Geologists examine time in two ways:
Today in class we will discuss how to figure out the relative sequence of events, using the following principles:
The oldest layer of sedimentary and extrusive igneous rocks is always at the bottom
Sedimentary and extrusive igneous rocks are originally laid down in horizontal layers and any change from that is viewed as a disturbance of those layers (something happened later) - folding, tilting (occur during mountain-building events, for example)
sedimentary and igneous extrusive rocks that are folded or tilted must have first been deposited in horizontal layers before being folded or tilted
Anything that cuts across a layer must have happened after that layer was already there. This principle is used in three instances:
This activity involves understanding the vastness of geologic time by taking the geologic events listed on p.173 and placing them into different metaphors for time. To fit into the metaphors, calculations must be done - a calculator would be helpful today. The geologic time scale with its absolute dates is presented on p.170.
Read through these notes and look over the activities in your manual to get a feel for the material covered this week. Read the material in your manual for each activity with care so that you understand what you missed, talk to a classmate to find out more. Contact Dr. Munn to arrange to make up the quiz that you missed (this must be done sometime before the next class). Worksheets collected for this lab will be listed on the Lab Schedule page and must be turned within a week. Click here for the syllabus information about missing class. Worksheets collected for this lab will be listed on the Lab Schedule page and must be turned within a week. Here are more specifics about the worksheets that were collected: