Presentation is loading. Please wait.

Presentation is loading. Please wait.

The Relative Age of Rocks

Similar presentations


Presentation on theme: "The Relative Age of Rocks"— Presentation transcript:

1 The Relative Age of Rocks

2 Why do sedimentary rocks have layers?
The sediments (particles of sand, rocks, etc) is deposited in flat layers one of top of the other. Over time, the sediment hardens and changes into sedimentary rock.

3 What is an unconformity?
An unconformity is a gap in the geological rock record. It is a surface of rock where new rock layers meet a much older rock surface beneath them. Erosion or weathering has removed part of the rock, causing this area to be an “unconformity”.

4 What characteristics must a fossil have in order to be useful as an index fossil?
An organism that was widespread geographically, but was around during a relatively short period of time can be classified as an “index fossil. (p.329)

5 Using Fossils to Date Rocks!
Scientists use index fossils to match rock layers. An index fossil must be widely distributed and represent a type of organism that existed only briefly. They are useful because they tell the relative ages of the rock layers they are found in.

6 The Trilobite One example of an index fossil is a trilobite.
Trilobites were a group of hard-shelled animals whose bodies had three distinct parts. They evolved in shallow seas more than 500 million years ago.

7 Absolute versus Relative Age
Absolute age is the age in years. Relative age is comparing two rock layers without giving an actual date. Paleontologists use both when dating rocks and the fossils within them. (p329)

8 Ages of Rocks The relative age of a rock is its age compared to other rocks. Use words like: “older or younger” The absolute age of a rock is the number of years since the rock was formed. Ex: mya

9 Law of Superposition The Law of Superposition states that in horizontal sedimentary rock layers, the oldest layer is at the bottom.

10 The Position of Rock Layers
It can be difficult to determine a rocks absolute age. So… scientists use the law of superposition. According to 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 A geologist finds a cliff where the edges of several different rock layers can be seen. Which layer is the oldest? Explain. The layer on the bottom is the older. The Law of Superposition states that older rock is under younger rock, if the rock layers have not been disturbed.

12 Other Clues to Relative Age
Clues From Igneous Rock Lava that cools at the surface is called an extrusion. Rock below an extrusion is always older. Magma that cools beneath the surface is called an intrusion. An intrusion is always younger than the rock layers around an beneath it.


Download ppt "The Relative Age of Rocks"

Similar presentations


Ads by Google