Relative and Absolute
Age of rocks to determine age. Using the Law of Superposition Other clues are from Igneous rocks Extrusion Intrusion Clues from Faults

- Record of sedimentary rock layers is not always complete - Deposition slowly builds layers upon layer of sedimentary rock, BUT some of these layers may erode away, exposing an older rock surface. Unconformity – is a gap in the geologic record. An unconformity shows where some rock layers have been lost because of erosion.

To date rock layers, geologists first give a relative age to a layer of rock at one location. THEN they can give the same age to matching layers of rock at other locations. Certain fossils, called Index Fossils help geologist match rock layers. INDEX FOSSILS – Fossils of widely distributed organisms that lived during only one short period.




28 Index Fossils Certain fossils, called index fossils, can be used to help find the relative age of rock layers. To be an index fossil – an organism must have lived only during a short part of Earth’s history; many fossils of the organism must be found in rock layers; the fossil must be found over a wide area of Earth; the organism must be unique.

29 The shorter time period a species lived, the better an index it is
The shorter time period a species lived, the better an index it is. A key example of an organism used as an index fossil are trilobites, a group of hard-shelled animals whose body had three sections, lived in shallow seas, and became extinct about 245 million years ago. Therefore, if a trilobite is found in a particular rock layer, it can be compared with trilobites from other layers to estimate the age of the layer in which it was found.

30 Fossils that are found in many rock layers, therefore living long periods of time, do not qualify as index fossils.

31 Example of an Index Fossil:
Trilobites (hard shelled animals whose bodies had three distinct parts. Trilobites evolved in shallow seas more than 500 million years ago. Over time, many types have appeared. They became extinct about 245 million years ago. They have been found in many different places.


33 To become a Index Fossil … a trilobite must be different in some way from other trilobites.
Example – type with large eyes These large-eyed ..bites survived for a time AFTER other bites became extinct. If a geologist finds large-eyed Trilobites in a rock layer, the geologist can infer that those rocks are younger than rocks containing other types of trilobites

34 The World's Biggest Trilobite
A team of Canadian paleontologists working along Hudson Bay in northern Manitoba has discovered the world's largest recorded complete fossil of a trilobite, a many-legged, sea-dwelling animal that lived 445 million years ago. The giant creature is more than 70 cm long (about 28 inches), 70 percent larger than the previous record holder. "This is an important and amazing find," says Bob Elias, a professor in the department of geological sciences at the University of Manitoba. "It looks like a huge bug!"

Download ppt "ordering of rock layers."

Similar presentations

Ads by Google